{"pageNumber":"639","pageRowStart":"15950","pageSize":"25","recordCount":16443,"records":[{"id":2485,"text":"wsp1475I - 1963 - Hydrology of small watersheds in western states","interactions":[],"lastModifiedDate":"2024-02-01T20:08:52.68234","indexId":"wsp1475I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"1475","chapter":"I","title":"Hydrology of small watersheds in western states","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1475I","usgsCitation":"Peterson, H.V., 1963, Hydrology of small watersheds in western states: U.S. Geological Survey Water Supply Paper 1475, Report: iii, 140 p.; 2 Plates: 20.00 x 15.45 inches and 20.00 x 15.35 inches, https://doi.org/10.3133/wsp1475I.","productDescription":"Report: iii, 140 p.; 2 Plates: 20.00 x 15.45 inches and 20.00 x 15.35 inches","costCenters":[],"links":[{"id":425241,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24412.htm","text":"Wind River basin area","linkFileType":{"id":5,"text":"html"}},{"id":28581,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1475i/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28580,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1475i/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28579,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1475i/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138778,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1475i/report-thumb.jpg"},{"id":425240,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24411.htm","text":"Cheyenne River basin area","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Nebraska, South Dakota, Wyoming","otherGeospatial":"Cheyenne River basin, Wind River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -109.05,\n              43.5\n            ],\n            [\n              -109.05,\n              42.733\n            ],\n            [\n              -107.5,\n              42.733\n            ],\n            [\n              -107.5,\n              43.5\n            ],\n            [\n              -109.05,\n              43.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -106,\n              44.167\n            ],\n            [\n              -106,\n              42.683\n            ],\n            [\n              -103.227,\n              42.683\n            ],\n            [\n              -103.227,\n              44.167\n            ],\n            [\n              -106,\n              44.167\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601f10","contributors":{"authors":[{"text":"Peterson, Harold V.","contributorId":9630,"corporation":false,"usgs":true,"family":"Peterson","given":"Harold","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":145272,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2478,"text":"wsp1613A - 1963 - Geology and ground-water conditions in southern Nassau and southeastern Queens Counties, Long Island, N.Y.","interactions":[{"subject":{"id":51254,"text":"ofr5377 - 1953 - Water-level and chloride-content data at outpost observation wells in southwestern Nassau County, Long Island, New York","indexId":"ofr5377","publicationYear":"1953","noYear":false,"title":"Water-level and chloride-content data at outpost observation wells in southwestern Nassau County, Long Island, New York"},"predicate":"SUPERSEDED_BY","object":{"id":2478,"text":"wsp1613A - 1963 - Geology and ground-water conditions in southern Nassau and southeastern Queens Counties, Long Island, N.Y.","indexId":"wsp1613A","publicationYear":"1963","noYear":false,"chapter":"A","title":"Geology and ground-water conditions in southern Nassau and southeastern Queens Counties, Long Island, N.Y."},"id":1},{"subject":{"id":51661,"text":"ofr5498 - 1954 - Supplementary data on water levels and chloride concentrations at outpost observation wells in southern Nassau County, Long Island, New York","indexId":"ofr5498","publicationYear":"1954","noYear":false,"title":"Supplementary data on water levels and chloride concentrations at outpost observation wells in southern Nassau County, Long Island, New York"},"predicate":"SUPERSEDED_BY","object":{"id":2478,"text":"wsp1613A - 1963 - Geology and ground-water conditions in southern Nassau and southeastern Queens Counties, Long Island, N.Y.","indexId":"wsp1613A","publicationYear":"1963","noYear":false,"chapter":"A","title":"Geology and ground-water conditions in southern Nassau and southeastern Queens Counties, Long Island, N.Y."},"id":2}],"lastModifiedDate":"2022-03-22T19:47:50.062941","indexId":"wsp1613A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"1613","chapter":"A","title":"Geology and ground-water conditions in southern Nassau and southeastern Queens Counties, Long Island, N.Y.","docAbstract":"Test drilling, electrical logging, and water sampling of 'outpost' and other \r\nwells have revealed the existence of a deep confined body of salt water in the \r\nMagothy(?) formation beneath southwestern Nassau and southeastern Queens \r\nCounties, Long Island, N.Y. In connection with a test-drilling program, cooperatively sponsored by the U.S. Geological Survey, the Nassau County Department \r\nof Public Works, and the New York State Water Resources Commission (formerly \r\nWater Power and Control Commission), 13 wells ranging in depth from about \r\n130 to 800 feet were drilled during 1952 and 1953 and screened at various depths \r\nin the Magothy(?) formation and Jameco gravel. On the basis of the preliminary \r\ngeologic, hydrologic, and chemical data from these wells, a detailed investigation \r\nof ground-water conditions from the water table to the bedrock was begun in a \r\n200-square-mile area in southern Nassau and southeastern Queens Counties. \r\nThe Inain purposes of the investigation were to delineate the bodies of fresh and \r\nsalty ground water in the project area, to relate their occurrence and movement \r\nto geologic and hydrologic conditions, to estimate the rate of encroachment, if \r\nany, of the salty water, and to evaluate the effectiveness of the existing network \r\nof outpost wells as detectors of salt-water encroachment. \r\nAbout a million people in the report area, residing mainly in southern Nassau \r\nCounty, are completely dependent on ground water as a source of supply. Fortunately, precipitation averages about 44 inches per year, of which approximately \r\nhalf is estimated to percolate into the ground-water reservoir. \r\nThe ground water is contained in and moves through eight differentiated geologic units composed of unconsolidated gravel, sand, and clay, of Late Cretaceous, \r\nPleistocene, and Recent age, having a maximum total thickness of about 1,700 \r\nfeet. The underlying metamorphic and igneous crystalline basement rocks are \r\nof Precambrian age and are not water bearing. \r\nThe water-yielding units from the surface down are (1) the upper Pleistocene \r\ndeposits, (2) the principal artesian aquifer, composed of the Jameco gravel and \r\nMagothy(?) formation, and (3) the Lloyd sand member of the Raritar formation. \r\nThe confining units are the '20-foot' clay, the Gardiners clay, and the clay member of the Raritan formation. The upper Pleistocene deposits contain an extensive unconfined body of fresh water. Fresh water under artesian conditions is \r\ncontained in the principal artesian aquifer and the Lloyd sand member. The \r\npiezometric surface of the principal artesian aquifer is similar in shape to the south-ward-sloping water table; it ranges in altitude from about sea level to 55 feet \r\nabove. \r\nThe chemical quality of the fresh ground water in most of the area in all aquifers \r\nis good to excellent, and concentrations of dissolved solids and of chloride generally \r\nare below 100 ppm (parts per million) and 10 ppm, respectively. Analyses of \r\nwater samples from selected wells show no progressive increase in concentration of \r\nchloride in most of the area. The data on quality of water have been used to \r\ndelineate one major and several minor bodies of salty ground water. The wedgeshaped main confined salt-water body, in which the concentration of chloride \r\nreaches about 17,000 ppm, is in the Magothy(?) formation and Jameco gravel in \r\nextreme southwestern Nassau County and southeastern Queens County. The \r\nbase of the salt-water wedge is about at the top of the clay member of the Raritan \r\nformation. Beneath the barrier beach in south-central and southeastern Nassau County a shallow extension of the main confined salt-water body contains as much as 4,000 ppm of chloride and is separated from the lower main salt-water body by fresh ground water. Shallow, thin bodies of unconfined salty ground water are common in the upper Pleistocene and Recent deposits adjacent to salty surface water in tidal creeks, bays, and the Atlantic","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1613A","usgsCitation":"Perlmutter, N.M., and Geraghty, J.J., 1963, Geology and ground-water conditions in southern Nassau and southeastern Queens Counties, Long Island, N.Y.: U.S. Geological Survey Water Supply Paper 1613, Report: vi, 205 p.; 7 Plates: 27.00 × 40.00 inches or smaller, https://doi.org/10.3133/wsp1613A.","productDescription":"Report: vi, 205 p.; 7 Plates: 27.00 × 40.00 inches or smaller","costCenters":[],"links":[{"id":28560,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1613a/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28559,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1613a/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28557,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1613a/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28556,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1613a/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28555,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1613a/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138751,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1613a/report-thumb.jpg"},{"id":28558,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1613a/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28561,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1613a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":394230,"rank":10,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24803.htm"},{"id":28554,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1613a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"96200","country":"United States","state":"New York","county":"Nassau County, Queens County","otherGeospatial":"Long Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73.812,\n              40.583\n            ],\n            [\n              -73.417,\n              40.583\n            ],\n            [\n              -73.417,\n              40.727\n            ],\n            [\n              -73.812,\n              40.727\n            ],\n            [\n              -73.812,\n              40.583\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685f9f","contributors":{"authors":[{"text":"Perlmutter, N. M.","contributorId":38972,"corporation":false,"usgs":true,"family":"Perlmutter","given":"N.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":145260,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Geraghty, J. J.","contributorId":74738,"corporation":false,"usgs":true,"family":"Geraghty","given":"J.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":145261,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2426,"text":"wsp1669I - 1963 - Water regimen of the Inner Valley of the San Pedro River near Mammoth, Arizona (A pilot study)","interactions":[],"lastModifiedDate":"2012-02-02T00:05:35","indexId":"wsp1669I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"1669","chapter":"I","title":"Water regimen of the Inner Valley of the San Pedro River near Mammoth, Arizona (A pilot study)","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1962","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1669I","usgsCitation":"Page, H.G., 1963, Water regimen of the Inner Valley of the San Pedro River near Mammoth, Arizona (A pilot study): U.S. Geological Survey Water Supply Paper 1669, iii, 22 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1669I.","productDescription":"iii, 22 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":139048,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1669i/report-thumb.jpg"},{"id":28445,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669i/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28446,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669i/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28447,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1669i/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f975d","contributors":{"authors":[{"text":"Page, Harry G.","contributorId":62203,"corporation":false,"usgs":true,"family":"Page","given":"Harry","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":145180,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2893,"text":"wsp1619B - 1963 - Ground-water geology and hydrology of Bunker Hill Air Force Base and vicinity, Peru, Indiana","interactions":[],"lastModifiedDate":"2012-02-02T00:05:20","indexId":"wsp1619B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"1619","chapter":"B","title":"Ground-water geology and hydrology of Bunker Hill Air Force Base and vicinity, Peru, Indiana","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1619B","usgsCitation":"Watkins, F., and Rosenshein, J.S., 1963, Ground-water geology and hydrology of Bunker Hill Air Force Base and vicinity, Peru, Indiana: U.S. Geological Survey Water Supply Paper 1619, iv, 32 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1619B.","productDescription":"iv, 32 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":138362,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1619b/report-thumb.jpg"},{"id":29542,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29543,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29544,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619b/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29545,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1619b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668e10","contributors":{"authors":[{"text":"Watkins, Frank A.","contributorId":21140,"corporation":false,"usgs":true,"family":"Watkins","given":"Frank A.","affiliations":[],"preferred":false,"id":145967,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rosenshein, Joseph S.","contributorId":32904,"corporation":false,"usgs":true,"family":"Rosenshein","given":"Joseph","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":145968,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2357,"text":"wsp1539Q - 1963 - Reconnaissance of the hydrology of the Little Lost River basin, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:05:20","indexId":"wsp1539Q","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"1539","chapter":"Q","title":"Reconnaissance of the hydrology of the Little Lost River basin, Idaho","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1539Q","usgsCitation":"Mundorff, M.J., Broom, H.C., and Kilburn, C., 1963, Reconnaissance of the hydrology of the Little Lost River basin, Idaho: U.S. Geological Survey Water Supply Paper 1539, iv, 51 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1539Q.","productDescription":"iv, 51 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":109984,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24739.htm","linkFileType":{"id":5,"text":"html"},"description":"24739"},{"id":137785,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1539q/report-thumb.jpg"},{"id":28292,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539q/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28293,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539q/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28294,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539q/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28295,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1539q/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db636c6b","contributors":{"authors":[{"text":"Mundorff, Maurice John","contributorId":41404,"corporation":false,"usgs":true,"family":"Mundorff","given":"Maurice","email":"","middleInitial":"John","affiliations":[],"preferred":false,"id":145073,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Broom, H. C.","contributorId":93024,"corporation":false,"usgs":true,"family":"Broom","given":"H.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":145075,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kilburn, Chabot","contributorId":83499,"corporation":false,"usgs":true,"family":"Kilburn","given":"Chabot","email":"","affiliations":[],"preferred":false,"id":145074,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2305,"text":"wsp1669Z - 1963 - Selected techniques in water resources investigations","interactions":[],"lastModifiedDate":"2012-02-02T00:05:20","indexId":"wsp1669Z","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"1669","chapter":"Z","title":"Selected techniques in water resources investigations","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1962","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. Department of the Interior, Geological Survey ;","doi":"10.3133/wsp1669Z","isbn":"pbk","usgsCitation":"Mesnier, G.N., and Iseri, K.T., 1963, Selected techniques in water resources investigations: U.S. Geological Survey Water Supply Paper 1669, vii, 64 p. :ill. ; 24 cm., https://doi.org/10.3133/wsp1669Z.","productDescription":"vii, 64 p. :ill. ; 24 cm.","costCenters":[],"links":[{"id":137714,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1669z/report-thumb.jpg"},{"id":28128,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1669z/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a01e4b07f02db5f8021","contributors":{"authors":[{"text":"Mesnier, Glennon N.","contributorId":67488,"corporation":false,"usgs":true,"family":"Mesnier","given":"Glennon","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":144981,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Iseri, Kathleen T.","contributorId":77910,"corporation":false,"usgs":true,"family":"Iseri","given":"Kathleen","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":144982,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2903,"text":"wsp1669P - 1963 - Water in the Dakota and Purgatoire Formations in Otero County and the southern part of Crowley County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:05:21","indexId":"wsp1669P","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"1669","chapter":"P","title":"Water in the Dakota and Purgatoire Formations in Otero County and the southern part of Crowley County, Colorado","docAbstract":"The hardness of available shallow ground water in Otero County and in the southern part of Crowley County generally exceeds 1,000 parts per million, and the water requires treatment for most uses. To obtain a supply of softer water, wells have been drilled into the Dakota Sandstone and the Cheyenne Sandstone Member of the Purgatoire Formation, both Early Cretaceous in age. These aquifers underlie most of ,the area at depths from 0 to 2,000 feet and have a general regional dip northward into the Denver Basin. More than 50 wells have been drilled into the aquifers in this area to obtain water for stock, domestic, and industrial purposes and for public supply. The aquifers are recharged in areas where they crop out or are overlain by sand, principally to the south and west of Otero County. Because water in the aquifers is generally under pressure, it rises above the top of the aquifer in wells penetrating it; at least 20 wells in the area flow. Yields from wells tapping the aquifers range from 4 to 75 gpm (gallons per minute). Flows as great as 50 gpm have been obtained.\r\n\r\nWater in the aquifers is commonly soft and of good chemical quality. There appears to be little difference in quality of water from the two aquifers. Most residents and drillers know that soft water can be obtained from wells throughout most of the area described in this report, but many are not aware of certain factors related to the development of this water. This report should be of value in further developing the sources of soft water by showing: (a) The approximate depth of a well needed to tap these supplies, (b) the range in yields that may be expected, (c) the range in chemical quality that may be expected, (d) the depth to which water will rise in wells, and (e) information on the factors affecting the durability of the supply.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1962","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1669P","usgsCitation":"Weist, W., 1963, Water in the Dakota and Purgatoire Formations in Otero County and the southern part of Crowley County, Colorado: U.S. Geological Survey Water Supply Paper 1669, iii, 17 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1669P.","productDescription":"iii, 17 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":138392,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1669p/report-thumb.jpg"},{"id":29583,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1669p/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa133","contributors":{"authors":[{"text":"Weist, William G.","contributorId":21526,"corporation":false,"usgs":true,"family":"Weist","given":"William G.","affiliations":[],"preferred":false,"id":145984,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2258,"text":"wsp1800 - 1963 - The role of ground water in the national water situation: With state summaries based on reports by District Offices of Ground Water Branch","interactions":[],"lastModifiedDate":"2018-03-12T15:44:46","indexId":"wsp1800","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"1800","title":"The role of ground water in the national water situation: With state summaries based on reports by District Offices of Ground Water Branch","docAbstract":"<p>Ground water in the United States has emerged from a quantitatively minor (though incalculably valuable) water source, whose chief role was in the settlement of primitive areas, to a major source now accounting for one-fifth to one-sixth of the Nation's total withdrawal requirements for water. With the growth in ground-water withdrawals is an accompanying growth in the realization that large-scale development of ground water is feasible only on the basis of a fuller understanding than has existed to date of the complex interrelations of the hydrologic cycle and of ground water's place in the cycle</p>\n<p>This report outlines briefly the principles of water occurrence and describes the water situation in the United States as of 1960-61, with emphasis on the occurrence of ground water and the status of development and accompanying problems. The Nation has been divided into 10 major ground-water regions by H. E. Thomas (1952a). The report summarizes the occurrence and development of ground water in each of Thomas' regions. In a large terminal section it also describes the occurrence and development of water, again with emphasis on ground water, in each of the 50 States and in certain other areas. The main text ends with a discussion of the water situation and prospects of the Nation.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1800","usgsCitation":"McGuinness, C.L., 1963, The role of ground water in the national water situation: With state summaries based on reports by District Offices of Ground Water Branch: U.S. Geological Survey Water Supply Paper 1800, Report: xii, 1121 p.; 4 Plates: 43.44 x 26.28 inches or smaller, https://doi.org/10.3133/wsp1800.","productDescription":"Report: xii, 1121 p.; 4 Plates: 43.44 x 26.28 inches or smaller","numberOfPages":"1134","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true},{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true},{"id":610,"text":"Utah Water Science 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,{"id":2206,"text":"wsp1475M - 1963 - Ground-water resources of the Bryce Canyon National Park area, Utah, with a section on the drilling of a test well","interactions":[{"subject":{"id":23797,"text":"ofr5866 - 1958 - Ground-water resources of the Bryce Canyon National Park area, Utah","indexId":"ofr5866","publicationYear":"1958","noYear":false,"title":"Ground-water resources of the Bryce Canyon National Park area, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":2206,"text":"wsp1475M - 1963 - Ground-water resources of the Bryce Canyon National Park area, Utah, with a section on the drilling of a test well","indexId":"wsp1475M","publicationYear":"1963","noYear":false,"chapter":"M","title":"Ground-water resources of the Bryce Canyon National Park area, Utah, with a section on the drilling of a test well"},"id":1}],"lastModifiedDate":"2024-06-17T18:55:36.649675","indexId":"wsp1475M","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"1475","chapter":"M","title":"Ground-water resources of the Bryce Canyon National Park area, Utah, with a section on the drilling of a test well","docAbstract":"<p>The water need at Bryce Canyon National Park in 1957 was about 1.3 million cubic feet for a tourist season that lasted from the middle of May to the middle of October. To evaluate the adequacy of water-supply sources, a hypothetical future need of 5 million cubic feet of water per season is used. This amount of water might be obtained from the East Fork of the Sevier River, from wells in the alluvium of the East Fork, from Yellow Creek Spring and nearby springs, which are below the canyon rim, or from a well drilled about 2,000 feet to the top of the Tropic shale. Although the present source of water, consisting of wells in the alluvium of East Creek valley, may be an important supplemental source in the future, it will not yield sufficient water in dry years to meet the total demand for water at the park.</p><p>The yield of Yellow Creek Spring and nearby springs is estimated at a total of 7.8 million cubic feet of water per season. The springs provide water of satisfactory chemical quality, and are a reliable source even in times of drought. A serious disadvantage of using this source of water is the difficulty of constructing a pipeline over extremely rugged terrain from the source to the lodge and headquarters area.</p><p>A well drilled to the top of the Tropic shale of Cretaceous age in the lodge and headquarters area might penetrate two or more aquifers, one at the base of the Wasatch formation of Eocene age and one or more in the Wahweap and Straight Cliffs sandstones of Cretaceous age. The yield of this well would depend to a large degree on the number of fractures encountered. To assure the most favorable conditions for intercepting fracture zones in the bedrock, a test-well site is proposed near the crest of a gentle anticline where tension fractures in the rocks should be common.</p><p>Shallow wells in the alluvium of East Creek valley cannot be depended upon to yield sufficient water in times of drought, but they are nevertheless an important source. The water-storage capacity of the alluvium of East Creek valley in the vicinity of the wells of the Utah Parks Co. is estimated at 1.4 million cubic feet. By lowering the water table in the valley uniformly without creating excessively large cones of depression, the alluvium could supply the 1.3 million cubic feet of water per season estimated as the water need in 1957. However, in times of drought this alluvium cannot supply the hypothetical future needs of 5 million cubic feet of water per season.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Hydrology of the Public Domain (Water Supply Paper 1475)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1475M","collaboration":"Prepared in cooperation with the National Park Service, Department of the Interior","usgsCitation":"Marine, I.W., 1963, Ground-water resources of the Bryce Canyon National Park area, Utah, with a section on the drilling of a test well: U.S. Geological Survey Water Supply Paper 1475, Report: iv, 46 p.; 3 Plates: 16.20 x 24.41 inches or smaller, https://doi.org/10.3133/wsp1475M.","productDescription":"Report: iv, 46 p.; 3 Plates: 16.20 x 24.41 inches or smaller","startPage":"441","endPage":"486","numberOfPages":"50","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true},{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":430318,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24416.htm","linkFileType":{"id":5,"text":"html"}},{"id":27877,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1475m/plate-2.pdf","text":"Plate 25","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"<i>A</i>, Map of East Creek Valley showing area underlain by alluvium; <i>B</i>, North-South section of East Creek Valley showing inferred maximum depth to bedrock and the position of the water table in May 1957"},{"id":27876,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1475m/plate-1.pdf","text":"Plate 24","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map of Bryce Canyon National Park area, Utah, showing physiographic features and the location of springs and wells"},{"id":138341,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1475m/report-thumb.jpg"},{"id":27879,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1475m/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27878,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1475m/plate-3.pdf","text":"Plate 26","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Logs of the test well at Bryce Canyon National Park, Utah"}],"country":"United States","state":"Utah","otherGeospatial":"Bryce Canyon National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -112.47262325325637,\n              37.73847091078626\n            ],\n            [\n              -112.47262325325637,\n              37.27074325321638\n            ],\n            [\n              -112.06792128542472,\n              37.27074325321638\n            ],\n            [\n              -112.06792128542472,\n              37.73847091078626\n            ],\n            [\n              -112.47262325325637,\n              37.73847091078626\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66dde6","contributors":{"authors":[{"text":"Marine, I. Wendell","contributorId":49339,"corporation":false,"usgs":true,"family":"Marine","given":"I.","email":"","middleInitial":"Wendell","affiliations":[],"preferred":false,"id":144825,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2205,"text":"wsp1669K - 1963 - Correlation of water-level fluctuations with climatic cycles in the Oklahoma Panhandle","interactions":[],"lastModifiedDate":"2012-02-02T00:05:24","indexId":"wsp1669K","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"1669","chapter":"K","title":"Correlation of water-level fluctuations with climatic cycles in the Oklahoma Panhandle","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1962","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1669K","usgsCitation":"Marine, I.W., 1963, Correlation of water-level fluctuations with climatic cycles in the Oklahoma Panhandle: U.S. Geological Survey Water Supply Paper 1669, iii, 10 p. :ill., map ;24 cm., https://doi.org/10.3133/wsp1669K.","productDescription":"iii, 10 p. :ill., map ;24 cm.","costCenters":[],"links":[{"id":138170,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1669k/report-thumb.jpg"},{"id":27874,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669k/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27875,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1669k/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db68454c","contributors":{"authors":[{"text":"Marine, I. Wendell","contributorId":49339,"corporation":false,"usgs":true,"family":"Marine","given":"I.","email":"","middleInitial":"Wendell","affiliations":[],"preferred":false,"id":144824,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2972,"text":"wsp1619DD - 1963 - Analysis and evaluation of available hydrologic data for San Simon Basin, Cochise and Graham Counties, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:05:41","indexId":"wsp1619DD","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"1619","chapter":"DD","title":"Analysis and evaluation of available hydrologic data for San Simon Basin, Cochise and Graham Counties, Arizona","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1619DD","usgsCitation":"White, N.D., 1963, Analysis and evaluation of available hydrologic data for San Simon Basin, Cochise and Graham Counties, Arizona: U.S. Geological Survey Water Supply Paper 1619, iv, 33 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1619DD.","productDescription":"iv, 33 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":139280,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1619dd/report-thumb.jpg"},{"id":29709,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619dd/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29710,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619dd/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29711,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619dd/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29712,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619dd/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29713,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619dd/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29714,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619dd/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29715,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619dd/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29716,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619dd/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29717,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1619dd/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad0e4b07f02db680c41","contributors":{"authors":[{"text":"White, Natalie D.","contributorId":97064,"corporation":false,"usgs":true,"family":"White","given":"Natalie","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":146072,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2141,"text":"wsp1669Q - 1963 - Ground-water conditions in the vicinity of the Lake Mead base, Las Vegas Valley, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1669Q","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"1669","chapter":"Q","title":"Ground-water conditions in the vicinity of the Lake Mead base, Las Vegas Valley, Nevada","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1962","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1669Q","usgsCitation":"Loeltz, O.J., 1963, Ground-water conditions in the vicinity of the Lake Mead base, Las Vegas Valley, Nevada: U.S. Geological Survey Water Supply Paper 1669, iii, 17 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1669Q.","productDescription":"iii, 17 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":137795,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1669q/report-thumb.jpg"},{"id":27744,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1669q/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d0c0","contributors":{"authors":[{"text":"Loeltz, Omar J.","contributorId":86312,"corporation":false,"usgs":true,"family":"Loeltz","given":"Omar","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":144731,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2058,"text":"wsp1475O - 1963 - Hydrologic and geologic reconnaissance of Pinto Basin, Joshua Tree National Monument, Riverside County, California","interactions":[{"subject":{"id":23112,"text":"ofr5672 - 1956 - A brief hydrologic and geologic reconnaissance of Pinto Basin, Joshua Tree National Monument, Riverside County, California","indexId":"ofr5672","publicationYear":"1956","noYear":false,"title":"A brief hydrologic and geologic reconnaissance of Pinto Basin, Joshua Tree National Monument, Riverside County, California"},"predicate":"SUPERSEDED_BY","object":{"id":2058,"text":"wsp1475O - 1963 - Hydrologic and geologic reconnaissance of Pinto Basin, Joshua Tree National Monument, Riverside County, California","indexId":"wsp1475O","publicationYear":"1963","noYear":false,"chapter":"O","title":"Hydrologic and geologic reconnaissance of Pinto Basin, Joshua Tree National Monument, Riverside County, California"},"id":1},{"subject":{"id":52115,"text":"ofr6090 - 1960 - Summary of hydrologic conditions at Joshua Tree National Monument, Riverside County, California, 1956-1959","indexId":"ofr6090","publicationYear":"1960","noYear":false,"title":"Summary of hydrologic conditions at Joshua Tree National Monument, Riverside County, California, 1956-1959"},"predicate":"SUPERSEDED_BY","object":{"id":2058,"text":"wsp1475O - 1963 - Hydrologic and geologic reconnaissance of Pinto Basin, Joshua Tree National Monument, Riverside County, California","indexId":"wsp1475O","publicationYear":"1963","noYear":false,"chapter":"O","title":"Hydrologic and geologic reconnaissance of Pinto Basin, Joshua Tree National Monument, Riverside County, California"},"id":2}],"lastModifiedDate":"2023-01-06T22:49:59.861671","indexId":"wsp1475O","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"1475","chapter":"O","displayTitle":"Hydrologic and Geologic Reconnaissance of Pinto Basin, Joshua Tree National Monument, Riverside County, California","title":"Hydrologic and geologic reconnaissance of Pinto Basin, Joshua Tree National Monument, Riverside County, California","docAbstract":"Pinto basin, in the north-central part of Riverside County, Calif., is a typical desert valley formed by downfaulting along several major fault zones. The valley is filled with alluvium, and ground water in the alluvium discharges as subsurface outflow through an alluvium-filled gap at the east end of the valley. Occasionally surface water from cloudburst floods also discharges in a wash through the gap at the east end of the valley.\r\n\r\nA northeastward extension of the major fault along the south side of the valley acts as a barrier to the discharge of ground water from the valley. The average ground-water gradient is less than 1 foot per mile across the main part of the valley above this barrier, but the water level drops abruptly across the fault. The ground-water storage capacity of the uppermost 100 feet of saturated alluvium beneath the central valley area is estimated to be about 230,000 acre-feet. All this water in storage occurs at depths greater than 95 feet below the land surface and cannot be reached by plants or animals. During 1959 virtually all the water pumped in the area was withdrawn from storage. However, the quantity of water pumped is small in relation to the total quantity in storage. Except for a small decline in head, no evidence indicates that the pumping will greatly impair the yield for many years or cause the water to deteriorate in quality.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Hydrology of the Public Domain","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1475O","usgsCitation":"Kunkel, F., 1963, Hydrologic and geologic reconnaissance of Pinto Basin, Joshua Tree National Monument, Riverside County, California: U.S. Geological Survey Water Supply Paper 1475, Report: iii, 24 p.; 1 Plate: 30.90 x 20.80 inches, https://doi.org/10.3133/wsp1475O.","productDescription":"Report: iii, 24 p.; 1 Plate: 30.90 x 20.80 inches","startPage":"537","endPage":"561","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":27600,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1475o/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27599,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1475o/plate-28.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138561,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1475o/report-thumb.jpg"}],"scale":"62500","country":"United States","state":"California","county":"Riverside County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -115.733,\n              33.9\n            ],\n            [\n              -115.733,\n              34\n            ],\n            [\n              -115.333,\n              34\n            ],\n            [\n              -115.333,\n              33.9\n            ],\n            [\n              -115.733,\n              33.9\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db6118db","contributors":{"authors":[{"text":"Kunkel, Fred","contributorId":47766,"corporation":false,"usgs":true,"family":"Kunkel","given":"Fred","email":"","affiliations":[],"preferred":false,"id":144611,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2042,"text":"wsp1669O - 1963 - Ground-water conditions at Argonne National Laboratory, Illinois, 1948-60","interactions":[],"lastModifiedDate":"2012-02-02T00:05:19","indexId":"wsp1669O","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"1669","chapter":"O","title":"Ground-water conditions at Argonne National Laboratory, Illinois, 1948-60","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1962","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1669O","usgsCitation":"Knowles, D., Drescher, W., and LeRoux, E.F., 1963, Ground-water conditions at Argonne National Laboratory, Illinois, 1948-60: U.S. Geological Survey Water Supply Paper 1669, iv, 40 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1669O.","productDescription":"iv, 40 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":137709,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1669o/report-thumb.jpg"},{"id":27531,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1669o/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d2e9","contributors":{"authors":[{"text":"Knowles, Doyle B.","contributorId":85566,"corporation":false,"usgs":true,"family":"Knowles","given":"Doyle B.","affiliations":[],"preferred":false,"id":144578,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Drescher, W.J.","contributorId":35713,"corporation":false,"usgs":true,"family":"Drescher","given":"W.J.","email":"","affiliations":[],"preferred":false,"id":144577,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"LeRoux, E. F.","contributorId":29795,"corporation":false,"usgs":true,"family":"LeRoux","given":"E.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":144576,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2034,"text":"wsp1669H - 1963 - Sedimentation and chemical quality of water in Salt Creek basin, Nebraska","interactions":[],"lastModifiedDate":"2012-02-02T00:05:19","indexId":"wsp1669H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"1669","chapter":"H","title":"Sedimentation and chemical quality of water in Salt Creek basin, Nebraska","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1962","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1669H","usgsCitation":"Kister, L.R., and Mundorff, J.C., 1963, Sedimentation and chemical quality of water in Salt Creek basin, Nebraska: U.S. Geological Survey Water Supply Paper 1669, vi, 47 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1669H.","productDescription":"vi, 47 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":137687,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1669h/report-thumb.jpg"},{"id":27515,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1669h/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbcd7","contributors":{"authors":[{"text":"Kister, Lester Ray","contributorId":107670,"corporation":false,"usgs":true,"family":"Kister","given":"Lester","email":"","middleInitial":"Ray","affiliations":[],"preferred":false,"id":144562,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mundorff, J. C.","contributorId":63374,"corporation":false,"usgs":true,"family":"Mundorff","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":144561,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2031,"text":"wsp1595 - 1963 - Effects of hydraulic and geologic factors on streamflow of the Yakima River Basin, Washington","interactions":[],"lastModifiedDate":"2014-03-06T14:11:36","indexId":"wsp1595","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"1595","title":"Effects of hydraulic and geologic factors on streamflow of the Yakima River Basin, Washington","docAbstract":"<p>The Yakima River basin, in south-central Washington, is the largest single river system entirely within the confines of the State. Its waters are the most extensively utilized of all the rivers in Washington.</p>\n<br/>\n<p>The river heads high on the eastern slope of the Cascade Mountains, flows for 180 miles in a generally southeast direction, and discharges into the Columbia River. The western part of the basin is a mountainous area formed by sedimentary, volcanic, and metamorphic rocks, which generally have a low capacity for storing and transmitting water. The eastern part of the basin is. formed by a thick sequence of lava flows that have folded into long ridges and troughs. Downwarped structural basins between many of the ridges are partly filled with younger sedimentary deposits, which at some places are many hundreds of feet thick. The Yakima River flows from structural basin to structural basin through narrow water gaps that have been eroded through the anticlinal ridges. Each basin is also a topographic basin and a ground-water subbasin. A gaging station will measure the total outflow of a drainage area only if it is located at the surface outlet of a ground-water subbasin and then only if the stream basin is nearly coextensive with the ground-water subbasin. Many gaging stations in the Yakima basin are so located. The geology, hydrology, size. and location of 25 ground-water subbasins are described. </p>\n<br/>\n<p>Since the settlement of the valley began, the development of the land and water resources have caused progressive changes in the natural regimen of the basin's runoff. These changes have resulted from diversion of water from the streams, the application of water on the land for irrigation, the storage and release of flood waters, the pumping of ground water, and other factors Irrigation in the Yakima basin is reported 'to have begun about 1864. In 1955 about 425,000 acres were under irrigation. </p>\n<br/>\n<p>During the past 60-odd years many gaging stations have been operated at different sites within the basin. Only stations in the upper reaches, such as those below Keechelus, Kachess, or Cle Elum Lakes, give discharge records which are an accurate measure of the natural outflow of the drainage area. Farther down, stream, as the utilization of water becomes more extensive, the records at a gaging station show the discharge passing a particular point, but they do not reflect the natural outflow of the basin. Large canals divert water for use on lands above a station or carry it around a station for irrigation downstream. The deep sedimentary deposits within subbasins and the overlying alluvial gravels permit downvalley movement of large subsurface flows which bypass the gaging stations, except in the near vicinity of the water gaps. At the water gaps ground water rises to the surface, becoming streamflow, and can be accurately measured. The location of gaging stations within each subbasin is important, therefore, in determining whether the flow measured represents the total downvalley outflow or whether it is merely the surface-water component. Surface and subsurface factors that may affect the discharge records at each gaging station in the Yakima River basin include a description of upstream diversions, surface return flows, bypass canals, storage reservoirs, subsurface bypass flows, ground-water withdrawals, and other items. The available data are not sufficiently complete to permit a quantitative determination of the total basin yield at most gaging stations. However, data on the existing bypass channels, such as canals and drainage ditches, and on related subsurface movement of water provide valuable information necessary to proper use and interpretation of the streamflow records.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1595","usgsCitation":"Kinnison, H.B., and Sceva, J.E., 1963, Effects of hydraulic and geologic factors on streamflow of the Yakima River Basin, Washington: U.S. Geological Survey Water Supply Paper 1595, Report: vii, 134 p.; 3 Plates: 29.5 x 30.0 inches or smaller, https://doi.org/10.3133/wsp1595.","productDescription":"Report: vii, 134 p.; 3 Plates: 29.5 x 30.0 inches or smaller","numberOfPages":"144","costCenters":[],"links":[{"id":137648,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1595/report-thumb.jpg"},{"id":27507,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1595/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27508,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1595/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27509,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1595/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27510,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1595/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Washington","otherGeospatial":"Yakima River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.8361,45.5437 ], [ -124.8361,49.0024 ], [ -116.9174,49.0024 ], [ -116.9174,45.5437 ], [ -124.8361,45.5437 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611e92","contributors":{"authors":[{"text":"Kinnison, Hallard B.","contributorId":84337,"corporation":false,"usgs":true,"family":"Kinnison","given":"Hallard","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":144555,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sceva, Jack E.","contributorId":79086,"corporation":false,"usgs":true,"family":"Sceva","given":"Jack","email":"","middleInitial":"E.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":144554,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1996,"text":"wsp1669A - 1963 - Geology and ground-water conditions in the southern part of the Camp Ripley Military Reservation, Morrison County, Minnesota","interactions":[],"lastModifiedDate":"2024-01-11T21:40:35.247717","indexId":"wsp1669A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"1669","chapter":"A","title":"Geology and ground-water conditions in the southern part of the Camp Ripley Military Reservation, Morrison County, Minnesota","docAbstract":"<p>The southern part of the Camp Ripley Military Reservation, in central Minnesota, includes an area of about 20 square miles. This investigation was conducted to assist the U.S. National Guard Bureau in locating adequate water supplies for expansion and standby needs.</p>\n<p>Bedrock in the area consists of Precambrian phyllite which is equivalent to the Virginia slate. The area is covered largely by Pleistocene deposits in the form of moraines, ice-contact features, outwash plains, and the valley train of the Mississippi River. Almost all the surface deposits consist of outwash-plain and valley-train sediments that are generally permeable. Test drilling and an electrical-resistivity survey indicate that the post area, in the southeast part of the reservation, is underlain by about 50 to 115 feet of glacial drift. The west side of the post area is underlain by a bedrock valley filled in part by permeable glaciofluvial deposits in which there is a narrow, highly permeable channel deposit of sand and gravel. Aquifers of this type are probably the most important source of ground water in the area, although substantial quantities of water also may be obtained from other types of glacial aquifers. Properly constructed and developed wells tapping the channel deposits should yield 2,000 to 3,000 gallons per minute, or more.</p>\n<p>Recharge to the aquifers in the reservation is derived from the downward percolation of local precipitation. Most recharge occurs during the spring breakup when accumulated winter snows melt and during the warmer months when the heaviest rains occur.</p>\n<p>Sufficient water is stored in sands and gravels in the area to support substantial water-supply developments for several years, even without normal recharge.</p>\n<p>The water is harder than is desirable for domestic uses, and it is relatively highly colored, probably owing to the presence of iron. Otherwise, the water is satisfactory for most domestic purposes as it contains only about 250 parts per million of dissolved solids.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1962","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1669A","collaboration":"Prepared in cooperation with the U.S. National Guard Bureau","usgsCitation":"Jones, J., Akin, P., and Schneider, R., 1963, Geology and ground-water conditions in the southern part of the Camp Ripley Military Reservation, Morrison County, Minnesota: U.S. Geological Survey Water Supply Paper 1669, Document: iv, 32 p.; 3 Plates: 17.00 x 25.85 inches or smaller, https://doi.org/10.3133/wsp1669A.","productDescription":"Document: iv, 32 p.; 3 Plates: 17.00 x 25.85 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":424353,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24859.htm","linkFileType":{"id":5,"text":"html"}},{"id":27399,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669a/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27398,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669a/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27397,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27400,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1669a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138485,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1669a/report-thumb.jpg"}],"country":"United States","state":"Minnesota","county":"Morrison County","otherGeospatial":"Camp Ripley Military Reservation","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -94.37504768371582,\n              46.070551078344444\n            ],\n            [\n              -94.37504768371582,\n              46.10400631094191\n            ],\n            [\n              -94.32929992675781,\n              46.10400631094191\n            ],\n            [\n              -94.32929992675781,\n              46.070551078344444\n            ],\n            [\n              -94.37504768371582,\n              46.070551078344444\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685f81","contributors":{"authors":[{"text":"Jones, J.R.","contributorId":15967,"corporation":false,"usgs":true,"family":"Jones","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":144495,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Akin, P.D.","contributorId":104471,"corporation":false,"usgs":true,"family":"Akin","given":"P.D.","email":"","affiliations":[],"preferred":false,"id":144497,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schneider, Robert","contributorId":102460,"corporation":false,"usgs":true,"family":"Schneider","given":"Robert","email":"","affiliations":[],"preferred":false,"id":144496,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1975,"text":"wsp1662A - 1963 - Specific Yield--Column drainage and centrifuge moisture content","interactions":[],"lastModifiedDate":"2012-02-02T00:05:24","indexId":"wsp1662A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"1662","chapter":"A","title":"Specific Yield--Column drainage and centrifuge moisture content","docAbstract":"The specific yield of a rock or soil, with respect to water, is the ratio of (1) the volume of water which, after being saturated, it will yield by gravity to (2) its own volume. Specific retention represents the water retained against gravity drainage. The specific yield and retention when added together are equal to the total interconnected porosity of the rock or soil. Because specific retention is more easily determined than specific yield, most methods for obtaining yield first require the determination of specific retention. Recognizing the great need for developing improved methods of determining the specific yield of water-bearing materials, the U.S. Geological Survey and the California Department of Water Resources initiated a cooperative investigation of this subject. The major objectives of this research are (1) to review pertinent literature on specific yield and related subjects, (2) to increase basic knowledge of specific yield and rate of drainage and to determine the most practical methods of obtaining them, (3) to compare and to attempt to correlate the principal laboratory and field methods now commonly used to obtain specific yield, and (4) to obtain improved estimates of specific yield of water-bearing deposits in California. An open-file report, 'Specific yield of porous media, an annotated bibliography,' by A. I. Johnson, D. A. Morris, and R. C. Prill, was released in 1960 in partial fulfillment of the first objective. This report describes the second phase of the specific-yield study by the U.S. Geological Survey Hydrologic Laboratory at Denver, Colo. Laboratory research on column drainage and centrifuge moisture equivalent, two methods for estimating specific retention of porous media, is summarized. In the column-drainage study, a wide variety of materials was packed into plastic columns of 1- to 8-inch diameter, wetted with Denver tap water, and drained under controlled conditions of temperature and humidity. The effects of cleaning the porous media; of different column diameters; of dye and time on drainage; and of different methods of drainage, wetting, and packing were all determined. To insure repeatability of porosity in duplicate columns, a mechanical technique of packing was developed. \r\n\r\nIn the centrifuge moisture-content study, the centrifuge moisture-equivalent (the moisture content retained by a soil that has been first saturated and then subjected to a force equal to 1,000 times the force of gravity for 1 hour) test was first reviewed and evaluated. It was determined that for reproducible moisture-retention results the temperature and humidity should be controlled by use of a controlled-temperature centrifuge. In addition to refining this standard test, the study determined the effect of length of period of centrifuging and of applied tension on the drainage results. \r\n\r\nThe plans for future work require the continuation of the laboratory standardization study qith emphasis on investigation of soil-moisture tension and unsaturated-permeability techniques. A detailed study in the field then will be followed by correlation and evaluation of laboratory and field methods.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1662A","usgsCitation":"Johnson, A., Prill, R., and Morris, D.A., 1963, Specific Yield--Column drainage and centrifuge moisture content: U.S. Geological Survey Water Supply Paper 1662, v, 60 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1662A.","productDescription":"v, 60 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":138314,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1662a/report-thumb.jpg"},{"id":27351,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1662a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db648529","contributors":{"authors":[{"text":"Johnson, A.I.","contributorId":82676,"corporation":false,"usgs":true,"family":"Johnson","given":"A.I.","email":"","affiliations":[],"preferred":false,"id":144464,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Prill, R.C.","contributorId":27034,"corporation":false,"usgs":true,"family":"Prill","given":"R.C.","affiliations":[],"preferred":false,"id":144462,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Morris, D. A.","contributorId":56204,"corporation":false,"usgs":true,"family":"Morris","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":144463,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":15714,"text":"ofr63117 - 1963 - Uranium in sediments","interactions":[],"lastModifiedDate":"2025-06-06T15:14:29.156687","indexId":"ofr63117","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"63-117","title":"Uranium in sediments","docAbstract":"<p>An oceanographic approach is used to study the distribution of abnormal occurrences of uranium in sediments. The occurrences predominate in marine phosphorites, black marine shales, and deposits in terrestrial-fluvial sandstones and ancient conglomerites. In early Paleozoic times, marine shales accounted for the majority of uranium deposition. By the beginning of Tertiary time, the balance had shifted to predominant deposition in marine phosphorites which continued to the present. Much smaller total quantities of uranium are associated with terrestrial sandstones and ancient conglomerates, although its concentration is greater and its economic recovery is more feasible. All the abnormal occurrences fit into a unique niche in the hydrologic cycle, and emplacement was largely controlled by cycles of organic substances in water.</p><p>Radiochemical analyses of Pa<sub>231</sub>, Th<sub>230</sub>, and Ra<sub>226</sub> were made on a few hundred samples from sandstone-type uranium deposits. These results, in comparison to the uranium content of samples, indicate that much of the uranium in terrestrial sediments is presently in a slow, continual state of migration toward the ocean.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr63117","usgsCitation":"Rosholt, J.N., 1963, Uranium in sediments: U.S. Geological Survey Open-File Report 63-117, 211 p., https://doi.org/10.3133/ofr63117.","productDescription":"211 p.","costCenters":[],"links":[{"id":490202,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1963/0117/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148444,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1963/0117/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db60548b","contributors":{"authors":[{"text":"Rosholt, John Nicholas","contributorId":101679,"corporation":false,"usgs":true,"family":"Rosholt","given":"John","email":"","middleInitial":"Nicholas","affiliations":[],"preferred":false,"id":171590,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1881,"text":"wsp1619Z - 1963 - Water-resources reconnaissance in southeastern part of Honey Lake Valley, Lassen County, California","interactions":[],"lastModifiedDate":"2022-02-09T22:46:38.230427","indexId":"wsp1619Z","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"1619","chapter":"Z","title":"Water-resources reconnaissance in southeastern part of Honey Lake Valley, Lassen County, California","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1961","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1619Z","usgsCitation":"Hilton, G.S., 1963, Water-resources reconnaissance in southeastern part of Honey Lake Valley, Lassen County, California: U.S. Geological Survey Water Supply Paper 1619, Report: iii, 8 p.; 2 Plates: 23.00 × 29.50 inches and 19.00 × 29.50 inches, https://doi.org/10.3133/wsp1619Z.","productDescription":"Report: iii, 8 p.; 2 Plates: 23.00 × 29.50 inches and 19.00 × 29.50 inches","costCenters":[],"links":[{"id":138542,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1619z/report-thumb.jpg"},{"id":27170,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619z/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27171,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1619z/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":395742,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24839.htm"},{"id":27169,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619z/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"Lassen County","otherGeospatial":"Honey Lake Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120.27488708496095,\n              40.07912221750036\n            ],\n            [\n              -120.04692077636719,\n              40.07912221750036\n            ],\n            [\n              -120.04692077636719,\n              40.35910267579199\n            ],\n            [\n              -120.27488708496095,\n              40.35910267579199\n            ],\n            [\n              -120.27488708496095,\n              40.07912221750036\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd32e","contributors":{"authors":[{"text":"Hilton, George Stockbridge","contributorId":56206,"corporation":false,"usgs":true,"family":"Hilton","given":"George","email":"","middleInitial":"Stockbridge","affiliations":[],"preferred":false,"id":144299,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1846,"text":"wsp1663D - 1963 - Ground water for public supply in St. Croix, Virgin Islands","interactions":[{"subject":{"id":52247,"text":"ofr6259 - 1962 - Suggestions for the development of the ground-water resources of St. Croix, Virgin Islands","indexId":"ofr6259","publicationYear":"1962","noYear":false,"title":"Suggestions for the development of the ground-water resources of St. Croix, Virgin Islands"},"predicate":"SUPERSEDED_BY","object":{"id":1846,"text":"wsp1663D - 1963 - Ground water for public supply in St. Croix, Virgin Islands","indexId":"wsp1663D","publicationYear":"1963","noYear":false,"chapter":"D","title":"Ground water for public supply in St. Croix, Virgin Islands"},"id":1}],"lastModifiedDate":"2022-02-18T21:10:51.634302","indexId":"wsp1663D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"1663","chapter":"D","title":"Ground water for public supply in St. Croix, Virgin Islands","docAbstract":"The ground-water resources of St. Croix, V.I., if properly developed should be adequate to supply the present and near-future demand for water for public supply. Ground water is obtained from weathered volcanic and intrusive rocks (bedrocks), from limestone, and from alluvium. The water obtained from weathered bedrocks and from alluvium in the valleys of the North Side Range is generally of better quality than that obtained elsewhere on the island. The greatest yields are obtained from the limestone and alluvium of the south-central coastal plain, but the water there is generally of poor to only fair quality. In the East End area no water, or salty water, is obtained from wells.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to hydrology of Latin America and the Antilles","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. G.P.O.","doi":"10.3133/wsp1663D","usgsCitation":"Hendrickson, G.E., 1963, Ground water for public supply in St. Croix, Virgin Islands: U.S. Geological Survey Water Supply Paper 1663, iii, 27 p., https://doi.org/10.3133/wsp1663D.","productDescription":"iii, 27 p.","costCenters":[],"links":[{"id":27061,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1663d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138528,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1663d/report-thumb.jpg"},{"id":396200,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24853.htm"}],"otherGeospatial":"St. Croix, U.S. Virgin Islands","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -64.91409301757812,\n              17.65318261616436\n            ],\n            [\n              -64.56047058105469,\n              17.65318261616436\n            ],\n            [\n              -64.56047058105469,\n              17.797727159121898\n            ],\n            [\n              -64.91409301757812,\n              17.797727159121898\n            ],\n            [\n              -64.91409301757812,\n              17.65318261616436\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668eda","contributors":{"authors":[{"text":"Hendrickson, Garth Edison","contributorId":100685,"corporation":false,"usgs":true,"family":"Hendrickson","given":"Garth","email":"","middleInitial":"Edison","affiliations":[],"preferred":false,"id":144245,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1800,"text":"wsp1669G - 1963 - Low-flow frequency curves for selected long-term stream gaging stations in eastern United States","interactions":[],"lastModifiedDate":"2012-02-02T00:05:15","indexId":"wsp1669G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"1669","chapter":"G","title":"Low-flow frequency curves for selected long-term stream gaging stations in eastern United States","docAbstract":"Curves showing the magnitude and frequency of annual low flow at 85 streamgaging stations located in 17 States east and 5 States west of the Mississippi River have been smoothed and adjusted to one of four long-term periods. They are presented to show the similarity and dissimilarity of curves even in the same State and to provide background information for studies of the statistical properties of low-flow frequency curves and for studies of the relation between hydrologic environment and low flow. The results are presented as greatly reduced graphs to facilitate comparison and are summarized in tables from which expanded graphs can be plotted.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1962","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. Govt. Print. Off. :\r\nfor sale by the Supt. of Docs., U.S. Govt. Print. Off.,","doi":"10.3133/wsp1669G","usgsCitation":"Hardison, C.H., and Martin, R.O., 1963, Low-flow frequency curves for selected long-term stream gaging stations in eastern United States: U.S. Geological Survey Water Supply Paper 1669, iv, 30 p. :ill., map ;24 cm., https://doi.org/10.3133/wsp1669G.","productDescription":"iv, 30 p. :ill., map ;24 cm.","costCenters":[],"links":[{"id":137012,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1669g/report-thumb.jpg"},{"id":26955,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1669g/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648748","contributors":{"authors":[{"text":"Hardison, Clayton H.","contributorId":46073,"corporation":false,"usgs":true,"family":"Hardison","given":"Clayton","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":144178,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Martin, Robert O.R.","contributorId":18737,"corporation":false,"usgs":true,"family":"Martin","given":"Robert","email":"","middleInitial":"O.R.","affiliations":[],"preferred":false,"id":144177,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1799,"text":"wsp1669N - 1963 - Water-supply characteristics of streams in the Delaware River Basin and in southern New Jersey","interactions":[],"lastModifiedDate":"2012-02-02T00:05:15","indexId":"wsp1669N","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"1669","chapter":"N","title":"Water-supply characteristics of streams in the Delaware River Basin and in southern New Jersey","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1962","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1669N","usgsCitation":"Hardison, C., and Martin, R., 1963, Water-supply characteristics of streams in the Delaware River Basin and in southern New Jersey: U.S. Geological Survey Water Supply Paper 1669, iv, 45 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1669N.","productDescription":"iv, 45 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":137011,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1669n/report-thumb.jpg"},{"id":26953,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669n/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26954,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1669n/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4d8b","contributors":{"authors":[{"text":"Hardison, C.H.","contributorId":32506,"corporation":false,"usgs":true,"family":"Hardison","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":144175,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Martin, R.O.R.","contributorId":40193,"corporation":false,"usgs":true,"family":"Martin","given":"R.O.R.","email":"","affiliations":[],"preferred":false,"id":144176,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1762,"text":"wsp1475P - 1963 - Hydrology of stock-water development in southeastern Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:05:15","indexId":"wsp1475P","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"1475","chapter":"P","title":"Hydrology of stock-water development in southeastern Idaho","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Hydrology of the Public Domain","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1475P","usgsCitation":"Hadley, R.F., 1963, Hydrology of stock-water development in southeastern Idaho: U.S. Geological Survey Water Supply Paper 1475, iv, 563-599 p. :maps ;24 cm., https://doi.org/10.3133/wsp1475P.","productDescription":"iv, 563-599 p. :maps ;24 cm.","costCenters":[],"links":[{"id":137114,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1475p/report-thumb.jpg"},{"id":26875,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1475p/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26876,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1475p/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26877,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1475p/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601f16","contributors":{"authors":[{"text":"Hadley, R. F.","contributorId":27028,"corporation":false,"usgs":true,"family":"Hadley","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":144102,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1005,"text":"wsp1669L - 1963 - Ground-water potential of the alluvium of the Arkansas River between Little Rock and Fort Smith, Arkansas","interactions":[],"lastModifiedDate":"2012-02-02T00:05:16","indexId":"wsp1669L","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"1669","chapter":"L","title":"Ground-water potential of the alluvium of the Arkansas River between Little Rock and Fort Smith, Arkansas","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1962","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1669L","usgsCitation":"Bedinger, M.S., Emmett, L.F., and Jeffery, H., 1963, Ground-water potential of the alluvium of the Arkansas River between Little Rock and Fort Smith, Arkansas: U.S. Geological Survey Water Supply Paper 1669, iv, 29 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1669L.","productDescription":"iv, 29 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":137949,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1669l/report-thumb.jpg"},{"id":25582,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669l/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25583,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669l/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25584,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1669l/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6674b5","contributors":{"authors":[{"text":"Bedinger, M. S.","contributorId":65452,"corporation":false,"usgs":true,"family":"Bedinger","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":143006,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Emmett, L. F.","contributorId":43332,"corporation":false,"usgs":true,"family":"Emmett","given":"L.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":143005,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jeffery, H. G.","contributorId":74353,"corporation":false,"usgs":true,"family":"Jeffery","given":"H. G.","affiliations":[],"preferred":false,"id":143007,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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