INTELLIGENCE HANDBOOK(Classified) BRAZIL
Document Type:
Collection:
Document Number (FOIA) /ESDN (CREST):
CIA-RDP85-00671R000300020001-8
Release Decision:
RIPPUB
Original Classification:
S
Document Page Count:
331
Document Creation Date:
November 17, 2016
Document Release Date:
September 15, 1998
Sequence Number:
1
Case Number:
Publication Date:
February 1, 1968
Content Type:
REPORT
File:
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CIA-RDP85-00671R000300020001-8.pdf | 34.74 MB |
Body:
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No Foreign Dissem
RETIRED FILE
JOB 5-OO(i7j'R
BOX FOLDER 0 a
DESENSITIZED
DIRECTORATE OF
INTELLIGENCE
Inte11ience Handbook
BRAZIL
25X1A2g
February 1968
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WARNING
This document contains information affecting the national
defense of the United States, within the meaning of Title
18, sections 793 and 794, of the US Code, as amended.
Its transmission or revelation of its contents to or re-
ceipt by an unauthorized person is prohibited by law.
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_
mf
V
URUGUAY
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56826 10--67
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NO FOREIGN DISSEM
INTELLIGENCE HANDBOOK
25X6D
BRAZIL
SECRET
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CONTENTS
Page
Foreword ..........................................
xv
I.
Introduction ................................
1
II.
Historical Background ........................
5
A.
Chronology ..............................
5
B.
History
.................................
7
Reading List .................................
14
III.
Physical. Geography ...........................
15
A.
Introduction ............................
15
B.
Northern Region .........................
16
1. General ............................
16
2. Amazon Flood Plain .................
16
a. Terrain and Drainage ..........
16
b. Climate .......................
17
c. Vegetation ................. .
25X6D Land Use .............. .
20
3. Terra Firme ........................
a. Terrain and Drainage ..........
b. Climate .......................
c. Vegetation ....................
25X6D Land Use ......................
23
23
24
26
28
C. West-Central Region ..................... 30
1. General ............................ 30
2. Central Plateau .................... 31
a. Terrain and Drainage .......... 31
b. Climate ....................... 32
c. Vegetation .................... 32
2X6D Land Use ...................... 35
Pantanal .......................
Terrain and Drainage ..........
Climate .......................
Vegetation ....................
Land Use ......................
38
38
39
39
39
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e. Factors Affecting Land and Air
Operations .................... 40
D. Northeastern Region ..................... 42
1. General ............................ 42
2. Zona da Mata ....................... 42
a. Terrain and Drainage 42
b. Climate ........................ 43
c. Vegetation .................... 45
25X6D Land Use ....................... 45
3. The Agreste 47
a. Terrain and Drainage 47
b. Climate ........................ 48
c. Vegetation 50
25X6D Land Use ....................... 50
4. The Sertgo .......................... 53
a. Terrain and Drainage ........... 53
b. Climate ........................ 55
c. Vegetation ..................... 58
Land Use ....................... 58
5. Parnaiba - Mearim Area ..............
a. Terrain and Drainage ...........
b. Climate ........................
C. Vegetation .....................
256D Land use .......................
61
61
61
61
62
E. Eastern Region ........................... 64
1. General ............................. 64
2. Central Highland ................... 64
a. Terrain and Drainage ........... 64
b. Climate ....................... 67
c. Vegetation .................... 69
25X6D Land Use ...................... 69
3. Eastern Slope ...................... 70
a. Terrain and Drainage .......... 70
b. Climate ....................... 71
c. Vegetation .................... 75
26X6D Land Use ...................... 76
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4. Sao Francisco River Basin .......... 79
a. Terrain and Drainage ........... 79
b. Climate ....................... 81
c Vegetation .................... 81
25(6D Land Use ...................... 82
F. Southern Region ......................... 82
1. General ............................ 82
2. Southern Plateau ................... 83
a. Terrain and Drainage .......... 83
b. Climate ....................... 89
c. Vegetation .................... 90
25X6D Land Use ...................... 92
3. Eastern Slope ......................
a. Terrain and Drainage ..........
b. Climate .......................
c. Vegetation ....................
25X6D Land Use ......................
96
96
98
99
100
Gazetteer .................................... 104
Glossary ..................................... 109
Reading List ................................. 113
IV. Population ................................... 115
A. General ................................. 115
1. Size and Growth .................... 115
2. Distribution ....................... 115
3. Mobility ........................... 116
4. Settlement Patterns ................ 116
5. Demographic Terminology ............ 117
B. Composition ............................. 120
1. Color and Race ..................... 120
2. Immigrants ......................... 121
3. Indigenous Indian Groups ........... 126
4. Indian Culture Areas ............... 130
C. Language ................................ 130
D. Education ............................... 131
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E. Religion ............................... 134
F. Housing ................................ 139
G. Health ................................. 152
H. Occupations ............................ 157
I. Attitudes and Loyalties ................ 160
J. Insurgency Potential ................... 161
Reading List ................................ 182
V. Politics and Government ..................... 183
A. Current Problems ....................... 183
B. Structure of Government ................ 184
1. Central Government ................ 184
a. The Executive ................ 184
b. The Legislature .............. 186
c. The Judiciary ................ 187
2. State and Local Government ........ 187
C. Political Parties ...................... 188
D. Current Administration ................. 190
E. Foreign Relations ...................... 192
F. Subversion and Insurgency .............. 195
1. General ........................... 195
2. Brazilian Exile Groups ............ 196
a. Nationalist Revolutionary Move-
ment (MNR) ................... 197
b. Nationalist Armed Resistance
(RAN) 198
c. Other Exiles ........ .... 198
3. Brazilian Communist Party (PCB) ... 199
4. The Communist Party of Brazil
(CPB) ............. ........... 200
5. The Popular Action (Agao Popular -
AP) .............. ................ 201
6. Workers' Politics (POLOP) ......... 201
7. The Trotskyite Groups ............. 201
8. Paraguayan Exiles ................. 202
9. The Role of Cuba .................. 202
10. The Rightists ..................... 203
11. Recent Insurgency Incidents ..... 203
a. Rio Grande do Sul Guerrilla
Incident .......... ? ......... 203
b. The Serra do Caparad Guerrilla
Group ........................ 204
OR
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c. The Uberlandia Terrorist
Group ......................... 205
d. Itaucu Insurgency Group ....... 205
Reading List ................................. 207
VI. Economy ...................................... 209
A. General ................................. 209
B. Agriculture ............................. 210
C. Manufacturing ........................... 211
D. Fuels, Power, and Mining ................ 212
E. Investment, Finance, and Banking ........ 212
F. International Economic Relations ........ 213
G. Prime Economic Targets .................. 215
Reading List ................................. 216
VII. Transportation ............................... 217
A. General ................................. 217
B. Roads and Trails ........................ 217
1. Roads .............................. 217
a. Extent and Characteristics .... 217
b. Numbering Systems ............. 219
c. Regional Networks ............. 226
(1) Northeastern Region ..... 226
(2) Eastern Region .......... 227
(3) Southern Region ......... 228
(4) Northern and West-Central
Regions ................. 229
2. Trails ............................. 229
C. Railroads ............................... 231
1. Northeastern Region ................ 231
2. Eastern Region ..................... 232
3. Southern Region .................... 233
4. Northern and West-Central Regions 236
D. Inland Waterways ........................ 236
1. The Amazon and Its Tributaries ..... 237
2. The Rio Sao Francisco and Other
Rivers of the Northeast and East ... 240
3. Rivers and Lakes of the South and
Southwest .......................... 241
E. Maritime Ports and Shipping ............. 249
F. Air Transportation ...................... 254
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G. Cross-Border Movement ................... 257
1. Movement Across Guianan, Venezuelan,
Colombian, Peruvian, and Bolivian
Borders ............................ 259
2. Movement Across Paraguayan Border .. 261
3. Movement Across Argentine Border ... 263
25X6D4? Movement Across Uruguayan Border ... 265
Reading List ................................. 273
VIII. Telecommunications ........................... 275
A. General ................................. 275
B. Organization of Telecommunications
Services ................................ 275
C. Telephone and Telegraph Facilities ...... 276
1. Domestic ........................... 276
2. International ...................... 277
D. Broadcasting ............................ 277
1. Radio .............................. 277
2. Television ......................... 278
E. Special-Purpose Telecommunications
Systems .................................. 278
1. Military ........................... 278
2. Railroad 278
25X6D3? State Police ........................ 279
Reading List .................................. 280
IX. Military and Internal Security Forces 281
A. General .................................. 281
B. Ground Forces ........................... 282
C. Naval Forces ............................. 285
D. 2"'SA [5orce ................................ 288
25X6Drhe Police .......................... 291
Ask
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25X6D Reading List .................................. 295
25X6D
Appendixes
Appendix B -- Recommended Films ....................
Tables
`fable 1 -- Population of Brazil ................... 163
Table 2 -- Brazilian Cities with Populations
over 150,000 ........................... 165
Table 3 -- Immigration to Brazil by Major Sources
of Origin .............................. 166
Table 4 -- Culture Areas .......................... 167
Table 5 -- Road Mileage in Brazil ................. 218
Table 6 -- New and Old Numbers of Selected Federal
Highways in Brazil ..................... 220
Table 7 -- International Boundaries of Brazil and
25X6D Factors Related to Cross-Border Move-
ment ................................... 258
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Photographs
(Abbreviated Titles)
Figure No.
Page
1
Bluffs along flood plain
18
2
Cumulus clouds in Northern Region .......
18
3
Tropical rain forest
19
4
Forests on Amazon .......................
19
5
Jute grown on Amazon flood plain ..:.....
21
6
Dense foliage in tropical rain forest ...
21
7
Riverine vegetation
22
8
Side channel of Amazon ..................
22
9
Terra Firme near Venezuelan border ......
25
10-
Rain forest on Terra Firme .....,.........
27
11-
Tropical rain forest .....................
27
12
Subsistence farm .........................
29
13
Surface of Terra Firme
29
14
High Brasilia Planalto ...................
33
15
Central Plateau ..........................
33
16
Tropical semideciduous forest
34
17
Vegetation on Central Plateau ..,..=......
34
18=
Steep slopes of Central Plateau ..........
36
19
Woodland savanna .........................
36
20
Tropical semideciduous forest ............
37
21
Buriti palms of the Patanal
41
22
Sand dunes of Zona da Mata ...............
41
23?
Crystalline hills ........................
44
24-
Land use in Zona da Mata .................
44
25
Sugarcane in Zona da Mata ................
46
26
Hilly terrain in Agreste .................
49
27
Small farm in Agreste ....................
51
28
Spineless cactus, Palma ..................
51
29:.
Sisal field in Agreste
52
30`
Slopes of Chapada do Araripe .............
52
31
Serra da Ibiapaba .......................
54
32
Rugged terrain of Borborema Plateau .....
54
33
Southern Sertao .........................
56
34,
Sa.o Francisco Valley
56
35
The Sertao ..............................
56
36
High-water level in Sertao ..............
57
37
Reservoir in the Sert .o .................
57
38
,r
Storm in the Sertao .....................
57
39
Caatinga ................................
59
40
Carnaiiba grove ..........................
63
41'
Serra do Espinhago ......................
63
42'
Southern Serra do Espinhaco .............
65
43
Rolling area of Serra do Espinhacbo ......
65
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Figure No.
Page
44 ti Serra do Curral 66
45 Peixoto Dam across Rio Grande ........... 66
46 Southern Minas Plateau 68
47' Vegetation on Central Highland .......... 68
48 Northeastern Bahian Plateau 72
49 Campos Plain ................ .......... 72
50 Serra do Mar ............................ 773
3
51 Hilly area of Serra do Mar 3
52 Rugged area of Serra do Caparao~ ......... 74
53 Coastal rain forest ..................... 74
54 Cacao growing on Bahian coast 77
55 Charcoal burners 77
78
56 Harvesting sugarcane and maize .......... 78
57' Escarpments in Zona da Mata ............?
80
58 Shore near Cabo Frio .................... 80
59 Low hills near Sao Francisco River ...... 84
60 Campanha Gaucha 84
61. Plateau southeast of Sao Paulo .......... 85
62_ Hills east of Campinas 85
63 Second Plateau .... ' 86
64' Third Plateau near Londrina, Parana ..... 86
65. V-shaped valleys of Third Plateau 87
66- Flood plain of Rio Parana ............... 88
67 Falls on Rio Igua,u ....... 91
68-' Rio Ibirapuita in flood .................
69 Parana pine forest ...................... 91
70 The Campos de Guarapuava 93
71 Citrus plantation on Second Plateau 93
72= Grasslands of Campanha Gaucha .... ' ......
73' Cliffs of Southern Plateau, Parana...... 94
74`~ Great Escarpment northwest of Santos .... 95
Coastal lowland near Santos 97
76, Serra do Paranapiacaba 97
77_ Steep hills of Itajai Basin .............
78 Mangroves ............................... 101
101
79 Farm on slope of Serra Geral ............ 102
80 Ricefields on coastal plain .????????" .. 102
81- Harvesting rice near Porto Alegre
82 Caboclo family in the North ............. 122
122
83 Caboclo family with stock of farinha 123
84 Gauchos in Rio Grande do Sul 123
85 Cattlemen typical of the sertFSes ........
86 Fishermen on Amazon at Santarem ......... 125
125
87 Classroom in Rio de Janeiro ............. 133
88 School children in Londrina ............. 138
89 Shrine of African cult in Rio ........... 138
g0 Northeasterner selling charms ...........
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Figure No.
Page
91 Woman carrying water on her head ........ 141
92 Favelas of Rio de Janeiro ............... 142
93 Public water supply in Rio .............. 143
94 Favelas in Rio de Janeiro ............... 144
95 Copacabana Beach in Rio de Janeiro 146
96 Business district of Curitiba 147
97 Lower middle class homes, Sao Paulo 148
98 Houses in Novo Hamburgo 148
99 Stilt house on Amazon ...., ...... 149
100 Wattle-and-daub house 149
101 Houses in Waika village. . . ......150
102 Houses of Xavante Indians...... 150
103 House of Kaxinaua Indians 151
104 Hygiene class in Rio 154
105 Nurses in training 154
106 Northeastern town waterhole~ ............. 155
107 Rubber tapping in Amazon Basin .......... 159
108 Tapirape' family of Amazon area 171
109 Karaja woman of Rio Araguaia area........ 172
110 Krahd Indian women .. . . . 173
111 Indian girl harvesting peanuts ......... 174
112 Krahd Indians on fishing trip ........... 175
113 Indian woman bearing items on trip ...... 176
114 Indian huntsman . . ? . 177
115 Kaxinaua Indians with canoe ............ 178
116 Suya tribal dance .. . 179
117 Xiriana Indians .......... .... 180
118 Makuxi Indians north ofBoa.Vista /?..... 180
119 Indians .... ..
poling small canoe 181
120 Heavy traffic in Sao Paulo . . . 221
121 Carreta in rural area, Parana......... 221
122 Donkeys used to transport goods ~......... ~ 222
123 Via Anchieta on Serra do Mar 222
124 Flat stretch on BR-50 . 223
125 Typical red clay road, Parana.... 223
126 Sandy road in Northeast; ......... .. . 224
127 Concrete arch bridge, Sergipe .~ 225
128 Primitive ferry, Mato Grosso 225
129 Madureira Station in Rio de Janeiro ~~~~? 234
130 Passenger train, Sao Paulo
. ? ....... 234
131 Funicular railroad on Serro do Mar 235
132 Canoe on the Amazon . 243
133 Canoeists on lower Amazon 243
134 Vessels at Belem ? .. . . . 244
135 Loading ore at P8rtoSantana ........ 244
136 Ship at PCrto Velho . ? 245
137 Bark canoes of Camiuras Indians ......... 245
40
tow
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Figure No. Page
138 Pier at Cameta ........ . ................ 246
139 Native produce at Maraba ................ 246
140 Small boats on Rio Negro ................ 247
141 Ferry on Rio Sao Francisco .............. 247
142 Rio Iguap .............................. 248
143 Trucks at port of Santos ................ 251
144 Ship loading from lighter, Ilhe'us ....... 251
145 Small-craft basin at Belem .............. 252
146 Port of Paranagua, Parana ............... 253
147 DC-3 at airfield near Foz do Iguap ..... 255
148 Airstrip near Oiapoque, Amapa ........... 255
149 Baggage oxcart at airfield, Maraba ...... 256
150 Bridge linking Brazil and Paraguay ...... 264
151 Bridge at Florianopolis ...... ? ......... 272
Z-6D Railroad bridge over Rio Itajai ......... 272
Following
Maps Page
55895 Brazil: Northern Region .................
55898 Brazil: West-Central Region .............
55896 Brazil: Northeastern Region .............
55897 Brazil: Eastern Region ..................
55899 Brazil: Southern Region .................
57935 Brazil: Population Density, 1950 ........
57611 Brazil: Socio-Economic Regions ..........
57545 Brazil: Indian Tribes ...................
28
40
62
80
102
116
158
170
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Following
Page
55736
56752
Brazil: Transportation
(Railroads, Federal High-
ways, Coastal Shipping
Routes, and Navigability
of Streams) ......................
USAF Chart of Airfields and Seaplane
236
Stations of the World -- Brazil
(ACIC Vol 4-OlA)
(Runways of 4000' and over) ......
256
56753
USAF Chart of Airfields and Seaplane
Stations of the World -- Brazil
56150
(ACIC Vol 4-01)
(Runways under 4000')
Brazil: Principal Telecommunications
Following
Map 56752
Facilities, 1966 (Map 1)
(Open Wirelines -- Telegraph,
Open Wirelines -- Telephone,
Submarine Telegraph Cables,
Major Radiobroadcasting Sta-
tions, and Television Stations)
278
56151
Brazil:
Principal Telecommunications
Facilities, 1966 (Map 2)
(High-Frequency Radio, Microwave
Radio Relay, Microwave Radio
Relay [Planned], Coaxial Cable,
Radiotelegraph, Radiotelephone)
Following
Map 56150
55894
Brazil:
Physical Regions
(Including Insets on Population
and Administrative Divisions,
Natural Vegetation, Land Use and
Agriculture, and Mining and
54734
Industry) ........................ 358
Esso Roadmap of Brazil Inside
(two sides) ...................... Rear Cover
oft
E-C2E-
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5X6 D
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1. Introduction
Brazil, the fifth largest country in the world, has an
area greater than that of the continental United States, a
population equal to that of the rest of South America, and
a culture predominantly Portuguese in origin. It is located
in the eastern half of South America and borders all but two
of the nations of the continent. It is a land of immense
dimensions, dramatic diversities, growing strength and
unity, and with a determination to play an international
role commensurate with its power potential.
Brazil is a federal republic composed of 22 states, 4
territories, and the Federal District. For practical pur-
poses, however, it is usually treated in five geographical
regions, the North, Northeast, East, South, and West-Central,
which are distinguished by variations in topography, climate,
and economy. The greater part of the country consists of
highlands which fall sharply to a narrow coastal plain in
the east and rather gradually to the west to form an exten-
sive and almost level plain for the vast rain forests of the
Amazon and its tributaries.
In 1967 there were some 85.2 million Brazilians. Their
distribution, racial composition, and way of life differ
widely, but most of them share the Roman Catholic faith, the
Portuguese language, and values related to national pride
and destiny. Eighty percent of them live within 200 miles
of the Atlantic coast, where the principal cities are situ-
ated; relatively few have penetrated far inland. To stimu-
late westward movement and development the national capital
was transferred from Rio de Janeiro to the newly built inland
city of Brasilia in 1960.
If the country were able fully to exploit its natural
resources, it could become one of the most prosperous nations
in the world. It is well endowed with minerals, has a well-
established agricultural base with heavy emphasis on export
crops such as coffee and cocoa, and it has a substantial
labor supply. On the other hand, Brazil's topography and
climate retard progress. The transportation system, hampered
by lack of navigable waterways connecting the seacoast with
the hinterland except for the vast and inhospitable Amazon
valley, has not advanced sufficiently to adequately exploit
and market goods. Progress in some sectors of the economy,
such as industry, and in some geographical regions, as in the
South and East, has been notable, however, but population
increases have absorbed most of the gains.
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The three principal racial groups, European whites,
African Negroes, and South American Indians, have inter-
mingled and interbred to such an extent that racial or
ethnic background plays only a minor role in social and
economic advancement. Old cultural and political patterns
are being replaced by new ones more suited to the challenges
of an exploding population, industrialization, and a growing
demand for social justice and an improved standard of living.
The gap between the way of life of the relatively small
upper class and that of the underprivileged masses is great.
About 50 percent of the population is illiterate, poor, and
effectively excluded from the political process. This is
especially true in rural areas where some 60 percent of the
population lives. Attempts to improve their situation
through economic development have been underway since the
1930's, but only during the last eight or nine years have
they sought a role in politics. Although Brazil's political
institutions are still not representative of the broad masses
and the political parties serve only in a very limited way as
channels for permitting the entry of new groups and interests
into the political arena, the balance of power within the
national government is shifting away from the older agrarian
interests to the urban-industrial and professional upper
and middle class. At the same time the urban working class
is gradually being organized and is playing an increasingly
important role in politics.
Conservative forces, nevertheless, feel confident in
their own strength and in the support of the armed forces,
stanch and reliable defenders of the constitutional process.
However, a radical nationalist left has emerged, challenging
the vested interests and seeking to mobilize popular support
for the reform of existing social and political institutions.
National self-assertion, as expressed in pride in history,
intellectual, artistic, and economic achievements, and in
efforts to assume an independent and leading role in hemis-
pheric and world affairs, has been growing for some time
especially among the upper and middle classes and has now
reached part of the organized working class. It is frequently
expressed in an increasing demand for economic independence
from the United States and for nationalization of public
utilities and basic industries.
There is a polarization of public opinion regarding the
United States. On the one hand, the United States is acknowl-
edged as the principal trading partner, as the source of credit
and skills for economic development, and as the representative
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of a material culture to which many Brazilians aspire. On
the other hand, the dominating role played by the "northern
colossus", its overwhelming wealth, and its value system
presumed to be exclusively materialistic, are causes which
can be found at the roots of anti-North American sentiment
and on which extremists capitalize. Anti-North American for-
mulas are being used with increased frequency by political
parties and are the principal theme of the Communists, both
Russophile and Sinophile. The Communists, of course, capi-
talize on nationalist sentiments and recruit a number of their
popular supporters from among nationalists, making it extremely
difficult to differentiate between subversive Communist ele-
ments and genuine nationalists.
Although the Communist Party has been outlawed since
1947, Communists have had a powerful press and strong influence
in most political and social institutions. Their strongest
influence is evident in labor unions and student organizations
from where they point their fingers to the United States as
the principal cause of social and economic ills.
The Communists are established in the coastal Northeast,
the oldest and poorest section of the country where the large
rural population, composed mostly of plantation workers, has
been breaking away from traditional institutions without
creating new ones to cope with their problems. Here, and
sporadically in other parts of the country, armed clashes
between land-hungry peasants and landowners occur. Although
regionalism is strong and unrest in the Northeast is growing,
it is unlikely that any particular region alone will have a
decisive influence on political development in the near future.
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II. Historical Background
A. Chronology
This chronology is essentially the chronology
to be found in the NIS General Survey, Brazil.
Pedro Alvares Cabral, an explorer on
his way to India, lands in Brazil and
claims it for the Portuguese crown.
Bands of gold seekers begin century-
long series of expeditions into the
interior resulting in vast expansion
of Brazil's frontiers.
Dom Pedro, son of King of Portugal and
regent in Brazil, refuses to return to
Portugal and proclaims Brazilian inde-
pendence.
1864 - Combined forces of Brazil, Argentina,
1870 and Uruguay win costly war against
Paraguay.
1888
1-917
1929
Complete emancipation of slaves decreed.
Brazil declares war on Germany.
World economic upheaval causes a col-
lapse of the coffee market. Brazil
plagued by financial and political
disorders.
1930 Revolution brings Getulio Dornelles
Vargas to power as provisional president.
1934 Constituent Assembly approves new con-
stitution and elects Vargas president.
1937 Vargas becomes dictator.
1942 Brazil declares war on Germany and Italy.
1945 Military overthrow Vargas dictatorship.
1946 General Eurico Gaspar Dutra inaugurated
president. New constitution promulgated.
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1947 Communist Party outlawed. Brazil breaks
relations with USSR.
1951 Vargas inaugurated as president.
1954 Bowing to military demands, Vargas resigns
and commits suicide.
1956
Juscelino Kubitschek inaugurated as presi-
dent, Joao Goulart as vice president.
1960 Capital moved to Brasilia.
1961
1962
Janio Quadros inaugurated as president,
Joao Goulart as vice president in Janu-
ary. Quadros resigns in August blaming
domestic and foreignpr'essures; succession
of Goulart opposed by many of military.
Compromise by Congress permits Goulart
succession in September; constitution
amended to introduce parliamentary govern-
ment, stripping president of important
powers. Relations with USSR restored in
November.
Communist Party dissidents in February
form pro-China Communist Party of Brazil
(CPB).
1963 Plebiscite in January restores presiden-
tial system and full power to Goulart.
1964
1965
Goulart, in March, expropriates certain
unused private lands and all privately
owned Brazilian oil refineries. Military
and civilian leaders, convinced that
Goulart with the help of Communist and
leftist ultra-nationalist allies is seek-
ing to increase his power illegally, move
against him. Castello Branco is elected
by the Congress in April to serve remain-
der of Goulart's term (until 31 January
1966). New government; initiates anti-
inflationary measures and extensive
reform program. Brazil breaks relations
with Cuba in May.
Brazil, in April, contributes soldiers to
Inter-American Peace Force during the
Dominican Republican crisis. Gubernatorial
Alk
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1966
1967
elections in October lead to a political
crisis resolved by the issuance of Insti-
tutional Act II abolishing all political
parties and laying the basis for restruc-
turing the political system. Shortly
later two broad parties are formed: the
pro-government National Renewal Alliance
(ARENA) and the opposition Brazilian
Democratic Movement (MDB).
Arthur da Costa e Silva is elected presi-
dent in October. ARENA party maintains
its majorities in congressional elections
in November.
Congress passes stringent new press law
in January. President decrees sweeping
National Security Law in March. Govern-
ment promulgates new constitution in
March embodying many principles advocated
under the Castello Branco regime. Costa
e Silva is installed as president on 15
March.
B. History
Brazil was discovered in 1500 by Pedro Alvares Cabral, a
Portuguese navigator, who landed at Porto Seguro in the southern
part of the present state of Bahia. He claimed the new terri-
tory for King Manuel of Portugal and called it Vera Cruz (True
Cross), a name eventually changed to Brasil, after the red dye-
wood pau-brasil, brazilwood, found and exported by the early
Portuguese settlers.
During the thirty years following the discovery of Brazil,
small Portuguese communities gradually grew up along the coast.
Reports of the vast riches of Peru and the discovery of gold in
Brazil, in small but promising amounts, led to an increase in
Portuguese immigration and induced King Joao III to initiate
colonization under royal grants. Some fifteen "captaincies,"
extending from the coast inland to Spanish-held territory, were
laid out in 1534 and granted as hereditary holdings to gover-
nors who had almost unlimited authority within their respective
domains.
The excessively decentralized captaincy system was not a
success. To inject more vigor into the colonies and provide
protection against pirates and other marauders, King Jogo
decided in 1548 to place one central political authority,
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answerable directly to the Crown, over the captaincies.
Therefore, he purchased the captaincy of Bahia and appointed
Tome de Sousa as governor-general of the colony. The gov-
ernor arrived at the bay of Todos os Santos in March 1549,
and established the city of Sao Salvador (Bahia), which was
the colonial capital until 1763 when Rio de Janeiro superseded
it. Colonial development went forward at a faster pace under
the governors-general. In 1567 the city Sao Sebastiao do Rio
de Janeiro was established.
After 1580, when King Philip II of Spain incorporated
Portugal into the Spanish Empire, colonizing; activities in
Brazil received scant attention and the colony became the
target for attacks by Philip's enemies. Sea. marauders under
British, French, and Dutch flags harassed the coast and
attempted to occupy territory.
Following the restoration of Portuguese independence in
1640, the colony progressed rapidly, and there was a notable
growth of national feeling in Brazil. The discovery of gold
and diamonds in important quantities in the interior precipi-
tated a rush.to the regions of Mato Grosso, Minas Gerais, and
Goias, resulting in their settlement and exploitation.
From 1750 to 1777, Portuguese colonial affairs were under
the direction of the Marquis of Pombal, whose enlightened
policies and intelligent promotion of the economic and com-
mercial welfare of the colony and the empire earned for him
the title of "the great marquis." Local governors, however,
far from the scrutiny of the crown officials, were often
oppressive, and local resentment sometimes reached a high
pitch. This situation, combined with the sharply whetted
feeling of nationalism that had developed during the previous
century and a half, fostered a growing desire for independence
in Brazil. The first movement for independence came in 1789
in Ouro Preto, then the capital of Minas Gerais. The leader
of the movement was an enthusiastic idealist, Joaquim Jose da
Silva Xavier, better known by his nickname, Tiradentes ("Tooth-
puller"), because of his occasional practice of dentistry.
He and the other members of the movement were finally betrayed,
jailed, and executed. Tiradentes' name became symbolic of
Brazilian independence.
In 1808 Prince Regent Joao VI moved to Brazil after Napo-
leon invaded Portugal. Establishing himself in Rio de Janeiro,
Dom Joao instituted many reforms of great benefit to the country.
His was a reign of commercial, scientific, artistic, and literary
awakening in the country.
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In 1815, Portugal was freed from French domination, and
Brazil was declared a kingdom under the Portuguese monarch.
The next year, on the death of his mother, Queen Maria, Dom
Jogo became King Joao VI. For five year he ruled Portugal
from Brazil. His autocratic temperament at times made him
unpopular in Brazil, and a strong element in Portugal demanded
that Brazil be returned to her colonial status; also, that
the King return to Portugal or lose his crown. Rather than
lose the Portuguese crown, he returned to Portugal in 1821,
leaving his son, Dom Pedro, to govern Brazil as regent.
Ignoring orders from Portugal to return, young Dom Pedro,
on September 7, 1822, declared Brazil's independence and
became constitutional Emperor of Brazil. The new regime was
inaugurated without violence or bloodshed and with popular
enthusiasm.
The new nation had initial difficulties. In 1822 Dom
Pedro dissolved the Constituent Assembly, which appeared
about to adopt a liberal and almost republican constitution
with the Emperor as titular head. Sentiment in the country
was not greatly mollified by the Emperor's proclamation in
1824 of a liberal constitution he had drafted. This consti-
tution, with amendments, was the one under which Brazil was
governed until the proclamation of the Republic in 1889.
Liberal opposition was further strengthened by the loss in
1828 of the Cisplatine Province -- now the Republic of Uru-
guay. Finally, in 1831, Dom Pedro, worn out and disheartened,
abdicted in favor of his five-year-old son, Dom Pedro II,
with Jose' Bonifacio de Andrada as regent.
Ten years of government by regents representing both of
the then-existing parties failed to quiet the country; so the
young Emperor, though but fifteen years old, was declared of
age in 1840 and proclaimed constitutional Emperor. His fifty-
year reign was one of the most important periods in the coun-
try's history. With able assistance Dom Pedro II succeeded
in bringing about the internal pacification and consolidation
of the country, and in scoring diplomatic achievements that
increased Brazil's prestige abroad. He encouraged immigration,
assisted in the construction of railroads, expanded agriculture,
industry, and commerce, and stimulated the intellectual and
cultural development of the country. Two foreign wars of con-
sequence were fought during his reign. In the first, in 1851,
Brazil joined forces with a faction in Argentina to bring
about the downfall of the dictator of that country. In the
second, 1865-70, Brazil, in alliance with Uruguay and Argen-
tina, defeated Paraguay.
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In 1831, a law was passed prohibiting slave trade, but
it wasn't until 1850 that the government succeeded in con-
trolling it entirely. In 1888, all slaves were declared free.
Planters, who lost slaves without compensation, joined the
republicans and the army in agitating for the overthrow of
the monarchy. In 1889, a coup d'etat occurred and a federal
republic was proclaimed. Dom Pedro II quietly left the country.
A provisional government under General Manuel Deodoro
da Fonseca was installed until a constitution could be formu-
lated and a president chosen in accordance with its terms.
Early in 1891 General da Fonseca was elected president, only
to be succeeded in November of the same year by the vice
President, Floriano Peixoto. Commencing with the elections
of 1894, a series of civilian presidents was elected.
From 1930 to 1945, the dominant figure in Brazil was
Getulio Vargas, placed in power by a revolution in 1930. In
1942, Brazil declared war on Germany and Italy and was the
only South American country to send troops overseas. Brazil
also gave naval and air support and provided bases and stra-
tegic raw materials to the Allies.
In October 1945 the military overthrew Vargas shortly
before presidential elections (deferred since 1937) were to
take place. General Eurico Gaspar Dutra (1945-1950) was
elected president and a new, liberal, and progressive consti-
tution was formally promulgated September 18, 1946. After
Vargas' reelection in 1950, economic and political diffi-
culties became increasingly complex; in 1954 Vargas committed
suicide and Vice President Joao Cafe Filho became head of the
government.
The national elections in 1955 were won by Vargas' politi-
cal heirs, the leaders of the two parties he had founded;
Juscelino Kubitschek of the Social Democratic Party (PSD)
became president, and Joao Goulart, head of the Brazilian
Labor Party (PTB), his vice president. Some of the military
opposed their taking office, but a countercoup led by War
Minister Henrique Teixeira Lott ensured their inauguration.
Kubitschek, whose campaign slogan had been "50-years' progress
in 5," greatly accelerated economic development projects but
neglected social welfare. He constructed, at great expense,
the new capital of Brasilia. Kubitschek's term, however, was
marked by a steep rise in the cost of living and increased
social unrest. In the election of 1960 the voters gave a land-
slide victory to Sa.o Paulo Governor Jftnio Quadros, the "man
with the broom," who had promised to sweep out the corruption
and inefficiency which had grown during the three decades fol-
lowing Vargas' accession to power.
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In his impatience with congressional and other forces
that were frustrating his reform efforts, Quadros, in what
many considered a ploy to gain a free hand, tendered his
resignation. To his surprise it was accepted, and he
departed after only 7 months as president. The resulting
crisis brought the country to the brink of civil strife
between military constitutionalist forces and military and
other elements unwilling to allow Goulart to take power;
he had sought Communist support and had narrowly won
reelection as vice president. The crisis was settled by
a typically Brazilian compromise: a modified parliamentary
government with circumscribed presidential powers was
instituted as a prerequisite to Goulart's taking office.
Goulart's conduct during his 31 months in office con-
firmed the misgivings of those who had opposed his accession.
Even after a popular referendum in January 1963 had restored
full presidential powers, he proved a most inept and irre-
sponsible administrator, incapable of coping with the serious
economic and political problems he had inherited. Inflation
mounted rapidly, the country's foreign indebtedness reached
critical proportions, foreign investment dwindled to a trickle,
and economic growth was sharply reduced. Goulart called for
"basic reforms," but the opposition was convinced that he
wanted to revise the constitution so that he could continue
in power beyond the end of his term in January 1966. More-
over, he permitted and even encouraged infiltration of the
labor movement by Communists and other extreme leftists in
return for their help in exerting pressure on the Congress
by political strikes and demonstrations. Among his closest
advisers were a number of Communists and other Marxists, and
he abetted extensive Communist infiltration not only in the
trade unions but also in journalism, education, and in many
government agencies. By early 1964 there was a widespread
conviction that Brazil was drifting toward economic catastro-
phe, that Goulart was incapable of governing, and that he
perhaps planned soon to set up either a dictatorship of the
Peronist type or an authoritarian regime which might fall
under Communist domination. After Goulart had condoned
political agitation and mutinous attitudes on the part of
noncommissioned officers of the armed forces and after he
endorsed an ultimatum by the Communist-dominated Workers'
General Command to the Congress to accept drastic reforms by
20 April 1964 or face a general strike, the military, joined
by leading state governors, revolted against him on 31 March.
His support evaporated within a day, and his flight into exile
met with approval or at least apathy among the great majority
of the population.
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The Brazilian military has several times intervened in
national politics to overthrow dictatorships or otherwise
assure the continuation of the democratic process. It has
always restored power to civilian authority after a short
period.
Humberto Castello Branco, a highly respected army gen-
eral who had played a leading role in the anti-Goulart plot,
was chosen by the Congress to serve for the remainder of
Goulart's term -- until January 1966; the term was later
extended by Congress to 15 March 1967. The new President
pursued moderate reformist policies with a shift towards
greater private participation in the economy? He filled
the key cabinet posts with experienced, non-political tech-
nicians but relied to a great extent on former military
colleagues, particularly those of the so-cal__ed "Sorbonne
group" -- senior officers associated with the Superior War
College -- for advice on policy matters.
The government focused its early efforts on checking
subversion and eliminating corruption. Several hundred
politicians, subversives, and other persons charged with
illegal activities were stripped of their political rights,
and many public officials, including a substantial number
of congressmen, were ousted from office for similar reasons.
Political activities by labor unions and student groups
were sharply curtailed. Congress, with many of the opposition
leaders purged from its ranks, approved most of the admini-
stration's bills.
The government instituted a sweeping financial stabili-
zation and austerity program designed to bring the rampant
inflation under control. The program was only partially
successful. Major reforms were initiated in agriculture,
housing, and the banking system, as well as in other fields,
but with varying degrees of progress, ranging from slight
to moderate.
Although President Castello Branco exercised power with
relative restraint, his period of rule was marked by strong
executive authority embodied in four Institutional Acts and
more than 30 Complementary Acts. In October 1965, for example,
Institutional Act II abolished all political parties then in
existence.
The new Constitution approved by Congress in January
1967 includes many of the special powers employed by Castello
Branco. The Constitution was intended to codify the authority
believed necessary for Castello Branco's successor, Arthur
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de Costa e Silva, a retired army marshal, to continue the
moderate reforms instituted after Goulart's ouster in 1964.
Costa e Silva, who took office on 15 March 1967, has given
strong indications of following the same general policies
as his predecessor.
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READING LIST
1. Bello, Jose Maria, A History of Modern Brazil, 1889-1964,
Stanford: Stanford University Press, 1966. U.
2. Young, Jordan M., The Brazilian Revolution of 1930 and
the Aftermath, New Brunswick: Rutgers University Press,
1967. U.
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III. Physical Geography*
See Map 55894
A. Introduction
Highlands, consisting mainly of tablelands and dissected
plateaus, cover almost 60 percent of Brazil. Mountain ranges
rise above the general surface level in only a few places --
mostly near the east coast where they have hampered the devel-
opment of transportation lines into the interior. Lowlands
and valleys, situated primarily within the Amazon Basin, occupy
the remaining 40 percent of Brazil. A narrow, discontinuous
coastal plain extends along the Atlantic coast, and lowland
areas occur in Rio Grande do Sul and southwestern Mato Grosso.
The climate of Brazil reflects the tropical location of
most of the country. The tropical climate is ameliorated
somewhat by elevation in the highlands. Only in the three
southernmost states is there a subtropical climate.
Tropical rain forest covers most of the Amazon Basin and
the windward slopes of the east coast highlands. A large part
of eastern and southern Brazil was originally covered by tropi-
cal semideciduous forest. These stands have been largely
cleared for cultivation or grazing, but scattered tracts of
second growth remain. A distinctive Parana pine forest grows
in the cool highland areas of southern Brazil. Many of these
stands, too, have been cut over or cleared. Savanna extends
over large areas in the interior highlands, while thorny scrub
is characteristic of semiarid northeastern Brazil. Prairie
grasslands are confined mainly to the extreme southern part of
the country.
For the purposes of this study Brazil is divided into
five physical regions: (1) the Northern Region, (2) the West-
Central Region, (3) the Northeastern Region, (4) the Eastern
Region, and (5) the Southern Region.
The Northern Region corresponds essentially to the Amazon
Basin and includes slightly more than half the country. It is
sparsely populated, and the collection of forest products is
the principal economic activity.
*A more detailed study of the physical geography of Brazil
is available in manuscript form in the Geography Division,
Office of Basic and Geographic Intelligence.
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The West-Central Region includes the interior highland area
commonly referred to as the Central Plateau. It is a sparsely
populated region of savannas devoted primarily to open-range
cattle grazing.
The Northeastern Region includes the coastal states that
form the northeastern bulge of Brazil. The humid, densely
populated coastal sector of this region is an important center
of sugar production; the semiarid interior is an area of open-
range livestock grazing and cotton and sisal production that
is subject to periodic calamitous droughts.
The Eastern Region is a complex area of rugged hills,
basins, and low mountains. It has pockets of dense population,
particularly in the southern part, and land use runs the gamut
from subsistence farming to heavy industry. Dairying, mining,
and the cultivation of coffee, cacao, and sugarcane are impor-
tant economic activities.
The Southern Region, the smallest of all, is the most
populous and the most economically developed part of the country.
It leads in the production of industrial goods, lumber, and a
variety of agricultural products.
B. Northern Region
See Map 55895
1. General
The Northern Region corresponds to Amazonian Brazil and
includes the states of Acre, Amazonas, and Para; the territories
of Amapa. Rondania, and Roraima; and parts of the states of
Goias, Mato Grosso, and Maranhao. The region as a whole has
not been accurately mapped, and very little is known about siza-
ble areas remote from the principal navigable rivers. The Ama-
zon Flood Plain -- the stereotype Amazon of popular literature --
comprises only a very small percent of the total area. Most of
the region lies at elevations above flood level and is called
the terra firme (firm ground) to distinguish it from the flood
plain. A relatively narrow coastal plain north of the Amazon
Delta separates the seaward margin of the terra firme from the
Atlantic shore.
2. Amazon Flood Plain
a. Terrain and Drainage
The Amazon Flood Plain consists of the lowlands that border
both the main river and the lower courses of its principal
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tributary streams. The flood plain is narrow along the upper
course of the Amazon but attains a width of over 125 miles
near the river mouth. Lines of bluffs mark its outer margins
(see Figure 1). The configuration of the flood plain is
irregular and constantly changing, as the river at flood stage
frequently shifts its course -- abandoning old channels and
forming new ones. Side channels join and rejoin the main
channel at varying intervals, enclosing numerous islands.
Natural levees of varying width rise above the general level
of the flood plain, bordering the present channel of the river
and also many of the former channels. The levees are submerged
only during the highest floods.
Upstream from Manaus there are two periods of high water;
a major rise occurs from early May to early July and a lesser
rise from early November to early March. Downstream from
Manaus the high-water period extends from early March to early
September, with the maximum level occurring generally in June.
At flood stage the drainage of the flood plain becomes chaotic.
Once the floodwaters start to recede the temporary lakes along
the abandoned channels are gradually reduced to marsh or meadow-
land, lesser connecting channels dry up, and sandy beaches
reappear along the riverbanks and islands. A sufficient number
of side and connecting channels, however, carry enough water
during the dry season to permit relatively free movement by
canoes and other small craft.
The flood plains of the tributary streams within the
upper Amazon Basin are similar in general characteristics to
the flood plain of the main river. Within the lower Amazon
Basin, however, the lower reaches of many tributaries appear
as broad estuaries or lakes.
b. Climate
The average annual rainfall ranges from 78 to 122 inches
at the various stations in the subregion. In general, the
greatest amount of rain falls during the summer (December
through May) and the least during the winter (June through
November). The duration and intensity of the dry season vary
considerably in the subregion, ranging froma pronounced dry
season in the vicinity of Obidos and Santarem to only a "less
rainy season" along the upper river.
Cumulus clouds predominate (see Figure 2); frequently
they develop into towering cumulonimbus masses on summer after-
noons. Fog is rare on the Amazon or its major tributaries;
however, low stratus clouds or fog sometimes form over forested
areas at about treetop level in the early morning.
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Figure 1. Bluffs along margins of flood plain.
Figure 2. Cumulus clouds in Northern Region.
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x ?a
iY }
p ~r
Figure 3. Tropical rain forest.
4,4 ?
Figure 4. Amazon Flood Plain. Forests on the
flood plain are inundated seasonally.
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Calms prevail throughout the subregion in summer; they
are interrupted only by the gusts of wind that accompany
thundershowers. The trade wind penetrates the lower Amazon
during the dry season and has a cooling effect there along
the main river and its immediate margins.
The average annual temperatures within the subregion vary
between 77?F and 82?F. Mean monthly temperatures are relatively
constant throughout the year, the range between the warmest
and coolest months being only about 4 Fahrenheit degrees. The
daily temperature range is considerably greater than the annual
range -- the average daily maximum and minimum being about
88?F and 73?F, respectively.
c. Vegetation
Tropical rain forest predominates on the Amazon Flood
Plain (see Figure 3). This forest has a nearly closed canopy,
100 to 130 feet high. A few scattered giant trees rise above
the main canopy, and smaller trees form two layers below.
Saplings, bushes, and tall herbaceous plants comprise the
undergrowth. Numerous ropelike lianas (climbing plants) are
entwined in the trees, and long air roots hang from many of
the epiphytes (air plants) perched on the larger branches or
in the forks of trees. The lianas and air roots together form
a tangled net. Vegetation is generally densest along the
edges of clearings and along riverbanks. Most of the forests
of the flood plain are inundated seasonally (see Figure 4);
some stands on the lowlands of the Amazon Delta are flooded
daily; and in some poorly drained areas where the ground never
dries out a true swamp forest exists.
Seasonally flooded grasslands occur on. some parts of the
flood plain. Grasslands are most extensive on the eastern
half of Ilha de Marajo and in the Lago Grande do Curuai area.
Mangrove swamps rim the small islands of the delta and the
north and east coasts of Ilha de Marajo.
d. Land Use
Much of the flood plain is forested, and the collection
of forest products during the dry season is an important eco-
nomic activity. Jute and cacao are grown commercially, and a
variety of subsistence crops are raised (see Figure 5). Live-
stock are grazed on the natural grasslands.
Wherever possible, habitations are built on natural levees
or other areas of high ground that are inundated only during
the highest floods. Many houses, however, are built on stilts
on lower ground.
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Figure 5. Amazon Flood Plain. Jute is the prin-
cipal commercial crop.
Figure 6. Tropical rain forest. Dense vegetation
impedes movement inland from the river margins.
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Figure 7. Riverine vegetation. Stands of aninga
frequently form natural palisades along the river
sides.
Figure 8. Side channel. The narrow watercourses
paralleling the Amazon are used by the natives as
canoe trails.
ink
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3. Terra Firme
a. Terrain and Drainage
The terra firme includes the extensive area of higher
ground in the Amazon Basin that spreads out to the north and
to the south of the main flood plain. It is separated from
the flood plain in most places by low bluffs, and it is
divided into segments by valleys of the principal Amazon
tributaries. The surface of the individual plateau segments
is generally flat to rolling; however, scattered hills and
mesas rise above the general surface level.
The segment adjacent to the Amazon Flood Plain is low and
is commonly referred to as the Amazon Plain. It is relatively
narrow along the lower Amazon, but widens in the upper basin
to embrace most of the vast area between the Rio Madeira and
Rio Negro. The segments of the terra firme situated to the north
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and south of the Amazon Plain are higher and more rugged.
Northward the land ranges from flat-to-rolling plains to
rugged hills, mountains, and high tablelands (see Figure 9).
Southward the terra firme is generally more tabular in con-
figuration. The plateaus rise in successive steps southward
toward massive tablelands situated along the southern border
of the subregion. Fingerlike extensions of the high tablelands
project northward into the subregion along either side of the
Juruena, Teles Pires, and Xingu rivers.
The seaward margin of the terra firme north of the Amazon
Delta is bordered by a coastal plain made up of several broad
terraces. The lowest terrace level is poorly drained and parts
of it are inundated during the rainy season. The margin of
the terra firme east of the delta is indented, consisting of
small peninsulas separated by numerous small bays and inlets.
In places a very narrow coastal plain backs the shore.
Many tributaries of the Amazon are themselves large rivers,
having tributary streams of their own that exceed 500 feet in
width for great distances. In addition, hundreds of smaller
tributaries rise in areas remote from the principal rivers.
Many streams overflow their banks during the height of the rainy
season. The high-water level is reached at different times on
various tributaries as well as along different sectors of some
individual streams because of differences in the rainfall regime.
b. Climate
The climate of the terra firme is generally similar to that
of the Amazon Flood Plain, although there is a wider range in
the amount of rainfall and in the duration and intensity of the
dry season. The average annual rainfall ranges from 56 to 139
inches.
The
greatest amount falls on the superhumid western
part of
the
Amazon Plain, where there is no appreciable dry
season.
The
least falls in the savanna areas along the south-
eastern
and
north-central peripheries of the subregion, which
experience a pronounced winter dry season. The dry season ex-
tends from May through September (the Southern Hemisphere winter)
in the area along the southeastern periphery and from October
through April (the Northern Hemisphere winter) in the area along
the north-central periphery.
Cumulus clouds are the characteristic c=_oudform of the
subregion. During the rainy season they frequently develop into
towering cumulonimbus clouds by noon or early afternoon, culmi-
nating in thunderstorms. Fog or low stratus clouds occasionally
norm over the forests at near treetop level in the early morning,
but they usually lift and dissipate within an hour or two after
sunrise.
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Figure 9. Terra Firme. Near the Venezuelan
border are high tablelands rimmed by cliffs.
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Smoke from grass fires restricts visibility in parts of
the subregion during the dry season. The fires occur over
extensive areas of savanna and, locally, in clearings in the
rain forest.
The northeasterly trade winds prevail throughout most of
the subregion in summer, and the weak southeasterly trades
prevail in winter. The trade winds seldom reach the upper
Amazon, however, and the local winds there are generally light
and variable. Strong surface winds are uncommon in the sub-
region, except for the gusty local winds that accompany thunder-
storms.
The mean annual temperature averages about 77?F, and
there is a difference of only about 5 Fahrenheit degrees be-
tween the coolest and warmest months. The temperature range
between the warmest and coldest parts of the day is about 16
Fahrenheit degrees.
c. Vegetation
Tropical rain forest covers most of the subregion (see
Figure 10). In structure the terra firme forest is similar
to that of the Amazon Flood Plain. Three or four layers of
trees can generally be distinguished, and the tops of indi-
vidual layers are commonly somewhat higher than in the flood
plain forest. The understory of saplings, bushes, and tall
herbaceous plants is relatively open, but dangling roots and the
stems of lianas and epiphytes form tangled nets between trees
(see Figure 11). The vegetation is generally densest along
the margins of clearings and along riverbanks. Various trees
and plants are equipped with sharp spines or thorns that may
tear clothing or lacerate the skin and cause infections.
A woodland savanna occurs in those parts of the subregion
having a pronounced dry season, as well as in some areas having
porous sandy soils, such as on the tops of high tablelands.
This vegetation is typically composed of grasses, shrubs, and
low gnarled trees. The ratio of one to another varies greatly,
ranging from grasslands with widely scattered shrubs and low
trees to parklike stands of trees that form an open canopy
above a grassy floor.
Areas of open grassland occur along the middle part of
the Rio Branco Valley and on the Amapa coastal plain. Mangroves
fringe the coasts of the subregion.
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Figure 10. Tropical rain forest on
Terra Firme. Brasilia - Belem high-
way.
Figure 11. Tropical rain for-
est. Nets of lianas and air
roots retard movement.
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d. Land Use
The collection of forest products is the principal economic
activity of the subregion, and the largest revenues come from
the sale of rubber, Brazil nuts, and rosewood oil. Agriculture
is confined primarily to small subsistence p=_ots, although agri-
cultural colonies have developed near the larger centers to
supply the urban population (see Figure 12). Two commercial
crops of increasing economic value are mallow (a fiber plant)
and black pepper. Modern manganese mining operations are car-
ried on in the Macapa area, and placer mining for gold and
diamonds is common along streams in the territories of Roraima
and Rond6nia.
The gatherers of forest products live primarily in small
villages or isolated huts along streambanks accessible by boat.
The tribal Indians construct their primitive villages at some
distance from the streams for protection from enemies who
25X6D.vel on them.
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Figure 12. Subsistence farm in forest clearing.
Figure 13. Terra Firme. The various surface levels are
generally separated by lines of low bluffs.
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C. West-Central Region
See Map 55898
1. General
The West-Central Region is an area of plains, plateaus,
and hills. It includes the greater parts of the states of
Goias and Mato Grosso, the extreme western parts of Bahia and
Minas Gerais, the southern tips of Maranhao and Piaui, and the
Federal District (Brasilia). The region has no sharply defined
natural boundaries but includes the physiog:'aphic regions com-
monly referred to as the Central Plateau and the Pantanal.
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2. Central Plateau
a. Terrain and Drainage
The term "Central Plateau" is used broadly to denote the
series of high plateaus of interior Brazil that extend westward
from the Sao Francisco Valley to the lowlands of the Paraguay
River Basin (see Figure 14). The plateaus are contiguous, but
their surfaces are at different elevations, and generally they
are separated by escarpments. Some plateaus are known locally
as chapadas. They are high, relatively flat tablelands, bor-
dered by steep slopes or escarpments. Other plateaus appear
as slightly tilted tablelands (cuestas), bordered by escarp-
ments on at least one side. Frequently, parallel lines of
cuestas rise steplike, one above the other, as platforms or
broad terraces. The steep slopes that border the chapadas and
cuestas often appear as low mountains when viewed from below,
and locally they are referred to as serras (mountain ridges).
Scattered hill groups and isolated hills rise above the general
surface level of the chapadas and cuestas. In a few areas, par-
ticularly in the northeast, the plateaus have been dissected
into complexes of sharp-crested hills of relatively uniform height.
Terrain units within the Central Plateau include the Bra-
silia Planalto and associated highlands, the Espigao Mestre,
the Upper Araguaia and Tocantins Hill Zone, the Goias Depression,
the Parana Plateaus, the Alcantilados and Furnas Plateaus, the
Serra da Bodoquena, the Rio das Mortes Plateau, the Cuiaba
Basin, and the Serra das Araras. The Brasilia Planalto and
associated highlands, 3,000 to 4,600 feet in elevation, consti-
tute the highest surface level. The Espigao Mestre adjoins the
Brasilia Planalto to the northeast, forming the water divide
between the Amazon and Sao Francisco river systems. The complex
Upper Araguaia and Tocantins Hill Zone lies within the "L" between
the Espigao Mestre and the Brasilia Planalto. Another hill zone,
the Goias Depression, lies to the south of the Brasilia Planalto.
To the west of the Goias Depression, at successively lower ele-
vations, are the Parana, Alcantilados, and Furnas Plateaus, and
the Serra da Bodoquena. To the north of the Alcantilados Plateau
is the Rio das Mortes Plateau, overlooking the Amazon Basin, and
to the west of the Rio das Mortes Plateau are the Serra das
Araras and the Cuiaba Basin.
Streams within the Central Plateau generally are swift and
are interrupted by numerous rapids along their upper reaches
and by occasional rapids along their lower reaches. Although
perennial along their lower courses, many streams carry little
or no water in their upper reaches during the dry season. Most
streams are confined by high banks and have no flood plains.
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The Rio Parana, the largest river, is bordered by a flood plain
along much of its middle and lower course arid overflows its
banks during the high-water period. In general, stream levels
start to rise with the onset of the rainy season, beginning in
late September in the southern part of the subregion and between
late October and early November in the northern part. The water
level starts to drop as the rains taper off in April, but the
low-water stage may not be reached until late June.
A tropical savanna climate with a summer rainy season and
a winter dry season prevails over most of the subregion. The
average annual rainfall ranges from 40 to 76 inches, with the
greatest amount falling on the higher plateaus and the least
on the Espig,o Mestre and in the Parana Basin. The rainy sea-
son extends from October through April for the subregion as a
whole.
Cumulus clouds are the characteristic cloudform in the
subregion (see Figure 15). They form during the morning and,
during the rainy season, frequently build into cumulonimbus
clouds by noon or early afternoon, culminating in thunderstorms.
Low stratus clouds occasionally restrict visibility during
the early morning. The incidence of fog is not great. Smoke
from grass fires restricts visibility significantly during the
latter part of the dry season.
Northerly surface winds prevail in most of the subregion
during the summer, and southeasterly to northeasterly winds
prevail during the winter. Strong surface winds are uncommon
except for gusts that accompany thunderstorms.
The hot tropical climate is moderated locally by the
effects of altitude. The mean annual temperature varies be-
tween 68?F and 78?F. Mean daily maximum temperatures range
from 84?F to 97?F in September, the hottest month, and mean
daily minimum temperatures range from 48?F to 68?F in June and
July, the coldest months. The daily temperature range extends
from a minimum of about 25 Fahrenheit degrees to a maximum of
nearly 43 Fahrenheit degrees. Within the highlands, nighttime
temperatures in the narrow valleys drop significantly below
those on the adjacent plateau.
c. Vegetation
The natural vegetation ranges from grassland through open
woodland savanna to dense tropical semideciduous forest. The
grasslands and woodland savanna are generally associated with
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Figure 14. High Brasilia Planalto. The surface is flat to
undulating.
Figure 15. Cumulus clouds over Central Plateau.
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Figure 16. Tropical semideciduous forest. Bands
of forest extend along the principal stream valleys.
Figure 17. Vegetation on Central Plateau. Wood-
land savanna, composed of grasses, shrubs, and low
gnarled trees, predominates.
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the flat surfaces on the plateaus and cuestas, and the forests
occur more commonly on slopes and along stream valleys (see
Figure 16). Woodland savanna, composed of grasses, shrubs,
and low gnarled trees, is the predominant form of vegetation
(see Figure 17). It varies in structure from grasslands with
widely scattered shrubs and low trees, through parklike stands
of low trees with open canopy and a grassy floor, to scrub
woodland. The tropical semideciduous forest stands are usually
stratified into three layers, but they are not uniform in struc-
ture. From 10 to 30 percent of the trees shed their leaves
during the dry season. The undergrowth tends to be more dense
in these stands than in the tropical rain forest. Lianas and
epiphytes are present, their number varying considerably with
local conditions.
Land Use
The herding of range cattle is the principal economic
activity in the Central. Plateau. Subsistence agriculture,
based on the slash-and-burn method, is carried on in scattered
areas -- primarily along river valleys and on cutover forest
land. Small-scale commercial agriculture is practiced in a
few areas, such as the Triftngulo Mineiro, the Mato Grosso do
Goias, and parts of the Parana Basin. Significant commercial
crops are rice, coffee, cotton, wheat, and sugarcane. In
addition, some mining of diamonds, quartz crystals, and nickel
25X6.? carried on within the subregion.
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Figure 18. Central Plateau. Locally, movement is somewhat
restricted by steep slopes.
Figure 19. Woodland savanna. Movement is relatively free
on foot or on horseback.
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Figure 20. Tropical semideciduous forest. The dense under-
growth retards movement across country.
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3. The Pantanal
a. Terrain and Drainage
The Pantanal is an extensive lowland area that extends
along the Paraguay River and its tributaries. The flat to
undulating surface rises gradually eastward, away from the
river. Much of the lowland near the river is inundated during
the rainy season and is marshy at other times. Eastward, the
surface has a swell and swale appearance, with numerous shallow
depressions separated by stretches of slightly higher ground
situated above flood level. A belt of low, rolling foothills
extends along the outer margin of the Pantanal, near the base
of the bordering escarpments. Scattered hill masses and steep
mesas occur along the western side of the Paraguay River near
the Bolivian border.
Streams within the Pantanal are characteristically'wide
and sluggish. The winding Paraguay River is dotted with numer-
ous small islands. Its banks rise above the general flood
level, but those of the tributaries flowing through the marsh-
land near the main river are very low and are almost indistin-
guishable locally. Numerous short, shallow watercourses inter-
connect the many depressions and the main stream network. Many
minor streams dry up during the dry season. Even large rivers
such as the Rio Negro reportedly dry up during particularly
long and intense dry seasons. Some of the depressions contain
lakes or ponds throughout the year; others are reduced to marshes
or dry up completely during the dry season.
The Paraguay River begins to rise in January and good
navigable stages prevail from February to September. The depres-
sions and extensive flood plains are generally inundated from
December to May. Ponds and lakes either expand greatly in
size, individually, or coalesce to form extensive bodies of
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water. The inundated flood plains of the Paraguay River and
its east-bank tributaries frequently form a continuous sheet
of water as much as 15 miles wide and 13 feet deep in places.
The water level remains high on the principal streams after
the rainy season ends until the excess surface water on the
lowlands has gradually drained off into the streams.
b. Climate
The Pantanal has a tropical savanna climate, similar in
most respects to that of the Central Plateau. The average
annual rainfall. is somewhat lower in the Pantanal, ranging
from about 40 to 50 inches, and the temperature readings are
somewhat higher. The mean annual temperature ranges from
about 73?F to 78?F, and the mean daily maximum temperatures
for the hottest months range from 89?F to 93?F at selected
stations.
C. Vegetation
Grasslands predominate in the Pantanal but alternate with
woodland savanna and forests. Grassland and woodland savanna
spread out over the extensive lowland area and are subject in
varying degrees to alternate inundation and drought. Bands of
tropical semideciduous forest grow on the natural levees along
the principal streams and on stretches of higher ground that
rise slightly above the normal flood level. A distinctive
Chaco type of drought-resistant vegetation, including many spiny
plants, occurs on dry lowlands along the east side of the Para-
guay River southward from Porto Esperanca and on the dry slopes
of scattered limestone hills along the west side of the river.
It varies from open stands to dense thorny thickets.
Tall sedges, some having sharp edges that cut like Florida
sawgrass, grow in the permanently moist swales and marshes.
Dense stands of reeds 8 to 10 feet tall cover the lowest wet
spots, and floating mats of aquatic plants grow on the surfaces
of shallow lakes and on quiet lagoons along the main rivers.
When the waters recede at the end of the high-water period the
floating islands move out toward the main channels and often
solidly choke the side channels.
d. Land Use
Cattle raising is the principal economic activity in the
Pantanal. During the dry season cattle graze on grassy low-
lands throughout the area. During the rainy season many are
driven to poor pastures on higher ground or to fattening pas-
tures far away in the western parts of the states of Minas Gerais
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and Sdo Paulo. Some cattle are marketed or processed locally.
Manganese and iron are extracted from the Urucum mines
south of Corumba. Most of the ore is produced for a small
al mill
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B O L I V I A
BRAZIL
WEST-CENTRAL REGION
seu r.~.~o
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Figure 21.
waterholes
region.
ms enc
l
1
he
sub-
The Pantanal. Burlt? pa
on the elevated eastern part of t
Zona da Nlata. Sand dunes border a lagoon
Figure 22. lain.
on the coastal p
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D. Northeastern Region
See Map 55896
1. General
The Northeast is an amorphous region with boundaries
variously defined to suit different frames of reference. In
this handbook the Northeastern Region is delimited primarily
in terms of terrain, climate, and vegetation and includes not
only the six states of the traditional Northeast -- Ceara,
Rio Grande do Norte, Paraiba, Pernambuco, Alagoas, and Sergipe but also the state of Piaui and parts of Bahia and Maranhao.
Three low mountain ranges and a dissected high plateau form the
skeletal framework of the region. The mountain ranges project
northward, eastward, and southwestward from the Chapada do
Araripe like the spokes of a wheel, forming water divides
between extensive areas of plains arid. 1cw, plateaus. The Serra
da Ibiapaba forms the northern spoke, the Serra dos Cariris
Velhos the eastern spoke, and a series of ranges including
the Serra da Farinha and Serra Tabatinga the southwestern
spoke. The high Borborema Plateau lies at the eastern end of
the Serra dos Cariris Velhos and constitutes the dominant ter-
rain feature in the eastern part of the region north of the
Sao Francisco Valley. The climate varies considerably within
the region, primarily in amount of rainfall. Variations in
natural vegetation and land use are closely related to the
rainfall regime. As a result, the subregions within the North-
eastern Region correspond more closely to climatic zones than
to terrain regions. The Zona da Mata is a humid area along
the east coast; the Sert2'o includes the extensive semiarid
interior of the region; the Agreste is a transitional area
between the Zona da Mata and the Sertgo; and. the Parnaiba-
Mearim Subregion is a transitional area between the Sertgo
and the humid Amazon Basin.
2. Zona da Mata
a. Terrain and Drainage
The Zona da Mata, extending along the humid east coast of
the region, is 25 to 60 miles wide. It includes three distinc-
tive belts -- the narrow coastal plain, the low sandy table-
lands (tabuleiros), and the crystalline hills.
The sandy coastal plain, seldom exceeding 5 miles in width,
extends inland to the steep margin of the coastal tablelands.
The shore is generally low and sandy, and the beaches are backed
in most places by a belt of sand dunes or raised beaches (see
Figure 22).
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The coastal tablelands range from approximately 5 to 30
miles in width. Their seaward margins are marked by discon-
tinuous low cliffs. Streams flowing eastward across the zone
have cut steep-sided valleys that divide the surface into
parallel blocks -- whence the name tabuleiros.
The belt of crystalline hills, west of the tabuleiros,
corresponds in general to the sugarcane area and is the most
densely populated and economically productive part of the
Northeast. The rolling hills increase in height and degree
of slope inland (see Figure 23). The area is drained by a
few main rivers and a maze of small tributary streams.
Meadows and flood plains extend along most of the main val-
leys, and discontinuous narrow ribbons of flood plain extend
along many of the minor valleys.
The principal streams are perennial, but some minor
streams may dry up completely during the dry season. The
period of high water on the main rivers extends from April
through September. The mouths of many of the main streams
are drowned, forming small bays. Drowned side valleys or
channels branch off some of the bays and reach into the ad-
jacent coastal plain, forming lagoons and swamps. The Rio
Slo Francisco flows across the Northeastern Region. Its
lower course is sluggish and interrupted by sandbars and mud-
flats, and an extensive delta has formed at its mouth.
Climate
A tropical humid climate prevails in the Zona da Mata.
The mean annual rainfall exceeds 40 inches throughout the
zone and probably exceeds 80 inches in the more humid part
of southeastern Pernambuco. Throughout most of the zone the
rainy season occurs during autumn and winter (March through
August), and the dry season extends from September through
January. The amount of rainfall received diminishes from the
coast inland until high hills are reached and then increases
on the windward slopes.
Low ceilings and poor visibility occur in winter in asso-
ciation with frontal activity. The occurrence of dense mist
or fog is minimal along the coast but increases inland as
elevation increases.
The discomforting effects of high humidity and tempera-
ture are alleviated somewhat by the persistent trade winds and
the land and sea breezes, although the latter are relatively
weak.
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Figure 23. Crystalline hills. The hill belt is
widest and most dissected in southeastern Pernambuco.
Figure 24. Land use in the Zona da Mate.. Cane
fields generally cover the gentle slopes of the
crystalline hills, and forest remnants occupy the
hilltops and steep slopes.
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Temperatures are high and fairly uniform throughout the
year. The mean annual temperature ranges from 77?F at Salva-
dor to 79?F at Natal. The mean daily maximum temperature for
the warmest month ranges from 86?F to 88?F, and the mean daily
minimum for the coldest month ranges from 68?F to 71?F.
C. Ve eg tation
The natural vegetation of the Zona da Mata varies con-
siderably. The coastal mixture includes sparse beach and sand
dune vegetation, coconut groves, mangrove swamps, occasional
stands of cashew, and scrubby second-growth forest. In the
coastal tableland zone woodland savanna generally covers the
level areas on the tops of the tabuleiros, and second-growth
forest grows on the slopes. The woodland savanna varies from
open grassland with scattered scrawny low trees and shrubs
through parklike stands of low trees with open canopy and grassy
floor to tall scrub woodland. The second-growth forest consists
of a scrubby growth of young slender trees and a dense underbrush.
The stands include some semideciduous species that lose their
leaves briefly during the dry season. Lianas and epiphytes are
present. Most of the land in the zone of crystalline hills is
under cultivation, and the natural vegetation is reduced to
scattered remnants of tropical forest, mostly second growth, on
steep slopes and hilltops (see Figure 24). These forest rem-
nants are generally more dense than the second-growth forest on
the tabuleiros and contain more lianas, epiphytes, and ferns.
The trees are mostly broadleaf evergreens.
d. Land Use
Coconut groves extend along the low marine terraces and
beaches of the Zona da Mata. Numerous fishermen live along
the shore -- some in thatched huts scattered among the palms
and others in fishing villages. On the sandy coastal plain,
scattered subsistence farms are interspersed among areas of
low scrub growth. On the tabuleiros the principal activities
are lumbering, firewood cutting, and charcoal burning in the
wooded areas and open range cattle raising in the woodland
savanna. The few scattered habitations of the tabuleiros are
generally located along the roads or in small valleys. In the
zone of crystalline hills, growing sugarcane is virtually the
only economic activity (see Figure 25). Fields of sugarcane
cover the flood plains and, in some areas, the adjacent hill-
sides. Houses and small garden plots associated with them are
25Dted on land unsuitable for sugarcane.
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Figure 25. Vast sugarcane fields in Zona da Mata.
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3. The Agreste
a. Terrain and Drainage
The Agreste is a transitional area lying between the humid
Zona da Mata and the semiarid interior (the Sertdo). This
relatively small subregion consists of two areas separated by
a semiarid corridor along the lower SAo Francisco Basin.
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The northern Agreste area is an elongated belt, 15 to
100 miles wide, extending from the northeastern tip of Rio
Grande do Norte south-southwestward to the Sao Francisco
Valley. It extends along a segment of the coast of Rio
Grande do Norte and continues southward along the Borborema
Plateau. A line of rugged heights, rising above the flat-
to-rolling surface of the Borborema Plateau, forms the west-
ern border. The abrupt eastern edge of the plateau has been
deeply dissected, forming a ridge-and-valley landscape (see
Figure 26).
The southern Agreste is located in Bahia. It is a U-
shaped area with its base coinciding roughly with the Para-
guacu Valley, its eastern arm extending along the inner mar-
gin of the Zona da Mata and its western arm stretching along
the eastern margin of the Chapada Diamantina. The eastern
arm consists primarily of low sandy plateaus similar to the
coastal tabuleiros. The western arm includes part of the
steep eastern slope of the Chapada Diamantina and an adjacent
zone of rugged hill masses separated by relatively broad low-
land corridors. The hills have been dissected by innumerable
small streams whose narrow, irregularly oriented valleys form
a chaotic drainage pattern.
With few exceptions the streams in the Agreste are inter-
mittent. Most of the larger rivers carry water throughout
the rainy season but dry up for at least a short period dur-
ing the latter part of the dry season. Many of the minor
streams flow only for brief periods after ra_Lnstorms. A few
that have their sources on the higher hills carry water most
of the year. The Rio Paraguacu is perennial except along its
extreme upper reaches.
Climate
In general, the climate of the Agreste is similar to
that of the Zona da Mata, but it differs significantly in
terms of amount and regularity of rainfall. The average
annual rainfall is less than 40 inches throughout the sub-
region, with as little as 25 inches in parts of the northern
Agreste. Violent deviations from the norm occur from year to
year. In most of the subregion the rainy season occurs during
the autumn and winter (March through August). In the southern
Agreste, however, there is a gradual transition from an autumn-
winter rainfall pattern in the eastern part, through a summer
rainfall regime in the central part, to a regime with no
marked dry season in the zone along the eastern slopes of the
Chapada Diamantina.
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Figure 26. Hilly terrain in Agreste area of northern Paraiba.
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c. Vegetation
Most of the original agreste vegetation has been cut and
replaced by cultivated fields on the arable land and by dry
scrub vegetation in areas that are either too steep for culti-
vation or have unsuitable soils. The dry scrub ranges from
high thorn forest to low thorny scrub. The trees of the thorn
forest are only 25 to 30 feet in height, and many lose their
leaves during the dry season. A dense undergrowth, including
thorny species and cactuses, covers the ground beneath the
trees. These stands are frequently separated by grassy areas.
Low thorny scrub grows in the driest locations. It is bushy
and more open than the thorn forest. Small tracts of second-
growth tropical forest occur on some of the humid heights, and
limited areas of woodland savanna occur on the sandy tabuleiros
in Bahia.
d. Land Use
The diversified agricultural land use of the Agreste
contrasts sharply with the virtual monoculture of sugarcane
in the adjacent Zona da Mata and of open range cattle raising
in the Sert'Ao. Small farms predominate, and subsistence farm-
ing is generally combined with the cultivation of one or more
commercial crops and open range cattle raising (see Figures 27
and 28). Range cattle are generally grazed on the poorer land
where the low thorny scrub or woodland savanna vegetation is
interspersed with natural grassland. The most important com-
mercial crops in the northern Agreste are cot;ton and sisal
(see Figure 29). Specialty crops such as tomatoes and various
fruits are grown in a few favored "oases." In the southern
Agreste tobacco and manioc are the most important crops, and
beef cattle are raised on improved pastures. Some lumbering
25k%burs on the humid slope of the Chapada Diamantina.
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Figure 27. Small farm in the Agreste. Hedgerows
separate landholdings.
Figure 28. Palma. This is a species of spineless
cactus grown as a forage crop in the Agreste and
the Sertffo.
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Figure 29. Sisal field in the Agreste.
Aoki
Figure 30. Steep slopes along northern margin of
Chapada do Araripe.
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4. The Sertao
a. Terrain and Drainage
The semiarid Sertao constitutes the largest part of the
Northeastern Region. Irregular chains of low mountains, table-
:Lands, and rugged hills radiate from a central tableland and
separate broad areas of plains, basins, and low plateaus into
a series of compartments. This overall radial pattern is dis-
torted by the basin of the Rio Sgo Francisco, which forms a
giant loop across the southern part of the subregion.
The Chapada do Araripe, about 2,500 feet in elevation, is
the central tableland (see Figure 30). The Serra da Ibiapaba
extends northward from the western end of the Chapada do Araripe
to within 25 miles of the north coast (see Figure 31). The
Serra dos Cariris Velhos reaches eastward from the Chapada do
Araripe to the arid western part of the Borborema Plateau (see
Figure 32). Lesser chains of low mountains and hills extend
northward and northeastward from the Chapada do Araripe into
the broad area between the Serra da Ibiapaba and the Serra dos
Cariris Velhos. Interior basins are enclosed between these les-
ser chains and the main mountain ranges. A zone of lowlands and
low plateaus extends along the north coast and penetrates varying
distances inland between the several mountain and hill ranges.
To the south of the Borborema Plateau and the Chapada do
Araripe is the vast southern Sertao. It includes much of the
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Figure 31. Serra da Ibiapaba. A high escarpment
marks the eastern edge.
Ask
Figure 32. Rugged terrain along northwestern part
of Borborema Plateau.
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lower and middle Sao Francisco River Basin, the Chapada Dia-
mantina, and an area of hills and low tablelands to the east
of the Chapada Diamantina exclusive of the Agreste (see Fig-
ures 33 and 34).
An irregular chain of hills and low mountains, including
the Serra da Farinha and Serra Tabatinga, extends southwest-
ward from the Chapada do Araripe and separates the southern
Sertao from the western Sertao. The latter includes the
semiarid part of the upper Rio Parnaiba Basin.
Most of the streams that drain the Sertao are intermit-
tent and may be dry 5 to 9 months a year. The secondary
streams, in particular, have a torrential regime, and flash
floods are common (see Figure 35). Most rivers and streams
are subject to floods at the onset of the rainy season.
Despite these floods, the average volume of flow is relatively
small during the early part of the season, increasing gradu-
ally as the season progresses. In the northern Sertao the
high-water level is reached in March and sustained until May
(see Figure 36). In the southern Sertao the maximum level is
reached earlier -- late December or early January -- and
lasts until March or April. Within a month after the onset of
the dry season the streams are usually either dry or reduced
to stagnant pools of water occupying depressions along the
streambeds. The Rio Sao Francisco, the Rio Grande, and the
Rio Itapicuru are perennial streams atypical of the Sertao as
a whole.
Dams have been constructed on many streams of the Sertao
to store water for use during the dry season. The dams and
associated reservoirs vary greatly in size, and many smaller
reservoirs dry up during the latter part of the dry season
(see Figure 37).
Climate
The climate of the semiarid Sertao is characterized by
a short rainy season, a long dry season, and great irregularity
in rainfall from month to month and from year to year.
In general, the average annual rainfall ranges between 15
and 30 inches; however, higher amounts are received on mountain
slopes exposed to moisture-bearing winds and along the lowlands
of northern Ceara, and lower amounts are received on the west-
ern part of the Borborema Plateau and in parts of the lower
Sao Francisco Valley. The rainy season occurs in summer (Novem-
ber to April) in most of the area south of the Chapada do
Araripe and in summer and autumn (January to June) in the
northern Sertao (see Figure 38).
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Figure 33. Southern
Sertgo. Hills rise
above the general
surface level to ele-
vations of 2,000 or
3,000 feet.
Figure 34. Slo Fran-
cisco Valley. The
river is deeply en-
trenched downstream
from the falls of
Paulo Afonso.
Figure 35. The Ser-
ta.o. Flash floods
are common.
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Figure 36. High-water
level on stream in
northern Sertao.
Figure 37. Reservoir
in the Sert.o. Dams
have been constructed
across many streams in
the Sert.o.
Figure 38. Storm in
the Sertao. Most of
the rainfall occurs as
scattered showers.
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Little information is available concerning cloudiness
and visibility, but visibility is probably unrestricted 90
percent of the time, except on the windward slopes along
the north coast and on the eastern margin of the Sertao in
Bahia.
The prevailing winds are light and are from the easterly
quadrants.
The Sertao has the highest average annual temperatures
in Brazil, ranging from approximately 68?F on the highest
mountains to nearly 82?F on the northern lowlands. There
is little seasonal variation in temperature;, daily tempera-
ture variation ranges from about 11 to 18 Fahrenheit degrees.
C. Vegetation
A thorny scrub vegetation (caatinga) predominates in the
Sertao. The vegetation in its most characteristic form con-
sists of clumps of thorny trees, bushes, and cactuses sepa-
rated by open areas (see Figure 39). These open areas are
essentially bare during the dry season but are carpeted with
grasses and spiny herbaceous plants during the rainy season.
Most of the trees are low, twisted, and profusely branched.
In the more characteristic clumps of caatinga the branches of
trees, cactuses, and bushes are entangled, forming virtually
impenetrable thickets.
Tropical forest occurs in humid areas on the summit of
the Serra da Ibiapaba, and modified thorn forest occurs along
the western slope. The thorn forest has a dense undergrowth
of high bushes and various cactus species flourish. The stands
are discontinuous and are separated by palm groves and grassy
areas.
The sparse rural population is supported primarily by
open range cattle raising, the cultivation of tree cotton, and
subsistence farming. Specialty crops such as castor beans,
sugarcane, and sisal, as well as various tree crops, are grown
HAD favored locations.
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Figure 39. Caatinga. Clumps of thorn
trees, bushes, and cactuses are separated
by open areas.
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5. Parnaiba - Mearim Area
a. Terrain and Drainage
The Parnaiba - Mearim Subregion is a transitional zone
between the humid Amazon Basin and the semiarid Sertao. It
occupies much of the extensive basin area drained by the
Parnaiba, Itapicuru, and Mearim rivers. The terrain rises
gradually inland from a broad coastal plain through belts of
rolling hills and fragmented tablelands to the Chapada das
Mangabeiras, 2,000 to 3,300 feet in elevation, at the southern
extremity of the region. The terrain also rises eastward
from the Parnaiba Valley to comparable elevations along the
crest of the Serra da Ibiapaba.
Most of the streams are perennial; however, the right-
bank tributaries of the Rio Parnaiba become dry or nearly dry
during the dry season (June through December). The principal
rivers are bordered along their lower reaches by broad flood
plains that are inundated during the high-water period.
Climate
The modified tropical savanna climate has two distinct
seasons -- a summer-autumn rainy season and a winter-spring
dry season. The rainy season extends from November through
April in the southern part of the subregion and from January
through June in the northern part. The average amount of
rainfall received annually increases from southeast to north-
west -- from a minimum of 36 inches to a maximum of 82 inches.
The incidence of fog is relatively high along the extreme
eastern part of the coast -- from the Parnaiba Delta eastward.
Surface winds are variable in the interior, but northeast
trade winds predominate along the coast.
The mean daily temperature of the subregion is about 80?F.
The difference in temperature between the coolest and hottest
months is about 5 Fahrenheit degrees. The daily temperature
range is considerably greater than the annual range, averaging
11 Fahrenheit degrees near the coast and 22 Fahrenheit degrees
at Barra do Corda in the interior.
c. Vegetation
The natural vegetation of the subregion is transitional
between tropical rain forest and thorny scrub, its composition
varying considerably from place to place. Mangrove swamps rim
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the bays and river mouths along the coast, and sand dune vege-
tation -- sparse grasses and low bushes -- covers most of the
intervening coastal segments. An extensive area of marshy
grassland subject to seasonal flooding occurs on the low-lying
land south and west of Bahia de Sao Marcos. Gallery forests
extend along the riverbanks, and discontinuous palm forests
grow along river flood plains and in moist depressions on the
coastal plain (see Figure 40). Small areas of second-growth
forest occur on low hills and stream divides on the coastal
lowland and in the adjacent belt of rolling .tills. Various
gradations of woodland savanna and dry forest cover the table-
lands.
d. Land Use
Collecting forest products, primarily babassu nuts and
carnauba wax, constitutes one of the principal economic activi-
ties of the subregion. Large numbers of range cattle are
grazed on the tablelands. Rice, cotton, manioc, sugar, and
25X6bsistence crops are grown along the principal valleys.
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ATLANTIC
7 Zona de M-
2 Ayrc re
3 sanao
a Chapada do Aradpa
b Norrhern Mounral. end 11111 Chain,
t Northern Law Plareau. and Plain,
d Wcrzern Borborama
e Southern Sert o
Wc.rcrn Scnao
4Parnaiba-Mcarim
Paula Afons 2 1
BRAZIL
NORTHEASTERN REGION
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Figure 40. Carnauba grove. This palm is dominant in
the palm forests east of the Rio Parnaiba.
Figure 41. Serra do Espinhaco. Mountain ridges mark
the eastern margin near Ouro Preto.
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E. Eastern Region
See Map 55897
1. General
The populous Eastern Region is a complex area of hills,
basins, and low mountains. It includes the states of Espirito
Santo, Rio de Janeiro, and Guanabara, together with southern
Bahia, most of Minas Gerais, and the extreme eastern part of
Sao Paulo.
The region is divided into three subregions: the Central
Highland, the Eastern Slope, and the Sao Francisco River Basin.
The Central Highland, extending north-south through the center
of the region, forms the high main water divide separating the
dissected Eastern Slope from the Sgo Francisco River Basin.
Central Highland
a. Terrain and Drainage
The Central Highland consists of two mountain ranges and
a broad dissected plateau -- the Serra do Espinhaco, the Serra
da Mantiqueira, and the Southern Minas Plateau.
The Serra do Espinhaco, 2,500 to about 6,900 feet in ele-
vation, extends roughly from Consel.heiro Lafaiete, in Minas
Gerais, northward to the Chapada Diamantina. It is a highland
belt whose summit area is flat to rolling along some sectors
but is dissected into a confusion of ridges, hills, and deeply
incised river valleys along other sectors (see Figures 41
through 44). The eastern and western margins of the highland
belt are marked by steep slopes in most places.
W,
AM
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Figure 42. Southern Serra do Espinhago. The interior is
hilly near Itabirito.
Figure 43. Serra do Espinha~o. This gently rolling high-
land area is located between Itabirito and Belo Horizonte.
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Figure 44. Serra do Curral. This is a segment of
the Serra do Fspinha~o near Belo Horizonte.
Figure 45. Peixoto Dam across Rio Grande on Southern
Minas Plateau.
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Only the western part of the Serra da Mantiqueira lies
within the subregion. It extends from the extreme southern
corner of Minas Gerais northeastward along the edge of the
Southern Minas Plateau to Barbacena. The south-facing slope
of the range rises abruptly 2,000 to 7,000 feet above the
adjacent Paraiba do Sul Valley -- the main transportation
corridor linking Sao Paulo and Rio de Janeiro. The north-
facing slope merges with the Southern Minas Plateau.
The Southern Minas Plateau constitutes the upper drainage
basin of the Rio Grande and slopes gradually northwestward
from the Serra da Mantiqueira toward the Parana Basin. Much
of the plateau has been dissected into a sea of low hills that
rise to a common summit level (see Figures 45 and 46).
Most mountain streams of the Serra do Espinha;o and the
Serra da Mantiqueira flow through narrow, steep-sided valleys
interrupted by rapids and falls, whereas the rivers of the
Southern Minas Plateau meander along broad valleys that are
marshy in places. Most streams are perennial, although some
of the mountain streams originating on dry leeward slopes are
intermittent. High water occurs from November through April
or May in the greater part of the subregion, and low water
occurs in the winter, reaching the lowest level in August or
September.
The Furnas Dam backs up the waters of the Rio Grande and
its tributary, the Rio Sapucai, forming an extensive reservoir
in the north-central part of the Southern Minas Plateau.
Climate
The mild climate reflects the cooling effects of altitude.
Distinct dry and rainy seasons are experienced throughout the
subregion. The average annual rainfall ranges from 25 to 79
inches -- increasing in amount from north to south and from
west to east. The rainy season extends, in general, from Octo-
ber or November through March or April.
Cumulus clouds predominate over the highlands. During the
rainy season clouds may envelop the windward slopes of the
higher mountain ridges in the afternoon, when the greatest
cloud development normally occurs. Early morning fog occurs
along the southern and eastern margins of the subregion on an
average of 60 to 90 days per year.
Surface winds are generally relatively weak, but high
winds may be experienced briefly during thunderstorms. Wind
directions are primarily from the easterly quadrants.
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Figure 46. Southern Minas Plateau. Rugged terrain prevails
along the southwestern border.
Figure 47. Vegetation on Central Highland. Open grasslands
occur locally on flat to rounded summit areas.
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The mean annual temperature ranges from a low of 53?F on
the highest part of the Serra da Mantiqueira to a high of 72?F
in the northern Espinha~o. Similarly, the mean maximum tempera-
ture ranges from 57?F to 82?F, and the mean mimimum temperature
ranges from 50?F to 60?F.
c. Vegetation
The natural vegetation ranges from caatinga and woodland
savanna to open grassland and scattered tracts of second-growth
forest.
Caatinga predominates in the drier northern part of the
Serra do Espinhaco. It consists of clumps of thorny trees,
bushes, and cactuses separated by open areas that are covered
with grasses and spiny herbaceous plants during the rainy season
and are bare during the dry season.
The woodland savanna is the predominant vegetation on the
middle and southern parts of the Serra do Espinhaco and along
the northern margin of the Southern Minas Plateau. It consists
of a ground cover of grasses and herbaceous plants interrupted
by scattered trees and clumps of trees and shrubs. The grasses
flourish during the rainy season but dry up during the dry
season.
The patches of second-growth tropical semideciduous forest
generally occur on the steeper slopes in humid areas of the
highland. About 10 to 30 percent of the trees in the forest
stands lose their leaves during the dry season. The stands are
relatively dense, and numerous lianas are interlaced among the
trees.
The grasslands, which are characterized by a sparse growth
of grasses, mosses, and small bushes, occur on high flat-to-
rounded summit areas (see Figure 47).
d. Land Use
The northern and central parts of the Serra do Espinha~o
are sparsely populated, and the principal economic activity is
open range grazing. In the southern part the population is
primarily centered around the iron mining and metallurgical
centers. A sparse population occupies the intervening rural
areas, where subsistence farming and livestock grazing are the
principal agricultural activities.
The Campos do Jord.o area of the Serra da Mantiqueira has
become an important health and tourist resort center. Horti-
culture is practiced along the broad river valleys of this area,
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and range cattle are grazed on the grassy rounded summits.
Dairying and subsistence farming are the principal forms of
land use on the lower slopes of the Serra da Mantiqueira.
Mixed farming and livestock raising are practiced on
2's'[5 of the Southern Minas Plateau.
Eastern Slope
a. Terrain and Drainage
The Eastern Slope, by far the largest subregion in the
Eastern Region, encompasses the complex zone of hills, low
mountains, plateaus, and valleys between the Central Highland
and the coast. In general, the land rises in a series of broad
steps from the coast toward the interior, but this progression
is interrupted locally by discontinuous low mountains and by
complex river basins.
The Northern Sector of the subregion consists of a belt
of low coastal hills and/or tablelands (tabuleiros) backed by
a belt of more rugged hills. These, in turn, are backed by
broad segments of the Bahian Plateau (see Figure 48). To the
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south the deeply grooved Jequitinhonha River Basin forms a
transitional zone between the Bahian Plateau and the hilly
Central Sector.
The Central Sector includes a coastal plain and tabuleiro
belt, a complex belt of ridges and valleys situated along the
Espirito Santo - Minas Gerais border (the Serra dos Aimores),
and the Rio Doce Basin, which cuts back through the ridge and
valley complex and spreads out to form a large, hilly basin in
the interior.
The Southern Sector consists of an irregular zone of
coastal lowlands (see Figure 49), the Serra do Mar (known also
as the Great Escarpment of the coastal mountain range) (see
Figures 50 and 51), the drainage basin of the Rio Paraiba do
Sul, and the massive Serra do Caparao and associated highlands
that form the water divide between the Rio Doce and Rio Paraiba
do Sul drainage basins (see Figure 52). The Serra do Caparao
culminates in the Pico da Bandeira, the highest point in Brazil
(elevation 9,482 feet).
The main rivers of the Northern Sector are perennial, but
their flow is greatly reduced from June through August or Sep-
tember, when they meander along wide beds strewn with alluvial
debris. The secondary streams in the interior have a torrential
flow during the high-water period (November through April or
May) but dry up during the dry season. The rivers and streams
of the Central and Southern Sectors are perennial, and most of
them flow along narrow, steep beds interrupted by frequent rapids
and falls. The Rio Doce and Rio Paraiba do Sul are exceptions,
having low gradients along parts of their middle and lower
courses. The period of high water within the Central and South-
ern Sectors generally extends from October through April, with
the highest or flood level occurring in December or January.
Climate
The climate of the Eastern Slope is varied -- ranging
from semiarid to superhumid and from tropical to subtropical.
The amount of rainfall received decreases from the coast inland
and from south to north. A summer rainy season and a winter
dry season are experienced throughout most of the subregion.
In general, the rainy season extends from October or November
through March or April, but along the Bahian coast the maximum
rainfall occurs from March to August. The length and intensity
of the dry season varies markedly, being greatest in the interior
of the Northern Sector and least along the Bahian coast and
along the seaward-facing slopes of the Serra do Mar and Serra
do Caparao. The annual average rainfall ranges from 25 inches
to 157 inches.
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Figure 48. Northeastern margin of Bahian Plateau. Oddly shaped
hills with nearly vertical slopes of bare rock occur locally.
Figure 49. Campos Plain. This extensive coastal lowland is
situated along the lower Rio Paraiba do Sul.
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Figure 50. Serra do Mar between Rio de Janeiro and
Sao Paulo.
Figure 51. Serra do Mar. Parts of the backslope
have been eroded into a sea of hills.
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Figure 52. Rugged terrain along southern margin of
Serra do Caparad.
Figure 53. Coastal rain forest on Eastern Slope.
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Stratus clouds, low ceilings, and poor visibility may all
occur during the passage of cold fronts in winter. In summer,
cumulus clouds may envelop the windward slopes of the mountain
ridges in the afternoon, when the greatest cloud development
normally occurs. Early morning fog occurs on an average of 30
to 90 days per year. The incidence appears to be greatest in
areas of rugged terrain and lowest in the larger valleys that
open toward the east.
Surface winds are generally weak. In the Northern Sector
southeasterly trade winds prevail in winter and easterly winds
tend to predominate in summer. Winds are variable in the Cen-
tral and Southern Sectors.
Average annual temperatures range from a high of 75?F in
the valleys and low hill belts near the coast to a low of about
55?F on the highest mountain crests. Mean annual maximum tem-
peratures range from a high of about 86?F to a low of 65?F;
mean annual minimum temperatures range from a high of approxi-
mately 68?F to a low of less than 50?F.
c. Vegetation
The natural vegetation varies considerably from the coast
inland and, to a lesser extent, from north to south. Mangrove
and beach vegetation extend along the shore. Stands of coastal
rain forest cover some of the windward slopes of the rugged
hills and low mountains that parallel the coast (see Figure 53).
The rain forest gives way to scattered patches of tropical semi-
deciduous forest on rugged terrain in the interior of the sub-
region. In the Northern Sector caatinga predominates on the
western part of the Bahian Plateau. Throughout the subregion
extensive areas have been cut over and are devoted to pasture
or cultivation.
The stands of coastal rain forest are quite similar to the
tropical rain forest of the Northern Region. The trees of the
upper story form a closed canopy. Lower trees and shrubs crowd
the space below the canopy, but no clearly marked stratification
is discernible. The undergrowth is dense, and lianas and dang-
ling aerial roots form a tangled net between trees.
About 10 to 30 percent of the trees in the semideciduous
forest lose their leaves during the dry season. There are num-
erous clearings in the forest, some in various states of re-
growth and others planted in grass or subsistence crops. The
undergrowth is generally dense.
Caatinga vegetation consists of virtually impenetrable
thickets of low trees, bushes, and cactuses, interspersed
among generally open areas.
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Cacao cultivation and livestock grazing are the princi-
pal forms of land use in the Northern Sector? Cacao is grown
on low hills near the coast, and livestock is raised on the
plateaus, valleys, and lower hill slopes in the interior (see
Figure 54).
The basic pattern of land use in the relatively densely
populated Central Sector consists of cattle raising and shift-
ing cultivation. However, coffee growing is significant in
parts of the Rio Doce Basin and on the eastern slopes of the
Serra dos Aimores, and some sugarcane is grown along the main
river valleys. Mining and metallurgy are important in the
western part of the Rio Doce Basin and along the eastern slope
of the Serra do Espinhaco. Some of the forests are exploited
for wood and charcoal (see Figure 55).
Land use is varied in the Southern Sector. Dairying and
shifting cultivation are widespread. Coffee, sugarcane, and
rice are important commercial crops (see Figure 56). Several
industrial centers have developed along the valley of the Rio
Paraiba do Sul, and several resort towns are located on the
25LUit of the Serra do Mar.
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Figure 54. Cacao cul-
tivation on low hills
along Bahian coast.
Cacao is grown in the
shade of stands of
partially cutover
forest.
Figure 55. Charcoal burn-
ers at work.
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Figure 56. Harvesting sugarcane and maize. View
is along the middle basin of the Rio Paraiba do Sul.
Figure 57. Escarpments in the Zona da Mata of
Minas Gerais.
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4. Sao Francisco River Basin
a. Terrain and Drainage
The upper basin and part of the middle basin of the Rio
Sao Francisco fall within the Eastern Region. The headwaters
of the river are situated along the northern margin of the
Southern Minas Plateau. The basin is bordered on the east by
the scarped slopes of the Serra do Espinhato and on the west
by the bluffs of the Espig,o Mestre. The upper basin is gen-
erally hilly (see Figure 59), whereas most of the middle basin
consists of broad, relatively flat surfaces, separated by stream
valleys cut below the general surface level. Scattered rocky
hills rise above the basin floor at various places. The main
river is bordered by a broad marshy flood plain.
Most of the tributary streams south of the Bahia - Minas
Gerais border are perennial; in contrast only the main rivers
are perennial north of the border, where many secondary streams
flow only after rainstorms and some may be dry several years
in succession. Numerous small lakes, marshes, and swamps are
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Figure 58. Shore near Cabo Frio. Beaches are backed by sand
dunes.
ARk
Figure 59. Maze of dissected low hills within upper Sao Fran- Ask
cisco River Basin.
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1
BRAZIL
EASTERN REGION
Physical Division Boundaries
Region
- Subregion
---- Minor unit
Central Highland
a Serra do Eapinhee
IS er a da Manttqueire
I Southern Ml- Plateau
Eastern Slope
a Northern Sector
bCcntral Sector
e Southern Sector
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scattered along the flood plain of the main river. The water
level on the Rio Sao Francisco usually starts to rise in Novem-
ber and reaches its highest level in December or January. The
period of low water generally occurs between June and October.
The Tres Marias Dam across the Rio Sao Francisco has formed
a sizable reservoir along a 60-mile segment of the upper river
valley.
b. Climate
A tropical savanna climate, characterized by a distinct
summer rainy season and winter dry season, prevails over most
of the subregion. The length of the rainy season varies from
3 to 6 months, increasing from north to south. The average
annual rainfall ranges from a low of about 30 inches at the
northern border of the subregion to a high of about 60 inches
along its southern margin.
Little reliable information is available on the winds of
the subregion. Normally, there are no high winds other than
gusts accompanying thundershowers. Visibility is generally
good, except during summer showers.
The average annual temperature normally decreases from
north to south and from the basin floor to the bordering high-
lands. The mean annual temperature ranges roughly from 70?F
to 79?F. The mean minimum temperature ranges from 60?F to 71?F3
and the mean maximum from 79?F to about 93?F.
Vegetation
The vegetation consists mainly of caatinga and woodland
savanna, although bands of gallery forest extend along the
river valleys.
Caatinga predominates in the part of the basin extending
northward from the Bahia - Minas Gerais border.
Woodland savanna predominates south of the state boundary.
This vegetation consists basically of sparse natural grassland
with scattered trees and clumps of trees and shrubs. The grass
is high during the rainy season but dries up during the dry
season.
Semideciduous gallery forest border most of the rivers in
the basin. These forest belts are relatively broad south of
the Bahia - Minas Gerais border and spread out over the flood
plain of the Rio Sao Francisco and its principal tributaries.
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d. Land Use
Much land is devoted to livestock grazing. Cattle are
raised in the zone of woodland savanna, and goats and donkeys
are grazed on the caatinga. Subsistence crops are grown in
many localities in the southern part of the subregion and in
humid areas in the north. Castor beans and cotton are fre-
quently raised as cash crops by subsistence farmers. Fish are
caught in considerable quantity from the sandbars along the
Southern Region
See Map 55899
1. General
The Southern Region, consisting of the states of Rio Grande
do Sul, Santa Catarina, Parana, and most of S!.o Paulo, is the
smallest of the five regions of Brazil. It enjoys a relatively
cool climate, and is the most populous and the most economically
developed part of the country.
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The principal terrain units of the region are the extensive
Southern Plateau and the Eastern Slope. The Southern Plateau
encompasses about 75 percent of the area and varies considerably
in surface configuration from state to state. The Eastern Slope
consists of the dissected eastern edge of the plateau and the
coastal belt at its base.
2. Southern Plateau
a. Terrain and Drainage
The Southern Plateau rises abruptly above the narrow coast-
al zone and slopes gradually westward to the valleys of the Rio
Parana and Rio Uruguai. In the northern half of the subregion
the plateau is divided into three segments, known as the First
Plateau, the Second Plateau, and the Third or Western Plateau.
The segments are situated at different elevations and separated
from each other by roughly parallel lines of escarpments. These
escarpments are breached by the principal westward-flowing
rivers that drain the plateau. The Third Plateau is by far the
most extensive, and it constitutes the entire plateau in the
southern part of the subregion. The plateau decreases in ele-
vation both from east to west and from north to south. The low
undulating section in the southwestern part of Rio Grande do
Sul forms part of the cattle-raising zone known as the Campanha
Gaucha (see Figure 60).
The First Plateau is hilly, and the relief is generally
rugged (see Figures 61 and 62). The Second Plateau is an area
of generally low relief, and, in S.o Paulo, it is called the
Inner Lowland since it is situated below the general surface
level of the other segments of the plateau (see Figure 63).
Historically, it has served as a natural corridor of movement --
particularly as the route of the famous cattle and mule drives.
The Third Plateau is one of the largest lava plateaus in the
world, and it exhibits a relatively uniform tabular relief
(see Figures 64 and 65). The steep-sided valleys of the prin-
cipal rivers subdivide it into a series of broad, roughly
parallel surfaces trending from east-southeast to west-north-.
west.
Flood plains are generally lacking along the rivers of
the First Plateau. On the Second Plateau, however, the main
rivers meander along broad, marshy flood plains. On the Third
Plateau the valleys vary in width in different sectors, and
marshy flood plains occur along some of the wider sectors. In
general, the river courses are interrupted by scattered falls
and rapids, and most of the minor tributaries on the Third
Plateau enter the main valleys over such obstacles. The Rio
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Figure 60. Low undu-
lating surface of
Campanha Gaucha.
Figure 61. First Plateau south-
east of Sao Paulo. The Rio
Grande Reservoir is in the back-
ground.
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Hills east of Campinas. Coffee cultivation in
Figure 62. ground; and patches
the foreground; pastures in the middle g
of forest in the background on the hilltop and steep slopes.
Figure 63. The Second Plateau. The area is of gen-
erally low relief. -85-
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Figure 64. The Third Plateau. The area is flat to
gently rolling in the vicinity of Londrina, Parana.
Coffee is grown extensively on the terra roxa soils
in this area.
A*
Figure 65. The Third Plateau. Narrow V-shaped val-
leys are cut below the general surface level along
the high eastern margin in Rio Grande do Sul.
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Figure 66. Rio Parand and flood plain upstream
from Guaira.
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Figure 67. Iguacu Falls. Tributaries, such as the Rio
Iguacu, enter the canyon of the Rio Parana over falls
situated at the heads of short side canyons.
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Parana is a broad river of low gradient downstream as far as
Guaira, where it flows over spectacular waterfalls (see Figure
66). Below the falls the river is confined within canyon walls,
and all the tributaries that enter it along this sector flow
over waterfalls (see Figure 67).
Rivers and streams are perennial, but minor tributaries
are generally quite shallow at low-water stage. In Sao Paulo
and northern Parana the period of high water extends from Novem-
ber or December through April or May. In southern Parana and
Santa Catarina there is a slight spring-summer rainfall maxi-
mum; however, the period or periods of high water vary somewhat
locally. In Rio Grande do Sul the high-water period extends
from April or May through October or November (see Figure 68).
b. Climate
The climate of the Southern Plateau ranges from tropical
savanna in northern Sao Paulo to humid subtropical in southern
Parana, Santa Catarina, and Rio Grande do Sul. A zone of tran-
sitional climate occurs in southern Sgo Paulo and northwestern
Parana.
The amount and seasonal distribution of rainfall varies
considerably within the subregion. Areas of heaviest rainfall
coincide with higher elevations situated in the path of mois-
ture-bearing winds. The average annual rainfall ranges from
40 inches to more than 80 inches. In most of Sao Paulo and
extreme northwestern Parana, rain falls primarily during the
summer (October through March). Rain occurs throughout the
year in Santa Catarina and most of Parana, with a slight maxi-
mum during the spring-summer period. In Rio Grande do Sul the
maximum amount of precipitation occurs during the autumn-winter
period. In mid-winter frontal passages frequently bring snow
to the higher parts of the plateau in Rio Grande do Sul. Snow
seldom remains on the ground for more than a few days, however.
Dense fogs and low clouds restrict visibility along the
coastal margin of the plateau. Fog occurs here about 9 to 18
days per month during the autumn-winter period (April through
August) and with lesser frequency during the rest of the year.
Dense fogs also occur from 6 to 12 days per month during the
autumn-winter period along the Uruguai Valley and along segments
of the Parana Valley. Visibility is generally unrestricted in
other parts of the subregion about 90 percent of the time.
Surface winds are generally weak. High winds, when they
occur, are associated with thunderstorms. Wind direction varies
considerably, but winds from easterly quadrants tend to dominate.
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The temperature decreases from north to south and with
increased elevation. The mean annual temperature ranges from
about 60?F to 74?F. The mean minimum temperature ranges from
50?F to 64?F, and the mean maximum temperature ranges from
68 OF to 860F. Frosts occur from 5 to 25 days per year in the
southern part of the subregion. The incidence of frost ranges
from 5 days a year to 1 day in two years.
c. Vegetation
The vegetation of the Southern Plateau consists of tropi-
cal semidecicjuous forest, Parana pine forest (arauceria)
natural grassland, and woodland savanna. '
Some virgin stands of tropical semidec_Lduous forest remain
on parts of the plateau in northwestern Parana and along the
middle and lower valleys of the principal rivers in that state.
Scattered small tracts of forest remain on steep slopes and
along stream courses in S,o Paulo. In general, the undergrowth
is dense, and lianas and dangling aerial roots form a tangled
net between trees.
A Parana pine forest grows on parts of the plateau within
southern :Parana, Santa Catarina, and northern Rio Grande do
Sul (see Figure 69). The Parana pine is a tall needle-leaf
evergreen tree with an umbrella-shaped crown. The upper tree
layer, consisting primarily of tall pines, has an open canopy.
Various broadleaf evergreen trees and shrubs, including the
erva-mate, form a relatively dense lower story. The erva-mate'
(Paraguay tea plant) is exploited commercially, and in some
stands competing tree species of the lower story are cut in
order to promote its growth. The forest stands are relatively
free of lianas and epiphytes.
The grasslands a>e of two kinds -- treeless savannas
(campos limpos) and prairie. Treeless savannas extend along
the eastern part of the Second Plateau and occur in several
areas of high elevation on the Third Plateau in Parana, Santa
Catarina, and Rio Grande do Sul (see Figure 70). The prairie
grasslands cover the low undulating surface of the Campanha
Gaucha in southwestern Rio Grande do Sul.
The scattered small areas of woodland savanna in the sub-
region occur mainly on the Second Plateau within Sgo Paulo.
The woodland savanna consists of clumps of low, twisted trees
and shrubs dispersed over a sparse mantle of grasses and other
herbaceous plants.
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Figure 68. Campanha Gaucha. Rio Ibirapuit. in flood.
Figure 69. Parana' pine forest. Pines form an open upper
story, and various small trees and shrubs form the dense
lower story.
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d. Land Use
Land use varies considerably within the subregion. Tropi-
cal crops, such as coffee, cotton, sugarcane, and citrus fruits
are grown commercially in Sao Paulo and in parts of northern
Parana (see Figure 71) and crops that can withstand light frosts,
such as wheat, barley, and potatoes, are grown in the southern
part of the subregion. In Slo Paulo commercial crops are gen-
erally grown on large plantations; in the southern states they
are grown on small to medium-sized land holdings. Mixed farm-
ing is common in parts of eastern Sao Paulo on former coffee
lands exhausted from extended one-crop farming. On these lands
dairying is practiced in conjunction with the cultivation of
various cash and subsistence crops. Maize, rice, and manioc
are subsistence crops cultivated throughout the subregion. In
many areas of the southern part of the subregion hogs, fattened
on maize, are produced in conjunction with subsistence farming.
Cattle grazing is common throughout. The fattening of cattle
on improved pastures is characteristic of Slo Paulo, and the
grazing of cattle on natural grasslands is more characteristic
of the southern states (see Figure 72).
Industry is concentrated mainly within the greater S lo
Paulo urban area and in cities located along the fall line
separating the first and second segments of the plateau in
25 state of Sao Paulo.
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Figure 70. The Campos de Guarapuava. One of sev-
eral grassland areas on the highest elevations of
the Third Plateau.
Figure 71. Citrus plantation on Second Plateau
near Campinas, Sgo Paulo.
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Figure 72. Range cattle on prairie grasslands of
Campanha Gadcha.
Figure 73. Lines of cliffs separating differe:11t surface
levels on Southern Plateau. These sandstone cliffs are at
Vila Velha, Parana..
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Figure 74. Steep, forested slope of
Great Escarpment northwest of Santos.
Figure 75. Coastal lowland near
Santos viewed from Great Escarpment.
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Eastern Slope
a. Terrain and Drainage
The Eastern Slope Subregion includes the dissected east-
ern edge of the Southern Plateau and the coastal zone situated
at its base. The subregion ranges in width from a minimum of
about 5 miles in eastern Sdo Paulo to a maximum of about 250
miles in southern Rio Grande do Sul. Its western boundary is
the water divide separating rivers that drain eastward directly
to the Atlantic Ocean from those draining westward into the
Parana - Uruguai drainage system. The Great Escarpment, which
marks the edge of the plateau along most of its extent, appears
from the coast as a formidable mountain range rising sharply
2,000 to 6,000 feet above the coastal lowland (see Figures 74
and 75). Various local names are applied to the different seg-
ments of the range -- the Serra do Mar, the Serra do Paranapia-
caba, and the Serra Geral (see Figure 76). This mountain
facade has been breached by two rivers, the Rio Ribeira de
Iguape and the Rio Itajai, which have carved out rugged upper
basins in back of the facade (see Figure 77). In southern
Rio Grande do Sul the Great Escarpment curves abruptly inland,
and the subregion widens to encompass a broad central lowland
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Figure 76. Serra do Paranapiacaba viewed from Ribeira de
Iguape Basin.
Figure 77. Steep hills along segment of Itajai Basin.
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(the Jacui Valley), a hill zone in the southeastern part of
the state, and a broad coastal plain rimmed. by extensive
lagoons and a long barrier island.
The streams of the subregion are perennial. They descend
the slopes of the Great Escarpment to the narrow coastal low-
land via precipitous courses marked with numerous falls and
rapids. Extensive areas of marsh and swamp border their
meandering courses near the coast. The stream network of
southern Rio Grande do Sul differs from that in the rest of
the subregion. There the principal streams -- the Rio Jacui
and Rio Camaqu. -- have longer courses and empty into the
coastal lagoons rather than directly into the ocean. The
flow of streams descending the Great Escarpment, always swift,
is frequently torrential during the rainy season. On the
coastal lowland at the foot of the escarpment these streams
are generally sluggish except at flood stage. The period of
high water occurs from November or December through April or
May in the northern part of the subregion, and from May to
September in the southern part. Two periods of high water
occur on some streams in the transition zone in Santa Catarina
and northern Rio Grande do Sul.
b. Climate
The climate of the subregion is humid subtropical except
for an area of superhumid tropical climate along the coast of
Sao Paulo. There is no distinct dry season in this subregion.
The rainfall exceeds 60 inches along most parts of the
Eastern Slope southward as far as Florianopois, Santa
Catarina. The amount of rainfall increases with elevation,
and exposed locations on the upper slopes of this sector
receive more than 120 inches. From Florianopolis southward
the rainfall decreases from 60 inches to 46 inches near the
Uruguay border. It increases inland to between 50 and 60
inches on the central lowland and southeastern hills of Rio
Grande do Sul. The seasonality of rainfall varies within
the subregion. Autumn-winter rainfall predominates in Rio
Grande do Sul, but a summer maximum occurs in the rest of
the subregion. Some snow falls in winter on the south
slope of the Serra Geral and in the southeastern hills.
The incidence of dense fog and low clouds is relatively
high, particularly along the Great Escarpment, with the high-
est frequency being from April through August,.
The predominant winds in the northern half of the sub-
region are from the southerly quadrants. In the southern half
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of the subregion the northeast wind is dominant, although it
is interrupted periodically by southeasterly and westerly
winds. Gale winds seldom blow.
The mean annual temperature increases from south to north
and from the summit of the Great Escarpment to the coastal low-
land. Along the coastal lowland it ranges from about 62?F at
the southern extremity to 72?F at the northern extremity. Along
the summit of the escarpment it ranges from 60?F to 68?F. The
mean minimum temperature ranges from 55?F to 64?F on the low-
lands and from 50?F to 57?F on the escarpment. Similarly, the
mean maximum temperature ranges from 71?F to 82?F on the low-
lands and from 68?F to 78?F on the escarpment.
Frosts occur in southern Rio Grande do Sul and at higher
elevations throughout the subregion.
C. Vewetation
The vegetation consists of coastal rain forest, a coastal
complex of mangrove and beach vegetation, and a zone of prairie
grassland in southern Rio Grande do Sul.
Luxuriant coastal rain forest covers the steep slopes of
the Great Escarpment, as well as parts of the coastal lowland.
The forest is almost as rich and varied in composition as the
Amazonian rain forest. Lianas and epipr.,,tes are common. The
trees are reduced in size and somewhat deformed in appearance
at the higher elevations. Mosses, lichens, and epiphytes are
very abundant at these elevations due to the high frequency
of rain, mist, and fog.
The southern slope of the Serra Geral has been mostly
deforested, except for the highest and steepest slop,-,:; second-
growth forest in various stages of growth is interspersed
among cultivated fields and pastures.
Along sandy coasts a thin cover of grasses and creeping
plants extends over the inner margin of the beaches and on low
dunes. On the higher dunes and on beach ridge plains the vege-
tation consists of a dense tangled growth of stunted trees,
thorny bushes, and cactuses. Mangroves reach their southern
arana - Santa Catarina border.
limit along the coast near the Parana'
They fringe the shallow parts of bays and river mouths and
frequently extend several miles inland along the tidal reaches
of rivers (see Figure 78).
Prairie grassland predominates on the central lowland
and in the southeastern hills of Rio Grande do Sul, although
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tropical semideciduous forest covers the summits of the highest
hills. These forest stands are lower and much less luxuriant
than the stands of coastal rain forest characteristic of the
Great Escarpment.
d. Land Use
Primitive subsistence farming and firewood extraction are
carried on in some parts of the Great Escarpment. Hogs, fat-
tened on maize, and various subsistence crcps are raised in
the Ribeira de Iguape and the Itajai river basins and along
the southern slope of the Serra Geral (see Figure 79). Along
the coast in the northern part of the subregion the population
is centered primarily at the ports, and some fishing villages
are dispersed along the shore. Along the more densely popu-
lated Santa Catarina coast, coffee and bananas are grown on
the lower hill slopes, and sugarcane and paddy rice are grown
along the river flood plains (see Figure 80). Livestock graz-
ing is the principal activity in the southeastern hills and on
the central lowland of Rio Grande do Sul, although paddy rice
is raised along the Rio Jacul flood plain and on the coastal
plain along the west side of Lagoa dos Pates (see Figure 81).
Several coal mines are located in the foothills of the
Serra Geral in southern Santa Catarina and on the central low-
25X66 d of Rio Grande do Sul, near Sao Jeronimo.
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Figure 78. Mangroves. They extend along the
tidal reaches of rivers and fringe the shallow
parts of bays.
Figure 79. Small farm on southern slope of Serra Geral, Rio
Grande do Sul. -101-
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AiXAI
Figure 80. Ricefields on Santa Catarina coastal plain.
Figure 81. Harvesting rice on central lowland of
Rio Grande do Sul, near Porto Alegre.
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1c
4, c `~ itiba0r a"~P
/"~ \ cemOlnas
/Jerd mo da Serra 'ti la.!N
pNOU NAS P,grEf 1
q \ ~JOinville'
f 1
P J., a "men "
L. ;G
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i : {~c ,Pal ree do Sul
BRAZIL
SOUTHERN REGION
Physical Division Roundarlas
Reglon
~?- Subregion
Minor unit
1 Southern Plareau
a Fk. Plvreeu
b sr~aaa Pmta.a
Thud lrte.
d Cmv.nhe Ge4ch.
2 aaarn siay.
Scale 1:4,000,000
i.mli~m~TT.
roo
~ ., s,
iTease- t09/2~ : C1A=RD 0004-8
d?. ~t J parulbe'
6
/~_~ ~f
,
~
Cas`ro/
~~./ Jr2 P /Ilha Comprid.
L~ndia
5X6 D
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S-E-C-R-E-T
Gazetteer
Place Name
Coordinates
Alcantilados Plateau
17?00'S 54?00'W
Amazon River
00?10'S 49?00'W
Bahia de Sao Marcos
02036'S 44?28'W
13ahiari Plateau
140401S 40?30'W
Baia de Marajo
01?00'S 48?30'W
Barbacena
21?14'S 43?46'W
Barra do Corda
05?30'S 45?15'W
Belo Horizonte
19?55'S 43?56'W
l3orborema Plateau
07?00'S 37?00'W
Braganrca
01?03'S 46?46'w
Brasilia
15?47'S 47?55'W
Campanha Gaucha
30?00'S 56?00'W
Campos do Jordao
22?44'S 45?35'W
Chapada das Mangabeiras
10?15'S 45?45'W
Chapada Diamantina
11?30'S 41?15'W
Chapada do Araripe
07?20'S 40?00'W
Conselheiro Lafaiete
20?40'S 43?48'W
Corumba
19?01'S 57?39'W
Cuiaba
15?35'S 56?05'W
Espigo Mestre
14?00'S 46?10'W
111orianopolis
27?35tS 48?34'W
Furnas Dam
20?40tS 46?20'W
Furnas Plateau
17?00'S 54040'W
-104-
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Coordinates
Goias
15?56'S 50?08'W
Guaira
24?04'S 54?15'W
Ilha de Marajo
01?oo'S 49?30'W
Itabirito
20?15'S 43?48'W
Lago Grande Do Curuai
02?15'S 55?20'W
Lagoa dos Patos
31?06'S 51?15'W
Lagoa Mirim
32?45'S 52?50'W
Macapa
00?02'N 51?03'W
Manaus
03?08's 60?ol'W
Mato Grosso de Goias
16?3o'S 49?30'W
Natal
05?47'S 35?13'W
Ouro Preto
20?23'S 43?30'W
Paraguay River
27018'S 58?381W
Paulo Afonso
09?24'S 38?13'W
Pelotas
31?46'S 52?20'W
Pico da Bandeira
20?26'S 41?47'W
Priapora
17?21'S 44?56'W
Porto Alegre
30?04'S 51?11'W
Porto Lsperanca
19?37'S 57?27W
Rio Araguaia
05?21'S 48?41'W
Rio Branco
01?24'S 61?51'W
Rio Camaqu
31?17'S 51?47'W
Rio Corrente
13?08'S 43?28'W
Rio Cuiaba
17?05'S 56?36'W
Rio das Mortes
11?45'S 50?44'W
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Ii "-
Place Name
Rio das Mortes Plateau
Rio das Velhas
Rio de Janeiro
Rio Doce
Rio Grande
Rio Grande
Rio Grande
Rio Itajai
Rio Itapicuru
Rio Itapicuru
Rio Jacui
Rio Jequitinhonha
Rio Juruena
Rio Madeira
Rio Mearim
Rio Negro
Rio Negro
Rio Paracatu
Rio ParaguaQu
Rio Paraiba do Sul
Rio Parana
Rio Parnaiba
Rio Ribeira de Iguape
Rio Sf,o Francisco
Coordinates
15?oo'S 54?001W
17?13'S 44?49'W
22?54'S 43?14'W
19?37'S 39?49'W
11?05'S 43?09'W
20?06'S 51?04'W
320021S 520051W
26?54'S 48?33'w
02?52'S 44?12'W
11?47'S 37?32'W
30002'S 51?15'W
15?51'S 38?53'w
07?20'S 58?03'W
03?22'S 58?45'W
03?04'S 44?35'W
03?08'S 59?55'W
19?13'S 57?17'W
16?35'S 45?o6'W
12?45'S 38?54'W
21?37'S 41?03'W
33?43'S 58?17'W
03?00'S 41?50'W
24? 40' S 47?24'W
10?30'S 36?24'W
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Place Name
Coordinates
Rio Sapucai
20?43'S 46008'W
Rio Teles Pires
07?21'S 58?03'W
Rio Tocantins
01?45'S 49?lo'W
Rio Uruguai
34?12'S 58?18'W
Rio Xingu
01?30'S 51?53'W
Salto das Sete Quedas
24?02'S 54?16'W
Salto do Urubupunga
20?36'S 51?33'W
Salvador
12?59'S 38?31'W
Sao Paulo
23-321S 46?37'W
Serra da Bodoquena
21?00'S 56?50 'W
Serra da Farinha
08?42'S 41?21'W
Serra da Ibiapaba
04?00'S 41?00'W
Serra da Mantiqueira
22?00'S 44?45'W
Serra das Araras
16?00'S 57?25'W
Serra do Caparao
200221S 41?48'W
Serra do Espinhaco
17?30 'S 43?30 'W
Serra do Mar
23000'S 44?50 'W
Serra do Paranapiacaba
24?00'S 47?50 'W
Serra do Urucum
19?13'S 57?33'W
Serra dos Aimores
19?00'S 41?00 'W
Serra dos Cariris Velhos
07?30'S 37?00 'W
Serra Geral
27?40s 49? 40 'W
Serra Tabatinga
10? 25 'S 44? 00 'W
Southern Minas Plateau
21?30'S 45?00 'W
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Place Name Coordinates
`I'ris Marias Dam 18? 1:L' S 45?15 W
TriAngulo Mineiro 19?00'S 48000'W
Zona da Mata of Minas Gerais 21?301S 43?00'W
AOk
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agreste
beach ridge
beach ridge plain
(restinga)
caatinga
campo limpo
campo cerrado
chapada
cuesta
epiphyte
Scrub woodland; a type of natural
vegetation transitional in nature
between tropical forest and thorny
scrub.
An elongated island comprised of
multiple beach ridges extending
generally parallel to the coast
but separated from the coast by a
lagoon, bay, or marsh; the island
commonly has dunes and narrow,
elongated swampy areas.
A ridge of sand and gravel built
up along the beach by wave action.
A plain consisting of parallel
lines of beach ridges separated
by narrow swales.
Thorny scrub vegetation; a type
of natural vegetation character-
istic of the semiarid Sertao.
"Clean" savanna; open grassland
devoid of trees.
A tableland, generally steep-
sided and more than 600 meters
(about 2,000 feet) nigh.
A sloping plain or tilted table-
land having a scarp face at its
raised end and a gentle back slope.
An air plant; a nonparasitic plant
that grows on another plant but
gets its nourishment from the air.
Rainfall induced as the result of
the interaction of dissimilar masses
or currents of air brought together
along a frontal surface.
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gallery forest
igarape'
Bands of forest occurring along
both banks of a river in what is
otherwise a region of open country.
A canoe passage; a seasonal, nar-
row waterway occurring on a flood
plain and often parallel to the
main river (Northern Region).
intermittent stream A stream that flows part of the
year and is dry the remainder of
the year.
me s a
natural levee
nearshore approach
offshore approach
A woody, climbing, tropical vine
that roots in the ground; occurs
entwined snakelike about tree
trunks and, often, entwined in
the tree crowns as well; flexible
stems hang down from the crowns
like ropes.
A type of swamp formed on tidal
land consisting primarily of
species of mangrove; the common
or red mangrove has stilt roots;
the overlapping roots of these
trees are covered by water at
high tide but rise above the mud-
flats at low tide forming a "king-
size jungle gym".
A flat-topped, steep-sided hill
or mountain of smaller extent
than a plateau.
The low ridge sometimes built up
by streams on their flood plains
on either side of their channels.
The sea area wh_ch extends from
the 30-foot (5-fathom) depth con-
tour to the low--water line of the
beach.
The sea area wh_ch extends from
approximately the 600-foot (100-
fathom) depth contour to the 30-
foot depth contour.
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planalto
restinga
slough
sertao; Sertlo;
sertoes pl.)
slash-and-burn
cultivation
tropical
semideciduous
forest
woodland savanna
(campo cerrado)
A former beach, now elevated above
high-water level.
See beach ridge plain.
A broad term applied to a tropical
or subtropical grassland containing
scattered trees.
A marshy place lying in a local
depression of dry land.
A shallow, elongated depression
that is at least seasonally wet or
marshy.
Mountain range; applied locally to
any topographic feature exhibiting
strong relative relief.
Backland or remote interior; a
subregion comprising the semiarid
interior of the Northeastern Region.
Shifting cultivation; a form of
agriculture in which fields are
cleared by burning and are culti-
vated for a short period of years
until the soil shows signs of
exhaustion, after which the land
is left to the natural vegetation
while cultivation is carried on at
a new site.
A low, steep-sided tableland.
Firm ground; land not subject to
inundation.
Tropical forest composed mostly
of broadleaf evergreen species,
but with some broadleaf deciduous
species.
A type of savanna vegetation con-
sisting of grassland with parklike
stands of low trees and shrubs;
grassland with scattered thickets
of deciduous scrub forest.
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xerophytic
Drought resistant; capable of
thriving in a hot, dry climate,
as certain plants and animals.
A
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READING LIST
1. Azevedo, Aroldo de, Brasil: A Terra e o Homem, vol I,
Sao Paulo: Companhia Editora National, 19. U.
English translation of selected parts available as:
US Dept of Commerce, Joint Publications Research Service.
Translations on Latin America, no 302, GUO 737, 28 May
19 5. GUO.
2. CIA. NIS 94, Brazil, pts I and II, sec 22, "Coasts and
Landing Beaches," May - Jun 1957. C/NFD.
3. CIA. NIS 94, Brazil, pt I, supp II, "Coasts and Landing
Beaches," May 1957. C/NFD.
4. Cowell, Adrian, The Heart of the Forest, London: Gollancz,
1960. U.
5. da Cunha, Euclides, Rebellion in the Backlands, Chicago:
University of Chicago Press, 1944. U.
6. Instituto Brasileiro de Geografia e Estatistica, Conselho
National de Geografia. Geografia do Brasil: Grande
Regiao Norte, vol I, serie A, Rio de Janeiro, 1959. U.
7. Instituto Brasileiro de Geografia e Estatistica, Conselho
National de Geografia. Geografia do Brasil: Grande
Regiao Centro-Oeste, vol II, serie A, Rio de Janeiro,
19 0. U.
8. Instituto Brasileiro de Geografia e Estatistica, Conselho
National de Geografia. Geografia do Brasil: Grandes
Regines Meio-Norte e Nordeste, vol III, s rie A, Rio de
Janeiro, 1962. U.
9. Instituto Brasileiro de Geografia e Estatistica, Conselho
National de Geografia. Geografia do Brasil: Grande
Regiao Sul, vol IV, tomo 1, Rio de Janeiro, 1963. U.
10. Instituto Brasileiro de Geografia e Estatistica, Conselho
Nacional de Geografia. Geografia do Brasil: Grande
Regiao Leste, vol V, serie A, 19 5. U.
11. International Geographical Union. Excursion Guidebook
No. 1, "The West Central Plateau and Mato-Grosso Pantanal,"
Rio de Janeiro, 1956. U.
S-E-C-R-E-T
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READING LIST (Continued)
12. International Geographical Union. Guide of Excursion 3,
"The Coffee Trail and Pioneer Fringes," Rio de Janeiro,
1956. U.
13. International Geographical Union. Excursion Guidebook
No. 4, "Paraiba Valley, Serra da Mantiqueira, and Sao
Paulo City and Surroundings," Rio de Janeiro, 1956. U.
14. International Geographical Union. Excursion Guidebook
No. 5, "The Coastal Lowlands and Sugarcane Zone of the
State of Rio de Janeiro," Rio de Janeiro, 1956. U.
1.5. International Geographical Union. Excursion Guidebook
No. 7, "Northeast," Rio de Janeiro, 1956. U.
16. International Geographical Union. Excursion Guidebook
No. 8, "Amazonia," Rio de Janeiro, 1956. U. __
17. International Geographical Union. Excursion Guidebook
No. 9, "The Southern Plateau," Rio de Janeiro, 1956. U.
18. James, Preston, Latin America, 3d ed, New York: Odyssey
Press, 1959. U.
1.9. Korabiewicz, Waclaw, Matto Grosso, London: J. Cape,
1954. U.
20. Prewett, Virginia, Beyond the Great Forest, New York:
E. P. Dutton, 1953. U.
21. Sick, Helmut, Tukani, New York: Eriksson-Taplinger,
1960. U.
22. Siemel, Sasha, phi rero, New York: Prentice-Hall, 1953. U.
23. Union Geographique Internationale. Livret-Guide No. 2,
"Zone Metallurgique de Minas Gerais et Val-le du Rio
Doce," Rio de Janeiro, 1956. U.
24. Union Geographique Internationale. Livret-Guide No. 6,
"Bahia," Rio de Janeiro, 1956. U.
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IV. Population
A. General
1. Size and Growth
More than half of all South Americans live in Brazil,
where the population in 1960 numbered 70,967,185; by July 1966,
official estimates set the total at 84,679,000. This increase
:reflects a phenomenal rate of growth -- 3.1 percent annually
between 1950 and 1960 -- ranking Brazil first among the major
nations of the world. Unless birth rates are substantially
lowered, there will be more than 120 million people in Brazil
by 1980.
Because Brazil is so large (3,286,000 square miles -- the
fifth largest country in the world) and has vast areas that
are virtually uninhabited, the overall density of population
is only 25 persons per square mile. As in all Latin American
countries, however, actual densities vary greatly from one
region to another. According to official computations, the
density of population ranges from less than 0.5 per square mile
in parts of the Amazon Basin to 130 per square mile for the
state of Rio de Janeiro and to 3,927 per square mile for the
state of Guanabara -- the urban complex that was the Federal
District and national capital until 1960. See Map 5735 for
density patterns in 1950, which have remained essentially the
same to this date.
Except in the South, most of Brazil's population lives
within 300 miles of the coast, reflecting the historic settle-
ment of the country. Nearly 45 percent of the population is
concentrated in the six southern and southeastern states on
a tenth of the national territory. More than 18 percent of
all Brazilians live in the state of Sao Paulo alone. The
East and Northeast, with approximately 20 and 25 percent of
the population, respectively, are also densely populated. The
remaining 10 percent are widely scattered across the vast
sert'~)es of the interior and along the waterways in the endless
forests of the Amazon Basin. See Table 1 for population by
state and territory in 1960 and 1966 and for the increase of
population (in percent) during the period 1950 to 1960.
Brazil has always been a predominantly rural country,
with agriculture the mainstay of its economy. The rural
character of the country is much more pronounced than the
rural-to-urban settlement ratios -- 55:45 in 1960 and 64:36
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in 1950 -- indicate. Many very small and primitive towns are
counted in the statistics as partially urban simply because
they are municipio or distrito seats. True urban areas are
relatively few; only 17 cities have a population of over
150,000 (see Table 2), and only 51 others have more than
50,000. Most cities are not effectively connected with the
rural communities by modern transportation and communications
facilities. They have little cultural impact beyond their
immediate surroundings, and in general they have tended to
grow and function quite independently of rural areas. Conse-
quently, the rural dweller has lived apart, largely unaware
of the city, and has clung to established and traditional
ways. The homogenization of these widely d'Lvergent worlds
has now begun with the migration of rural dwellers to the
cities, the development of new educational, health, and coloni-
zation programs, and an awakening stemming from the cumulative
effects of modern means of communication.
3. Mobility
Internal migration is considered by many to be a Brazil-
ian national trait; the economic expansion of the country
during the 18th and 19th centuries can be attributed, in large
measure, to the speculative daring of the restless settlers
who welcomed new ventures. Willingness to migrate to new
areas or to new Jobs -- especially among the lower rural classes
-- is so readily apparent that foreign observers typically
comment on the instability of the Brazilian populace. Migra-
tion is the result of: (1) the system of slash-and-burn
agriculture, (2) the seasonal movement of workers to the
cotton, sugarcane, and cacao areas along the eastern coast,
(3) the flight of people from catastrophic droughts which
periodically reduce the Northeast to a dust bowl, (4) the
opening up of new agricultural frontiers, most recently in
western S2[o Paulo, northern Parana, and the newly developing
areas around Brasilia, and (5) rural-urban transfers, in
which people search better opportunities than the countryside
provides, especially in schooling for children. Most notable
of all such movements has been the influx of hundreds of
thousands of workers into the state of Sr1o Paulo, first as
agricultural workers and in more recent yearns to take city
jobs.
Settlement patterns in Brazil have for centuries reflected
the rural, agricultural, and extractive economy which has
prevailed, essentially unchanged, even to the present. A
journey inland today can be likened to a trip into the past,
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Brazil: Population Density, 1950
Population Density
Per Square Kilometer Per Square Mile
Miles
0 200 400
T~
0 200 400
Kilometers
15.0-25.0
10.0-15.0
5.0-10.0
2.5-5.0
r.0-2.S
0.5-1.0
Less than 0.5
0
38.8-64.8
25.9-38.8
12.9-25.9
6.4-12.9
2.6-6.4
1.3-2.6
Less than 1.3
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in which two decades are left behind for each day of travel.
Modern communities are largely a phenomenon of the past few
decades.
Three distinctive settlement patterns prevail: estate
villages, line villages, and isolated farmsteads. Villages
occupied by independent freeholders are not as common in
Brazil as in most countries, nor are they as common as a
passing observer might assume.
The estate village accommodates large groups of workers
on the coffee fazendas, sugar usinas (mills), large cotton
plantations, and to a lesser extent the extensive cattle
ranches. Typically the casa grande of the landlord dominates
the scene. Nearby are all of the crop-processing facilities
as well as such essentials as a chapel, commissary, school,
and perhaps infirmary. The workers' houses surround this
complex. On very large estates there may be more than one
such village, but all are subordinate to the property manage-
ment.
The line village, widely distributed in Brazil, consists
of long narrow properties on which the dwellings face a common
road or river. Line villages have been characteristic of
many colonization schemes, but they also have been developed
independently -- in thousands of small cacao holdings along
the coast from Ceara to Bahia and in the many riverine settle-
ments of the Sl.o Francisco and Amazon basins.
The scattered farmstead is the third type of settlement
in Brazil. Usually it is associated with areas of poor soil
and is sandwiched between large landholdings. Thatched huts
are typical. Many owners of these small farms work for hire
on the remote extremities of large estates; others are inde-
pendent, wresting a bare existence from the marginal soils.
The mobility of these people is notable, and every year millions
of them move to some new area, taking along little more than
the skills required to clear a new plot and erect another
wattle-and-daub hut.
5. Demographic Terminology
Hundreds of terms are used to designate different elements
of Brazilian society. The more widely used of these terms --
knowledge of which would be useful to non-Brazilians -- are
listed below along with translations. In certain instances
the area in which usage prevails is also indicated.
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a. Color
Amarelo Yellow
Branco White
Moreno Dark skinned
Pardavasco Brown; dark mulatto
Pardo Brown; offic'_al census term
for mulattoes, mestizos, and
Indians
Preto Black
Sarara Light mulatto
b. Race
Cafus, Cafuso, Black/Indian
Cabore
Cariboca White/Indian
Creulo, Creole Black (Negro)
Homen de cor Colored man
Mameluco White/Indian
Mulato Mulatto; white/black
Mestico Mixed; usually white/Indian
c. Country people of low status
Bruaqueira Minas Gerais
Caboclo Widely used; originally White/
Indian halfb:^eed
Caicara Along Sao Paulo coast; also
term for low.-class fisherman
Caipira Widely used for uncouth rural
dweller; derogatory
Cangussu S.o Paulo
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Aft
Aft
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C ap uava
Casaca
Casacudo
Corumba
Guasca
Homen de campo Widely used; general term
Mamb i ra
Mandioqueiro
Ploca
Praiano
Queijeiro
Tabareu
d. Farm People
Agregado
Camarada
Co_lono
Foreiro
Gaucho
Vaqueiro
Iotrudor
Morador
Parceiro
Minas Gerais and Bahia
Piaui
Along Rio Sa.o Francisco
In northeast
Rio Grande do Sul
Rio Grande do Sul
Minas Gerais
Widely used
Along seacoast
Minas Gerais
Widely used; like caboclo
and caipira
Agricultural laborer who
lives on the estate
Hired farmer who does not
live on the estate
Tenant farmer on 1-year
contract
Squatter
Rio Grande do Sul cowboy
Cowboy
Squatter
Squatter
Landless farmer, share-
cropper
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Posseiro
Roceiro
Sitiante
Miscellaneous
Bandeirante
Cangaceiro
Carioca
Chapadeiro
Garimpeiro
Machadeiro
Mascato
Mat u t o
Seringueiro
Sertane j o
Sertanista
Squatter
Slash-and-burn farmer
Independent rural worker
Resident of the city of
Rio de Janeiro
Plainsman
Diamond searcher in streams
Woodsman, rubber gatherer
Ambulant peddler
Backwoodsman
Rubber tapper
Common man in the sert.o
Upper class person in the
sertao; also synonym for
bandeirante
B. Composition
Brazil stands first among the countries of the world as
an effective "melting pot," a position it has continuously held
from the first days of Portuguese colonizat_Lon. For 400 years
red, white, and black people were thrown into close physical
and social contact, and in the last 100 years millions of Euro-
peans and many thousands of Japanese have become a part of
the composite whole. The resultant mixture of racial strains
defies analysis, and in Brazil color rather than race determines
the categories into which people are grouped. According to
the 1950 census the population was enumerated as follows:
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Number
Percent
of Total
Brancos (Whites)
32,027,661
61.7
Pretos (Blacks)
5,692,657
11.0
Amarelos (Yellows)
329,092
0.6
Pardos (Mixed)
13,786,742
2b.5
Undeclared
108,255
0.2
These data should be considered approximations, since there
is no reasonable way to define color, especially in view of
the prestige status attached to light skin. Thus, white
probably should be considered "whitish," and black can be
assumed to be undeniably black. The determination of the
proper category for the many millions of persons in between
is a subjective matter. Numerous terms are used locally
in reference to the various hues of skin or to blood mixture
(see list of terms, pagell8). Pardo, as used by the census,
is an unfortunately broad and meaningless term that includes
not only all persons of mixed blood (excluding those claiming
to be white) but also all pure Indians. The term preto is
applied to black-skinned people; "Negro" is used only in an
academic sense in Brazil except when meant as a derogatory
designation.
The prOtos are the descendants of the estimated 3 to
18 million Negro slaves brought from Africa in the 16th, 17th,
and 1.8th centuries. Most of the slaves were either Bantus
from the Congo and Mozambique or west African Sudanese from
former French Soudan. The Sudanese were settled mainly in
the area around Bahia, while the Bantus went to the area
around Rio de Janeiro and to the Northeast. Over the centuries
the two groups melded into one. The zone of greatest African
influence in Brazil stretches from the state of Pernambuco
southward along the coast to Rio de Janeiro and inland across
Minas Gerais, southern Gciis, and northern Slo Paulo. Through-
out this area, African traits have spread into local. customs,
language, food, music, folk tales, and religious cults.
2. Immigrants
Immigrants to Brazil make up only a small percentage of
the national population, but despite minority status, they
play a significant role in the economic and social makeup of
the country. Approximately 5 million immigrants entered
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Figure 82. Caboclo family in the North. These
people live on a precarious subsistence level with
few amenities.
Oak
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Figure 83. Northeast caboclo family with its
stock of farinha (manioc flour). The tipiti
across the trough is used to squeeze poison
juices from ;round up manioc roots.
Figure 84. Gauchos examining prize bull
at fair in Rio Grande do Sul.
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Ask
Figure 85. Northeastern cattlemen typical of the
dry sertoes.
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Figure 86. Fishermen and children on banks of Amazon at
Santarem, Para'. Skins of various hues are characteristic
of people along the lower Amazon. Note the variety of
boats.
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brazil between 1884 and 1962, coming primarily from European
countries. The greatest influx took place after the abolition
of slavery in 1888 and prior to 1934 (see Table 3 for numbers
of immigrants from major countries of origin). Since 1934
immigration has been controlled by a quota system based on
2 percent of the total previous immigration from each country.
Almost equal numbers of immigrants have come from Italy
and Portugal, which have contributed more than 60 percent
of the total. Spanish immigrants rank third (about 14 per-
cent), followed by those from Japan (less than 5 percent).
The yellow race is represented almost entirely by the Japa-
nese who came in large numbers in the late 1920's and 19301s.
Since World War II some 20,000 more have come. German immi-
gration, amounting to roughly 200,000, is of primary signifi-
cance because of its cultural impact on a sizable part of
southern Brazil. The early German colonizers deliberately
isolated themselves from other groups, reproduced very rapidly,
and retained their language, customs, dress, types of housing,
and attitudes to such an extent that nearby Brazilians appeared
to be the strangers. Although this isolation has lessened
in recent years, much of Rio Grande do Sul and Santa Catarina
still has a German appearance.
Sao Paulo State has the greatest number of foreign set-
tlers, it having been most successful in attracting agricultural
colonists after the abolition of slavery. As of 1950, 56.6
percent of all immigrants lived within its confines. Immigrant
groups included the Japanese, Italians, Spaniards, Germans,
Dutch, Turks, Syrians, and Portuguese. The Federal District
of that time ranked next with 17.2 percent of the total, fol-
lowed by Rio Grande do Sul (6.4 percent), Parana (6.3 percent),
and the state of Rio de Janeiro (3.2 percent). These areas
contained all of the nationalities resident in Sao Paulo as
well as scattered groups of Poles. Small settlements of
Spanish, Turkish, Japanese, and Italians were located in Mato
Grosso, Minas Gerais, Espirito Santo, and Bahia, and the
Japanese, Turks, and Portuguese had made their way into the
Amazon Valley. The Northeast Region and most of the East and
West-Central Regions have had little attraction for immigrants,
and even today non-Brazilian types in these areas are considered
outsiders.
Indigenous Indian Groups
Millions of Brazilians today can claim Indian blood as
a result of 400 years of continuous fusion of Indian with
Portuguese, and to a lesser extent, with Negro racial strains.
In addition, innumerable cultural traits in modern Brazilian
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life are identifiable as Indian in character. The strict
use of the term "Indian," however, is limited to those
groups in Brazil who think of themselves as Indians and who
are considered so by others because of tenacious loyalty to
their ethnic background. Such groups are located throughout
Brazil, except in the densely populated parts of the South.
In northeastern and southwestern Brazil nearly all of the
Indian tribal groups have become acculturated to a great
extent, but their core groups still retain their Indian
identity.
Brazilian ethnologists estimate the total number of
Indians in Brazil today to be somewhere between 65,000 and
100,000 -- a staggering decimation of the 1 to 2 million
believed to have inhabited the area when the first Europeans
came. The small number of remaining tribes would be of
little relative consequence were it not for the fact that the
great majority of them are the primary inhabitants of vast
areas of the interior. Not only are they the most knowledge-
able about these areas, but they also determine the degree to
which outsiders may move about, develop extractive industries,
or establish settlements. These tribes also constitute the
best source of untapped labor in the remote areas. It is
estimated that about
65
percent
of
the
Indian population is
located in Amazonia;
20
percent
in
Mato
Grosso and northern
Goias; 8 percent in
the
South;
and
the
remaining 7 percent
in the East and Northeast.
It is impossible to determine exact population figures
for specific groups (except in integrated communities), since
census enumerators cannot reasonably contact those that are
in remote areas. A 1957 study, however, estimated that
approximately half of the Indian groups contain 250 persons
or less; at least another third had between 250 and 2,000
persons each; and the remaining few groups may have numbered
as many as 4,000 to 5,000 each. Sometimes groups may be
further divided into small villages.
Estimates also were made to determine the amount of
contact that exists between Indians and their Brazilian neigh-
bors, that is, whether they are seldom or occasionally in
contact, are permanently in contact, or have been essentially
integrated as laborers into Brazilian settlements. Based on
minimum numbers, it was calculated that at least 21,000
Indians remain isolated, having essentially no contact with
outsiders, either because of the remote locations of their
villages or because of their previously hostile and bloody
conflicts with civilization; some 8,000 to 10,000 have only
intermittent contact, because their lands, often economically
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marginal, have only recently been penetrated by Brazilians;
approximately 13,500 have permanent contact with settlements
in rural Brazil; and 24,500 are integrated as indigenous
"islands" in the national populace -- such as in Sao Paulo
State or in the Northeast.
At least 35 independent Indian languages, divided into
more than 100 mutually unintelligible dialects, are spoken
in Brazil. All stem primarily from six major linguistic
stocks:
Tupi Most widespread. Originally spoken
along the coast and the Amazon Valley,
it was adopted as the lingua franca
during the first 200 years of coloni-
zation and is still used in remote areas.
Aruak Spoken along the upper tributaries of
the Amazon and in souther Mato Grosso.
Karib Spoken north of the Amazon.
Je Spoken along the Xingu, the Araguaia,
and the Tocantins rivers, and in the
South.
Pano Spoken along the upper tributaries of
the Jurua and Purus rivers.
Xiriana Spoken north of the Rio Negro.
Ordinarily Indians communicate with outsiders in Portu-
guese, which is also frequently used between tribes whose
languages are unintelligible to each other. In the Northeast,
where acculturation has existed the longest, most Indian groups
spears Portuguese to the exclusion End loss of their own native
tongues.
All Indian groups fall under the custody of the Indian
Protective Service (Servico de Proterao aos Indios -- SPI),
established in 1910 and an autonomous federal agency under
the Ministry of Agriculture since 1939. By the time of the
inception of the SPI, Indian tribes were in danger of extinc-
tion. As the SPI began operations it faced several monumental
tasks, including: (1) the pacification of belligerent tribes
whose deep-seated hatred of the white man had generated savage
and destructive attacks on outlying settlements; (2) the
protection of Indians from unwarranted abuse, both in the
appropriation of their lands and in the utilization of their
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labor, particularly in such economic ventures as the rubber
"boom"; and (3) the education of Indians so that they might
understand the advance of civilization and appreciate the
ultimate goal of the government -- the assimilation and con-
version of the Indian into productive citizenship.
The SPI can be credited with effecting a large number
of peaceful adjustments between settlers and previously hos-
tile Indians. It has establisned throughout the country
more than 100 reservations (SPI posts) on which the Indians
may adjust to "civilized" life. Nevertheless, many more
reservations are needed. The SPI also assists with legisla-
tion, whenever possible, to solve the serious problems of
land use and occupancy that still arise in remote areas.
Two other groups have done significant work with the
Indians. Since World War II, Orlando Villas Boas -- a
unique and dedicated Brazilian -- and his two brothers have
worked in the area known as the Upper Xingu. In this area
one of the world's most remarkable examples of intertribal
acculturation among primitive peoples has taken place.
Retreating from the pressures of early colonization on the
north, east, and south, Indian groups from four linguistic
stocks (Tupi, Aruak, Karib, and J(~) coincidentally converged
into this region of central Brazil and evolved an amicable
adaptation of cultural traits. The Villas Boas brothers
have devoted their efforts to pacifying and protecting these
tribes; through their efforts an 8,500 square-mile National
Park (Parque National do Xingu) was established in 1961.
This park is a living museum of history and Indian culture
wherein tribes can remain without threat to their survival
and into which strangers cannot enter without hard-to-get
permits. Some tribes outside the area, threatened with
extinction, have elected to move in, and the Villas Boas
brothers urge others to do the same.
The Summer Institute of Linguistics (SIL), also referred
to as the Wycliffe Bible Translators, has also done notable
work with the Indians. This organization of nondenominational
linguists has as its worldwide objective the enscribing of
previously unwritten languages, followed by translations of
parts of the Bible. In Brazil SIL teams, each consisting of
two women or a married couple, have worked with some 40 dif-
ferent tribes since 1956. Usually these teams live in a
village for several months at a time. In 1964, at the request
of the SPI, they surveyed most of Brazil's Indian tribes and
provided data for a report that contains the most accurate
and complete estimates of tribal locations, numbers, and
linguistic families ever produced.
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4. Indian Culture Areas
The immensity of the area over which these tribes are
distributed (more than 2 million square miles), the high
degree of intertribal acculturation that has occurred, and
the small size of the individual groups make it difficult
to summarize significant factors about the Indians if enumer-
ated tribe by tribe. Consequently, they are presented
according to a system of Culture Areas devised in the 1950's
by the Brazilian ethnographer Galva-o. The criteria used in
determining these Culture Areas included geographical simi-
larities, the integration of common cultural traits, and the
degree of Indian contact with outsiders. Eleven such areas
have been identified: seven in the tropical forests and
grasslands of the Amazon Basin, three in the subtropical
forests and Pantanal of southern and southwestern Brazil,
and one in northeastern Brazil. See Map 57545 for the deline-
ation of Culture Areas; the locations of individual groups,
their numbers, and linguistic families; the locations of
Summer Institute teams; and the areas in which hostile Indians
live.
Table 4 summarizes for each Culture Area its geographical
nature; the number of Indians in each linguistic family (includ-
ing some besides the six major families); characteristic cul-
tural traits such as occupations, type of rivercraft, type
of house, and religious practices; and the level of contact
and attitudes toward outsiders.
C. Language
Brazil is the only country in the Western Hemisphere in
which Portuguese is the national language. Although it was
the official language in the early days of colonization, the
language of the street was the quickly adopted Tupi tongue of
the coastal Indians which was energetically oromoted as the
lingua franca by Jesuit missionaries. Not until the Jesuits
were expelled in 1759 did Portuguese become the commonly
used language. Tupi and several other Indian languages are
still used by the indigenous Indians, although all but the
most isolated tribes speak Portuguese to a limited degree.
The common use of Tupi left a permanent impression on the
Brazilian language, especially in place names, topographic
features, and the names of flora and fauna. Similarly, African
Negroes have contributed words and phrases to the language of
Brazil, as have European colonists through the past 100 years.
In 1943,Brazilian Portuguese was officially adopted by
the government, with simplifications in spelling and differences
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in usage from the original language. In spoken "Brazilian,"
variations in pronunciation and in slang reflect regional
differences and cultural levels. Regional dialects are
quickly identified by Brazilians just as Americans can
deduce a person's native region by his speech. Final vowels
are dropped in the North, natives of Rio de Janeiro tend to
slur their words, and Bahians are frequently quite blunt.
The spoken Portuguese of Brazil differs from that of Portugal
much as the English of America differs from that of England.
The large numbers of Europeans who poured into Brazil
in the late 1800's and early 1900's maintained their native
languages in the isolated colonies they established. With
the advent of World War I, attention was focused on the wide-
spread use of German and Italian, especially in Brazil's remote
colonial schools. Educational reforms were then instituted,
and by 1938 it was required that all pupils study the Portu-
guese language and that all lessons be taught in Portuguese
by Brazilian-born teachers. Immigrants are now expected to
learn Portuguese as quickly as possible, and new colonies,
institutions, businesses, and other establishments must bear
Portuguese names. At least 30 percent of the population of
all new colonies must be native-born or of Portuguese origin,
and no other single nationality group may exceed 25 percent
of the total. Such laws and the natural inclination of
Brazilians to accept newcomers have promoted cultural assimi-
lation. Only the Japanese tend to remain culturally consoli-
dated, and even they use Portuguese in business transactions.
Thus, few places can be found in Brazil where Portuguese is
not spoken by nearly everyone.
Educational standards throughout Brazil are deplorably
low at all levels, and educational opportunities are inade-
quate except in the larger cities. As a consequence, the
majority of the rural populace normally completes no more
than 2 or 3 years of elementary school education. Travelers
in some areas experience difficulty in finding persons who can
read or write.
Approximately 45 percent of Brazil's population was
defined as illiterate in 1962. The actual amount of illiteracy
was undoubtedly much higher, however, since literacy was
determined by the ability to sign one's name and an oral
declaration of reading ability. Illiteracy is higher among
adult females than males, but it is about the same among
female and male children. It varies greatly among age groups,
directly reflecting the lack of basic schooling in the past.
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Thus, illiteracy among people over 50 years of age is much
higher than it is among younger people who have had better
educational opportunities. Far more people are illiterate
in the northeastern states (70 percent) than in the southern
and southeastern states (30 percent), and the percentage of
illiterates among rural dwellers is three times as high as it
is among their urban counterparts. Racial differences are
also notable. Less than 20 percent of persons in the yellow
race (mostly Japanese) and 34 percent of those classed. as
white are illiterate, while 69 percent of the pardos (mes-
tizos, mulattoes, and Indians) and 73 percent of the Negroes
are illiterate.
The school system includes a free elementary school, in
which 4 years are theoretically compulsory and 3 more years
are encouraged; academic and vocational secondary schools,
which offer 4 years of ginasio (roughly junior high school)
followed by 3 years of colegio (senior high school); and a
number of universities with courses lasting from 1 to 6
years. Despite official programs to promote education and
to reduce illiteracy to 5 percent of the population by the
year 2000, the rapid increase of the population makes progress
toward these goals difficult. The situation today is only
slightly better than it was in 1950, when it was determined
that 82 percent of the population over 10 years of age had
not completed any level in the school system.
Of those completing elementary school, less than 15
percent were pardos or Negroes. This is explained, in part,
by the distribution of existing schools, most of which are
in urban areas. In the rural areas, where the population
consists largely of pardos and Negroes, schools are fewer
and the percentage of graduates is very low. In 1960, of
the 2,764 municipios in Brazil, only 275 had secondary
schools through the colegio level and 1,359 had no schools
beyond the elementary level. The schools (escolas isoladas)
in many remote areas consist of one ungraded classroom, with
an inadequately trained teacher and little if any equipment
for the motley assortment of pupils who live within walking
distance.
The school dropout (evasno) is a serious educational
problem. A 1960 study indicated that 50 percent of Brazilian
children quit school after 1 year or less of elementary edu-
cation, and less than 5 percent complete 6 years. Although
school conditions are poor in some of the large cities,
instruction is better and programs are more organized than
in the small towns. In many small communities good teachers
are hard to find or keep, and impractical curriculums make
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Figure 87. Elementary school classroom in Rio de
Janeiro. The children are of various racial back-
grounds.
Figure 88. School children in Londrina,
Parana. 't'heir faces reveal that they
are of German, Japanese, and Italian
parentage.
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school seem like a waste of time for children who can be use-
fully employed at home.
As of 1963 there were 27 legally recognized universities
in Brazil, of which 19 are supported by the government.
Most are located in the southeastern and southern states.
Brazilian universities follow a pattern typical of several
Latin American countries, in which many of the professors
teach only part time, depending for their livelihood on
income derived from two jobs. Students also generally
attend part time, and many of them hold jobs while attending
the university. Brazilian student unions are highly organized
and wield considerable influence in the university and nation-
ally. Student academic centros (centers) within each school
are affiliated into so-called central student directorates,
which in turn are organized on a state and national level and
receive financial subsidies from the government. From this
unique position of strength, students can and do influence
national affairs, and from the hierarchy of student unions
many of the nation's political leaders emerge.
E. Religion
The overwhelming characteristic of religion in Brazil
is the blending of folk religions with elements of Christianity,
especially Catholicism. Four centuries of fusing African and
native Indian magico-religious practices, Spiritualism, and
Christian monotheism have produced a heterogeneous mixture of
religions that almost defies analysis. Although regionally
there are wide variations both in degree and outward mani-
festation, folk religion is prevalent all over Brazil and
permeates the daily behavior of a very large percentage of
the population, even devout Catholics and Protestants. The
degree of adherence to folk religions can be equated to a
large degree with social and racial factors. Moving from the
white upper classes down through the color and social scale,
one may note the shift from intellectual Christianity to the
conscious mingling of Christian principles with some fetish
rites until, at the bottom, the beliefs in magico-religious
cults reaches its zenith.
Geographically, African influences predominate in the
Northeast and East -- reflecting the largest, influx of slaves
in colonial times -- while European influence and adherence
to accepted Church dogma is evident in the southern part of
Brazil. Large numbers of active Catholics and Protestants
are found in urban areas where education and social status
reach a sophisticated level. The rural Brazilian has absorbed
religious concepts and practices from several directions, with
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little if any guidance or restraint on the spiritual inter-
pretations that seem to suit his needs best. Unacculturated
Indian tribes of the interior observe primitive rites that
differ in detail from group to group, but all are character-
ized by animistic beliefs, shamanism and other powers of
the supernatural.
brazil is nominally a Roman Catholic country (nearly
95 percent) despite a tradition of religious freedom that
has existed since colonial times. If the 1960 census figures
are accurate, Brazil has more declared Catholics than any
other country in the world -- nearly 68 million. In view of
actual religious practice, however, most of these are "margi-
nal" Catholics who combine some aspects of folk religion and
mystical rites with the rituals of the Church. According to
the Catholic clergy, only 6 to 8 million Brazilians may be
strictly defined as practicing Catholics. In addition to
these, some 245,000 persons belong to the Greek Orthodox Catho-
lic Church. A somewhat larger number of Syrian immigrants
are Maronites, adhering to an Eastern Mediterranean branch
of the Uniate Church.
The city of Salvador is the center of the Catholic Church
in Brazil and the residence of the primate, the Cardinal of
Bahia. Countrywide, the ratio of priests to parishioners is
about 1 to 8,000, based on the estimated number of actual
practicing Catholics; if based on the recorded number of
Catholics, the ratio is 1 to 60,000. Nearly half of the
clergy, however, are located in the states of Sao Paulo, Rio
Grande do Sul, and Minas Gerais, leaving the balance to
serve the large remainder of the country. In some rural
areas, one priest may serve as many as 20 to 30 churches.
Because churches are widely dispersed, he may conduct Mass
in any given church only once a year or less. Consequently
widespread laxity in religious matters is the normal pattern,
and the impact of the Church on daily living is much less
effective than in most Latin American countries. For much of
the nominally Catholic population, conformity to traditional
custom -- especially at weddings, funerals, and the numerous
holy days -- reflects acknowledgment of the role of the Church
as a catalyst rather than any dependence upon it as a bulwark
of spiritual strength.
Because the Church historically has had less authority
and prestige under the Portuguese pattern of colonization,
it has played a much less influential role in the development
of Brazil than in such countries as Peru and Mexico. The
caliber of the Brazilian clergy has been unfortunately low,
often drawing on recruits having little education or few moral
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qualifications. Indifference toward religious proprieties is
common, and a generally low degree of respect for the clergy
has produced a somewhat lax attitude toward the formalities
of the Church. The past two decades, however, have witnessed
determined efforts by the Church to raise its standards,
especially by more careful selection of new priests and
greater depth in ecclesiastical training.
The increased participation of the Church in local reli-
gious, social, and political activities has led to the devel-
opment of Catholic action groups. These groups support pro-
grams to eliminate slum conditions and to improve rural welfare
and land reform, and they also urge the participation of
laymen in cooperative ventures, particularly banking, storage,
and marketing. The Catholic-sponsored Rural. Labor Unions
and Institute of Rural Leaders are examples of Church programs
designed to counterbalance the more radical, Communist-
influenced Peasant Leagues and other leftist, groups pressing
for social reforms.
The Protestant Church is relatively unimportant in
Brazil, despite a membership of nearly 2,000,000 -- the largest
number of Protestants in any Latin American country. Sixty
percent of all Protestants are members of either the Evangel-
ical Lutheran Church or the Assembly of God, each having about
500,000 members. The remainder belong to some 70 churches,
the strongest being the Baptist, Presbyterian, and Methodist.
Protestants are concentrated mostly in the southern states.
Smaller groups are scattered through the eastern states, and
missionary groups are in the rural areas to the west. In the
nearly 8,000 Protestant churches in Brazil, the ratio of
ministers to members is 1 to 250. The common fundamentalist
precepts of the leading Protestant groups are not generally
appealing to the Brazilian temperament, and many converts
need continuing inspiration.
Other large religious groups include 680,000 Spiritual-
ists, according to the 1960 census, but some estimates indi-
cate that there are actually three times that many; Brazil
has more Spiritualists than any country in the world. Buddhists,
tabulated in 1960 at 175,000, probably are even more numerous
than that and are found among the rural Japanese population,
which totals over 400,000. Approximately 1L'0,000 Jews live
in Brazil, mostly in cities. No official figures are available
for the number of persons (mostly Negroes) who belong to the
cults that were brought to Brazil from Africa, as many of
them identify themselves as Catholics or as Spiritualists
despite adherence to primitive groups. As result, the many
variations of folk religion throughout Brazil are difficult
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to isolate or evaluate statistically as identifiable religious
movements.
The most dominant of the cults that abound in Brazil are
the numerous versions of the Gege-Nago religion introduced by
Sudanese Negroes. The core aspect of these Sudanese cults is
the grigri or fetish which is a "prepared material object"
endowed, through special rituals, with the presence of a
spirit. The ceremonies of such cults are known as macumbas
in the Rio de Janeiro area, candombles around Salvador and
xangos and catimbos in the Northeast. They include spiritual
communication with one or more of the numerous dieties or
orishas that embody specific spiritual realms. Communication
between human beings and these gods presumably can be effected
through male or female mediums or sacerdotes, people who have
special attributes and make special preparations. An inner
group of devotees is consecrated to the cult of the orishas
and undergoes involved rites of "initiation." Drum-dominated
music and dances, many of which are of African origin, are
integral parts of the magical rituals that may last for hours
and even days of hypnotic trance, culminating in the total
physical and emotional collapse of those possessed of the
spirit of the fetish.
Bantu religious culture is also evident in these Brazilian
rituals, but its original theological framework was never as
complex in Brazil as the Gege-Naga. Its primary contribution
to Brazilian religion has consisted of a cult of the dead,
ancestor worship, a belief in transmigration of the soul, and
many beliefs that relate it to the practices of spiritualism.
Bantu macumbas are simpler in ritual and physical setting
than those of the Gege-Nago, and their high priests,called
quimbandas, are often referred to as "mediums" because of the
spiritualistic influence. The amalgamation of Gege-Nago,
Bantu, aboriginal Indian, Spiritualist, and Catholic forms of
ritual has been taking place during the past 300 years, with
more emphasis on one or another ritual in different locales.
It is practically impossible to trace back the various elements
of the rituals to their original, pure form.
Throughout Brazil a strong belief in the supernatural
prevails, and in every locale there are mysterious beings
who exist in the minds of the populace as friends or enemies.
The pe de garrafa (bottle-footed man) lures herb collectors
until they are lost in the woods of southwestern Mato Grosso;
the mal d'agua (water mother) attracts men to their doom in
lakes or rivers, and her masculine counterpart -- the boto --
similarly lures women. The lobis homen (werewolf) is feared
in rural Brazil, and anemia is an indication that one has been
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Figure 89. Christianized shrine of African cult in slum area
of Rio de Janeiro. Shrines such as this attract regular wor-
shipers and are the scenes of highly emotional religious cere-
monies.
Figure 90. Northeasterner selling leather charms that are
presumed to guard against snakes. Note the Indian, European,
and Negro features of the Brazilian bystanders.
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victimized by such a fiend. In some areas the curupira is a
vicious little man feared because his feet are backwards,
leaving tracks that lead victims into his destructive arms.
Many other beings figure daily in the monotonous lives of
rural Brazilians throughout a large part of the country, pro-
viding emotional outlets for fear, anger, frustration, or even
rejoicing and adding some zest to the simple subsistence pat-
terns of living that prevail.
F. Housing
The miles of ultramodern skyline of Brazil's major cities
are a false facade for the miserable hovels that are typical
for the country as a whole. A study based on the 1950 housing
census (still largely valid) showed that only 15.6 percent of
all homes had running water, only 24.6 percent had electricity,
and 33 percent had indoor toilets. If urban homes are excluded
from the analysis, the comparable percentages for rural homes
were 1.4, 3.6, and 10.4, respectively. The "public utility
services," in small towns fortunate enough to have them, fre-
quently serve only public buildings and, perhaps, the few per-
sons able to pay high rates .
In 1963 estimates indicated that 5.25 million new houses
were needed and that 2 million existing houses were unfit for
habitation. The population expansion has for years completely
outdistanced the construction of new houses, and the result
has been overcrowding in inadequate quarters.
The outstanding example of housing shortage is the growth
of the favelas in Rio de Janeiro -- conglomerations of shacks
pieced together out of zinc sheeting, canvas, packing cases,
rough tile, or anything else that can be gotten cheaply or at
no cost. These shacks are often so small that there is no
room for beds. Described by one authority as "communities of
squalor," the favelas occupy precipitous slopes and are separated
by crooked paths. There is no effective sewage system; occa-
sional rainstorms wash away refuse in the gullies between and
through the shacks. One survey in Rio de Janeiro located 194
favelas in which nearly a million people live -- almost a
third of the city's population. Although many people who live
here work at respectable jobs, they can find no better dwellings
in the overcrowded city. Water is the greatest problem; some
favelas are a kilometer away from the nearest public spigot,
and 5-gallon cans of water are carried daily up the steep slopes.
Similar clusters of shanties are called corti os in Sao Paulo,
malocas in Porto Alegre and Belo Horizonte, and mocambos in
Recife (where 50 percent of that city's population live ; all
of these settlements are inhabited primarily by migrants from
rural areas.
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The more stable elements of society in Brazilian cities
live in considerably better circumstances, even if by American
standards the houses are small and crowded. Typically, the
houses are connected to one another and constructed flush
with the sidewalk. Each has several rooms a--_ong a long hall
which leads to an open patio in the back. Only the wealthy
have open ground around their houses, usually in the elegant
suburbs. Recent decades have seen the construction of high-
rise apartments in the larger cities. Services unfortunately
have not kept up with the new structures, and dependable water
supplies, electricity, sewage systems, and garbage collection
are often lacking.
Rural homes are typically 2- or 3-room wattle-and-daub
houses constructed with wooden frames filled with mud and
roofed with thatch. The best of them are coated with a lime
and soil plaster that retards deterioration somewhat, but
none last many years. Windows are simple openings, usually
without glass. Floors are ordinarily bare dirt, often with
puddles of dirty water and littered with kitchen refuse, but
sometimes have raised wooden, cement, or brick floors. Open
hearths without chimneys are used for cooking, and the smoke
seeps through cracks in the soot-covered walls and roof.
Knowledge of hygiene does not exist, and. ordinarily there are
no sanitary facilities either indoors or outside. Consequently,
water and food are polluted, and vermin breed in the wattle-
and-daub walls and thatch roofs.
Not all rural dwellers live in abject poverty, but there
is little incentive or opportunity for the average family to
alter its circumstances. The casa grande of the fazenda is
a structure of comparative splendor, having numerous amenities
unknown to the workers nearby. Midway between the large land-
owners and ordinary caboclos, are a few prosperous, small
landowners -- particularly among the southern colonization
areas -- who have comfortable houses not unlike those in the
part of Europe from which they came.
Houses along the flood plains of the tropical Amazon
Basin are built on stilts to protect both family and animals
during periods of high water; walls of dwellings are woven of
palm to permit free air circulation. The ent;ire structure is
simple and suited to the transitory life of subsistence farmers.
Houses of the primitive Indians scattered throughout the Amazon
Basin are similarly temporary, usually built with no walls,
having only heavily thatched roofs supported by timbers.
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Figure 91. Woman transporting 5-gallon
can of water on her head in typical Bra-
zilian fashion.
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Figure 92. Favelas on steep hillsides of Rio de Janeiro. These
slums have no water, sewage, or unused space.
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Figure 93. Residents of slum area in Rio de Janeiro obtaining
water at public water spigots.
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Figures 94a and b. Favelas in Rio de Janeiro.
Some houses are supported by the roofs of
houses below.
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94b
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Figure 95. Copacabana Beach in Rio he Janeiro, ringed with
elegant apartments and backed by sprawling favelas on the
hillsides.
Ask
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Figure 96. Business district of Curitiba, Parana. The modern
skyscrapers are typical of most of the growing cities in Brazil.
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Figure 97. Poorly maintained lower middle class homes in
Sao Paulo. Homes like these are served by public utilities.
Figure 98. Residential street in Novo Hamburgo, a progressive
Dutch colonization settlement in Rio Grande do Sul.
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Figure 99. Stilt house along the Amazon. Such houses are
typical where the wide flood plain is inundated seasonally.
Figure 100. Wattle-and-daub house, characteristic of much
of interior Brazil. In many sections thatch is commonly
used for roofs instead of tile. Note manioc in the fore-
ground.
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Figure 101. Thatched-roof and frame houses in a Waika Indian
village in Roraima.
Figure 102. Typical houses of Xavante Indians on the Rio das
Mortes. An intricate wooden framework supports the dense
cover of thatch.
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Figure 103. Thatched-roof house of Kaxinaua Indians. This house
is long enough (85 feet) to house a dozen or more families, each
in its own section with a separate hearth.
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G. Health
The general state of health of the population throughout
Brazil is poor. Ignorance, poverty, polluted water and food,
lack of sanitary facilities, inadequate means of food preser-
vation, improper diet, insufficient medical facilities, reli-
ance on folk medicine, and many similar conditions make
improvement slow and costly. The government has for several
decades been aware of the urgent need for widespread health
controls, and numerous programs under the Ministerio de Saude
(Ministry of Health) and other organizations are gradually
raising health standards.
Health conditions in the cities are far superior to
those in smaller towns or rural areas, but even in the urban
centers sanitation facilities and health services are not
available to the poor. Diseases that have long been con-
sidered under control in most modern societies -- typhoid
fever, diphtheria, tuberculosis, smallpox, malaria -- are
still endemic in many parts of Brazil. Nevertheless, improved
health conditions are clearly measurable from year to year as
a result of the continued efforts throughout the country,
especially those of the rural postos de saude (health posts),
active since 1942. Between 1950 ET-11-9-6-0-average life expect-
ancies were increased by 10 years in the North and West-Central
regions and by 20 years in the South. Infant: mortality is only
a little over 100 per 1,000 births for the capital cities but
ranges between 300 and 400 per 1,000 live births in the North-
east. If infants born in backward areas escape tetanus, acquired
by unsanitary practices of midwives, they often succumb to mal-
nutrition, since no milk is available and they eat a regular
adult diet (black beans, manioc meal, and jerked beef) as soon
as they are weaned. The principal causes of death during the
first 4 years are gastroenteritis, diarrhea, and parasitic
diseases.
The high death rate among all age levels in Brazil stems
from widespread conditions that are conducive to a variety of
chronic or fatal diseases. Schistosomiasis (liver fluke) is
extremely difficult to control, especially in the Northeast
where the host snails and mollusks are common foods and the
drinking water is ordinarily polluted. The wattle-and-daub
houses typical of the Brazilian countryside are infested with
the insect that transmits the incurable Chagas' disease that
reportedly affects 4 million Brazilians, and control measures
are difficult to administer. Malaria still occurs, although
it has been eradicated in all urban and most rural areas; the
same is true for bubonic plague. Ordinary yellow fever was
considered eradicated by 1954, but a jungle variation of the
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disease still occurs sporadically in the Amazon rain forest,
where mosquitoes breed and certain species of monkeys provide
the vehicle for the complete cycle of the disease. Brazil has
recurring epidemics of smallpox and continuing incidence of
leprosy and trachoma, although control measures are becoming
more effective every year. Venereal diseases are widespread.
Parasitic diseases are the rule rather than the exception for
the entire rural populace; over 90 percent of the children
in the Northeast are reported to have some worm disease, par-
ticularly hookworm which is easily acquired by walking bare-
foot in the polluted soil. In order of importance the prin-
cipal causes of death due to illness throughout Brazil are
heart diseases, gastritis and enteritis, influenza and pneu-
monia, cancer, tuberculosis, diseases of the central nervous
system, and parasitic illnesses. Respiratory ailments account
for 25 percent of all deaths.
Use of narcotics is not uncommon in Brazil, creating
serious social problems, especially in urban areas. The con-
sumption of marijuana is most widespread and cocaine ranks
second. Marijuana is grown as a secondary crop on plantations
in the Northeast where its use is traditional, but it is widely
sold in the South; 5 tons are estimated to be consumed annually
in Sao Paulo alone. Little is done to enforce the law pro-
hibiting the sale of narcotics, and a maximum sentence of 5
years does little to deter its promoters.
Brazil has about 40 doctors per 100,000 persons -- nearly
average for Latin American countries. The World Health Organi-
zation reported in 1959 that 27,111 physicians were serving
either on hospital staffs or in health services; at that time
31 medical schools were graduating about 1,600 doctors annually.
In addition, six schools of public health enrolled approximately
300 students per year. Beginning in 1959 the National School
of Public Health provided graduate training in all branches of
medical practice.
Over 60 percent of the country's physicians are located
in the states of Sao Paulo and Guanabara, where they serve only
28 percent of the population. The distribution of the remain-
ing 40 percent of the physicians is therefore sparse in many
sections; for example, in 1963, 25 percent of the municipios in
the state of Pernambuco had no resident doctors. Although
highly respected, most physicians are poorly paid and often
combine government and private practice to increase their
incomes. The lack of available doctors has placed undue depend-
ence on pharmacists, who dispense advice, home remedies, and
drugs across the counter without prescriptions. In rural areas,
people consult doctors rarely if at all. Midwives are relied
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Figure 104. Residents of Rio de Janeiro favelas
attending hygiene class.
Figure 105. Nurses in training. Nursing is still
considered a very lowly occupation in Brazil.
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Figure 106. Northeastern child leading donkey from
town waterhole. All over Brazil daily water supplies
are procured from such easily polluted sources.
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upon to a great extent, and efforts are being made to get
basic instruction to them on simple first aid and hygiene.
The native healers (curandeiros and pages) are commonly con-
sulted, but no training has been instituted to modify their
magical and superstitious practices.
Qualified nurses are scarce in Brazil, and most of those
that are adequately trained serve in the better-paying private
:institutions. As a result, partly trained or even untrained
nurses staff many public hospitals, often performing beyond
the limits of their professional capability. Thirty-seven
professional nursing schools produce graduates at varying
levels of competency, and 53 schools offer a 6-month nurse's
aid course for elementary school graduates.
As of 1960, Brazil had only 2,622 hospitals of all types,
more than two-thirds of which were in the six southernmost
states. There were at that time a total of 233,403 hospital
beds -- less than four per 1,000 Brazilians. The 18 percent
of the total number of hospital beds that were located in
institutions run by the government or other nonprofit organi-
zations were generally filled. The 82 percent of the beds
that were in private hospitals were often empty.
A wide range of public health services is available in
Brazil, and overall governmental expenditures for health
account for approximately 5 percent of the total national
budget. The Ministerio de Saude is responsible for medical
care and disease prevention, and it is augmented by the
Servi9o Especial de Saude Publico (Special Service for Public
Health), which runs 400 health stations throughout the country.
The best of these stations offer X-ray service, laboratory
examinations, dentistry, home visits, syphilis tests, prenatal
advice, immunizations, and instructions regarding sanitation,
but because of the limitations of personnel and equipment
many stations offer little more than first aid.
State departments of health also provide health centers,
the best of which are manned by doctors, nurses, and a small
staff; the poorest are operated by nurse's aids. In addition
to the health centers, there are some 450 medical posts and
about 1,800 child welfare posts. At the latter, prenatal
clinics, milk dispensaries, and examination stations strive
to raise the level of child health. The Ministry of Education
and Culture has instituted health examinations of school chil-
dren in some states. Attention to the health of children, as
well as mothers, has always been predominant in Brazilian
efforts to improve health conditions.
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Industries, some of the larger agricultural enterprises,
and labor organizations also provide their personnel with
clinics, medical services, and occasionally private hospitals.
A very complex system of social security institutes -- under
the general supervision of the Ministerio da Trabalho e Previ-
de"ncia Social (Ministry of Labor and Social Welfare) -- also
provides clinic and hospital services, some in the institute's
own facilities but most under contract to independent hospitals.
H. Occupations
Brazilian workers are predominantly agricultural; in
1950 (latest data available) 58 percent were engaged in agri-
culture, herding, and forestry. Other occupations of the
economically active (in percent of the total) were as follows:
Manufacturing and processing
9.6
Wholesale and retail trade
5.6
Transportation, communication, storage
4.1
Domestic service
to
Construction
Extractive industries
3.4
Social activities (educational and church) 2.5
Public administration
National defense and security
Real estate, banking, insurance
Professions
Other services
1.4
Estimates in the late 1950's indicated that the increase
in industrial activity since 1950 had caused an influx of
workers into industry, many of whom shifted from the agricul-
tural labor force. On the other hand, the 200,000 annual
migrants to the urban areas are generally ill equipped for
work in the cities, and a third of them migrate home again.
Trends and proportions indicated by the 1950 census are still
essentially valid.
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Occupational statistics in Brazil are difficult to inter-
pret, as it is customary for those in moderate and well-to-do
circumstances to hold down more than one job. Reports for
1950 illustrate this confusion since the small percent of the
working force that indicated supplemental employment was from
domestic or agricultural groups rather than from more sophis-
ticated levels. Another complicating factor was the inclusion
of 6,308,567 children, aged 10 to 14, with no cross-tabulations
by age, making it impossible to evaluate the dimension of the
productive adult working force. Only a small proportion of
the populace was registered as self-employed,. The census also
revealed a high correlation between socioeconomic status and
color; whites and Japanese ranked highest in employer status,
and Negroes ranked highest in the employee category.
A 1960 study of human activities on a regional basis
divides the country into nine socioeconomic regions (see
Map 57611) based on economic and occupational. factors, as
follows:
Zone
Activity
Typical worker
Northeast Pastoral
Cattle fazendas
Mamelucos, Vaqueiros
Southern Pastoral
Cattle and agriculture
Gauchos
Northeast
Sugar usinas
Mulattoes
Agricultural
Cattle, small farms,
Ilamelucos
extraction of precious
stones
Cacao
Cacao
Mulattoes and Negro
migratory workers
Plateau Mineral
Mining and Metallurgy
Mamelucos, Mulattoes,
Jews
Foreign Coloniza-
.Diversified farming,
Europeans and Japanese
tion
Japanese truck farms
Coffee and Indus-
Coffee, cattle,
Whites, Mestizoes,
trialization
industries
Mamelucos
Subsistence crops,
Indians, Mestizoes
rubber, nuts, timber
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Brazil: Socio-Economic Regions
NORTHEAST PASTORAL
SOUTHERN PASTORAL
NORTHEAST AGRICULTURAL
WEST CENTRAL
CACAO
PLATEAU MINERAL
FOREIGN COLONIZATION
COFFEE AND INDUSTRY
AMAZON
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107c
Figure 107. Rubber tapping in Amazon Basin. The slit bark (10'(a)
yields dripping latex (107b), which is reduced to huge balls that
are spot checked (107c) for quality before shipping.
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I. Attitudes and Loyalties
Defining the basic attitudes and loyalties of a people
that are dispersed geographically and diversified economically
and socially demands oversimplification. Brazilians have a
well-established reputation for tolerance, warmth, and candor.
They have a flair for the speculation that has dictated much
of their historical expansion into new fields of endeavor.
They are notorious opportunists, not only in business and
politics, but in personal situations as well. Abundantly
endowed with a keen sense of humor, even when directed at
themselves, Brazilians tend to maintain a genuine attitude of
cordiality under the most difficult situations. One of the
characteristics for which Brazilians are best known is the
ability to compromise -- a trait which has guided the country's
political history through numerous transitions without the
violence typical of most of the rest of Latin America.
Brazil's national unity has been called its chief miracle,
particularly in view of the fact that some of its regions
surpass in size most of the neighboring countries. Regional
differences have resulted in several identifiable "types"
among the Brazilian people. In the south the gaucho is sym-
bolic of the frontier spirit of individualism and energy.
Here also are found the most concentrated groups of immigrants
in Brazil, primarily from Europe, and they are characterized
by individual initiative and propensity for hard work. Strong
loyalties abound among the mineiros of Minas Gerais, the
rluminense of Rio de Janeiro state, the famous cariocas of
Guanabara State and the city of Rio de Janeiro, and the capixa-
bas of Espirito Santo. Political rivalries exist between Sao
Paulo and Minas Gerais, and competition is always rampant
between Paulistas and cariocas.
Regional consciousness in the Northeast is less pro-
nounced than in any other settled part of Brazil. The constant
struggle for existence by the lower classes and the power of
the absentee landowners have reduced loyalties in that region,
and migration from it has been constant for many years. The
development of social and political consciousness among the
poor and underprivileged of the area has been a significant
development, however, and their collective attitudes -- as yet
relatively passive -?- may ultimately emerge as one of the domi-
nant social forces of the country.
The West-Central Region of Brazil is a pioneer fringe,
where settlement is slowly being pushed westward into the
interior. The development of Brasilia has initiated a new
surge into this area, bringing a new level of sophistication
into the back country.
Approved For Release 1496167&4 'c1A-RDP85-00671 R000300020001-8
Approved For Release 1999/09d4rt1ARRrJE 85-00671 R000300020001-8
Brazilians in the Northern Region lack regional aware-
ness, being woodsmen, boatmen, or collectors in the forest
living on the most elementary level in Brazil.
The outstanding characteristic of Brazilian life is the
lack of racial discrimination in a society once divided into
masters and slaves. Although there is a very distinct class
structure in Brazil, its levels are based on attainment rather
than race. Wealth, education, talent, social manners, dress,
family background, and cultural activities all are factors,
but Brazilians do not automatically identify class status
with race. Thus, persons of dark skin may belong in the upper
class while others of light skin may fall far lower in the
class structure. While it is true that most Negroes are in
the lower classes, their lot has not been cast by the color
of their skin.
J. Insurgency Potential
Throughout its history, Brazil has endeavored through
nonviolence and compromise to cope with economic and political
conditions that would have produced inflammatory reactions in
the more volatile Latin American countries. Brazilians have
traditionally avoided disruptive revolutions, championed law
and order, bowed to authoritative control, and sought peaceful,
if inadequate, solutions to critical problems. Still, there
can be little doubt that a dormant potential for dissidence
exists in the complex social, economic, and political dimen-
sions of the country.
The army has a long tradition of loyalty and patriotism,
and the armed forces can be expected to counter any threat
to the Constitution or to representative government in an
orderly manner. The revolution of April 196+ against Jolo
Goulart's leftist regime was conducted quickly under consti-
tutionally sanctioned procedures, and there was little violence
beyond the few incidents that occurred during mass demonstra-
tions. Goulart, himself, had gained power in a similarly
tense but nonviolent and adroit shift in government when
Quadros resigned unexpectedly in 1961.
Recent decades have brought profound changes in all
phases of economic, social, and political life, thereby alter-
ing established social patterns and value systems. A restive
element among Brazilian youth is responding to leftist agita-
tion. Massive internal migration from rural to urban areas
has permitted previously passive and extremely poor peasants
to discover the possibilities for change in their traditional
way of life. Intense social problems are developing in urban
Approved For Release I 999/09/ 4 '_1A' RJbi 85-00671 R000300020001-8
Approved For Release 19MMU-1EC1A-RDP85-00671 R000300020001-8
slums, such as Rio de Janeiro's favelas, and in the overcrowded
and intolerable sections of the Northeast. A growing trend
among the masses of underprivileged Brazilians has been called
a "revolution of rising expectations," which is based on the
desire for a higher standard of living and is stifled by the
inability to achieve it.
The rural peasant has had little or no experience with
firearms and is typically uninformed about national affairs.
A 1960 poll revealed that one-half of a rural. sampling could
not name the president or president-elect. Throughout vast
areas, the peasant has always looked to his patroo (patron,
landowner) for solutions to his needs, and any shift from
this traditional pattern would require strong; evidence that
it would be for the better. If he were persuaded to become
involved in some action of a paramilitary nature, his role
would be one of minor support rather than active, intelligent,
or responsive participation.
Little in the way of support for established order could
be expected from the primitive indigenous Indians. Although
some groups have had ample practice in their own brand of hos-
tile behavior, their motivations have been aimed at tribal
isolation and self-preservation, and issues of vital concern
to the Brazilian populace are beyond the comprehension or con-
cern of the unacculturated Indian groups.
Approved For Release 1910?12 EC A-RDP85-00671 R000300020001-8
Approved For Release I 999/09/24 :r It-RR8'5-00671 R000300020001-8
Population of Brazil
Percent Increase
Population
In Thousands
State or Territory
1950-60
1960
196 (est)
Sao Paulo
42
12,974
15,845
Minas Gerais
27
9,798
11,189
Bahia
24
5,991
6,750
Parana
102
4,278
6,450
Rio Grande do Sul
21
5,449
6,340
Pernambuco
22
4,137
4,620
Rio de Janeiro
48
3,403
4,259
Guanabara
39
3,307
3,977
Ceara
24
3,338
3,755
Maranhao
57
2,493
3,234
Santa Catarina
38
2,147
2,579
Goias
73
1,955
2,565
Paraiba
18
2,018
2,211
Para
40
1,551
1,857
Espirito Santo
38
1,189
1,427
Piaui
21
1,263
1,397
Alag8as
16
1,271
1,380
Rio Grande do Norte
20
1,157
1,274
-163-
Approved For Release I 999/09/24 : GtA- P85-00671 R000300020001-8
Approved For Release 199091=CIA-RDP85-00671 R000300020001-8
Table 1 (Continued)
Percent Increase
Population
In Thousands
State or Territory*
1950-60
1960
19 5 (est)
Mato Grosso
76
910
1,254
Amazonas
41
722
870
Sergipe
18
760
834
Serra dos Aimores
140
384
640
Acre
40
160
193
Rond8nia (T)
92
71
103
Amapa (T)
84
69
97
Roraima (T)
63
29
39
Fernando do Noronha (T)
139
1
2
Brasilia
0
142
na
Total
70,96'7
85,141
Territories are designated by (T).
-164-
Approved For Release 19999LW241-CIA-RDP85-00671 R000300020001-8
Aft
Approved For Release 1999/09/241,-QWRDl?85-00671 R000300020001-8
Brazilian Cities With Populations Over 150,000
1960
City
Population
Rio de Janeiro
3,223,408
Slo Paulo
3,164,804
Recife
788,569
Belo Horizonte
642,912
Salvador
630,878
Porto Alegre
617,629
Belem
359,988
Fortaleza
354,942
Curitiba
344,560
Santos
262,048
Santo Andre'
230,196
Niteroi
228,826
Campinas
179,797
Duque de Caxias
173,077
Natal
154,276
Manaus
154,040
Maceio
153,305
-165-
Approved For Release I 999/09124 :OC P85-00671 R000300020001-8
Approved For Release I 999/ ,9/2 : I -RDP85-00671 R000300020001-8
Immigration to Brazil by Major Sources of Origin
1884-1962
Country of Origin
Number o:' Persons
Italy
1,479,295
Portugal
1,407,062
Spain
654,512
Japan
235,338
Germany
185,380
Russia
110,988
Austria
88,385
Turkey
78,854
Poland
53,771
Rumania
40,058
France
39,570
United States
34,224
England
29,460
Lithuania
28,665
Argentina
26,823
Yugoslavia
24,130
Syria
22,959
The Netherlands
1.3,049
Approved For Release 1999JO J? C4A,1RDP85-00671 R000300020001-8
Approved For Release 1999/09/24: CIA-RDP85-00671 R000300020001-8
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Approved For Release 1999/09/24: CIA-RDP85-00671 R000300020001-8
Approved For Release I 999/09 +._q RQJP85-00671 R000300020001-8
1. Movement Across Guianan, Venezuelan, Colombian,
Peruvian, and Bolivian Borders
Smuggling on a smaller scale is carried out overland with
the Guianas. Diamonds are brought from Guyana (formerly British
Guiana) to buyers in Boa Vista in northern Roraima, and small-
scale prospectors known as garimpeiros probably make frequent
illegal boundary corssings in search of minerals. Illegal
transit of the border for those who can afford air passage has
been facilitated by the establishment of small landing fields
associated with trading posts in the frontier zones. All
other movement, legal or illegal, between Brazil and the Guia-
nas is by water or trail, as there are no roads or railroads.
Inland waterways and trails also provide the only means
of transportation in the Brazilian border zones with Venezuela,
Colombia, and Peru. The Rio Negro is the principal avenue for
movement in the Brazil - Venezuela - Colombia trifrontier area,
but traffic is very light. Farther south, where Brazil,
Colombia, and Peru come together, the Amazon forms the main
transportation artery and cross-border traffic is heavy. Much
of the local trade focuses on the free port of Leticia,
Colombia's only outlet on the Amazon. Nearby is the small
Brazilian frontier post of Tabatinga.
Oceangoing ships continue up the Amazon to Iquitos, Peru,
some 300 miles from the border, or call at Benjamin Constant
on the Rio Javari a short distance upstream from its juncture
with the Amazon. The Javari forms over 500 miles of the
boundary between Brazil and Peru and is a major route for
contraband traffic between the two countries. The Rio Jurua
and the Rio Purus with its tributary, the Rio Acre, provide
additional navigable routes between Brazil and Peru.
The Acre also serves as a route between Brazil and north-
ern Bolivia's forest-covered Pando Department. Cobija, capi-
tal of the Pando, is located on the right bank of the Acre
directly across from the Brazilian town of Brasileia. Small
launches ferry passengers back and forth across the river.
No immigration or customs checks were reported on either side
as late as May 1963, and people and goods move freely in both
directions. At times during the dry season (May through
August), the Acre is fordable between Cobija and Brasileia.
Brazil's only surface connection with northern Bolivia,
other than the Rio Acre, consists of navigable tributaries of
the Rio Madeira system. Chief of these is the Rio Mamore.
The Mamore, forming some 160 miles of the boundary between
Bolivia and Brazil, is noted as an avenue for contraband.
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Thousands of head of cattle as well as dried meat are brought
into Brazil from Bolivia via the Mamore every year. Guajara-
Mirim, on the right bank of the river, is the principal Bra-
zilian port, whereas Puerto Sucre (also known as Guayamerin)
on the left bank, is the principal Bolivian port in the area.
Guajara-Mirim is linked by road and railroad to POrto
Velho on the Rio Madeira. Puerto Sucre is connected by trail
with Riberalta near the confluence of two navigable rivers,
the Rio Beni and its tributary the Rio Madre de Dios. The
Beni is navigable to shallow-draft boats for nearly 600 miles
southwestward in the direction of La Paz while the Madre de
Dios is navigable to small stream launches throughout its
course in Bolivia and for 50 miles in Peru to Puerto Maldonado.
Cuban-trained subversives, after transiting Brazil and Bolivia,
have used the Madre de Dios to enter Peru.
The Rio Guapore, a major tributary of the Mamore, forms
approximately 500 miles of the boundary between Bolivia and
Brazil. Traffic on the river is extremely light, but regular
service is maintained from Guajara-Mirim on the Mamore all
the way upstream to the town of Mato Grosso at the head of
navigation on the Guapore. There are few settlements in the
area other than small Indian villages and scattered outposts
for gathering rubber. From Mato Grosso numerous trails extend
into Bolivia and a road (BR-416) runs southeastward to Caceres
on the Rio Paraguai.
During 1964 guerrillas operating in Bolivia's Beni and
Santa Cruz Departments were reported to have crossed the Rio
Guapore into Brazil often. Crossings are said to have been
made in the vicinity of Principe da Beira and at several
other points along the river. Supplies for the Bolivian
guerrillas reportedly were flown in from Brazil by Catalina-
type flying boats, which used some of the many small lakes in
the frontier zone south of the Rio Guapore.
The only rail link between Bolivia and Brazil is the
meter-gauge Santa Cruz - Corumba line, which enters the State
of Mato Grosso from eastern Bolivia. It has been said that
the Bolivian border town on the line, Puerto Suarez, practically
exists on smuggling. Goods brought to Puerto Suarez by rail
reportedly are smuggled across the border at night to Corumba,
Brazil, where they demand good prices. In addition to the
usual cigarettes, whisky, and perfume, machineguns and ammunition
concealed in sacks of salt were recently discovered being shipped
into Corumba from Bolivia.
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Regular ferry service is maintained between Puerto Suarez
and Corumba. Ladario, near Corumba, serves as headquarters
of the Mato Grosso Naval Command on the border, and its facili-
ties provide maintenance for the gunboats that patrol the
river. A number of small lakes along the border give Bolivia
access to the Rio Paraguai. For a short distance the Rio
Paraguai forms the southernmost part of the boundary between
Bolivia and Brazil.
2. Movement Across Paraguayan Border
The Rio Paraguai forms nearly 200 miles of the Brazil -
Paraguay boundary. Transportation facilities along both the
Brazilian and Paraguayan sides of the river are very limited.
Several narrow-gauge lumbering railroads extend back into the
Paraguayan Chaco from minor ports on the river. Most of the
other settlements on the river have few or no landing facili-
ties. At Bahia Negra and Olimpio, for example, boats simply
tie up to the river bluff. Going downstream on the Brazilian
side the first town of any importance is Porto Murtinho,
which has a road connection (BR-267) running eastward to join
the main highway network of Mato Grosso. Isla Margarita, a
small Paraguayan island in the river near Porto Murtinho, has
allegedly been the site of considerable contraband activity.
River vessels tie up directly to the beach.
About 25 miles south of Porto Murtinho the boundary is
formed by the Rio Apa, a left-bank tributary of the Rio Para-
guai. Bela Vista, on the Brazilian side, is the only sizable
town on this river. It has an airstrip and a road (BR-74)
that runs northward to Jardim to connect with the rest of the
road system of Mato Grosso. On the Paraguayan side, opposite
Bela Vista, is Bella Vista, which also has a small airstrip
and a poor dirt road that leads southward to Concepcion.
Recent plans call for a bridge over the Rio Apa to connect
the two towns.
Southeast of Bela Vista, beyond the headwaters of the
Apa, the Brazil - Paraguay boundary follows a drainage divide
as far as the Rio Parana. At a number of places in this seg-
ment, settlements actually straddle the boundary. For example,
Ponta Porgy. (Brazil) and Pedro Juan Caballero (Paraguay) are
practically a single town, with the boundary extending down
the main street. The movement of people or goods from one
town to the other is not controlled, and the place has long
been the center of a flourishing contraband trade. Coffee,
cotton, electrical appliances, and other items have entered
Paraguay through this border town, whereas whisky, drugs,
cloth, and firearms reportedly have moved in the other direction.
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Since the Brazilian revolution of 1 April 1964, however, mili-
tary checkpoints have been established along the roads out of
Ponta Porn, and these may have reduced the flow of contraband.
Jeepable roads parallel the border on the Brazilian side north
and south of Ponta Pora, and a federal highway (BR-86) runs
northeastward to Dourados. A branch line of the Northwestern
of Brazil Railway extends from Ponta Fora to Campo Grande, where
it joins the trunk route from Bauru to Corumba. An airfield
with gravel-surfaced runways is located a short distance south-
east of Ponta Porl.
Transportation facilities on the Paraguayan side of the
border are more limited. Roads are usable in good weather for
trucking out coffee, but there are no railroads, and the all-
weather road to Concepcion is still under construction. A
small airfield southeast of Concepcion is used for semiweekly
flights of DC-3 aircraft of the Paraguayan Military Air Trans-
port service. Reportedly, many of the contraband goods that
arrive in Pedro Juan Caballero continue their journeys to other
destinations by air.
The relationship between the border villages of Antonio
Jogo (Brazil) and Capitan Bado (Paraguay) is similar to that
between Ponta Porn and Pedro Juan Caballero, though the villages
are smaller. The boundary runs down the main street, and
commerce between the two sections is probably completely free.
Roads on the Paraguayan side are little better than trails. On
the Brazilian side a dirt road extends to Amabai and connects
with the highway leading to Ponta Por5.. A small airfield is
Located about a mile north of Antonio Joao. During the wet
season (November to May) small, shallow-draft; boats can navigate
the nearby Rio Iguatemi for about 130 miles downstream to its
confluence with the Rio Parana.
The Rio Parana forms the boundary between Brazil and
Paraguay for about 130 miles -- from just above the great
waterfalls known as the Sete Quedas downstream to the mouth of
the Rio IguaQu. Several minor ports -- Guaira, Porto Mendes,
Porto Britania, Porto Santa Helena, and Foz do Iguagu -- are
located on the Brazilian side of the river but, except for a
few primitive landings, most of the area along the Paraguayan
side includes nothing but dense forests. The Brazilian river
ports are connected by secondary roads to the main road network
of Parana, and a short railroad runs from PC--to Mendes to Guaira
as a bypass to the Sete Quedas. The few small settlements on
the Paraguayan side of the river are connected by foot trails
and logging roads.
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A recently opened international bridge spanning the Rio
Parana just north of Foz do Iguazu provides an important
highway link in the Pan American Highway system between Brazil
and Paraguay (see Figure 150). Completion of the bridge opens
a route all the way from Asuncidn, Paraguay, to the port of
Paranagud. on the Atlantic coast. The Paraguayan Military Air
Transport service makes regular flights to a small airfield
at Puerto Presidente Stroessner, a new village at the Para-
guayan end of the international bridge. On the Brazilian side
of the river a small airstrip near Foz do Iguazu is used regu-
larly on flights between Brazil and Paraguay. Many tourists
land at this airfield and visit the famous Iguazu waterfalls
a short distance upstream on the Rio Iguazu, especially in the
period from May to November. A gravel road (BR-277) runs
northeastward from Foz do Iguazu to Cascavel.
3. Movement Across Argentine Border
The Rio Iguazu forms part of the boundary between Brazil
and the northeastern tip of Argentina. Large national parks
of Brazil and Argentina occupy the densely forested country
immediately north and south of the river. Puerto Iguazu,
near the confluence of the Rio Parana and the Rio Iguazu, is
the only sizable town on the Argentine side. An outboard
motorboat ferries passengers across the river from Puerto
Iguazu to the village of Porto Meira on the Brazilian side.
From PSrto Meira a road leads to Foz do Iguazu, a few miles
away. Argentine Route 101 extends from Puerto Iguazu to
Cataratas del Iguazu near the waterfalls, which has an air-
field and a hotel. Small boats can cross the river a short
distance above the falls. From Cataratas del Iguazu, Route
101 continues to Bernardo de Irigoyen, about 60 miles to the
southeast on the Brazilian frontier. Another gravel road,
Argentine Route 12, extends from Cataratas del Iguazu south-
westward along the Rio Parana to Posadas.
Rio Santo Antonio, a tributary of the Iguazu, forms
about 40 miles of the border between Parana and Argentina's
Missiones Province. On the Brazilian side, a gravel road
runs southward to Santo Antonio and on to Barracao, a border
town at the headwaters of the Rio Peperi Guaju. From Barracgo,
dirt and gravel roads radiate into Argentina (northeastward to
Puerto Iguazd and southeastward to Posadas) as well as eastward
through Parana and southward into Santa Catarina.
The Rio Peperi Guacu, flowing southward from Barrac.o,
constitutes most of the boundary between Argentina and Brazil
in the Santa Catarina State segment; it is navigable by shallow-
draft boats for a short distance above its juncture with the
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Figure 150. Recently completed international bridge
over the Rio Faran4 between Brazil and Paraguay
near Foz do Iguacu. With a central concrete span
951 feet long, this bridge is one of the longest
of its kind in South America.
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Rio Uruguai not far from Itapiranga. The Rio Uruguai forms all
of the remaining 445 miles of the Brazil - Argentina boundary.
Moving downstream along the river, settlements become larger
and their supporting transportation facilities correspondingly
better developed. Sffo Borja and Itaqui on the Brazilian side
and Santo Tome and La Cruz in Argentina have airports and road
and rail connections, as well as minor river port facilities.
Sdo Borja is the export point for Brazilian timber and grain
destined for shipment across the river to Santo Tome; it also
handles the importation of a considerable amount of Argentine
salt. Contraband trade reportedly has thrived in the vicinity
of SSo Borja.
Farther downstream, at Uruguaiana, is the only bridge
across the Rio Uruguai between Brazil and Argentina. It is
a combination railroad and highway bridge that extends from
Uruguaiana to Paso de los Libres on the Argentine side. A
dual-gauge track across the bridge provides an interconnection
between the standard-gauge line on the Argentine side, which
runs from Buenos Aires to Posadas, and the meter-gauge line of
the Rio Grande do Sul Railway on the Brazilian side, which
extends eastward to Santa Maria. Roads parallel the river
north and south of Uruguaiana, and an all-weather gravel road
(BR-290) extends eastward to Alegrete.
4. Movement Across Uruguayan Border
The Brazilian border with Uruguay is approximately 525
miles long. Slightly over two-thirds is defined by rivers,
streams, and other water bodies, and the remainder -- the
central segment -- is defined by drainage divides and other
terrain features.
The Rio Quarai (known as the Rio Cuareim in Uruguay)
forms most of the western third of the boundary. It is navi-
gable by small craft for only a short distance above its con-
fluence with the Rio Uruguai, and its upper reaches are
fordable in numerous places except during high-water stages.
Both railroad and highway bridges cross the Rio Quarai between
Barra do Quarai and Bella Union. The meter-gauge Rio Grande
do Sul Railway extends southward from Uruguaiana and makes an
international connection at Barra do Quarai where a dual-gauge
line crosses the Rio Quarai to Bella Union, Uruguay. A stand-
ard-gauge Uruguayan line continues southward to'Montevideo.
There are also rail and road connections farther upstream
between the towns of Quarai (Brazil) and Artigas (Uruguay).
A gravel road and several dirt roads extend into Brazil from
Quarai, and a paved highway (Uruguay Route 30) connects Artigas
with other points in Uruguay. Small airfields are located about
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a mile northeast of Quarai and a short distance southwest of
Artigas.
Continuing to the southeast along the border, the Brazil-
ian town of Santana do Livramento is separated by a street
from the Uruguayan town of Rivera. Two lines of the Rio Grande
do Sul Railway system focus on Santana do Livramento -- one
running southwestward from Rosario do Sul and the other west-
ward from the deep-water port of Rio Grande. A dual-gauge
track connects these meter-gauge lines with a standard-gauge
line extending from Rivera to Montevideo via Tacuarembo. An
airfield is located about 6 miles northwest of Santana do
Livramento, and three other small ones are situated within 5
miles of Rivera. Two gravel roads and numerous dirt roads
radiate from Santana do Livramento, and a paved highway (Uru-
guay Route 5) extends southward from Rivera to Tacuarembo.
Dirt roads cross the border at several places southeast
of Santana do Livramento, but the only significant border-
crossing point northwest of Jaguarao is at Acegua where a
gravel road runs northward to Bage' and southward to Melo,
Uruguay. Beginning at a point not far from Acegua and extend-
ing southeastward to Lagoa Mirim the boundary is formed by the
Rio Jaguaro. This stream, like the Rio Quarai, is navigable
for a relatively short distance above its mouth, and its upper
reaches are usually fordable in numerous places.
The Brazilian town of Jaguar2[o is situated about 14 miles
upstream from the mouth of the Rio Jaguardo. It is connected
by a combination rail and highway bridge with Rio Branco on
the Uruguayan side. With a total length of 6,900 feet, the
bridge is one of the longest in South America.. A meter-gauge
branch line of the Rio Grande do Sul Railway extends northward
and connects with the trunk line to Rio Grandde; a standard-
gauge line extends from Rio Branco to Montevideo. Port facili-
ties at Jaguarlo and Rio Branco are used by small coastal ves-
sels and river steamers. A small airfield is located about
4 miles north-northwest of Jaguarfto, and another airfield or
landing site is probably located near Rio Branco on the Uru-
guayan side. In addition to several dirt roads that radiate
from the two towns, gravel roads extend northeastward to Pelotas
and westward to Mele, Uruguay.
From the mouth of the Rio Jaguarlo southward the boundary
between Brazil and Uruguay runs down the center of Lagoa Mirim
and, for a short distance, along a small stream at the southern
end of the lake. Lagoa Mirim is used mostly by shallow-draft
Brazilian trading vessels and Uruguayan fishing boats. Reportedly,
the lake and surrounding area have been the scene of considerable
contraband traffic.
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The bordering towns of Chui (Brazil) and Chuy (Uruguay)
are situated midway along the short segment of frontier
stretching from the extreme southern tip of Lagoa Mirim to
the Atlantic Ocean. A street marks the boundary between the
two towns. A gravel road (BR-471) runs northward out of Chui
and along the dune-bordered tract separating Lagoa Mirim from
the sea. Uruguayan Route 9 extends southward along the coast.
The nearest known airfield to this segment of the border
on the Brazilian side is a grass field about 2-1/2 miles
northeast of Santa Vitoria do Palmar, which is approximately
10 miles northeast of Chui. It is used in civil light trans-
port operations and is the southernmost airfield in Brazil.
A privately owned pasture on the Uruguayan side of the border,
near Chuy, has also been used as a landing field by light air-
craft. After shopping in Chui, Brazil, Uruguayans return across
the border and depart from this field to avoid the customs
checkpoints on the access roads to Chuy.
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Figure 151. Hercilio Luz bridge connecting Floriano'polis on
Ilha de Santa Catarina with the mainland of Santa Catarina
State.
Figure 152. Railroad bridge over the Rio Itajai near Blumenau
on the trunkline of the Santa Catarina Railway.
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READING LIST
1. CIA. NIS 94, Brazil, sec 31, "Railway," Aug 1963. C/NFD.
2. CIA. NIS 94, Brazil, sec 32, "Highway," Oct 1961. C/NFD.
3. CIA. NIS 94, Brazil, sec 33, "Inland Waterway," Mar 1959.
C/NFD.
4. CIA. NIS 94, Brazil, sec 35, "Ports and Naval Facilities,"
Aug 1964. C/NFD.
5. CIA. NIS 94, Brazil, sec 36, "Merchant Marine," Jan 1962.
C/NFD.
6. CIA. NIS 94, Brazil, sec 37, "Civil Air," Mar 1964.
C/NFD.
7. DIA. LOC, Brazil, Sep 1963. C.
8. Railway Gazette. "Brazilian Railways," Overseas Railways
1964, London, 1964. U.
9. Estradas de Ferro do Brasil -- 1960, supp to Revista
Ferroviaria, Rio de Janeiro, 19 0. U.
10. Conselho Nacional de Estatistica. Anuario Estatistico
do Brasil, 1966, Rio de Janeiro, 1976-. U.
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A. General
Brazil's common carrier telecommunications system is
seriously inadequate in relation to national needs. For
domestic telephone and telegraph service, most users must
depend mainly on open wirelines and high-frequency (HF)
radio facilities, which are relatively low in both capacity
and reliability. Modern high-capacity transmission media,
such as microwave radio relay and coaxial cable, are avail-
able only between several of the larger cities in south-
eastern Brazil. In addition to common carrier facilities,
the armed forces, police, and railroads operate special-
purpose telecommunications networks; for the most part, these
specialized networks are not accessible to the general public.
International communications and broadcasting services
are relatively better developed than domestic common carrier
telecommunications. Brazil is connected by open wireline to
neighboring countries in the south and by HF radio and sub-
marine telegraph cable to more distant points. Brazil's
broadcasting facilities number more than 800 radio stations
and about 60 television stations. The Brazilian reception
base consists of about 10 million radio sets and approximately
2.5 million television sets.
B. Organization of Telecommunications Services
Over 500 companies, both governmental and private, operate
Brazil's telecommunications system, under the supervision of
the National Telecommunications Council (Conselho Nacional de
Telecomunicag('es, or CONTEL), created in 19 2. The principal
telecommunications enterprise owned by the government is the
Department of Posts and Telegraphs (Departamento dos Correios
e Telegrafos, or DCT), which operates an extensive tele-
graphic open wireline system and some HF radio stations. The
major private firm is the Brazilian Telephone Company (Companhia
TelefOnica Brasileira, or CTB), which operates about 75
percent of the country's telephone service. The CTB has been
under government intervention since 1962. Other important
private firms are the International Radio Company of Brazil
(Radio Internacional do Brasil, or RADIONAL) and the Radio-
telegraph Company of Brazil (Companhia Radiotelegrafica
Brasileira, or RADIOBRAS) which provide domestic and inter-
national high-frequency radio services. Also noteworthy are
are Italcable Cable, Telegraph, and Radio Services (Italcable
Servizi Cablografici, Radiotelegrafici, e Radioelettrici S.A.)
and the Western Telegraph Company, operators of coastwise and
international submarine cables.
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C. Telephone and Telegraph Facilities
1. Domestic
Brazil's domestic telephone and telegraph transmission
media consist of a mixture of open wirelines; HF radio, micro-
wave radio relay, coaxial cable, and submarine cable (see Maps
56150 and 56151). The open wireline system, although quite
widespread, is of generally poor quality and inadequate to
fulfill the telephone and telegraph transmission needs of
the country. Most of the open wirelines are owned by the
DCT and are used for telegraph transmission. The DCT, how-
ever, does lease some of its lines to private firms, and in
the southeast private firms own and operate open wirelines
providing telephone services. The public open wireline
system is supplemented by the open wireline system of the
railroads. This network is integrated into the public net-
work and, thus, extends telecommunications services into
areas of the country not reached by the DCT system itself.
In addition to open wirelines, a network of HF radio
facilities also handles telephone and telegraph traffic.
These facilities are operated primarily by RADIONAL and
the DCT. The HF radio network provides telephone and
telegraph connections among the more widely separated
major cities and constitutes the primary means of communi-
cations for many of the towns of the interior.
Brazil's most modern and efficient telecommunications
media are located in the geographic triangle described by
Rio de Janeiro, Sao Paulo, and Brasilia. They consist of
microwave radio relay routes and coaxial cable lines with
capacities ranging from 120 to 420 voice channels. As
shown in Map 56151, microwave radio relay routes radiate
from Rio de Janeiro to Sao Paulo, Campinas, and also to
.3rasilia via Belo Horizonte. Coaxial cables of high capac-
ity augment the microwave radio relay system by providing
connections between Rio de Janeiro and Petropolis and also
between Sao Paulo and Santos.
Submarine cables capable of single-channel telegraph
transmission connect the coastal cities of Rio Grande,
Floriandpolis, Santos, Rio de Janeiro, Vitdria, Salvador,
Maceio, Recife, Natal, Fortaleza, Sao Luis, and Belem.
By 1966 Brazil had approximately 1.3 million telephones
ror a population of about 84 million. This ratio is not only
far below those of North America and Western Europe, but is
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also substantially lower than comparable ratios for Argentina,
Chile, Colombia, Uruguay, and Venezuela. Most of Brazil's
telephones are located in the southeast, the most industrialized
part of the country. More than 50 percent of them are con-
centrated in just two cities: Rio de Janeiro with about
375,000 and Sao Paulo with about 300,000. Telephone exchanges
in Brazil are generally automatic in the major cities, except
for Rio de Janeiro, where 68 out of 95 exchanges are manual.
2. International
Brazil uses a variety of media for international tele-
communications, including open wirelines, HF radio, and
submarine telegraph cables. International telephone and
telegraph connections via open wireline run from southern
Brazil into the adjoining countries of Argentina, Paraguay,
and Uruguay. Submarine cables provide international tele-
graph links to North and South America, Europe, and Africa
from terminals located in Rio de Janeiro, Rio Grande, Santos,
Recife, and Sa'o Luis. Brazil's chief means of international
telephone and telegraph communication, however, is HF radio.
Both RADIONAL and RADIOBRAS have HF facilities which provide
connections with major cities in North and South America,
Europe, Africa, and Asia. RADIONAL's transmitter site is
located at Marapicu (near Rio) and the RADIOBRAS transmitting
facility is located at Sepetiba (also near Rio). The inter-
national receiver sites of both companies are located at
Jacarepagua, a Rio suburb. The DCT also operates HF radio-
telegraph links from other cities in Brazil to adjoining
countries of South America. All of these international
facilities are tied into the domestic telecommunications
system, enabling them to handle traffic to and from the cities
of the interior.
D. Broadcasting
1. Radio
Radiobroadcasting is the most extensively developed
telecommunications service in Brazil. Brazil has more than
800 AM broadcasting stations and about 115 FM stations, most
of which are privately owned. The vast majority of these
are low-power facilities designed for local listening.
Brazil has no well-developed broadcasting network system,
although the government does operate "Radio Nacional"
stations in Brasilia, Rio de Janeiro, and Sao Paulo which
broadcast the official viewpoints of the Brazilian government.
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Also, the government requires the private radio stations to
broadcast regularly the government program "Aggncia National."
In addition, the Catholic Church owns or controls a group of
approximately 90 radio stations, located for the most part
in the smaller towns of the interior. There are about 10,000,000
radio receivers in Brazil.
2. Television
Brazil has about 60 television stations, most of which
are concentrated in the populous southeast area of the country.
As with the radiobroadcasting stations, most of the television
stations are privately owned and operated. The government does,
however, operate "Radio Nacional" television stations in
Brasilia and Rio de Janeiro. There are approximately 2.5
million television receivers in Brazil.
E. Special-Purpose Telecommunications Systems
Brazil has several rather extensive special-purpose
telecommunications systems, the most important of which are
those of the military, the railroads, and the state police
forces.
1. Military
The army, navy, and air force each operate telecommunica-
tions systems designed to service their own specialized needs.
These systems use HF radio, microwave radio relay, and open
wirelines. All of the networks have HF radio links between
regional headquarters and their respective ministries in
Brasilia. The air force has greater communications cap-
abilities than the other services, since it is normally
responsible for civil aviation control. During an emergency
the navy can enlarge its communications system by taking
over the networks of the merchant marine and the oil
industry.
2. Railroad
The railroads operate an extensive network consisting
of open wirelines, HF radio, and microwave relay. The open
wireline system provides telegraph circuits between minor
stations, while the major stations are linked by HF radio.
This system interconnects with the public network, thus
extending common carrier communications into the more
isolated areas of Brazil.
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3. State Police
Many of the state police forces of Brazil have HF radio
networks which connect the state capital with other state
municipalities. For many of the smaller towns, this is the
only telecommunications link with the outside world. At
present, the state of Minas Gerais has a 58-station network
and the state of Goias has an 11-station network. Many of
the state police networks now are being improved and expanded
with the assistance of the US Agency for International Develop-
25
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LEADING LIST
1. CI.A. NIS 94, Brazil, sec 38, "Telecommunications", Jan
1965. C/NFD.
25X1A8a p
2. Broadcasting Stations of the World, pt I and
3. International Bank for Reconstruction and Development.
Current Economic Position and Prospects of Brazil, vol IV,
"Telecommunications," 11 May 1965. OUO.
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IX. Military and Internal Security Forces
A. General
The Brazilian military establishment, the largest in
South America, consists of an army of 150,000, an air force
with 28,100 personnel and nearly 900 aircraft, and a navy
with 20 major combatant ships and 39,900 men, including
9,500 marines. These forces are supplemented by state mili-
tary police forces totaling 114,050. The armed forces are
capable of maintaining internal security and of defending the
country against attack by neighboring countries, but they
would be incapable of sustained defense against substantial
forces of a major military power. The armed forces could
conduct effective offensive operations against any neighboring
country, with the possible exception of Argentina, but would
be seriously handicapped by logistic difficulties except in
the southern portion of the country. With outside logistic
support, they could assist materially in hemispheric defense
and provide a small expeditionary force, as they have in the
past.
The strengths of the armed forces include a strong esprit
de corps, the discipline of the enlisted men and their capa-
bility to operate under conditions of physical hardship, the
generally high level of education of officers, and the experi-
ence of some of the officers in World War II, the Dominican
Republic, and in the United Nations mission in the Gaza Strip.
Weaknesses include dependence upon foreign sources for aircraft,
naval vessels, and other major military items; the scarcity of
specialists, technicians, and highly qualified noncommissioned
officers; the illiteracy of many enlisted personnel and the
frequent turnover of conscripts; the heterogeneous nature of
equipment; and a restrictive military budget.
The armed forces of Brazil, especially the army, have been
a major force in the efforts to consolidate the country eco-
nomically and politically and to develop its communications
and bring civilization to the underdeveloped regions of the
interior. They have generally played the role of protector
of the nation's traditions and defenders of constitutionality.
The post of Commander in Chief of the Armed Forces is
held by the President of the Republic. He directs all activi-
ties concerned with national security and appoints the service
ministers and chiefs of staff. He is assisted by the Presi-
dential Military Staff, the National Security Council, and the
Armed Forces General Staff.
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The presidential Military Staff serves as the President's
personal staff, assisting him on military matters, including
relations with high military authorities. It is also respon-
sible for his safety.
The National Security Council advises the president on
matters of security, war planning, and conduct of war. The
Council consists of the president, as its head, the ministers
of state, the Chief of the Armed Forces General Staff, the
chiefs of general staff of the army, navy, and air force, plus
such other high-ranking officers and officials as the president
may appoint.
The Armed Forces General Staff prepares plans involving
joint organization and employment of the armed forces, provides
staff support for wartime operational command of the armed
forces, and assists in total mobilization in time of war. The
Chief of the Armed Forces General Staff is a general or flag
officer appointed by the president; the chiefs of the general
staffs of the army, navy, and air force are also members.
Subordinate to the Armed Forces General Staff are the Superior
War College, the Brazilian Delegation to the Joint Brazil-United
States Military Commission (JBUSMC), and wartime theaters of
operations.
Except for the wartime functions of the Armed Forces Gen-
eral Staff, none of the president's advisory elements has
operational control over the armed forces. Final responsibility
and authority in army, navy, and air force matters are vested,
respectively, in the Minister of the Army, the Minister of the
Navy, and the Minister of Aeronautics.
Ground Forces
The Brazilian Army, the largest in South America, is capa-
ble of maintaining internal security and of defending the coun-
try against any combination of South American countries. The
army has traditionally considered its principal mission to be
defense against attack from Argentina. Its major troop concen-
tration is in southern Brazil.
The army makes an important contribution to the national
economy through the construction of roads, railroads, and dams,
the suppression of smuggling, and flood and other disaster
relief activities. A significant part of the army's effort is
spent on civic action projects such as providing the general
population in remote areas with medical care, instruction in
reading, and assistance in land settlement. Since 1961, when
organized rural unrest in northeastern Brazil appeared to offer
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favorable opportunities for Communist exploitation, the army
has given increased emphasis to internal security. Most of
the independent units of less than division size scattered
throughout Brazil have internal security as their primary
mission, and the army is capable of controlling any overt
internal threat to national security.
Although its combat capability compares favorably with
that of other South American armies, the army has a number
of weaknesses. Its funds are insufficient for the acquisition
of new equipment, and many weapons are obsolete. Combat
training is largely theoretical. The army is weak in organi-
zation, planning, and experience at division level and above,
in noncommissioned officer leadership, and in all support
services. It lacks the weapons and equipment required for
mobilization and is dependent upon foreign sources for most
heavy equipment.
The army, however, has certain important strengths.
Esprit de corps, particularly among the officers, is strong,
and military training is good in comparison with that in most
Latin American armies. Many key senior officers had active
combat experience in Italy during World War II. More recently,
others have acquired useful experience with the Inter-American
Peace Force in the Dominican Republic and with the UN mission
in the Gaza Strip. Enlisted men are willing, amenable to dis-
cipline, and inured to hardship.
The army is divided into four numbered territorial armies
and two special commands -- the Amazon and the Brasilia Military
Commands -- all of which are directly under the Ministry of the
Army. Subordinate to the armies and commands are 11 military
regions. The numbered army is the highest tactical echelon.
The division is the basic major unit and the echelon directly
responsible for the tactical training of troops. Except for
cavalry, division organization is based on US models.
The army's strength averages about 150,000, with 14,000
officers, 30,000 career noncommissioned officers, and the
remainder conscripts (82,000) and volunteers (24,000). It is
organized into 12 divisions (7 infantry, 4 cavalry, 1 armored),
1 mixed brigade, 3 coast artillery groups, 6 independent regi-
ments (3 cavalry, 1 infantry, 1 airborne, 1 field artillery),
and 41 separate battalions (20 infantry, 2 coast artillery,
2 field artillery, 3 armored, 1 anti-aircraft artillery, 3
military police, 7 engineer, 3 signal), and various service
units.
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Over 40 percent of the army is concentrated in the three
southern states, with about one-third of total strength in
the southernmost state of Rio Grande do Sul. Over 30 percent
are in the four key industrial and agricultural states around
Rio de Janeiro and S.o Paulo. Of the remainder, about half
is in northeastern Brazil, and the balance is dispersed through-
out the rest of the country.
Brazil has a growing capability to produce small arms and
ammunition. Various models of pistols, revolvers, rifles,
carbines, and submachine guns are now being manufactured by
Brazilian industry in small quantities. In spite of this, the
military and police still rely primarily on European and Ameri-
can small arms. The principal foreign small arms in use are:
the Belgian FN FAL 7.62mm rifle, the Belgian M1908 Mauser 7mm
rifle and carbine, the Belgian FN M1949 .30 cal. rifle, the
US M1903 .30 cal. rifle, and the US M-1 .30 cal. rifle and
carbine.
Most mortars, artillery, and military equipment are of
US WWII vintage, but there is also a large inventory of widely
differing, generally outmoded European equipment of French,
Swedish, German, British, Danish, and Swiss origin. Brazilian
industry supplies most mortars, artillery, ammunition up to
155mm, and light military vehicles.
Brazil has no long-range agreements with governments other
than the US for supply of weapons or equipment.
Before World War II, training followed European, particu-
larly French patterns. Since 1942, US methods have been intro-
duced, especially through the Joint Brazil-United States Mili-
tary Commission and the Military Assistance Advisory Group
(MAAG) in Brazil. Since about 1950, MAP-supported units have
followed US Army training programs, but progress has been slow.
Although there are qualified instructor personnel, training is
handicapped by insufficient funds, a shortage of facilities,
much obsolete and nonstandard equipment, the low educational
level of trainees, limited field exercises, and overreliance
on theoretical instruction. Most of the first 3 months is
devoted to close order drill, improvement of health and stamina,
and instruction in reading, writing, and citizenship. Little
time is available for unit training because of the 8-month
conscript cycle. Unit training normally takes place in unreal-
istic small-scale field exercises held annually by various
units and lasting a week or less.
Noncommissioned officers of the combat arms are trained in
the School of Sergeants of Arms at Tres Coral es, Minas Gerais.
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Advanced and specialized courses are provided in armored,
coast artillery, medical, veterinary, physical education,
communications, specialist training, airborne, and anti-
aircraft schools.
Most officer candidates are trained at the Military
Academy at Resende in the state of Rio de Janeiro. Higher
schooling for officers is provided at the specialized schools
mentioned above, at the Officers Advanced School at Vila
Militar in the state of Rio de Janeiro, and at the Army Com-
mand and General Staff School at Rio de Janeiro. Selected
officers receive more advanced training at the Superior War
College, also in Rio de Janeiro. In recent years, many offi-
cers have received advanced branch and general staff training
in the United States, and some officers and noncommissioned
officers have been trained at the US Army School in Panama.
The army makes excellent use of personnel trained by the United
States, assigning many of them as instructors. A limited
number of officers are sent to French and German military
schools.
C. Naval Forces
The Brazilian Navy vies with the Argentine Navy as the
largest in South America. It is capable of defending Brazil
from seaborne attack by any neighboring country, but could
offer only limited resistance against a modern naval force
of comparable size.
The missions of the navy are to protect sea communica-
tions, coastal. shipping, and river traffic and to defend the
country against attack from the sea. Brazil is, in addition,
committed to the defense of the Western Hemisphere in a patrol
and anti submarine warfare (ASW) capacity. ASW capabilities
have improved in recent years with the transfer of destroyers
and submarines from the United States, and the participation
of the Brazilian fleet in combined ASW exercises with US,
Uruguayan, and Argentine naval forces.
The lack of naval base facilities outside of Rio de Janeiro
has been a serious limiting factor in naval operations. The
navy has begun a program of building outlying bases (notably
at Belem, Salvador, Natal, and Recife) and is improving the
relatively extensive facilities in Rio de Janeiro. There are
drydocks in Rio de Janeiro and Belem capable of handling the
largest navy ships, and naval and commercial facilities capable
of handling all but the largest ships have been or are being
built in other ports.
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General policy matters are the responsibility of the Mini-
ster of the Navy. Overall control of the forces afloat is
vested in the Chief of Naval Staff, who delegates authority for
operational matters to the Vice Chief of Naval Staff. The
Ministry of the Navy and the Naval Staff are mostly located
in Rio de Janeiro. Parts of the ministry and staff have
moved to Brasilia. The headquarters of the operational forces
are also in Rio de Janeiro.
The fleet is composed of several commands: cruiser
division, destroyer flotilla, submarine flotilla, and mine
force. Other operational forces afloat are The transport
force, the hydrographic survey ships, two coastal patrol
forces, and two river flotillas. The navy's one aircraft
carrier operates directly under the Chief of Naval Staff.
Brazil is divided into seven naval districts each headed
by a commandant. Headquarters of the districts are at Rio
de Janeiro, Salvador, Recife, Belem, Florianepolis, Ladario,
and Brasilia. The naval district commandants exercise command
over the ships, installations, establishment, forces, and
naval personnel assigned to the districts.
The personnel strength of the navy is approximately
39,900 of which about 30,400 are in general service (4,000
officers and 26,400 enlisted men) and about 9,500 are in the
marine corps (400 officers and 9,100 enlisted men). Some
12,500 officers and enlisted men serve afloat. A majority of
naval and marine personnel, afloat as well as ashore, are
based in Rio de Janeiro and its environs.
The Brazilian Navy consists of the following ships: 1 ASW
support aircraft carrier (CVS), 2 light cruisers (CL), 9 destroy-
ers (DD), 5 destroyer escorts (DE), 3 submarines (SS), 3 small
submarine chasers (SC), 2 river gunboats (PR), 4 old coastal
minesweepers (MSC [0]), 3 coastal surveying ships (AGSC), 2 sur-
veying ships (AGS), 1 oceanographic research ship (AGOR), 2
gasoline tankers (AOG), 4 transports (AP), 3 auxiliary ocean
tugs (ATA), 10 fleet ocean tugs (ATF), 1 battle damage repair
ship (ARB), 1 floating drydock (ARD), 2 small, auxiliary floating
drydocks (AFDL), and 34 service craft. Most combatant ships
were built in the US, UK, or Brazil. Many are of WWII or
earlier construction. The condition of ships ranges generally
from fair to good.
The major part of the fleet is based at Rio de Janeiro.
The river gunboats, attached to the Mato Grosso Flotilla, are
based at Lada'rio on the Paraguay River; 1 SC and 2 ATF are
based at Recife; and 4 ATF and several service craft are based
at Belem.
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The Brazilian Naval Air Arm (BNAA), a small, integral
part of the Brazilian Navy, is under the Directorate of Naval
Aeronautics, the Director General of which is directly respon-
sible to the Chief of Naval Staff.
The BNAA is composed of 84 naval air personnel and 43
helicopters. It is not formed into tactical units. The air-
craft carrier Minas Gerais is used jointly by aircraft of the
navy and air force. All helicopters belong to the BNAA,and
all fixed wing aircraft are in the air force inventory. Joint
usage of the Minas Gerais has already improved ASW capability,
but considerable basic and advanced ASW training will be neces-
sary to develop this capability to its full potential.
Enlisted men receive basic training at apprentice seamen's
schools. These schools offer a 10-month program, with courses
in general grammar school subjects, elementary seamanship, and
physical education. The effectiveness of basic training is
seriously limited by the poor education of the recruits and by
lack of equipment and qualified instructors. Enlisted person-
nel may be selected for specialist training after they have
served 5 years in the fleet.
Candidates for commissions in the line, marine corps, and
supply corps pursue a 4-year course at the Naval Academy. The
academy courses are followed by a year of practical training
before commissions are awarded.
US Navy training influence has been strong in the Brazil-
ian Navy. There has been a US Naval Mission in Brazil almost
continuously since 1922, and the Brazilian Navy has relied
heavily on the United States for training and advice. In
addition to the mission, there is a naval communications tech-
nical group and an air utility unit which give training support.
Selected naval personnel are sent to the United States for
specialized training. Various joint exercises have contributed
to the close ties between the two navies.
The navy has approximately 30 days supply of ammunition,
fuel, spare parts, and provisions on hand at all times, and
the fleet can maintain itself at sea cruising at 14-16 knots
for approximately five days. The navy itself has no tankers
but has the ability to refuel at sea; if it refuels from the
carrier and the two cruisers, it can extend the time at sea to
10 days.
The Naval Arsenal at Rio de Janeiro, the navy's major
yard, has an extensive complex of facilities. It has assembled
destroyers from imported parts and has built a number of ships,
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including patrol escorts (PF) and coastal surveying ships
(AGSC). The Naval Arsenal can repair or overhaul any of the
ships in the Brazilian Navy. Naval or commercial drydocks
in Rio de Janeiro and Belem can accommodate any of the naval
ships including the aircraft carrier.
The Corps of Naval Riflemen or marine corps has its own
commander and is operationally subordinate to the Chief of
Naval Staff. The primary missions of the marine corps are to
provide security and defense of naval installations and to
conduct land and amphibious operations essential to the prose-
cution of naval campaigns. The headquarters of the marine
corps is at Rio de Janeiro. The Fleet Marine Force, also based
at Rio de Janeiro, provides a mobile amphibious force in readi-
ness and is the nucleus of a marine division.. Guard units and
security detachments, some of them embarked in the larger ships,
provide a light infantry potential.
Present strength of the marine corps is approximately 400
officers and 9,100 enlisted men. They are moderately well
trained and in a fair state of readiness. They would be capable
of conducting amphibious landings with up to two battalions if
the necessary sealift, air, naval gunfire, and logistic support
were made available.
D. Air Force
The Brazilian Air Force (BAF) is the largest air force
in South America. Despite budgetary limitations and short-
comings in logistics and training, its general capabilities
are greater than those of any other South American air force.
However, it would be ineffective against an attack by a major
air power. The missions of the BAF include air defense, sup-
port of ground forces, internal security, protection of coastal
shipping and the sea approaches to Brazil, the maintenance of
essential air service in areas where private airlines do not
operate, and the provision of civil aviation services of the
type performed in the US by the Federal Aviation Agency and the
Civil Aeronautics Board.
The BAF fighter squadrons, equipped with Meteor F-8 and
T-33 jet aircraft, have demonstrated effectiveness in ground
support exercises. The pilots are proficient and frequently
give excellent demonstrations of precision acrobatics in for-
mation. The Meteor and T-33 pilots have demonstrated high
accuracy in air-to-ground firing with machineguns and rockets
and in low-level bombing with napalm and high-explosive bombs.
Although all fighter squadrons conduct tactical training, the
absence of mobile ground-air communications equipment precludes
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fully effective support of ground forces. Recently organized
special commando flights of armed T-61s, assigned to the com-
manding officers of several airbases, are increasing the air
force's counterinsurgency capabilities. The BAF does not
envision the strategic employment of its bomber squadrons --
they are used mainly for training, reconnaissance, and commu-
nications -- and their aircraft have only a limited bombing
potential.
In air defense, the BAF would be almost completely inef-
fective, since it has no all-weather fighters or early warning/
ground-controlled intercept (EW/GCI) system. Its two air
defense radar direction centers lack the equipment and trained
personnel to become operational. Air defense would be hampered
further by the lack of a coordinated antiaircraft artillery
command, and the scarcity and obsolescense of antiaircraft
weapons. The BAF reconnaissance squadrons have enough aircraft
and combat-ready crews to support the other tactical units but
are limited to visual observation. They can provide effective
reconnaissance for army units. A search and rescue unit, which
provides assistance in civilian disasters, could also support
the ground forces.
BAF capabilities for antisubmarine warfare (ASW) are fair,
but have been steadily improving since joint usage of the air-
craft carrier Minas Gerais became a reality. Capabilities for
antishipping operations, aerial mining, or support of amphibious
operations are slight with no signs of any significant improve-
ment in the near future.
Although the bulk of the air transport fleet is outmoded
and half theC-47's are regularly grounded for maintenance and
lack of parts, the BAF can fulfill its own requirements for air
transport. It can also provide airlift for army paratroop
operations and aerial resupply in the event of an internal
uprising. It has successfully executed drops of from 150 to
300 paratroopers. To improve BAF air transport operations,
the Ministry of Aeronautics purchased six AVRO 748 turboprop
medium transports from the United Kingdom in 1962 and five
C-130's from the United States in 1965.
Under a Mutual Defense Assistance Agreement with the
United States the BAF has received both grant aid and reim-
bursable military assistance. Spare parts, electronic equip-
ment, and technical advice are also provided under the MAP.
The Brazilian Air Force is headed by the Minister of
Aeronautics, usually a senior air force officer. He reports
directly to the president but is subordinate to the Chief of
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the Armed Forces General Staff on matters affecting other
services. He directs the activities of the air force through
the Air General Staff, eight directorates (personnel, train-
ing, health, quartermaster and finance, materiel, engineering,
air routes, and civil aeronautics), the commands (Army Tacti-
cal, Tactical Navy, and Air Transport), which are, with the
six air zones, the operational commands.
Headquarters for each air zone is located at the most
important BAF base in the zone -- Val de Cles, Guararapes,
GaleAo, Cumbica, Gravatai, and Brasilia. All air force tac-
tical units, services, establishments, and activities located
within an air zone are under the control of the air zone com-
mander, a general officer, unless specifically exempted by
the Minister of Aeronautics. Air zone commanders report
directly to the Minister of Aeronautics, but they also deal
with the directorates and the Air General Staff, as appro-
priate. Each commander has considerable latitude in dis-
charging his responsibility for maintaining, training, and
employing the units assigned to his zone.
The BAF has a personnel strength of approximately 28,100
including some 1,250 pilots, over 200 of whom are jet quali-
fied. The aircraft strength is nearly 900, including about
100 jets, many of which are often nonoperational.
Most BAF personnel are volunteers. Officers are pre-
dominantly graduates of military schools, but, a few are from
civilian universities. There are no organized reserve units.
The BAF training system and facilities are good in com-
parison with those of other South American countries, but they
are inadequate for a modern air force. The principal short-
coming is the absence of a program to provide progressive
training in a particular specialty to individuals at different
levels of experience and ability. Inefficient administration
and the low educational level of the average trainee are addi-
tional complicating factors. The US MAP is aimed at improving
the training system and expanding capabilities. Brazilian Air
Force training is supplemented by the advisory support of the
USAF Air Mission in Brazil and by the specialized training
(advanced pilot training and instruction in maintenance and
supply operations) of selected students in USAF schools in the
United States and Panama.
Logistics is the responsibility of the Air General Staff.
In general, the BAF logistic organization is characterized by
poor planning and control. A major task of the USAF Section
of the Joint Brazil-United States Military Commission is
improvement of supply procedures and organization.
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The BAF is almost completely dependent upon foreign sources
for aircraft and related equipment. Most of its aircraft are
imported, principally from the United States; the Meteors and
AVRO 748's came from the United Kingdom. Domestic factories
2596bduce liaison and trainer aircraft.
2. The Police
The Federal Department of Public Safety (DFSP) is directly
subordinate to the Ministry of Justice and carries out its
operations through eight regional offices located in Rio de
Janeiro and other major cities. The principal functions of
the DFSP are:
a. Controlling land and ocean borders and
supervision of maritime, aerial, and border
police.
b. The prevention of crimes against the
properties, works, and interests of the govern-
ment.
c. Providing for protection of the presi-
dent, diplomats, and official foreign visitors.
The DFSP is the most effective government agency employed
against Communist and other subversion. It works in close
cooperation with the National Intelligence Service and the
Intelligence Section of the Army Ministry.
The DFSP operates the National Police Academy, which pro-
vides training for all law enforcement agencies in Brazil.
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Another DFSP department, the National Institute of Criminology,
provides scientific and technical facilities for all police
services. The DFSP's National Institute of Identification
serves as a central repository for all criminal and civil
identification records, which are made available to other
police organizations.
Most normal law enforcement is carried out by the police
forces of the 22 states and the Federal District Security
Forces. Each state maintains military police forces (policia
militar -- military police, not to be confused with the regular
military police in the army) and civil police, both of which
operate on a statewide basis. The civil police can arrest,
commit, and prosecute throughout the state but operate pri-
marily in the capitals, while the military police concentrate
on the hinterlands. Personnel strength ranges from several
hundred in the smaller states to approximately 25,000 military
police and 14,000 civil police in the state of Slo Paulo. In
mid-1967 the total number of state military police was about
105,000 and civil police about 45,000. The military police,
organized along army lines, are frequently headed by an active
duty military officer and constitute a reserve component of
the armed forces in times of emergency. State police organi-
zations usually include a variety of special units such as
highway police, railway police, forest police, and bank police.
Training, equipment, and files are usually inadequate for
both the civil and military police. Communications facilities
range from radio and teletype in the larger cities to telephone
in the smaller but are often poor or nonexistent in rural areas.
Many high-level officials are political appointees, not career
officers, and the civil police, very poorly paid, are open to
bribery.
The public distrusts the police; in some areas citizens
prefer to forego justice rather than request police assistance.
The military police, which is better trained and disciplined
and also assists in educational and sports programs, is more
respected than its civil counterpart.
Censorship of communications media, particularly motion
pictures, is conducted by the Censorship Office of the DFSP.
There is rather strict censorship of theater, cinema, and
television, based on both political and moral standards.
In addition to the normal units each state police force
contains a security organization; in Guanabara and Sao Paulo,
for example, this component is called the Department of Political
and Social Order (DOPE). Although lacking in modern equipment
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and small in size -- the DOPS in Guanabara has approximately
300 members -- these units are usually among the more effec-
tive organizations working against Communists and other extrem-
ist groups. The DOPS also is charged with investigating
political and social crimes, controlling the use of firearms
and explosives, surveillance of aliens, and protecting the
25X6[ransportation system.
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5X6D
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READING LIST
2eX6D CIA. NIS 94, Brazil, "General Survey," Aug 1967. S/NFD.
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5X6D
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S-E-C-R-E-T
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Appendix B
Recommended Films
1. Amazon Awakens. Walt Disney Studios, 1944, 16mm, sound,
color, 33 min. CIA Film J7080.
2. The Amazon Family. International Film Foundation, 1961,
16mm, sound, color, 19 min. CIA Film P7063.
3. The Amazon -- People and Resources of Northern Brazil.
Encyclopedia Britannica Films, 1957, 1 mm, sound, black
& white, 22 min. CIA Film N6271.
4. Brasilia -- David Brinkley's Journal. NBC/TV, 1963, 16mm,
sound, black & white, 29 min. CIA Film 56215.
5. Brazil. NBC/TV, 1962, 16mm, sound, black & white, 16 min.
CIA Film R6499.
6. Brazil. US Army, 1953, 16mm, sound, black & white, 17 min.
CIA Film j6726.
7. Brazil -- The Gathering Millions. National Educational
Television, 1965, l6mm, sound, black & white or color,
60 min. CIA Film V6500.
8. Brazil -- People of the Highlands. Encyclopedia Britannica
Films, 1957, 16mm, sound, color, 19 min. CIA Film K6995.
9. Brazil -- Rude Awakening. CBS/TV, 1961, 16mm, sound, black
& white, 54 min. CIA Film P7001.
10. Brazil, the Takeoff Point -- Changing World. National
Educational Television, 1964, 1 mm, sound, black & white,
59 min. CIA Film V6247.
11. Brazil, the Troubled Land. ABC/TV, 1964, 16mm, sound,
black & white, 27 min.
12. Forty Million Shoes: A Report on Brazil. Canadian Broad-
casting System, 1961, 116mm, sound, black & white, 61 min.
CIA Film R6188.
13. Geography of South America: Brazil. Coronet Films, 1961,
1 mm, sound, color, 14 min. CIA Film P7027.
-357-
S-E-C-R-E-T
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14. Have Patience, Brazil is Big. ABC/TV, 1964, 16mm, sound,
black & white, 34 min. CIA Film T6787-
15. The Head Men. National Film Board of Canada, 1963, 16mm,
sound, black & white, 28 min.
16. The Thin Edge -- Chet Huntley Reporting. NBC/TV, 1962,
3mm, sound, black & white, 33 min. CIA Film 56072.
17. Three Apprentices. National Film Board of Canada, 1963,
lGMm, sound, black & white, 28 min.
AM,
-358-
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NO FOREIGN DISSEM
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