{"pageNumber":"419","pageRowStart":"10450","pageSize":"25","recordCount":11004,"records":[{"id":56120,"text":"ofr5863 - 1958 - Ground water in the alluvial deposits of the Washita River and its tributaries in Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:12:04","indexId":"ofr5863","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1958","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":"58-63","title":"Ground water in the alluvial deposits of the Washita River and its tributaries in Oklahoma","docAbstract":"Physical features.--The Washita River heads in the Texas Panhandle, in Hemphill, Roberts, and Wheeler Counties. It flows generally east-southeastward through southwestern and south-central Oklahoma to its confluence with the Red River above Denison, Texas, at a point about 4 miles northwest of Cartwright, Oklahoma. That point of confluence is now beneath the waters of Lake Texoma, into which the river flows near Tishomingo in southern Johnston County.\r\nThe average gradient of the Washita River is about 3.7 feet per mile, beginning with an elevation of about 2,800 feet at its source, and ending with an elevation of about 510 feet at its mouth. The river is about 626 miles in length.\r\n\r\nThe total area of the Washita River drainage basin is about 7,945 square miles, of which about 463 square miles is in Texas. The 7,482 square miles of the basin in Oklahoma is in the 17 counties of Roger Mills, Beckham, Comanche, Grady, Stephens, McClain, Custer, Washita, Caddo, Kiowa, Garvin, Carter, Bryan, Murray, Pontotoc, Johnston and Marshall. The river has a winding, sinuous course. In some reaches, such as near Anadarko, it flows in broad meanders 3 or 4 miles across which have incised the bedrock. Throughout its course in Oklahoma the river meanders within its alluvial valley, so that the valley is much shorter than the river channel. In Texas and at the western edge of Oklahoma the Washita flows in a valley cut in rocks of the High Plains; much of the coarse gravel and sand of the alluvium is derived from these rocks. About nine-tenths of the Oklahoma portion of the valley, from western Roger Mills County to near Davis in northern Murray County, is cut in Permian redbeds. These red beds consist largely of shale, siltstone, and fine-grained sandstone. In the western part of the basin, down to about Mountain View in northeastern Kiowa County, they contain irregular layers of gypsum. The gypsum locally forms steep valley walls, such as those along State Highway 152 east of Cordell.\r\n\r\n(available as photostat copy only)","language":"ENGLISH","doi":"10.3133/ofr5863","usgsCitation":"Leonard, A., Davis, L., and Stacy, B., 1958, Ground water in the alluvial deposits of the Washita River and its tributaries in Oklahoma: U.S. Geological Survey Open-File Report 58-63, 13 p., 1 fig., https://doi.org/10.3133/ofr5863.","productDescription":"13 p., 1 fig.","costCenters":[],"links":[{"id":181981,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699ce6","contributors":{"authors":[{"text":"Leonard, A.R.","contributorId":101669,"corporation":false,"usgs":true,"family":"Leonard","given":"A.R.","email":"","affiliations":[],"preferred":false,"id":254789,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davis, L.V.","contributorId":106197,"corporation":false,"usgs":true,"family":"Davis","given":"L.V.","email":"","affiliations":[],"preferred":false,"id":254790,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stacy, B.L.","contributorId":88816,"corporation":false,"usgs":true,"family":"Stacy","given":"B.L.","email":"","affiliations":[],"preferred":false,"id":254788,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":61436,"text":"mf181 - 1958 - Bedrock geology of the southwestern part of the North Range, Cuyuna district, Minnesota","interactions":[],"lastModifiedDate":"2018-12-14T11:19:25","indexId":"mf181","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1958","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"181","title":"Bedrock geology of the southwestern part of the North Range, Cuyuna district, Minnesota","docAbstract":"<p>The Cuyuna manganiferous iron-ore district is in central Minnesota in Morrison, Crow Wing, and Aitkin Counties.&nbsp; The length of the district is about 68 miles, extending northeastward from a point near Randall, in Morrison County, to a point 11 miles east of the community of Hassmann in Aitkin County; the maximum known width is about 25 miles near the center of the district.&nbsp; Current mining activity is confined to a much smaller area, commonly called the North range, about 10 miles long and 3 miles wide near Crosby and Ironton in Crow Wing County.&nbsp; The average annual production of iron ore and manganiferous iron ore during 1940-50 was slightly less than 3 million tons.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf181","usgsCitation":"Schmidt, R.G., 1958, Bedrock geology of the southwestern part of the North Range, Cuyuna district, Minnesota: U.S. Geological Survey Miscellaneous Field Studies Map 181, 3 Sheets: 31.71 x 28.66 inches or smaller, https://doi.org/10.3133/mf181.","productDescription":"3 Sheets: 31.71 x 28.66 inches or smaller","costCenters":[],"links":[{"id":360308,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0181/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":182873,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0181/report-thumb.jpg"},{"id":360309,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0181/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":360310,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0181/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -94.08472222222221,46.41694444444444 ], [ -94.08472222222221,46.5 ], [ -94,46.5 ], [ -94,46.41694444444444 ], [ -94.08472222222221,46.41694444444444 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5ee4b07f02db633f58","contributors":{"authors":[{"text":"Schmidt, R. G.","contributorId":107690,"corporation":false,"usgs":true,"family":"Schmidt","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":265638,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":47375,"text":"b1082A - 1958 - Zirconium and hafnium in the southeastern Atlantic States","interactions":[{"subject":{"id":47375,"text":"b1082A - 1958 - Zirconium and hafnium in the southeastern Atlantic States","indexId":"b1082A","publicationYear":"1958","noYear":false,"chapter":"A","title":"Zirconium and hafnium in the southeastern Atlantic States"},"predicate":"IS_PART_OF","object":{"id":33208,"text":"b1082 - 1962 - Contributions to economic geology, 1958","indexId":"b1082","publicationYear":"1962","noYear":false,"title":"Contributions to economic geology, 1958"},"id":1}],"isPartOf":{"id":33208,"text":"b1082 - 1962 - Contributions to economic geology, 1958","indexId":"b1082","publicationYear":"1962","noYear":false,"title":"Contributions to economic geology, 1958"},"lastModifiedDate":"2017-10-18T13:01:54","indexId":"b1082A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1958","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1082","chapter":"A","title":"Zirconium and hafnium in the southeastern Atlantic States","docAbstract":"<p>The principal source of zirconium and hafnium is zircon, though a minor source is baddeleyite, mined only in Brazil. Zircon is an accessory mineral in igneous, metamorphic, and sedimentary rocks, but rarely occurs in hardrock in minable quantities. The principal sources of zircon are therefore alluvial deposits, which are mined in many countries of five continents. The principal commercial deposits in the United States are in Florida, though others exist elsewhere in the southeastern Coastal Plain. </p><p>The evidence indicates that conditions for the accumulation of workable deposits of heavy minerals were more favorable during the interglacial stages of the Pleistocene epoch than during Recent time. Therefore detrital ores of large volume and high tenor are more likely to be found in the terrace deposits than along the present beaches. Other concentrations of heavy minerals, however, are possible at favored sites close to the Fall Line where the Tuscaloosa formation rests upon the crystalline rocks of the Piedmont province. </p><p>A score of heavy and semiheavy minerals occur in the detrital deposits of Florida, but the principal salable minerals are ilmenite, leucoxene, rutile, and zircon, though monazite and staurolite are saved at some mining plants. Commercial deposits of heavy minerals are generally required to have a tenor of 4 percent, though ores with a lower tenor can be mined at a profit if the content of monazite is notably high. The percentages of zircon in the concentrates ranges from 10 to 16 percent, and in eastern Florida from 13 to 15 percent. Thus the tenor in zircon of the ore-bearing sands ranges from 0.4 to 0.6 percent. </p><p>The content of hafnium in zircon is immaterial for many uses, but for some purposes very high or very low tenors in hafnium are required. Alluvial zircon cannot be separated into such varieties, which, if needed, must be obtained from sources in bedrock. It thus becomes necessary to determine the Hf : Zr ratios in zircon from many kinds of bedrock.</p><p>Granitic rocks are the principal sources of zircon, though not the best sources of zircon with a high tenor in hafnium. A general study by the Geological Survey of the granitic rocks of the Southeastern Atlantic States has been in progress for 10 years, and hundreds of samples of granitic accessory minerals have been acquired. Thirty samples of zircon from these collections were selected for spectrographic and X-ray determinations of their tenors in hafnium. Nine other samples of alluvial zircon were included, of which three are from Florida and six from foreign countries. No domestic zircon was discovered with very high or very low tenors in hafnium.</p><p>The volume of zircon in the southeastern Coastal Plain is enormous, but most of it is not recoverable. The minable reserves of heavy minerals, however, are very large, and from these it is estimated conservatively that 10 million short tons of zircon can be obtained. The corresponding amounts of zirconium and hafnium, using the mean Hf:Zr ratio of the deposits in Florida, are 4,868,000 and 112,000 tons, respectively. These reserves could be delivered, if needed, at the rate of 100,000 tons a year.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to economic geology, 1958","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/b1082A","usgsCitation":"Mertie, J., 1958, Zirconium and hafnium in the southeastern Atlantic States: U.S. Geological Survey Bulletin 1082, 28 p., https://doi.org/10.3133/b1082A.","productDescription":"28 p.","numberOfPages":"28","costCenters":[],"links":[{"id":99993,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1082a/report.pdf","text":"Report","size":"2.08 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":170647,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1082a/report-thumb.jpg"}],"country":"United States","state":"Florida, Georgia, North Carolina, South Carolina, Tennessee, Virginia","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-81.582923,24.658732],[-81.451267,24.747464],[-81.298028,24.656774],[-81.765993,24.552103],[-81.582923,24.658732]]],[[[-84.777208,29.707398],[-84.696726,29.76993],[-85.036219,29.588919],[-84.777208,29.707398]]],[[[-82.255777,26.703437],[-82.038403,26.456907],[-82.186441,26.489221],[-82.255777,26.703437]]],[[[-80.250581,25.34193],[-80.611693,24.93842],[-80.192336,25.473331],[-80.250581,25.34193]]],[[[-81.444124,30.709714],[-81.256711,29.784693],[-80.567361,28.562353],[-80.566432,28.09563],[-80.031362,26.796339],[-80.152896,25.702855],[-80.229107,25.732509],[-80.409103,25.25346],[-80.652253,25.146705],[-81.079859,25.118797],[-81.362272,25.824401],[-81.678287,25.845301],[-81.868983,26.378648],[-82.094748,26.48393],[-82.076349,26.958263],[-82.147068,26.789803],[-82.301736,26.841588],[-82.714521,27.500415],[-82.393383,27.837519],[-82.716522,27.958398],[-82.566819,27.858002],[-82.721622,27.663908],[-82.851126,27.8863],[-82.674787,28.441956],[-82.702618,28.932955],[-83.679219,29.918513],[-84.245668,30.093021],[-84.335953,29.912962],[-85.343619,29.672004],[-85.405052,29.938487],[-86.222561,30.343585],[-87.518324,30.280435],[-87.395941,30.643968],[-87.626228,30.857127],[-87.548543,30.997927],[-85.057534,31.000585],[-85.141831,31.839261],[-84.925427,32.221551],[-85.188741,32.889727],[-85.598781,34.944915],[-90.309297,34.995694],[-90.09061,35.118287],[-90.166594,35.274588],[-89.992975,35.560774],[-89.923161,35.514428],[-89.915491,35.754917],[-89.68182,35.88999],[-89.699677,36.230821],[-89.534507,36.261802],[-89.5391,36.498201],[-88.045304,36.504081],[-88.068208,36.659747],[-87.872062,36.665089],[-83.690714,36.582581],[-83.156696,36.742187],[-81.968297,37.537798],[-81.896001,37.331967],[-81.560625,37.206663],[-81.367052,37.334504],[-81.225104,37.234874],[-80.332038,37.493744],[-79.649075,38.591515],[-79.291813,38.419627],[-79.023053,38.798613],[-78.869276,38.762991],[-78.439429,39.132146],[-78.346718,39.427618],[-77.828157,39.132329],[-77.687124,39.319914],[-77.46021,39.228359],[-77.47701,39.100331],[-77.038898,38.800813],[-77.291103,38.515721],[-77.286202,38.347025],[-77.024866,38.386791],[-76.910832,38.197073],[-76.265998,37.91138],[-76.339892,37.655966],[-76.722156,37.83668],[-76.252415,37.447274],[-76.475927,37.250543],[-76.300352,37.00885],[-76.780532,37.209336],[-76.482407,36.917364],[-75.972151,36.842268],[-75.533012,35.787377],[-75.960069,36.495025],[-75.791637,36.082267],[-76.132005,36.287773],[-76.191715,36.107197],[-76.447812,36.192514],[-76.298733,36.1012],[-76.575936,36.006167],[-76.721445,36.147838],[-76.675462,36.266882],[-76.744436,36.212725],[-76.608052,35.936668],[-76.014685,35.960361],[-76.046813,35.717935],[-75.86042,35.978262],[-75.713502,35.693993],[-76.165392,35.328659],[-76.499251,35.381492],[-76.586349,35.508957],[-76.476706,35.511707],[-76.634468,35.510332],[-76.580187,35.387113],[-77.023912,35.514802],[-76.472273,35.294936],[-76.801426,34.964369],[-76.958465,35.047647],[-76.762931,34.920374],[-76.463468,35.076411],[-76.332044,34.970917],[-76.524712,34.681964],[-76.673619,34.71491],[-76.523303,34.652271],[-76.093349,35.048705],[-76.524199,34.615416],[-76.990262,34.669623],[-77.556943,34.417218],[-77.956881,33.87779],[-78.383964,33.901946],[-78.772737,33.768511],[-79.359961,33.006672],[-79.55756,33.021269],[-79.968468,32.639732],[-80.413487,32.470672],[-80.466342,32.31917],[-80.905378,32.051943],[-80.841913,32.002643],[-81.065255,31.877095],[-81.254218,31.55594],[-81.17831,31.52241],[-81.276862,31.254734],[-81.490586,30.984952],[-81.408484,30.977718],[-81.444124,30.709714]]],[[[-75.753765,35.199612],[-75.523952,35.318198],[-75.533512,35.773577],[-75.52592,35.233839],[-75.982812,35.081513],[-75.753765,35.199612]]],[[[-75.242266,38.027209],[-75.962596,37.117535],[-75.981624,37.434116],[-75.712065,37.936082],[-75.242266,38.027209]]]]},\"properties\":{\"name\":\"Florida\",\"nation\":\"USA 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,{"id":745,"text":"wsp1433 - 1958 - Surface waters of the United States 1956, Part II-A, South Atlantic slope and eastern Gulf of Mexico basins, James River to Savannah River","interactions":[],"lastModifiedDate":"2012-02-02T00:05:09","indexId":"wsp1433","displayToPublicDate":"1994-01-01T00:00:00","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":"1433","title":"Surface waters of the United States 1956, Part II-A, South Atlantic slope and eastern Gulf of Mexico basins, James River to Savannah River","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1433","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1958, Surface waters of the United States 1956, Part II-A, South Atlantic slope and eastern Gulf of Mexico basins, James River to Savannah River: U.S. Geological Survey Water Supply Paper 1433, viii :ill. ; 23 cm., https://doi.org/10.3133/wsp1433.","productDescription":"viii :ill. ; 23 cm.","costCenters":[],"links":[{"id":136382,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1433/report-thumb.jpg"},{"id":25314,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1433/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db6911ea","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527681,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":12418,"text":"ofr581 - 1958 - Geology and ore deposits of the east Shasta copper-zinc district, Shasta County, California","interactions":[{"subject":{"id":12418,"text":"ofr581 - 1958 - Geology and ore deposits of the east Shasta copper-zinc district, Shasta County, California","indexId":"ofr581","publicationYear":"1958","noYear":false,"title":"Geology and ore deposits of the east Shasta copper-zinc district, Shasta County, California"},"predicate":"SUPERSEDED_BY","object":{"id":39060,"text":"pp338 - 1961 - Geology and ore deposits of east Shasta copper-zinc district, Shasta County, California","indexId":"pp338","publicationYear":"1961","noYear":false,"title":"Geology and ore deposits of east Shasta copper-zinc district, Shasta County, California"},"id":1}],"supersededBy":{"id":39060,"text":"pp338 - 1961 - Geology and ore deposits of east Shasta copper-zinc district, Shasta County, California","indexId":"pp338","publicationYear":"1961","noYear":false,"title":"Geology and ore deposits of east Shasta copper-zinc district, Shasta County, California"},"lastModifiedDate":"2025-05-30T17:40:39.77374","indexId":"ofr581","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1958","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":"58-1","title":"Geology and ore deposits of the east Shasta copper-zinc district, Shasta County, California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr581","usgsCitation":"Albers, J.P., 1958, Geology and ore deposits of the east Shasta copper-zinc district, Shasta County, California: U.S. Geological Survey Open-File Report 58-1, Report: xxxvi, 337 p.; 6 Plates: 63.38 x 29.37 inches or smaller, https://doi.org/10.3133/ofr581.","productDescription":"Report: xxxvi, 337 p.; 6 Plates: 63.38 x 29.37 inches or smaller","costCenters":[],"links":[{"id":489313,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1958/0001/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":489312,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1958/0001/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":489311,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1958/0001/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":489310,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1958/0001/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":489309,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1958/0001/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":489308,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1958/0001/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":489307,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1958/0001/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144029,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1958/0001/report-thumb.jpg"}],"country":"United States","state":"California","county":"Shasta County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -123.41344924573305,\n              41.15461559091611\n            ],\n            [\n              -123.41344924573305,\n              39.94270771512089\n            ],\n            [\n              -120.93861877988127,\n              39.94270771512089\n            ],\n            [\n              -120.93861877988127,\n              41.15461559091611\n            ],\n            [\n              -123.41344924573305,\n              41.15461559091611\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db6843ce","contributors":{"authors":[{"text":"Albers, John Patrick","contributorId":26669,"corporation":false,"usgs":true,"family":"Albers","given":"John","email":"","middleInitial":"Patrick","affiliations":[],"preferred":false,"id":166107,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":64317,"text":"gp140 - 1958 - Aeromagnetic map of eastern Roseau County, Minnesota","interactions":[{"subject":{"id":44222,"text":"ofr54206 - 1954 - Total intensity aeromagnetic map of eastern Roseau County, Minnesota","indexId":"ofr54206","publicationYear":"1954","noYear":false,"title":"Total intensity aeromagnetic map of eastern Roseau County, Minnesota"},"predicate":"SUPERSEDED_BY","object":{"id":64317,"text":"gp140 - 1958 - Aeromagnetic map of eastern Roseau County, Minnesota","indexId":"gp140","publicationYear":"1958","noYear":false,"title":"Aeromagnetic map of eastern Roseau County, Minnesota"},"id":1}],"lastModifiedDate":"2025-03-31T18:37:11.56754","indexId":"gp140","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1958","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"140","title":"Aeromagnetic map of eastern Roseau County, Minnesota","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, DC","doi":"10.3133/gp140","collaboration":"Prepared in cooperation with the Minnesota Geological Survey","usgsCitation":"Books, K.G., Schwartz, G.M., Meuschke, J.L., and Dempsey, W., 1958, Aeromagnetic map of eastern Roseau County, Minnesota: U.S. Geological Survey Geophysical Investigations Map 140, 2 Plates: 35.00 x 37.88 inches and  22.21 x 40.51 inches, https://doi.org/10.3133/gp140.","productDescription":"2 Plates: 35.00 x 37.88 inches and  22.21 x 40.51 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":484035,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3053.htm","linkFileType":{"id":5,"text":"html"}},{"id":100773,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0140/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":100771,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0140/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":187374,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0140/report-thumb.jpg"},{"id":100772,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0140/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","county":"Roseau County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -95.916667,\n              49\n            ],\n            [\n              -95.916667,\n              48.541667\n            ],\n            [\n              -95.316667,\n              48.541667\n            ],\n            [\n              -95.316667,\n              49\n            ],\n            [\n              -95.916667,\n              49\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae6e4b07f02db68b305","contributors":{"authors":[{"text":"Books, Kenneth G.","contributorId":25910,"corporation":false,"usgs":true,"family":"Books","given":"Kenneth","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":270550,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schwartz, G. M.","contributorId":20380,"corporation":false,"usgs":true,"family":"Schwartz","given":"G.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":270549,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Meuschke, J. L.","contributorId":53349,"corporation":false,"usgs":true,"family":"Meuschke","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":270551,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dempsey, W.J.","contributorId":13988,"corporation":false,"usgs":true,"family":"Dempsey","given":"W.J.","affiliations":[],"preferred":false,"id":270548,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":64316,"text":"gp143 - 1958 - Aeromagnetic map of eastern Marshall and northwestern Beltrami Counties, Minnesota","interactions":[{"subject":{"id":44260,"text":"ofr54202 - 1954 - Total intensity aeromagnetic map of eastern Marshall and northwestern Beltrami Counties, Minnesota","indexId":"ofr54202","publicationYear":"1954","noYear":false,"title":"Total intensity aeromagnetic map of eastern Marshall and northwestern Beltrami Counties, Minnesota"},"predicate":"SUPERSEDED_BY","object":{"id":64316,"text":"gp143 - 1958 - Aeromagnetic map of eastern Marshall and northwestern Beltrami Counties, Minnesota","indexId":"gp143","publicationYear":"1958","noYear":false,"title":"Aeromagnetic map of eastern Marshall and northwestern Beltrami Counties, Minnesota"},"id":1}],"lastModifiedDate":"2021-12-08T19:33:14.909721","indexId":"gp143","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1958","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"143","title":"Aeromagnetic map of eastern Marshall and northwestern Beltrami Counties, Minnesota","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp143","usgsCitation":"Books, K.G., Schwartz, G.M., Meuschke, J.L., and Dempsey, W., 1958, Aeromagnetic map of eastern Marshall and northwestern Beltrami Counties, Minnesota: U.S. Geological Survey Geophysical Investigations Map 143, 2 Plates: 39.49 × 32.18 inches and 17.36 × 46.93 Inches, https://doi.org/10.3133/gp143.","productDescription":"2 Plates: 39.49 × 32.18 inches and 17.36 × 46.93 Inches","costCenters":[],"links":[{"id":392635,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3056.htm"},{"id":187316,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0143/report-thumb.jpg"},{"id":100770,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0143/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":100769,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0143/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":100768,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0143/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"63360","country":"United States","state":"Minnesota","county":"Beltrami County, Marshall County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -95.987548828125,\n              48.17707562779612\n            ],\n            [\n              -95.284423828125,\n              48.17707562779612\n            ],\n            [\n              -95.284423828125,\n              48.52024290640028\n            ],\n            [\n              -95.987548828125,\n              48.52024290640028\n            ],\n            [\n              -95.987548828125,\n              48.17707562779612\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689e3d","contributors":{"authors":[{"text":"Books, Kenneth G.","contributorId":25910,"corporation":false,"usgs":true,"family":"Books","given":"Kenneth","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":270546,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schwartz, G. M.","contributorId":20380,"corporation":false,"usgs":true,"family":"Schwartz","given":"G.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":270545,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Meuschke, J. L.","contributorId":53349,"corporation":false,"usgs":true,"family":"Meuschke","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":270547,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dempsey, W.J.","contributorId":13988,"corporation":false,"usgs":true,"family":"Dempsey","given":"W.J.","affiliations":[],"preferred":false,"id":270544,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":60472,"text":"mf126 - 1958 - Preliminary tectonic map of eastern Montana, showing the distribution of uranium deposits","interactions":[],"lastModifiedDate":"2024-02-22T21:26:50.199129","indexId":"mf126","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1958","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"126","title":"Preliminary tectonic map of eastern Montana, showing the distribution of uranium deposits","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf126","collaboration":"Prepared in cooperation with the U.S. Atomic Energy Commission","usgsCitation":"Osterwald, F.W., and Dean, B., 1958, Preliminary tectonic map of eastern Montana, showing the distribution of uranium deposits: U.S. Geological Survey Miscellaneous Field Studies Map 126, 2 Plates: 33.85 x 21.99 inches and 33.78 x 21.90 inches, https://doi.org/10.3133/mf126.","productDescription":"2 Plates: 33.85 x 21.99 inches and 33.78 x 21.90 inches","costCenters":[],"links":[{"id":261798,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1958/0126/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":182659,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":261799,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1958/0126/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":425884,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2538.htm","linkFileType":{"id":5,"text":"html"}},{"id":261800,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1958/0126/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Montana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109.1269,\n              49\n            ],\n            [\n              -109.1269,\n              46\n            ],\n            [\n              -104.0542,\n              46\n            ],\n            [\n              -104.0542,\n              49\n            ],\n            [\n              -109.1269,\n              49\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db628102","contributors":{"authors":[{"text":"Osterwald, F. W.","contributorId":46950,"corporation":false,"usgs":true,"family":"Osterwald","given":"F.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":263813,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dean, B.G.","contributorId":18845,"corporation":false,"usgs":true,"family":"Dean","given":"B.G.","email":"","affiliations":[],"preferred":false,"id":263812,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":60477,"text":"mf127 - 1958 - Preliminary tectonic map of Wyoming, east of the overthrust belt, showing distribution of uranium deposits","interactions":[],"lastModifiedDate":"2018-12-14T11:25:39","indexId":"mf127","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1958","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"127","title":"Preliminary tectonic map of Wyoming, east of the overthrust belt, showing distribution of uranium deposits","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf127","usgsCitation":"Osterwald, F.W., and Dean, B., 1958, Preliminary tectonic map of Wyoming, east of the overthrust belt, showing distribution of uranium deposits: U.S. Geological Survey Miscellaneous Field Studies Map 127, 63.81 x 39.77 inches, https://doi.org/10.3133/mf127.","productDescription":"63.81 x 39.77 inches","costCenters":[],"links":[{"id":360315,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0127/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":182753,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0127/report-thumb.jpg"}],"country":"United States","state":"Wyoming","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111,41 ], [ -111,45 ], [ -104,45 ], [ -104,41 ], [ -111,41 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de66f","contributors":{"authors":[{"text":"Osterwald, F. W.","contributorId":46950,"corporation":false,"usgs":true,"family":"Osterwald","given":"F.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":263823,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dean, B.G.","contributorId":18845,"corporation":false,"usgs":true,"family":"Dean","given":"B.G.","email":"","affiliations":[],"preferred":false,"id":263822,"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":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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,{"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":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":70212070,"text":"70212070 - 1958 - Uranium deposits under conglomeratic sandstone of the Morrison Formation, Colorado and Utah","interactions":[],"lastModifiedDate":"2020-08-14T14:05:19.628286","indexId":"70212070","displayToPublicDate":"1958-08-13T11:40:12","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":"Uranium deposits under conglomeratic sandstone of the Morrison Formation, Colorado and Utah","docAbstract":"<p><span>In southwestern Colorado and southeastern Utah, strata of conglomeratic sandstone are localized at the base of the Brushy Basin Member of the Morrison Formation of Jurassic age. These discrete lithologic units contain sedimentary structures oriented in a prevailing easterly direction. They are believed to cover about one-third of the underlying Salt Wash Member in southwestern Colorado and southeastern Utah, and they locally rest on ore-bearing sandstone in the Salt Wash Member. Eastward-trending planar cross-stratification and trough cross-stratification and a general westward coarsening of sediments in the conglomeratic sandstone strata suggest that they are the products of stream aggradation from westerly source areas. Uranium-vanadium deposits in the uppermost, almost continuous, layer of sandstone of the Salt Wash Member are classified according to their association with the conglomerate strata. Of the 363 deposits studied in the uppermost sandstone layer of the Salt Wash Member, 101 are known to be directly beneath conglomeratic sandstone strata, 211 are below the projected extension of conglomeratic sandstone strata, 33 are beyond the safe limits of such projection, and 18 are lateral to the margins of conglomeratic sandstone strata. At places, near clusters of deposits in the uppermost sandstone of the underlying Salt Wash Member, conglomeratic sandstone strata of the Brushy Basin Member are also mineralized. It is postulated that ground-water movement during deposition of the Morrison Formation in Late Jurassic time localized the uranium and vanadium. The direction of this ground-water movement is believed to have been related to streams that deposited the conglomeratic strata, so that in the ore-bearing sandstone metal ions contained in the ground water were localized in places of high transmissibility and in the vicinity of decaying organic debris. According to the age of the ores, precipitation of the metals was much later than their localization, probably during Late Cretaceous or early Tertiary time.</span></p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1958)69[403:UDUCSO]2.0.CO;2","usgsCitation":"Phoenix, D.A., 1958, Uranium deposits under conglomeratic sandstone of the Morrison Formation, Colorado and Utah: GSA Bulletin, v. 69, no. 4, p. 403-418, https://doi.org/10.1130/0016-7606(1958)69[403:UDUCSO]2.0.CO;2.","productDescription":"16 p.","startPage":"403","endPage":"418","costCenters":[],"links":[{"id":377497,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado, Utah","otherGeospatial":"Morrison Formation","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.0830078125,\n              37.020098201368114\n            ],\n            [\n              -108.160400390625,\n              37.020098201368114\n            ],\n            [\n              -108.160400390625,\n              39.16414104768742\n            ],\n            [\n              -110.0830078125,\n              39.16414104768742\n            ],\n            [\n              -110.0830078125,\n              37.020098201368114\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"69","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Phoenix, D. A.","contributorId":92665,"corporation":false,"usgs":true,"family":"Phoenix","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":796222,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5220127,"text":"5220127 - 1957 - Eastern glossy ibis nesting in southeastern Maryland","interactions":[],"lastModifiedDate":"2017-06-07T12:18:07","indexId":"5220127","displayToPublicDate":"2010-06-16T12:18:25","publicationYear":"1957","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3544,"text":"The Auk","onlineIssn":"1938-4254","printIssn":"0004-8038","active":true,"publicationSubtype":{"id":10}},"title":"Eastern glossy ibis nesting in southeastern Maryland","docAbstract":"<p>On June 25, 1956, Don P. Fankhauser and I investigated a large heron colony of mixed species, on Mills Island in Chincoteague Bay, Worcester County, Maryland. Large numbers of American Egrets (<i>Casmerodius albus</i>), Snowy Egrets (<i>Leucophoyx</i> <i>thula</i>), Louisiana Herons (<i>Hydranassa tricolor</i>), Little Blue Herons (<i>Florida caerulea</i>), and Black-crowned Night Herons (<i>Nycticorax nycticorax</i>) were found, all nesting in a dense grove of young red cedar (<i>Juniperus virginiana</i>). Much to our surprise, the colony also included at least two pairs of the Eastern Glossy Ibis (<i>Plegadis falcinellus</i>). Four adults of this species were repeatedly observed flying low overhead and frequently perching in nearby tree-tops. In addition, two young ibis, about three-fourths grown, were found. These two birds, still unable to fly, would hop and flutter among the tree branches whenever they were approached too closely. The large white crown patch and the peculiar barred markings of the bill were especially noticeable on both of the young.</p>","language":"English","publisher":"American Ornithological Society","doi":"10.2307/4081758","usgsCitation":"Stewart, R.E., 1957, Eastern glossy ibis nesting in southeastern Maryland: The Auk, v. 74, no. 4, p. 509-509, https://doi.org/10.2307/4081758.","productDescription":"1 p.","startPage":"509","endPage":"509","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":480406,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2307/4081758","text":"Publisher Index Page"},{"id":193672,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryland","county":"Worcester County","otherGeospatial":"Chincoteague Bay, Mills Island","volume":"74","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db6283de","contributors":{"authors":[{"text":"Stewart, R. E.","contributorId":93426,"corporation":false,"usgs":true,"family":"Stewart","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":331379,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56086,"text":"ofr5789 - 1957 - Seventh progress report on the cooperative investigation of springs and streamflow in the Tecolote tunnel area of Santa Barbara County, California","interactions":[],"lastModifiedDate":"2014-05-21T09:31:00","indexId":"ofr5789","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1957","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":"57-89","title":"Seventh progress report on the cooperative investigation of springs and streamflow in the Tecolote tunnel area of Santa Barbara County, California","docAbstract":"<p>This report is the seventh in a a continuing series of progress reports giving the results of discharge measurements made at selected springs and streams in the Tecolote Tunnel are area of the Santa Ynez  Mountains. The mountains. The measurement program was begun on its present scale in the latter part of 1948 by the Geological Survey at the request of the Santa Barbara County Water Agency and is being continued under a cooperative agreement whereby each agency pays half the cost of the investigation.</p>\n<br>\n<p>The purpose of the program is to obtain sufficient factual data to determine what effect, if any, the inflow of ground water into Tecolote Tunnel will have on the flow of springs and streams in the vicinity of the tunnel. The area involved in the study, shown by plate 1, was made large enough to include a number of springs and steams believe to be outside the zone of influence of the tunnel.</p>\n<br>\n<p>Tecolote Tunnel, completed late in 1955, was built by the Bureau of Reclamation for the purpose of conveying water stored in Cachuma Reservoir to the city of Santa Barbara and adjacent coastal communities. The alinement of the tunnel is roughly north and south through the center of the arbitrarily chosen study area which extends from the Painted Cave area on the east to Refugio Pass on the west and from the Santa Ynez River on the North to the Pacific Ocean on the south.</p>\n<br>\n<p>The purpose of this report is to make available the factual data obtained from July 1954 to June 1956, together with a brief presentation of precipitation, springflow, and tunnel outflow for the entire period of investigation.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr5789","collaboration":"Prepared in cooperation with the Santa Barbara County Water Agency","usgsCitation":"Peterson, W.C., 1957, Seventh progress report on the cooperative investigation of springs and streamflow in the Tecolote tunnel area of Santa Barbara County, California: U.S. Geological Survey Open-File Report 57-89, 138 p., https://doi.org/10.3133/ofr5789.","productDescription":"138 p.","numberOfPages":"138","temporalStart":"1954-07-01","temporalEnd":"1956-06-30","costCenters":[],"links":[{"id":287405,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":287404,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1957/0089/report.pdf"}],"scale":"50000","country":"United States","state":"California","county":"Santa Barbara County","otherGeospatial":"Tecolote Tunnel","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.083333,34.633333 ], [ -120.083333,34.416667 ], [ -119.75,34.416667 ], [ -119.75,34.633333 ], [ -120.083333,34.633333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f4b58","contributors":{"authors":[{"text":"Peterson, W. C.","contributorId":57051,"corporation":false,"usgs":true,"family":"Peterson","given":"W.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":254746,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14401,"text":"ofr5760 - 1957 - Records available to September 30, 1956, on use of water in the Delaware Basin Project area","interactions":[],"lastModifiedDate":"2014-05-21T08:30:12","indexId":"ofr5760","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1957","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":"57-60","title":"Records available to September 30, 1956, on use of water in the Delaware Basin Project area","docAbstract":"<p>The purpose of this report is to summarize data on the use of water in the Delaware Basin Project area (fig. 2) and to list the principal data sources that are available in published form. The tables and bibliography will assist Geological Survey personnel  assigned to the Delaware Basin Project in evaluating the scope and deficiencies of previous studies of the basin. Information is also given on the use of water by public supplies in the New York-New Jersey region comprising the New York City Metropolitan Area and in the remaining north-central and south-eastern parts of New Jersey. These regions may depend increasingly on water from the Delaware River basin for part of their public supplies.</p>\n<br>\n<p>The Geological Survey has the responsibility for appraising and describing the water resources of the Nation as a guide to use, development, control, and conservation of these resources. Cooperative Federal-State water-resources investigations in the Delaware Basin States have been carried on the the Geological Survey for more than 50 years. In July 1956 the Survey began the \"Delaware Basin Project,\" a hydrologic study of the Delaware River basin in order to: 1) Determine present status and trends in water availability, quality, and use, 2) assess and improve the adequacy of the Survey's basic water data program in the basin, 3) interpret and evaluate the water-resources data in terms of past and possible future water-use and land-use practices, and 4) disseminate promptly the results of this investigation for the benefit of all interested agencies and the general public. The Geological Survey is working closely with the U.S. Corps of Engineers and other cooperating Federal and State agencies in providing water data which will contribute to the present coordinated investigation aimed at developing a plan for long-range water development in the Delaware River basin.</p>\n<br>\n<p>Estimates of quantities of water used are given for water withdrawn from streams and aquifers during calendar year 1955, as compiled or estimated from publications and manuscripts prepared between 1950 and 1956. All quantities are given in millions of gallons per day (mgd). The source of the water used, ground or surface, and the type of use to which is was put -- public supply, industrial supply, irrigation, or rural use -- is given. Use of water for hydroelectric power was not compiled for this report. Most tables in this report do not subdivide withdrawals into fresh and saline water; however, most supplies are fresh, except some of those withdrawn directly from the Delaware River downstream from Philadelphia, Pa. All quantities are expressed as an average rate for a full year and are lower, therefore, than rates resulting from the increased demand for water during the summer for air conditioning and supplemental irrigation.</p>\n<br>\n<p>The primary emphasis of this study was to get an over-all picture of water use throughout large parts of the basin. Therefore, publications relating to a dingle city or county, other than New York City, seldom were used; revisions and refinement based on such sources of information are best made by the field personnel most familiar with locally filed publications and published data. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington D.C.","doi":"10.3133/ofr5760","usgsCitation":"Kammerer, J., 1957, Records available to September 30, 1956, on use of water in the Delaware Basin Project area: U.S. Geological Survey Open-File Report 57-60, ii, 33 p., https://doi.org/10.3133/ofr5760.","productDescription":"ii, 33 p.","numberOfPages":"37","costCenters":[],"links":[{"id":287385,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":287384,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1957/0060/report.pdf"}],"country":"United States","state":"Delaware","otherGeospatial":"Delaware Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -76.0,39.0 ], [ -76.0,42.0 ], [ -75.0,42.0 ], [ -75.0,39.0 ], [ -76.0,39.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db63579e","contributors":{"authors":[{"text":"Kammerer, John C.","contributorId":53815,"corporation":false,"usgs":true,"family":"Kammerer","given":"John C.","affiliations":[],"preferred":false,"id":169392,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15450,"text":"ofr5791 - 1957 - Glacial features and surficial deposits of the Malaspina district, Alaska","interactions":[{"subject":{"id":15450,"text":"ofr5791 - 1957 - Glacial features and surficial deposits of the Malaspina district, Alaska","indexId":"ofr5791","publicationYear":"1957","noYear":false,"title":"Glacial features and surficial deposits of the Malaspina district, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":66820,"text":"i271 - 1958 - Glacial features and surficial deposits of the Malaspina district, Alaska","indexId":"i271","publicationYear":"1958","noYear":false,"title":"Glacial features and surficial deposits of the Malaspina district, Alaska"},"id":1}],"supersededBy":{"id":66820,"text":"i271 - 1958 - Glacial features and surficial deposits of the Malaspina district, Alaska","indexId":"i271","publicationYear":"1958","noYear":false,"title":"Glacial features and surficial deposits of the Malaspina district, Alaska"},"lastModifiedDate":"2024-01-26T21:33:37.679674","indexId":"ofr5791","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1957","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":"57-91","title":"Glacial features and surficial deposits of the Malaspina district, Alaska","docAbstract":"<p>The Malaspina district extends about 50 miles along the north shore of the Gulf of Alaska from Icy Bay and the Guyot Glacier on the west to Yakutat Bay and Disenchantment Bay on the east (see index map). The district includes a coastal lowland flanked on the north by a belt of rugged foothills, the higher ridges and peaks of which rise to altitudes of 1,000 to 6,000 feet. The southern front of the St. Ell as Mountains rises abruptly at the northern margin of the foothills belt, about 30 miles from the coast, culminating in Mount St. Elias (18,008 ft.).</p><p>The Malaspina Glacier, the dominant feature of the Malaspina district, has long been regarded as the type example of the piedmont glacier. This huge ice sheet covers an area of about 840 square miles of the coastal lowland, rising gradually from an altitude of 100 feet or less at the outer margin to altitudes ranging from 1,000 feet to 2,000 feet at the southern margin of the foothills belt. The Malaspina Glacier is of special interest to glaciologists because its strikingly developed morainic banding offers clues to the nature of glacier movement. The processes of wastage and deposition at the stagnant margin of Malaspina Glacier can be compared with the mode of retreat of the former continental ice sheets; much can be learned here of the origin<br>of the deposits formed along a stagnant ice margin.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5791","usgsCitation":"Plafker, G., and Miller, D.J., 1957, Glacial features and surficial deposits of the Malaspina district, Alaska: U.S. Geological Survey Open-File Report 57-91, Report: 13 p.; 2 Plates: 22.64 x 45.69 inches and 48.66 x 41.99 inches, https://doi.org/10.3133/ofr5791.","productDescription":"Report: 13 p.; 2 Plates: 22.64 x 45.69 inches and 48.66 x 41.99 inches","costCenters":[],"links":[{"id":149011,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1957/0091/report-thumb.jpg"},{"id":425068,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1957/0091/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":425067,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1957/0091/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":425066,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1957/0091/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"96000","country":"United States","state":"Alaska","otherGeospatial":"Malaspina district","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -141.31365442885615,\n              60.237641221178194\n            ],\n            [\n              -141.31365442885615,\n              59.68683300309837\n            ],\n            [\n              -139.80902050605346,\n              59.68683300309837\n            ],\n            [\n              -139.80902050605346,\n              60.237641221178194\n            ],\n            [\n              -141.31365442885615,\n              60.237641221178194\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db679cfb","contributors":{"authors":[{"text":"Plafker, George","contributorId":3920,"corporation":false,"usgs":false,"family":"Plafker","given":"George","email":"","affiliations":[],"preferred":false,"id":171152,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, Don John","contributorId":77120,"corporation":false,"usgs":true,"family":"Miller","given":"Don","email":"","middleInitial":"John","affiliations":[],"preferred":false,"id":171153,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56083,"text":"ofr5783 - 1957 - Streamflow East Fork Bruneau River below Three Creek, near Three Creek, Idaho","interactions":[],"lastModifiedDate":"2019-11-25T16:13:14","indexId":"ofr5783","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1957","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":"57-83","title":"Streamflow East Fork Bruneau River below Three Creek, near Three Creek, Idaho","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr5783","usgsCitation":"Newell, T.R., 1957, Streamflow East Fork Bruneau River below Three Creek, near Three Creek, Idaho: U.S. Geological Survey Open-File Report 57-83, 42 p., 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,{"id":2368,"text":"wsp1330D - 1957 - Water requirements of the rayon- and acetate-fiber industry","interactions":[{"subject":{"id":2368,"text":"wsp1330D - 1957 - Water requirements of the rayon- and acetate-fiber industry","indexId":"wsp1330D","publicationYear":"1957","noYear":false,"chapter":"D","title":"Water requirements of the rayon- and acetate-fiber industry"},"predicate":"IS_PART_OF","object":{"id":70188911,"text":"wsp1330 - 1955 - Water requirements of selected industries","indexId":"wsp1330","publicationYear":"1955","noYear":false,"title":"Water requirements of selected industries"},"id":1}],"isPartOf":{"id":70188911,"text":"wsp1330 - 1955 - Water requirements of selected industries","indexId":"wsp1330","publicationYear":"1955","noYear":false,"title":"Water requirements of selected industries"},"lastModifiedDate":"2017-06-27T14:04:40","indexId":"wsp1330D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1957","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":"1330","chapter":"D","title":"Water requirements of the rayon- and acetate-fiber industry","docAbstract":"<p>Water is required for several purposes in the manufacture of rayon and acetate fiber. These water requirements, as indicated by a survey of the water used by the plants operating in 1953, are both quantitative and qualitative. </p><p>About 300 mgd (million gallons per day) of water was used in 1953 in the preparation of purified wood cellulose and cotton linters, the basic material from which the rayon and acetate fiber is made. An additional 620 mgd was used in the process of converting the cellulose to rayon and acetate fiber. The total, 920 mgd, is about 1 percent of the total estimated withdrawals of industrial water in the United States in 1953. </p><p>The rayon- and acetate-fiber plants are scattered through eastern United States and generally are located in small towns or rural areas where there are abundant supplies of clean, soft water. Water use at a typical rayon-fiber plant was about 9 mgd, and at a typical acetate-fiber plant about 38 mgd. </p><p>About 110 gallons of water was used to produce a pound of rayon fiber 32 gallons per pound was process water and the remainder was used largely for cooling in connection with power production and air conditioning. For the manufacture of a pound of acetate fiber about 170 gallons of water was used. However, the field survey on which this report is based indicated a wide range in the amount of water used per pound of product. For example, in the manufacture of viscose rayon, the maximum unit water use was 8 times the minimum unit water use. Water use in summer was about 22 percent greater than average annual use. About 8 mgd of water was consumed by evaporation in the manufacture of rayon and acetate fiber. </p><p>More than 90 percent of the water used by the rayon and acetate industry was withdrawn from surface-water sources, about 8 percent from ground water, and less than 2 percent from municipal water supplies. </p><p>All available analyses of the untreated waters used by the rayon and acetate industry were collected and studied. The untreated waters were generally cool, low in content of calcium and magnesium, and very low in iron and manganese. At many plants, water was obtained from more than one source, and thus had different quality characteristics. Dissolved solids in all the untreated waters analyzed ranged between 14 and 747 ppm (parts per million) but in those waters used in processing the dissolved solids content was less than 200 ppm. </p><p>The cooling water used by the industry is also generally of very high quality, principally because the requirements for a high-quality process water necessitate location of the plants in areas where such water is available.</p>","largerWorkTitle":"Water requirements of selected industries","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp1330D","usgsCitation":"Mussey, O.D., 1957, Water requirements of the rayon- and acetate-fiber industry: U.S. Geological Survey Water Supply Paper 1330, vi, 39 p., https://doi.org/10.3133/wsp1330D.","productDescription":"vi, 39 p.","startPage":"141","endPage":"179","costCenters":[],"links":[{"id":28307,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1330d/report.pdf","text":"Report","size":"867.98 kB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":137742,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1330d/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47c8e4b07f02db4ab9b1","contributors":{"authors":[{"text":"Mussey, Orville Durey","contributorId":45688,"corporation":false,"usgs":true,"family":"Mussey","given":"Orville","email":"","middleInitial":"Durey","affiliations":[],"preferred":false,"id":145088,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2113,"text":"wsp1421 - 1957 - Geology and ground-water resources of Outagamie County, Wisconsin","interactions":[],"lastModifiedDate":"2015-10-05T09:02:03","indexId":"wsp1421","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1957","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":"1421","title":"Geology and ground-water resources of Outagamie County, Wisconsin","docAbstract":"<p>Outagamie County is in east-central Wisconsin. It has no serious groundwater problem at present, but the county is important as a recharge area for the principal aquifers supplying water to Brown County and industrial Green Bay to the east.</p>\n<p>The county is covered by glacial drift and lake deposits of the Wisconsin stage of glaciation. In the northwestern quarter of the county these deposits rest upon Precambrian crystalline rocks; throughout the remainder of the county they are underlain by sandstone, limestone, dolomite, and shale of Cambrian and Ordovician age. &middot;where they are sufficiently thick, and where more productive formations are absent, glacial sand and gravel are an important source of ground water. The major sources, however, are the St. Peter sandstone, of Ordovician age, and the sandstones of the Upper Cambrian series. The Precambrian crystalline rocks, which underlie all the county, yield little or no water to wells.</p>\n<p>The regional dip of the Paleozoic bedrocks is 25 to 30 feet per mile eastward and southeastward. There are no major folds, but the thickness of each geologic unit may change from place to place because of predepositional or postdepositional erosion. There is no conclusive evidence of major faulting in the area.</p>\n<p>Ground water in Outagamie County occurs under both water-table (unconfined) and artesian (confined) conditions. The source of the ground water is precipitation which falls on the surface and percolates downward into the underlying permeable materials. Regional movement of ground water in the eastern third of the county is controlled by the bedrock structure, and the discharge is toward the east and south. Throughout the rest of the county the movement of water is controlled mainly by bedrock and surface topography, and the water moves toward the streams and bedrock valleys.</p>\n<p>Water-level :fluctuations follow definite patterns. Where the effects of pumping are at a minimum, water levels reach a high in April or May, decline through the summer months owing to natural discharge, and lack of recharge, and do not begin to recover until after the ground thaws in the spring. In areas of heavy pumping where this pattern is distorted, the lowest water levels occur in the early fall and recoveries begin in October or November after the period of heaviest pumping.</p>\n<p>Pumpage in the county was estimated to be about 9.0 million gallons per day (mgd) in 1951 and 1952. Nearly half of this was for industrial, commercial, and public-supply use along the Fox River. Wells, most of which are drilled by the cable-tool method, range in diameter from 3 to 16 inches and in depth from 10 or 20 feet to 804 feet. In the alluvium and glacial drift 1~- to 2&yen;2-inch driven wells are common.</p>\n<p>Pumping tests were made to determine the hydraulic characteristics of the aquifers at Seymour, Appleton, and Hortonville. The average coefficient of transmissibility at Seymour is about 18,000 gpd per foot; at Appleton it is about 19,000 gpd per foot. The coefficients of storage are 0.00022 and 0.00015 at Seymour and Appleton, respectively. Movement of ground water out of the county, assuming an average transmissibility of 18,000 gpd per foot, was calculated to be more than 10 mgd toward the southeast.</p>\n<p>The ground water differs greatly in chemical quality from well to well, but it is generally a very hard calcium magnesium bicarbonate water, some of it high in iron. To aid in determining the source of well waters, 22 chemical analyses were plotted on a logarithmic diagram to obtain characteristic patterns for waters from several geologic sources.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1421","usgsCitation":"LeRoux, E.F., 1957, Geology and ground-water resources of Outagamie County, Wisconsin: U.S. Geological Survey Water Supply Paper 1421, Report: 57 p.; 7 Plates: 26.60 x 19.80 inches or smaller, https://doi.org/10.3133/wsp1421.","productDescription":"Report: 57 p.; 7 Plates: 26.60 x 19.80 inches or smaller","numberOfPages":"57","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":138327,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1421/report-thumb.jpg"},{"id":27696,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1421/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27695,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1421/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27689,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1421/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27693,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1421/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27694,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1421/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27690,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1421/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27691,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1421/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27692,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1421/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","county":"Outagamie County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-88.6062,44.5903],[-88.4889,44.5894],[-88.3671,44.5875],[-88.2453,44.5846],[-88.2203,44.5858],[-88.1908,44.5864],[-88.1918,44.5016],[-88.1921,44.4167],[-88.1921,44.3871],[-88.1919,44.3288],[-88.193,44.2421],[-88.2536,44.2432],[-88.2835,44.243],[-88.3754,44.2443],[-88.4041,44.244],[-88.4966,44.2443],[-88.5247,44.2441],[-88.6185,44.2438],[-88.6453,44.2435],[-88.7397,44.2432],[-88.7381,44.3307],[-88.7365,44.4164],[-88.7368,44.5021],[-88.7371,44.5906],[-88.6152,44.5903],[-88.6062,44.5903]]]},\"properties\":{\"name\":\"Outagamie\",\"state\":\"WI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db6859f8","contributors":{"authors":[{"text":"LeRoux, E. F.","contributorId":29795,"corporation":false,"usgs":true,"family":"LeRoux","given":"E.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":144693,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56089,"text":"ofr5796 - 1957 - Surface water supply of eastern and central North Carolina","interactions":[],"lastModifiedDate":"2016-12-09T11:11:51","indexId":"ofr5796","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1957","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":"57-96","title":"Surface water supply of eastern and central North Carolina","docAbstract":"None of the many factors that influence the economic growth of eastern and central North Carolina plays a more important role than water. Adequate water supply for municipal, rural domestic, industrial, and agricultural uses, is a basic need of any region.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5796","collaboration":"Prepared in cooperation with Division of Water Resources, Inlets and Coastal Waterways, North Carolina Department of Conservation and Development","usgsCitation":"Rice, E.B., 1957, Surface water supply of eastern and central North Carolina: U.S. Geological Survey Open-File Report 57-96, v, 92 p., https://doi.org/10.3133/ofr5796.","productDescription":"v, 92 p.","numberOfPages":"96","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":287409,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":287408,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1957/0096/report.pdf"}],"country":"United States","state":"North 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,{"id":61225,"text":"mf68 - 1957 - Preliminary geologic map of the east-central part of the Minnekahta quadrangle, Fall River County, South Dakota","interactions":[],"lastModifiedDate":"2018-12-10T10:43:22","indexId":"mf68","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1957","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"68","title":"Preliminary geologic map of the east-central part of the Minnekahta quadrangle, Fall River County, South Dakota","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf68","usgsCitation":"Wilmarth, V., and Smith, R., 1957, Preliminary geologic map of the east-central part of the Minnekahta quadrangle, Fall River County, South Dakota: U.S. Geological Survey Miscellaneous Field Studies Map 68, 36.66 x 32.51 inches, https://doi.org/10.3133/mf68.","productDescription":"36.66 x 32.51 inches","costCenters":[],"links":[{"id":360093,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0068/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":183172,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0068/report-thumb.jpg"}],"country":"United States","state":"South Dakota","county":"Fall River County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.68361111111112,43.416666666666664 ], [ -103.68361111111112,43.450833333333335 ], [ -103.61749999999999,43.450833333333335 ], [ -103.61749999999999,43.416666666666664 ], [ -103.68361111111112,43.416666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db674316","contributors":{"authors":[{"text":"Wilmarth, V.R.","contributorId":20803,"corporation":false,"usgs":true,"family":"Wilmarth","given":"V.R.","email":"","affiliations":[],"preferred":false,"id":265213,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, R.D.","contributorId":6529,"corporation":false,"usgs":true,"family":"Smith","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":265212,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":55764,"text":"ofr5738 - 1957 - Memorandum on availability of ground water for irrigation in certain areas of eastern Arkansas","interactions":[],"lastModifiedDate":"2014-05-21T08:09:20","indexId":"ofr5738","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1957","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":"57-38","title":"Memorandum on availability of ground water for irrigation in certain areas of eastern Arkansas","docAbstract":"This memorandum was prepared in response to a request from the Soil Conservation Service, Little Rock, Ark., for information on the future prospects of irrigation of rice with water from wells in certain areas in the basins of the Bache, St. Francis, and L'Anguille Rivers, Big and Dials Creeks, and Bayou Meto and the Bouef-Tensas-Macon basin. It was prepared as a aprt of the Statewide ground-water investigation in cooperation with the Arkansas Geological and Conservation Commission ad the University of Arkansas. The specific areas and water requirement specified by the Soil Conservation Service are listed in the appendix.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5738","usgsCitation":"Dennis, P., and and others, 1957, Memorandum on availability of ground water for irrigation in certain areas of eastern Arkansas: U.S. Geological Survey Open-File Report 57-38, 10 p., https://doi.org/10.3133/ofr5738.","productDescription":"10 p.","numberOfPages":"12","costCenters":[],"links":[{"id":287373,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":287372,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1957/0038/report.pdf"}],"country":"United States","state":"Arkansas","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -94.6179,33.0041 ], [ -94.6179,36.4997 ], [ -89.6468,36.4997 ], [ -89.6468,33.0041 ], [ -94.6179,33.0041 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ce4b07f02db613d5c","contributors":{"authors":[{"text":"Dennis, P.E.","contributorId":73627,"corporation":false,"usgs":true,"family":"Dennis","given":"P.E.","email":"","affiliations":[],"preferred":false,"id":254211,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"and others","contributorId":127886,"corporation":true,"usgs":false,"organization":"and others","id":532394,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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