IRON AND MANGANESE DEPOSITS IN UKRAINE

Document Type: 
Collection: 
Document Number (FOIA) /ESDN (CREST): 
CIA-RDP80-00809A000600050325-6
Release Decision: 
RIPPUB
Original Classification: 
C
Document Page Count: 
2
Document Creation Date: 
December 22, 2016
Document Release Date: 
July 25, 2011
Sequence Number: 
325
Case Number: 
Publication Date: 
March 12, 1954
Content Type: 
REPORT
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PDF icon CIA-RDP80-00809A000600050325-6.pdf113.96 KB
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Sanitized Copy Approved for Release 2011/07/27: CIA-RDP80-00809A000600050325-6 .SUBJECT Iron, an" Manganese Deposits in '_rcrsine 'DATE OF D FORNATI0N Y! VII Y.,..I ! ~Il I. 11,.1. 1 ! II. I III NO. OF ENCLS. (LISTED BELOW) THlS IS i'.'JE'JAL DATED !NFORMATiON One of the largest deposits of iron ore in the Ukraine is in the so-called Krivoi Rog region, located in the area of the per part of the Itlgulets River Valley and the tributaries, Zovta and Saksahan. This region is 90 kilometers long and three to ;a kilometers vide. Usually, the einole ore layer is about 10 to -,0 +er chick, but at es reaches 1+5 t 6 o 5 meters and in places as much as 100 to 150 meters. The ore contains from 0.017 to 0.037', of phosphorous ac compared to the finest iron ore with a content of 0,005;',. 7t 1 ;wits are found in metamorphosed Precambrian schirts about 300 tc 350 meters under the surface, and are estimated to be about 1.1, illiccn tons. In addition to these deposits there is an estimated 100 1,illion tons of quartzitec ore in the region with an iron composition of aho;;t. 33%- 2. The southern part of the cc-called Kursk Magnetic Anomaly is located in the northern portion of the t_fl rain. Here are found accumulations of magnetite. The iron deposits a-e located about 200 to 600 meters below the surface. The (mown reserves of ferrsCinous quartzites in the area are estimated to be about 200 billion torso, A very similar magnetic an0Mly was discovered. just befc_?e 20 in western Ukraine near Halych and Gorodok. Future geoloCiai e plurati--n .rill have to be made to determine the extent of these deposits. 3? Iron deposits are found on the Kerch PeninsL.la in an area of about 2,400 square meters. Etraction here ie verv easy because the layers are but four meters or so under the surface. The beds are not as thick as those in the Krivoi Rog region, reaching o thickness of about eight to 12 meters, 71Y wpm b Ia As aw wl,Iiu *a USA of IL LmE gnIm vm%*.,m n[ Iha rt; a[?ealo a Apw.-1. Ioiu.1 Enna It b art a w a-O'- MM,iM as awwwaaw al do wwwj g see, di.*' th Miwne Dassa of -he Olla d CdiaaMa w1 Di-- --- , CIA, Sanitized Copy Approved for Release 2011/07/27: CIA-RDP80-00809A000600050325-6 CL_ASSfillCATtorq CENTRAL INTELLIGENCE AGENCY INFORMATION REPORT Sanitized Copy Approved for Release 2011/07/27: CIA-RDP80-00809A000600050325-6 nor is the percentage value of the ore as high, is brittle and has about one percent of phosphorous present. A small erc nt- age of vanadium is present and is extracted. It has hreent- is about 1.6% of, sulphur and about 0.05% of arsenic, the latter cathat ussingea weakness in iron that makes it worthless for certain products. It is also an expensive process to remove the arsenic from the iron. The iron ore reserves tons. in the Kerch Peninsula area are estimated to be about 2.7 billion 41 Qii tZftiC deposits with a high per e + of deposits and in an(! 5lavgorod The total t1eaticnc the 77.rF5ine one ct the richest iron ore regions in the work, 5? The r ganese in the Ukraine are found in an area about 150 kilhometersp square o ~ateloc d on the. right ba Dnepr Iiver around Nikcpol;(one of the largest in of the lower art the world.) The reserves areestimated to be about 450 million tons, from which 190 million tons of pure manganese can be extracted. The beds average 6,5 feet in thickness and are found at a depth of from 50 to 250 feet under the surface. The ore yields about 35 to 506 of manganese and contains oolitic earthy lenses and nodules of pyrolusite, vad, polianite, manganite and iron oxides. Other deposits are found near 1Q1oshchevatka in the vicinity of Haisyn on the left bank of the Bob River,(estimated at about eight million tons.) 6. Prior to World War II deposits of manganese were found in the Carpathian Mountains near the springs of the White and Black Chereemosh Rivers. These deposits were estimated to be about 10 million tons, however, because of the difficult terrain, the field is not exploited. There are additional deposits located on the north sloops of the CaLL`___._ m .. of the Bila and aus ountains in the basin Iam Rivers in the vicinity of Labynska,(estimnted to be between 34 and 38 million tons. -;2/733?, 4N ic, 32. 4N Sanitized Copy Approved for Release 2011/07/27: CIA-RDP80-00809A000600050325-6