{"pageNumber":"7029","pageRowStart":"175700","pageSize":"25","recordCount":184617,"records":[{"id":71438,"text":"tei404 - 1953 - Radioactivity of some coal and shale of Pennsylvanian age in Ohio","interactions":[],"lastModifiedDate":"2014-03-25T08:54:59","indexId":"tei404","displayToPublicDate":"1953-03-06T10:31:00","publicationYear":"1953","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":"404","title":"Radioactivity of some coal and shale of Pennsylvanian age in Ohio","docAbstract":"Channel samples of the commercially important coal beds and associated rocks in the Pottsville, Allegheny, and Monogahela series of the Pennsylvanian system were collected in eastern Ohio. Equivalent uranium content of 0.001 percent or more was determined in the laboratory for five samples. The uranium content of the coal is less than the equivalent uranium content indicated by radioactivity measurements. None of the samples collected contain recoverable quantities of uranium in the ash.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/tei404","collaboration":"Prepared by the Geological Survey for the United States Atomic Energy Commission","usgsCitation":"Snider, J.L., 1953, Radioactivity of some coal and shale of Pennsylvanian age in Ohio: U.S. Geological Survey Trace Elements Investigations 404, 22 p., https://doi.org/10.3133/tei404.","productDescription":"22 p.","costCenters":[],"links":[{"id":283408,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei404.png"},{"id":284567,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0404/report.pdf"}],"country":"United States","state":"Ohio","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -83.0,39.0 ], [ -83.0,41.0 ], [ -79.0,41.0 ], [ -79.0,39.0 ], [ -83.0,39.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd6f04e4b0b29085106267","contributors":{"authors":[{"text":"Snider, John L.","contributorId":23236,"corporation":false,"usgs":true,"family":"Snider","given":"John","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":284184,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70222249,"text":"70222249 - 1953 - Stratigraphy and structure of part of Big Bend anticline, Alaska","interactions":[],"lastModifiedDate":"2022-06-01T21:06:21.026401","indexId":"70222249","displayToPublicDate":"1953-03-01T14:24:10","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":5963,"text":"Geological Investigations, Naval Petroleum Reserve No. 4, Alaska","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"43","subseriesTitle":"Preliminary Report","title":"Stratigraphy and structure of part of Big Bend anticline, Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70222249","usgsCitation":"Detterman, R.L., and Bickel, R., 1953, Stratigraphy and structure of part of Big Bend anticline, Alaska: Geological Investigations, Naval Petroleum Reserve No. 4, Alaska 43, Report: 4 p.; 1 Plate: 69.11 x 29.02 inches, https://doi.org/10.3133/70222249.","productDescription":"Report: 4 p.; 1 Plate: 69.11 x 29.02 inches","costCenters":[],"links":[{"id":401611,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70222249/plate1.pdf","text":"Plate 1"},{"id":401610,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70222249/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":387357,"rank":1,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74592.htm","linkFileType":{"id":5,"text":"html"}},{"id":396961,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70222249/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Big Bend anticline","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -152,\n              69.05\n            ],\n            [\n              -151.1667,\n              69.05\n            ],\n            [\n              -151.1667,\n              69.1628\n            ],\n            [\n              -152,\n              69.1628\n            ],\n            [\n              -152,\n              69.05\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Detterman, Robert L.","contributorId":71526,"corporation":false,"usgs":true,"family":"Detterman","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":837689,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bickel, Robert S.","contributorId":14042,"corporation":false,"usgs":true,"family":"Bickel","given":"Robert S.","affiliations":[],"preferred":false,"id":837690,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70221524,"text":"70221524 - 1953 - Nonradiogenic isotopes in geology: A review","interactions":[],"lastModifiedDate":"2021-06-21T17:51:04.954027","indexId":"70221524","displayToPublicDate":"1953-03-01T12:47:12","publicationYear":"1953","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Nonradiogenic isotopes in geology: A review","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1953)64[301:NIIGAR]2.0.CO;2","usgsCitation":"Ingerson, E., 1953, Nonradiogenic isotopes in geology: A review: Geological Society of America Bulletin, v. 64, no. 3, p. 301-374, https://doi.org/10.1130/0016-7606(1953)64[301:NIIGAR]2.0.CO;2.","productDescription":"74 p.","startPage":"301","endPage":"374","costCenters":[],"links":[{"id":386619,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"64","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Ingerson, E.","contributorId":48305,"corporation":false,"usgs":true,"family":"Ingerson","given":"E.","email":"","affiliations":[],"preferred":false,"id":817932,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221519,"text":"70221519 - 1953 - Pumping from wells on the floor of the Sevier Desert, Utah","interactions":[],"lastModifiedDate":"2021-06-21T17:12:34.015216","indexId":"70221519","displayToPublicDate":"1953-02-01T12:05:46","publicationYear":"1953","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Pumping from wells on the floor of the Sevier Desert, Utah","docAbstract":"<p><span>Data collected at the Topaz Relocation Center provide an excellent record of the development and subsequent disappearance of a cone of depression caused by&nbsp;</span>pumping<span>. This Center occupied temporarily an area of natural ground‐water discharge on the&nbsp;</span>floor<span>&nbsp;of the&nbsp;</span>Sevier<span>&nbsp;</span>Desert<span>&nbsp;in west‐central&nbsp;</span>Utah<span>. Water for a population of 6500 was pumped from artesian&nbsp;</span>wells<span>&nbsp;which tapped aquifers of sand. Overlying these sand beds are lake‐bed sediments too impermeable to yield water to&nbsp;</span>wells<span>, but apparently permeable enough to permit slow upward movement of water from the artesian aquifers. The water table is near the surface, and there is natural discharge by evapotranspiration, accumulation of “alkali” in the soil, and a need for drainage of irrigated lands. The&nbsp;</span>wells<span>&nbsp;were abandoned when the Relocation Center was closed, apparently because these handicaps were so great that the ground water could not be used profitably for irrigation.&nbsp;</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR034i001p00074","usgsCitation":"Nelson, W., and Thomas, H., 1953, Pumping from wells on the floor of the Sevier Desert, Utah: Eos, Transactions, American Geophysical Union, v. 34, no. 1, p. 74-84, https://doi.org/10.1029/TR034i001p00074.","productDescription":"11 p.","startPage":"74","endPage":"84","costCenters":[],"links":[{"id":386614,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Utah","otherGeospatial":"Sevier Desert","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.0380859375,\n              37.79676317682161\n            ],\n            [\n              -112.1044921875,\n              37.79676317682161\n            ],\n            [\n              -112.1044921875,\n              40.463666324587685\n            ],\n            [\n              -114.0380859375,\n              40.463666324587685\n            ],\n            [\n              -114.0380859375,\n              37.79676317682161\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"34","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Nelson, W.B.","contributorId":30282,"corporation":false,"usgs":true,"family":"Nelson","given":"W.B.","email":"","affiliations":[],"preferred":false,"id":817921,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thomas, H.E.","contributorId":243568,"corporation":false,"usgs":false,"family":"Thomas","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":817922,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":71942,"text":"tem507 - 1953 - Wavellite Spherulites in the Bone Valley Formation of Central Florida","interactions":[],"lastModifiedDate":"2014-07-16T11:57:44","indexId":"tem507","displayToPublicDate":"1953-02-01T11:55:00","publicationYear":"1953","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":"507","title":"Wavellite Spherulites in the Bone Valley Formation of Central Florida","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior, Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/tem507","collaboration":"Performed for the Division of Raw Materials, U.S. Atomic Energy Commission.","usgsCitation":"Bergendahl, M.H., 1953, Wavellite Spherulites in the Bone Valley Formation of Central Florida: U.S. Geological Survey Trace Elements Memorandum 507, 14 p., https://doi.org/10.3133/tem507.","productDescription":"14 p.","numberOfPages":"14","costCenters":[],"links":[{"id":290278,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Florida","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87.6349,24.5211 ], [ -87.6349,31.001 ], [ -80.0311,31.001 ], [ -80.0311,24.5211 ], [ -87.6349,24.5211 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c79f57e4b01948416424ca","contributors":{"authors":[{"text":"Bergendahl, Maximilian Hilmar","contributorId":21229,"corporation":false,"usgs":true,"family":"Bergendahl","given":"Maximilian","email":"","middleInitial":"Hilmar","affiliations":[],"preferred":false,"id":284913,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71936,"text":"tem536 - 1953 - Preliminary report on geologic investigations in Monument Valley area, Arizona, 1952","interactions":[],"lastModifiedDate":"2014-07-16T11:28:43","indexId":"tem536","displayToPublicDate":"1953-02-01T11:26:28","publicationYear":"1953","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":"536","title":"Preliminary report on geologic investigations in Monument Valley area, Arizona, 1952","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of Interior, Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/tem536","usgsCitation":"Witkind, I.J., Thaden, R., and Lough, C., 1953, Preliminary report on geologic investigations in Monument Valley area, Arizona, 1952: U.S. Geological Survey Trace Elements Memorandum 536, 8 p., https://doi.org/10.3133/tem536.","productDescription":"8 p.","numberOfPages":"8","costCenters":[],"links":[{"id":290271,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Arizona","otherGeospatial":"Monument Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.057591,36.885959 ], [ -110.057591,36.998971 ], [ -109.603672,36.998971 ], [ -109.603672,36.885959 ], [ -110.057591,36.885959 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c79f10e4b0194841642493","contributors":{"authors":[{"text":"Witkind, Irving Jerome","contributorId":87517,"corporation":false,"usgs":true,"family":"Witkind","given":"Irving","email":"","middleInitial":"Jerome","affiliations":[],"preferred":false,"id":284907,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thaden, R.E.","contributorId":12098,"corporation":false,"usgs":true,"family":"Thaden","given":"R.E.","affiliations":[],"preferred":false,"id":284905,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lough, C.F.","contributorId":67014,"corporation":false,"usgs":true,"family":"Lough","given":"C.F.","email":"","affiliations":[],"preferred":false,"id":284906,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70210474,"text":"70210474 - 1953 - Regional interpretation of the geology of the Kongakut - Firth Rivers area, Alaska","interactions":[],"lastModifiedDate":"2025-01-27T14:49:11.008506","indexId":"70210474","displayToPublicDate":"1953-01-01T17:01:50","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":5963,"text":"Geological Investigations, Naval Petroleum Reserve No. 4, Alaska","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"43","subseriesTitle":"Special Report","title":"Regional interpretation of the geology of the Kongakut - Firth Rivers area, Alaska","docAbstract":"<p>In 1952 the National Park Service became interested in setting aside a large wilderness area in northeastern Alaska. The area is approximately 7,000 square miles in size, with boundaries as follows: beginning at Camden Bay south along the Katakturuk River to lat. 68° N.; then east to long. 144° 33' W.; south to lat. 68° N.; then east to the Canadian Boundary. The two river areas which the Park Service is most interested in examining for ecology, botany, archaeology, and geology are the upper Firth and Kongakut Rivers.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70210474","usgsCitation":"Mangus, M.D., 1953, Regional interpretation of the geology of the Kongakut - Firth Rivers area, Alaska: Geological Investigations, Naval Petroleum Reserve No. 4, Alaska 43, Report: 22 p.; 1 Plate: 35.93 x 27.49 inches, https://doi.org/10.3133/70210474.","productDescription":"Report: 22 p.; 1 Plate: 35.93 x 27.49 inches","costCenters":[],"links":[{"id":466292,"rank":2,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70210474/report-thumb.jpg"},{"id":466293,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70210474/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":466294,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70210474/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":375344,"rank":1,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74638.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"500000","country":"United States","state":"Alaska","otherGeospatial":"Firth Rivers, Kongakut","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -147,\n              70.5\n            ],\n            [\n              -147,\n              68\n            ],\n            [\n              -139,\n              68\n            ],\n            [\n              -139,\n              70.5\n            ],\n            [\n              -147,\n              70.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Mangus, Marvin D.","contributorId":81556,"corporation":false,"usgs":true,"family":"Mangus","given":"Marvin","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":925014,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70210473,"text":"70210473 - 1953 - Structure of the discovery anticline","interactions":[],"lastModifiedDate":"2025-01-27T14:50:52.392695","indexId":"70210473","displayToPublicDate":"1953-01-01T16:31:01","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":5963,"text":"Geological Investigations, Naval Petroleum Reserve No. 4, Alaska","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"42","subseriesTitle":"Special Report","title":"Structure of the discovery anticline","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70210473","usgsCitation":"Marshall, C.H., and Rosendale, A., 1953, Structure of the discovery anticline: Geological Investigations, Naval Petroleum Reserve No. 4, Alaska 42, Report: 3 p.; 1 Plate: 51.18 x 23.54 inches, 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,{"id":70098184,"text":"tei410 - 1953 - Uranium in the Poison Basin area, Carbon County, Wyoming - a preliminary report","interactions":[],"lastModifiedDate":"2014-06-11T13:51:06","indexId":"tei410","displayToPublicDate":"1953-01-01T16:11:00","publicationYear":"1953","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":"410","title":"Uranium in the Poison Basin area, Carbon County, Wyoming - a preliminary report","docAbstract":"<p>Uranium minerals were found on October 15, 1953, about seven miles west of Baggs in the Browns Park formation of the Poison Basin area, Carbon County, Wyo. The occurrences extend over an area of at least several square miles in secs. 4 and 5, T. 12 N., R. 92 W., and secs. 32 and 33, T. 13 N., R. 92 W. Uranophane-bearing sandstones contain as much as 3.21 percent uranium in select samples. The occurrences cannot be evaluated because their dimensions and average grade have not been determined. The presence of uranium, however, is significant because it indicates that uranium deposits may be present in the Browns Park formation and also in the underlying formations unconformably overlapped by the Browns Park.<p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei410","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Vine, J.D., and Prichard, G., 1953, Uranium in the Poison Basin area, Carbon County, Wyoming - a preliminary report: U.S. Geological Survey Trace Elements Investigations 410, 23 p., https://doi.org/10.3133/tei410.","productDescription":"23 p.","numberOfPages":"24","costCenters":[],"links":[{"id":284107,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei410.jpg"},{"id":285826,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0410/report.pdf"}],"country":"United States","state":"Wyoming","county":"Carbon County","otherGeospatial":"Poison Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -107.9326,41.0008 ], [ -107.9326,42.4349 ], [ -106.0708,42.4349 ], [ -106.0708,41.0008 ], [ -107.9326,41.0008 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"535595d6e4b0120853e8c2d2","contributors":{"authors":[{"text":"Vine, James D.","contributorId":105287,"corporation":false,"usgs":true,"family":"Vine","given":"James","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":491689,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Prichard, George E.","contributorId":86017,"corporation":false,"usgs":true,"family":"Prichard","given":"George E.","affiliations":[],"preferred":false,"id":491688,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70048457,"text":"tem601 - 1953 - Uranium-bearing coal in the Red Desert, Great Divide Basin, Sweetwater county, Wyoming","interactions":[],"lastModifiedDate":"2014-03-04T13:48:51","indexId":"tem601","displayToPublicDate":"1953-01-01T15:47:00","publicationYear":"1953","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":"601","title":"Uranium-bearing coal in the Red Desert, Great Divide Basin, Sweetwater county, Wyoming","docAbstract":"Uranium-bearing coal in the Wasatch formation occurs in a zone extending 30 miles north of U.S. Highway 30 and the Union Pacific Railroad at Wamsutter, Sweetwater County, Wyoming. The Wasatch formation intertongues with the Green River formation and the beds are nearly flat lying. Preliminary estimation of total reserves in the area indicates the presence of 610,000,000 tons of subbituminous coal containing 14,800 tons of uranium in beds more than 30 inches thich and overlain by less than 75 feet of overburden. The uranium content of the coal ash ranges from 0.010 percent to 0.020 percent throughout most the area included in the reserves. Locally, the uranium content ranges from 0.001 percent to 0.047 in the coal and 0.005 percent to 0.14 percent in the ash.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem601","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Masursky, H., and Pipiringos, G.N., 1953, Uranium-bearing coal in the Red Desert, Great Divide Basin, Sweetwater county, Wyoming: U.S. Geological Survey Trace Elements Memorandum 601, Report: 20 p.; 7 Plates: 37.46 x 21.37 inches and smaller, https://doi.org/10.3133/tem601.","productDescription":"Report: 20 p.; 7 Plates: 37.46 x 21.37 inches and smaller","numberOfPages":"23","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278161,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0601/report-thumb.jpg"},{"id":283264,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0601/plate-2.pdf"},{"id":283265,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0601/plate-4.pdf"},{"id":283266,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0601/plate-5.pdf"},{"id":283263,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0601/report.pdf"},{"id":283267,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0601/plate-6.pdf"},{"id":283268,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0601/plate-7.pdf"},{"id":283269,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0601/plate-8.pdf"},{"id":283270,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0601/plate-9.pdf"}],"country":"United States","state":"Wyoming","county":"Sweetwater County","otherGeospatial":"Red Desert;Great Divide Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.4637,41.3774 ], [ -108.4637,42.2705 ], [ -107.4967,42.2705 ], [ -107.4967,41.3774 ], [ -108.4637,41.3774 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5245576be4b0b3d37307e1c6","contributors":{"authors":[{"text":"Masursky, Harold","contributorId":94304,"corporation":false,"usgs":true,"family":"Masursky","given":"Harold","email":"","affiliations":[],"preferred":false,"id":484700,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pipiringos, George N.","contributorId":103170,"corporation":false,"usgs":true,"family":"Pipiringos","given":"George","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":484701,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70048456,"text":"tem588 - 1953 - Photogeologic map, Emery-9 quadrangle, Emery county, Utah","interactions":[{"subject":{"id":70048456,"text":"tem588 - 1953 - Photogeologic map, Emery-9 quadrangle, Emery county, Utah","indexId":"tem588","publicationYear":"1953","noYear":false,"title":"Photogeologic map, Emery-9 quadrangle, Emery county, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":51224,"text":"ofr5341 - 1953 - Photogeologic map, Emery 9 quadrangle, Emery County, Utah","indexId":"ofr5341","publicationYear":"1953","noYear":false,"title":"Photogeologic map, Emery 9 quadrangle, Emery County, Utah"},"id":1}],"supersededBy":{"id":51224,"text":"ofr5341 - 1953 - Photogeologic map, Emery 9 quadrangle, Emery County, Utah","indexId":"ofr5341","publicationYear":"1953","noYear":false,"title":"Photogeologic map, Emery 9 quadrangle, Emery County, Utah"},"lastModifiedDate":"2014-03-04T13:47:20","indexId":"tem588","displayToPublicDate":"1953-01-01T15:36:00","publicationYear":"1953","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":"588","title":"Photogeologic map, Emery-9 quadrangle, Emery county, Utah","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem588","collaboration":"Prepared in cooperation with the Atomic Energy Commission","usgsCitation":"Condon, W.H., 1953, Photogeologic map, Emery-9 quadrangle, Emery county, Utah: U.S. Geological Survey Trace Elements Memorandum 588, Report: 3 p.; 1 Plate: 23.42 x 30.01 inches, https://doi.org/10.3133/tem588.","productDescription":"Report: 3 p.; 1 Plate: 23.42 x 30.01 inches","numberOfPages":"3","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278158,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0588/report-thumb.jpg"},{"id":283262,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0588/report.pdf"},{"id":283261,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0588/plate-1.pdf"}],"scale":"24000","country":"United States","state":"Utah","county":"Emery County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.125,38.625 ], [ -111.125,38.75 ], [ -111.0,38.75 ], [ -111.0,38.625 ], [ -111.125,38.625 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52455766e4b0b3d37307e19c","contributors":{"authors":[{"text":"Condon, W. H.","contributorId":28611,"corporation":false,"usgs":true,"family":"Condon","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":484699,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70048742,"text":"tem705 - 1953 - Geology of the Red Canyon quadrangle, Montrose county, Colorado","interactions":[{"subject":{"id":70048742,"text":"tem705 - 1953 - Geology of the Red Canyon quadrangle, Montrose county, Colorado","indexId":"tem705","publicationYear":"1953","noYear":false,"title":"Geology of the Red Canyon quadrangle, Montrose county, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":60262,"text":"mf17 - 1954 - Red Canyon quadrangle, Colorado","indexId":"mf17","publicationYear":"1954","noYear":false,"title":"Red Canyon quadrangle, Colorado"},"id":1}],"supersededBy":{"id":60262,"text":"mf17 - 1954 - Red Canyon quadrangle, Colorado","indexId":"mf17","publicationYear":"1954","noYear":false,"title":"Red Canyon quadrangle, Colorado"},"lastModifiedDate":"2014-03-04T14:28:22","indexId":"tem705","displayToPublicDate":"1953-01-01T15:22:00","publicationYear":"1953","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":"705","title":"Geology of the Red Canyon quadrangle, Montrose county, Colorado","docAbstract":"The Red Canyon quadrangle is one of eighteen 7 1/2-minute quadrangles covering the principal carnotite-producing area of southwestern Colorado.  The geology of these quadrangles was mapped by the U.S. Geological Survey for the Atomic Energy Commission as part of a comprehensive study of carnotite deposits. The rocks exposed in the eighteen quadrangles consist of crystalline rocks of pre-Cambrian age and sedimentary rocks that range in age from late Paleozoic to Quaternary. Over much of the area the sedimentary rocks are flat lying, but in places the rocks are disrupted by high-angle faults, and northwest-trending folds.  Conspicuous among the folds are large anticlines having cores of intrusive salt and gypsum. Most of the carnotite deposits are confined to the Salt Wash sandstone member of the Jurassic Morrison formation. Within this sandstone, most of the deposits are spottily distributed through an arcuate zone known as the \"Uruvan Mineral Belt\". Individual deposits range in size from irregular masses containing only a few tons of ore to large, tabular masses containing many thousands of tons.  The ore consists largely of sandstone selectively impregnated and in part replaced by uranium and vanadium, minerals. Most of the deposits appear to be related to certain sedimentary structures in sandstones of favorable composition.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem705","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"McKay, E.J., and Jobin, D., 1953, Geology of the Red Canyon quadrangle, Montrose county, Colorado: U.S. Geological Survey Trace Elements Memorandum 705, Report: 31 p.; 1 Plate: 33.79 x 27.82 inches, https://doi.org/10.3133/tem705.","productDescription":"Report: 31 p.; 1 Plate: 33.79 x 27.82 inches","numberOfPages":"33","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278618,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0705/report-thumb.jpg"},{"id":283339,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0705/plate-1.pdf"},{"id":283340,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0705/report.pdf"}],"country":"United States","state":"Colorado","county":"Montrose County","otherGeospatial":"Red Canyon Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.875,38.375 ], [ -108.875,38.5 ], [ -108.75,38.5 ], [ -108.75,38.375 ], [ -108.875,38.375 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52737beee4b097f32ac3db49","contributors":{"authors":[{"text":"McKay, E. J.","contributorId":57040,"corporation":false,"usgs":true,"family":"McKay","given":"E.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":485526,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jobin, D. A.","contributorId":41062,"corporation":false,"usgs":true,"family":"Jobin","given":"D. A.","affiliations":[],"preferred":false,"id":485525,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":71429,"text":"tei394 - 1953 - The aluminum phosphate zone in the Peace River area, land-pebble phosphate field, Florida","interactions":[],"lastModifiedDate":"2014-06-11T13:09:56","indexId":"tei394","displayToPublicDate":"1953-01-01T15:21:00","publicationYear":"1953","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":"394","title":"The aluminum phosphate zone in the Peace River area, land-pebble phosphate field, Florida","docAbstract":"<p>The Peace River area, comprising T. 30 and 31 S., R. 24 and 25 E., contains a thicker and more persistent aluminum phosphate zone, and one that is higher in P<sub>2</sub>O<sub>5</sub> and uranium content than is known elsewhere in the land-pebble phosphate district. This report has been prepared to bring together all of the information on the aluminum phosphate zone in the area where the first plant to treat this material will probably be located. The area may be divided into three physiographic units, (1) the ridge, (2) the flatwoods, and (3) the valley. Maps showing distribution and grade of the aluminum phosphate zone indicate that the zone is thin or absent in the ridge unit, thickest and most persistent, and of the best grade in P<sub>2</sub>O<sub>5</sub> and uranium in the flatwoods unit, and absent or very low in grade in the valley unit. Maps of thickness and of chemical composition show that even in favorable areas there are places where the aluminum phosphate zone is missing or of questionable economic importance.<p>\n<br/>\n<p>The distribution maps also show that areas of high P<sub>2</sub>O<sub>5</sub> and high uranium content coincide closely. Areas containing thick aluminum phosphate material usually have high uranium and P<sub>2</sub>O<sub>5</sub> contents.</p>\n <br/>\n<p>It is estimated that an average of 13,000 tons per day of aluminum phosphate material might be mined from this area. This figure is based on the probable amount of time, per year, that mining would be in favorable ground. When all mines in the area are in favorable ground, the tonnage per day might be about 23,000 tons.</p>\n<br/>\n<p>Tonnages of aluminum phosphate material have been computed for about 36 percent of the area of T. 30 S., R. 25 E., and for 18 percent of the area of T. 31 S., R. 25 E. The total inferred tonnage is about 150,000,000 short tons, with an average grade of 0.012 percent U<sub>3</sub>O<sub>8</sub>.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei394","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Cathcart, J.B., 1953, The aluminum phosphate zone in the Peace River area, land-pebble phosphate field, Florida: U.S. Geological Survey Trace Elements Investigations 394, Report: 55 p.; 6 Plates: 18.53 x 15.45 inches and smaller, https://doi.org/10.3133/tei394.","productDescription":"Report: 55 p.; 6 Plates: 18.53 x 15.45 inches and smaller","numberOfPages":"56","costCenters":[],"links":[{"id":285819,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0394/figure-11.pdf"},{"id":285820,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0394/figure-12.pdf"},{"id":285816,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0394/figure-09.pdf"},{"id":285818,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0394/figure-10.pdf"},{"id":285821,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0394/figure-13.pdf"},{"id":285822,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0394/figure-15.pdf"},{"id":285823,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0394/report.pdf"},{"id":284100,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei394.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Peace River Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -81.9085,27.7429 ], [ -81.9085,28.195 ], [ -81.2601,28.195 ], [ -81.2601,27.7429 ], [ -81.9085,27.7429 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5355959ee4b0120853e8c275","contributors":{"authors":[{"text":"Cathcart, James B.","contributorId":51201,"corporation":false,"usgs":true,"family":"Cathcart","given":"James","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":284163,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70048587,"text":"tem611 - 1953 - Airborne radioactivity survey of the West Lonetree area, Uinta county, Wyoming","interactions":[],"lastModifiedDate":"2014-03-04T13:54:34","indexId":"tem611","displayToPublicDate":"1953-01-01T15:19:00","publicationYear":"1953","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":"611","title":"Airborne radioactivity survey of the West Lonetree area, Uinta county, Wyoming","docAbstract":"The accompanying map shows the results of an airborne radioactivity survey in an area of 154 square miles in Uinta county, Wyoming. The survey was made by the U.S. Geological Survey, October 23, 1952, as part of a cooperative program with the U.S. Atomic Energy Commission. The survey was made with scintillation-detection equipment mounted in a Douglas DC-3 aircraft. Parallel traverse lines, spaced at quarter-mile intervals, were flown approximately 500 feet above the ground. Aerial photographs were used for pilot guidance, and the flight path of the aircraft was recorded by a gyro-stabilized, continuous-strip-film camera. The distance of the aircraft from the ground was measured with a continuously recording radio altimeter. At 500 feet above the ground, the width of the zone from which anomalous radioactivity is measured varies with the intensity of radiation of the source and, for strong sources, the width would be as much as 1,400 feet. Quarter-mile spacing of the flight paths of the aircraft should be adequate to detect anomalies from strong sources of radioactivity. However, small areas of considerable radioactivity midway between flight paths may not be noted. The approximate location of each radioactivity anomaly is shown on the accompanying map. The plotted position of an anomaly may be in error by as much as a quarter of a mile owing to errors in the available base maps up to several square miles in which it is impossible to find and plot recognizable landmarks. The radioactivity anomaly that is recorded by airborne measurements at 500 feet above the ground can be caused by: 1. A moderately large area in which the rocks and soils are slightly more radioactive than the rocks and soils of the surrounding area. 2. A smaller area in which the rocks and soils are considerably more radioactive than rocks and soils in the surrounding area. 3. A very small area in which to rocks and soils are much more radioactive than the rocks and soils of the surrounding area. Any particular anomaly, therefore, may represent either slightly greater-than-average radioactivity over an area of a few thousand square feet, or high radioactivity over an area of a few hundred square feet. The radioactivity anomalies shown on the accompanying map indicate localities of more-than-average radioactivity, and therefore, suggest areas in which uranium or thorium deposits are more likely to occur.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem611","collaboration":"Prepared in cooperation with the United States Atomic Energy Commission","usgsCitation":"Meuschke, J.L., and Moxham, R., 1953, Airborne radioactivity survey of the West Lonetree area, Uinta county, Wyoming: U.S. Geological Survey Trace Elements Memorandum 611, Report: 3 p.; 1 Plate: 17.32 x 22.22 inches, https://doi.org/10.3133/tem611.","productDescription":"Report: 3 p.; 1 Plate: 17.32 x 22.22 inches","numberOfPages":"3","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278388,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0611/report-thumb.jpg"},{"id":283284,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0611/report.pdf"},{"id":283283,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0611/plate-1.pdf"}],"country":"United States","state":"Wyoming","county":"Uinta County","otherGeospatial":"West Lonetree Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.25,41.033333 ], [ -110.25,41.15 ], [ -110.15,41.15 ], [ -110.15,41.033333 ], [ -110.25,41.033333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"526a416ee4b0c0d229f9f666","contributors":{"authors":[{"text":"Meuschke, J. L.","contributorId":53349,"corporation":false,"usgs":true,"family":"Meuschke","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":485145,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moxham, R.M.","contributorId":42234,"corporation":false,"usgs":true,"family":"Moxham","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":485144,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":71396,"text":"tei352 - 1953 - Reconnaissance for uranium in the southeastern states, 1953","interactions":[],"lastModifiedDate":"2014-05-27T14:42:17","indexId":"tei352","displayToPublicDate":"1953-01-01T15:15:00","publicationYear":"1953","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":"352","title":"Reconnaissance for uranium in the southeastern states, 1953","docAbstract":"<p>During the last quarter of 1952 and most of 1953 the U.S. Geological Survey carried on a program of reconnaissance for radioactive material in the southeastern states on behalf to the Atomic Energy Commission. In the course of the study 111 localities were examined and 43 samples were taken for radioactivity measurements at the Survey's Trace Elements laboratory in Denver, Colo.</p>\n<br/>\n<p>No economic deposits of uranium were found as a result of this work, but weak radioactivity was noted at the Tungsten Mining Coperation property near Townsville, N. C.; the Comolli granite quarry near Elberton, Ga.; in the Beech and Cranberry granite near Roan Mountain, Tenn.; and in several shales in the Valley and Ridge and Appalachian Plateau provinces. Devonian through Pennsylvanian rocks in these two provinces probably constitute the most favorable ground for new discoveries of uranium in the Southeast.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei352","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Johnson, H.S., 1953, Reconnaissance for uranium in the southeastern states, 1953: U.S. Geological Survey Trace Elements Investigations 352, 25 p., https://doi.org/10.3133/tei352.","productDescription":"25 p.","numberOfPages":"26","temporalStart":"1953-01-01","temporalEnd":"1953-12-31","costCenters":[],"links":[{"id":283498,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei352.jpg"},{"id":284550,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0352/report.pdf"}],"country":"United States","state":"Alabama;Florida;Georgia;Kentucky;Mississippi;North Carolina;South Carolina;Tennessee;Virginia;West Virginia","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -91.65,28.5 ], [ -91.65,40.64 ], [ -75.29,40.64 ], [ -75.29,28.5 ], [ -91.65,28.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53559532e4b0120853e8c199","contributors":{"authors":[{"text":"Johnson, Henry S. Jr.","contributorId":86397,"corporation":false,"usgs":true,"family":"Johnson","given":"Henry","suffix":"Jr.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":284101,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70098155,"text":"tei389 - 1953 - Mineralogy and geochemistry of a uraniferous coal from the Red Desert Area, Sweetwater County, Wyoming","interactions":[],"lastModifiedDate":"2014-06-11T13:00:30","indexId":"tei389","displayToPublicDate":"1953-01-01T15:09:00","publicationYear":"1953","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":"389","title":"Mineralogy and geochemistry of a uraniferous coal from the Red Desert Area, Sweetwater County, Wyoming","docAbstract":"<p>A sample of subbituminous uraniferous coal from the Red Desert, Sweetwater County, Wyo., was studied mineralogically. The coal contains gypsum (6 percent), kaolinite (1 percent), quartz (0.3 percent), calcite (trace), and limonite (trace). This suite of minerals and the absence of pyrite show that the coal has been subjected to weathering and oxidation. No uranium minerals have been found; mechanical fractionation has indicated that the uranium is associated with the organic constituents of the coal. The minerals that have been isolated contain 0.0006 percent uranium, a content which is to be expected for nonuraniferous sedimentary rocks. The organic components of the coal contain approximately 0.002 percent uranium. On the basis of material balance calculations, the organic components carry 98 percent of the uranium in the coal.<p>\n<br/>\n<p>Fischer assays of this weathered coal from the Red Desert indicate a yield of 16.7 gallons of tar per ton on low-temperature retorting. In view of the large reserve of subbituminous coal in the Red Desert, its probable ease of mining, and its tar yield, it may be desirable to carry out further evaluation of the coal as a fuel or raw material for the manufacture of tar or chemicals. If economic factors permit utilization of the coal, the uranium, although present in small percentages, could be recovered as a byproduct.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei389","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Breger, I., Deul, M., Meyrowitz, R., and Rubinstein, S., 1953, Mineralogy and geochemistry of a uraniferous coal from the Red Desert Area, Sweetwater County, Wyoming: U.S. Geological Survey Trace Elements Investigations 389, 19 p., https://doi.org/10.3133/tei389.","productDescription":"19 p.","numberOfPages":"20","costCenters":[],"links":[{"id":284095,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei389.jpg"},{"id":285815,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0389/report.pdf"}],"country":"United States","state":"Wyoming","county":"Sweetwater County","otherGeospatial":"Red Desert","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.0539,42.2705 ], [ -110.0539,40.9971 ], [ -107.4994,40.9971 ], [ -107.4994,42.2705 ], [ -110.0539,42.2705 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"535594b5e4b0120853e8c086","contributors":{"authors":[{"text":"Breger, Irving A.","contributorId":41901,"corporation":false,"usgs":true,"family":"Breger","given":"Irving A.","affiliations":[],"preferred":false,"id":491651,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Deul, Maurice","contributorId":67562,"corporation":false,"usgs":true,"family":"Deul","given":"Maurice","email":"","affiliations":[],"preferred":false,"id":491653,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Meyrowitz, Robert","contributorId":62680,"corporation":false,"usgs":true,"family":"Meyrowitz","given":"Robert","email":"","affiliations":[],"preferred":false,"id":491652,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rubinstein, Samuel","contributorId":85886,"corporation":false,"usgs":true,"family":"Rubinstein","given":"Samuel","email":"","affiliations":[],"preferred":false,"id":491654,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70048741,"text":"tem704 - 1953 - Geology of the Pine Mountain quadrangle, Mesa county, Colorado","interactions":[{"subject":{"id":70048741,"text":"tem704 - 1953 - Geology of the Pine Mountain quadrangle, Mesa county, Colorado","indexId":"tem704","publicationYear":"1953","noYear":false,"title":"Geology of the Pine Mountain quadrangle, Mesa county, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":59108,"text":"mf20 - 1955 - Pine Mountain quadrangle, Colorado","indexId":"mf20","publicationYear":"1955","noYear":false,"title":"Pine Mountain quadrangle, Colorado"},"id":1}],"supersededBy":{"id":59108,"text":"mf20 - 1955 - Pine Mountain quadrangle, Colorado","indexId":"mf20","publicationYear":"1955","noYear":false,"title":"Pine Mountain quadrangle, Colorado"},"lastModifiedDate":"2014-03-04T14:27:38","indexId":"tem704","displayToPublicDate":"1953-01-01T15:07:00","publicationYear":"1953","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":"704","title":"Geology of the Pine Mountain quadrangle, Mesa county, Colorado","docAbstract":"The Pine Mountain quadrangle is one of eighteen 7 1/2-minute quadrangles covering the principal carnotite-producing area of southwestern Colorado.  The geology of these quadrangles was mapped by the U.S. Geological Survey for the Atomic Energy Commission as part of a comprehensive study of carnotite deposits.  The rocks exposed in the eighteen quadrangles consist of crystalline rocks of pre-Cambrian age and sedimentary rocks that range in age from Paleozoic to Quaternary. Over mush of the area the sedimentary rocks are flat lying, but in places the rocks are disrupted by high-angle faults, and northwest-trending folds.  Conspicuous among the folds are large anticlines having cores of intrusive salt and gypsum.  Most of the carnotite deposits are confines to the Salt Wash sandstone member of the Jurassic Morrison formation.  Within this sandstone, most of the deposits are spottily distributed through an arcuate zone known as the \"Uravan Mineral Belt\". Individual deposits range in sizer from irregular masses containing only a few ton of ore to large, tabular masses containing many thousands of tons.  The ore consists largely of sandstone selectively impregnated and in part replaced by uranium and vanadium minerals. Most of the deposits appear to be related to certain sedimentary structures in sandstones of favorable composition.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem704","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Cater, F.W., 1953, Geology of the Pine Mountain quadrangle, Mesa county, Colorado: U.S. Geological Survey Trace Elements Memorandum 704, Report: 30 p.; 1 Plate: 33.18 x 27.87 inches, https://doi.org/10.3133/tem704.","productDescription":"Report: 30 p.; 1 Plate: 33.18 x 27.87 inches","numberOfPages":"33","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278617,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0704/report-thumb.jpg"},{"id":283337,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0704/report.pdf"},{"id":283338,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0704/plate-1.pdf"}],"country":"United States","state":"Colorado","county":"Mesa County","otherGeospatial":"Pine Mountain Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.875,38.625 ], [ -108.875,38.75 ], [ -108.75,38.75 ], [ -108.75,38.625 ], [ -108.875,38.625 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52737beee4b097f32ac3db46","contributors":{"authors":[{"text":"Cater, Fred W. Jr.","contributorId":36988,"corporation":false,"usgs":true,"family":"Cater","given":"Fred","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":485524,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71886,"text":"tei310 - 1953 - Search for and geology of radioactive deposits, semiannual progress report: June 1 to November 30, 1952","interactions":[],"lastModifiedDate":"2014-03-25T08:59:02","indexId":"tei310","displayToPublicDate":"1953-01-01T15:03:00","publicationYear":"1953","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":"310","title":"Search for and geology of radioactive deposits, semiannual progress report: June 1 to November 30, 1952","docAbstract":"The Colorado Plateau geologic studies comprise a number of geologic mapping and specialized geologic studies of the pre-Morrison (mainly Triassic) and Morrison uranium-bearing formations.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei310","collaboration":"This report concerns work done chiefly on behalf of the Division of Raw Materials and Division of Research of the U.S. Atomic Energy Commission","usgsCitation":"U.S. Geological Survey, 1953, Search for and geology of radioactive deposits, semiannual progress report: June 1 to November 30, 1952: U.S. Geological Survey Trace Elements Investigations 310, 336 p., https://doi.org/10.3133/tei310.","productDescription":"336 p.","numberOfPages":"353","temporalStart":"1952-06-01","temporalEnd":"1952-11-30","costCenters":[],"links":[{"id":283497,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei310.jpg"},{"id":284575,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0310/report.pdf"}],"country":"United States","state":"Arizona;Colorado;New Mexico;Utah","otherGeospatial":"Colorado Plateau","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.115269,36.799136 ], [ -110.115269,37.301078 ], [ -109.545994,37.301078 ], [ -109.545994,36.799136 ], [ -110.115269,36.799136 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd71a2e4b0b29085107cd4"}
,{"id":70048585,"text":"tem610 - 1953 - Airborne radioactivity survey of the Tabernacle Buttes area, Sublette and Fremont counties, Wyoming","interactions":[],"lastModifiedDate":"2014-03-04T13:53:49","indexId":"tem610","displayToPublicDate":"1953-01-01T14:47:00","publicationYear":"1953","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":"610","title":"Airborne radioactivity survey of the Tabernacle Buttes area, Sublette and Fremont counties, Wyoming","docAbstract":"The accompanying map shows the results of an airborne radioactivity survey in an area of 670 square miles in Sublette and Fremont counties, Wyoming. The survey was made by the U.S. Geological Survey, October 20, 1952, as part of a cooperative program with the U.S. Atomic Energy Commission. The survey was made with scintillation-detection equipment mounted in a Douglas DC-3 aircraft. Parallel traverse lines, spaced at quarter-mile intervals, were flown approximately 500 feet above the ground. Aerial photographs were used for pilot guidance, and the flight path of the aircraft was recorded by a gyro-stabilized, continuous-strip-film camera. The distance of the aircraft from the ground was measured with a continuously recording radio altimeter. At 500 feet above the ground, the width of the zone from which anomalous radioactivity is measured varies with the intensity of radiation of the source and, for strong sources, the width would be as much as 1,400 feet. Quarter-mile spacing of the flight paths of the aircraft should be adequate to detect anomalies from strong sources of radioactivity. However, small areas of considerable radioactivity midway between flight paths may not be noted. The approximate location of each radioactivity anomaly is shown on the accompanying map. The plotted position of an anomaly may be in error by as much as a quarter of a mile owing to errors in the available base maps up to several square miles in which it is impossible to find and plot recognizable landmarks. The radioactivity anomaly that is recorded by airborne measurements at 500 feet above the ground can be caused by: 1. A moderately large area in which the rocks and soils are slightly more radioactive than the rocks and soils of the surrounding area. 2. A smaller area in which the rocks and soils are considerably more radioactive than rocks and soils in the surrounding area. 3. A very small area in which to rocks and soils are much more radioactive than the rocks and soils of the surrounding area. Any particular anomaly, therefore, may represent either slightly greater-than-average radioactivity over an area of a few thousand square feet, or high radioactivity over an area of a few hundred square feet. The radioactivity anomalies shown on the accompanying map indicate localities of more-than-average radioactivity, and therefore, suggest areas in which uranium or thorium deposits are more likely to occur.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem610","collaboration":"Prepared in cooperation with the United States Atomic Energy Commission","usgsCitation":"U.S. Geological Survey, 1953, Airborne radioactivity survey of the Tabernacle Buttes area, Sublette and Fremont counties, Wyoming: U.S. Geological Survey Trace Elements Memorandum 610, Report: 3 p.; 1 Plate: 21.92 x 17.27 inches, https://doi.org/10.3133/tem610.","productDescription":"Report: 3 p.; 1 Plate: 21.92 x 17.27 inches","numberOfPages":"3","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278387,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0610/report-thumb.jpg"},{"id":283282,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0610/report.pdf"},{"id":283281,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0610/plate-1.pdf"}],"country":"United States","state":"Wyoming","county":"Fremont County;Sublette County","otherGeospatial":"Tabernacle Buttes Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.333333,42.4 ], [ -109.333333,42.5 ], [ -109.0,42.5 ], [ -109.0,42.4 ], [ -109.333333,42.4 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"526a416ee4b0c0d229f9f660"}
,{"id":70048584,"text":"tem609 - 1953 - Airborne radioactivity survey of the Aspen Mountain area, Sweetwater county, Wyoming","interactions":[],"lastModifiedDate":"2014-03-04T13:53:09","indexId":"tem609","displayToPublicDate":"1953-01-01T14:31:00","publicationYear":"1953","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":"609","title":"Airborne radioactivity survey of the Aspen Mountain area, Sweetwater county, Wyoming","docAbstract":"The accompanying map shows the results of an airborne radioactivity survey covering 700 square miles in the Aspen Mountain area, Sweetwater county, Wyoming. The survey was made by the U.S. Geological Survey, October 22, 1952, as part of a cooperative program with the U.S. Atomic Energy Commission. The survey was made with scintillation-detection equipment mounted in a Douglas DC-3 aircraft. Parallel traverse lines, spaced at quarter-mile intervals, were flown approximately 500 feet above the ground. Aerial photographs were used for pilot guidance, and the flight path of the aircraft was recorded by a gyro-stabilized, continuous-strip-film camera. The distance of the aircraft from the ground was measured with a continuously recording radio altimeter. At 500 feet above the ground, the width of the zone from which anomalous radioactivity is measured varies with the intensity of radiation of the source and, for strong sources, the width would be as much as 1,400 feet. Quarter-mile spacing of the flight paths of the aircraft should be adequate to detect anomalies from strong sources of radioactivity. However, small areas of considerable radioactivity midway between flight paths may not be noted. The approximate location of each radioactivity anomaly is shown on the accompanying map. The plotted position of an anomaly may be in error by as much as a quarter of a mile owing to errors in the available base maps up to several square miles in which it is impossible to find and plot recognizable landmarks. The radioactivity anomaly that is recorded by airborne measurements at 500 feet above the ground can be caused by: 1. A moderately large area in which the rocks and soils are slightly more radioactive than the rocks and soils of the surrounding area. 2. A smaller area in which the rocks and soils are considerably more radioactive than rocks and soils in the surrounding area. 3. A very small area in which to rocks and soils are much more radioactive than the rocks and soils of the surrounding area. Any particular anomaly, therefore, may represent either slightly greater-than-average radioactivity over an area of a few thousand square feet, or high radioactivity over an area of a few hundred square feet. The radioactivity anomalies shown on the accompanying map indicate localities of more-than-average radioactivity, and therefore, suggest areas in which uranium or thorium deposits are more likely to occur.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem609","collaboration":"Prepared in cooperation with the United States Atomic Energy Commission","usgsCitation":"Meuschke, J.L., and Moxham, R., 1953, Airborne radioactivity survey of the Aspen Mountain area, Sweetwater county, Wyoming: U.S. Geological Survey Trace Elements Memorandum 609, Report: 2 p.; 1 Plate: 22.11 x 16.99 inches, https://doi.org/10.3133/tem609.","productDescription":"Report: 2 p.; 1 Plate: 22.11 x 16.99 inches","numberOfPages":"2","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278386,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0609/report-thumb.jpg"},{"id":283279,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0609/report.pdf"},{"id":283280,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0609/plate-1.pdf"}],"country":"United States","state":"Wyoming","county":"Sweetwater County","otherGeospatial":"Aspen Mountain Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.283333,41.116667 ], [ -109.283333,41.25 ], [ -109.0,41.25 ], [ -109.0,41.116667 ], [ -109.283333,41.116667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"526a416de4b0c0d229f9f64e","contributors":{"authors":[{"text":"Meuschke, J. L.","contributorId":53349,"corporation":false,"usgs":true,"family":"Meuschke","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":485135,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moxham, R.M.","contributorId":42234,"corporation":false,"usgs":true,"family":"Moxham","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":485134,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70048739,"text":"tem702 - 1953 - Geology of the Naturita NW quadrangle, Colorado","interactions":[],"lastModifiedDate":"2014-03-04T14:26:16","indexId":"tem702","displayToPublicDate":"1953-01-01T14:27:00","publicationYear":"1953","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":"702","title":"Geology of the Naturita NW quadrangle, Colorado","docAbstract":"The Naturita NW quadrangle is one of eighteen 7 1/2-minute quadrangles covering the principal carnotite-producing area of southwestern Colorado. The geology of these quadrangles were mapped by the U.S. Geological Survey on behalf of the U.S. Atomic Energy Commission as part of a comprehensive study of carnotite deposits. The rocks exposed in the eighteen quadrangles consist of crystalline rocks of pre-Cambrian age and sedimentary rocks that range in age from late Paleozoic to Quaternary. Over much of the area the sedimentary rocks are flat lying, but in places the rocks are disrupted by high-angle faults, and northwest-trending folds.  Conspicuous among the folds are large anticlines having cores of intrusive salt and gypsum. Most of the carnotite deposits are confined to the Salt Wash sandstone member of the Jurassic Morrison formation.  Within this sandstone, most of the deposits are spottily distributed through an arcuate zone known as the \"Uravan Mineral Belt\".  Individual deposits range in size from irregular masses containing only a few tons of ore to large, tabular masses containing many thousands of tons. The ore consists largely of sandstone selectively impregnated and in part replaced by uranium and vanadium minerals. Most of the deposits appear ro be related to certain sedimentary structures in sandstones of favorable composition.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem702","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Cater, F.W., and Vogel, J., 1953, Geology of the Naturita NW quadrangle, Colorado: U.S. Geological Survey Trace Elements Memorandum 702, Report: 27 p.; 1 Plate: 33.93 x 27.96 inches, https://doi.org/10.3133/tem702.","productDescription":"Report: 27 p.; 1 Plate: 33.93 x 27.96 inches","numberOfPages":"29","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278613,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0702/report-thumb.jpg"},{"id":283333,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0702/plate-1.pdf"},{"id":283334,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0702/report.pdf"}],"country":"United States","state":"Colorado","otherGeospatial":"Naturita Nw Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.75,38.125 ], [ -108.75,38.25 ], [ -108.625,38.25 ], [ -108.625,38.125 ], [ -108.75,38.125 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52737bede4b097f32ac3db40","contributors":{"authors":[{"text":"Cater, Fred W. Jr.","contributorId":36988,"corporation":false,"usgs":true,"family":"Cater","given":"Fred","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":485521,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vogel, J.D.","contributorId":101725,"corporation":false,"usgs":true,"family":"Vogel","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":485522,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70048445,"text":"tem526A - 1953 - Photogeologic map, Navajo Mountain-13 quadrangle, San Juan and Kane counties, Utah, and Coconino county, Arizona","interactions":[{"subject":{"id":70048445,"text":"tem526A - 1953 - Photogeologic map, Navajo Mountain-13 quadrangle, San Juan and Kane counties, Utah, and Coconino county, Arizona","indexId":"tem526A","publicationYear":"1953","noYear":false,"chapter":"A","title":"Photogeologic map, Navajo Mountain-13 quadrangle, San Juan and Kane counties, Utah, and Coconino county, Arizona"},"predicate":"SUPERSEDED_BY","object":{"id":66093,"text":"i184 - 1956 - Photogeologic map of the Navajo Mountain-13 quadrangle, Kane and San Juan Counties, Utah, and Coconino County, Arizona","indexId":"i184","publicationYear":"1956","noYear":false,"title":"Photogeologic map of the Navajo Mountain-13 quadrangle, Kane and San Juan Counties, Utah, and Coconino County, Arizona"},"id":1}],"supersededBy":{"id":66093,"text":"i184 - 1956 - Photogeologic map of the Navajo Mountain-13 quadrangle, Kane and San Juan Counties, Utah, and Coconino County, Arizona","indexId":"i184","publicationYear":"1956","noYear":false,"title":"Photogeologic map of the Navajo Mountain-13 quadrangle, Kane and San Juan Counties, Utah, and Coconino County, Arizona"},"lastModifiedDate":"2014-03-04T13:42:36","indexId":"tem526A","displayToPublicDate":"1953-01-01T14:10:00","publicationYear":"1953","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":"526","chapter":"A","title":"Photogeologic map, Navajo Mountain-13 quadrangle, San Juan and Kane counties, Utah, and Coconino county, Arizona","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem526A","collaboration":"Prepared in cooperation with the U.S. Atomic Energy Commission","usgsCitation":"Hackman, R., 1953, Photogeologic map, Navajo Mountain-13 quadrangle, San Juan and Kane counties, Utah, and Coconino county, Arizona: U.S. Geological Survey Trace Elements Memorandum 526, Report: 3 p.; 1 Plate: 23.66 x 28.78 inches, https://doi.org/10.3133/tem526A.","productDescription":"Report: 3 p.; 1 Plate: 23.66 x 28.78 inches","numberOfPages":"3","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278147,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0526-A/report-thumb.jpg"},{"id":283250,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0526-A/report.pdf"},{"id":283249,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0526-A/plate-1.pdf"}],"scale":"24000","country":"United States","state":"Arizona;Utah","county":"Coconino County;Kane County;San Juan County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.0,37.0 ], [ -111.0,37.125 ], [ -110.875,37.125 ], [ -110.875,37.0 ], [ -111.0,37.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52455767e4b0b3d37307e1a5","contributors":{"authors":[{"text":"Hackman, R.J.","contributorId":95086,"corporation":false,"usgs":true,"family":"Hackman","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":484677,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70048444,"text":"tem523A - 1953 - Photogeologic map, Orange Cliffs-11 quadrangle, Garfield and Wayne counties, Utah","interactions":[{"subject":{"id":70048444,"text":"tem523A - 1953 - Photogeologic map, Orange Cliffs-11 quadrangle, Garfield and Wayne counties, Utah","indexId":"tem523A","publicationYear":"1953","noYear":false,"chapter":"A","title":"Photogeologic map, Orange Cliffs-11 quadrangle, Garfield and Wayne counties, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":66897,"text":"i187 - 1956 - Photogeologic map of the Orange Cliffs-11 quadrangle, Wayne and Garfield Counties, Utah","indexId":"i187","publicationYear":"1956","noYear":false,"title":"Photogeologic map of the Orange Cliffs-11 quadrangle, Wayne and Garfield Counties, Utah"},"id":1}],"supersededBy":{"id":66897,"text":"i187 - 1956 - Photogeologic map of the Orange Cliffs-11 quadrangle, Wayne and Garfield Counties, Utah","indexId":"i187","publicationYear":"1956","noYear":false,"title":"Photogeologic map of the Orange Cliffs-11 quadrangle, Wayne and Garfield Counties, Utah"},"lastModifiedDate":"2014-03-04T13:41:28","indexId":"tem523A","displayToPublicDate":"1953-01-01T14:03:00","publicationYear":"1953","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":"523","chapter":"A","title":"Photogeologic map, Orange Cliffs-11 quadrangle, Garfield and Wayne counties, Utah","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem523A","collaboration":"Prepared in cooperation with the U.S. Atomic Energy Commission","usgsCitation":"Ray, R., 1953, Photogeologic map, Orange Cliffs-11 quadrangle, Garfield and Wayne counties, Utah: U.S. Geological Survey Trace Elements Memorandum 523, Report: 3 p.; 1 Plate: 24.13 x 30.40 inches, https://doi.org/10.3133/tem523A.","productDescription":"Report: 3 p.; 1 Plate: 24.13 x 30.40 inches","numberOfPages":"3","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278146,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0523-A/report-thumb.jpg"},{"id":283248,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0523-A/plate-1.pdf"},{"id":283247,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0523-A/report.pdf"}],"scale":"24000","country":"United States","state":"Utah","county":"Garfield County;Wayne County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.375,38.125 ], [ -110.375,38.25 ], [ -110.25,38.25 ], [ -110.25,38.125 ], [ -110.375,38.125 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52455768e4b0b3d37307e1a8","contributors":{"authors":[{"text":"Ray, R.G.","contributorId":60664,"corporation":false,"usgs":true,"family":"Ray","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":484676,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70048583,"text":"tem607 - 1953 - Airborne radioactivity of portions of the Defiance Uplift and Carrizo Mountains, Apache county, Arizona","interactions":[{"subject":{"id":70048583,"text":"tem607 - 1953 - Airborne radioactivity of portions of the Defiance Uplift and Carrizo Mountains, Apache county, Arizona","indexId":"tem607","publicationYear":"1953","noYear":false,"title":"Airborne radioactivity of portions of the Defiance Uplift and Carrizo Mountains, Apache county, Arizona"},"predicate":"SUPERSEDED_BY","object":{"id":51306,"text":"ofr53139 - 1953 - Photogeologic map showing airborne radioactivity anomalies in the Defiance uplift and Carrizo Mountains, Apache County, Arizona","indexId":"ofr53139","publicationYear":"1953","noYear":false,"title":"Photogeologic map showing airborne radioactivity anomalies in the Defiance uplift and Carrizo Mountains, Apache County, Arizona"},"id":1}],"supersededBy":{"id":51306,"text":"ofr53139 - 1953 - Photogeologic map showing airborne radioactivity anomalies in the Defiance uplift and Carrizo Mountains, Apache County, Arizona","indexId":"ofr53139","publicationYear":"1953","noYear":false,"title":"Photogeologic map showing airborne radioactivity anomalies in the Defiance uplift and Carrizo Mountains, Apache County, Arizona"},"lastModifiedDate":"2014-03-04T13:52:14","indexId":"tem607","displayToPublicDate":"1953-01-01T14:01:00","publicationYear":"1953","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":"607","title":"Airborne radioactivity of portions of the Defiance Uplift and Carrizo Mountains, Apache county, Arizona","docAbstract":"The accompanying map shows the results of an airborne radioactivity survey covering 940 square miles in Apache county, Arizona. The survey was made by the U.S. Geological Survey from September 8 to October 3, 1952, as part of a cooperative program with the U.S. Atomic Energy Commission. The survey was made with scintillation-detection equipment mounted in a Douglas DC-3 aircraft. Parallel traverse lines, spaced at quarter-mile intervals, were flown approximately 500 feet above the ground. Aerial photographs were used for pilot guidance, and the flight path of the aircraft was recorded by a gyro-stabilized, continuous-strip-film camera. The distance of the aircraft from the ground was measured with a continuously recording radio altimeter. At 500 feet above the ground, the width of the zone from which anomalous radioactivity is measured varies with the intensity of radiation of the source and, for strong sources, the width would be as much as 1,400 feet. Quarter-mile spacing of the flight paths of the aircraft should be adequate to detect anomalies from strong sources of radioactivity. However, small areas of considerable radioactivity midway between flight paths may not be noted. The approximate location of each radioactivity anomaly is shown on the accompanying map. The plotted position of an anomaly may be in error by as much as a quarter of a mile owing to errors in the available base maps up to several square miles in which it is impossible to find and plot recognizable landmarks. The radioactivity anomaly that is recorded by airborne measurements at 500 feet above the ground can be caused by: 1. A moderately large area in which the rocks and soils are slightly more radioactive than the rocks and soils of the surrounding area. 2. A smaller area in which the rocks and soils are considerably more radioactive than rocks and soils in the surrounding area. 3. A very small area in which to rocks and soils are much more radioactive than the rocks and soils of the surrounding area. Any particular anomaly, therefore, may represent either slightly greater-than-average radioactivity over an area of a few thousand square feet, or high radioactivity over an area of a few hundred square feet. The radioactivity anomalies shown on the accompanying map indicate localities of more-than-average radioactivity, and therefore, suggest areas in which uranium or thorium deposits are more likely to occur.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem607","collaboration":"Prepared in cooperation with the United States Atomic Energy Commission","usgsCitation":"Johnson, R., and Moxham, R., 1953, Airborne radioactivity of portions of the Defiance Uplift and Carrizo Mountains, Apache county, Arizona: U.S. Geological Survey Trace Elements Memorandum 607, Report: 2 p.; 1 Plate: 31.03 x 39.32 inches, https://doi.org/10.3133/tem607.","productDescription":"Report: 2 p.; 1 Plate: 31.03 x 39.32 inches","numberOfPages":"2","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278385,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0607/report-thumb.jpg"},{"id":283278,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0607/plate-1.pdf"},{"id":283277,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0607/report.pdf"}],"country":"United States","state":"Arizona","county":"Apache County","otherGeospatial":"Carrizo Mountains;Defiance Uplift","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.5,35.75 ], [ -109.5,37.0 ], [ -109.25,37.0 ], [ -109.25,35.75 ], [ -109.5,35.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"526a416ce4b0c0d229f9f643","contributors":{"authors":[{"text":"Johnson, R.W.","contributorId":83194,"corporation":false,"usgs":true,"family":"Johnson","given":"R.W.","affiliations":[],"preferred":false,"id":485133,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moxham, R.M.","contributorId":42234,"corporation":false,"usgs":true,"family":"Moxham","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":485132,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70048735,"text":"tem700 - 1953 - Geology of the Joe Davis Hill quadrangle, Dolores and San Miguel counties, Colorado","interactions":[],"lastModifiedDate":"2014-03-04T14:24:32","indexId":"tem700","displayToPublicDate":"1953-01-01T13:54:00","publicationYear":"1953","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":"700","title":"Geology of the Joe Davis Hill quadrangle, Dolores and San Miguel counties, Colorado","docAbstract":"The Joe Davis Hill quadrangle is one of eighteen 7 1/2-minute quadrangles covering the principal carnotite-producing area of southwestern Colorado.  The geology of these quadrangles was mapped by the U.S. Geological Survey for the Atomic Energy Commission as part of a comprehensive study of carnotite deposits. The rocks exposed in the eighteen quadrangles consist of crystalline rocks of pre-Cambrian age and sedimentary rocks that range in age from late Paleozoic to Quaternary. Over much of the area the sedimentary rocks are flat lying, but in places the rocks are disrupted by hih-angle faults, and northwest-trending folds.  Conspicuous among the folds are large anticlines having cores of intrusive salt and gypsum.  Most of the carnotite deposits are confined to Salt Wash sandstone member of the Jurassic Morrison formation.  Within this sandstone, most of the deposits are spottily distributed through an arcuate zone known as the \"Uravan Mineral Belt\".  Individual deposits range in size from irregular masses containing only a few tons of ore to large, tabular masses containing many thousands of tons. The ore consists largely of sandstone selectively impregnated and in part replaced by uranium and vanadium minerals. Most of the deposits appear to be related to certain sedimentary structures in sandstones of favorable composition.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem700","collaboration":"This report concerns work partly done on behalf of the Division of Raw Materials of the U.S Atomic Energy Commission","usgsCitation":"Cater, F.W., and Bell, H., 1953, Geology of the Joe Davis Hill quadrangle, Dolores and San Miguel counties, Colorado: U.S. Geological Survey Trace Elements Memorandum 700, Report: 24 p.; 1 Plate: 33.68 x 27.93 inches, https://doi.org/10.3133/tem700.","productDescription":"Report: 24 p.; 1 Plate: 33.68 x 27.93 inches","numberOfPages":"26","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278610,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0700/report-thumb.jpg"},{"id":283329,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0700/plate-1.pdf"},{"id":283330,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0700/report.pdf"}],"country":"United States","state":"Colorado","county":"Dolores County;San Miguel County","otherGeospatial":"Joe Davis Hill Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.875,37.875 ], [ -108.875,38.0 ], [ -108.75,38.0 ], [ -108.75,37.875 ], [ -108.875,37.875 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52737bece4b097f32ac3db38","contributors":{"authors":[{"text":"Cater, Fred W. Jr.","contributorId":36988,"corporation":false,"usgs":true,"family":"Cater","given":"Fred","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":485509,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bell, Henry III","contributorId":37710,"corporation":false,"usgs":true,"family":"Bell","given":"Henry","suffix":"III","email":"","affiliations":[],"preferred":false,"id":485510,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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