{"pageNumber":"6254","pageRowStart":"156325","pageSize":"25","recordCount":165658,"records":[{"id":5220251,"text":"5220251 - 1954 - The use of fire in quail management","interactions":[],"lastModifiedDate":"2012-02-02T00:14:37","indexId":"5220251","displayToPublicDate":"2010-06-16T12:18:22","publicationYear":"1954","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3140,"text":"Proceedings of the Annual Conference of the Southeastern Association of Game and Fish Commissioners","active":true,"publicationSubtype":{"id":10}},"title":"The use of fire in quail management","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Proceedings of the Annual Conference of the Southeastern Association of Game and Fish Commissioners","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"held New Orleans, November 1-3, 1954","usgsCitation":"Rosene, W., 1954, The use of fire in quail management: Proceedings of the Annual Conference of the Southeastern Association of Game and Fish Commissioners, v. 8, p. 9-11.","productDescription":"9-11","startPage":"9","endPage":"11","numberOfPages":"3","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193722,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4ebe","contributors":{"authors":[{"text":"Rosene, W.","contributorId":67609,"corporation":false,"usgs":true,"family":"Rosene","given":"W.","email":"","affiliations":[],"preferred":false,"id":331549,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70048361,"text":"tei456 - 1954 - Results of core drilling for uranium-bearing lignite, Mendenhall area, Harding County, South Dakota","interactions":[],"lastModifiedDate":"2013-11-22T09:22:35","indexId":"tei456","displayToPublicDate":"2009-02-10T15:01:00","publicationYear":"1954","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"456","title":"Results of core drilling for uranium-bearing lignite, Mendenhall area, Harding County, South Dakota","docAbstract":"Core drilling for data on uranium-bearing lignite in the Mendenhall area, Harding County, S. Dak. , was conducted by the U. S. Bureau of Mines during the period October 1952 to July 1953. Forty-two core holes totaling 9, 683 feet drilled in an area of about six square miles indicate a reserve of about 127/000,000 tons of lignite of which about 49,000,000 tons contain an average of 0.005 percent uranium or more. The Mendenhall area is near the center of the Slim Buttes, which are about 30 miles long from north to south. The uranium-bearing lignite averages, 5. 4 feet in thickness and occurs in the Ludlow member of the Fort Union formation of Paleocene age. Fuel analyses of about 130 samples indicate that the lignite contains about 15 percent ash, 36.7 percent moisture, 24r percent fixed carbon, 23.9 percent volatile matter, and 1.5 percent sulfur and has heating values of about 5,800 btu (as received). Uranium analyses of about 700 samples of lignite core indicate that about 2, 790 tons of uranium are present in the Mendenhall area. Inferred uranium reserves of 2,335 and .1. 050 tons are indicated by grade cutoffs of 0. 005 and 0. 01 percent uranium in the lignites, and 2, 065 and l s 35Stons are indicated by grade cutoffs of 0.03 and 0.05 percent uranium in the lignite ash. The above grade cutoffs have been incorporated on maps showing areal distribution:\nand thickness of mineralized beds.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei456","collaboration":"Prepared in cooperation with the U.S. Atomic Energy Commission","usgsCitation":"Gill, J.R., 1954, Results of core drilling for uranium-bearing lignite, Mendenhall area, Harding County, South Dakota: U.S. Geological Survey Trace Elements Investigations 456, Report: 90 p.; Plate 3: 17.87 inches x 10.60 inches; Plate 4: 23.47 inches x 21.84 inches; Plate 5: 18.13 inches x 27.54 inches; Plate 6: 19.59 inches x 26.01 inches; Plate 7: 16.60 inches x 24.97 inches; Plate 8: 17.12 inches x 21.07 inches, https://doi.org/10.3133/tei456.","productDescription":"Report: 90 p.; Plate 3: 17.87 inches x 10.60 inches; Plate 4: 23.47 inches x 21.84 inches; Plate 5: 18.13 inches x 27.54 inches; Plate 6: 19.59 inches x 26.01 inches; Plate 7: 16.60 inches x 24.97 inches; Plate 8: 17.12 inches x 21.07 inches","costCenters":[],"links":[{"id":278014,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/456/report-thumb.jpg"},{"id":279527,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/456/plate-3.pdf"},{"id":279528,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/456/plate-4.pdf"},{"id":279526,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/456/report.pdf"},{"id":279529,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/456/plate-5.pdf"},{"id":279530,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/456/plate-6.pdf"},{"id":279531,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/456/plate-7.pdf"},{"id":279532,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/456/plate-8.pdf"}],"country":"United States","state":"South Dakota","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.238635,45.387284 ], [ -103.238635,45.47112 ], [ -103.127169,45.47112 ], [ -103.127169,45.387284 ], [ -103.238635,45.387284 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"524162e8e4b0ec672f073b03","contributors":{"authors":[{"text":"Gill, James R.","contributorId":44904,"corporation":false,"usgs":true,"family":"Gill","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":484419,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70048092,"text":"tei290 - 1954 - Exploration for uranium deposits in the Atkinson Mesa area, Montrose County, Colorado","interactions":[],"lastModifiedDate":"2014-03-25T08:42:48","indexId":"tei290","displayToPublicDate":"2009-01-14T09:40:00","publicationYear":"1954","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"290","title":"Exploration for uranium deposits in the Atkinson Mesa area, Montrose County, Colorado","docAbstract":"The U.S. Geological Survey explored the Atkinson Mesa area for uranium- and vanadium-bearing deposits from July 2, 1951, to June 18, 1953, with 397 diamond-drill holes that totaled 261,251 feet. Sedimentary rocks of Mesozoic age are exposed in the Atkinson Mesa area. They are: the Brushy Basin member of the Upper Jurassic Morrison formation, the Lower Cretaceous Burro Canyon formation, and the Upper and Lower Cretaceous Dakota sandstone. All of the large uranium-vanadium deposits discovered by Geological Survey drilling are in a series of sandstone lenses in the upper part of the Salt Wash member of the Jurassic Morrison formation. The deposits are mainly tabular and blanket-like, but some elongate pod-shaped masses, locally called \"rolls\" may be present. The mineralized material consists of sandstone impregnated with a uranium mineral which is probably coffinite, spme carnotite, and vanadium minerals, thought to be mainly corvusite and montroseite. In addition,, some mudstone and carbonaceous material is similarly impregnated. Near masses of mineralized material the sandstone is light gray or light brown, is generally over 40 feet thick, and usually contains some carbonaceous material and abundant disseminated pyrite or limonite stain. Similarly, the mudstone in contact with the ore-bearing sandstone near bodies of mineralized rock is commonly blue gray, as compared to its dominant red color away from ore deposits. Presence and degree of these features are useful guides in exploring for new deposits.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/tei290","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission.","usgsCitation":"Brew, D.A., 1954, Exploration for uranium deposits in the Atkinson Mesa area, Montrose County, Colorado: U.S. Geological Survey Trace Elements Investigations 290, Report: 11 p.; Plate 2: 43.63 inches x 29.49 inches; Plate 3: 34.41 inches x 29.23 inches, https://doi.org/10.3133/tei290.","productDescription":"Report: 11 p.; Plate 2: 43.63 inches x 29.49 inches; Plate 3: 34.41 inches x 29.23 inches","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":277448,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/290/report-thumb.jpg"},{"id":279897,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0290/figure-2.pdf"},{"id":279898,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0290/figure-3.pdf"},{"id":279896,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/290/report.pdf"}],"country":"United States","state":"Colorado","county":"Montrose County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.060256,38.151752 ], [ -109.060256,38.667801 ], [ -107.498924,38.667801 ], [ -107.498924,38.151752 ], [ -109.060256,38.151752 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd58cfe4b0b290850f8529","contributors":{"authors":[{"text":"Brew, Daniel Allen","contributorId":26616,"corporation":false,"usgs":true,"family":"Brew","given":"Daniel","email":"","middleInitial":"Allen","affiliations":[],"preferred":false,"id":483732,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70048368,"text":"tei467 - 1954 - Uranium-bearing lignite and its relation to the White River and Arikaree formations in northwestern South Dakota and adjacent states","interactions":[],"lastModifiedDate":"2014-04-07T14:53:38","indexId":"tei467","displayToPublicDate":"2009-01-13T09:13:00","publicationYear":"1954","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"467","title":"Uranium-bearing lignite and its relation to the White River and Arikaree formations in northwestern South Dakota and adjacent states","docAbstract":"In northwestern South Dakota and adjacent areas uranium-bearing lignite beds occur at many horizons in the Hell Creek formation of late Cretaceous age and the overlying Ludlow, Tongue River, and Sentinel Butte members of the Fort Union formation of Paleocene age. Uranium analyses of 275 surface and auger samples and about 1,000 core samples show that many of the lignite beds contain 0. 005 to 0. 02 percent uranium with concentrations of 0. 05 to 0.10 percent uranium in the lignite ash. Analytical data indicate that the region contains an aggregate of at least 47,500, 000 tons of lignite with an average grade of slightly more than .0. 008 percent containing 3, 900 tons of uranium. Almost a fifth of the estimated reserves are adapted to strip mining and are in beds averaging about 4 feet in thickness. Uranium concentrations of this magnitude in lignite indicate that these deposits upon the development of proper utilization techniques and processes may be an important future source of uranium. Recent discoveries of ore-grade deposits of autunite-bearing lignite and secondary uranium minerals in carbonaceous sandstone at Cave Hills and Slim Buttes indicate that northwestern South Dakota and adjacent areas may containimportant reserves of uranium-ore. The stratigraphic units containing the uraniferous lignite beds have a combined thickness of about 1, 500 feet and are unconformably overlapped by 300 feet or more of tuffaceous sandstone and bentonitic claystone of the White River and Arikaree formations of Oligocene and Miocene age. The stratigraphically highest lignite beds in the local sequence have the greatest concentration of uranium,, and the uranium content is greatest at the top of thick lignite beds, diminishing progressively downward to a vanishing point in their lower parts. Variations in permeability of the rock overlying the mineralized lignite beds seem to be reflected in the intensity of uranium mineralization. Most of the known uranium-bearing lignite deposits in the region are closely overlain by the White River and Arikaree formations. Field evidence indicates that the uranium in the lignite is independent of the age of the formation in which the lignite occurs and that the uranium has been concentrated by downward and laterally moving ground water from the overlying mildly radioactive, tuffaceous rocks. The White River and Arikaree formations have about 1.2 times more uranium than the average sedimentary rock. The uranium content of spring water from these formations is 30 times as great or greater than that of normal ground water. Field relations suggest that the uranium is of secondary origin and has been introduced subsequent to the accumulation and marked regional warping of the lignite beds and associated rocks. During the transportation of the uranium-bearing volcanic materials from their place of origin to the site of deposition in South Dakota, the uranium is believed to have been held as a finely disseminated constituent in volcanic ash. Subsequent release or displacement of the uranium is thought to have resulted from weathering and chemical breakdown, thus freeing and allowing the transportation of the uranium, probably in ionic form, to the lignite by downward and laterally moving groundwaters 0 Gar bonaceous material in the path of these uranium-bearing waters is believed to have acted as a receptor that extracted the uranium as a result of an ion exchange mechanism or by the formation of organo-metallic compounds Geologic factors that seem most significant in controlling the distribution and concentration of uranium in Dakota lignites are as follows: 1) stratlgraphic proximity of the lignite to the base of the White River formation; 2) permeability of the rocks overlying the lignites; 3) adsorptive properties and porosities of the lignitic constituents; 4) present and past position of the groundwater table; and 5) the amount of uranium in\nthe original White River and Arikaree sediments. Individual maps showing the extent, thickness, and variations in mineral content of the important deposits in the Table Mountain, Cave Hills, Slim Buttes, Lodgepole, and Medicine Pole areas are included. Conditions controlling the concentration of uranium are described and their application as guides to finding additional reserves by the presently held concepts are explained and illustrated.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei467","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Denson, N., Bachman, G., and Zeller, H.D., 1954, Uranium-bearing lignite and its relation to the White River and Arikaree formations in northwestern South Dakota and adjacent states: U.S. Geological Survey Trace Elements Investigations 467, Report: 97 p., https://doi.org/10.3133/tei467.","productDescription":"Report: 97 p.","numberOfPages":"100","costCenters":[],"links":[{"id":284152,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei467.jpg"},{"id":285870,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0467/report.pdf"}],"country":"United States","state":"Montana;North Dakota;South Dakota;Wyoming","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.7324,44.0718 ], [ -105.7324,46.4227 ], [ -102.7881,46.4227 ], [ -102.7881,44.0718 ], [ -105.7324,44.0718 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5242b467e4b096ee6246420e","contributors":{"authors":[{"text":"Denson, N.M.","contributorId":79458,"corporation":false,"usgs":true,"family":"Denson","given":"N.M.","affiliations":[],"preferred":false,"id":484449,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bachman, G.O.","contributorId":55858,"corporation":false,"usgs":true,"family":"Bachman","given":"G.O.","email":"","affiliations":[],"preferred":false,"id":484448,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zeller, H. D.","contributorId":104872,"corporation":false,"usgs":true,"family":"Zeller","given":"H.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":484450,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":78620,"text":"tem709 - 1954 - Age Determinations of the San Gabriel anorthosite Massif","interactions":[],"lastModifiedDate":"2012-02-02T00:14:23","indexId":"tem709","displayToPublicDate":"2006-08-27T00:00:00","publicationYear":"1954","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"709","title":"Age Determinations of the San Gabriel anorthosite Massif","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/tem709","usgsCitation":"Neuerburg, G.J., and Gottfried, D., 1954, Age Determinations of the San Gabriel anorthosite Massif: U.S. Geological Survey Trace Elements Memorandum 709, 4 p. ; 27 cm., https://doi.org/10.3133/tem709.","productDescription":"4 p. ; 27 cm.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":101674,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0709/report.pdf","size":"369","linkFileType":{"id":1,"text":"pdf"}},{"id":195563,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0709/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db6897fc","contributors":{"authors":[{"text":"Neuerburg, George Joseph","contributorId":107702,"corporation":false,"usgs":true,"family":"Neuerburg","given":"George","email":"","middleInitial":"Joseph","affiliations":[],"preferred":false,"id":288989,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gottfried, David","contributorId":82295,"corporation":false,"usgs":true,"family":"Gottfried","given":"David","email":"","affiliations":[],"preferred":false,"id":288988,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":78586,"text":"tem784 - 1954 - Reconnaissance for Uranium in the Indiana Coal Field","interactions":[],"lastModifiedDate":"2012-02-02T00:14:00","indexId":"tem784","displayToPublicDate":"2006-08-27T00:00:00","publicationYear":"1954","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"784","title":"Reconnaissance for Uranium in the Indiana Coal Field","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/tem784","collaboration":"Prepared jointly by the Bureau of Mines and Geological Survey for the U.S. Atomic Energy Commission","usgsCitation":"Snider, J.L., 1954, Reconnaissance for Uranium in the Indiana Coal Field: U.S. Geological Survey Trace Elements Memorandum 784, iv, 26 p. : ill., map ; 27 cm., https://doi.org/10.3133/tem784.","productDescription":"iv, 26 p. : ill., map ; 27 cm.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":101672,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0784/report.pdf","size":"1438","linkFileType":{"id":1,"text":"pdf"}},{"id":193155,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0784/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a74e4b07f02db6440d4","contributors":{"authors":[{"text":"Snider, John L.","contributorId":23236,"corporation":false,"usgs":true,"family":"Snider","given":"John","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":288969,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":71347,"text":"tei297 - 1954 - Uranium deposits in Fall River County, South Dakota","interactions":[],"lastModifiedDate":"2014-05-27T12:52:36","indexId":"tei297","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1954","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"297","title":"Uranium deposits in Fall River County, South Dakota","docAbstract":"

In 1951 uranium deposits contained carnotite were discovered in the southern Black Hills near Edgemont, Fall River County, S. Dak. Numerous carnotite deposits have since been found in sandstones in the Inyan Kara group of early Cretaceous age, and uranium-bearing material has been discovered in the Pennsylvania Minnelusa sandstone of Pennsylvanian age and the Deadwood formation of Cambrian age in the southern Black Hills. Ore has been produced only from the Inyan Kara group, mostly within an area of about 30 square miles along the southwest flank of the Black Hills uplift between Dewey and Hot Springs in Custer and Fall River Counties. In addition, occurrences of uranium in other parts of the Black Hills and the surrounding area are known or reported from sedimentary, igneous, and metamorphic rocks of pre-Cambrian to Tertiary age.

\n
\n

The upper and lowermost formations of the Inyan Kara group - the Fall River and Lakota sandstones - contain the productive uranium deposits. These terrestrial formations are composed predominantly of massive sandstone lenses within units of thinly bedded sandstone and mudstone, but locally these formations contain abundant mudstone and thinly bedded sandstone. Massive sandstone lenses in the Lakota sandstone commonly overlap and truncate underlying lenses. The lenses are separated by thin units of thinly bedded sandstone and mudstone. Iron stain, carbonaceous material, thin seams of gypsum, ripple marks, concretions, and fossil roots are common in the mudstone and thinly bedded portions of these formations.

\n
\n

Some high angle normal faults of small displacement are found in the area containing the largest number of uranium occurrences in the Inyan Kara group. Although no ore deposits seen were cut by faults, high-angle fractures parallel and at right angles to the faults contain carnotite for short distances.

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\n

The productive uranium deposits are most common where the Fall River and Lakota sandstones locally contain a large proportion of mudstone and thinly bedded sandstone. Other deposits are in the massive sandstone lenses of the Lakota sandstone and in the thin units between the lenses.

\n
\n

Although carnotite is the most conspicuous and important mineral in most deposits, corvusite is an important constituent of some deposits. Other uranium minerals in the deposits are tyuyamunite, rauvite, and autunite. Ore produced in 1952 from the Fall River and Lakota sandstones contained about 0.2 percent U3O8 and 0.6 percent V2O5. In general, deposits in the Fall River and Lakota sandstones contain about the same percentage of U3O8, but the deposits in the Fall River sandstone appear to have a higher percentage of vanadium. The grade of individual deposits, however, is highly variable. Most deposits are small, but a few have yielded as much as a thousand tons of ore.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei297","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Bell, H., and Bales, W., 1954, Uranium deposits in Fall River County, South Dakota: U.S. Geological Survey Trace Elements Investigations 297, Report: 47 p.; 7 Plates: 24.29 x 26.65 inches and smaller, https://doi.org/10.3133/tei297.","productDescription":"Report: 47 p.; 7 Plates: 24.29 x 26.65 inches and smaller","numberOfPages":"48","costCenters":[],"links":[{"id":186497,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei297.jpg"},{"id":284538,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0297/figure-04.pdf"},{"id":284539,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0297/figure-05.pdf"},{"id":284540,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0297/figure-10.pdf"},{"id":284541,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0297/figure-11.pdf"},{"id":284536,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0297/figure-02.pdf"},{"id":284537,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0297/figure-03.pdf"},{"id":284542,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0297/figure-12.pdf"},{"id":284543,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0297/report.pdf"}],"country":"United States","state":"South Dakota","county":"Fall River County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104.0,43.25 ], [ -104.0,43.5 ], [ -103.5,43.5 ], [ -103.5,43.25 ], [ -104.0,43.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db6055f0","contributors":{"authors":[{"text":"Bell, Henry III","contributorId":37710,"corporation":false,"usgs":true,"family":"Bell","given":"Henry","suffix":"III","email":"","affiliations":[],"preferred":false,"id":284026,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bales, W.E.","contributorId":101311,"corporation":false,"usgs":true,"family":"Bales","given":"W.E.","email":"","affiliations":[],"preferred":false,"id":284027,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":71941,"text":"tem503 - 1954 - Preliminary Summary of Uranium Occurrences in Carbon County, Pennsylvania","interactions":[],"lastModifiedDate":"2012-02-02T00:14:04","indexId":"tem503","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1954","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"503","title":"Preliminary Summary of Uranium Occurrences in Carbon County, Pennsylvania","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/tem503","usgsCitation":"Klemic, H., and Baker, R.C., 1954, Preliminary Summary of Uranium Occurrences in Carbon County, Pennsylvania: U.S. Geological Survey Trace Elements Memorandum 503, 22 leaves : ill., maps ; 27 cm.; Maps folded in pocket, https://doi.org/10.3133/tem503.","productDescription":"22 leaves : ill., maps ; 27 cm.; Maps folded in pocket","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":101636,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0503/report.pdf","size":"982","linkFileType":{"id":1,"text":"pdf"}},{"id":101637,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0503/plate-1.pdf","size":"394","linkFileType":{"id":1,"text":"pdf"}},{"id":101638,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0503/plate-2.pdf","size":"169","linkFileType":{"id":1,"text":"pdf"}},{"id":192576,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0503/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e433","contributors":{"authors":[{"text":"Klemic, Harry","contributorId":49767,"corporation":false,"usgs":true,"family":"Klemic","given":"Harry","email":"","affiliations":[],"preferred":false,"id":284911,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baker, Roger Crane","contributorId":75131,"corporation":false,"usgs":true,"family":"Baker","given":"Roger","email":"","middleInitial":"Crane","affiliations":[],"preferred":false,"id":284912,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":71962,"text":"tei440 - 1954 - Geologic investigations of radioactive deposits : Semiannual progress report, December 1, 1953 to May 31, 1954","interactions":[],"lastModifiedDate":"2012-02-02T00:14:02","indexId":"tei440","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1954","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"440","title":"Geologic investigations of radioactive deposits : Semiannual progress report, December 1, 1953 to May 31, 1954","language":"ENGLISH","doi":"10.3133/tei440","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1954, Geologic investigations of radioactive deposits : Semiannual progress report, December 1, 1953 to May 31, 1954: U.S. Geological Survey Trace Elements Investigations 440, 247 p., 45 fig., https://doi.org/10.3133/tei440.","productDescription":"247 p., 45 fig.","costCenters":[],"links":[{"id":193266,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/440/report-thumb.jpg"},{"id":91051,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/440/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4fd4","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":534731,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":71966,"text":"tei473 - 1954 - Lithium resources of North America","interactions":[],"lastModifiedDate":"2012-02-02T00:14:02","indexId":"tei473","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1954","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"473","title":"Lithium resources of North America","language":"ENGLISH","doi":"10.3133/tei473","usgsCitation":"Norton, J., and Schlegel, D.M., 1954, Lithium resources of North America: U.S. Geological Survey Trace Elements Investigations 473, 38 p., 1 fig., https://doi.org/10.3133/tei473.","productDescription":"38 p., 1 fig.","costCenters":[],"links":[{"id":193270,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/473/report-thumb.jpg"},{"id":91057,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/473/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4e04","contributors":{"authors":[{"text":"Norton, James J.","contributorId":6127,"corporation":false,"usgs":true,"family":"Norton","given":"James J.","affiliations":[],"preferred":false,"id":284929,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schlegel, Dorothy McKenney","contributorId":31847,"corporation":false,"usgs":true,"family":"Schlegel","given":"Dorothy","email":"","middleInitial":"McKenney","affiliations":[],"preferred":false,"id":284930,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":71474,"text":"tei444 - 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1954 - Zoning of the Bitter Creek vanadium-uranium deposit, Montrose County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:13:44","indexId":"tei443","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1954","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"443","title":"Zoning of the Bitter Creek vanadium-uranium deposit, Montrose County, Colorado","language":"ENGLISH","doi":"10.3133/tei443","usgsCitation":"Heyl, A.V., 1954, Zoning of the Bitter Creek vanadium-uranium deposit, Montrose County, Colorado: U.S. Geological Survey Trace Elements Investigations 443, 27 p., 4 fig., https://doi.org/10.3133/tei443.","productDescription":"27 p., 4 fig.","costCenters":[],"links":[{"id":185826,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/443/report-thumb.jpg"},{"id":90745,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/443/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d5e4b07f02db5ddbf2","contributors":{"authors":[{"text":"Heyl, Allen Van","contributorId":91078,"corporation":false,"usgs":true,"family":"Heyl","given":"Allen","email":"","middleInitial":"Van","affiliations":[],"preferred":false,"id":284238,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":71471,"text":"tei439 - 1954 - Montroseite and paramontroseite","interactions":[],"lastModifiedDate":"2012-02-02T00:13:44","indexId":"tei439","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1954","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"439","title":"Montroseite and paramontroseite","language":"ENGLISH","doi":"10.3133/tei439","usgsCitation":"Evans, H.T., and Mrose, M.E., 1954, Montroseite and paramontroseite: U.S. Geological Survey Trace Elements Investigations 439, 27 p., 4 fig., https://doi.org/10.3133/tei439.","productDescription":"27 p., 4 fig.","costCenters":[],"links":[{"id":185825,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/439/report-thumb.jpg"},{"id":90744,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/439/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a69e4b07f02db63c077","contributors":{"authors":[{"text":"Evans, Howard Tasker Jr.","contributorId":81992,"corporation":false,"usgs":true,"family":"Evans","given":"Howard","suffix":"Jr.","email":"","middleInitial":"Tasker","affiliations":[],"preferred":false,"id":284234,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mrose, Mary E.","contributorId":84750,"corporation":false,"usgs":true,"family":"Mrose","given":"Mary","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":284235,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":71459,"text":"tei425 - 1954 - The stratigraphic and structural controls of the uranium deposits on Long Mountain, Fall River County, South Dakota","interactions":[],"lastModifiedDate":"2015-10-20T13:57:22","indexId":"tei425","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1954","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"425","title":"The stratigraphic and structural controls of the uranium deposits on Long Mountain, Fall River County, South Dakota","docAbstract":"

Numerous occurrences of uranium have been found in the Long Mountain area, Fall River County, S. Dak. Correlation diagrams prepared from drill, cores obtained from the U.S. Atomic Energy Commission indicate that the uranium is most abundant in two sandstone units, separated by mudstone in the Lakota sandstone of Early Cretaceous age. The lower uraniferous unit is composed of thick beds of very fine- to fine-grained sandstone with a few interfingering lentils of mudstone. The upper uraniferous unit is composed of interfingering beds of very fine-, fine-, and coarse-grained sandstone and mudstone.

\n

The uranium deposits on Long Mountain and in the area to the west are most numerous in a northeast-trending zone about a mile wide between two normal faults. The deposits between these faults are in two groups of different trend; the northern group has been incompletely explored.

\n

The sedimentary structures of the upper and lower mineralized sandstone between the faults have controlled the deposition of uranium and vanadium.

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