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,{"id":69260,"text":"coal32 - 1955 - Preliminary geologic map of the Kirtland quadrangle, San Juan County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-10T00:11:23","indexId":"coal32","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":309,"text":"Coal Map","code":"COAL","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"32","title":"Preliminary geologic map of the Kirtland quadrangle, San Juan County, New Mexico","language":"ENGLISH","doi":"10.3133/coal32","isbn":"0607758759","usgsCitation":"Beaumont, E.C., and O'Sullivan, R., 1955, Preliminary geologic map of the Kirtland quadrangle, San Juan County, New Mexico: U.S. Geological Survey Coal Map 32, 1 map., https://doi.org/10.3133/coal32.","productDescription":"1 map.","costCenters":[],"links":[{"id":111053,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_19585.htm","linkFileType":{"id":5,"text":"html"},"description":"19585"},{"id":115580,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/coal/032/report.pdf","size":"32","linkFileType":{"id":1,"text":"pdf"}},{"id":115581,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/coal/032/plate-1.pdf","size":"9253","linkFileType":{"id":1,"text":"pdf"}},{"id":188265,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/coal/032/report-thumb.jpg"}],"scale":"63360","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.75,36.25 ], [ -108.75,36.75 ], [ -108.25,36.75 ], [ -108.25,36.25 ], [ -108.75,36.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b1c6","contributors":{"authors":[{"text":"Beaumont, E. C.","contributorId":69631,"corporation":false,"usgs":true,"family":"Beaumont","given":"E.","middleInitial":"C.","affiliations":[],"preferred":false,"id":279903,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O'Sullivan, Robert Brett","contributorId":26695,"corporation":false,"usgs":true,"family":"O'Sullivan","given":"Robert Brett","affiliations":[],"preferred":false,"id":279902,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":15585,"text":"ofr55145 - 1955 - Geology of the Fourmile pegmatite area, Custer County, South Dakota","interactions":[{"subject":{"id":15585,"text":"ofr55145 - 1955 - Geology of the Fourmile pegmatite area, Custer County, South Dakota","indexId":"ofr55145","publicationYear":"1955","noYear":false,"title":"Geology of the Fourmile pegmatite area, Custer County, South Dakota"},"predicate":"SUPERSEDED_BY","object":{"id":39086,"text":"pp297D - 1963 - Geology and pegmatites of the Fourmile quadrangle, Black Hills, South Dakota","indexId":"pp297D","publicationYear":"1963","noYear":false,"chapter":"D","title":"Geology and pegmatites of the Fourmile quadrangle, Black Hills, South Dakota"},"id":1}],"supersededBy":{"id":39086,"text":"pp297D - 1963 - Geology and pegmatites of the Fourmile quadrangle, Black Hills, South Dakota","indexId":"pp297D","publicationYear":"1963","noYear":false,"title":"Geology and pegmatites of the Fourmile quadrangle, Black Hills, South Dakota"},"lastModifiedDate":"2025-08-08T16:48:35.305634","indexId":"ofr55145","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"55-145","title":"Geology of the Fourmile pegmatite area, Custer County, South Dakota","docAbstract":"<p>The Fournile pegmatite area covers 32 sq. mi. in the western part of the Custer pegmatite mining district, Custer County, South Dakota. This area has been one of the major sources of sheet mica in the United States, especially between 1906 and 1911, and it has been a significant source of potash-feldspar, beryl and spodumene.</p><p>The area is part of the much larger area of pegmatites and metamorphic rocks to the north and east that surround Harney Peak and extend throughout the southern part of the pre-Cambrian core of the Black Hills. Paleozoic rocks underlie the western part of the Fourmile area.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr55145","usgsCitation":"Redden, J.A., 1955, Geology of the Fourmile pegmatite area, Custer County, South Dakota: U.S. Geological Survey Open-File Report 55-145, Report: 231 p.; 1 Plate: 32.82 x 50.76 inches; 7 Figures: 23.52 x 23.44 or smaller, https://doi.org/10.3133/ofr55145.","productDescription":"Report: 231 p.; 1 Plate: 32.82 x 50.76 inches; 7 Figures: 23.52 x 23.44 or smaller","costCenters":[],"links":[{"id":493877,"rank":10,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1955/0145/figure-1.pdf","text":"Figure 1","linkFileType":{"id":1,"text":"pdf"}},{"id":493875,"rank":8,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1955/0145/figure-14.pdf","text":"Figure 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,{"id":14428,"text":"ofr5581 - 1955 - Geology of the Du Noir area, Fremont County, Wyoming","interactions":[],"lastModifiedDate":"2025-07-17T17:36:08.467269","indexId":"ofr5581","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"55-81","title":"Geology of the Du Noir area, Fremont County, Wyoming","docAbstract":"<p>The Du Noir area includes about 250 square miles in the northwestern part of the Wind River Basin, Fremont County, Wyoming. It is bounded on the south by the Wind River and Warm Spring Creek, which flow along the northeast flank of the Wind River Mountains, and on the north by the steep scarps of the southern margin of the Absaroka Mountains. Rugged mountainous terrain dominates both the southwest and northern portions of the mapped area while badland topography and deeply dissected upland surfaces characterize the central part. One of the most significant physiographic and structural features of the region is a belt of folded and faulted Paleozoic and Mesozoic rocks, referred to as the Washakie Range, which lies along the southern margin of the Absaroka Mountains. These highlands, attaining elevations of es much as 10,000 feet, were buried by Tertiary volcanic debris and subsequently partly exhumed as the Wind River Basin was reexcavated by Wind River and its tributaries.</p><p>The sedimentary rocks exposed in the Du Noir area are more than 12,500 feet thick and range in age from Cambrian to Recent. All systems, with the exception of the Silurian, are represented. Precambrian granite and granite gneiss are present in both the Wind River and Washakie Ranges.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5581","usgsCitation":"Keefer, W.R., 1955, Geology of the Du Noir area, Fremont County, Wyoming: U.S. Geological Survey Open-File Report 55-81, Report: 235 p.; 2 Figures: 16.00 x 12.95 inches and 14.76 x 18.09 inches; 8 Plates: 32.84 x 37.91 inches, https://doi.org/10.3133/ofr5581.","productDescription":"Report: 235 p.; 2 Figures: 16.00 x 12.95 inches and 14.76 x 18.09 inches; 8 Plates: 32.84 x 37.91 inches","costCenters":[],"links":[{"id":492434,"rank":12,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1955/0081/figure-2.pdf","text":"Figure 2","linkFileType":{"id":1,"text":"pdf"}},{"id":492433,"rank":11,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1955/0081/figure-25.pdf","text":"Figure 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,{"id":71549,"text":"tei523 - 1955 - Age determinations on New Hampshire granites","interactions":[],"lastModifiedDate":"2012-02-02T00:13:44","indexId":"tei523","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"523","title":"Age determinations on New Hampshire granites","language":"ENGLISH","doi":"10.3133/tei523","usgsCitation":"Lyons, J.B., Gottfried, D., Smith, W., Jaffe, H., and Waring, C.L., 1955, Age determinations on New Hampshire granites: U.S. Geological Survey Trace Elements Investigations 523, 23 p., https://doi.org/10.3133/tei523.","productDescription":"23 p.","costCenters":[],"links":[{"id":185980,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/523/report-thumb.jpg"},{"id":90826,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/523/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db689394","contributors":{"authors":[{"text":"Lyons, John B.","contributorId":68801,"corporation":false,"usgs":true,"family":"Lyons","given":"John","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":284367,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gottfried, D.","contributorId":92346,"corporation":false,"usgs":true,"family":"Gottfried","given":"D.","email":"","affiliations":[],"preferred":false,"id":284369,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, W.L.","contributorId":78407,"corporation":false,"usgs":true,"family":"Smith","given":"W.L.","email":"","affiliations":[],"preferred":false,"id":284368,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jaffe, H.W.","contributorId":62682,"corporation":false,"usgs":true,"family":"Jaffe","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":284366,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Waring, C. L.","contributorId":96355,"corporation":false,"usgs":true,"family":"Waring","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":284370,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":71528,"text":"tei502 - 1955 - A spectrographic method for determining the hafnium-zirconium ratio in zircon","interactions":[],"lastModifiedDate":"2012-02-02T00:14:04","indexId":"tei502","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"502","title":"A spectrographic method for determining the hafnium-zirconium ratio in zircon","language":"ENGLISH","doi":"10.3133/tei502","usgsCitation":"Waring, C.L., and Worthing, H., 1955, A spectrographic method for determining the hafnium-zirconium ratio in zircon: U.S. Geological Survey Trace Elements Investigations 502, 15 p. : ill. ; 27 cm., https://doi.org/10.3133/tei502.","productDescription":"15 p. : ill. ; 27 cm.","costCenters":[],"links":[{"id":192709,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/502/report-thumb.jpg"},{"id":90793,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/502/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a6361","contributors":{"authors":[{"text":"Waring, C. L.","contributorId":96355,"corporation":false,"usgs":true,"family":"Waring","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":284328,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Worthing, H.W.","contributorId":13104,"corporation":false,"usgs":true,"family":"Worthing","given":"H.W.","affiliations":[],"preferred":false,"id":284327,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":71567,"text":"tei543 - 1955 - The spectrophotometric determination of vanadium as thiocyanate in acetone-water medium","interactions":[],"lastModifiedDate":"2012-02-02T00:13:44","indexId":"tei543","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"543","title":"The spectrophotometric determination of vanadium as thiocyanate in acetone-water medium","language":"ENGLISH","doi":"10.3133/tei543","usgsCitation":"Feinstein, H., 1955, The spectrophotometric determination of vanadium as thiocyanate in acetone-water medium: U.S. Geological Survey Trace Elements Investigations 543, 11 p., 3 fig., https://doi.org/10.3133/tei543.","productDescription":"11 p., 3 fig.","costCenters":[],"links":[{"id":186632,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/543/report-thumb.jpg"},{"id":90840,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/543/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db636028","contributors":{"authors":[{"text":"Feinstein, H.I.","contributorId":61102,"corporation":false,"usgs":true,"family":"Feinstein","given":"H.I.","email":"","affiliations":[],"preferred":false,"id":284403,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71564,"text":"tei538 - 1955 - Coffinite, a uranous silicate with hydroxyl substitution : a new mineral","interactions":[],"lastModifiedDate":"2012-02-02T00:13:44","indexId":"tei538","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"538","title":"Coffinite, a uranous silicate with hydroxyl substitution : a new mineral","language":"ENGLISH","doi":"10.3133/tei538","usgsCitation":"Stieff, L.R., Stern, T.W., and Sherwood, A., 1955, Coffinite, a uranous silicate with hydroxyl substitution : a new mineral: U.S. Geological Survey Trace Elements Investigations 538, 22 p., 1 fig., https://doi.org/10.3133/tei538.","productDescription":"22 p., 1 fig.","costCenters":[],"links":[{"id":186069,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/538/report-thumb.jpg"},{"id":90837,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/538/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae97a","contributors":{"authors":[{"text":"Stieff, Lorin Rollins","contributorId":46509,"corporation":false,"usgs":true,"family":"Stieff","given":"Lorin","email":"","middleInitial":"Rollins","affiliations":[],"preferred":false,"id":284399,"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":284398,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sherwood, A.M.","contributorId":25987,"corporation":false,"usgs":true,"family":"Sherwood","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":284397,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":39726,"text":"pp260R - 1955 - Bikini and nearby atolls, Marshall Islands; physical oceanography in the Marshall Islands area","interactions":[],"lastModifiedDate":"2012-02-02T00:10:17","indexId":"pp260R","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"260","chapter":"R","title":"Bikini and nearby atolls, Marshall Islands; physical oceanography in the Marshall Islands area","language":"ENGLISH","doi":"10.3133/pp260R","usgsCitation":"Mao, H., and Yoshida, K., 1955, Bikini and nearby atolls, Marshall Islands; physical oceanography in the Marshall Islands area: U.S. Geological Survey Professional Paper 260, p. 645-684 : ill. ; 29 cm., https://doi.org/10.3133/pp260R.","productDescription":"p. 645-684 : ill. ; 29 cm.","costCenters":[],"links":[{"id":120449,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0260r/report-thumb.jpg"},{"id":67489,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0260r/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db625f48","contributors":{"authors":[{"text":"Mao, Han-Lee","contributorId":75612,"corporation":false,"usgs":true,"family":"Mao","given":"Han-Lee","email":"","affiliations":[],"preferred":false,"id":222044,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yoshida, Kozo","contributorId":32590,"corporation":false,"usgs":true,"family":"Yoshida","given":"Kozo","email":"","affiliations":[],"preferred":false,"id":222043,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":71527,"text":"tei501 - 1955 - A colloidal method for the concentration of carbonaceous matter from rocks","interactions":[],"lastModifiedDate":"2012-02-02T00:14:04","indexId":"tei501","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"501","title":"A colloidal method for the concentration of carbonaceous matter from rocks","language":"ENGLISH","doi":"10.3133/tei501","usgsCitation":"Deul, M., 1955, A colloidal method for the concentration of carbonaceous matter from rocks: U.S. Geological Survey Trace Elements Investigations 501, 21 p. : ill. ; 28 cm., https://doi.org/10.3133/tei501.","productDescription":"21 p. : ill. ; 28 cm.","costCenters":[],"links":[{"id":192708,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/501/report-thumb.jpg"},{"id":90792,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/501/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd498be4b0b290850ef448","contributors":{"authors":[{"text":"Deul, Maurice","contributorId":67562,"corporation":false,"usgs":true,"family":"Deul","given":"Maurice","email":"","affiliations":[],"preferred":false,"id":284326,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71534,"text":"tei508 - 1955 - The mineral composition of gummite","interactions":[],"lastModifiedDate":"2012-02-02T00:14:05","indexId":"tei508","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"508","title":"The mineral composition of gummite","language":"ENGLISH","doi":"10.3133/tei508","usgsCitation":"Frondel, C., 1955, The mineral composition of gummite: U.S. Geological Survey Trace Elements Investigations 508, 54 p., https://doi.org/10.3133/tei508.","productDescription":"54 p.","costCenters":[],"links":[{"id":193233,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/508/report-thumb.jpg"},{"id":90799,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/508/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db649f8b","contributors":{"authors":[{"text":"Frondel, Clifford","contributorId":47002,"corporation":false,"usgs":true,"family":"Frondel","given":"Clifford","email":"","affiliations":[],"preferred":false,"id":284342,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71597,"text":"tei573 - 1955 - Radioactivity and uranium content of the Sharon Springs member of the Pierre shale and associated rocks in western Kansas and eastern Colorado","interactions":[],"lastModifiedDate":"2014-06-19T06:43:00","indexId":"tei573","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"573","title":"Radioactivity and uranium content of the Sharon Springs member of the Pierre shale and associated rocks in western Kansas and eastern Colorado","docAbstract":"<p>As a part of the Geological Survey's program of investigating uranium-bearing carbonaceous rocks on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission, a reconnaissance of the Sharon Springs member of the Pierre shale in western Kansas and eastern Colorado was conducted during 1954.</p>\n<br/>\n<p>The Sharon Springs member of the Pierre shale and its lateral equivalents ranges from 155 to about 500 feet in thickness and generally contains about 0.001 percent uranium, but some beds contain larger amounts. A 6-foot thick shale bed in Cheyenne County, Colo., contains about 0.006 percent uranium, a 4 1/2-foot thick sequence of beds in Crowley County, Colo., is estimated to contain between 0.004 and 0.005 percent uranium, and a 3 1/2-foot thick sequence of beds in Kiowa County, Colo., contains about 0.004 percent uranium. At several outcrop localities, sequences of beds as much as 9 1/2 feet thick contain about 0.003 percent uranium. Data from wells indicate that the 4 1/2-foot thick sequence of beds in Crowley County, Colo., may have a lateral extent of at least 5 1/2 miles. A gamma-ray log of a well in Yuma County, Colo., indicates the presence of a sequence of beds 66 feet thick which contains 0.005 to 0.010 percent equivalent uranium.</p>\n<br/>\n<p>No definite pattern of areal distribution of radioactivity and uranium content in the Sharon Springs is indicated by available data. Lateral variation in uranium content of individual beds was not noted in outcrops, which seldom extend more than 150 feet, but subsurface data from gamma-ray logs of wells indicate that both the maximum radioactivity and the thickness of radioactive beds are variable within distances of a few miles. Vertical variation in radioactivity and uranium content of the more radioactive beds is usually abrupt, but in the rocks as a whole the range of uranium content is so small that large variations in content are absent.</p>\n<br/>\n<p>In most of the gamma-ray logs examined there is only part of the sequence of rocks comprising the Pierre shale and Niobrara formation that exhibits radioactivity in excess of the average radioactivity of the two formations. Comparison of features of gamma-ray logs of wells in north-eastern Colorado suggests that the most radioactive part referred to above is a laterally correlatable sequence of beds.</p>\n<br/>\n<p>The stratigraphic position of the radioactive unit relative to the Pierre shale-Niobrara formation contact in oil industry scout reports, as identified from electric logs and wells, is variable within short distances. This may indicate that some of the Pierre-Niobrara contacts picked from electric logs may not correspond to the boundary that would be selected by examination of the rocks themselves, or may indicate that there is a facies relationship between teh lowermost part of the Pierre shale and the uppermost part of the Niobrara formation.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei573","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission.","usgsCitation":"Landis, E.R., 1955, Radioactivity and uranium content of the Sharon Springs member of the Pierre shale and associated rocks in western Kansas and eastern Colorado: U.S. Geological Survey Trace Elements Investigations 573, Report: 38 p.; 3 Plates: 15.59 x 23.75 inches or smaller, https://doi.org/10.3133/tei573.","productDescription":"Report: 38 p.; 3 Plates: 15.59 x 23.75 inches or smaller","numberOfPages":"39","onlineOnly":"Y","costCenters":[],"links":[{"id":288861,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0573/figure-4.pdf"},{"id":288862,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0573/report.pdf"},{"id":288863,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":288859,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0573/figure-2.pdf"},{"id":288860,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0573/figure-3.pdf"}],"country":"United States","state":"Colorado;Kansas","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.1551,36.9927 ], [ -105.1551,39.135518 ], [ -100.811628,39.135518 ], [ -100.811628,36.9927 ], [ -105.1551,36.9927 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db649d5d","contributors":{"authors":[{"text":"Landis, Edwin R.","contributorId":48553,"corporation":false,"usgs":true,"family":"Landis","given":"Edwin","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":284449,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":45,"text":"wsp1260B - 1955 - Floods of April 1952 in the Missouri River basin","interactions":[],"lastModifiedDate":"2019-12-30T08:58:02","indexId":"wsp1260B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1260","chapter":"B","title":"Floods of April 1952 in the Missouri River basin","docAbstract":"<p>The floods of April 1952 in the Milk River basin, along the Missouri River from the mouth of the Little Missouri River to the mouth of the Kansas River, and for scattered tributaries of the Missouri River in North and South Dakota were the greatest ever observed. The damage amounted to an estimated $179 million. The outstanding featur6 of the floods was the extraordinary peak discharge generated in the Missouri River at and downstream from Bismarck, N. Dak., on April 6 when a large ice jam upstream from the city was suddenly released. Inflow from flooding tributaries maintained the peak discharge at approximately the same magnitude in the transit of the flood across South Dakota; downstream from Yankton, S. Dak., attenuation of the peak discharge was continuous because of natural storage in the wide flood plains. The outstanding characteristic of floods in the Milk River basin was their duration--the flood crested at Havre, Mont., on April 3 and at Nashua, Mont.. on April 18. The floods were caused by an abnormally heavy accumulation of snow that was converted into runoff in a few days of very warm weather at the end of March. The heaviest water content of the snow pack at breakup was in a narrow arc extending through Aberdeen, S. Dak., Pierre, S. Dak.. and northwestward toward the southwest corner of North Dakota. The water content in part of this concentrated cover exceeded 6 inches. The winter of 1951-52, which followed a wet cold fall that made the ground impervious, was one of the most severe ever experienced in South Dakota and northern Montana. Depths of snow and low temperatures combined to produce, at the end of March, one of the heaviest snow covers in the history of the Great Plains. The Missouri River ice was intact upstream from Chamberlain, S. Dak., at the end of March, and the breakup of the ice with inflow of local runoff was one of the spectacular features of the flood. Runoff from the Yellowstone River combining with the flood pouring from the Little Missouri River caused the Missouri River to crest at an all-time high at Elbowoods, N. Dak., on April 4. As this crest moved downstream to Bismarck, its intensity was increased by the alternate storing and release of ice jams plus the inflow from the Knife River. The crest discharge of 500,000 cfs came at Bismarck at 6 p. m. on April 6. following a very sharp rise from 80,000 cfs at 11 a.m. Overflow occurred along the Missouri River from Elbowoods to the mouth with high damage to cities. farmland, and installations located in the flood plain. Cleanup and repair operations following the flood continued for many weeks. Few of the flooded farms produced a crop during 1952. This report presents detailed records of stage and discharge for the flood period on the Missouri River and tributaries from Fort Peck. Mont., to the mouth. Information on damages and river stages collected by other agencies is also presented.</p>","language":"English","publisher":"U.S. Government Print Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1260B","usgsCitation":"Wells, J.V., 1955, Floods of April 1952 in the Missouri River basin: U.S. Geological Survey Water Supply Paper 1260, Report: x, 302 p.; 3 Plates: 16.50 x 19.00 inches or smaller, https://doi.org/10.3133/wsp1260B.","productDescription":"Report: x, 302 p.; 3 Plates: 16.50 x 19.00 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":24669,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1260b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24670,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1260b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137523,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1260b/report-thumb.jpg"},{"id":24671,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1260b/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24672,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1260b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","otherGeospatial":"Missouri River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.345703125,\n              49.38237278700955\n            ],\n            [\n              -113.90625,\n              47.57652571374621\n            ],\n            [\n              -110.56640625,\n              42.35854391749705\n            ],\n            [\n              -104.32617187499999,\n              37.78808138412046\n            ],\n            [\n              -96.94335937499999,\n              36.1733569352216\n            ],\n            [\n              -89.033203125,\n              37.50972584293751\n            ],\n            [\n              -88.9453125,\n              38.13455657705411\n            ],\n            [\n              -92.63671875,\n              43.197167282501276\n            ],\n            [\n              -93.955078125,\n              45.706179285330855\n            ],\n            [\n              -99.228515625,\n              49.26780455063753\n            ],\n            [\n              -102.919921875,\n              49.32512199104001\n            ],\n            [\n              -114.345703125,\n              49.38237278700955\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478ee4b07f02db4899d8","contributors":{"authors":[{"text":"Wells, J. 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,{"id":71533,"text":"tei507 - 1955 - Contribution to the crystallography of uranium minerals","interactions":[],"lastModifiedDate":"2012-02-02T00:14:05","indexId":"tei507","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"507","title":"Contribution to the crystallography of uranium minerals","language":"ENGLISH","doi":"10.3133/tei507","usgsCitation":"Donnay, G., and Donnay, J., 1955, Contribution to the crystallography of uranium minerals: U.S. Geological Survey Trace Elements Investigations 507, 42 p. : ill. ; 27 cm., https://doi.org/10.3133/tei507.","productDescription":"42 p. : ill. ; 27 cm.","costCenters":[],"links":[{"id":193232,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/507/report-thumb.jpg"},{"id":90798,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/507/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db698553","contributors":{"authors":[{"text":"Donnay, Gabrielle","contributorId":37430,"corporation":false,"usgs":true,"family":"Donnay","given":"Gabrielle","email":"","affiliations":[],"preferred":false,"id":284340,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Donnay, J.D.H.","contributorId":65940,"corporation":false,"usgs":true,"family":"Donnay","given":"J.D.H.","email":"","affiliations":[],"preferred":false,"id":284341,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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