Part I, T. S. Lovering. Preliminary work in the Tintic district, Utah, determined the relative distance of migration of ore metals in moist carbonate and silicic wall rocks near ore, and in ground water having a very sluggish circulation through mineralized ground. The analyses of efflorescences in the Tintic Standard mine openings at suitable localities indicated that under the conditions existing during the past 25 years lead has not moved perceptibly; gold has migrated only a few inches; copper has moved a few score feet at most and only in acid solutions; and zinc has traveled hundreds of feet, but not as far as some silver. Silver may travel far in the oxidized zone, but if it comes in contact with sulfides its migration is quickly halted. The chief chemical factors that influence the migration of metals in supergene solutions are the hydrogen ion concentration (pH) of hydrolysis of the metal ion, the solubility of sulfates of the metals, and the position of the metals in Schuermann's series if the solutions are in contact with sulfides for a considerable time.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.47.7.685","usgsCitation":"Morris, H.T., and Lovering, T.S., 1952, Supergene and hydrothermal dispersion of heavy metals in wall rocks near ore bodies, Tintic district, Utah: Economic Geology, v. 47, no. 7, p. 685-716, https://doi.org/10.2113/gsecongeo.47.7.685.","productDescription":"32 p.","startPage":"685","endPage":"716","costCenters":[],"links":[{"id":386622,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"southern Utah","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -114.01611328125,\n 36.99377838872517\n ],\n [\n -109.072265625,\n 36.99377838872517\n ],\n [\n -109.072265625,\n 39.977120098439634\n ],\n [\n -114.01611328125,\n 39.977120098439634\n ],\n [\n -114.01611328125,\n 36.99377838872517\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"47","issue":"7","noUsgsAuthors":false,"publicationDate":"1952-11-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Morris, H. T.","contributorId":15585,"corporation":false,"usgs":true,"family":"Morris","given":"H.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":817935,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lovering, T. S.","contributorId":108085,"corporation":false,"usgs":true,"family":"Lovering","given":"T.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":817936,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70221613,"text":"70221613 - 1952 - Glaciation and drainage changes in the fish Lake Plateau, Utah","interactions":[],"lastModifiedDate":"2021-06-25T14:19:04.69803","indexId":"70221613","displayToPublicDate":"1952-11-01T09:12:24","publicationYear":"1952","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":"Glaciation and drainage changes in the fish Lake Plateau, Utah","docAbstract":"The Fish Lake Plateau, nearly centrally located among the High Plateaus of Utah, exhibits glacial and other geomorphic features of regional significance. The plateau is divided into two areas by Fish Lake and the wide valley of Sevenmile Creek. The Fish Lake trough is a structural basin; Sevenmile Valley may be largely erosional. Volcanic rocks of Tertiary age underlie most of the plateau; early Tertiary sedimentary rocks are also present. Glaciated canyons with well-developed cirques are especially prominent along the east-facing sides of the Fish Lake trough and Sevenmile Valley. Ice-eroded features occur over much of the plateau top. Near the mouths of several of the glaciated canyons are two conspicuous sets of moraines. The older set is more extensive and less rugged than the younger and occurs at somewhat lower elevations. Two substages of glaciation thus recognized are correlated with Wisconsin I and II of Ray; probable correlatives of Wisconsin III, IV, and V are represented by moraines which are younger than these two sets. Fish Lake drains north into Fremont River, a tributary of the Colorado River. An abandoned southern outlet and waterfall, the latter at a higher elevation than the present elevation of the original northern bedrock divide, indicate drainage reversal. Evidence is presented which suggests that this reversal was pre-glacial and probably the result of fault-block tilting.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1952)63[1109:GADCIT]2.0.CO;2","usgsCitation":"Hardy, C.T., and Muessig, S., 1952, Glaciation and drainage changes in the fish Lake Plateau, Utah: Geological Society of America Bulletin, v. 63, no. 11, p. 1109-1116, https://doi.org/10.1130/0016-7606(1952)63[1109:GADCIT]2.0.CO;2.","productDescription":"8 p.","startPage":"1109","endPage":"1116","costCenters":[],"links":[{"id":386738,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Fish Lake Hightop","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.796875,\n 38.16047628099622\n ],\n [\n -111.03881835937499,\n 38.16047628099622\n ],\n [\n -111.03881835937499,\n 39.04478604850143\n ],\n [\n -111.796875,\n 39.04478604850143\n ],\n [\n -111.796875,\n 38.16047628099622\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"63","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hardy, Clyde T.","contributorId":260420,"corporation":false,"usgs":false,"family":"Hardy","given":"Clyde","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":818264,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Muessig, S.","contributorId":19287,"corporation":false,"usgs":true,"family":"Muessig","given":"S.","email":"","affiliations":[],"preferred":false,"id":818265,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":37847,"text":"37847 - 1952 - Pelagic fur seal research off Japan in 1950","interactions":[],"lastModifiedDate":"2014-07-24T11:07:02","indexId":"37847","displayToPublicDate":"1952-10-01T11:05:42","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"338","title":"Pelagic fur seal research off Japan in 1950","docAbstract":"No abstract available.","language":"English","publisher":"General Headquarters, Supreme Commander for the Allied Powers","publisherLocation":"Tokyo, Japan","usgsCitation":"Wilke, F., 1952, Pelagic fur seal research off Japan in 1950: Wildlife Leaflet 338, 35 p.","productDescription":"35 p.","numberOfPages":"35","costCenters":[],"links":[{"id":290886,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Japan","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 122.93,24.05 ], [ 122.93,45.52 ], [ 153.99,45.52 ], [ 153.99,24.05 ], [ 122.93,24.05 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd7c6e4b0824b2d177f29","contributors":{"authors":[{"text":"Wilke, Ford","contributorId":7192,"corporation":false,"usgs":true,"family":"Wilke","given":"Ford","email":"","affiliations":[],"preferred":false,"id":218601,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221616,"text":"70221616 - 1952 - Method for determining the age of igneous rocks using the accessory minerals","interactions":[],"lastModifiedDate":"2021-06-25T15:03:30.864413","indexId":"70221616","displayToPublicDate":"1952-10-01T09:58:36","publicationYear":"1952","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":"Method for determining the age of igneous rocks using the accessory minerals","docAbstract":"The age of igneous rocks is determinable by a method based on the included accessory minerals. In the common igneous rocks, most of the lead is concentrated in the potassium minerals, and most of the radioactivity is in the zircon and other accessory minerals. The lead in the potassium minerals is believed to be mostly primary lead; that in zircon is probably chiefly radiogenic lead. By separating the zircon of fresh igneous rocks, determining the amount of lead with the spectrograph and the radioactivity by alpha counters, the age of Paleozoic and Precambrian rocks can be determined with an accuracy of approximately 90 per cent. Basalts and gabbros may contain too few accessory minerals for satisfactory age determination by this method. Zircon is the most satisfactory mineral for this kind of determination. Apatite and sphene give high results and therefore must contain primary lead. Sphene gives erratic results.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1952)63[1045:MFDTAO]2.0.CO;2","usgsCitation":"Larsen, E., Keevil, N., and Harrison, C., 1952, Method for determining the age of igneous rocks using the accessory minerals: Geological Society of America Bulletin, v. 63, no. 10, p. 1045-1052, https://doi.org/10.1130/0016-7606(1952)63[1045:MFDTAO]2.0.CO;2.","productDescription":"8 p.","startPage":"1045","endPage":"1052","costCenters":[],"links":[{"id":386740,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"63","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Larsen, E.S.","contributorId":77130,"corporation":false,"usgs":true,"family":"Larsen","given":"E.S.","email":"","affiliations":[],"preferred":false,"id":818268,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Keevil, N.B.","contributorId":257511,"corporation":false,"usgs":false,"family":"Keevil","given":"N.B.","email":"","affiliations":[],"preferred":false,"id":818269,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harrison, C.","contributorId":260640,"corporation":false,"usgs":false,"family":"Harrison","given":"C.","email":"","affiliations":[],"preferred":false,"id":818270,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":37862,"text":"37862 - 1952 - Abstract of fur laws, 1952-53","interactions":[],"lastModifiedDate":"2014-07-22T09:39:18","indexId":"37862","displayToPublicDate":"1952-10-01T09:38:43","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"343","title":"Abstract of fur laws, 1952-53","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","usgsCitation":"Ashbrook, F.G., 1952, Abstract of fur laws, 1952-53 (Reissued from Wildlife Leaflet BS-118 (1938).): Wildlife Leaflet 343, 43 p.","productDescription":"43 p.","numberOfPages":"43","costCenters":[],"links":[{"id":290657,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Reissued from Wildlife Leaflet BS-118 (1938).","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd7c6e4b0824b2d177f2b","contributors":{"authors":[{"text":"Ashbrook, Frank G.","contributorId":77980,"corporation":false,"usgs":true,"family":"Ashbrook","given":"Frank","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":218613,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70205295,"text":"70205295 - 1952 - Phosphate mineralization at Bomi hill and Bambuta, Liberia, west Africa","interactions":[],"lastModifiedDate":"2019-09-13T10:54:18","indexId":"70205295","displayToPublicDate":"1952-09-12T08:22:46","publicationYear":"1952","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":738,"text":"American Mineralogist","active":true,"publicationSubtype":{"id":10}},"title":"Phosphate mineralization at Bomi hill and Bambuta, Liberia, west Africa","docAbstract":"Iron phosphate minerals which cement talus ore below cliffs formed by massive magnetite- hematite deposits at Bomi hill, Liberia, and also occur in place in fissures and caves in the ore both at Bomi hill and Bambuta, were formed by the interaction of bat dung and iron oxides. The minerals include leucophosphite (previously known only from Western Australia), phosphosiderite, and strengite. Analyses of the leucophosphite are included.
","issn":"19453027","usgsCitation":"Axelrod, J.M., Carron, M.K., and Thayer, T.P., 1952, Phosphate mineralization at Bomi hill and Bambuta, Liberia, west Africa: American Mineralogist, v. 37, no. 11-12, p. 883-909.","productDescription":"27 p. ","startPage":"883","endPage":"909","numberOfPages":"27","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":367376,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Liberia","otherGeospatial":"West Africa ","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -11.42578125,\n 5.943899579425587\n ],\n [\n -9.4482421875,\n 5.943899579425587\n ],\n [\n -9.4482421875,\n 7.040927423719928\n ],\n [\n -11.42578125,\n 7.040927423719928\n ],\n [\n -11.42578125,\n 5.943899579425587\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"37","issue":"11-12","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Axelrod, J. M.","contributorId":29796,"corporation":false,"usgs":true,"family":"Axelrod","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":770767,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carron, M. K.","contributorId":59492,"corporation":false,"usgs":true,"family":"Carron","given":"M.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":770768,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thayer, Thomas P","contributorId":218870,"corporation":false,"usgs":false,"family":"Thayer","given":"Thomas","email":"","middleInitial":"P","affiliations":[{"id":7198,"text":"Oregon Department Geology and Mineral Industries","active":true,"usgs":false},{"id":6605,"text":"USGS","active":true,"usgs":false}],"preferred":false,"id":770769,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70222246,"text":"70222246 - 1952 - Stratigraphy and structure of the Shaviovik and Canning Rivers area, Alaska","interactions":[],"lastModifiedDate":"2022-06-01T19:46:58.700534","indexId":"70222246","displayToPublicDate":"1952-09-01T13:39:01","publicationYear":"1952","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":"40","subseriesTitle":"Preliminary Report","title":"Stratigraphy and structure of the Shaviovik and Canning Rivers area, Alaska","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70222246","usgsCitation":"Keller, A.S., and Morris, R.H., 1952, Stratigraphy and structure of the Shaviovik and Canning Rivers area, Alaska: Geological Investigations, Naval Petroleum Reserve No. 4, Alaska 40, Report: 21 p.; 5 plates: 75.67 x 23.82 inches or smaller; 1 Supplement, https://doi.org/10.3133/70222246.","productDescription":"Report: 21 p.; 5 plates: 75.67 x 23.82 inches or smaller; 1 Supplement","costCenters":[],"links":[{"id":401595,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70222246/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":401594,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70222246/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":401593,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70222246/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":401592,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70222246/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":401591,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70222246/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":401590,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70222246/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":387354,"rank":1,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74589.htm","linkFileType":{"id":5,"text":"html"}},{"id":396967,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70222246/report-thumb.jpg"},{"id":401596,"rank":9,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/unnumbered/70222246/supplement.pdf","text":"Supplement","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Shaviovik and Canning Rivers area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -147.8333,\n 69.3333\n ],\n [\n -146,\n 69.3333\n ],\n [\n -146,\n 69.6833\n ],\n [\n -147.8333,\n 69.6833\n ],\n [\n -147.8333,\n 69.3333\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Keller, A. Samuel","contributorId":287142,"corporation":false,"usgs":false,"family":"Keller","given":"A.","email":"","middleInitial":"Samuel","affiliations":[],"preferred":false,"id":837681,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morris, Robert H.","contributorId":85269,"corporation":false,"usgs":true,"family":"Morris","given":"Robert","email":"","middleInitial":"H.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":837682,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":37850,"text":"37850 - 1952 - Availability of surplus big-game animals on National Wildlife Refuges","interactions":[],"lastModifiedDate":"2014-07-24T11:20:08","indexId":"37850","displayToPublicDate":"1952-09-01T11:19:41","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"341","title":"Availability of surplus big-game animals on National Wildlife Refuges","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","usgsCitation":"U.S. Fish and Wildlife Service, 1952, Availability of surplus big-game animals on National Wildlife Refuges (Supersedes Wildlife Leaflet 277 (1945).): Wildlife Leaflet 341, 6 p.","productDescription":"6 p.","numberOfPages":"6","costCenters":[],"links":[{"id":290892,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Supersedes Wildlife Leaflet 277 (1945).","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd7c6e4b0824b2d177f2d","contributors":{"authors":[{"text":"U.S. Fish and Wildlife Service","contributorId":128143,"corporation":true,"usgs":false,"organization":"U.S. Fish and Wildlife Service","id":529750,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":71932,"text":"tem354 - 1952 - Radon in the Dillon Tunnel in Miners' Basin, north La Sal Mountains, Grand County, Utah","interactions":[],"lastModifiedDate":"2014-07-16T11:07:01","indexId":"tem354","displayToPublicDate":"1952-09-01T11:04:45","publicationYear":"1952","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":"354","title":"Radon in the Dillon Tunnel in Miners' Basin, north La Sal Mountains, Grand County, Utah","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior, Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/tem354","collaboration":"Performed for the Division of Raw Materials of the U.S. Atomic Energy Commission.","usgsCitation":"Faul, H., 1952, Radon in the Dillon Tunnel in Miners' Basin, north La Sal Mountains, Grand County, Utah: U.S. Geological Survey Trace Elements Memorandum 354, 9 p., https://doi.org/10.3133/tem354.","productDescription":"9 p.","numberOfPages":"9","costCenters":[],"links":[{"id":290268,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Utah","county":"Grand County","otherGeospatial":"La Sal Mountains","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.1793,38.5 ], [ -110.1793,39.4998 ], [ -109.0508,39.4998 ], [ -109.0508,38.5 ], [ -110.1793,38.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c79f12e4b019484164249f","contributors":{"authors":[{"text":"Faul, Henry","contributorId":60234,"corporation":false,"usgs":true,"family":"Faul","given":"Henry","email":"","affiliations":[],"preferred":false,"id":284902,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221612,"text":"70221612 - 1952 - Correlation of the jurassic formations of North America, exclusive of Canada","interactions":[],"lastModifiedDate":"2021-06-25T13:59:16.945907","indexId":"70221612","displayToPublicDate":"1952-09-01T08:49:28","publicationYear":"1952","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":"Correlation of the jurassic formations of North America, exclusive of Canada","docAbstract":"No abstract available.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1952)63[953:COTJFO]2.0.CO;2","usgsCitation":"Imlay, R.W., 1952, Correlation of the jurassic formations of North America, exclusive of Canada: Geological Society of America Bulletin, v. 63, no. 9, p. 953-992, https://doi.org/10.1130/0016-7606(1952)63[953:COTJFO]2.0.CO;2.","productDescription":"40 p.","startPage":"953","endPage":"992","costCenters":[],"links":[{"id":386737,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -143.08593749999997,\n 48.922499263758255\n ],\n [\n -61.87499999999999,\n 48.922499263758255\n ],\n [\n -61.87499999999999,\n 71.41317683396566\n ],\n [\n -143.08593749999997,\n 71.41317683396566\n ],\n [\n -143.08593749999997,\n 48.922499263758255\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"63","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Imlay, Ralph W.","contributorId":40981,"corporation":false,"usgs":true,"family":"Imlay","given":"Ralph","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":818263,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70198446,"text":"70198446 - 1952 - The relation between the lowering of the piezometric surface and the rate and duration of discharge of a well using ground-water storage","interactions":[],"lastModifiedDate":"2018-08-07T09:29:20","indexId":"70198446","displayToPublicDate":"1952-08-03T07:53:04","publicationYear":"1952","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"The relation between the lowering of the piezometric surface and the rate and duration of discharge of a well using ground-water storage","docAbstract":"No abstract available
","conferenceTitle":"American Geophysical Union Transactions, 16th Annual Meeting","conferenceDate":"August 1952","conferenceLocation":"Washington, D.C.","language":"English","usgsCitation":"Theis, C.V., 1952, The relation between the lowering of the piezometric surface and the rate and duration of discharge of a well using ground-water storage, American Geophysical Union Transactions, 16th Annual Meeting, v. 16, no. 2, Washington, D.C., August 1952, p. 519-524.","productDescription":"6 p.","startPage":"519","endPage":"524","costCenters":[],"links":[{"id":356236,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":356126,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://water.usgs.gov/ogw/pubs/Theis-1935.pdf"}],"volume":"16","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Theis, Charles V.","contributorId":48080,"corporation":false,"usgs":true,"family":"Theis","given":"Charles","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":741484,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70217842,"text":"70217842 - 1952 - Discussion of “tide‐producing forces and artesian pressures”","interactions":[],"lastModifiedDate":"2021-02-05T18:44:33.420843","indexId":"70217842","displayToPublicDate":"1952-08-01T12:40:56","publicationYear":"1952","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":"Discussion of “tide‐producing forces and artesian pressures”","docAbstract":"I was an employee of the Texas State Board of Water Engineers in charge of the Fort Stockton field office at the time that the data for this paper were gathered. Since I have done both extensive and detailed ground‐water work in the Fort Stockton area, including the setting and maintaining of the water‐stage recorder at the Gonzales well, I believe I can add some pertinent hydrologic remarks about this paper.
The authors state that the principal water‐bearing formation is a limestone. This opinion is not shared by myself and most likely the majority of other geologists in this area. Adkins [1927] favored the basal Cretaceous sands as the principal source of water to Comanche Springs. I believe that the most extensive and the principal water‐bearing formation is a sand and sandstone. The crevices and channels reported in wells and exposed at the springs are only a localized condition resulting from structural weakness and solution caused by a high water surface. The piezometric surface in sand and crevice wells is essentially identical; this suggests that there exists but one principal aquifer in this area. W.N. White, former District Geologist in Texas for the U.S. Geological Survey, in a personal communication to me in 1948, reported Comanche Springs to be the most reliable springs in Texas. This reliable flow strongly supports the concept of a sand aquifer, whose catchment area, or source, is of vast and varied extent, and a great distance from its outlet.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR033i004p00597","usgsCitation":"Culbertson, T., George, W., and Romberg, F.E., 1952, Discussion of “tide‐producing forces and artesian pressures”: Eos, Transactions, American Geophysical Union, v. 33, no. 4, p. 597-600, https://doi.org/10.1029/TR033i004p00597.","productDescription":"4 p.","startPage":"597","endPage":"600","costCenters":[],"links":[{"id":383059,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"4","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Culbertson, Tom","contributorId":248797,"corporation":false,"usgs":false,"family":"Culbertson","given":"Tom","email":"","affiliations":[],"preferred":false,"id":809882,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"George, William O.","contributorId":106016,"corporation":false,"usgs":true,"family":"George","given":"William O.","affiliations":[],"preferred":false,"id":809883,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Romberg, Frederick E.","contributorId":248796,"corporation":false,"usgs":false,"family":"Romberg","given":"Frederick","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":809884,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70221614,"text":"70221614 - 1952 - Nonsteady flow to a well of constant drawdown in an extensive aquifer","interactions":[],"lastModifiedDate":"2021-06-26T11:10:30.966986","indexId":"70221614","displayToPublicDate":"1952-08-01T09:48:48","publicationYear":"1952","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":"Nonsteady flow to a well of constant drawdown in an extensive aquifer","docAbstract":"A mathematical theory is given for the discharge of a well of constant drawdown, discharging as by natural flow from an effectively infinite aquifer of uniform transmissibility and uniform compressibility. This theory is based on the solution by L. P. Smith of the analogous problem in heat conduction. The mathematical function involved in the solution, which cannot be integrated directly, is evaluated by numerical integration. A table of its values is given for a wide range of its argument. This function is compared with other,asymptotic solutions, and simple, useful approximations are given.
Two graphical methods are outlined for determining the coefficients of storage and transmissibility from variations in the rate of discharge of wells flowing at constant drawdown. Data from the Grand Junction, Colo., artesian basin are treated by these methods. In the Grand Junction artesian basin there are about 25 flowing wells ranging in depth from 600 to 1600 ft, most of which obtain water from the Entrada sandstone. A few of the wells obtain water from a sandstone in the overlying Morrison formation and a few tap the underlying Wingate sandstone.
The procedure of the tests is outlined, and the “ink-well” mercury gage used to measure the artesian pressures is described. Recovery tests were run on the same wells after the discharge tests. Values of transmissibility obtained from the recovery tests check those obtained by means of the discharge tests.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR033i004p00559","usgsCitation":"Jacob, C., and Lohman, S., 1952, Nonsteady flow to a well of constant drawdown in an extensive aquifer: Eos, Transactions, American Geophysical Union, v. 33, no. 4, p. 559-569, https://doi.org/10.1029/TR033i004p00559.","productDescription":"11 p.","startPage":"559","endPage":"569","costCenters":[],"links":[{"id":386770,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","city":"Grand Junction","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -108.8525390625,\n 38.831149809348744\n ],\n [\n -108.30322265624999,\n 38.831149809348744\n ],\n [\n -108.30322265624999,\n 39.257778150283364\n ],\n [\n -108.8525390625,\n 39.257778150283364\n ],\n [\n -108.8525390625,\n 38.831149809348744\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"33","issue":"4","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Jacob, C.E.","contributorId":260638,"corporation":false,"usgs":false,"family":"Jacob","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":818349,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lohman, S.W.","contributorId":260639,"corporation":false,"usgs":false,"family":"Lohman","given":"S.W.","email":"","affiliations":[],"preferred":false,"id":818350,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70221615,"text":"70221615 - 1952 - Nonsteady flow to a well of constant drawdown in an extensive aquifer","interactions":[],"lastModifiedDate":"2021-06-25T14:55:06.628535","indexId":"70221615","displayToPublicDate":"1952-08-01T09:48:48","publicationYear":"1952","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":"Nonsteady flow to a well of constant drawdown in an extensive aquifer","docAbstract":"A mathematical theory is given for the discharge of a well of constant drawdown, discharging as by natural flow from an effectively infinite aquifer of uniform transmissibility and uniform compressibility. This theory is based on the solution by L. P. Smith of the analogous problem in heat conduction. The mathematical function involved in the solution, which cannot be integrated directly, is evaluated by numerical integration. A table of its values is given for a wide range of its argument. This function is compared with other,asymptotic solutions, and simple, useful approximations are given.
Two graphical methods are outlined for determining the coefficients of storage and transmissibility from variations in the rate of discharge of wells flowing at constant drawdown. Data from the Grand Junction, Colo., artesian basin are treated by these methods. In the Grand Junction artesian basin there are about 25 flowing wells ranging in depth from 600 to 1600 ft, most of which obtain water from the Entrada sandstone. A few of the wells obtain water from a sandstone in the overlying Morrison formation and a few tap the underlying Wingate sandstone.
The procedure of the tests is outlined, and the “ink-well” mercury gage used to measure the artesian pressures is described. Recovery tests were run on the same wells after the discharge tests. Values of transmissibility obtained from the recovery tests check those obtained by means of the discharge tests.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR033i004p00559","usgsCitation":"Jacob, C., and Lohman, S., 1952, Nonsteady flow to a well of constant drawdown in an extensive aquifer: Eos, Transactions, American Geophysical Union, v. 33, no. 4, p. 559-569, https://doi.org/10.1029/TR033i004p00559.","productDescription":"11 p.","startPage":"559","endPage":"569","costCenters":[],"links":[{"id":386739,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","city":"Grand Junction","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -108.896484375,\n 38.92522904714054\n ],\n [\n -108.1494140625,\n 38.92522904714054\n ],\n [\n -108.1494140625,\n 39.27478966170308\n ],\n [\n -108.896484375,\n 39.27478966170308\n ],\n [\n -108.896484375,\n 38.92522904714054\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"33","issue":"4","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Jacob, C.E.","contributorId":260638,"corporation":false,"usgs":false,"family":"Jacob","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":818266,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lohman, S.W.","contributorId":260639,"corporation":false,"usgs":false,"family":"Lohman","given":"S.W.","email":"","affiliations":[],"preferred":false,"id":818267,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":71296,"text":"tei237 - 1952 - Origin of the Chattanooga shale","interactions":[],"lastModifiedDate":"2014-04-03T14:49:59","indexId":"tei237","displayToPublicDate":"1952-07-01T13:43:00","publicationYear":"1952","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":"237","title":"Origin of the Chattanooga shale","docAbstract":"Tonight I will try to present to you the chief facts we have observed that have a bearing on\nthe old problem of how the black shales originated. Some of the ideas have been used before, and\nsome are new. Some of those that have been used before, have been used to support arguments for\nboth shallow and deep water, yet I shall use them again and try to show why our use of them in support\nof shallow water is justified, and the other fellow's use of them in support of deep water is not justified.
\nThese conclusions are strictly our own. Early in our studies we gave serious consideration to\ndeep-water possibilities, but always we ran into such highly improbable circumstances and implications\nthat we were forced to abandon them. The shallow-water theory seems to encounter no such formidable\nobstacles. We know of no facts that are incompatible with a shallow-water theory; we think that all\nknown facts lend themselves to such an explanation; and we believe that a shallow-water explanation of\nthese black shales is the simpler and sounder of the alternatives.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/tei237","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Conant, L.C., 1952, Origin of the Chattanooga shale: U.S. Geological Survey Trace Elements Investigations 237, 23 p., https://doi.org/10.3133/tei237.","productDescription":"23 p.","costCenters":[],"links":[{"id":283950,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei237.png"},{"id":285624,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0237/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"535594e6e4b0120853e8c0c1","contributors":{"authors":[{"text":"Conant, Louis C.","contributorId":83921,"corporation":false,"usgs":true,"family":"Conant","given":"Louis","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":283955,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5220490,"text":"5220490 - 1952 - The foods of fur animals of the Patuxent Research Refuge, Maryland","interactions":[],"lastModifiedDate":"2023-02-16T17:18:16.886243","indexId":"5220490","displayToPublicDate":"1952-07-01T12:18:20","publicationYear":"1952","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":737,"text":"American Midland Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"The foods of fur animals of the Patuxent Research Refuge, Maryland","docAbstract":"Patterns formed by the networks of furrows separating the natural mounds of pimpled plains in eastern Oklahoma are regarded as attributable to shrinkage-polygon systems of coarse texture comparable to those occurring (1) in mound-studded parts of the northwestern United States that are underlain by vertically jointed basalt, (2) in tracts of Alaskan tundra that are occupied by ice-wedge networks, and (3) in beds of playa lakes in the arid southwest that are cut by systems of giant desiccation fissures. While the inter-mound furrow networks characteristic of pimpled plains in the mid-continent region may owe their origin to former frigid climatic conditions, one of a number of alternative possibilities is that the peculiar configuration of these surfaces, as exemplified in eastern Oklahoma, has resulted from erosion of systems of giant soil polygons caused by desiccation. The time of origin of the pimpled plains of eastern Oklahoma is believed to have been not earlier than late Pleistocene.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1952)63[689:PPOEO]2.0.CO;2","usgsCitation":"Knechtel, M., 1952, Pimpled plains of Eastern Oklahoma: Geological Society of America Bulletin, v. 63, no. 7, p. 689-700, https://doi.org/10.1130/0016-7606(1952)63[689:PPOEO]2.0.CO;2.","productDescription":"12 p.","startPage":"689","endPage":"700","costCenters":[],"links":[{"id":386728,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oklahoma","otherGeospatial":"Eastern Oklahoma","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -98.12988281249999,\n 35.209721645221386\n ],\n [\n -94.74609374999999,\n 35.209721645221386\n ],\n [\n -94.74609374999999,\n 36.94989178681327\n ],\n [\n -98.12988281249999,\n 36.94989178681327\n ],\n [\n -98.12988281249999,\n 35.209721645221386\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"63","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Knechtel, M. M.","contributorId":72354,"corporation":false,"usgs":true,"family":"Knechtel","given":"M. M.","affiliations":[],"preferred":false,"id":818258,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011123,"text":"70011123 - 1952 - Identification and lead-uranium ages of massive uraninites from the Shinarump conglomerate, Utah","interactions":[],"lastModifiedDate":"2026-03-10T16:48:44.227747","indexId":"70011123","displayToPublicDate":"1952-06-27T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Identification and lead-uranium ages of massive uraninites from the Shinarump conglomerate, Utah","docAbstract":"No abstract available.
","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.115.3000.706","issn":"00368075","usgsCitation":"Stieff, L.R., and Stern, T.W., 1952, Identification and lead-uranium ages of massive uraninites from the Shinarump conglomerate, Utah: Science, v. 115, no. 3000, p. 706-708, https://doi.org/10.1126/science.115.3000.706.","productDescription":"3 p.","startPage":"706","endPage":"708","costCenters":[],"links":[{"id":221730,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"southeastern Utah","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.61560058593749,\n 37.00255267215955\n ],\n [\n -109.039306640625,\n 37.00255267215955\n ],\n [\n -109.039306640625,\n 38.56105262446978\n ],\n [\n -111.61560058593749,\n 38.56105262446978\n ],\n [\n -111.61560058593749,\n 37.00255267215955\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"115","issue":"3000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3810e4b0c8380cd613f6","contributors":{"authors":[{"text":"Stieff, L. R.","contributorId":25619,"corporation":false,"usgs":true,"family":"Stieff","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":360330,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stern, T. W.","contributorId":36122,"corporation":false,"usgs":true,"family":"Stern","given":"T.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":360331,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70096345,"text":"tei232 - 1952 - Reconnaissance of uranium and copper deposits in parts of New Mexico, Colorado, Utah, Idaho, and Wyoming","interactions":[],"lastModifiedDate":"2014-06-06T08:04:48","indexId":"tei232","displayToPublicDate":"1952-06-01T13:34:00","publicationYear":"1952","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":"232","title":"Reconnaissance of uranium and copper deposits in parts of New Mexico, Colorado, Utah, Idaho, and Wyoming","docAbstract":"Because of the common association of uranium and copper in several of the commercial uranium deposits in the Colorado Plateau Province, a reconnaissance was made of several known deposits of copper disseminated through sandstone to determine whether they might be a source of uranium. In order to obtain more information regarding the relationship between copper, uranium and carbonaceous materials, some of the uraniferious asphaltrite deposits in the Shinarump conglomerate along the west flank of the San Rafael Swell were also investigated briefly.
\nDuring this reconnaissance 18 deposits were examined in New Mexico, eight in Utah, two in Idaho, and one each in Wyoming and Colorado.
\nNo uranium deposits of commercial grade are associated with the copper deposits that were examined. The uraniferous asphaltites in the Shinarump conglomerate of Triassic age on the west flank of the San Rafael Swell, however, are promising from the standpoint of commercial uranium production.
\nSpectrographic analyses of crude oil, asphalt, and bituminous shales show a rather consistent suite of trace metals including vanadium, nickel, copper, cobalt, chromium, lead zinc, and molybdenum. The similarity of the metal assemblage, including uranium of the San Rafael Swell asphaltites, to the metal assemblage in crude oil and other bituminous materials suggests that these metals were concentrated in the asphaltites from petroleum. However, the hypothesis that uranium minerals were already present before the hydrocarbons were introduced and that some sort of replacement or uranium minerals by carbon compounds was effected after the petroleum migrated into the uranium deposit should not be disregarded.
\nThe widespread association of uranium with asphaltic material suggests that it also may have been concentrated by some agency connected with the formation of petroleum. The problem of the association of uranium and other trace metals with hydrocarbons should be studied further both in the field and in the laboratory.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/tei232","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Gott, G.B., and Erickson, R., 1952, Reconnaissance of uranium and copper deposits in parts of New Mexico, Colorado, Utah, Idaho, and Wyoming: U.S. Geological Survey Trace Elements Investigations 232, 34 p., https://doi.org/10.3133/tei232.","productDescription":"34 p.","costCenters":[],"links":[{"id":283949,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei232.png"},{"id":285623,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0232/report.pdf"}],"country":"United States","state":"Colorado;Idaho;New Mexico;Utah;Wyoming","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114,34.0 ], [ -114,43.0 ], [ -104,43.0 ], [ -104,34.0 ], [ -114,34.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5355955ce4b0120853e8c1a5","contributors":{"authors":[{"text":"Gott, Garland B.","contributorId":8837,"corporation":false,"usgs":true,"family":"Gott","given":"Garland","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":491505,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Erickson, Ralph L.","contributorId":51599,"corporation":false,"usgs":true,"family":"Erickson","given":"Ralph L.","affiliations":[],"preferred":false,"id":491506,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70221527,"text":"70221527 - 1952 - \"How to write geologese\"; Discussion","interactions":[],"lastModifiedDate":"2021-06-21T18:29:57.563037","indexId":"70221527","displayToPublicDate":"1952-06-01T13:27:57","publicationYear":"1952","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"\"How to write geologese\"; Discussion","docAbstract":"No abstract available.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.47.4.460","usgsCitation":"Calkins, F.C., 1952, \"How to write geologese\"; Discussion: Economic Geology, v. 47, no. 4, p. 460-461, https://doi.org/10.2113/gsecongeo.47.4.460.","productDescription":"2 p.","startPage":"460","endPage":"461","costCenters":[],"links":[{"id":386623,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"47","issue":"4","noUsgsAuthors":false,"publicationDate":"1952-06-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Calkins, F. C.","contributorId":55402,"corporation":false,"usgs":true,"family":"Calkins","given":"F.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":817937,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":71925,"text":"tem355 - 1952 - Reconnaissance for a uranothorianite-bearing lode in the vicinity of the headwaters of the Peace River, Candle Quadrangle, Seward Peninsula, Alaska","interactions":[],"lastModifiedDate":"2014-07-16T10:48:36","indexId":"tem355","displayToPublicDate":"1952-06-01T10:45:54","publicationYear":"1952","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":"355","title":"Reconnaissance for a uranothorianite-bearing lode in the vicinity of the headwaters of the Peace River, Candle Quadrangle, Seward Peninsula, Alaska","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior, Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/tem355","collaboration":"Performed for the Division of Raw Materials of the U.S. Atomic Energy Commission.","usgsCitation":"West, W.S., 1952, Reconnaissance for a uranothorianite-bearing lode in the vicinity of the headwaters of the Peace River, Candle Quadrangle, Seward Peninsula, Alaska: U.S. Geological Survey Trace Elements Memorandum 355, 12 p., https://doi.org/10.3133/tem355.","productDescription":"12 p.","numberOfPages":"12","costCenters":[],"links":[{"id":290265,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Peace River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -167.7249,64.4795 ], [ -167.7249,66.4404 ], [ -159.491,66.4404 ], [ -159.491,64.4795 ], [ -167.7249,64.4795 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c79f13e4b01948416424a3","contributors":{"authors":[{"text":"West, Walter Scott","contributorId":30095,"corporation":false,"usgs":true,"family":"West","given":"Walter","email":"","middleInitial":"Scott","affiliations":[],"preferred":false,"id":284901,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221559,"text":"70221559 - 1952 - Report of the Committee on Land Erosion, 1950–1951","interactions":[],"lastModifiedDate":"2021-06-22T14:33:11.468201","indexId":"70221559","displayToPublicDate":"1952-06-01T09:26:39","publicationYear":"1952","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":"Report of the Committee on Land Erosion, 1950–1951","docAbstract":"Activities of the Committee on Land Erosion, since the present Committee was appointed in September, 1950, have been confined mainly to correspondence among members as a means of becoming better acquainted and of deciding on a suitable program for consideration of the Committee Erosion being such a far-flung and complex phenomenon defies any small group to consider all of its many facets. It is obvious, therefore, that greatest practical results would be obtained if Committee activities were confined in the main to those investigations in which members are currently engaged.
Colman and Sinclair state that one of their chief current interests is the study of possibilities for decreasing creep on steep mountain slopes in Southern California. They have reason to believe that a considerable part (the precise amount being unknown) of the debris issuing from the canyons starts its way to channels as dry sliding or other type of soil movement that takes place during the dry seasons although the actual damage occurs during wet periods. Initially they hope to obtain more information on channel accumulations and to learn more about where the material comes from and how and when it moves to the channel. With this information they expect to be in a better position to study means of decreasing debris movement. The importance of debris movement into the densely populated valleys of Southern California is of such an order that additional planning along these lines can be well justified.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR033i003p00450","usgsCitation":"Peterson, H., 1952, Report of the Committee on Land Erosion, 1950–1951: Eos, Transactions, American Geophysical Union, v. 33, no. 3, p. 450-452, https://doi.org/10.1029/TR033i003p00450.","productDescription":"3 p.","startPage":"450","endPage":"452","costCenters":[],"links":[{"id":386649,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"southern California","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -114.12597656249999,\n 34.19817309627726\n ],\n [\n -114.7412109375,\n 35.137879119634185\n ],\n [\n -117.68554687499999,\n 37.33522435930639\n ],\n [\n -121.904296875,\n 36.27970720524017\n ],\n [\n -120.5419921875,\n 34.45221847282654\n ],\n [\n -117.0703125,\n 32.509761735919426\n ],\n [\n -114.82910156249999,\n 32.731840896865684\n ],\n [\n -114.521484375,\n 32.80574473290688\n ],\n [\n -114.12597656249999,\n 34.19817309627726\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"33","issue":"3","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Peterson, H.V.","contributorId":86007,"corporation":false,"usgs":true,"family":"Peterson","given":"H.V.","email":"","affiliations":[],"preferred":false,"id":818051,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011110,"text":"70011110 - 1952 - Effect of wind-generated waves on migration of the Yukon River in the Yukon Flats, Alaska","interactions":[],"lastModifiedDate":"2026-03-10T16:57:56.681824","indexId":"70011110","displayToPublicDate":"1952-05-09T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Effect of wind-generated waves on migration of the Yukon River in the Yukon Flats, Alaska","docAbstract":"No abstract available.
","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.115.2993.519","issn":"00368075","usgsCitation":"Williams, J., 1952, Effect of wind-generated waves on migration of the Yukon River in the Yukon Flats, Alaska: Science, v. 115, no. 2993, p. 519-520, https://doi.org/10.1126/science.115.2993.519.","productDescription":"2 p.","startPage":"519","endPage":"520","costCenters":[],"links":[{"id":221571,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"east-central Alaska, Yukon Flats, Yukon River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -150.33749189864903,\n 66.88609719216143\n ],\n [\n -150.33749189864903,\n 65.10704282973526\n ],\n [\n -143.69564163643955,\n 65.10704282973526\n ],\n [\n -143.69564163643955,\n 66.88609719216143\n ],\n [\n -150.33749189864903,\n 66.88609719216143\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"115","issue":"2993","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a062fe4b0c8380cd5113d","contributors":{"authors":[{"text":"Williams, John R.","contributorId":41832,"corporation":false,"usgs":true,"family":"Williams","given":"John R.","affiliations":[],"preferred":false,"id":360300,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":37849,"text":"37849 - 1952 - Pocket gopher control","interactions":[],"lastModifiedDate":"2014-07-24T11:15:23","indexId":"37849","displayToPublicDate":"1952-05-01T11:13:49","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"340","title":"Pocket gopher control","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","usgsCitation":"U.S. Fish and Wildlife, 1952, Pocket gopher control: Wildlife Leaflet 340, 6 p.","productDescription":"6 p.","numberOfPages":"6","costCenters":[],"links":[{"id":290891,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd7c6e4b0824b2d177f2f","contributors":{"authors":[{"text":"U.S. Fish and Wildlife","contributorId":128089,"corporation":true,"usgs":false,"organization":"U.S. Fish and Wildlife","id":529749,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5220691,"text":"5220691 - 1952 - Sex ratios in pheasant research and management","interactions":[],"lastModifiedDate":"2025-01-29T16:36:04.636332","indexId":"5220691","displayToPublicDate":"1952-04-04T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Sex ratios in pheasant research and management","docAbstract":"No abstract available.
","language":"English","publisher":"Wiley","doi":"10.2307/3796924","usgsCitation":"Dale, F.H., 1952, Sex ratios in pheasant research and management: Journal of Wildlife Management, v. 16, no. 2, p. 156-163, https://doi.org/10.2307/3796924.","productDescription":"8 p.","startPage":"156","endPage":"163","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":487080,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2307/3796924","text":"Publisher Index Page"},{"id":197847,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wisconsin","county":"Green County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-89.8377,42.8598],[-89.7196,42.8587],[-89.6026,42.8575],[-89.4832,42.858],[-89.3688,42.8575],[-89.3689,42.8484],[-89.3677,42.7743],[-89.3671,42.7607],[-89.3666,42.6906],[-89.3667,42.677],[-89.3656,42.5998],[-89.3656,42.5907],[-89.3645,42.5029],[-89.4018,42.503],[-89.4031,42.503],[-89.4537,42.5038],[-89.4883,42.5044],[-89.5693,42.5057],[-89.6811,42.5074],[-89.803,42.5077],[-89.8379,42.5076],[-89.8377,42.5975],[-89.8375,42.6857],[-89.8373,42.7735],[-89.8375,42.8135],[-89.8377,42.8598]]]},\"properties\":{\"name\":\"Green\",\"state\":\"WI\"}}]}","volume":"16","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4c0b","contributors":{"authors":[{"text":"Dale, Fred H.","contributorId":70698,"corporation":false,"usgs":true,"family":"Dale","given":"Fred","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":332239,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}