{"pageNumber":"6874","pageRowStart":"171825","pageSize":"25","recordCount":184769,"records":[{"id":70056315,"text":"tem1101 - 1958 - Preliminary geologic map of the Cortez SW quadrangle, Montezuma County, Colorado (NGMDB)","interactions":[],"lastModifiedDate":"2014-03-04T14:35:12","indexId":"tem1101","displayToPublicDate":"1968-01-30T10:43:00","publicationYear":"1958","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":"1101","title":"Preliminary geologic map of the Cortez SW quadrangle, Montezuma County, Colorado (NGMDB)","docAbstract":"No abstract available","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem1101","collaboration":"Prepared in cooperation the the U.S. Atomic Energy Commission","usgsCitation":"Ekren, E.B., and Houser, F.N., 1958, Preliminary geologic map of the Cortez SW quadrangle, Montezuma County, Colorado (NGMDB): U.S. Geological Survey Trace Elements Memorandum 1101, Report: 1 p.; Plate: 23.79 inches x 36.14 inches; Plate List: 1 p., https://doi.org/10.3133/tem1101.","productDescription":"Report: 1 p.; Plate: 23.79 inches x 36.14 inches; Plate List: 1 p.","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":279167,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/1101/report-thumb.jpg"},{"id":283353,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/1101/report.pdf"},{"id":283351,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/1101/plate-1.pdf"},{"id":283352,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/1101/plate-list.pdf"}],"country":"United States","state":"Colorado","county":"Montezuma County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.7500,37.2500 ], [ -108.7500,37.3750 ], [ -108.6250,37.3750 ], [ -108.6250,37.2500 ], [ -108.7500,37.2500 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"528c96b6e4b0c629af44dddf","contributors":{"authors":[{"text":"Ekren, E. B.","contributorId":14371,"corporation":false,"usgs":true,"family":"Ekren","given":"E.","middleInitial":"B.","affiliations":[],"preferred":false,"id":486519,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Houser, F. N.","contributorId":79111,"corporation":false,"usgs":true,"family":"Houser","given":"F.","middleInitial":"N.","affiliations":[],"preferred":false,"id":486520,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70114668,"text":"tei2042 - 1958 - Geology and ore deposits of the Monument Valley area, Apache and Navajo counties, Arizona: Part II","interactions":[],"lastModifiedDate":"2014-07-14T14:08:49","indexId":"tei2042","displayToPublicDate":"1960-01-01T14:24:56","publicationYear":"1958","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":"204-2","title":"Geology and ore deposits of the Monument Valley area, Apache and Navajo counties, Arizona: Part II","docAbstract":"<p>In 1951 and 1952, the U.S. Geological Survey conducted a program of uranium investigations and geologic mapping in the Monument Valley area, Apache and Navajo Counties, Ariz. About 700 square miles were mapped on the Navajo Indian Reservation. A resource appraisal of the area was an inherent part of the program, and is detailed in this report.</p>\n<br/>\n<p>Production of vanadium and uranium is from two areas, the Monument No. 1 mine area in Navajo County, and the Monument No. 2 mine area in Apache County. In the period 1942-53 about 200,300 tons of ore was produced from these two areas. This ore yielded about 1,700,000 pounds of U<sub>3</sub>O<sub>8</sub> and about 6,500,000 pounds of V<sub>2</sub>O<sub>5</sub>. The grade ranged from 0.15 percent U<sub>3</sub>O<sub>8</sub> to 0.60 percent U<sub>3</sub>O<sub>8</sub>, and from 0.38 percent V<sub>2</sub>O<sub>5</sub> to 3.02 percent V<sub>2</sub>O<sub>5</sub>. The vanadium-uranium ratio is about 4:1.</p>\n<br/>\n<p>The ore deposits are composed principally of the hydrous calcium-uranium vanadate tyuyamunite in basal channel sediments of the Shinarump member off the Chinle formation. Four types of ore bodies are present: (1) rods, (2) tabular ore bodies, (3) corvusite-type ore bodies, and (4) rolls.</p>\n<br/>\n<p>The reserves of uranium- and vanadium-bearing material are classed as measured, indicated, inferred, and potential. The reserves are further divided into three grade classes for material 1 foot or more thick: (1) 0.10 percent U<sub>3</sub>O<sub>8</sub> and 1.00 percent V<sub>2</sub>O<sub>5</sub> and above; (2) 0.05 percent U<sub>3</sub>O<sub>8</sub> and 0.50 percent V<sub>2</sub>O<sub>5</sub> and less than 0.10 percent U<sub>3</sub>O<sub>8</sub> and 1.00 percent V<sub>2</sub>O<sub>5</sub>; and (3) 0.01 percent U<sub>3</sub>O<sub>8</sub> and 0.10 percent V<sub>2</sub>O<sub>5</sub> and less than 0.05 percent U<sub>3</sub>O<sub>8</sub> and 0.05 percent V<sub>2</sub>O<sub>5</sub>.</p>\n<br/>\n<p>Measured reserves as of June 1953, in the Monument Valley area, Arizona, (all in the Monument No. 2 mine) total about 36,000 tons. Indicated reserves in the first grade class amount to about 62,000 tons. In this same grade class inferred reserves total about 3,000,000 tons. In the second grade class indicated and inferred reserves amount to about 2,000,000 tons. Inferred reserves in the third grade class total about 345,000 tons of mineralized material. Potential reserves in all grade classes for the Monument Valley area amount to about 13,000,000 tons.</p>\n<br/>\n<p>It is recommended that an extensive exploration program be carried out in the Monument Valley area, Arizona. This program would consist of two phases. The first phase would involve a geophysical survey of selected channels and would have at its principal objective the delineation of the trend, length, width, and depth of scour of the channels. The second phase would consist of a diamond-drilling program that would make use of the data secured by the geophysical survey. This drilling program would have as one of its principal objectives the determination of which channels are most likely to contain ore bodies. Once the favorable channels are discovered, the drilling program could be carried on most suitably by private operators.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei2042","usgsCitation":"Witkind, I.J., and Thaden, R., 1958, Geology and ore deposits of the Monument Valley area, Apache and Navajo counties, Arizona: Part II: U.S. Geological Survey Trace Elements Investigations 204-2, 29 p., https://doi.org/10.3133/tei2042.","productDescription":"29 p.","startPage":"281","endPage":"309","numberOfPages":"38","costCenters":[],"links":[{"id":289963,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":289962,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0204-2/report.pdf"}],"country":"United States","state":"Arizona","county":"Apache County;Navajo County","otherGeospatial":"Monument Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.7509,33.4754 ], [ -110.7509,37.0043 ], [ -109.0452,37.0043 ], [ -109.0452,33.4754 ], [ -110.7509,33.4754 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ad40f1e4b0729c154181c5","contributors":{"authors":[{"text":"Witkind, I. J.","contributorId":54221,"corporation":false,"usgs":true,"family":"Witkind","given":"I.","middleInitial":"J.","affiliations":[],"preferred":false,"id":495402,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thaden, R.E.","contributorId":12098,"corporation":false,"usgs":true,"family":"Thaden","given":"R.E.","affiliations":[],"preferred":false,"id":495401,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":72032,"text":"tem1103 - 1958 - Preliminary geologic map of the Sentinel Peak NE Quadrangle, Montezuma County, Colorado","interactions":[],"lastModifiedDate":"2014-01-30T10:45:21","indexId":"tem1103","displayToPublicDate":"1959-01-21T11:13:00","publicationYear":"1958","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":"1103","title":"Preliminary geologic map of the Sentinel Peak NE Quadrangle, Montezuma County, Colorado","docAbstract":"No abstract available","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem1103","collaboration":"Prepared in cooperation the the U.S. Atomic Energy Commission","usgsCitation":"Ekren, E.B., and Houser, F.N., 1958, Preliminary geologic map of the Sentinel Peak NE Quadrangle, Montezuma County, Colorado: U.S. Geological Survey Trace Elements Memorandum 1103, Report 2 p.; Plate List: 1 p.; Plate: 27.90 inches x 41.76 inches, https://doi.org/10.3133/tem1103.","productDescription":"Report 2 p.; Plate List: 1 p.; Plate: 27.90 inches x 41.76 inches","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":279172,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/1103/report-thumb.jpg"},{"id":281706,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/1103/plate-1.pdf"},{"id":281707,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/1103/plate-list.pdf"},{"id":281705,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/1103/report.pdf"}],"country":"United States","state":"Colorado","county":"Montezuma County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.8750,37.1250 ], [ -108.8750,37.2500 ], [ -108.7500,37.2500 ], [ -108.7500,37.1250 ], [ -108.8750,37.1250 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"528c96b8e4b0c629af44ddee","contributors":{"authors":[{"text":"Ekren, E. B.","contributorId":14371,"corporation":false,"usgs":true,"family":"Ekren","given":"E.","middleInitial":"B.","affiliations":[],"preferred":false,"id":285021,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Houser, F. N.","contributorId":79111,"corporation":false,"usgs":true,"family":"Houser","given":"F.","middleInitial":"N.","affiliations":[],"preferred":false,"id":285022,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2399,"text":"wsp1460E - 1958 - Geological and geophysical study of the preglacial Teays Valley in west-central Ohio","interactions":[],"lastModifiedDate":"2023-12-15T22:44:35.683417","indexId":"wsp1460E","displayToPublicDate":"1959-01-01T00:00:00","publicationYear":"1958","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":"1460","chapter":"E","title":"Geological and geophysical study of the preglacial Teays Valley in west-central Ohio","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1460E","usgsCitation":"Norris, S.E., and Spicer, H.C., 1958, Geological and geophysical study of the preglacial Teays Valley in west-central Ohio: U.S. Geological Survey Water Supply Paper 1460, Report: iii, 34 p.; 2 Plates: 12.00 x 18.00 inches and 17.00 x 13.00 inches, https://doi.org/10.3133/wsp1460E.","productDescription":"Report: iii, 34 p.; 2 Plates: 12.00 x 18.00 inches and 17.00 x 13.00 inches","startPage":"199","endPage":"232","costCenters":[],"links":[{"id":28378,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1460e/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28379,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1460e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138960,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1460e/report-thumb.jpg"},{"id":28377,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1460e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":423659,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24390.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Ohio","county":"Champaign County, Clark County, Madison County","otherGeospatial":"Teays Valley","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-83.5514,40.2294],[-83.4942,40.2254],[-83.5024,40.126],[-83.504,40.111],[-83.3747,40.1106],[-83.2797,40.1099],[-83.2063,40.1076],[-83.2123,40.0477],[-83.2616,40.0497],[-83.2627,40.042],[-83.2609,40.0338],[-83.2559,40.0221],[-83.2565,40.0184],[-83.2606,40.013],[-83.2648,40.0098],[-83.266,40.007],[-83.2605,39.998],[-83.2568,39.993],[-83.2531,39.9813],[-83.253,39.9699],[-83.2498,39.955],[-83.2462,39.9514],[-83.2425,39.9469],[-83.2383,39.9428],[-83.2376,39.9347],[-83.2388,39.9306],[-83.2369,39.927],[-83.2351,39.9256],[-83.2524,39.9169],[-83.2436,39.8131],[-83.2499,39.7301],[-83.2525,39.6952],[-83.423,39.7031],[-83.6252,39.7146],[-83.6534,39.7166],[-83.6471,39.7729],[-83.6466,39.7761],[-83.7388,39.7811],[-83.7407,39.7888],[-83.8079,39.7958],[-83.8295,39.7979],[-83.827,39.8224],[-83.9415,39.8288],[-83.94,39.8438],[-84.0059,39.8475],[-84.0245,39.8487],[-84.0539,39.8501],[-84.051,39.8801],[-84.0427,39.9673],[-84.0358,40.0399],[-84.0349,40.0535],[-84.035,40.0558],[-84.0232,40.1838],[-84.0188,40.2274],[-84.0188,40.2297],[-84.0143,40.2737],[-83.9829,40.2714],[-83.9739,40.271],[-83.9546,40.2699],[-83.875,40.2653],[-83.8707,40.2649],[-83.7839,40.2599],[-83.7848,40.2481],[-83.7854,40.2449],[-83.5514,40.2294]]]},\"properties\":{\"name\":\"Champaign\",\"state\":\"OH\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db687525","contributors":{"authors":[{"text":"Norris, Stanley Eugene","contributorId":24772,"corporation":false,"usgs":true,"family":"Norris","given":"Stanley","email":"","middleInitial":"Eugene","affiliations":[],"preferred":false,"id":145136,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spicer, H. Cecil","contributorId":67075,"corporation":false,"usgs":true,"family":"Spicer","given":"H.","email":"","middleInitial":"Cecil","affiliations":[],"preferred":false,"id":145137,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70194827,"text":"70194827 - 1958 - References on laboratory and equipment methods in ground water hydrology","interactions":[],"lastModifiedDate":"2018-01-10T15:37:36","indexId":"70194827","displayToPublicDate":"1959-01-01T00:00:00","publicationYear":"1958","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"References on laboratory and equipment methods in ground water hydrology","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70194827","usgsCitation":"1958, References on laboratory and equipment methods in ground water hydrology, 18 p., https://doi.org/10.3133/70194827.","productDescription":"18 p.","numberOfPages":"22","costCenters":[],"links":[{"id":350418,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a615b03e4b06e28e9c260d8","contributors":{"compilers":[{"text":"Johnson, A. I.","contributorId":120232,"corporation":false,"usgs":true,"family":"Johnson","given":"A.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":725482,"contributorType":{"id":3,"text":"Compilers"},"rank":1}]}}
,{"id":70217847,"text":"70217847 - 1958 - Computations in magnetic and gravity interpretation","interactions":[],"lastModifiedDate":"2021-02-05T19:31:52.992078","indexId":"70217847","displayToPublicDate":"1958-12-31T13:29:50","publicationYear":"1958","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Computations in magnetic and gravity interpretation","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"ACM '58: Preprints of papers presented at the 13th national meeting of the Association for Computing Machinery","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"ACM '58: 13th national meeting of the Association for Computing Machinery","language":"English","publisher":"Association for Computing Machinery","doi":"10.1145/610937.610947","usgsCitation":"Henderson, R., and Marsheck, J.R., 1958, Computations in magnetic and gravity interpretation, <i>in</i> ACM '58: Preprints of papers presented at the 13th national meeting of the Association for Computing Machinery, 4 p., https://doi.org/10.1145/610937.610947.","productDescription":"4 p.","costCenters":[],"links":[{"id":383065,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Henderson, Roland G.","contributorId":65139,"corporation":false,"usgs":true,"family":"Henderson","given":"Roland G.","affiliations":[],"preferred":false,"id":809896,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Marsheck, J. R.","contributorId":248802,"corporation":false,"usgs":false,"family":"Marsheck","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":809897,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70207433,"text":"70207433 - 1958 - Metamorphosed middle Paleozoic fossils from Central Massachusetts, eastern Vermont, and western New Hampshire","interactions":[],"lastModifiedDate":"2020-03-19T14:41:02","indexId":"70207433","displayToPublicDate":"1958-12-31T11:08:33","publicationYear":"1958","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":"Metamorphosed middle Paleozoic fossils from Central Massachusetts, eastern Vermont, and western New Hampshire","docAbstract":"<p><span>Study of thin and polished sections and spectrographic analyses indicate that the brachiopod most recently used to date the Bernardston Formation in Massachusetts probably came from Lower Devonian beds (chlorite zone) in Nova Scotia, and not from Bernardston, Massachusetts. Restudy of the faunule from the calcareous quartzite (garnet zone) of the Bernardston Formation indicates that it is probably of Silurian rather than Devonian age. The upper part of the Clough Formation on Skitchewaug Mountain (garnet zone) in eastern Vermont contains tetracorals of Silurian or Devonian age. The Clough Formation on Croydon Mountain (sillimanite zone) in west-central New Hampshire contains tetracorals. The fossiliferous zone in the lower part of the Bernardston Formation is possibly equivalent to the upper part of the Clough Formation.&nbsp;</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1958)69[855:MMPFFC]2.0.CO;2","usgsCitation":"Boucot, A., Macdonald, G., Milton, C., and Thompson, J.B., 1958, Metamorphosed middle Paleozoic fossils from Central Massachusetts, eastern Vermont, and western New Hampshire: Geological Society of America Bulletin, v. 69, no. 7, p. 855-870, https://doi.org/10.1130/0016-7606(1958)69[855:MMPFFC]2.0.CO;2.","productDescription":"16 p. 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J.","contributorId":30620,"corporation":false,"usgs":true,"family":"Boucot","given":"A. J.","affiliations":[],"preferred":false,"id":777990,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Macdonald, G.J.F.","contributorId":221370,"corporation":false,"usgs":false,"family":"Macdonald","given":"G.J.F.","email":"","affiliations":[],"preferred":false,"id":777991,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Milton, C.","contributorId":37472,"corporation":false,"usgs":true,"family":"Milton","given":"C.","affiliations":[],"preferred":false,"id":777992,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Thompson, James B. Jr.","contributorId":48273,"corporation":false,"usgs":false,"family":"Thompson","given":"James","suffix":"Jr.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":777993,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70207211,"text":"70207211 - 1958 - Military use of geologists in World War II","interactions":[],"lastModifiedDate":"2020-08-31T16:11:55.489433","indexId":"70207211","displayToPublicDate":"1958-12-31T10:09:42","publicationYear":"1958","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":"Military use of geologists in World War II","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1958)69[615:MUOGIW]2.0.CO;2","issn":"00167606","usgsCitation":"Nace, R.L., 1958, Military use of geologists in World War II: Geological Society of America Bulletin, v. 69, no. 5, p. 615-616, https://doi.org/10.1130/0016-7606(1958)69[615:MUOGIW]2.0.CO;2.","productDescription":"2 p.","startPage":"615","endPage":"616","costCenters":[],"links":[{"id":370205,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"69","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Nace, R. L.","contributorId":11332,"corporation":false,"usgs":true,"family":"Nace","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":777278,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70207267,"text":"70207267 - 1958 - Stratigraphy of ocoee series, Great Smoky Mountains, Tennessee and North Carolina","interactions":[],"lastModifiedDate":"2019-12-16T06:51:23","indexId":"70207267","displayToPublicDate":"1958-12-31T09:11:00","publicationYear":"1958","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":"Stratigraphy of ocoee series, Great Smoky Mountains, Tennessee and North Carolina","docAbstract":"<p><span>Much of the Great Smoky Mountains, which span the boundary between Tennessee and North Carolina, is formed of the Ocoee series, of later Precambrian age. This is a body of terrigenous clastic sedimentary rocks, which has minor intercalations of limestone and dolomite but no volcanic components or known fossils. The series is probably 30,000 feet or more thick. It lies unconformably on a basement of earlier Precambrian granitic and gneissic rocks, and on the northwest side of the mountains it is overlain by the Cochran formation, or basal unit of the Chilhowee group, which is of Cambrian and Precambrian(?) age. South of the mountains it is overlain by rocks of the Murphy marble belt; here, the top of the Ocoee is placed tentatively at the base of the Nantahala slate. The Ocoee series is divisible into three broad units of regional extent and contrasting lithologic character, which are herewith designated groups and named the Snowbird group, the Great Smoky group, and the Walden Creek group. The groups consist of local intergrading and intertonguing formations and have complex stratigraphic and structural relations. The Ocoee series is split by major thrust faults into three sequences, a southern, central, and northern, none of which contains more than two groups of the series. The lowest group, the Snowbird, is best developed in the central sequence where it is more than 13,000 feet thick; it is much thinner in the southern sequence. In both sequences it lies unconformably on granites and gneisses. Toward the east it is largely sandstone, but this is interbedded with and intertongues westward into finer-grained sandstone, siltstone, and argillaceous rocks. These differences permit the Snowbird group to be divided, in ascending order, into the Wading Branch formation, Longarm quartzite, Roaring Fork sandstone, and Pigeon siltstone. Toward the west the Snowbird is represented by more strongly metamorphosed rocks termed the Metcalf phyllite. Above the Snowbird group in the southern sequence is the Great Smoky group, more than 25,000 feet thick. The lower part, termed the Elkmont sandstone, is fine-grained sandstone. The middle part, termed the Thunderhead sandstone, is poorly sorted, coarse, feldspathic sandstone in graded beds. The upper part, termed the Anakeesta formation, includes many beds of dark argillaceous and silty rocks. South of the Great Smoky Mountains the Great Smoky group is overlain by the rocks of the Murphy marble belt. The Snowbird group in the central sequence is overlain in a few places by coarser-grained rocks. These somewhat resemble those of the Great Smoky group, but their stratigraphic relations to it are not demonstrable, so that they are left as unclassified parts of the Ocoee series. In one area such rocks are named the Rich Butt sandstone, in another the Cades sandstone. In the northern sequence the Walden Creek group, about 8000 feet thick, forms a varied assemblage of argillaceous and silty rocks and quartz-pebble conglomerate, with locally prominent quartzite, limestone, and dolomite. The Walden Creek group is divided, in ascending order, into the Licklog formation, Shields formation, Wilhite formation, and Sandsuck formation; the Wilhite is in turn divided into the Dixon Mountain member and Yellow Breeches member. The Walden Creek is overlain by the Chilhowee group of Cambrian and Precambrian(?) age but is in fault contact with the Snowbird group on the southeast; it is not in contact with the Great Smoky group. Northeast of the Great Smoky Mountains, the Walden Creek group is reported to overlie the Snowbird group as part of a sedimentary sequence from the basement rocks upward through the Chilhowee group into the overlying Paleozoic. © 1958, The Geological Society of America, Inc.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1958)69[947:SOOSGS]2.0.CO;2","issn":"00167606","usgsCitation":"King, P., Hadley, J.B., Neuman, R.B., and Hamilton, W., 1958, Stratigraphy of ocoee series, Great Smoky Mountains, Tennessee and North Carolina: Geological Society of America Bulletin, v. 69, no. 8, p. 947-966, https://doi.org/10.1130/0016-7606(1958)69[947:SOOSGS]2.0.CO;2.","productDescription":"20 p. 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B.","contributorId":51267,"corporation":false,"usgs":true,"family":"Hadley","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":777496,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Neuman, R. B.","contributorId":83579,"corporation":false,"usgs":true,"family":"Neuman","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":777497,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hamilton, W.","contributorId":46683,"corporation":false,"usgs":true,"family":"Hamilton","given":"W.","email":"","affiliations":[],"preferred":false,"id":777498,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70206773,"text":"70206773 - 1958 - The environmental control of sedimentary iron minerals","interactions":[],"lastModifiedDate":"2019-11-21T13:29:44","indexId":"70206773","displayToPublicDate":"1958-11-21T13:22:16","publicationYear":"1958","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":"The environmental control of sedimentary iron minerals","docAbstract":"<p><span>An Eh-pH stability diagram is developed for hematite, magnetite, siderite, pyrite, and iron sulfide that indicates the relative position of their stability fields in a normal sea water system. With the exception of the magnetite-siderite relationship, Eh is much more critical than pH. In general terms, hematite is stable under oxidizing conditions, siderite and magnetite under intermediate to moderately reducing conditions, pyrite under moderate to strongly reducing conditions, and iron sulfide under still stronger reducing conditions. Because of numerous variables involved the relative positions of the stability fields are stressed rather than their limits on the Eh and pH scales. The inclusion of a magnetite field suggests that magnetite should be much more important as a primary or diagenetic mineral in sedimentary rocks than has been commonly recognized. This is in accord with numerous recent suggestions to that effect. The importance of thermodynamic equilibrium is stressed and it is suggested that differences in rates of formation of the various minerals and the persistence of some metastable phases are among the commonest causes of lack of equilibrium.</span></p>","language":"English","publisher":"Society of Economic Geology","doi":"10.2113/gsecongeo.53.2.123","usgsCitation":"Huber, N., 1958, The environmental control of sedimentary iron minerals: Economic Geology, v. 53, no. 2, p. 123-140, https://doi.org/10.2113/gsecongeo.53.2.123.","productDescription":"18 p.","startPage":"123","endPage":"140","costCenters":[],"links":[{"id":369393,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"53","issue":"2","noUsgsAuthors":false,"publicationDate":"1958-03-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Huber, N.K.","contributorId":73610,"corporation":false,"usgs":true,"family":"Huber","given":"N.K.","affiliations":[],"preferred":false,"id":775728,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72016,"text":"tem1079 - 1958 - Photogeologic map of the Mount Ellen-4 Quadrangle, Wayne County, Utah","interactions":[],"lastModifiedDate":"2014-03-25T10:22:44","indexId":"tem1079","displayToPublicDate":"1958-11-18T15:07:00","publicationYear":"1958","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":"1079","title":"Photogeologic map of the Mount Ellen-4 Quadrangle, Wayne County, Utah","docAbstract":"No abstract available","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem1079","collaboration":"Prepared in cooperation with the U.S. Atomic Energy Commission","usgsCitation":"Hemphill, W.R., 1958, Photogeologic map of the Mount Ellen-4 Quadrangle, Wayne County, Utah: U.S. Geological Survey Trace Elements Memorandum 1079, Report: 3 p.; Plate: 23.67 inches x 30.90 inches, https://doi.org/10.3133/tem1079.","productDescription":"Report: 3 p.; Plate: 23.67 inches x 30.90 inches","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":279028,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":284805,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/1079/plate-1.pdf"},{"id":284806,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/1079/report.pdf"}],"country":"United States","state":"Utah","county":"Wayne County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.00,38.375 ], [ -111.00,38.500 ], [ -110.875,38.500 ], [ -110.875,38.375 ], [ -111.00,38.375 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd6b3be4b0b29085103c77","contributors":{"authors":[{"text":"Hemphill, W. R.","contributorId":19525,"corporation":false,"usgs":true,"family":"Hemphill","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":284999,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72009,"text":"tem1071 - 1958 - Photogeologic map of the east half of Cahone Quadrangle, Montezuma and Dolores counties, Colorado","interactions":[],"lastModifiedDate":"2014-03-25T10:17:33","indexId":"tem1071","displayToPublicDate":"1958-11-01T12:45:00","publicationYear":"1958","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":"1071","title":"Photogeologic map of the east half of Cahone Quadrangle, Montezuma and Dolores counties, Colorado","docAbstract":"No abstract available","language":"English","publisher":"U.S. Geological Service","doi":"10.3133/tem1071","collaboration":"Prepared in cooperation with the U.S. Atomic Energy Commission","usgsCitation":"Hackman, R., 1958, Photogeologic map of the east half of Cahone Quadrangle, Montezuma and Dolores counties, Colorado: U.S. Geological Survey Trace Elements Memorandum 1071, Report: 3 p.; Plate: 20.07 inches x 21.66 inches, https://doi.org/10.3133/tem1071.","productDescription":"Report: 3 p.; Plate: 20.07 inches x 21.66 inches","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":279017,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":284791,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/1071/plate-1.pdf"},{"id":284792,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/1071/report.pdf"}],"country":"United States","state":"Colorado","county":"Dolores County;Montezuma County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.000,37.500 ], [ -109.000,37.750 ], [ -108.750,37.750 ], [ -108.750,37.500 ], [ -109.000,37.500 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd6b4ae4b0b29085103cec","contributors":{"authors":[{"text":"Hackman, R.J.","contributorId":95086,"corporation":false,"usgs":true,"family":"Hackman","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":284991,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5220642,"text":"5220642 - 1958 - The isolation and identification of Trypanosoma cruzi from raccoons in Maryland","interactions":[],"lastModifiedDate":"2023-02-23T16:39:09.157785","indexId":"5220642","displayToPublicDate":"1958-11-01T12:18:16","publicationYear":"1958","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":733,"text":"American Journal of Tropical Medicine and Hygiene","active":true,"publicationSubtype":{"id":10}},"displayTitle":"The isolation and identification of <i>Trypanosoma cruzi</i> from raccoons in Maryland","title":"The isolation and identification of Trypanosoma cruzi from raccoons in Maryland","docAbstract":"<p><span>Five raccoons trapped at Patuxent Research Refuge, Laurel, Maryland, were found to have trypanosomes in the blood which were morphologically indistinguishable from&nbsp;</span><i>Trypanosoma cruzi</i><span>&nbsp;on stained smears. The organism grew well in culture. It developed and reproduced in&nbsp;</span><i>Triatoma protracta, T. infestans, T. phyllosoma</i><span>, and&nbsp;</span><i>Rhodnius prolixus</i><span>. Experimental infections were produced in raccoons, opossums, mice, rats, and monkeys by inoculation of blood, culture, and triatome forms. Typical leishmaniform bodies were found in tissue sections of cardiac muscle fibers from naturally and experimentally infected animals. Cross agglutinations carried out with living cultural forms and rabbit antisera demonstrated a close antigenic relationship between the raccoon trypanosome and&nbsp;</span><i>T. cruzi</i><span>&nbsp;(Brazil strain). On the basis of (1) morphology, (2) presence of leishmaniform tissue stages, (3) development in triatomes, (4) infectivity to a variety of mammals, (5) culture characteristics, and (6) cross reactions in serological tests, this parasite is considered conspecific with&nbsp;</span><i>Trypanosoma cruzi</i><span>&nbsp;(Chagas, 1909) the causative agent of American human trypanosomiasis.</span></p>","language":"English","publisher":"American Society of Tropical Medicine and Hygiene","doi":"10.4269/ajtmh.1958.7.603","usgsCitation":"Walton, B., Bauman, P.M., Diamond, L.S., and Herman, C.M., 1958, The isolation and identification of Trypanosoma cruzi from raccoons in Maryland: American Journal of Tropical Medicine and Hygiene, v. 7, no. 6, p. 603-610, https://doi.org/10.4269/ajtmh.1958.7.603.","productDescription":"8 p.","startPage":"603","endPage":"610","numberOfPages":"8","costCenters":[{"id":531,"text":"Patuxent Wildlife Research 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,{"id":70010561,"text":"70010561 - 1958 - Use and renewal of natural resources","interactions":[],"lastModifiedDate":"2026-02-27T16:43:35.916774","indexId":"70010561","displayToPublicDate":"1958-09-19T00:00:00","publicationYear":"1958","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Use and renewal of natural resources","docAbstract":"Science and technology can create new materials faster than consumers can exhaust present resources.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.128.3325.631","issn":"00368075","usgsCitation":"Nolan, T.B., 1958, Use and renewal of natural resources: Science, v. 128, no. 3325, p. 631-636, https://doi.org/10.1126/science.128.3325.631.","productDescription":"6 p.","startPage":"631","endPage":"636","costCenters":[],"links":[{"id":219081,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"128","issue":"3325","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbe51e4b08c986b329511","contributors":{"authors":[{"text":"Nolan, T. B.","contributorId":71610,"corporation":false,"usgs":true,"family":"Nolan","given":"T.","middleInitial":"B.","affiliations":[],"preferred":false,"id":359173,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":37814,"text":"37814 - 1958 - Fur catch in the United States, 1957","interactions":[],"lastModifiedDate":"2014-07-24T10:08:48","indexId":"37814","displayToPublicDate":"1958-09-01T10:08:15","publicationYear":"1958","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":"398","title":"Fur catch in the United States, 1957","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","collaboration":"Compiled in the Bird and Mammal Laboratories, Branch of Wildlife Research, Bureau of Sport Fisheries and Wildlife.","usgsCitation":"U.S. Branch of Wildlife Research, 1958, Fur catch in the United States, 1957 (Supersedes Wildlife Leaflet 388 (1957).): Wildlife Leaflet 398, 3 p.","productDescription":"3 p.","numberOfPages":"3","costCenters":[],"links":[{"id":290865,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Supersedes Wildlife Leaflet 388 (1957).","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd338e4b0824b2d176dca","contributors":{"authors":[{"text":"U.S. Branch of Wildlife Research","contributorId":127903,"corporation":true,"usgs":false,"organization":"U.S. Branch of Wildlife Research","id":529736,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70009845,"text":"70009845 - 1958 - The solusphere - its inferences and study","interactions":[],"lastModifiedDate":"2024-09-16T22:55:59.544268","indexId":"70009845","displayToPublicDate":"1958-09-01T00:00:00","publicationYear":"1958","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"The solusphere - its inferences and study","docAbstract":"<p>Water is a fundamental geologic agent active in rock decomposition, erosion, and synthesis. Solutes in water are of particular interest to geochemists as sources of raw material for synthesis or as products of decomposition. When geochemical studies move from the laboratory into natural environment many variables relating to solute hydrology must be considered.</p><p>As a focal point there has been designed a graphical representation of solute hydrology, the solusphere, which embodies the concepts of land-water occurrence and movement on which are superimposed geologic, biologic, physical, chemical, and cultural processes affecting solutes. The solusphere is demonstrated by passing an imaginary plane through the centre of the earth. This plane intercepts concentric zones designated as rock flowage, saturation, aeration, surface activity, and atmosphere. Transport processes carry solutes within and between zones without alteration or conversion. However, whether stationary or in motion, the water's solute character is constantly subject to (1) alteration processes that change concentration by addition or subtraction of solutes or solvent without loss of solute identities, and (2) conversion processes that change the chemical state and form of solutes.</p><p>The geochemist is concerned with specific conversion processes, but he also must consider transport, alteration, and other conversion processes that are continually modifying the materials with which he is dealing in nature. The solusphere is an attempt to organize processes affecting the chemical quality of land waters into a unified field of science much like the field of marine chemistry.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(58)90083-8","usgsCitation":"Rainwater, F.H., and White, W.F., 1958, The solusphere - its inferences and study: Geochimica et Cosmochimica Acta, v. 14, no. 3, p. 244-249, https://doi.org/10.1016/0016-7037(58)90083-8.","productDescription":"6 p.","startPage":"244","endPage":"249","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":218830,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb045e4b08c986b324d4f","contributors":{"authors":[{"text":"Rainwater, F. H.","contributorId":41402,"corporation":false,"usgs":true,"family":"Rainwater","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":357273,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"White, W. F.","contributorId":80259,"corporation":false,"usgs":true,"family":"White","given":"W.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":357274,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010646,"text":"70010646 - 1958 - Accumulator plants and rock weathering","interactions":[],"lastModifiedDate":"2026-02-27T16:48:13.41299","indexId":"70010646","displayToPublicDate":"1958-08-22T00:00:00","publicationYear":"1958","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Accumulator plants and rock weathering","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.128.3321.416","issn":"00368075","usgsCitation":"Lovering, T.S., 1958, Accumulator plants and rock weathering: Science, v. 128, no. 3321, p. 416-417, https://doi.org/10.1126/science.128.3321.416.","productDescription":"2 p.","startPage":"416","endPage":"417","costCenters":[],"links":[{"id":219259,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"128","issue":"3321","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e686e4b0c8380cd47489","contributors":{"authors":[{"text":"Lovering, T. S.","contributorId":108085,"corporation":false,"usgs":true,"family":"Lovering","given":"T.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":359343,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70212511,"text":"70212511 - 1958 - Root growth near tensiometer cups as a cause of diurnal fluctuations of readings","interactions":[],"lastModifiedDate":"2020-08-18T18:53:44.059125","indexId":"70212511","displayToPublicDate":"1958-08-18T13:37:04","publicationYear":"1958","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3419,"text":"Soil Science","active":true,"publicationSubtype":{"id":10}},"title":"Root growth near tensiometer cups as a cause of diurnal fluctuations of readings","docAbstract":"<p><span>No abstract available.</span></p>","language":"English","publisher":"Wolters Kluwer","doi":"10.1097/00010694-195803000-00008","usgsCitation":"Remson, I., and Randolph, J., 1958, Root growth near tensiometer cups as a cause of diurnal fluctuations of readings: Soil Science, v. 85, no. 3, p. 167-171, https://doi.org/10.1097/00010694-195803000-00008.","productDescription":"5 p.","startPage":"167","endPage":"171","costCenters":[],"links":[{"id":377631,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"85","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Remson, Irwin","contributorId":89115,"corporation":false,"usgs":true,"family":"Remson","given":"Irwin","email":"","affiliations":[],"preferred":false,"id":796636,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Randolph, J.R.","contributorId":19532,"corporation":false,"usgs":true,"family":"Randolph","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":796637,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70212509,"text":"70212509 - 1958 - Geology of Kapingamarangi Atoll, Caroline Islands","interactions":[],"lastModifiedDate":"2020-08-18T18:03:02.703072","indexId":"70212509","displayToPublicDate":"1958-08-18T12:40:01","publicationYear":"1958","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Geology of Kapingamarangi Atoll, Caroline Islands","docAbstract":"<p><span>Kapingamarangi Atoll of the Caroline Islands consists of a peripheral reef, 1000-4000 feet across, surrounding a nearly circular lagoon which is 5 by 6 nautical miles in area and about 240 feet at maximum depth. Thirty-three islands, most of which are less than half a mile in length, are scattered along the eastern half of the peripheral reef. At least 75 patch reefs, most of which are small, nearly symmetrical mounds, rise to the surface of the lagoon. The peripheral reef and the patch reefs, composed largely of the stony structures of corals and coralline algae, have flat upper surfaces, apparently the result of bevelling by waves during a recent lowering of sea level. The islands on the peripheral reef are formed of partially consolidated stratified sediments composed of clastic limestone particles and the shells of marine animals. These islands are migrating lagoonward across the reef flat because of erosion on the seaward sides and the growth of beaches and bars on the opposite sides. Soils on the islands are poorly developed and retain much of the texture, structure, and composition of the parent rock or sediment. They consist chiefly of mechanical mixtures of carbonaceous material and lime gravel, lime sand, or lime mud. Phosphorite is present on some islands and is still forming locally where apatite derived from bird guano is reacting with limestones. The tidal fluctuation of ground-water lenses, determined on islands of several sizes, ranges from about 4 to 18 inches. In one very small island where the water is brackish, the rise is much greater. The time lag between tidal movements and the rise and fall of fresh water in the islands ranges from a few minutes on very small islands up to 5 hours on some large ones. This time lag is controlled by the permeability of rocks composing an island and varies from one area to another according to the distribution of rock types. The lagoon contains six concentric belts of bottom sediment; in each, the composition and texture depend on the depth of water in which it occurs. Lime sand and lime gravel derived for the most part from the shells of animals form most of the sediment, but a lime mud covers the bottom of the deepest parts of the lagoon. Waves and currents cause gradation between types of sediment to a depth of about 30 feet, but little mixing was detected at greater depths.</span></p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1958)69[241:GOKACI]2.0.CO;2","usgsCitation":"McKee, E.D., 1958, Geology of Kapingamarangi Atoll, Caroline Islands: GSA Bulletin, v. 69, no. 3, p. 241-278, https://doi.org/10.1130/0016-7606(1958)69[241:GOKACI]2.0.CO;2.","productDescription":"37 p.","startPage":"241","endPage":"278","costCenters":[],"links":[{"id":377628,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Federated States of Micronesia","otherGeospatial":"Kapingamarangi Atoll, Caroline Islands","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              151.89697265625,\n              0.21972602392080884\n            ],\n            [\n              157.34619140625,\n              0.21972602392080884\n            ],\n            [\n              157.34619140625,\n              5.834616165610059\n            ],\n            [\n              151.89697265625,\n              5.834616165610059\n            ],\n            [\n              151.89697265625,\n              0.21972602392080884\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"69","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"McKee, Edwin D.","contributorId":60207,"corporation":false,"usgs":true,"family":"McKee","given":"Edwin","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":796633,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70212508,"text":"70212508 - 1958 - Mineralogy and petrology of the currant creek magnesite deposits and associated rocks of Nevada: New data","interactions":[],"lastModifiedDate":"2020-08-18T17:20:47.201955","indexId":"70212508","displayToPublicDate":"1958-08-18T12:16:09","publicationYear":"1958","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"title":"Mineralogy and petrology of the currant creek magnesite deposits and associated rocks of Nevada: New data","docAbstract":"<p><span>No abstract available.</span></p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1958)69[353:MAPOTC]2.0.CO;2","usgsCitation":"Faust, G., and Callaghan, E., 1958, Mineralogy and petrology of the currant creek magnesite deposits and associated rocks of Nevada: New data, v. 69, no. 3, p. 353-354, https://doi.org/10.1130/0016-7606(1958)69[353:MAPOTC]2.0.CO;2.","productDescription":"2 p.","startPage":"353","endPage":"354","costCenters":[],"links":[{"id":377622,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"69","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Faust, George T.","contributorId":15186,"corporation":false,"usgs":true,"family":"Faust","given":"George T.","affiliations":[],"preferred":false,"id":796631,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Callaghan, Eugene","contributorId":79855,"corporation":false,"usgs":true,"family":"Callaghan","given":"Eugene","email":"","affiliations":[],"preferred":false,"id":796632,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}