{"pageNumber":"2568","pageRowStart":"64175","pageSize":"25","recordCount":68807,"records":[{"id":2525,"text":"wsp1669T - 1963 - Reconnaissance of ground-water conditions in Maine","interactions":[],"lastModifiedDate":"2012-02-02T00:05:27","indexId":"wsp1669T","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":"T","title":"Reconnaissance of ground-water conditions in Maine","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/wsp1669T","usgsCitation":"Prescott, G., 1963, Reconnaissance of ground-water conditions in Maine: U.S. Geological Survey Water Supply Paper 1669, iv, 52 p. :ill., maps ;23 cm., https://doi.org/10.3133/wsp1669T.","productDescription":"iv, 52 p. :ill., maps ;23 cm.","costCenters":[],"links":[{"id":138718,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1669t/report-thumb.jpg"},{"id":28745,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669t/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28746,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1669t/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ce4b07f02db63e812","contributors":{"authors":[{"text":"Prescott, Glenn C.","contributorId":38126,"corporation":false,"usgs":true,"family":"Prescott","given":"Glenn C.","affiliations":[],"preferred":false,"id":145346,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2657,"text":"wsp1619BB - 1963 - Ground-water exploration and test pumping in the Halma-Lake Bronson area, Kittson County, Minnesota","interactions":[{"subject":{"id":52130,"text":"ofr60121 - 1960 - Ground-water exploration and test pumping in the Halma-Lake Bronson area, Kittson County, Minnesota","indexId":"ofr60121","publicationYear":"1960","noYear":false,"title":"Ground-water exploration and test pumping in the Halma-Lake Bronson area, Kittson County, Minnesota"},"predicate":"SUPERSEDED_BY","object":{"id":2657,"text":"wsp1619BB - 1963 - Ground-water exploration and test pumping in the Halma-Lake Bronson area, Kittson County, Minnesota","indexId":"wsp1619BB","publicationYear":"1963","noYear":false,"chapter":"BB","title":"Ground-water exploration and test pumping in the Halma-Lake Bronson area, Kittson County, Minnesota"},"id":1}],"lastModifiedDate":"2024-01-16T22:29:04.379831","indexId":"wsp1619BB","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":"BB","title":"Ground-water exploration and test pumping in the Halma-Lake Bronson area, Kittson County, Minnesota","docAbstract":"<p>The Halma-Lake Bronson area covers about 80 square miles in the northwestern corner of Minnesota. It is a relatively featureless poorly drained glacial drift plain which slopes gently to the west about 10 feet per mile. The plain is interrupted by sand dunes and by beach deposits of Glacial Lake Agassiz. In the northeastern part of the area, the glacial drift rests on Preeambrian crystalline basement rock; throughout the rest of the area the drift is underlain by shale, limestone, and sandstone of Ordovician age, and probably by shale and limestone of Cretaceous age.</p>\n<p>Information from 75 test holes showed that, except for minor amounts of surficial swamp sediments, eolian sand, and alluvium, the area is underlain by a'bout 320 to 420 feet of glacial drift. The most important aquifers are the relatively coarse-grained glacial outwash deposits that constitute part of the drift. The principal aquifer is a series of outwash deposits, ranging in thickness from 0 to about 280 feet, that fill a north-south trending valley cut in the underlying relatively impermeable drift. The deposits in this buried valley have an average thickness of about 130 feet in an area about 8 miles long and 3 miles wide, and are considered as a hydrologic unit.</p>\n<p>The main source of ground-water recharge is precipitation on the part of the area underlain by the principal series of outwash deposits; evapotranspiration accounts for most of the discharge. The sandy texture of the soil and the flat topography are particularly conducive to recharge, and there is extremely little surface runoff. The average depth to the water table is about 8 feet below land surface. Although the regional slope of the water table is probably to the west, locally the gradient is toward Lake Bronson and South Branch Two Rivers.</p>\n<p>Pumping tests of the outwash deposits in 2 parts of the buried valley indicate that the average coefficients of transmissibility were about 80,000 gpd per ft and about 50,000 gpd per ft. The field coefficients of permeability were about 800 and 300 gpd per sq ft, respectively.</p>\n<p>About 65 billion gallons of ground water is estimated to be in storage in the area underlain by the principal aquifer.</p>\n<p>There are no large ground-water developments in the area. The average depth of farm wells and the few municipal wells is about 25 feet.</p>\n<p>Chemical analyses of water from the principal aquifer show that the water is primarily of the bicarbonate type. The water is hard, and contains high iron Concentrations. Most wells yield water that is softer and less mineralized than ground water from the adjacent area to the west.</p>\n<p>Large quantities of water suitable for most industrial purposes are available in the Halma-Lake Bronson area. Yields of 1,000 to 2,000 gpm could probably be obtained from wells located by an adequate program of exploratory drilling and test pumping.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1619BB","collaboration":"Prepared in cooperation with the Division of Waters, Minnesota Department of Conservation, and the Department of Iron Range Resources and Rehabilitation","usgsCitation":"Schiner, G.R., 1963, Ground-water exploration and test pumping in the Halma-Lake Bronson area, Kittson County, Minnesota: U.S. Geological Survey Water Supply Paper 1619, Report: iv, 38 p.; 2 Plates: 23.50 x 18.50 inches and 19.0 x 21.0 inches, https://doi.org/10.3133/wsp1619BB.","productDescription":"Report: iv, 38 p.; 2 Plates: 23.50 x 18.50 inches and 19.0 x 21.0 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":28993,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1619bb/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138222,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1619bb/report-thumb.jpg"},{"id":28992,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619bb/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28991,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619bb/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":424455,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24815.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Minnesota","county":"Kittson County","otherGeospatial":"Halma-Lake Bronson area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -96.75,\n              48.75\n            ],\n            [\n              -96.75,\n              48.5\n            ],\n            [\n              -96.5,\n              48.5\n            ],\n            [\n              -96.5,\n              48.75\n            ],\n            [\n              -96.75,\n              48.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66ce89","contributors":{"authors":[{"text":"Schiner, George R.","contributorId":22743,"corporation":false,"usgs":true,"family":"Schiner","given":"George","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":145566,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1895,"text":"wsp1650B - 1963 - Floods of December 1955-January 1956 in the far Western States, Part 2, Streamflow data","interactions":[],"lastModifiedDate":"2012-02-02T00:05:23","indexId":"wsp1650B","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":"1650","chapter":"B","title":"Floods of December 1955-January 1956 in the far Western States, Part 2, Streamflow data","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey ;","doi":"10.3133/wsp1650B","isbn":"pbk","usgsCitation":"Hofmann, W., and Rantz, S., 1963, Floods of December 1955-January 1956 in the far Western States, Part 2, Streamflow data: U.S. Geological Survey Water Supply Paper 1650, iv, 580 p. :ill., charts ;24 cm., https://doi.org/10.3133/wsp1650B.","productDescription":"iv, 580 p. :ill., charts ;24 cm.","costCenters":[],"links":[{"id":138419,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1650b/report-thumb.jpg"},{"id":27185,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1650b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d9e4b07f02db5dfe17","contributors":{"authors":[{"text":"Hofmann, Walter","contributorId":30604,"corporation":false,"usgs":true,"family":"Hofmann","given":"Walter","email":"","affiliations":[],"preferred":false,"id":144327,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rantz, S. E.","contributorId":34106,"corporation":false,"usgs":true,"family":"Rantz","given":"S. E.","affiliations":[],"preferred":false,"id":144328,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1207,"text":"wsp1619GG - 1963 - Geology and ground-water resources of the town of Southold, Suffolk County, New York","interactions":[],"lastModifiedDate":"2022-03-22T18:33:48.468611","indexId":"wsp1619GG","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":"GG","title":"Geology and ground-water resources of the town of Southold, Suffolk County, New York","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1619GG","usgsCitation":"Crandell, H., 1963, Geology and ground-water resources of the town of Southold, Suffolk County, New York: U.S. Geological Survey Water Supply Paper 1619, Report: iv, 36 p.; 3 Plate: 36.00 × 17.00 inches or smaller, https://doi.org/10.3133/wsp1619GG.","productDescription":"Report: iv, 36 p.; 3 Plate: 36.00 × 17.00 inches or smaller","costCenters":[],"links":[{"id":397410,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24824.htm"},{"id":26093,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1619gg/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26092,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619gg/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26091,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619gg/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26090,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619gg/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138062,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1619gg/report-thumb.jpg"}],"scale":"48000","country":"United States","state":"New York","county":"Suffolk County","otherGeospatial":"Town of Southold","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -72.625,\n              40.95\n            ],\n            [\n              -72.242,\n              40.95\n            ],\n            [\n              -72.242,\n              41.167\n            ],\n            [\n              -72.625,\n              41.167\n            ],\n            [\n              -72.625,\n              40.95\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4448","contributors":{"authors":[{"text":"Crandell, Herbert C.","contributorId":15591,"corporation":false,"usgs":true,"family":"Crandell","given":"Herbert C.","affiliations":[],"preferred":false,"id":143366,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1299,"text":"wsp1605 - 1963 - Geology and hydrology of Agua Caliente Spring, Palm Springs, California","interactions":[],"lastModifiedDate":"2022-01-04T22:16:29.021388","indexId":"wsp1605","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":"1605","title":"Geology and hydrology of Agua Caliente Spring, Palm Springs, California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1605","usgsCitation":"Dutcher, L., and Bader, J., 1963, Geology and hydrology of Agua Caliente Spring, Palm Springs, California: U.S. Geological Survey Water Supply Paper 1605, Report: iv, 41 p.; 2 Plates: 18.94 × 14.81 inches and 9.82 × 14.42 inches, https://doi.org/10.3133/wsp1605.","productDescription":"Report: iv, 41 p.; 2 Plates: 18.94 × 14.81 inches and 9.82 × 14.42 inches","costCenters":[],"links":[{"id":393889,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24793.htm"},{"id":276510,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1605/plate-2.pdf"},{"id":276509,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1605/plate-1.pdf"},{"id":26312,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1605/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137047,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1605/report-thumb.jpg"}],"country":"United States","state":"California","city":"Palm Springs","otherGeospatial":"Agua Caliente Spring","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.56768798828125,\n              33.77343983379775\n            ],\n            [\n              -116.40289306640624,\n              33.77343983379775\n            ],\n            [\n              -116.40289306640624,\n              33.91259414191221\n            ],\n            [\n              -116.56768798828125,\n              33.91259414191221\n            ],\n            [\n              -116.56768798828125,\n              33.77343983379775\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4673","contributors":{"authors":[{"text":"Dutcher, L.C.","contributorId":42191,"corporation":false,"usgs":true,"family":"Dutcher","given":"L.C.","email":"","affiliations":[],"preferred":false,"id":143523,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bader, J. S.","contributorId":65830,"corporation":false,"usgs":true,"family":"Bader","given":"J. S.","affiliations":[],"preferred":false,"id":143524,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2814,"text":"wsp1619G - 1963 - Causes of depletion of the Pecos River in New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:05:26","indexId":"wsp1619G","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":"G","title":"Causes of depletion of the Pecos River in New Mexico","language":"ENGLISH","publisher":"United States Government Printing Office,","doi":"10.3133/wsp1619G","usgsCitation":"Thomas, H.E., 1963, Causes of depletion of the Pecos River in New Mexico: U.S. Geological Survey Water Supply Paper 1619, 14 p. :ill., map ;24 cm., https://doi.org/10.3133/wsp1619G.","productDescription":"14 p. :ill., map ;24 cm.","costCenters":[],"links":[{"id":138822,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1619g/report-thumb.jpg"},{"id":29363,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1619g/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db68490b","contributors":{"authors":[{"text":"Thomas, Harold E.","contributorId":36116,"corporation":false,"usgs":true,"family":"Thomas","given":"Harold","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":145842,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1295,"text":"wsp1619W - 1963 - Chemical quality of surface waters in Pennsylvania","interactions":[],"lastModifiedDate":"2017-07-07T09:16:55","indexId":"wsp1619W","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":"W","title":"Chemical quality of surface waters in Pennsylvania","docAbstract":"<p>Pennsylvania has an abundant supply of surface water of good quality. The average rainfall over the 45,300 square miles in the State is about 42 inches per year. Of this amount, about 50 percent appears in the streams as runoff. The combined mean annual runoff of the Delaware, Ohio, and Susquehanna Rivers, at their farthest downstream measuring points in the State, is in excess of 81,000 cubic feet per second. Variations in the chemical quality of the surface waters in Pennsylvania are caused by areal differences in geology, urban and industrial development, mining, quarrying, land use, and runoff. Waters having the least dissolved solids are found in the glaciated northeastern and northwestern parts of the State; waters having higher values of hardness are found in the limestone terranes in the southeastern and south-central parts. In the anthracite coal fields in the northeast and in the bituminous coal fields in the southwest, many streams receive acid mine drainage, which lowers the alkalinity and increases the sulfate content of the waters. The chemical quality of surface waters in Pennsylvania is discussed in general terms. Introductory sections of the report cover the main causative factors which influence chemical quality. </p>","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp1619W","usgsCitation":"Durfor, C.N., and Anderson, P.W., 1963, Chemical quality of surface waters in Pennsylvania: U.S. Geological Survey Water Supply Paper 1619, iv, 50 p. :ill., maps ;23 cm., https://doi.org/10.3133/wsp1619W.","productDescription":"iv, 50 p. :ill., maps ;23 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":26289,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1619w/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137035,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1619w/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e3845","contributors":{"authors":[{"text":"Durfor, Charles N.","contributorId":50881,"corporation":false,"usgs":true,"family":"Durfor","given":"Charles","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":143517,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, Peter W.","contributorId":10400,"corporation":false,"usgs":true,"family":"Anderson","given":"Peter","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":143516,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2602,"text":"wsp1669E - 1963 - Ground-water resources and geology of the Lyman-Mountain View area, Uinta County, Wyoming","interactions":[{"subject":{"id":2602,"text":"wsp1669E - 1963 - Ground-water resources and geology of the Lyman-Mountain View area, Uinta County, Wyoming","indexId":"wsp1669E","publicationYear":"1963","noYear":false,"chapter":"E","title":"Ground-water resources and geology of the Lyman-Mountain View area, Uinta County, Wyoming"},"predicate":"IS_PART_OF","object":{"id":76866,"text":"wsp1669 - 1964 - Contributions to the hydrology of the United States, 1962","indexId":"wsp1669","publicationYear":"1964","noYear":false,"title":"Contributions to the hydrology of the United States, 1962"},"id":1}],"isPartOf":{"id":76866,"text":"wsp1669 - 1964 - Contributions to the hydrology of the United States, 1962","indexId":"wsp1669","publicationYear":"1964","noYear":false,"title":"Contributions to the hydrology of the United States, 1962"},"lastModifiedDate":"2023-03-13T20:42:16.560743","indexId":"wsp1669E","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":"E","title":"Ground-water resources and geology of the Lyman-Mountain View area, Uinta County, Wyoming","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1962 (Water Supply Paper 1669)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1669E","usgsCitation":"Robinove, C.J., and Cummings, T.R., 1963, Ground-water resources and geology of the Lyman-Mountain View area, Uinta County, Wyoming: U.S. Geological Survey Water Supply Paper 1669, iv, 43 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1669E.","productDescription":"iv, 43 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":28884,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1669e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28883,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138701,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1669e/report-thumb.jpg"},{"id":414046,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24865.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Wyoming","county":"Uinta County","otherGeospatial":"Lyman-Mountain View area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -110.203,\n              41.406\n            ],\n            [\n              -110.203,\n              41.683\n            ],\n            [\n              -110.55,\n              41.683\n            ],\n            [\n              -110.55,\n              41.406\n            ],\n            [\n              -110.203,\n              41.406\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db660379","contributors":{"authors":[{"text":"Robinove, Charles Joseph","contributorId":71153,"corporation":false,"usgs":true,"family":"Robinove","given":"Charles","email":"","middleInitial":"Joseph","affiliations":[],"preferred":false,"id":145477,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cummings, T. Ray","contributorId":20722,"corporation":false,"usgs":true,"family":"Cummings","given":"T.","email":"","middleInitial":"Ray","affiliations":[],"preferred":false,"id":145476,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"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":2168,"text":"wsp1573 - 1963 - Quality of surface waters of the United States, 1958, Parts 7 and 8, lower Mississippi River basin and western Gulf of Mexico basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:23","indexId":"wsp1573","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":"1573","title":"Quality of surface waters of the United States, 1958, Parts 7 and 8, lower Mississippi River basin and western Gulf of Mexico basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1573","usgsCitation":"Love, S.K., 1963, Quality of surface waters of the United States, 1958, Parts 7 and 8, lower Mississippi River basin and western Gulf of Mexico basins: U.S. Geological Survey Water Supply Paper 1573, xi, 588 p. :ill., tables ;25 cm., https://doi.org/10.3133/wsp1573.","productDescription":"xi, 588 p. :ill., tables ;25 cm.","costCenters":[],"links":[{"id":138306,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1573/report-thumb.jpg"},{"id":27779,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1573/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651c3d","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":144763,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2180,"text":"wsp1532B - 1963 - Hydrologic and biotic characteristics of grazed and ungrazed watersheds of the Badger Wash basin in western Colorado, 1953-58","interactions":[],"lastModifiedDate":"2022-02-18T22:58:29.389041","indexId":"wsp1532B","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":"1532","chapter":"B","title":"Hydrologic and biotic characteristics of grazed and ungrazed watersheds of the Badger Wash basin in western Colorado, 1953-58","docAbstract":"A comprehensive study of the hydrologic and biotic characteristics of small drainage basins on the Colorado Plateau and the effect of grazing on these characteristics vas begun in 1953. This report presents data obtained during the first 5 years of the proposed 20-year study. \r\n\r\nPeriodic observations were made at permanent transects in 8 paired fenced and unfenced watersheds to characterize plant and ground cover, determine degree of use by livestock and measure changes in watershed cover. Results after 5 years of study indicate that changes in watershed cover have been relatively small on both grazed and ungrazed areas. Changes that did take place were mainly on shale and mixed type .soil. Ground-cover index on mixed type soil was significantly higher, 4 percent, on ungrazed ,areas than on grazed areas at the end of 5 years. \r\n\r\nPlot records were obtained using the Rocky Mountain Infiltrameter at 12 plots in each of the 8 study watersheds to determine the effect of livestock exclusion on infiltration and sheet erosion. Infiltration rates for the last 20 minutes of both the wet .and dry runs were significantly higher in 1958 than they were 5 years before, but this difference was not associated with treatment because rates on both grazed and ungrazed plots increased about .the same amount. The initial water-absorbing capacity increased significantly on ungrazed plots. No change in erosion rates was observed. \r\n\r\nRainfall was variable and below normal during 4 of the first 5 years of study. Runoff was produced mainly by thunderstorms during the summer months and was characterized by high rates of flow for short periods. Comparison of runoff in grazed and ungrazed watersheds indicates a change in the relation between precipitation and runoff because of exclusion of livestock. More sediment per unit area was produced during the 5 years of study from grazed .areas than from ungrazed areas. \r\n\r\nNo definite trend in small mammal population on grazed and ungrazed water- sheds has yet been determined. Results of preliminary studies on rabbit population indicates that rabbits prefer to inhabit ungrazed areas, but populations were judged to be not high in any area.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Hydrologic effects of land use","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U. S. Govt. Print. Off.","doi":"10.3133/wsp1532B","usgsCitation":"Lusby, G.C., Lusby, G.C., Turner, G.T., Thompson, J.R., and Reid, V.H., 1963, Hydrologic and biotic characteristics of grazed and ungrazed watersheds of the Badger Wash basin in western Colorado, 1953-58: U.S. Geological Survey Water Supply Paper 1532, Report: v, 73 p.; 1 Plate: 11.75 × 18.50 inches, https://doi.org/10.3133/wsp1532B.","productDescription":"Report: v, 73 p.; 1 Plate: 11.75 × 18.50 inches","costCenters":[],"links":[{"id":27802,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1532b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27801,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1532b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":109967,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24707.htm","linkFileType":{"id":5,"text":"html"},"description":"24707"},{"id":138221,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1532b/report-thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Badger Wash basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -108.948,\n              39.292\n            ],\n            [\n              -108.91,\n              39.292\n            ],\n            [\n              -108.91,\n              39.356\n            ],\n            [\n              -108.948,\n              39.356\n            ],\n            [\n              -108.948,\n              39.292\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db6118ab","contributors":{"authors":[{"text":"Lusby, Gregg C.","contributorId":68290,"corporation":false,"usgs":true,"family":"Lusby","given":"Gregg","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":144783,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lusby, George C.","contributorId":102860,"corporation":false,"usgs":true,"family":"Lusby","given":"George","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":144784,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Turner, George T.","contributorId":6833,"corporation":false,"usgs":true,"family":"Turner","given":"George","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":144780,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Thompson, J. R.","contributorId":27845,"corporation":false,"usgs":true,"family":"Thompson","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":144781,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Reid, Vincent H.","contributorId":57439,"corporation":false,"usgs":true,"family":"Reid","given":"Vincent","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":144782,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":1216,"text":"wsp1619FF - 1963 - Geology and ground-water resources of Bartow County, Georgia","interactions":[],"lastModifiedDate":"2017-02-01T09:11:00","indexId":"wsp1619FF","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":"FF","title":"Geology and ground-water resources of Bartow County, Georgia","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1619FF","usgsCitation":"Croft, M., 1963, Geology and ground-water resources of Bartow County, Georgia: U.S. Geological Survey Water Supply Paper 1619, iv, 32 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1619FF.","productDescription":"iv, 32 p. :ill., maps ;24 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science 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,{"id":2390,"text":"wsp1757A - 1963 - Ground-water exploration in Al Marj area, Cyrenaica, United Kingdom of Libya","interactions":[],"lastModifiedDate":"2012-02-02T00:05:33","indexId":"wsp1757A","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":"1757","chapter":"A","title":"Ground-water exploration in Al Marj area, Cyrenaica, United Kingdom of Libya","docAbstract":"The present report, based largely on fieldwork during 1959-61, describes the results of reconnaissance hydrogeologic studies and exploratory drilling to evaluate the general water-bearing properties of the rocks and the availability of groundwater supplies for irrigation, stock, and village uses in Al Marj area. These studies and the drilling were conducted under the auspices of the U.S. Operations Mission of the International Cooperation Administration. \r\n\r\nAl Marj area, located in the Province of Cyrenaica on the southern coast of the Mediterranean Sea, contains a land area of about 6,770 square kilometers. Along the Mediterranean shore is a narrow coastal plain that rises evenly to the base of an escarpment that forms the seaward front of an undulating plateau known as. Al Jabal al Akhgiar. The climate is semiarid; seasonal rainfall occurs during the winter months. Owing to orographic effects, the rainfall is somewhat higher in the Jabal than in the coastal plain. The average annual rainfall ranges from about 250 millimeters in the coastal plain to 450 millimeters on the Jabal. All the streams (wadis) of the area are ephemeral and flow only in response to heavy rains of the winter season. From a drainage divide on the Jabal some streams flow north and northwest toward the sea and the others, south and southeast to the interior desert. Solution features, such as limestone sink holes, are common in the coastal plain and a large solution depression occurs near Al Marj. \r\n\r\nThe rocks of A1 Marj area consist predominantly of limestone and some sandstone and shale; they range from Cretaceous to Miocene age. On the coastal plain Miocene limestone is locally mantled by Quaternary alluvial, beach and lagoonal deposits. The Miocene and older beds have a regional southerly dip. These rocks are broken by northeast-trending normal faults in the coastal and inland escarpments. \r\n\r\nThe ground-water reservoir is contained chiefly in fractures, bedding planes, and solution openings in the limestone country rock. The upper limit of this reservoir is marked by a water table which generally lies within 40 meters of the land surface in the coastal plain but is 100 meters or more below the surface of most of the Jabal and the interior desert. The ground-water reservoir is replenished chiefly by infiltration from surface-water runoff in wadis and to less extent by direct infiltration of rainfall. Ground water moves north and northwest toward the Mediterranean Sea and south toward the interior desert from a ground-water divide near the crest of A1 Jabal al Akhgiar. Discharge of ground water takes place by submarine outflow, spring flow, evapotranspiration, and withdrawals from wells. \r\n\r\nWells, springs, and cisterns furnish almost all water supplies for municipal, village, stock and irrigation purposes. Bengasi, A1 Marj, and A1 Abyar are the only centers of population with municipal distribution systems. Drafts from individual dug wells used for irrigation in the coastal plain generally are no more than 10 to 15 cubic meters per day. In the Jabal and the interior desert drafts from individual stock and village wells are generally less than 10 cubic meters per day and from most wells only a few thousand liters per day. \r\n\r\nSome 21 test wells were put down during the present investigation to depths ranging from 30 to 309 meters. The yields obtained by test pump and bailer ranged from 45 to 0.6 cubic meters per hour. With few exceptions, well yields sufficient for stock and village requirements were obtained. Well yields sufficient for irrigation even on a moderate scale, however, are not everywhere available. In the Jabal and the interior desert the ground water is generally of good to fair chemical quality and suitable for most purposes. In the coastal plain, however, the ground water is in places moderately to highly mineralized, and consequently for irrigation use it must be applied to the land under optimum crop soil, and drainage conditions.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1757A","usgsCitation":"Newport, T., and Haddor, Y., 1963, Ground-water exploration in Al Marj area, Cyrenaica, United Kingdom of Libya: U.S. Geological Survey Water Supply Paper 1757, iii, 24 p. :ill., maps ;24 cm. + plates folded in pocket., https://doi.org/10.3133/wsp1757A.","productDescription":"iii, 24 p. :ill., maps ;24 cm. + plates folded in pocket.","costCenters":[],"links":[{"id":139184,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1757a/report-thumb.jpg"},{"id":28365,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1757a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28366,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1757a/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28367,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1757a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66ce76","contributors":{"authors":[{"text":"Newport, T.G.","contributorId":80258,"corporation":false,"usgs":true,"family":"Newport","given":"T.G.","email":"","affiliations":[],"preferred":false,"id":145123,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haddor, Yousef","contributorId":78722,"corporation":false,"usgs":true,"family":"Haddor","given":"Yousef","email":"","affiliations":[],"preferred":false,"id":145122,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1218,"text":"wsp1539U - 1963 - Geology and ground-water resources of Hale County, Texas","interactions":[],"lastModifiedDate":"2016-08-19T14:45:24","indexId":"wsp1539U","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":"U","title":"Geology and ground-water resources of Hale County, Texas","docAbstract":"<p>Hale County, in the southern High Plains of Texas, has an area of 1,033 square miles. The land surface is one of low relief, and the regional slope is about 10 feet per mile toward the southeast. Surface runoff drains into numerous playa lakes and two intermittent streams: Running Water Draw and the Double Mountain Fork of the Brazos River.</p>\n<p>The Ogallala formation of Tertiary age is the principal water-bearing formation in the county. The Ogallala lies on red beds of Triassic age throughout most of the county and on rocks of Cretaceous age in approximately the southern fifth of the county. The Triassic and underlying Permian rocks are not fresh water bearing in the county. The Cretaceous rocks, on the other hand, are in direct hydraulic connection with the Ogallala, and a few wells tapping them yield large quantities of water from cracks and solution channels in the limestones. The Ogallala formation is overlain by thin deposits of sand, gravel, silt, and clay of Pleistocene and Recent age. These younger rocks are, for the most part, above the water table and, consequently, are not water bearing.</p>\n<p>The water in the Ogallala formation occurs principally as unconfined water in layers and lenses of sand and gravel. The hydraulic properties of the Ogallala were determined by a long-term aquifer test at Plainview, where coefficients of transmissibility ranging from 24,000 to 38,000 gpd per foot were measured. The coefficient of storage was determined to be about 0.14.</p>\n<p>The aquifer is recharged from precipitation in Hale County and in the southern High Plains northwest of the county. The water moves generally southeastward at about 2 inches a day.</p>\n<p>Ground water in Hale County is used principally for irrigation. In 1955 more than 3,700 wells were used to irrigate 470,000 acres; about 560,000 acre-feet of water was pumped. About 5,000 acre-feet was pumped for other purposes, including municipal, industrial, stock, and domestic uses.</p>\n<p>The water in the Ogallala formation in Hale County is suitable chemically for irrigation and most other uses; however, it should be softened for more satisfactory domestic use. The high silica content indicates that the water may be unsuitable for use in boilers. The fluoride content is excessive.</p>\n<p>It is estimated that in 1955 about 39 million acre-feet of water was in storage in the Ogallala formation in Hale County; however, only about 16 million is&nbsp;theoretically available to wells, and a somewhat smaller amount is practically available. About 3 million acre-feet was removed from storage during 1938-55. Water levels in wells have declined more or less steadily since 1938, and it is apparent that the ground-water resources of the county are insufficient to support large-scale perennial irrigation such as that of 1955.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1539U","usgsCitation":"Cronin, J., and Wells, L.C., 1963, Geology and ground-water resources of Hale County, Texas: U.S. Geological Survey Water Supply Paper 1539, Report: iv, 38 p.; 7 Plates, https://doi.org/10.3133/wsp1539U.","productDescription":"Report: iv, 38 p.; 7 Plates","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":137987,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1539u/report-thumb.jpg"},{"id":246987,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539u/plate-2.pdf","size":"5728","linkFileType":{"id":1,"text":"pdf"}},{"id":246988,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539u/plate-3.pdf","size":"1505","linkFileType":{"id":1,"text":"pdf"}},{"id":246989,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539u/plate-4.pdf","size":"2232","linkFileType":{"id":1,"text":"pdf"}},{"id":246990,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539u/plate-5.pdf","size":"568","linkFileType":{"id":1,"text":"pdf"}},{"id":246991,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539u/plate-6.pdf","size":"639","linkFileType":{"id":1,"text":"pdf"}},{"id":246992,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539u/plate-7.pdf","size":"600","linkFileType":{"id":1,"text":"pdf"}},{"id":109987,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24742.htm","linkFileType":{"id":5,"text":"html"},"description":"24742"},{"id":26123,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539u/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26124,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1539u/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685afb","contributors":{"authors":[{"text":"Cronin, J.G.","contributorId":47769,"corporation":false,"usgs":true,"family":"Cronin","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":143386,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wells, Lloyd C.","contributorId":29262,"corporation":false,"usgs":true,"family":"Wells","given":"Lloyd","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":143385,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2601,"text":"wsp1596 - 1963 - Geology and ground-water resources of the Greybull River-Dry Creek area, Wyoming","interactions":[],"lastModifiedDate":"2023-03-09T14:24:48.060149","indexId":"wsp1596","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":"1596","title":"Geology and ground-water resources of the Greybull River-Dry Creek area, Wyoming","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1596","usgsCitation":"Robinove, C.J., and Langford, R.H., 1963, Geology and ground-water resources of the Greybull River-Dry Creek area, Wyoming: U.S. Geological Survey Water Supply Paper 1596, Report: v, 88 p.; 4 Plates: 47.96 x 23.76 inches or smaller, https://doi.org/10.3133/wsp1596.","productDescription":"Report: v, 88 p.; 4 Plates: 47.96 x 23.76 inches or smaller","costCenters":[],"links":[{"id":138700,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1596/report-thumb.jpg"},{"id":265385,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1596/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":265388,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1596/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":265387,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1596/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":265389,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1596/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":265386,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1596/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":413892,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24785.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Wyoming","otherGeospatial":"Greybull River-Dry Creek area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -108.867,\n              44.45\n            ],\n            [\n              -108.867,\n              44.167\n            ],\n            [\n              -108.05,\n              44.167\n            ],\n            [\n              -108.05,\n              44.45\n            ],\n            [\n              -108.867,\n              44.45\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685518","contributors":{"authors":[{"text":"Robinove, Charles Joseph","contributorId":71153,"corporation":false,"usgs":true,"family":"Robinove","given":"Charles","email":"","middleInitial":"Joseph","affiliations":[],"preferred":false,"id":145475,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Langford, Russell H.","contributorId":48950,"corporation":false,"usgs":true,"family":"Langford","given":"Russell","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":145474,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2382,"text":"wsp1614 - 1963 - Water resources of Red River Parish, Louisiana","interactions":[],"lastModifiedDate":"2012-02-02T00:05:19","indexId":"wsp1614","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":"1614","title":"Water resources of Red River Parish, Louisiana","docAbstract":"Red River Parish is on the eastern flank of the Sabine uplift in northwestern Louisiana. The 'area is underlain by lignitic clay and sand of Paleocene and Eocene age which dip to the east at the rate of about 30 feet per mile. The Red River is entrenched in these rocks in the western part of the parish. Alternating valley filling and erosion during the Quaternary period have resulted in the present lowland with flanking terraces. \r\n\r\nIn the flood-plain area moderate to large quantities of very hard, iron-bearing water, suitable for irrigation, are available to wells in the alluvial sand and gravel of Quaternary age. The aquifer ranges in thickness from 20 to slightly more than 100 feet. It is recharged by downward seepage of rainfall through overlying clay and silt, by inflow from older sands adjacent to and beneath the entrenched valley, and by infiltration from the streams where the water table is below stream level during flood stages or as a result of pumping. Water levels are highest in the middle of the valley. Ground water moves mainly toward the Red River on the east and Bayou Pierre on the west, but small amounts move down the valley. Computations based on water-level and aquifer-test data indicate that the Quaternary alluvium contains more than 330 billion gallons of ground water in storage and that the maximum discharge of ground water to the streams is slightly more than 30 mgd (million gallons per day). At times of high river stage, surface water flows into the aquifer at a rate that depends in part upon the height and duration of the river stage. \r\n\r\nModerate supplies of soft, iron-bearing water may be obtained from dissected Pleistocene terrace deposits that flank the flood plains of the Red River and Black Lake Bayou. However, the quantity of water that can be pumped from these deposits varies widely from place to place because of differences in the areal extent and saturated thickness of the segments of the deposits; this extent and thickness are governed in turn by the amount of erosion the deposits have undergone. Beds of fine-grained lignitic sands of Tertiary age contain water of generally good quality to depths of 150 to 450 feet. The thinness and low permeability of the sands restrict their development to low-yield wells. Water from these sands in the western part of the parish, where they lie beneath the alluvial valley, is more mineralized than that from the younger Tertiary sands exposed in the east-central area. \r\n\r\nStreamflow records have been collected on the principal streams in Red River Parish since 1939. Additional spot low-flow data were obtained on several small streams originating within the parish for a study made in connection with the preparation of this report. Quality-of-water data for streams in the parish were collected on an occasional spot-sampling basis prior to and during this investigation. The largest source of surface water in the parish is the Red River, which drains approximately 63,400 square miles upstream from the parish. The Red River has an average flow of about 13,100 cfs (cubic feet per second), or about 8,500 mgd. Many of the streams that drain the upland area are not dependable sources of supply because their flows are not well sustained during dry seasons.\r\n\r\nThe average annual precipitation over the parish is about 52 inches, of which about 17 inches becomes runoff; this runoff is equivalent to a continuous flow of about 1.25 cfs per square mile. Seasonal and annual runoff varies, but no significant trends have been noticed.\r\n\r\nThe principal surface-water problems in the parish pertain to flood control, drainage, irrigation, and navigation. Flood problems have been alleviated considerably by the operation of Denison Dam (Lake Texoma), the completion of levees on the Red River, channel improvements on Bayou Pierre, and the completion of Wallace Lake reservoir on Cypress Bayou. There are wet lands along the Red River that would be very productive if properly drained ","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1614","usgsCitation":"Newcome, R., and Page, L.V., 1963, Water resources of Red River Parish, Louisiana: U.S. Geological Survey Water Supply Paper 1614, v, 133 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1614.","productDescription":"v, 133 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":109996,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24808.htm","linkFileType":{"id":5,"text":"html"},"description":"24808"},{"id":137824,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1614/report-thumb.jpg"},{"id":28344,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1614/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28345,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1614/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28346,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1614/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28347,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1614/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28348,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1614/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28349,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1614/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28350,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1614/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28351,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1614/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28352,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1614/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28353,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1614/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28354,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1614/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28355,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1614/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28356,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1614/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28357,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1614/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a16e4b07f02db603d22","contributors":{"authors":[{"text":"Newcome, Roy","contributorId":14796,"corporation":false,"usgs":true,"family":"Newcome","given":"Roy","affiliations":[],"preferred":false,"id":145113,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Page, Leland Vernon","contributorId":95450,"corporation":false,"usgs":true,"family":"Page","given":"Leland","email":"","middleInitial":"Vernon","affiliations":[],"preferred":false,"id":145114,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2744,"text":"wsp1536H - 1963 - Electric analog of three-dimensional flow to wells and its application to unconfined aquifers","interactions":[],"lastModifiedDate":"2012-02-02T00:05:34","indexId":"wsp1536H","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":"1536","chapter":"H","title":"Electric analog of three-dimensional flow to wells and its application to unconfined aquifers","docAbstract":"Electric-analog design criteria are established from the differential equations of ground-water flow for analyzing pumping-test data. A convenient analog design was obtained by transforming the cylindrical equation of flow to a rectilinear form. The design criteria were applied in the construction of an electric analog, which was used for studying pumping-test data collected near Grand Island, Nebr. \r\n\r\nData analysis indicated (1) vertical flow components near pumping wells in unconfined aquifers may be much more significant in the control of water-table decline than radial flow components for as much as a day of pumping; (2) the specific yield during the first few minutes of pumping appears to be a very small fraction of that observed after pumping for more than 1 day; and (3) estimates of specific yield made from model studies seem much more sensitive to variations in assumed flow conditions than are estimates of permeability. Analysis of pumping-test data where vertical flow components are important requires that the degree of anisotropy be known. A procedure for computing anisotropy directly from drawdowns observed at five points was developed. Results obtained in the analog study emphasize the futility of calculating unconfined aquifer properties from pumping tests of short duration by means of equations based on the assumptions that vertical flow components are negligible and specific yield is constant.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1536H","usgsCitation":"Stallman, R., 1963, Electric analog of three-dimensional flow to wells and its application to unconfined aquifers: U.S. Geological Survey Water Supply Paper 1536, iv, 37 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1536H.","productDescription":"iv, 37 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":139040,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1536h/report-thumb.jpg"},{"id":29170,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1536h/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60ede1","contributors":{"authors":[{"text":"Stallman, Robert W.","contributorId":32903,"corporation":false,"usgs":true,"family":"Stallman","given":"Robert W.","affiliations":[],"preferred":false,"id":145698,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2736,"text":"wsp1525 - 1963 - Geology and water resources of the Santa Fe area, New Mexico","interactions":[],"lastModifiedDate":"2024-02-01T21:39:54.322308","indexId":"wsp1525","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":"1525","title":"Geology and water resources of the Santa Fe area, New Mexico","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1525","usgsCitation":"Spiegel, Z., and Baldwin, B., 1963, Geology and water resources of the Santa Fe area, New Mexico: U.S. Geological Survey Water Supply Paper 1525, Report: xiii, 258 p.; 7 Plates: 25.50 x 27.00 inches or smaller, https://doi.org/10.3133/wsp1525.","productDescription":"Report: xiii, 258 p.; 7 Plates: 25.50 x 27.00 inches or smaller","costCenters":[],"links":[{"id":29162,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1525/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":425252,"rank":10,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_93055.htm","linkFileType":{"id":5,"text":"html"}},{"id":29161,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1525/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29160,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1525/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29159,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1525/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29158,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1525/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29157,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1525/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29156,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1525/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29155,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1525/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138914,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1525/report-thumb.jpg"}],"country":"United States","state":"New Mexico","city":"Santa Fe","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -106.10021096351649,\n              35.863211375763555\n            ],\n            [\n              -106.10021096351649,\n              35.51535393855693\n            ],\n            [\n              -105.74329798644887,\n              35.51535393855693\n            ],\n            [\n              -105.74329798644887,\n              35.863211375763555\n            ],\n            [\n              -106.10021096351649,\n              35.863211375763555\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db683e5d","contributors":{"authors":[{"text":"Spiegel, Zane","contributorId":17978,"corporation":false,"usgs":true,"family":"Spiegel","given":"Zane","email":"","affiliations":[],"preferred":false,"id":145688,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baldwin, Brewster","contributorId":40585,"corporation":false,"usgs":true,"family":"Baldwin","given":"Brewster","email":"","affiliations":[],"preferred":false,"id":145689,"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":95,"text":"wsp1770 - 1963 - Ground-water levels in the United States, 1956-60, southwestern states","interactions":[{"subject":{"id":23879,"text":"ofr6196 - 1961 - Water levels in observation wells in Santa Barbara County, California, in 1960","indexId":"ofr6196","publicationYear":"1961","noYear":false,"title":"Water levels in observation wells in Santa Barbara County, California, in 1960"},"predicate":"SUPERSEDED_BY","object":{"id":95,"text":"wsp1770 - 1963 - Ground-water levels in the United States, 1956-60, southwestern states","indexId":"wsp1770","publicationYear":"1963","noYear":false,"title":"Ground-water levels in the United States, 1956-60, southwestern states"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:10","indexId":"wsp1770","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":"1770","title":"Ground-water levels in the United States, 1956-60, southwestern states","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1770","usgsCitation":"Hackett, O.M., 1963, Ground-water levels in the United States, 1956-60, southwestern states: U.S. Geological Survey Water Supply Paper 1770, v, 160 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1770.","productDescription":"v, 160 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":136059,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1770/report-thumb.jpg"},{"id":24701,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1770/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6675b0","contributors":{"authors":[{"text":"Hackett, O. M.","contributorId":38527,"corporation":false,"usgs":true,"family":"Hackett","given":"O.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":141923,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":94,"text":"wsp1760 - 1963 - Ground-water levels in the United States, 1956-60, northwestern states","interactions":[],"lastModifiedDate":"2012-02-02T00:05:10","indexId":"wsp1760","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":"1760","title":"Ground-water levels in the United States, 1956-60, northwestern states","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1760","usgsCitation":"Hackett, O.M., 1963, Ground-water levels in the United States, 1956-60, northwestern states: U.S. Geological Survey Water Supply Paper 1760, v, 222 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1760.","productDescription":"v, 222 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":136058,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1760/report-thumb.jpg"},{"id":24700,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1760/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6675aa","contributors":{"authors":[{"text":"Hackett, O. M.","contributorId":38527,"corporation":false,"usgs":true,"family":"Hackett","given":"O.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":141922,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2727,"text":"wsp1475N - 1963 - Hydrology of stock-water development on the public domain of western Utah","interactions":[],"lastModifiedDate":"2017-09-06T18:19:14","indexId":"wsp1475N","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":"N","title":"Hydrology of stock-water development on the public domain of western Utah","docAbstract":"<p>A geologic and hydrologic reconnaissance was made on the public domain of western Utah to appraise the water resources of the area and to provide a basis for locating and developing sources of stock water. The study area includes the Bonneville, Pahvant, and Virgin Grazing Districts, in parts of Tooele, Utah, Juab, Millard, Beaver, Iron, and Washington Counties, Utah.</p><p>Western Utah is in the Great Basin section of the Basin and Range physiographic province and is typified by northward-trending parallel mountain ranges, and basins of interior drainage. Precipitation ranges from 5 to 9 inches annually in most of the valleys but in some places it is as much as 15 or 16 inches and probably is considerably greater in the mountains.</p><p>The valleys of western Utah have been classified in the report according to their hydrologic and topographic characteristics. The Great Salt Lake valley and the Sevier Lake valley are closed or terminal valleys having no outlet for the discharge of water except by evaporation. Such valleys are topographically closed and hydrologically undrained. Valleys tributary to these terminal valleys are topographically open valleys from which water is discharged by gravity flow to the terminal valley. Quality of ground water in the valleys of western Utah depends upon the valley type and place where the water is sampled with respect to the body of ground water in the valley fill. Quality of the water in the drained parts of the valleys is usually good whereas water in the undrained parts of the valleys may be heavily charged with dissolved mineral contaminants. Limits of tolerance for use of salt-contaminated water are cited.</p><p>The adequacy of distribution of water supplies in western Utah was determined by application of the service area concept to the existing supplies. Stock-water supplies are obtained from wells, springs, and reservoirs. Most of the wells are in the valleys where water is obtained from valley fill; the depth to water ranges from a few tens of feet to several hundred feet. Ground water generally cannot be obtained in the mountains because the rocks either lack permeability or are drained.</p><p>Data collected in 13 valleys, each valley forming a ground-water unit, are listed in the tables and are used to evaluate the prospects for obtaining additional water supplies.</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. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1475N","usgsCitation":"Snyder, C., 1963, Hydrology of stock-water development on the public domain of western Utah: U.S. Geological Survey Water Supply Paper 1475, Report: iv, 50 p.; Plate: 19.00 x 35.50 inches, https://doi.org/10.3133/wsp1475N.","productDescription":"Report: iv, 50 p.; Plate: 19.00 x 35.50 inches","startPage":"487","endPage":"536","numberOfPages":"57","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":138956,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1475n/report-thumb.jpg"},{"id":29135,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1475n/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29136,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1475n/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","publicComments":"Prepared as part of the soil and moisture program of the Department of the Interior","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db602036","contributors":{"authors":[{"text":"Snyder, Charles T.","contributorId":53767,"corporation":false,"usgs":true,"family":"Snyder","given":"Charles T.","affiliations":[],"preferred":false,"id":145673,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1298,"text":"wsp1419 - 1963 - Geologic and hydrologic features of the San Bernardino area, California; with special reference to underflow across the San Jacinto fault","interactions":[{"subject":{"id":51238,"text":"ofr5358 - 1953 - San Bernardion Area, California: Three maps showing water-level contours for the San Bernardino area for spring 1936, spring 1945, and spring 1951; east-west geologic section from Colton to Mill Creek Canyon; geologic section from Shandin Hills southeast to Bryn Mawr; and water level profiles along the section from Colton to Mill Creek Canyon","indexId":"ofr5358","publicationYear":"1953","noYear":false,"title":"San Bernardion Area, California: Three maps showing water-level contours for the San Bernardino area for spring 1936, spring 1945, and spring 1951; east-west geologic section from Colton to Mill Creek Canyon; geologic section from Shandin Hills southeast to Bryn Mawr; and water level profiles along the section from Colton to Mill Creek Canyon"},"predicate":"SUPERSEDED_BY","object":{"id":1298,"text":"wsp1419 - 1963 - Geologic and hydrologic features of the San Bernardino area, California; with special reference to underflow across the San Jacinto fault","indexId":"wsp1419","publicationYear":"1963","noYear":false,"title":"Geologic and hydrologic features of the San Bernardino area, California; with special reference to underflow across the San Jacinto fault"},"id":1},{"subject":{"id":51253,"text":"ofr5376 - 1953 - Maps and sections showing ground-water conditions in the San Bernardino area, California","indexId":"ofr5376","publicationYear":"1953","noYear":false,"title":"Maps and sections showing ground-water conditions in the San Bernardino area, California"},"predicate":"SUPERSEDED_BY","object":{"id":1298,"text":"wsp1419 - 1963 - Geologic and hydrologic features of the San Bernardino area, California; with special reference to underflow across the San Jacinto fault","indexId":"wsp1419","publicationYear":"1963","noYear":false,"title":"Geologic and hydrologic features of the San Bernardino area, California; with special reference to underflow across the San Jacinto fault"},"id":2}],"lastModifiedDate":"2022-02-01T20:10:25.234553","indexId":"wsp1419","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":"1419","title":"Geologic and hydrologic features of the San Bernardino area, California; with special reference to underflow across the San Jacinto fault","docAbstract":"<p>This is the second in a series of interpretive reports on subsurface outflow from the ground-water basins of San Bernardino County, Calif., prepared by the U.S. Geological Survey in cooperation with the San Bernardino County Flood Control District. One principal purpose of the study was to estimate the ground-water outflow from the Bunker Hill basin to the Rialto-Colton basin across the San Jacinto fault, which, except locally, forms a nearly impermeable boundary between the two basins. In addition, the report deals qualitatively with the geology, the fault barriers that divide the area into several ground-water basins, the physical nature and degree of imperviousness of the barriers, the occurrence and movement of ground water and fluctuations of water level in the basins, and the chemical quality of surface and ground waters in the San Bernardino area. The report includes a geologic map and sections, water-level-contour maps and profiles, and hydrographs of selected well. The Santa Ana River, the principal stream, flows generally westward across the area. Channels of the river and its tributaries overlie a large irregular structural depression filled with alluvial deposits ranging in age from late Tertiary to Recent and forming a valley bounded on the north by the San Gabriel Mountains, on the east by the San Bernardino Mountains, and on the south by an irregular group of hills. Large alluvial fans underlie most of the area, but its landforms also include alluvial benches and terraces near the mountains, stream channels, and elongate hills, ridges, and scarps along the trace of the San Jacinto fault, which strikes northwestward across the valley about in the center of the area. This fault and others divide the area into ground-water basins, which include the Bunker Hill, Rialto-Colton, upper and lower Lytle and Chino basins. The water-bearing deposits include the following units: the younger alluvium. of Recent age, which occupies principally the backfilled channels beneath the Santa Ana River and its tributaries and through which ground water moves from Bunker Hill basin to Rialto-Colton basin; the older alluvium, of Pleistocene age, which is the principal water-bearing unit of the area and yields water to more than a thousand wells; and continental deposits of Tertiary to Quaternary age, which crop out along the southern margin of the area and locally along the San Gabriel Mountains on the north. The younger alluvium attains a maximum thickness of about 125 feet beneath the Santa Ana River south of San Bernardino. Locally in the Bunker Hill basin it is composed of two members, an upper member of relatively impermeable clay and a lower member of highly permeable material in which water is confined by the upper member. The older alluvium locally has a known thickness greater than 700 feet; elsewhere in the San Bernardino Valley it may exceed 1,400 feet. Locally, where ground water is confined in Bunker Hill basin, the older alluvium is divided into three permeable water-bearing zones separated from each other and from the younger alluvium above by less permeable zones. In parts of Chino and Rialto-Colton basins the alluvium consists of a coarse-grained facies along a former course of a major stream that is interfingered with and overlain by relatively fine-grained deposits. The permeability of the younger alluvium in the area beneath the Santa Ana River downstream from the San Jacinto fault was determined from tests to be about 2,700 gallons per day per square foot. The permeability of the coarse water-yielding materials of the older alluvium several miles downstream was estimated from tests to be about the same magnitude. Rocks that yield practically no water include continental rocks of Tertiary age, which are not exposed in the area but are tapped by wells in Rialto-Colton basin, and crystalline and metamorphic rocks of pre-Tertiary age that form the bedrock of the area.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1419","usgsCitation":"Dutcher, L., and Garrett, A., 1963, Geologic and hydrologic features of the San Bernardino area, California; with special reference to underflow across the San Jacinto fault: U.S. Geological Survey Water Supply Paper 1419, Report: vi, 114 p.; 19 Plates: \t37.00 × 52.19 inches or smaller, https://doi.org/10.3133/wsp1419.","productDescription":"Report: vi, 114 p.; 19 Plates: \t37.00 × 52.19 inches or 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