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,{"id":38962,"text":"pp417E - 1965 - Natural water loss and recoverable water in mountain basins of southern California","interactions":[],"lastModifiedDate":"2012-02-02T00:10:37","indexId":"pp417E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"417","chapter":"E","title":"Natural water loss and recoverable water in mountain basins of southern California","language":"ENGLISH","doi":"10.3133/pp417E","usgsCitation":"Crippen, J., 1965, Natural water loss and recoverable water in mountain basins of southern California: U.S. Geological Survey Professional Paper 417, p. E1-E24, https://doi.org/10.3133/pp417E.","productDescription":"p. E1-E24","costCenters":[],"links":[{"id":122474,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0417e/report-thumb.jpg"},{"id":66030,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0417e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db6980c5","contributors":{"authors":[{"text":"Crippen, J. R.","contributorId":87985,"corporation":false,"usgs":true,"family":"Crippen","given":"J. R.","affiliations":[],"preferred":false,"id":220731,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2771,"text":"wsp1809B - 1965 - Geology and ground-water resources of Waushara County, Wisconsin","interactions":[],"lastModifiedDate":"2015-10-02T13:14:56","indexId":"wsp1809B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1809","chapter":"B","title":"Geology and ground-water resources of Waushara County, Wisconsin","docAbstract":"<p>Abundant ground water for irrigation is available in the outwash deposits in western Waushara County, and many more large-capacity wells can be developed in these deposits without seriously lowering the water level. Pumping for irrigation temporarily lowers water levels in the vicinity of the wells but has not lowered regional water levels. Pumpage has probably intercepted and utilized some of the recharge that would have been rapidly discharged from the aquifer. Ground water is continuously being discharged to streams and to the atmosphere by evapotranspiration, but intermittent recharge from precipitation replaces the discharged water. Recharge and discharge are in approximate balance, maintaining about the same amount of ground water in storage. Further recharge to the aquifer is rapidly discharged to streams. The sandstones, till, and glaciolacustrine deposits in Waushara County generally yield small to moderate amounts of water to wells but do not produce enough water for irrigation ; recent alluvium may yield large quantities of water to wells. In general, the ground water is of good quality, except for hardness and local high-iron concentrations.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1962","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1809B","collaboration":"Prepared in cooperation with the University of Wisconsin Geological and Natural History Survey","usgsCitation":"Summers, W.K., 1965, Geology and ground-water resources of Waushara County, Wisconsin: U.S. Geological Survey Water Supply Paper 1809, Report: iv, 32 p.; 3 Plates: 41.96 x 22.00 inches and 39.5 x 22.5 inches, https://doi.org/10.3133/wsp1809B.","productDescription":"Report: iv, 32 p.; 3 Plates: 41.96 x 22.00 inches and 39.5 x 22.5 inches","numberOfPages":"40","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":29216,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29217,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29218,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809b/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29219,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1809b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138609,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1809b/report-thumb.jpg"}],"country":"United States","state":"Wisconsin","county":"Waushara County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-89.5977,44.2458],[-89.488,44.244],[-89.4835,44.244],[-89.3649,44.2439],[-89.3464,44.2439],[-89.2469,44.2438],[-89.2245,44.2433],[-89.1288,44.243],[-89.104,44.243],[-89.007,44.2426],[-88.9821,44.243],[-88.8871,44.2426],[-88.8859,44.1587],[-88.8882,44.1136],[-88.8861,44.0713],[-88.8862,43.9833],[-88.944,43.9836],[-89.0063,43.9834],[-89.1283,43.9833],[-89.1658,43.983],[-89.2472,43.9827],[-89.3654,43.9824],[-89.4823,43.982],[-89.598,43.9824],[-89.5981,44.0685],[-89.5976,44.156],[-89.5977,44.2458]]]},\"properties\":{\"name\":\"Waushara\",\"state\":\"WI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685374","contributors":{"authors":[{"text":"Summers, William Kelly","contributorId":69532,"corporation":false,"usgs":true,"family":"Summers","given":"William","email":"","middleInitial":"Kelly","affiliations":[],"preferred":false,"id":145756,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2870,"text":"wsp1613E - 1965 - Geology and occurrence of fresh and brackish ground water in Glynn County, Georgia","interactions":[],"lastModifiedDate":"2019-12-30T10:05:52","indexId":"wsp1613E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1613","chapter":"E","title":"Geology and occurrence of fresh and brackish ground water in Glynn County, Georgia","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp1613E","usgsCitation":"Wait, R.L., 1965, Geology and occurrence of fresh and brackish ground water in Glynn County, Georgia: U.S. Geological Survey Water Supply Paper 1613, Report: vi, 94 p.; 4 Plates: 12.00 x 21.50 inches or smaller, https://doi.org/10.3133/wsp1613E.","productDescription":"Report: vi, 94 p.; 4 Plates: 12.00 x 21.50 inches or smaller","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":138966,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1613e/report-thumb.jpg"},{"id":29483,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1613e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29484,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1613e/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29485,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1613e/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29486,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1613e/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29487,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1613e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Georgia","county":"Glynn County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.0404052734375,\n              30.949346915468563\n            ],\n            [\n              -81.1505126953125,\n              30.949346915468563\n            ],\n            [\n              -81.1505126953125,\n              31.5504526754715\n            ],\n            [\n              -82.0404052734375,\n              31.5504526754715\n            ],\n            [\n              -82.0404052734375,\n              30.949346915468563\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db6848a0","contributors":{"authors":[{"text":"Wait, Robert L.","contributorId":12839,"corporation":false,"usgs":true,"family":"Wait","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":145937,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2901,"text":"wsp1799 - 1965 - Geology and occurrence of ground water in Otero County, and the southern part of Crowley County, Colorado","interactions":[],"lastModifiedDate":"2022-12-29T22:54:22.952403","indexId":"wsp1799","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1799","title":"Geology and occurrence of ground water in Otero County, and the southern part of Crowley County, Colorado","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1799","usgsCitation":"Weist, W.G., Jenkins, E., and Horr, C.A., 1965, Geology and occurrence of ground water in Otero County, and the southern part of Crowley County, Colorado: U.S. Geological Survey Water Supply Paper 1799, Report: vi, 90 p.; 5 Plates: 34.50 x 45.68 inches or smaller, https://doi.org/10.3133/wsp1799.","productDescription":"Report: vi, 90 p.; 5 Plates: 34.50 x 45.68 inches or smaller","costCenters":[],"links":[{"id":109902,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23271.htm","linkFileType":{"id":5,"text":"html"},"description":"23271"},{"id":29580,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1799/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29579,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1799/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29578,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1799/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29577,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1799/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29576,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1799/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29575,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1799/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138382,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1799/report-thumb.jpg"}],"country":"United States","state":"Colorado","county":"Crowley County, Otero County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -103.057,\n              38.266\n            ],\n            [\n              -103.057,\n              37.639\n            ],\n            [\n              -103.4,\n              37.639\n            ],\n            [\n              -103.4,\n              38.266\n            ],\n            [\n              -103.057,\n              38.266\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db684840","contributors":{"authors":[{"text":"Weist, William G. Jr.","contributorId":21527,"corporation":false,"usgs":true,"family":"Weist","given":"William","suffix":"Jr.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":145981,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jenkins, Edward D.","contributorId":17972,"corporation":false,"usgs":true,"family":"Jenkins","given":"Edward D.","affiliations":[],"preferred":false,"id":145980,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Horr, Clarence Albert","contributorId":60611,"corporation":false,"usgs":true,"family":"Horr","given":"Clarence","email":"","middleInitial":"Albert","affiliations":[],"preferred":false,"id":145982,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1488,"text":"wsp1641 - 1965 - Quality of surface waters of the United States, 1959, Parts 1 & 2, North Atlantic slope basins and South Atlantic slope and eastern Gulf of Mexico Basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:14","indexId":"wsp1641","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1641","title":"Quality of surface waters of the United States, 1959, Parts 1 & 2, North Atlantic slope basins and South Atlantic slope and eastern Gulf of Mexico Basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1641","usgsCitation":"Love, S.K., 1965, Quality of surface waters of the United States, 1959, Parts 1 & 2, North Atlantic slope basins and South Atlantic slope and eastern Gulf of Mexico Basins: U.S. Geological Survey Water Supply Paper 1641, xi, 460 p. :map ; 24 cm., https://doi.org/10.3133/wsp1641.","productDescription":"xi, 460 p. :map ; 24 cm.","costCenters":[],"links":[{"id":136924,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1641/report-thumb.jpg"},{"id":26556,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1641/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651b64","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":143766,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2899,"text":"wsp1801 - 1965 - Geology and availability of ground water in the northern part of the White Sands Missile Range and vicinity, New Mexico","interactions":[],"lastModifiedDate":"2022-01-11T22:38:15.201218","indexId":"wsp1801","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1801","title":"Geology and availability of ground water in the northern part of the White Sands Missile Range and vicinity, New Mexico","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1801","usgsCitation":"Weir, J., 1965, Geology and availability of ground water in the northern part of the White Sands Missile Range and vicinity, New Mexico: U.S. Geological Survey Water Supply Paper 1801, Report: v, 78 p.; 1 Plate: 37.00 × 28.00 inches, https://doi.org/10.3133/wsp1801.","productDescription":"Report: v, 78 p.; 1 Plate: 37.00 × 28.00 inches","costCenters":[],"links":[{"id":394227,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24996.htm"},{"id":29565,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1801/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29566,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1801/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138380,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1801/report-thumb.jpg"}],"country":"United States","state":"New Mexico","otherGeospatial":"White Sands Missile Range and vicinity","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.872,\n              33.233\n            ],\n            [\n              -106.013,\n              33.233\n            ],\n            [\n              -106.013,\n              33.953\n            ],\n            [\n              -106.872,\n              33.953\n            ],\n            [\n              -106.872,\n              33.233\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686459","contributors":{"authors":[{"text":"Weir, J. E.","contributorId":88715,"corporation":false,"usgs":true,"family":"Weir","given":"J. E.","affiliations":[],"preferred":false,"id":145978,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":747,"text":"wsp1615G - 1965 - Testing procedures and results of studies of artificial recharge in the Grand Prairie region, Arkansas","interactions":[],"lastModifiedDate":"2012-02-02T00:05:09","indexId":"wsp1615G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1615","chapter":"G","title":"Testing procedures and results of studies of artificial recharge in the Grand Prairie region, Arkansas","language":"ENGLISH","publisher":"U.S. Department of the Interior, Geological Survey ;","doi":"10.3133/wsp1615G","isbn":"pbk","usgsCitation":"Sniegocki, R.T., Bayley, F.H., Engler, K., and Stephens, J.W., 1965, Testing procedures and results of studies of artificial recharge in the Grand Prairie region, Arkansas: U.S. Geological Survey Water Supply Paper 1615, iv, 56 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1615G.","productDescription":"iv, 56 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":136384,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1615g/report-thumb.jpg"},{"id":25316,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1615g/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db684ab1","contributors":{"authors":[{"text":"Sniegocki, Richard T.","contributorId":67068,"corporation":false,"usgs":true,"family":"Sniegocki","given":"Richard","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":142678,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bayley, F. H.","contributorId":75896,"corporation":false,"usgs":true,"family":"Bayley","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":142679,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Engler, Kyle","contributorId":106862,"corporation":false,"usgs":true,"family":"Engler","given":"Kyle","email":"","affiliations":[],"preferred":false,"id":142680,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stephens, J. W.","contributorId":49771,"corporation":false,"usgs":true,"family":"Stephens","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":142677,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":2863,"text":"wsp1772 - 1965 - Geology and ground-water resources of Prowers County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:05:35","indexId":"wsp1772","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1772","title":"Geology and ground-water resources of Prowers County, Colorado","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/wsp1772","usgsCitation":"Voegeli, P., and Hershey, L.A., 1965, Geology and ground-water resources of Prowers County, Colorado: U.S. Geological Survey Water Supply Paper 1772, vi, 101 p. :illus., map. and portfolio (illus. (3 col.) fold. col. map) ;24 cm., https://doi.org/10.3133/wsp1772.","productDescription":"vi, 101 p. :illus., map. and portfolio (illus. (3 col.) fold. col. map) ;24 cm.","costCenters":[],"links":[{"id":110013,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24949.htm","linkFileType":{"id":5,"text":"html"},"description":"24949"},{"id":138989,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1772/report-thumb.jpg"},{"id":29463,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1772/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29464,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1772/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29465,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1772/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29466,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1772/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29467,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1772/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29468,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1772/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29469,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1772/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685983","contributors":{"authors":[{"text":"Voegeli, Paul T.","contributorId":19937,"corporation":false,"usgs":true,"family":"Voegeli","given":"Paul T.","affiliations":[],"preferred":false,"id":145925,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hershey, Lloyd A.","contributorId":6831,"corporation":false,"usgs":true,"family":"Hershey","given":"Lloyd","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":145924,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1194,"text":"wsp1759C - 1965 - Water resources in the vicinity of municipalities on the west-central Mesabi Iron Range, northeastern Minnesota","interactions":[{"subject":{"id":52315,"text":"ofr6323 - 1963 - Water resources in the vicinity of municipalities on the West-Central Mesabi Iron Range, northeastern Minnesota","indexId":"ofr6323","publicationYear":"1963","noYear":false,"title":"Water resources in the vicinity of municipalities on the West-Central Mesabi Iron Range, northeastern Minnesota"},"predicate":"SUPERSEDED_BY","object":{"id":1194,"text":"wsp1759C - 1965 - Water resources in the vicinity of municipalities on the west-central Mesabi Iron Range, northeastern Minnesota","indexId":"wsp1759C","publicationYear":"1965","noYear":false,"chapter":"C","title":"Water resources in the vicinity of municipalities on the west-central Mesabi Iron Range, northeastern Minnesota"},"id":1}],"lastModifiedDate":"2019-12-30T10:07:58","indexId":"wsp1759C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1759","chapter":"C","title":"Water resources in the vicinity of municipalities on the west-central Mesabi Iron Range, northeastern Minnesota","docAbstract":"<p>Additional supplies of water are available near the municipalities or the west-central Mesabi Iron Range. The largest sources are the ground-water aquifers in the Biwabik Iron-Formation and the stratified glacial drift. Areas of stratified drift that probably have good water potential have been outlined. Surface-water supplies are negligible in the eastern part of this area but increase toward the west. Flow records from one gaging station, results of discharge measurements at two miscellaneous sites, and data from many wells and test holes are presented.</p>\n<p>Most of the ground water is hard and has a high concentration of iron and manganese. The surface water generally has a high concentration of. iron and is colored. Analyses of water from many sources are .shown.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1759C","collaboration":"Prepared in cooperation with the Minnesota Department of Iron Range Resources and Rehabilitation","usgsCitation":"Cotter, R.D., Young, H.L., Petri, L.R., and Prior, C.H., 1965, Water resources in the vicinity of municipalities on the west-central Mesabi Iron Range, northeastern Minnesota: U.S. Geological Survey Water Supply Paper 1759, Report: iv, 21 p.; 1 Plate: 24.50 x 28.50 inches, https://doi.org/10.3133/wsp1759C.","productDescription":"Report: iv, 21 p.; 1 Plate: 24.50 x 28.50 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":137953,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1759c/report-thumb.jpg"},{"id":26062,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1759c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26063,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1759c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -93.27667236328125,\n              47.338822694822\n            ],\n            [\n              -93.19839477539062,\n              47.31741394628156\n            ],\n            [\n              -93.043212890625,\n              47.31741394628156\n            ],\n            [\n              -92.86056518554688,\n              47.40764414848437\n            ],\n            [\n              -92.779541015625,\n              47.48287279099342\n            ],\n            [\n              -92.82073974609375,\n              47.51349065484327\n            ],\n            [\n              -92.88803100585938,\n              47.52832925298343\n            ],\n            [\n              -92.9608154296875,\n              47.53852835471765\n            ],\n            [\n              -93.043212890625,\n              47.511635534978225\n            ],\n            [\n              -93.1585693359375,\n              47.447593738482304\n            ],\n            [\n              -93.2464599609375,\n              47.37975438400816\n            ],\n            [\n              -93.27667236328125,\n              47.338822694822\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db648595","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":143338,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Young, H. L.","contributorId":23922,"corporation":false,"usgs":true,"family":"Young","given":"H.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":143335,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Petri, L. R.","contributorId":48944,"corporation":false,"usgs":true,"family":"Petri","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":143336,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Prior, C. 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,{"id":2626,"text":"wsp1810 - 1965 - Summary of floods in the United States during 1961","interactions":[],"lastModifiedDate":"2017-09-06T16:28:04","indexId":"wsp1810","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1810","title":"Summary of floods in the United States during 1961","docAbstract":"<p>This report describes the most outstanding floods in the United States during 1961. The most damaging floods during the year were those caused by snowmelt in March and April in the upper Mississippi River basin and those accompanying Hurricane Carla in September.</p><p>Hurricane Carla traveled northward along the east edge of Texas and then northeastward through southeastern Oklahoma, northwestern Arkansas, southeastern Missouri, and central Illinois. Heavy rains and floods occurred east of the hurricane's path in Texas and west of its path for the remainder of its journey.</p><p>Mississippi, Alabama, and Georgia had moderate to severe floods in February and March from a series of large-area rainstorms. Many maximum peak discharges occurred, and streams remained at high stages for periods longer than any known before. Property damage was high and four lives were lost.</p><p>Extensive flooding took place in May from southeastern Kansas and northeastern Oklahoma through northern Arkansas, southern Missouri, northern Kentucky, and the southern parts of Illinois, Indiana, and Ohio. Maximum discharges occurred at many sites throughout the area.</p><p>Heavy flooding was experienced on Kootenai River at Bonners Ferry, Idaho, in May and June. These floods were noteworthy for their duration.</p><p>The most tragic flood of the year was in July in Charleston, W. Va. A small area cloudburst flood caused 22 deaths and damage of more than \\$1 million.</p><p>Severe flooding occurred in December in the Tombigbee River, Pearl River, and Pascagoula River basins in Mississippi, Louisiana, and Alabama. Much damage resulted, and from two to three thousand persons were evacuated from large flooded areas.</p><p>In addition to the floods mentioned above, 19 others of lesser magnitude are considered important enough to be included in this annual summary.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1810","collaboration":"Prepared in cooperation with Federal, State, and local agencies","usgsCitation":"Rostvedt, J., 1965, Summary of floods in the United States during 1961: U.S. Geological Survey Water Supply Paper 1810, vi, 123 p., https://doi.org/10.3133/wsp1810.","productDescription":"vi, 123 p.","numberOfPages":"128","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":28943,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1810/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138160,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1810/report-thumb.jpg"}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699281","contributors":{"authors":[{"text":"Rostvedt, J.O.","contributorId":24757,"corporation":false,"usgs":true,"family":"Rostvedt","given":"J.O.","email":"","affiliations":[],"preferred":false,"id":145524,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":183,"text":"wsp1642 - 1965 - Quality of surface waters of the United States, 1959, Parts 3 & 4, Ohio River Basin and St. Lawrence River Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:10","indexId":"wsp1642","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1642","title":"Quality of surface waters of the United States, 1959, Parts 3 & 4, Ohio River Basin and St. Lawrence River Basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1642","usgsCitation":"Love, S.K., 1965, Quality of surface waters of the United States, 1959, Parts 3 & 4, Ohio River Basin and St. Lawrence River Basin: U.S. Geological Survey Water Supply Paper 1642, x, 303 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1642.","productDescription":"x, 303 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":136327,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1642/report-thumb.jpg"},{"id":24794,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1642/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651cb1","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":142054,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1812,"text":"wsp1763 - 1965 - Water resources of the Pascagoula area, Mississippi","interactions":[{"subject":{"id":56147,"text":"ofr5950 - 1959 - Water resources of the Pascagoula area, Mississippi--Progress report","indexId":"ofr5950","publicationYear":"1959","noYear":false,"title":"Water resources of the Pascagoula area, Mississippi--Progress report"},"predicate":"SUPERSEDED_BY","object":{"id":1812,"text":"wsp1763 - 1965 - Water resources of the Pascagoula area, Mississippi","indexId":"wsp1763","publicationYear":"1965","noYear":false,"title":"Water resources of the Pascagoula area, Mississippi"},"id":1}],"lastModifiedDate":"2022-03-22T18:52:56.479653","indexId":"wsp1763","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1763","title":"Water resources of the Pascagoula area, Mississippi","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1763","usgsCitation":"Harvey, E.J., Golden, H.G., and Jeffery, H.O., 1965, Water resources of the Pascagoula area, Mississippi: U.S. Geological Survey Water Supply Paper 1763, Report: vii, 135 p.; 16 Plates: 32.00 × 56.00 inches or smaller, https://doi.org/10.3133/wsp1763.","productDescription":"Report: vii, 135 p.; 16 Plates: 32.00 × 56.00 inches or smaller","costCenters":[],"links":[{"id":27003,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1763/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27002,"rank":415,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1763/plate-16.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26991,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1763/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26990,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1763/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26989,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1763/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26988,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1763/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26987,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1763/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137174,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1763/report-thumb.jpg"},{"id":26996,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1763/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27000,"rank":413,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1763/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26999,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1763/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26997,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1763/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26995,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1763/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26994,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1763/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":397413,"rank":19,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24940.htm"},{"id":26998,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1763/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27001,"rank":414,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1763/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26993,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1763/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26992,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1763/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"Mississippi","otherGeospatial":"Pascagoula area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.393,\n              30.317\n            ],\n            [\n              -88.885,\n              30.317\n            ],\n            [\n              -88.885,\n              31\n            ],\n            [\n              -88.393,\n              31\n            ],\n            [\n              -88.393,\n              30.317\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602ba5","contributors":{"authors":[{"text":"Harvey, Edward Joseph","contributorId":32131,"corporation":false,"usgs":true,"family":"Harvey","given":"Edward","email":"","middleInitial":"Joseph","affiliations":[],"preferred":false,"id":144195,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Golden, Harold G.","contributorId":103244,"corporation":false,"usgs":true,"family":"Golden","given":"Harold","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":144197,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jeffery, H. O.","contributorId":38132,"corporation":false,"usgs":true,"family":"Jeffery","given":"H.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":144196,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1234,"text":"wsp1499J - 1965 - Water resources of the Waterbury-Bristol area, Connecticut","interactions":[],"lastModifiedDate":"2022-12-19T21:28:50.027076","indexId":"wsp1499J","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"J","title":"Water resources of the Waterbury-Bristol area, Connecticut","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1499J","usgsCitation":"Cushman, R.V., Pauszek, F.H., Randall, A., and Thomas, M.P., 1965, Water resources of the Waterbury-Bristol area, Connecticut: U.S. Geological Survey Water Supply Paper 1499, Report: v, 86 p.; 1 Plate: 24.00 × 39.44 inches, https://doi.org/10.3133/wsp1499J.","productDescription":"Report: v, 86 p.; 1 Plate: 24.00 × 39.44 inches","costCenters":[],"links":[{"id":410737,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24446.htm","linkFileType":{"id":5,"text":"html"}},{"id":26162,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1499j/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26161,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1499j/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138072,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1499j/report-thumb.jpg"}],"country":"United States","state":"Connecticut","city":"Bristol, Waterbury","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -72.881,\n              41.722\n            ],\n            [\n              -73.095,\n              41.722\n            ],\n            [\n              -73.095,\n              41.514\n            ],\n            [\n              -72.881,\n              41.514\n            ],\n            [\n              -72.881,\n              41.722\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f02d9","contributors":{"authors":[{"text":"Cushman, Robert Vittum","contributorId":96661,"corporation":false,"usgs":true,"family":"Cushman","given":"Robert","email":"","middleInitial":"Vittum","affiliations":[],"preferred":false,"id":143418,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pauszek, F. H.","contributorId":61399,"corporation":false,"usgs":true,"family":"Pauszek","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":143415,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Randall, A. D.","contributorId":81077,"corporation":false,"usgs":true,"family":"Randall","given":"A. D.","affiliations":[],"preferred":false,"id":143417,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Thomas, M. P.","contributorId":62574,"corporation":false,"usgs":true,"family":"Thomas","given":"M.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":143416,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":1810,"text":"wsp1697 - 1965 - Geology and ground water of the Tualatin Valley, Oregon","interactions":[{"subject":{"id":14012,"text":"ofr5559 - 1956 - Preliminary report on the ground-water resources of the Tualatin Valley, Oregon","indexId":"ofr5559","publicationYear":"1956","noYear":false,"title":"Preliminary report on the ground-water resources of the Tualatin Valley, Oregon"},"predicate":"SUPERSEDED_BY","object":{"id":1810,"text":"wsp1697 - 1965 - Geology and ground water of the Tualatin Valley, Oregon","indexId":"wsp1697","publicationYear":"1965","noYear":false,"title":"Geology and ground water of the Tualatin Valley, Oregon"},"id":1}],"lastModifiedDate":"2017-02-03T13:40:41","indexId":"wsp1697","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1697","title":"Geology and ground water of the Tualatin Valley, Oregon","docAbstract":"The Tualatin Valley proper consists of broad valley plains, ranging in altitude from 100 to 300 feet, and the lower mountain slopes of the drainage basin of the Tualatin River, a tributary of the Willamette River in northwestern Oregon. The valley is almost entirely farmed. Its population is increasing rapidly, partly because of the expansion of metropolitan Portland. \r\n\r\nStructurally, the bedrock of the basin is a saucer-shaped syncline almost bisected lengthwise by a ridge. The bedrock basin has been partly filled by alluvium, which underlies the valley plains. \r\n\r\nGround water occurs in the Columbia River basalt, a lava unit that forms the top several hundred feet of the bedrock, and also in the zones of fine sand in the upper part of the alluvial fill. It occurs under unconfined, confined, and perched conditions. Graphs of the observed water levels in wells show that the ground water is replenished each year by precipitation. The graphs show also that the amount and time of recharge vary in different aquifers and for different modes of ground-water occurrence. The shallower alluvial aquifers are refilled each year to a level where further infiltration recharge is retarded and water drains away as surface runoff. No occurrences of undue depletion of the ground water by pumping are known. The facts indicate that there is a great quantity of additional water available for future development. The ground water is developed for use by some spring works and by thousands of wells, most of which are of small yield. Improvements are now being made in the design of the wells in basalt and in the use of sand or gravel envelopes for wells penetrating the fine-sand aquifers. \r\n\r\nThe ground water in the basalt and the valley fill is in general of good quality, only slightly or moderately hard and of low salinity. Saline and mineralized water is present in the rocks of Tertiary age below the Columbia River basalt. Under certain structural and stratigraphic conditions this water of poor quality contaminates the fresh-water aquifers. \r\n\r\nDetailed hydrologic and geologic conditions are presented in 5 tables, 7 pictures, and 17 graphic figures and plates.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1697","usgsCitation":"Hart, D.H., and Newcomb, R.C., 1965, Geology and ground water of the Tualatin Valley, Oregon: U.S. Geological Survey Water Supply Paper 1697, v, 172 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1697.","productDescription":"v, 172 p. :ill., maps ;24 cm.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":26969,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1697/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26970,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1697/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26971,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1697/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26972,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1697/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137172,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1697/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db68618e","contributors":{"authors":[{"text":"Hart, D. H.","contributorId":16811,"corporation":false,"usgs":true,"family":"Hart","given":"D.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":144192,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Newcomb, R. C.","contributorId":77907,"corporation":false,"usgs":true,"family":"Newcomb","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":144193,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2639,"text":"wsp1784 - 1965 - Quality of surface waters in the lower Columbia River Basin","interactions":[],"lastModifiedDate":"2017-02-03T13:41:22","indexId":"wsp1784","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1784","title":"Quality of surface waters in the lower Columbia River Basin","docAbstract":"This report, made during 1959-60, provides reconnaissance data on the quality of waters in the lower Columbia River basin ; information on present and future water problems in the basin; and data that can be employed both in water-use studies and in planning future industrial, municipal, and agricultural expansion within this area. \r\n\r\nThe lower Columbia River basin consists of approximately 46,000 square miles downstream from the confluence of the Snake and Columbia Rivers The region can be divided into three geographic areas. The first is the heavily forested, sparsely populated mountain regions in which quality of water in general is related to geologic and climatological factors. The second is a semiarid plateau east of the Cascade Mountains; there differences in geology and precipitation, together with more intensive use of available water for irrigation, bring about marked differences in water quality. The third is the Willamette-Puget trough area in which are concentrated most of the industry and population and in which water quality is influenced by sewage and industrial waste disposal. \r\n\r\nThe majority of the streams in the lower Columbia River basin are calcium magnesium bicarbonate waters. In general, the rivers rising in the. Coast Range and on the west slope of the Cascade Range contain less than 100 parts per million of dissolved solids, and hardness of the water is less than 50 parts per million. Headwater reaches of the streams on the east slope of the Cascade Range are similar to those on the west slope; but, downstream, irrigation return flows cause the dissolved-solids content and hardness to increase. Most of the waters, however, remain calcium magnesium bicarbonate in type. \r\n\r\nThe highest observed dissolved-solids concentrations and also some changes in chemical composition occur in the streams draining the more arid parts of the area. In these parts, irrigation is chiefly responsible for increasing the dissolved-solids concentration and altering the chemical composition of the streams. The maximum dissolved-solids concentration and hardness of water observed in major irrigation areas were 507 and 262 parts per million, respectively, for the. Walla Walla River near Touchet, Wash. \r\n\r\nIn terms of the U.S. Salinity Laboratory Staff classification (1954, p. 80), water in most streams in the basin has low salinity and sodium hazards and is suitable for irrigation. A salt-balance problem does exist in the Hermiston-Stanfield, Oreg., area of the Umatilla River basin, and because of poor drainage, improper irrigation practices could cause salt-balance problems in the Willamette River Valley, Oreg., in which irrigation is rapidly increasing.\r\n\r\nPollution by sewage disposal has reached undesirable levels in the Walla Walla River, in the Willamette River from Eugene to Portland, Oreg., and in the Columbia River from Portland to Puget Island. In the lower reaches of the Willamette River, the pollution load from sewage and industrial-waste disposal at times depletes the dissolved oxygen in the water to concentrations below what is considered necessary for aquatic life. \r\n\r\nWater in most of the tributaries to the lower Columbia River is of excellent quality and after some treatment could be used for industrial and municipal supplies. The principal treatment required would be disinfection and turbidity removal.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1784","usgsCitation":"Santos, J.F., 1965, Quality of surface waters in the lower Columbia River Basin: U.S. Geological Survey Water Supply Paper 1784, iv, 78 p. :illus., maps. ;24 cm., https://doi.org/10.3133/wsp1784.","productDescription":"iv, 78 p. :illus., maps. ;24 cm.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":28958,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1784/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138744,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1784/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651877","contributors":{"authors":[{"text":"Santos, John F.","contributorId":21530,"corporation":false,"usgs":true,"family":"Santos","given":"John","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":145543,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1193,"text":"wsp1759F - 1965 - Water resources in the vicinity of municipalities on the eastern Mesabi Iron Range and the Vermilion Iron Range, northeastern Minnesota","interactions":[{"subject":{"id":52314,"text":"ofr6322 - 1963 - Water resources in the vicinity of municipalities on the Eastern Mesabi Iron Range and the Vermilion Iron Range, northeastern Minnesota","indexId":"ofr6322","publicationYear":"1963","noYear":false,"title":"Water resources in the vicinity of municipalities on the Eastern Mesabi Iron Range and the Vermilion Iron Range, northeastern Minnesota"},"predicate":"SUPERSEDED_BY","object":{"id":1193,"text":"wsp1759F - 1965 - Water resources in the vicinity of municipalities on the eastern Mesabi Iron Range and the Vermilion Iron Range, northeastern Minnesota","indexId":"wsp1759F","publicationYear":"1965","noYear":false,"chapter":"F","title":"Water resources in the vicinity of municipalities on the eastern Mesabi Iron Range and the Vermilion Iron Range, northeastern Minnesota"},"id":1}],"lastModifiedDate":"2021-11-02T21:27:50.468028","indexId":"wsp1759F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1759","chapter":"F","title":"Water resources in the vicinity of municipalities on the eastern Mesabi Iron Range and the Vermilion Iron Range, northeastern Minnesota","docAbstract":"<p>Additional supplies of water are available near the municipalities on the eastern Mesabi Iron Range and the Vermilion Iron Range. On the eastern Mesabi Range the potential for additional development of both ground-water and surface-water supplies are good, and on the Vermilion Range the best potential for development is from surface-water resources.</p>\n<p>The most productive aquifers in the area of this report are the Biwabik Iron-Formation and the stratified glacial drift; Bast of Colby Lake the Biwabik Iron-Formation is not an important aquifer, and it is entirely absent on the Vermilion Range. Also, on the Vermilion Range the glacial drift is generally too thin to yield the quantities of water found on the Mesabi Range.</p>\n<p>Surface-water supplies in the area of this report are good. An extensive network of river systems and many lakes form a large untapped potential supply. Records of flow from eight gaging stations are presented as are data from many wells and test holes.</p>\n<p>Ground water commonly has a high concentration of iron and manganese and is hard. Surface water generally has a high concentration of iron and is colored. Analyses of water from many sources are included.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Water resources of the Mesabi and Vermilion Iron Ranges","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1759F","usgsCitation":"Cotter, R.D., Young, H.L., Petri, L.R., and Prior, C.H., 1965, Water resources in the vicinity of municipalities on the eastern Mesabi Iron Range and the Vermilion Iron Range, northeastern Minnesota: U.S. Geological Survey Water Supply Paper 1759, Report: iv, 27 p.; 1 Plate: 31.18 x 23.60 inches, https://doi.org/10.3133/wsp1759F.","productDescription":"Report: iv, 27 p.; 1 Plate: 31.18 x 23.60 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":137952,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1759f/report-thumb.jpg"},{"id":26061,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1759f/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":278838,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1759f/plate-1.pdf"},{"id":391292,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24938.htm"}],"country":"United States","state":"Minnesota","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -93.62548828125,\n              47.09630525444073\n            ],\n            [\n              -91.99676513671875,\n              47.09630525444073\n            ],\n            [\n              -91.99676513671875,\n              47.945786463687185\n            ],\n            [\n              -93.62548828125,\n              47.945786463687185\n            ],\n            [\n              -93.62548828125,\n              47.09630525444073\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f08d4","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":143334,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Young, H. L.","contributorId":23922,"corporation":false,"usgs":true,"family":"Young","given":"H.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":143331,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Petri, L. R.","contributorId":48944,"corporation":false,"usgs":true,"family":"Petri","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":143332,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Prior, C. H.","contributorId":57827,"corporation":false,"usgs":true,"family":"Prior","given":"C.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":143333,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":1231,"text":"wsp1809D - 1965 - An evaluation of aquifer and well characteristics of municipal well fields in Los Alamos and Guaje Canyons, near Los Alamos, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1809D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1809","chapter":"D","title":"An evaluation of aquifer and well characteristics of municipal well fields in Los Alamos and Guaje Canyons, near Los Alamos, New Mexico","docAbstract":"The Jenkins-Whitesburg area includes approximately 250 square miles In Letcher and Pike Counties in the southeastern part of the Eastern Coal Field. In this area ground water is the principal source of water for nearly all rural families, most public supplies, several coal mines and coal processing plants, and one bottling plant. \r\n\r\nThe major aquifers in the Jenkins-Whitesburg area are the Breathitt and Lee Formations of Pennsylvanian age. Other aquifers range in age from Devonian to Quaternary but are not important in this area because they occur at great depth or yield little or no water. The Breathitt Formation occurs throughout the area except along the crest and slopes of Pine Mountain and where it is covered by unconsolidated material of Quaternary age. The Breathitt Formation consists of shale, sandstone, and lesser amounts of coal and associated underclay. The yield of wells penetrating the Breathitt Formation ranges from less than 1 to 330 gallons per minute. Well yield is controlled by the type and depth of well, character of the aquifer, and topography of the well site. Generally, deep wells drilled in valleys of perennial streams offer the best potential for high yields. Although enough water for a minimum domestic supply (more than 100 gallons per day) may be obtained from shale, all high-yielding wells probably obtain water from vertical joints and from bedding planes which are best developed in sandstone. About 13 percent of the wells inventoried in the Breathitt Formation failed to supply enough water for a minimum domestic supply. Most of these are shallow dug wells or drilled wells on hillsides or hilltops. Abandoned coal dunes are utilized as large infiltration galleries and furnish part of the water for several public supplies. \r\n\r\nThe chemical quality of water from the Breathitt Formation varies considerably from place to place, but the water generally is acceptable for most domestic and industrial uses. Most water is a calcium magnesium bicarbonate or sodium bicarbonate type, and nearly all sampled water contained enough iron to stain cooking and laundry utensils. The water ranged from soft to very hard, and only one well in the Breathitt Formation produced salty water. The absence of salty water may be due to abundant fractures which are associated with the Pine Mountain fault and which have allowed fresh water to enter the formation. The Lee Formation underlies the Cumberland Mountain section and is exposed along the crest and southeast slope of Pine Mountain. The Lee Formation consists of massive sandstone and conglomerate with thin beds of shale and a few thin coal seams.\r\n\r\nAlthough the Lee Formation is tapped by only a few wells in this area, it is potentially an important aquifer. Wells penetrating the Lee Formation in the Cumberland Mountain section would probably yield water under artesian pressure.\r\n\r\nUnlike most water from the Lee Formation in other part.3 of eastern Kentucky, all water from the Lee Formation in the Jenkins-Whitesburg area is fresh. All water from the Lee Formation contained more than 0.3 parts per million of iron and ranged from soft to moderately hard.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1809D","usgsCitation":"Cushman, R., 1965, An evaluation of aquifer and well characteristics of municipal well fields in Los Alamos and Guaje Canyons, near Los Alamos, New Mexico: U.S. Geological Survey Water Supply Paper 1809, v, 50 p. :ill., maps ;24 cm. + plates folded in pocket., https://doi.org/10.3133/wsp1809D.","productDescription":"v, 50 p. :ill., maps ;24 cm. + plates folded in pocket.","costCenters":[],"links":[{"id":138069,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1809d/report-thumb.jpg"},{"id":26149,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26150,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809d/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26151,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809d/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26152,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809d/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26153,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1809d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db684a57","contributors":{"authors":[{"text":"Cushman, Robert L.","contributorId":22751,"corporation":false,"usgs":true,"family":"Cushman","given":"Robert L.","affiliations":[],"preferred":false,"id":143410,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1839,"text":"wsp1667D - 1965 - Reduction and complexing of manganese gallic acids","interactions":[],"lastModifiedDate":"2012-02-02T00:05:22","indexId":"wsp1667D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1667","chapter":"D","title":"Reduction and complexing of manganese gallic acids","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1667D","usgsCitation":"Hem, J.D., 1965, Reduction and complexing of manganese gallic acids: U.S. Geological Survey Water Supply Paper 1667, iii, 28 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1667D.","productDescription":"iii, 28 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":138508,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1667d/report-thumb.jpg"},{"id":27044,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1667d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db635256","contributors":{"authors":[{"text":"Hem, John David","contributorId":42577,"corporation":false,"usgs":true,"family":"Hem","given":"John","email":"","middleInitial":"David","affiliations":[],"preferred":false,"id":144236,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1328,"text":"wsp1809S - 1965 - Suitability of irrigation water and changes in ground-water quality in the Lompoc subarea of the Santa Ynez River Basin, Santa Barbara County, California","interactions":[],"lastModifiedDate":"2015-02-19T08:59:47","indexId":"wsp1809S","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1809","chapter":"S","title":"Suitability of irrigation water and changes in ground-water quality in the Lompoc subarea of the Santa Ynez River Basin, Santa Barbara County, California","docAbstract":"<p>Analyses of water samples collected since 1934 from some of the irrigation wells in the Lompoc subarea of the Santa Ynes River valley have shown a gradual deterioration in the chemical quality of the water.</p>\n<p>Most of the ground water pumped in the subarea has a dissolved-solids contents ranging from about 700 to about 2,000 parts per million, of which sulfate and chloride are the predominant constituents. &nbsp;Suitability of the water for irrigation is variable and is dependent principally on \"potential salinity\" of the water, soil permeability, and type of crop.</p>\n<p>Changes in water quality are not consistent throughout the subarea. &nbsp;No doubt the chloride concentration increases as a result of both the recycling irrigation water and inflow of high-chloride low-sulfate connate water from the consolidated Tertiary rocks. &nbsp;The influence of recycled irrigation water is indicated by increase concentrations of chloride and sulfate in a ratio of 1:2. &nbsp;Inflow of high-chloride low-sulfate connate water is indicated by increased chloride concentration correlated with little or no change in sulfate concentration. &nbsp;Peak chloride concentrations in three local areas are probably the result of the inflow of connate water. &nbsp;Furthermore, ground-water gradients in each of the local areas are favorable for inflow from the consolidated rocks.</p>","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1809S","usgsCitation":"Evenson, R.E., 1965, Suitability of irrigation water and changes in ground-water quality in the Lompoc subarea of the Santa Ynez River Basin, Santa Barbara County, California: U.S. Geological Survey Water Supply Paper 1809, iii, 20 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1809S.","productDescription":"iii, 20 p. :ill., maps ;24 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":26380,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809s/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26381,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809s/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26382,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809s/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26383,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1809s/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137895,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1809s/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db6998a2","contributors":{"authors":[{"text":"Evenson, R. E.","contributorId":19933,"corporation":false,"usgs":true,"family":"Evenson","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":143570,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1107,"text":"wsp1762 - 1965 - Water in Georgia","interactions":[],"lastModifiedDate":"2017-02-01T09:19:08","indexId":"wsp1762","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1762","title":"Water in Georgia","language":"ENGLISH","publisher":"U. S. Dept. of the Interior, Geological Survey; for sale by the Superintendent of Documents, U.S. Govt. Print. Off.,","doi":"10.3133/wsp1762","usgsCitation":"Callahan, J.T., Newcomb, L.E., and Guerin, J.W., 1965, Water in Georgia: U.S. Geological Survey Water Supply Paper 1762, v. 88 p. :illus. (part col.) col. maps. ;24 cm., https://doi.org/10.3133/wsp1762.","productDescription":"v. 88 p. :illus. 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,{"id":2446,"text":"wsp1682 - 1965 - Magnitude and frequency of floods in the United States, part 8. Western Gulf of Mexico basins","interactions":[],"lastModifiedDate":"2022-02-04T19:52:53.142205","indexId":"wsp1682","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1682","title":"Magnitude and frequency of floods in the United States, part 8. Western Gulf of Mexico basins","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1682","usgsCitation":"Patterson, J.L., 1965, Magnitude and frequency of floods in the United States, part 8. Western Gulf of Mexico basins: U.S. Geological Survey Water Supply Paper 1682, Report: xvi, 506 p.; 1 Plate: 36.00 × 40.00 inches, https://doi.org/10.3133/wsp1682.","productDescription":"Report: xvi, 506 p.; 1 Plate: 36.00 × 40.00 inches","costCenters":[],"links":[{"id":395473,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24891.htm"},{"id":28519,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1682/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28518,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1682/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138126,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1682/report-thumb.jpg"}],"country":"United States","otherGeospatial":"western Gulf of Mexico basins","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -108.5,\n              26\n            ],\n            [\n              -92.5,\n              26\n            ],\n            [\n              -92.5,\n              38.333\n            ],\n            [\n              -108.5,\n              38.333\n            ],\n            [\n              -108.5,\n              26\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db635561","contributors":{"authors":[{"text":"Patterson, James L.","contributorId":17593,"corporation":false,"usgs":true,"family":"Patterson","given":"James","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":145218,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1129,"text":"wsp1498I - 1965 - Total bed-material discharge in alluvial channels","interactions":[],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1498I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1498","chapter":"I","title":"Total bed-material discharge in alluvial channels","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Studies in flow in alluvial channels","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. Geological Survey ;","doi":"10.3133/wsp1498I","usgsCitation":"Chang, F.M., Simons, D., and Richardson, E., 1965, Total bed-material discharge in alluvial channels: U.S. Geological Survey Water Supply Paper 1498, v, 23 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1498I.","productDescription":"v, 23 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":137928,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1498i/report-thumb.jpg"},{"id":25907,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1498i/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629af0","contributors":{"authors":[{"text":"Chang, Fred M.","contributorId":87913,"corporation":false,"usgs":true,"family":"Chang","given":"Fred","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":143224,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simons, D.B.","contributorId":50501,"corporation":false,"usgs":true,"family":"Simons","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":143223,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Richardson, E.V.","contributorId":105697,"corporation":false,"usgs":true,"family":"Richardson","given":"E.V.","email":"","affiliations":[],"preferred":false,"id":143225,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1950,"text":"wsp1809H - 1965 - Reconnaissance of the chemical quality of surface waters of the Sabine River Basin, Texas and Louisiana","interactions":[],"lastModifiedDate":"2016-08-22T11:26:52","indexId":"wsp1809H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1809","chapter":"H","title":"Reconnaissance of the chemical quality of surface waters of the Sabine River Basin, Texas and Louisiana","docAbstract":"<p>The Sabine River basin has an abundant supply .of surface water of excellent quality. The basin area of 9,700 square miles receives an average of about 48 inches of rainfall per year, of which about 13 inches flows to the Gulf of Mexico.</p>\n<p>Variations in the chemical quality of the surface waters in the Sabine River basin are caused principally by areal differences in geology and runoff; but industrial influences, particularly the disposal of oil-field brines, affect the quality in limited areas. Water having the least dissolved solids is found in the lower part of the basin, where rainfall is greatest. Water having higher values of hardness are found in the area of Cretaceous limestone, chalk, and marl in the northwestern part of the basin. Chloride concentrations are generally low except where streams are polluted by oil-field brines and localized natural saline inflow.</p>\n<p>Existing reservoirs in the basin contain water of excellent quality, and water to be stored in proposed reservoirs should be excellent.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1809H","usgsCitation":"Hughes, L.S., and Leifeste, D., 1965, Reconnaissance of the chemical quality of surface waters of the Sabine River Basin, Texas and Louisiana: U.S. Geological Survey Water Supply Paper 1809, Report: iv, 71 p.; Plate: 28.00 x 33.00 inches, https://doi.org/10.3133/wsp1809H.","productDescription":"Report: iv, 71 p.; Plate: 28.00 x 33.00 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":27286,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1809h/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138532,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1809h/report-thumb.jpg"},{"id":27285,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809h/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a68e4b07f02db63af98","contributors":{"authors":[{"text":"Hughes, Leon S.","contributorId":65056,"corporation":false,"usgs":true,"family":"Hughes","given":"Leon","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":144422,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leifeste, D.K.","contributorId":81079,"corporation":false,"usgs":true,"family":"Leifeste","given":"D.K.","affiliations":[],"preferred":false,"id":144423,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2475,"text":"wsp1809N - 1965 - Effects of waste water from A.E.C. plant on the hydrology of Glowegee Creek at West Milton, New York, 1958-61","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"wsp1809N","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1809","chapter":"N","title":"Effects of waste water from A.E.C. plant on the hydrology of Glowegee Creek at West Milton, New York, 1958-61","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1809N","usgsCitation":"Pauszek, F.H., and Ruggles, F., 1965, Effects of waste water from A.E.C. plant on the hydrology of Glowegee Creek at West Milton, New York, 1958-61: U.S. Geological Survey Water Supply Paper 1809, iv, 29 p. :ill., map ;24 cm., https://doi.org/10.3133/wsp1809N.","productDescription":"iv, 29 p. :ill., map ;24 cm.","costCenters":[],"links":[{"id":138748,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1809n/report-thumb.jpg"},{"id":28551,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1809n/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60fc24","contributors":{"authors":[{"text":"Pauszek, F. H.","contributorId":61399,"corporation":false,"usgs":true,"family":"Pauszek","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":145254,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ruggles, Frederick H.","contributorId":96665,"corporation":false,"usgs":true,"family":"Ruggles","given":"Frederick H.","affiliations":[],"preferred":false,"id":145255,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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