{"pageNumber":"2586","pageRowStart":"64625","pageSize":"25","recordCount":68807,"records":[{"id":1857,"text":"wsp1709 - 1961 - Surface water supply of the United States, 1960, Part 6-A, Missouri River basin above Sioux City, Iowa","interactions":[],"lastModifiedDate":"2012-02-02T00:05:22","indexId":"wsp1709","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"1709","title":"Surface water supply of the United States, 1960, Part 6-A, Missouri River basin above Sioux City, Iowa","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1709","usgsCitation":"Hendricks, E.L., 1961, Surface water supply of the United States, 1960, Part 6-A, Missouri River basin above Sioux City, Iowa: U.S. Geological Survey Water Supply Paper 1709, x, 449 p. :ill., tables ;25 cm., https://doi.org/10.3133/wsp1709.","productDescription":"x, 449 p. :ill., tables ;25 cm.","costCenters":[],"links":[{"id":138492,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1709/report-thumb.jpg"},{"id":27076,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1709/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af8e4b07f02db6942c4","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":144256,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1256,"text":"wsp1535B - 1961 - Geologic control of mineral composition of stream waters of the eastern slope of the Southern Coast Ranges, California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:13","indexId":"wsp1535B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"1535","chapter":"B","title":"Geologic control of mineral composition of stream waters of the eastern slope of the Southern Coast Ranges, California","docAbstract":"Chemical analyses of waters of streams that drain the semiarid eastern slope of the southern Coast Ranges in California demonstrate that differences in the anion composition, especially in the ratio of bicarbonate to sulfate, are related chiefly to the lithologic character of the rocks exposed in the tributary drainage area. Where more than hall the drainage area of a typical eastern-slope stream is underlain by clastic marine sedimentary rocks of Jurassic and Cretaceous age, bicarbonate generally predominates over sulfate; the ratio of bicarbonate to sullate, both expressed in equivalents per million, in samples of the streams at low-flow stage ranges from 0.8 to 6. Conversely, where more than hall the drainage area is underlain by marine and continental deposits of Tertiary age and continental deposits of Quaternary age, sulfate predominates over bicarbonate, and the ratio of bicarbonate to sulfate in samples taken during the low-flow stage ranges from 0.02 to 0.7. \r\n\r\nOrganic siliceous marine shale of Tertiary age deposited in a reducing environment is probably the primary source of sullate in the region. Secondary deposits of sulfate minerals, chiefly gypsum, which are abundant in the continental deposits of late Tertiary and Quaternary age, also contribute sullate to the stream waters.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1535B","usgsCitation":"Davis, G.H., 1961, Geologic control of mineral composition of stream waters of the eastern slope of the Southern Coast Ranges, California: U.S. Geological Survey Water Supply Paper 1535, iii, 30 p. :illus., maps ;24 cm., https://doi.org/10.3133/wsp1535B.","productDescription":"iii, 30 p. :illus., maps ;24 cm.","costCenters":[],"links":[{"id":137410,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1535b/report-thumb.jpg"},{"id":26193,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1535b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a6489","contributors":{"authors":[{"text":"Davis, G. H.","contributorId":40963,"corporation":false,"usgs":true,"family":"Davis","given":"G.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":143446,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1766,"text":"wsp1499A - 1961 - Water resources of the Providence area, Rhode Island","interactions":[],"lastModifiedDate":"2012-02-02T00:05:15","indexId":"wsp1499A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"1499","chapter":"A","title":"Water resources of the Providence area, Rhode Island","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1499A","usgsCitation":"Halberg, H., Knox, C., and Pauszek, F.H., 1961, Water resources of the Providence area, Rhode Island: U.S. Geological Survey Water Supply Paper 1499, iv, 50 p. :tables, fold. map., https://doi.org/10.3133/wsp1499A.","productDescription":"iv, 50 p. :tables, fold. map.","costCenters":[],"links":[{"id":137140,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1499a/report-thumb.jpg"},{"id":26887,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1499a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26888,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1499a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f03f9","contributors":{"authors":[{"text":"Halberg, Henry N.","contributorId":19929,"corporation":false,"usgs":true,"family":"Halberg","given":"Henry N.","affiliations":[],"preferred":false,"id":144110,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Knox, C. E.","contributorId":91835,"corporation":false,"usgs":true,"family":"Knox","given":"C. E.","affiliations":[],"preferred":false,"id":144112,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pauszek, F. H.","contributorId":61399,"corporation":false,"usgs":true,"family":"Pauszek","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":144111,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1260,"text":"wsp1534 - 1961 - Progress report on wells penetrating artesian aquifers in South Dakota","interactions":[{"subject":{"id":55762,"text":"ofr5732 - 1957 - Records of selected artesian wells in South Dakota","indexId":"ofr5732","publicationYear":"1957","noYear":false,"title":"Records of selected artesian wells in South Dakota"},"predicate":"SUPERSEDED_BY","object":{"id":1260,"text":"wsp1534 - 1961 - Progress report on wells penetrating artesian aquifers in South Dakota","indexId":"wsp1534","publicationYear":"1961","noYear":false,"title":"Progress report on wells penetrating artesian aquifers in South Dakota"},"id":1}],"lastModifiedDate":"2016-04-05T09:41:30","indexId":"wsp1534","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"1534","title":"Progress report on wells penetrating artesian aquifers in South Dakota","docAbstract":"<p>Artesian aquifers underlie most of South Dakota and large areas in adjacent States. About 15,000 wells have been completed since 1881 in these aquifers within South Dakota. Many wells that originally flowed have ceased to flow and have been abandoned, and others have been equipped with pumps. Many thousands, however, continue to flow. This report presents data collected through June 1958 and includes records of 1,045 flowing and nonflowing artesian wells</p>\n<p>Sufficient information is not available at present (1958) to permit a detailed description of the geologic and hydrologic properties of artesian aquifers or their correlation in South Dakota. The description of&nbsp;the various aquifers given in this report is, therefore, necessarily a general one.</p>","language":"English","publisher":"U.S. Government Print Office","doi":"10.3133/wsp1534","usgsCitation":"Davis, R.W., Dyer, C., and Powell, J., 1961, Progress report on wells penetrating artesian aquifers in South Dakota: U.S. Geological Survey Water Supply Paper 1534, Report: iv, 100 p.;  3 Plates: 26.00 x 17.50 inches or smaller, https://doi.org/10.3133/wsp1534.","productDescription":"Report: iv, 100 p.;  3 Plates: 26.00 x 17.50 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":137430,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1534/report-thumb.jpg"},{"id":26208,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1534/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26209,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1534/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26210,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1534/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26211,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1534/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"South Dakota","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -104.029541015625,\n              45.935870621190546\n            ],\n            [\n              -104.08447265624999,\n              43.004647127794435\n            ],\n            [\n              -98.536376953125,\n              42.99661231842139\n            ],\n            [\n              -98.031005859375,\n              42.74701217318067\n            ],\n            [\n              -97.811279296875,\n              42.85180609584705\n            ],\n            [\n              -97.23999023437499,\n              42.85180609584705\n            ],\n            [\n              -96.976318359375,\n              42.73894375124379\n            ],\n            [\n              -96.624755859375,\n              42.569264372193864\n            ],\n            [\n              -96.40502929687499,\n              42.21224516288584\n            ],\n            [\n              -96.317138671875,\n              42.25291778330197\n            ],\n            [\n              -96.40502929687499,\n              42.39912215986002\n            ],\n            [\n              -96.45996093749999,\n              42.553080288955826\n            ],\n            [\n              -96.64672851562499,\n              42.73087427928485\n            ],\n            [\n              -96.5478515625,\n              42.84375132629021\n            ],\n            [\n              -96.492919921875,\n              43.03677585761058\n            ],\n            [\n              -96.427001953125,\n              43.15710884095329\n            ],\n            [\n              -96.51489257812499,\n              43.29320031385282\n            ],\n            [\n              -96.51489257812499,\n              43.381097587278596\n            ],\n            [\n              -96.602783203125,\n              43.50872101129684\n            ],\n            [\n              -96.448974609375,\n              43.492782808225\n            ],\n            [\n              -96.43798828125,\n              45.24395342262324\n            ],\n            [\n              -96.51489257812499,\n              45.38301927899065\n            ],\n            [\n              -96.64672851562499,\n              45.40616374516014\n            ],\n            [\n              -96.778564453125,\n              45.51404592560424\n            ],\n            [\n              -96.866455078125,\n              45.63708709571876\n            ],\n            [\n              -96.624755859375,\n              45.767522962149904\n            ],\n            [\n              -96.56982421875,\n              45.94351068030587\n            ],\n            [\n              -104.029541015625,\n              45.935870621190546\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d9f3","contributors":{"authors":[{"text":"Davis, R. W.","contributorId":93459,"corporation":false,"usgs":true,"family":"Davis","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":143456,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dyer, C.F.","contributorId":23917,"corporation":false,"usgs":true,"family":"Dyer","given":"C.F.","email":"","affiliations":[],"preferred":false,"id":143454,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Powell, J.E.","contributorId":27030,"corporation":false,"usgs":true,"family":"Powell","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":143455,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2289,"text":"wsp1539H - 1961 - Ground-water resources of Olmsted Air Force Base, Middletown, Pennsylvania","interactions":[],"lastModifiedDate":"2017-06-21T10:38:54","indexId":"wsp1539H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"H","title":"Ground-water resources of Olmsted Air Force Base, Middletown, Pennsylvania","docAbstract":"<p>Olmsted Air Force Base is underlain by the Gettysburg shale of Triassic age. The Gettysburg shale at the Air Force Base consists of interbedded red sandstone, siltstone, and shale. The average strike of the strata is N. 43° E., and the strata dip to the northwest at an average angle of 26°. The transmissibility of known aquifers in the warehouse area of the Air Force Base is low. Therefore, wells in the warehouse area have low specific capacities and yield only small supplies of water. Wells on the main base, however, yield relatively large supplies of water because the transmissibilities of the aquifers are relatively high. Pumping tests in the warehouse area and the eastern area of the main base indicated the presence of impermeable boundaries in both areas. Pumping tests in the central and western parts of the main base revealed that the Susquehanna River probably is acting as a source of recharge (forms a recharge boundary) for wells in those areas. Data obtained during this investigation indicate that additional supplies of ground water for Olmsted Air Force Base could best be obtained from the western part of the main base. </p>","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp1539H","usgsCitation":"Meisler, H., and Longwill, S.M., 1961, Ground-water resources of Olmsted Air Force Base, Middletown, Pennsylvania: U.S. Geological Survey Water Supply Paper 1539, iv, 34 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1539H.","productDescription":"iv, 34 p. :ill., maps ;24 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":137657,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1539h/report-thumb.jpg"},{"id":28088,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1539h/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d5ca","contributors":{"authors":[{"text":"Meisler, Harold","contributorId":34103,"corporation":false,"usgs":true,"family":"Meisler","given":"Harold","email":"","affiliations":[],"preferred":false,"id":144961,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Longwill, Stanley Miller","contributorId":85565,"corporation":false,"usgs":true,"family":"Longwill","given":"Stanley","email":"","middleInitial":"Miller","affiliations":[],"preferred":false,"id":144962,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1761,"text":"wsp1532A - 1961 - Hydrologic effects of water spreading in Box Creek basin, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:05:15","indexId":"wsp1532A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"A","title":"Hydrologic effects of water spreading in Box Creek basin, Wyoming","language":"ENGLISH","publisher":"United States Government Printing Office,","doi":"10.3133/wsp1532A","usgsCitation":"Hadley, R.F., and McQueen, I., 1961, Hydrologic effects of water spreading in Box Creek basin, Wyoming: U.S. Geological Survey Water Supply Paper 1532, iv, 47, [1] p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1532A.","productDescription":"iv, 47, [1] p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":137113,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1532a/report-thumb.jpg"},{"id":26874,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1532a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db606e92","contributors":{"authors":[{"text":"Hadley, R. F.","contributorId":27028,"corporation":false,"usgs":true,"family":"Hadley","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":144100,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McQueen, I.S.","contributorId":59774,"corporation":false,"usgs":true,"family":"McQueen","given":"I.S.","email":"","affiliations":[],"preferred":false,"id":144101,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":714,"text":"wsp1622 - 1961 - Surface water supply of the United States, 1959, Part 1-B, North Atlantic slope basins, New York to York River","interactions":[],"lastModifiedDate":"2012-02-02T00:05:09","indexId":"wsp1622","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"1622","title":"Surface water supply of the United States, 1959, Part 1-B, North Atlantic slope basins, New York to York River","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1622","usgsCitation":"Wells, J.V., 1961, Surface water supply of the United States, 1959, Part 1-B, North Atlantic slope basins, New York to York River: U.S. Geological Survey Water Supply Paper 1622, xi, 537 p. :tables ;23 cm., https://doi.org/10.3133/wsp1622.","productDescription":"xi, 537 p. :tables ;23 cm.","costCenters":[],"links":[{"id":136264,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1622/report-thumb.jpg"},{"id":25277,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1622/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db696084","contributors":{"authors":[{"text":"Wells, J. V. B.","contributorId":57037,"corporation":false,"usgs":true,"family":"Wells","given":"J.","email":"","middleInitial":"V. B.","affiliations":[],"preferred":false,"id":142642,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2155,"text":"wsp1575 - 1961 - Quality of surface waters for irrigation, western United States, 1958","interactions":[],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1575","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"1575","title":"Quality of surface waters for irrigation, western United States, 1958","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1575","usgsCitation":"Love, S.K., 1961, Quality of surface waters for irrigation, western United States, 1958: U.S. Geological Survey Water Supply Paper 1575, viii, 177 p., [1] leaf of plates :map ;23 cm., https://doi.org/10.3133/wsp1575.","productDescription":"viii, 177 p., [1] leaf of plates :map ;23 cm.","costCenters":[],"links":[{"id":137847,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1575/report-thumb.jpg"},{"id":27765,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1575/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651dcd","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":144750,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2401,"text":"wsp1619A - 1961 - Hydrogeology of a spring in a glacial terrane near Ashland, Ohio","interactions":[],"lastModifiedDate":"2012-02-02T00:05:35","indexId":"wsp1619A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"A","title":"Hydrogeology of a spring in a glacial terrane near Ashland, Ohio","language":"ENGLISH","publisher":"U.S. GPO,","doi":"10.3133/wsp1619A","usgsCitation":"Norris, S.E., 1961, Hydrogeology of a spring in a glacial terrane near Ashland, Ohio: U.S. Geological Survey Water Supply Paper 1619, 17 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1619A.","productDescription":"17 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":139034,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1619a/report-thumb.jpg"},{"id":28390,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1619a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db685160","contributors":{"authors":[{"text":"Norris, Stanley Eugene","contributorId":24772,"corporation":false,"usgs":true,"family":"Norris","given":"Stanley","email":"","middleInitial":"Eugene","affiliations":[],"preferred":false,"id":145140,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2164,"text":"wsp1521 - 1961 - Quality of surface waters of the United States, 1957, Parts 5 and 6, Hudson Bay and upper Mississippi River basins and Missouri River Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:23","indexId":"wsp1521","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"1521","title":"Quality of surface waters of the United States, 1957, Parts 5 and 6, Hudson Bay and upper Mississippi River basins and Missouri River Basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1521","usgsCitation":"Love, S.K., 1961, Quality of surface waters of the United States, 1957, Parts 5 and 6, Hudson Bay and upper Mississippi River basins and Missouri River Basin: U.S. Geological Survey Water Supply Paper 1521, ix, 379 p. :tables ;25 cm., https://doi.org/10.3133/wsp1521.","productDescription":"ix, 379 p. :tables ;25 cm.","costCenters":[],"links":[{"id":27775,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1521/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138293,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1521/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651c5a","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":144759,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1705,"text":"wsp1475F - 1961 - Ground Water at Grant Village Site, Yellowstone National Park, Wyoming","interactions":[],"lastModifiedDate":"2012-02-10T00:10:06","indexId":"wsp1475F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"F","title":"Ground Water at Grant Village Site, Yellowstone National Park, Wyoming","docAbstract":"On behalf of the National Park Service, the U.S. Geological Survey during the summer of 1959 made a study of ground-water conditions in the area of the Grant Village site, along the shore of the West Thumb of Yellowstone Lake, 1 to 2 miles south of the present facilities at West Thumb. The water supply for the present development at West Thumb is obtained from Duck Lake, but the quantity of water available from this source probably will be inadequate for the planned development at Grant Village.\r\n\r\nDuring the investigation, 11 auger holes were bored and 6 test wells were drilled. Aquifer tests by pumping and bailing methods were made at two of the test wells. All material penetrated in the auger holes and test wells is of Quaternary age except the welded tuff of possible Pliocene age that was penetrated in the lower part of test well 4.\r\n\r\nSmall to moderate quantities of water were obtained from the test wells in the area. Test well 2 yielded 35 gpm (gallons per minute) at a temperature of nearly 100 deg F. Test well 6 yielded about 15 gpm at a temperature of 48 deg F. The yield of this well might be increased by perforation of additional sections of casing, followed by further development of the well. Water from the other four test wells was of inadequate quantity, too highly mineralized, or too warm to be effectively utilized.\r\n\r\nMost of the ground water sampled had high concentrations of silica and iron, and part of the water was excessively high in fluoride content. Otherwise, the ground water was of generally suitable quality for most uses.\r\n\r\nThe most favorable area for obtaining water supplies from wells is near the lakeshore, where a large part of the water pumped would be ground-water flow diverted from its normal discharge into the lake. Moderate quantities of relatively cool water of fairly good quality may be available near the lakeshore between test wells 5 and 6 and immediately east of test well 6.","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/wsp1475F","collaboration":"Prepared in cooperation with the National Park Service","usgsCitation":"Gordon, E.D., McCullough, R.A., and Weeks, E.P., 1961, Ground Water at Grant Village Site, Yellowstone National Park, Wyoming: U.S. Geological Survey Water Supply Paper 1475, 173-200 p., https://doi.org/10.3133/wsp1475F.","productDescription":"173-200 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":12519,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.nps.gov/history/history/online_books/geology/publications/wsp/1475-F/","linkFileType":{"id":5,"text":"html"}},{"id":137092,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1475f/report-thumb.jpg"},{"id":26783,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1475f/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.66666666666667,44.25 ], [ -110.66666666666667,44.5 ], [ -110.33333333333333,44.5 ], [ -110.33333333333333,44.25 ], [ -110.66666666666667,44.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db671f58","contributors":{"authors":[{"text":"Gordon, Ellis D.","contributorId":12451,"corporation":false,"usgs":true,"family":"Gordon","given":"Ellis","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":143995,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCullough, Richard A.","contributorId":78712,"corporation":false,"usgs":true,"family":"McCullough","given":"Richard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":143996,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Weeks, Edwin P. epweeks@usgs.gov","contributorId":2576,"corporation":false,"usgs":true,"family":"Weeks","given":"Edwin","email":"epweeks@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":143994,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2165,"text":"wsp1522 - 1961 - Quality of surface waters of the United States, 1957, Parts 7 and 8, lower Mississippi River basin and western Gulf of Mexico basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:23","indexId":"wsp1522","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"1522","title":"Quality of surface waters of the United States, 1957, 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/wsp1522","usgsCitation":"Love, S.K., 1961, Quality of surface waters of the United States, 1957, Parts 7 and 8, lower Mississippi River basin and western Gulf of Mexico basins: U.S. Geological Survey Water Supply Paper 1522, x, 494 p. :ill. ;25 cm., https://doi.org/10.3133/wsp1522.","productDescription":"x, 494 p. :ill. ;25 cm.","costCenters":[],"links":[{"id":138294,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1522/report-thumb.jpg"},{"id":27776,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1522/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651c65","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":144760,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1304,"text":"wsp1475D - 1961 - Geology and occurrence of ground water at Jewel Cave National Monument, South Dakota","interactions":[],"lastModifiedDate":"2016-04-05T09:49:55","indexId":"wsp1475D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"D","title":"Geology and occurrence of ground water at Jewel Cave National Monument, South Dakota","docAbstract":"<p>Jewel Cave National Monument occupies 2 square miles of a broad plateau of sedimentary rocks in western Custer County, S. Dak., and is at an altitude of about 5,400 feet above mean sea level. The sedimentary rocks that constitute the plateau range in age from Cambrian to Pennsylvanian. Rocks of Silurian and Devonian age are absent. The presence of rocks of Ordovician age has not been established definitely but they may be represented by 10 feet of sandstone directly beneath the Englewood limestone of Mississippian age. The sedimentary formations are underlain by schist of Precambrian age.</p>\n<p>Study of outcrops in the vicinity of the monument confirms the existence of a fault about 1,500 feet north of the entrance to Jewel Cave. The fault trends generally east-west across the monument and has a displacement of about 120 feet about 1 mile west of the entrance to the cave. The effect of the fault on the occurrence of ground water near the cave is not known. In addition to the spring that furnishes the present (1959) water supply for the facilities at Jewel Cave, three springs outside the monument were visited during the study. Combined yield of the 3 springs is less than 2 gpm (gallons per minute).</p>\n<p>A single test well indicates that the monument at the well site is underlain by 665 feet of limestone, dolomite, and sandstone of Paleozoic age and an undetermined thickness of quartzbiotite schist of Precambrian age. Pumping tests using a cylinder pump indicate that the test well is capable of producing 15 to 18 gpm for a short time from 2 zones of sandstone below the Englewood limestone. These sandstones are believed to present the best possibilities for development of a permanent water supply at the monument.</p>","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/wsp1475D","collaboration":"Prepared in cooperation with the National Park Service","usgsCitation":"Dyer, C., 1961, Geology and occurrence of ground water at Jewel Cave National Monument, South Dakota: U.S. Geological Survey Water Supply Paper 1475, 23 p., https://doi.org/10.3133/wsp1475D.","productDescription":"23 p.","startPage":"139","endPage":"157","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":137886,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1475d/report-thumb.jpg"},{"id":26336,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1475d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"South Dakota","otherGeospatial":"Jewel Cave National Monument","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -103.85478973388672,\n              43.71057158566884\n            ],\n            [\n              -103.85478973388672,\n              43.74381677850666\n            ],\n            [\n              -103.81153106689452,\n              43.74381677850666\n            ],\n            [\n              -103.81153106689452,\n              43.71057158566884\n            ],\n            [\n              -103.85478973388672,\n              43.71057158566884\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64986f","contributors":{"authors":[{"text":"Dyer, C.F.","contributorId":23917,"corporation":false,"usgs":true,"family":"Dyer","given":"C.F.","email":"","affiliations":[],"preferred":false,"id":143533,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2830,"text":"wsp1592A - 1961 - Resistance coefficients and velocity distribution smooth rectangular channel","interactions":[],"lastModifiedDate":"2012-02-02T00:05:27","indexId":"wsp1592A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"1592","chapter":"A","title":"Resistance coefficients and velocity distribution smooth rectangular channel","docAbstract":"Measurements were made in a smooth rectangular channel to establish the effect of the side walls of the channel on velocity distribution and resistance to flow. The velocity distribution in the central region of a section normal to the channel followed the log arithmetic law. In the vicinity of each wall, at a point in the vertical which varied with distance from the wall, the slope of the vertical velocity curve reversed. The velocity distribution over the entire section has been defined in dimensionless terms. As well, the width-depth ratio for the wall region is expressed as a function of a similar ratio for the channel. \r\n\r\nThe variation of a resistance coefficient computed from the measurements is shown to be a function of the flow Reynolds number. The resistance coefficient, for the same Reynolds number, is slightly greater than for smooth pipe or a smooth channel of infinite width.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1592A","usgsCitation":"Tracy, H., and Lester, C., 1961, Resistance coefficients and velocity distribution smooth rectangular channel: U.S. Geological Survey Water Supply Paper 1592, iv, 18 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1592A.","productDescription":"iv, 18 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":138829,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1592a/report-thumb.jpg"},{"id":29393,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1592a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629ed2","contributors":{"authors":[{"text":"Tracy, Hubert J.","contributorId":25925,"corporation":false,"usgs":true,"family":"Tracy","given":"Hubert J.","affiliations":[],"preferred":false,"id":145868,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lester, C.M.","contributorId":67497,"corporation":false,"usgs":true,"family":"Lester","given":"C.M.","email":"","affiliations":[],"preferred":false,"id":145869,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2166,"text":"wsp1523 - 1961 - Quality of surface waters of the United States, 1957, Parts 9-14, Colorado River basin to Pacific slope basins in Oregon and lower Columbia River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:23","indexId":"wsp1523","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"1523","title":"Quality of surface waters of the United States, 1957, Parts 9-14, Colorado River basin to Pacific slope basins in Oregon and lower Columbia River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1523","usgsCitation":"Love, S.K., 1961, Quality of surface waters of the United States, 1957, Parts 9-14, Colorado River basin to Pacific slope basins in Oregon and lower Columbia River basin: U.S. Geological Survey Water Supply Paper 1523, xiv, 497 p. :tables ;24 cm., https://doi.org/10.3133/wsp1523.","productDescription":"xiv, 497 p. :tables ;24 cm.","costCenters":[],"links":[{"id":138295,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1523/report-thumb.jpg"},{"id":27777,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1523/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651b18","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":144761,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2082,"text":"wsp1545B - 1961 - Methods for determining the proper spacing of wells in artesian aquifers","interactions":[],"lastModifiedDate":"2012-02-02T00:05:23","indexId":"wsp1545B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"1545","chapter":"B","title":"Methods for determining the proper spacing of wells in artesian aquifers","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1545B","usgsCitation":"Lang, S., 1961, Methods for determining the proper spacing of wells in artesian aquifers: U.S. Geological Survey Water Supply Paper 1545, 16 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1545B.","productDescription":"16 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":138154,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1545b/report-thumb.jpg"},{"id":27644,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1545b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a1dc","contributors":{"authors":[{"text":"Lang, S.M.","contributorId":34108,"corporation":false,"usgs":true,"family":"Lang","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":144650,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2407,"text":"wsp1459H - 1961 - Microbiologic factors in the solution and transport of iron","interactions":[],"lastModifiedDate":"2012-02-02T00:05:35","indexId":"wsp1459H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"1459","chapter":"H","title":"Microbiologic factors in the solution and transport of iron","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1459H","usgsCitation":"Oborn, E.T., and Hem, J.D., 1961, Microbiologic factors in the solution and transport of iron: U.S. Geological Survey Water Supply Paper 1459, iii, p. 213-235 :ill. ;24 cm., https://doi.org/10.3133/wsp1459H.","productDescription":"iii, p. 213-235 :ill. ;24 cm.","costCenters":[],"links":[{"id":139070,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1459h/report-thumb.jpg"},{"id":28409,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1459h/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a57e4b07f02db62e0f7","contributors":{"authors":[{"text":"Oborn, Eugene T.","contributorId":21937,"corporation":false,"usgs":true,"family":"Oborn","given":"Eugene","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":145153,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hem, John David","contributorId":42577,"corporation":false,"usgs":true,"family":"Hem","given":"John","email":"","middleInitial":"David","affiliations":[],"preferred":false,"id":145154,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":322,"text":"wsp1639 - 1961 - Surface water supply of Hawaii, 1958-59","interactions":[],"lastModifiedDate":"2012-02-02T00:05:10","indexId":"wsp1639","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"1639","title":"Surface water supply of Hawaii, 1958-59","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1639","usgsCitation":"Wells, J.V., 1961, Surface water supply of Hawaii, 1958-59: U.S. Geological Survey Water Supply Paper 1639, vii, 149 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1639.","productDescription":"vii, 149 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":136181,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1639/report-thumb.jpg"},{"id":24884,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1639/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697450","contributors":{"authors":[{"text":"Wells, J. V. B.","contributorId":57037,"corporation":false,"usgs":true,"family":"Wells","given":"J.","email":"","middleInitial":"V. B.","affiliations":[],"preferred":false,"id":142235,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2658,"text":"wsp1539F - 1961 - Aquifers in melt-water channels along the southwest flank of the Des Moines Lobe, Lyon County, Minnesota","interactions":[],"lastModifiedDate":"2018-04-02T10:18:18","indexId":"wsp1539F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"F","title":"Aquifers in melt-water channels along the southwest flank of the Des Moines Lobe, Lyon County, Minnesota","docAbstract":"<p>During the Gary and Mankato substages of Wisconsin glaciation the Des Moines lobe advanced southeastward through the broad lowland of the Minnesota River valley of southwestern Minnesota, and thence southward to central Iowa.</p>\n<p>Among the most prominent topographic features in Lyon County, Minn., are five southeastward-trending end moraines, two of which are associated with and parallel to belts of surficial outwash that are approximately half a mile to a mile wide. Test drilling indicated that one of the belts of outwash is underlain by a complex system of buried melt-water channels. The other is the upper part of a series of deposits in an incised channel. The channels are filled with till, glaciolacustrine deposits, and outwash, which includes permeable deposits of water-bearing sand and gravel.</p>\n<p>Associated with the surficial melt-water channels is a pronounced southeastward-trending linear drainage pattern. By studying the lineation of streams and lakes, analyzing the available water-well data, and drilling test holes, several elongate deposits of buried outwash having little or no topographic expression were located. The long axes of the deposits are generally parallel to the lineation of the drainage and the end moraines.</p>\n<p>The melt-water channels in Lyon County trend southeastward because the flank of the ice sheet was confined by a landmass that sloped to the northeast. Similar buried channels may be present elsewhere along the southwest flank of the Des Moines lobe. If so, they probably can be located by the methods described.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1539F","collaboration":"Prepared in cooperation with the Division of Waters, Minnesota Department of Conservation, and the Marshall Municipal Utilities, Marshall, Minnesota","usgsCitation":"Schneider, R., and Rodis, H.G., 1961, Aquifers in melt-water channels along the southwest flank of the Des Moines Lobe, Lyon County, Minnesota: U.S. Geological Survey Water Supply Paper 1539, iii, 11 p., https://doi.org/10.3133/wsp1539F.","productDescription":"iii, 11 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":28994,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1539f/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138223,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1539f/report-thumb.jpg"}],"country":"United States","state":"Minnesota","otherGeospatial":"Des Moines Lobe","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -96.1083984375,\n              44.18417357325395\n            ],\n            [\n              -96.1083984375,\n              44.67255939212045\n            ],\n            [\n              -95.57968139648438,\n              44.67255939212045\n            ],\n            [\n              -95.57968139648438,\n              44.18417357325395\n            ],\n            [\n              -96.1083984375,\n              44.18417357325395\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db679f5b","contributors":{"authors":[{"text":"Schneider, Robert","contributorId":102460,"corporation":false,"usgs":true,"family":"Schneider","given":"Robert","email":"","affiliations":[],"preferred":false,"id":145568,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rodis, Harry G.","contributorId":25141,"corporation":false,"usgs":true,"family":"Rodis","given":"Harry","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":145567,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1191,"text":"wsp1539A - 1961 - Exploratory drilling for ground water in the Mountain Iron-Virginia area, St. Louis County, Minnesota","interactions":[],"lastModifiedDate":"2024-01-16T21:07:28.817798","indexId":"wsp1539A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"A","title":"Exploratory drilling for ground water in the Mountain Iron-Virginia area, St. Louis County, Minnesota","docAbstract":"<p>The Mountain Iron-Virginia area is a broad, southwest-trending valley in the central part of the Mesabi Range. The valley, which heads in the Laurentian Divide, and covers about 120 square miles, coincides approximately with a bedrock valley filled with as much as 150 feet of glacial deposits.</p>\n<p>A complex sequence of glacioaqueous sediments made up of clay, silt, sand, and gravel was delineated from test holes drilled at 238 sites. These sediments range in thickness from 0 to 125 feet and can be considered a hydrologic unit, bounded below by sandy till or bedrock and above by as much as 60 feet of clayey till. The piezometric surface ranges from 0 to about 70 feet below land surface, thus, the glacioaqueous deposits are not everywhere completely saturated. In places, however, the water is under artesian pressure.</p>\n<p>Within the Mountain Iron-Virginia area about 50 square miles are underlain by deposits 20 feet or more in thickness of silt, sand, or gravel that constitute an aquifer that is a large potential source for additional water supplies. Except for iron and manganese, which are present in excessive amounts in some wells, the water meets U.S. Public Health Service standards for municipal supplies. Pumping tests of wells in the permeable sand or gravel deposits at five sites indicate that yields of several hundred gallons per minute and possibly as much as 2,000 gpm (gallons per minute) can be expected.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, DC","doi":"10.3133/wsp1539A","collaboration":"Prepared in cooperation with the Minnesota Iron Range Resources and Rehabilitation Commission and with the Division of Waters, Minnesota Department of Conservation","usgsCitation":"Cotter, R.D., and Rogers, J., 1961, Exploratory drilling for ground water in the Mountain Iron-Virginia area, St. Louis County, Minnesota: U.S. Geological Survey Water Supply Paper 1539, Document: 19 p.; 2 Plates: 33.00 x 40.48 inches and 39.00 x 22.02 inches, https://doi.org/10.3133/wsp1539A.","productDescription":"Document: 19 p.; 2 Plates: 33.00 x 40.48 inches and 39.00 x 22.02 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":424450,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24726.htm","linkFileType":{"id":5,"text":"html"}},{"id":26056,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137939,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1539a/report-thumb.jpg"},{"id":26058,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1539a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26057,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539a/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","county":"St. Louis County","otherGeospatial":"Mountain Iron-Virginia area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -92.75,\n              47.566667\n            ],\n            [\n              -92.75,\n              47.375\n            ],\n            [\n              -92.5,\n              47.375\n            ],\n            [\n              -92.5,\n              47.566667\n            ],\n            [\n              -92.75,\n              47.566667\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8c42","contributors":{"authors":[{"text":"Cotter, R. D.","contributorId":89874,"corporation":false,"usgs":true,"family":"Cotter","given":"R.","email":"","middleInitial":"D.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":143326,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rogers, J.E.","contributorId":61401,"corporation":false,"usgs":true,"family":"Rogers","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":143325,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1297,"text":"wsp1586A - 1961 - Water quality and hydrology in the Fort Belvoir area, Virginia, 1954-55","interactions":[{"subject":{"id":51905,"text":"ofr5640 - 1956 - Investigation of water-quality hydrology in the Ft. Belvoir, Virginia area, 1954-1955","indexId":"ofr5640","publicationYear":"1956","noYear":false,"title":"Investigation of water-quality hydrology in the Ft. Belvoir, Virginia area, 1954-1955"},"predicate":"SUPERSEDED_BY","object":{"id":1297,"text":"wsp1586A - 1961 - Water quality and hydrology in the Fort Belvoir area, Virginia, 1954-55","indexId":"wsp1586A","publicationYear":"1961","noYear":false,"chapter":"A","title":"Water quality and hydrology in the Fort Belvoir area, Virginia, 1954-55"},"id":1},{"subject":{"id":52977,"text":"ofr5096 - 1950 - Additional water wells at Fort Belvoir, Virginia","indexId":"ofr5096","publicationYear":"1950","noYear":false,"title":"Additional water wells at Fort Belvoir, Virginia"},"predicate":"SUPERSEDED_BY","object":{"id":1297,"text":"wsp1586A - 1961 - Water quality and hydrology in the Fort Belvoir area, Virginia, 1954-55","indexId":"wsp1586A","publicationYear":"1961","noYear":false,"chapter":"A","title":"Water quality and hydrology in the Fort Belvoir area, Virginia, 1954-55"},"id":2}],"lastModifiedDate":"2012-02-02T00:05:13","indexId":"wsp1586A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"1586","chapter":"A","title":"Water quality and hydrology in the Fort Belvoir area, Virginia, 1954-55","docAbstract":"This report summarizes the results of an investigation of water quality and hydrology in the Fort Belvoir, Va., area for the period August 1954 to September 1955. It summarizes and evaluates information about the water resources of this area that are pertinent to the choice of location and operation of an Army nuclear power reactor. The quantity, quality, nature, and use of the local water that might be affected by the location and operation of a reactor in the area were subjects of investigation. Variations in the quality of the water caused by variation in streamflow, tidal effects, and pollution were important facets of the investigation. \r\n\r\nDuring extended periods of low streamflow in the Potomac River (usually in the late summer months), salty water moves upstream from Chesapeake Bay and increases the dissolved solids content of the surface waters adjacent to Fort Belvoir. When the streamflow is low the concentration of dissolved solids in the water near the river bottom exceeds that near the surface. \r\n\r\nThe waters in Gunston Cove usually contain more dissolved oxygen than those in the Potomac River. During the summer, the content of dissolved oxygen in the cove waters frequently exceeds 100 percent of saturation. \r\n\r\nSurface floats that were released on a flood tide in Gunston Cove moved toward the inner portion of the cove in the same direction as the wind and the tide. The maximum average velocity of these floats was 0.65 feet per second. On an ebb tide, many surface floats that were released in Gunston Cove moved toward the inner portion of the cove in the direction of the wind, in opposition to the direction of the tidal movement. Floats released near the mouth of the cove on the same tide, moved with the tide out of the cove through a narrow pass at the end of a submerged sandbar extending from the Fort Belvoir shoreline. The maximum average velocity of the floats in the pass on this ebb tide was 0.85 feet per second. Measurements of subsurface flow direction indicate that the water in the deeper part of Gunston Cove tended to move toward Accotink Bay on the flood tide and out of the cove into the Potomac River on the ebb tide. The water 150-500 feet offshore from the reactor site tended to move toward Accotink Bay on the flood tide and toward Pohick Bay on the ebb tide, whereas waters 30 feet from the Fort Belvoir shoreline tended to move counterclockwise during part of the time. In Gunston Cove the maximum measured flood velocity was 0.48 feet-per second, and the maximum ebb velocity was 0.71 per second. \r\n\r\nDuring periods of low streamflow, pollutants that enter the Potomac River at Fort Belvoir may move as much as 5.5 miles upstream on a flood tide and as much as 5 miles downstream on an ebb tide. At higher flow rates movement of pollutants is less upstream and greater downstream. The time required to flush the 10-mile reach of the Potomac River adjacent to Fort Belvoir varies from a day or two at high-flow rates to several weeks at low-flow rates.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1586A","usgsCitation":"Durfor, C.N., 1961, Water quality and hydrology in the Fort Belvoir area, Virginia, 1954-55: U.S. Geological Survey Water Supply Paper 1586, iv, 57 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1586A.","productDescription":"iv, 57 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":137037,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1586a/report-thumb.jpg"},{"id":26291,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1586a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cfe4b07f02db545ed2","contributors":{"authors":[{"text":"Durfor, Charles N.","contributorId":50881,"corporation":false,"usgs":true,"family":"Durfor","given":"Charles","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":143520,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2416,"text":"wsp1497 - 1961 - Geologic features and ground-water storage capacity of the Sacramento Valley, California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:30","indexId":"wsp1497","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"1497","title":"Geologic features and ground-water storage capacity of the Sacramento Valley, California","docAbstract":"The Sacramento Valley constitutes the northern and smaller arm of the Central Valley of California. It is about 150 miles long by about 30 miles wide; and its area is about 5,000 square miles. The Sacramento Valley is drained by the Sacramento River, the largest in California, which rises west of Mount Shasta and flows southward to join the San Joaquin River near Suisun Bay and discharges through San Francisco Bay to the Pacific. Most of the valley floor is suitable for growing crops, and under irrigation the land is highly productive. \r\n\r\nThe Sacramento Valley is underlain by sediments transported from the surrounding mountains by the Sacramento River and its tributaries. The floor of the valley slopes southward from about 300 feet above sea level at the north end near Red Bluff to sea level at Suisun Bay. The Sutter Buttes, which are erosional remnants of an old volcano rise to 2,132 feet above sea level near the center of the valley. The valley floor is not a featureless plain but is characterized by various types of topography, which have been assigned to four principal groups: 1, low hills and dissected alluvial uplands; 2, low alluvial plains and fans; 3, flood plains and natural levees; and 4, flood basins; a fifth and relatively minor group consists of the tidal Islands of the Sacramento-San Joaquin Delta, which are south of the principal area of investigation. The rocks that underlie the Sacramento Valley and the bordering mountains range from crystalline rocks of Paleozoic and Mesozoic age to unconsolidated alluvium of Recent age. These rocks have been subdivided into 20 geologic units which may be assigned to 2 broad categories: rocks that yield little water and rocks that yield water freely. The rocks of the first category are chiefly marine sedimentary rocks of Late Jurassic, Cretaceous, and Early Tertiary age and a basement complex of pre-Tertiary crystalline rocks. The rocks of the second category consist predominantly of nonmarine valley-filling sediments of late Tertiary and Quaternary age, which constitute the principal ground-water reservoir in the Sacramento Valley. \r\n\r\nThe rocks that yield little or no water includes the following geologic units: 1, Basement complex of the Sierra Nevada (pre-Tertiary); 2, Shasta series (Lower Cretaceous); 3, Chico formation (Upper Cretaceous); 4, Paleocene series; 5, Eocene series (in part, water yielding); 6, basalt (Tertiary); 7, sedimentary rocks of volcanic origin on the west side of the Sacramento Valley (Tertiary, in part water yielding) ; 8, intrusive rhyolite and andesite and vent tuff of the Sutter Buttes (Pliocene); and 9, tuff-breccia of the Sutter Buttes (Pliocene, in part water yielding). \r\n\r\nThe rocks that yield water freely, comprises the following geologic units: 1, Volcanic rocks from the Sierra Nevada (Eocene to Pliocene; in part yield little or no water); 2, Tuscan formation (Pliocene; in part yield little or no water); 3, Tehama formation (Pliocene); 4, Tehama formation and related continental sediments, undifferentiated (Pliocene and Pleistocene); 5, Laguna formation and related continental sediments (Pliocene and Pleistocene); 6, fanglomerate from the Cascade Range (Pleistocene); 7, Red Bluff formation (Pleistocene); 8, Victor formation and related deposits (Pleistocene); 9, alluvial-fan deposits (Pleistocene and Recent); 10, river deposits (Recent); and 11, flood-basin deposits (Recent). \r\n\r\nThe volcanic rocks from the Sierra Nevada consist chiefly of andesitic and rhyolitic detritus. Most of these volcanic rocks are fragmental and were deposited either as mudflows or by streams. Their permeability is extremely variable, the poorly consolidated sandstone and conglomerate strata locally yield water copiously to wells, but the interbedded fine-grained and cemented strata are virtually impermeable and act as confining layers. \r\n\r\nThe Tuscan formation, which occurs in the northeastern part of the valley, consists of fragmental andesitic and basaltic mate","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/wsp1497","usgsCitation":"Olmsted, F.H., and Davis, G.H., 1961, Geologic features and ground-water storage capacity of the Sacramento Valley, California: U.S. Geological Survey Water Supply Paper 1497, vi, 241 p. :maps (1 col.) diagrs., tables. ;24 cm., https://doi.org/10.3133/wsp1497.","productDescription":"vi, 241 p. :maps (1 col.) diagrs., tables. ;24 cm.","costCenters":[],"links":[{"id":138671,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1497/report-thumb.jpg"},{"id":28421,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1497/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28422,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1497/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28423,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1497/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28424,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1497/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28425,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1497/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28426,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1497/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a60f3","contributors":{"authors":[{"text":"Olmsted, F. 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