The U.S. Geological Survey explored Outlaw Mesa for carnotite deposits from 1949 through 1951 with 1,302 diamond-drill holes that totaled 222,150 feet.
\nTotal production from Outlaw Mesa from 1914 through 1951 was about 30,000 short tons of carnotite ore, having an estimated grade of about 0.40 percent U3O8 and 1.7 percent V205.
\nThe known carnotite deposits are in a number of sandstone lenses in the upper part of the Salt Wash sandstone member of the Jurassic Morrison formation.
\nThe deposits are mainly impregnations of sandstone by carnotite and vanadium-bearing clay minerals. Commonly, the deposits are irregular tabular layers or pod-like or crescentic masses (\"rolls\") connected by thin layers of mineralized rock. The deposits and rolls have a dominant northeasterly trend.
\nUseful criteria for recognizing-sandstone that might contain mineralized rock are: (1) thick, light-brown sandstone, (2) gray mudstone at the base of and in this sandstone, and (3) abundant carbonaceous material.
\nThe indicated and inferred reserves of carnotite-bearing material, and the pounds of contained U308 and V205 are summarized in table 1. Potential reserves, whose existence is based on geologic evidence alone, are estimated to total about 80,000 short tones, averaging about 0.35 percent U308 and 1.5percent V205.
\nNo further exploration by the Geological Survey is planned; however, additional drilling by private operators is recommended, particularly in ground underlain by mineralized rock.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/tei163","collaboration":"Work done on behalf of the Division of Raw Materials, U.S. Atomic Energy Commission.","usgsCitation":"Brasher, G., 1952, Carnotite resources of Outlaw Mesa, Mesa County, Colorado: U.S. Geological Survey Trace Elements Investigations 163, Report: 117 p.; 6 Plates: 36.17 x 42.49 inches or smaller; Table, https://doi.org/10.3133/tei163.","productDescription":"Report: 117 p.; 6 Plates: 36.17 x 42.49 inches or smaller; Table","numberOfPages":"118","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":289802,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/TEI163.jpg"},{"id":310931,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/163/plate-4.pdf","text":"Plate 4","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 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About 200,000 short tons of carnotite ore containing an estimated 0.45 percent U3O8 and 2.1 percent V2O5 has been mined from the mesa. This production represents about one-fifth of the carnotite ore mined from the Colorado Plateau.
\nAll the principal deposits on the mesa are in the main ore-bearing sandstone which is in the top part of the Salt Wash sandstone member of the Jurassic Morrison formation. The deposits are in tabular masses of uneven thickness lying more or less parallel to the enclosing strata. The ore consists mainly of sandstone impregnated with carnotite and vanadiferous clay minerals. The sandstone near the deposits is generally over 30 feet in thickness, contains noticeable quantities of carbon, and vivid patches of limonite (?) stain. Also near ore deposits, the mudstone in contact with the sandstone is altered from red to gray or green through a thickness of 3 or 4 feet. Certain linear features of the ore bodies and of favorable parts of the main ore-bearing sandstone offer clues by their orientation to extensions of known ore bodies and of favorable ground. These features on Club Mesa trend mostly east to northeast.
\nBetween March 6, 1948, and January 22, 1952, the U.S. Geological Survey drilled 651 holes for a total of 167,495 feet. As a result of this drilling, 18 deposits were discovered and partly outlined. These range in size from 200 to 55,000 short tons of indicated ore reserves and are in layers 1 foot or more thick containing 0.10 percent or more U3O8 or 1.0 percent or more V2O5. About 85 percent of this ore is in public land; the remainder is in claims owned by the United States Vanadium Co.
\nReserves in deposits known from drill holes or exposures are classed as indicated or inferred, and those in deposits that are predicted solely on geologic evidence are classed as potential. The tons of indicated and inferred reserves and the pounds of contained U3O8 and V2O5 are summarized in table 1. These reserves are subdivided also by thickness and grade cutoffs. At the higher grade cutoff, reserve figures express approximately the tonnage and grade of material that might actually be mined from these deposits under 1951 conditions. Indicated and inferred reserves of this type total 198,000 short tons, averaging 0.35 percent U3O8 and 1.8 percent V2O5, and contain 1,1,372,000 pounds of U3O8 and 7,260,000 pounds of V2O5. These reserves are based on Geological Survey drilling. Potential reserves are predicted to total about 40,000 short tons, averaging about 0.35 percent U3O8 and 1.9 percent V2O5.
\nNo additional exploration on Club Mesa is planned by the Geological Survey, but exploration by private companies is recommended.
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