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,{"id":52217,"text":"ofr626 - 1962 - Geology and ground-water resources of the southern part of the Jicarilla Apache Indian Reservation and adjacent region to the south and east, New Mexico","interactions":[{"subject":{"id":52217,"text":"ofr626 - 1962 - Geology and ground-water resources of the southern part of the Jicarilla Apache Indian Reservation and adjacent region to the south and east, New Mexico","indexId":"ofr626","publicationYear":"1962","noYear":false,"title":"Geology and ground-water resources of the southern part of the Jicarilla Apache Indian Reservation and adjacent region to the south and east, New Mexico"},"predicate":"SUPERSEDED_BY","object":{"id":977,"text":"wsp1576H - 1967 - Ground-water resources of the southern part of Jicarilla Apache Indian Reservation and adjacent areas, New Mexico","indexId":"wsp1576H","publicationYear":"1967","noYear":false,"chapter":"H","title":"Ground-water resources of the southern part of Jicarilla Apache Indian Reservation and adjacent areas, New Mexico"},"id":1}],"supersededBy":{"id":977,"text":"wsp1576H - 1967 - Ground-water resources of the southern part of Jicarilla Apache Indian Reservation and adjacent areas, New Mexico","indexId":"wsp1576H","publicationYear":"1967","noYear":false,"title":"Ground-water resources of the southern part of Jicarilla Apache Indian Reservation and adjacent areas, New Mexico"},"lastModifiedDate":"2012-02-02T00:11:34","indexId":"ofr626","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"62-6","title":"Geology and ground-water resources of the southern part of the Jicarilla Apache Indian Reservation and adjacent region to the south and east, New Mexico","language":"ENGLISH","doi":"10.3133/ofr626","usgsCitation":"Baltz, E., and West, S.W., 1962, Geology and ground-water resources of the southern part of the Jicarilla Apache Indian Reservation and adjacent region to the south and east, New Mexico: U.S. Geological Survey Open-File Report 62-6, 296 p., https://doi.org/10.3133/ofr626.","productDescription":"296 p.","costCenters":[],"links":[{"id":100139,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1962/0006/report.pdf","size":"94541","linkFileType":{"id":1,"text":"pdf"}},{"id":177874,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1962/0006/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db685299","contributors":{"authors":[{"text":"Baltz, E.H.","contributorId":67146,"corporation":false,"usgs":true,"family":"Baltz","given":"E.H.","affiliations":[],"preferred":false,"id":244983,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"West, S. W.","contributorId":104029,"corporation":false,"usgs":true,"family":"West","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":244984,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":34585,"text":"b1147A - 1962 - Reconnaissance study of uranium deposits in Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:09:20","indexId":"b1147A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1147","chapter":"A","title":"Reconnaissance study of uranium deposits in Arizona","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1147A","usgsCitation":"Granger, H.C., and Raup, R., 1962, Reconnaissance study of uranium deposits in Arizona: U.S. Geological Survey Bulletin 1147, p. A1-A54  :fig. ;24 cm., https://doi.org/10.3133/b1147A.","productDescription":"p. A1-A54  :fig. ;24 cm.","costCenters":[],"links":[{"id":164296,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1147a/report-thumb.jpg"},{"id":62482,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1147a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db6364d4","contributors":{"authors":[{"text":"Granger, Harry Clifford","contributorId":8832,"corporation":false,"usgs":true,"family":"Granger","given":"Harry","email":"","middleInitial":"Clifford","affiliations":[],"preferred":false,"id":213220,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Raup, Robert B.","contributorId":67880,"corporation":false,"usgs":true,"family":"Raup","given":"Robert B.","affiliations":[],"preferred":false,"id":213221,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":62772,"text":"gq181 - 1962 - Geology of the Lenox quadrangle, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:11:00","indexId":"gq181","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"181","title":"Geology of the Lenox quadrangle, Kentucky","language":"ENGLISH","doi":"10.3133/gq181","usgsCitation":"Johnston, J.E., 1962, Geology of the Lenox quadrangle, Kentucky: U.S. Geological Survey Geologic Quadrangle 181, 1 map :col. ;78 x 84 cm., https://doi.org/10.3133/gq181.","productDescription":"1 map :col. ;78 x 84 cm.","costCenters":[],"links":[{"id":102181,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_630.htm","linkFileType":{"id":5,"text":"html"},"description":"630"},{"id":248927,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0181/report.pdf","size":"35","linkFileType":{"id":1,"text":"pdf"}},{"id":254402,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0181/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -83.25,37.8675 ], [ -83.25,38 ], [ -83.11749999999999,38 ], [ -83.11749999999999,37.8675 ], [ -83.25,37.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67f5f1","contributors":{"authors":[{"text":"Johnston, John Edward","contributorId":27946,"corporation":false,"usgs":true,"family":"Johnston","given":"John","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":267838,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":33750,"text":"b1140B - 1962 - Use of cesium-137 in the determination of cation exchange capacity","interactions":[],"lastModifiedDate":"2012-02-02T00:09:24","indexId":"b1140B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1140","chapter":"B","title":"Use of cesium-137 in the determination of cation exchange capacity","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/b1140B","usgsCitation":"Beetem, W., Janzer, V.J., and Wahlberg, J., 1962, Use of cesium-137 in the determination of cation exchange capacity: U.S. Geological Survey Bulletin 1140, p. B1-B8 ;24 cm., https://doi.org/10.3133/b1140B.","productDescription":"p. B1-B8 ;24 cm.","costCenters":[],"links":[{"id":163952,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1140b/report-thumb.jpg"},{"id":61623,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1140b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db6047c6","contributors":{"authors":[{"text":"Beetem, W.A.","contributorId":19173,"corporation":false,"usgs":true,"family":"Beetem","given":"W.A.","email":"","affiliations":[],"preferred":false,"id":211874,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Janzer, Victor J.","contributorId":36119,"corporation":false,"usgs":true,"family":"Janzer","given":"Victor","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":211875,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wahlberg, J.S.","contributorId":59850,"corporation":false,"usgs":true,"family":"Wahlberg","given":"J.S.","affiliations":[],"preferred":false,"id":211876,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":22804,"text":"ofr6234 - 1962 - Ground-water reconnaissance of the Sailor Creek area, Owyhee, Elmore, and Twin Falls Counties, Idaho","interactions":[],"lastModifiedDate":"2013-11-22T15:37:23","indexId":"ofr6234","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"62-34","title":"Ground-water reconnaissance of the Sailor Creek area, Owyhee, Elmore, and Twin Falls Counties, Idaho","docAbstract":"This reports evaluates the ground-water resources of about 1,000 square miles in the semiarid uplands south of the Snake River between Bruneau River and Salmon Falls Creek. The outcropping rocks are the Idavada Volcanics of Pliocene age, and the Idaho Group of Pliocene and Plieistocene age, consisting of the Banbury Basalt of middle Pliocene age and overlying predominantly sedimentary deposits of middle Pliocene through middle Pleistocene age. These rocks dip gently northward. The volcanic rocks are the best aquifers, but the yield of water from the sedimentary deposits is adequate for domestic and stock use. About 6,000 acre-feet of water is withdrawn annually from the Idavada Volcanics by 9 irrigation wells to irrigate about 3,000 acres. Only a few tends of acre-feet of water withdrawn from the other formations. The regional dip of the rocks induces weak artesian conditions in the volcanic rocks and somewhat higher artesian head in the sedimentary rocks. Estimated depth to water ranges from less than 250 feet to more than 750 feet, as shown in an accompanying map. The eastern part of the area appears to be more favorable for the development of ground water for irrigation than the western part because of better aquifers at shallower depth.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6234","collaboration":"Prepared in cooperation with the U.S. Bureau of Land Management","usgsCitation":"Crosthwaite, E., 1962, Ground-water reconnaissance of the Sailor Creek area, Owyhee, Elmore, and Twin Falls Counties, Idaho: U.S. Geological Survey Open-File Report 62-34, Report: ii, 53 p.; 3 Plates: 32.94 x 21.57 inches and smaller, https://doi.org/10.3133/ofr6234.","productDescription":"Report: ii, 53 p.; 3 Plates: 32.94 x 21.57 inches and smaller","numberOfPages":"56","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":155706,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1962/0034/report-thumb.jpg"},{"id":52232,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0034/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52233,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0034/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52234,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0034/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52235,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1962/0034/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","county":"Elmore County;Owyhee County;Twin Falls County","otherGeospatial":"Sailor Creek Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.4626,42.0584 ], [ -116.4626,44.1361 ], [ -112.07,44.1361 ], [ -112.07,42.0584 ], [ -116.4626,42.0584 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a0c5","contributors":{"authors":[{"text":"Crosthwaite, E. G.","contributorId":83098,"corporation":false,"usgs":true,"family":"Crosthwaite","given":"E. G.","affiliations":[],"preferred":false,"id":188903,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":35479,"text":"b1148 - 1962 - Summary of rock salt deposits in the United States as possible storage sites for radioactive waste materials","interactions":[{"subject":{"id":56172,"text":"ofr5995 - 1959 - Summary of rock salt deposits in the United States as possible disposal sites for radioactive waste","indexId":"ofr5995","publicationYear":"1959","noYear":false,"title":"Summary of rock salt deposits in the United States as possible disposal sites for radioactive waste"},"predicate":"SUPERSEDED_BY","object":{"id":35479,"text":"b1148 - 1962 - Summary of rock salt deposits in the United States as possible storage sites for radioactive waste materials","indexId":"b1148","publicationYear":"1962","noYear":false,"title":"Summary of rock salt deposits in the United States as possible storage sites for radioactive waste 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]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db698992","contributors":{"authors":[{"text":"Pierce, William Gamewell","contributorId":105361,"corporation":false,"usgs":true,"family":"Pierce","given":"William","email":"","middleInitial":"Gamewell","affiliations":[],"preferred":false,"id":214714,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rich, Ernest Isaac","contributorId":31451,"corporation":false,"usgs":true,"family":"Rich","given":"Ernest","email":"","middleInitial":"Isaac","affiliations":[],"preferred":false,"id":214713,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":35472,"text":"b1122F - 1962 - Geology and refractory clay deposits of the Haldeman and Wrigley quadrangles, Kentucky, with a section on coal resources","interactions":[],"lastModifiedDate":"2021-12-23T19:56:45.980641","indexId":"b1122F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1122","chapter":"F","title":"Geology and refractory clay deposits of the Haldeman and Wrigley quadrangles, Kentucky, with a section on coal resources","docAbstract":"The Haldeman and Wrigley 7th-minute quadrangles are near the western edge of the eastern Kentucky coal field and cover an area of approximately 117 square miles in parts of Carter, Rowan, Elliott, and Morgan Counties, Ky. The rocks exposed in the two quadrangles are of Early and Late Mississippian and Early and Middle Pennsylvanian age. The Mississippian rocks are composed of the thick Brodhead formation, which consists of siltstone and shale, and eleven thin marine limestone and shale formations, having an aggregate thickness of about 150 feet. The Lee and Breathitt formations, of Pennsylvanian age, consist of sandstone, siltstone, and shale; they also contain thin beds of coal and several beds of underclay, including the economically important Olive Hill clay bed of Crider, 1913. Pennsylvanian rocks include beds of both continental and marine origin. The eleven thin Mississippian formations and the upper-most part of the thick Brodhead formation are truncated by a prominent unconformity on which rocks of Pennsylvanian age rest. The rocks occupy a region of gentle dips between the Cincinnati arch and the Appalachian Mountains.\r\n\r\nRefractory clay deposits are in the Olive Hill clay bed, which occurs in the \r\nlower part of the Lee formation. The Olive Hill clay bed is discontinuous and \r\nconsists of a series of irregularly shaped lenses. The bed is approximately \r\ntwo-thirds semifiint clay and one-third flint clay, and it contains minor amounts of plastic clay. Some of the flint clay is nearly pure kaolinite, but the semi flint and plastic clay consists of mixtures of kaolinite, illite, and mixed-layer clay minerals. The structure of the kaolinite ranges from highly crystalline to very poorly crystalline 'fireclay' type. The degree of crystallinity of the kaolinite and the hardness of the clay vary inversely with the amount of illite and mixed-layer clay minerals present. The nearly pure kaolinite is believed to have formed by the removal of alkalies and some silica fram mixtures of kaolinite, illite, and mixed-layer clays by leaching in swamps to the deposition of the beds overlying the clay. The refractory properties of the clay vary directly with the purity of the kaolinite, and refractoriness decreases as the proportions of illite and mixed-layer clays increase. Certain nonclay minerals, chiefly siderite, pyrite, and iron oxide-bearing minerals, also act as fiuxes, reducing the refractory properties of the clay. The entire resources of clay in the Olive Hill clay bed are roughly and tentatively estimated to include 105,000,000 tons in the Haldeman quadrangle and 175,000,000 tons in the Wrigley quadrangle. Much of this clay is of poor quality and the amount that is better than the minimum requirements for use in refractories is probably about 30,000,000 tons. Only a fraction of this tonnage is suitable for superheat-duty products.\r\n\r\nLimestone is the only nonmetallic mineral resource other than refractory clay \r\nthat has been developed in the two quadrangles, but 1arge amounts of shale \r\nsuitable for use in making lightweight aggregate and structural clay products \r\nmay also be present. Most of the limestone, which is quarried. in both quadrangles, is used for road-metal, concrete aggregate, and agriculture stone, but some of the limestone is of the quality that would be suitable for other uses. Virtually all the Mississippian Beech Creek limestone of Malott, 1919 which is as much as 18 feet thick, consists of high-calcium limestone. Shale beds that appear most favoralble for making lightweight aggregate are in the shale facies of the Lee formation of Pennsylvanian age. Shale that is probably suitable for structural clay products is present in the shale flacles of the Lee formation and in the Muldraugh formation of Mississippian age.\r\n\r\nSeveral dry holes have been drilled in search for oil and gas within the area \r\nof the two quadrangles. Though no commercial production was ever attained, one well furnished a supply of gas f","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to economic geology (1960)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1122F","usgsCitation":"Patterson, S.H., Hosterman, J.W., and Huddle, J.W., 1962, Geology and refractory clay deposits of the Haldeman and Wrigley quadrangles, Kentucky, with a section on coal resources: U.S. Geological Survey Bulletin 1122, Report: vi, 113 p.; 8 Plates: 28 x 18 inches or smaller, https://doi.org/10.3133/b1122F.","productDescription":"Report: vi, 113 p.; 8 Plates: 28 x 18 inches or smaller","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":109365,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20827.htm","linkFileType":{"id":5,"text":"html"},"description":"20827"},{"id":63375,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1122f/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63374,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1122f/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63373,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1122f/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63372,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1122f/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63371,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1122f/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63376,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1122f/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63370,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1122f/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63369,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1122f/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63368,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1122f/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":166347,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1122f/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Kentucky","otherGeospatial":"Haldeman and Wrigley quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.375,\n              38.25\n            ],\n            [\n              -83.25,\n              38.25\n            ],\n            [\n              -83.25,\n              38.0\n            ],\n            [\n              -83.375,\n              38.0\n            ],\n            [\n              -83.375,\n              38.25\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db6863e2","contributors":{"authors":[{"text":"Patterson, Sam H.","contributorId":62996,"corporation":false,"usgs":true,"family":"Patterson","given":"Sam","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":214698,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hosterman, John W.","contributorId":48962,"corporation":false,"usgs":true,"family":"Hosterman","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":214697,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Huddle, John Warfield","contributorId":23932,"corporation":false,"usgs":true,"family":"Huddle","given":"John","email":"","middleInitial":"Warfield","affiliations":[],"preferred":false,"id":214696,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":68075,"text":"ha66 - 1962 - Floods at Tampa, Florida","interactions":[],"lastModifiedDate":"2012-02-10T00:11:24","indexId":"ha66","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"66","title":"Floods at Tampa, Florida","language":"ENGLISH","doi":"10.3133/ha66","usgsCitation":"Pride, R., 1962, Floods at Tampa, Florida: U.S. Geological Survey Hydrologic Atlas 66, 2 maps :col. ;58 x 114 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/ha66.","productDescription":"2 maps :col. ;58 x 114 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":187835,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89335,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/066/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89336,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/066/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"2000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.5,27.933333333333334 ], [ -82.5,28.034166666666668 ], [ -82.36749999999999,28.034166666666668 ], [ -82.36749999999999,27.933333333333334 ], [ -82.5,27.933333333333334 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7225","contributors":{"authors":[{"text":"Pride, R.W.","contributorId":96720,"corporation":false,"usgs":true,"family":"Pride","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":277607,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71780,"text":"tei827 - 1962 - Gravity Survey of the Nevada Test Site and Vicinity, Nye, Lincoln, and Clark Counties, Nevada: Interim Report","interactions":[],"lastModifiedDate":"2012-02-02T00:13:44","indexId":"tei827","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"827","title":"Gravity Survey of the Nevada Test Site and Vicinity, Nye, Lincoln, and Clark Counties, Nevada: Interim Report","language":"ENGLISH","doi":"10.3133/tei827","usgsCitation":"Healey, D., and Miller, C.H., 1962, Gravity Survey of the Nevada Test Site and Vicinity, Nye, Lincoln, and Clark Counties, Nevada: Interim Report: U.S. Geological Survey Trace Elements Investigations 827, 36 leaves : ill., maps ; 27 cm.; Three maps and 1 ill. folded in pocket, https://doi.org/10.3133/tei827.","productDescription":"36 leaves : ill., maps ; 27 cm.; Three maps and 1 ill. folded in pocket","costCenters":[],"links":[{"id":186399,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db672294","contributors":{"authors":[{"text":"Healey, D.L.","contributorId":52964,"corporation":false,"usgs":true,"family":"Healey","given":"D.L.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":284743,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, Carter H.","contributorId":73279,"corporation":false,"usgs":true,"family":"Miller","given":"Carter","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":284744,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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