{"pageNumber":"2524","pageRowStart":"63075","pageSize":"25","recordCount":68789,"records":[{"id":68582,"text":"ha243 - 1966 - Effect of drought on water resources in the Northeast","interactions":[],"lastModifiedDate":"2012-02-02T00:13:21","indexId":"ha243","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"243","title":"Effect of drought on water resources in the Northeast","language":"ENGLISH","doi":"10.3133/ha243","usgsCitation":"Barksdale, H., O’Bryan, D., and Schneider, W.J., 1966, Effect of drought on water resources in the Northeast: U.S. Geological Survey Hydrologic Atlas 243, 10 col. maps ;14 x 10 cm. on sheet 67 x 81 cm. folded to 30 x 24 cm., https://doi.org/10.3133/ha243.","productDescription":"10 col. maps ;14 x 10 cm. on sheet 67 x 81 cm. folded to 30 x 24 cm.","costCenters":[],"links":[{"id":190099,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90220,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/243/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db6257c5","contributors":{"authors":[{"text":"Barksdale, H.C.","contributorId":65912,"corporation":false,"usgs":true,"family":"Barksdale","given":"H.C.","email":"","affiliations":[],"preferred":false,"id":278514,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O’Bryan, Deric","contributorId":15179,"corporation":false,"usgs":true,"family":"O’Bryan","given":"Deric","email":"","affiliations":[],"preferred":false,"id":278512,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schneider, William J.","contributorId":47349,"corporation":false,"usgs":true,"family":"Schneider","given":"William","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":278513,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":185,"text":"wsp1645 - 1966 - Quality of surface waters of the United States, 1959, Parts 9-14, Colorado River basin to Pacific slope basins in Oregon and lower Columbia River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:10","indexId":"wsp1645","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1645","title":"Quality of surface waters of the United States, 1959, 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/wsp1645","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1966, Quality of surface waters of the United States, 1959, Parts 9-14, Colorado River basin to Pacific slope basins in Oregon and lower Columbia River basin: U.S. Geological Survey Water Supply Paper 1645, xv, 524 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1645.","productDescription":"xv, 524 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":136329,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1645/report-thumb.jpg"},{"id":24796,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1645/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651aeb","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527220,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52543,"text":"ofr6648 - 1966 - Ground-water conditions for 1965 at the Marine Corps Base, Twentynine Palms, California","interactions":[],"lastModifiedDate":"2012-02-02T00:11:45","indexId":"ofr6648","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"66-48","title":"Ground-water conditions for 1965 at the Marine Corps Base, Twentynine Palms, California","language":"ENGLISH","doi":"10.3133/ofr6648","usgsCitation":"Giessner, F., and Robson, S.G., 1966, Ground-water conditions for 1965 at the Marine Corps Base, Twentynine Palms, California: U.S. Geological Survey Open-File Report 66-48, 27 p., https://doi.org/10.3133/ofr6648.","productDescription":"27 p.","costCenters":[],"links":[{"id":173960,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d2a3","contributors":{"authors":[{"text":"Giessner, F. W.","contributorId":18404,"corporation":false,"usgs":true,"family":"Giessner","given":"F. W.","affiliations":[],"preferred":false,"id":245521,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robson, S. G.","contributorId":97102,"corporation":false,"usgs":true,"family":"Robson","given":"S.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":245522,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1300,"text":"wsp1757E - 1966 - The occurrence, chemical quality and use of ground water in the Tabulbah area, Tunisia","interactions":[],"lastModifiedDate":"2012-02-02T00:05:13","indexId":"wsp1757E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1757","chapter":"E","title":"The occurrence, chemical quality and use of ground water in the Tabulbah area, Tunisia","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1757E","usgsCitation":"Dutcher, L., and Thomas, H.E., 1966, The occurrence, chemical quality and use of ground water in the Tabulbah area, Tunisia: U.S. Geological Survey Water Supply Paper 1757, iii, 29 p. :ill., map ;24 cm., https://doi.org/10.3133/wsp1757E.","productDescription":"iii, 29 p. :ill., map ;24 cm.","costCenters":[],"links":[{"id":137474,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1757e/report-thumb.jpg"},{"id":26313,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1757e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26314,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1757e/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26315,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1757e/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26316,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1757e/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26317,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1757e/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26318,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1757e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64939a","contributors":{"authors":[{"text":"Dutcher, L.C.","contributorId":42191,"corporation":false,"usgs":true,"family":"Dutcher","given":"L.C.","email":"","affiliations":[],"preferred":false,"id":143526,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thomas, H. E.","contributorId":12829,"corporation":false,"usgs":true,"family":"Thomas","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":143525,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2400,"text":"wsp1808 - 1966 - Ground-water resources of the Dayton area, Ohio","interactions":[],"lastModifiedDate":"2022-03-22T19:45:16.408536","indexId":"wsp1808","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1808","title":"Ground-water resources of the Dayton area, Ohio","docAbstract":"The principal aquifers of the Dayton area are sand and gravel layers in the 150- to 250-foot thick glacial deposits filling the river valleys (Miami River and its tributaries), which were originally cut in bedrock by preglacial streams. The upper and lower aquifers are separated by a poorly permeable till-rich zone, which confines the water in the lower aquifer; recharge to the lower aquifer is by vertical leakage through the till zone. The upper aquifer is pumped extensively only at Rohrers Island well field of Dayton, where water levels are kept high by artificial recharge. Although few cities in Ohio are as abundantly endowed with ground-water resources as Dayton, the demand is estimated to rise to quantities that cannot be supplied by the year 2000. A comprehensive plan for conservation is needed to meet future growth.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1808","usgsCitation":"Norris, S.E., and Spieker, A.M., 1966, Ground-water resources of the Dayton area, Ohio: U.S. Geological Survey Water Supply Paper 1808, Report: vii, 167 p.; 9 Plates: 40.00 × 38.75 inches or smaller, https://doi.org/10.3133/wsp1808.","productDescription":"Report: vii, 167 p.; 9 Plates: 40.00 × 38.75 inches or smaller","costCenters":[],"links":[{"id":28388,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1808/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28387,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1808/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28383,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1808/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28382,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1808/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28381,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1808/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28380,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1808/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138961,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1808/report-thumb.jpg"},{"id":28386,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1808/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28385,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1808/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28384,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1808/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28389,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1808/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":397422,"rank":12,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25000.htm"}],"scale":"24000","country":"United States","state":"Ohio","city":"Dayton","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84.292,\n              39.658\n            ],\n            [\n              -84.067,\n              39.658\n            ],\n            [\n              -84.067,\n              39.85\n            ],\n            [\n              -84.292,\n              39.85\n            ],\n            [\n              -84.292,\n              39.658\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a051","contributors":{"authors":[{"text":"Norris, Stanley Eugene","contributorId":24772,"corporation":false,"usgs":true,"family":"Norris","given":"Stanley","email":"","middleInitial":"Eugene","affiliations":[],"preferred":false,"id":145138,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spieker, Andrew Maute","contributorId":78716,"corporation":false,"usgs":true,"family":"Spieker","given":"Andrew","email":"","middleInitial":"Maute","affiliations":[],"preferred":false,"id":145139,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2413,"text":"wsp1814 - 1966 - Geology and water resources of Winnebago County, Wisconsin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:30","indexId":"wsp1814","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1814","title":"Geology and water resources of Winnebago County, Wisconsin","docAbstract":"Sources or water in Winnebago County include surface water from the Fox and Wolf Rivers and their associated lakes, and ground water from sandstone, dolomite, and sand and gravel deposits. Surface water is hard and generally requires treatment, but is then suitable for municipal and most industrial uses. Pollution is only a local problem in the lakes and rivers, but algae are present in most of the lakes. Ground water in Winnebago County is hard to very hard, and dissolved iron is a problem in a large area of the county. A saline-water zone borders the eastern edge of the county and underlies the areas of concentrated pumpage at Neenah-Menasha and Oshkosh. \r\n\r\nA thick, southeastward-dipping sandstone aquifer, yielding as much as 1,000 gallons per minute to municipal and industrial wells, underlies Winnebago County. A dolomite aquifer in the eastern and southern part of the county yields as much as 50 gallons per minute to wells. Sand and gravel layers and lenses in preglacial bedrock channels, in northwestern Winnebago County and in the upper Fox River valley, yield as much as 50 gallons per minute to wells. Present water problems in the county include algae and local pollution in the Lake Winnebago Pool, iron in water from the sandstone aquifer, and saline ground Water in the eastern part of the county. Potential problems include rapid decline of water levels because of interference between closely spaced wells, migration of saline ground water toward areas of pumping, surface-water pollution from inadequate sewage and industrial-waste process plants, and ground-water pollution in dolomite formations. \r\n\r\nDevelopment of the water resources of the county should follow a comprehensive plan which takes into consideration all aspects of water use. Dispersal of wells, especially extending toward the west from the heavily pumped Neenah-Menasha and Oshkosh areas, is recommended to reduce water-level declines and to avoid saline water. Supplemental use of ground water is recmmended for municipal expansion of water facilities and to reduce the algae treatment problem of water from the Lake Winnebago Pool.","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/wsp1814","usgsCitation":"Olcott, P.C., 1966, Geology and water resources of Winnebago County, Wisconsin: U.S. Geological Survey Water Supply Paper 1814, 61 p. :illus., maps (4 fold., 3 col.) ;24 cm., https://doi.org/10.3133/wsp1814.","productDescription":"61 p. :illus., maps (4 fold., 3 col.) ;24 cm.","numberOfPages":"61","costCenters":[],"links":[{"id":138666,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1814/report-thumb.jpg"},{"id":28415,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1814/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28416,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1814/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28417,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1814/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28418,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1814/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":264393,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1814/plate-3.pdf","size":"882","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c2ac","contributors":{"authors":[{"text":"Olcott, Perry C.","contributorId":74362,"corporation":false,"usgs":true,"family":"Olcott","given":"Perry","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":145161,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":191,"text":"wsp1950 - 1966 - Quality of surface waters of the United States, 1963, Parts 7 and 8, lower Mississippi River basin and western Gulf of Mexico basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:10","indexId":"wsp1950","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1950","title":"Quality of surface waters of the United States, 1963, 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/wsp1950","usgsCitation":"Love, S.K., 1966, Quality of surface waters of the United States, 1963, Parts 7 and 8, lower Mississippi River basin and western Gulf of Mexico basins: U.S. Geological Survey Water Supply Paper 1950, xii, 635 p. ;23 cm., https://doi.org/10.3133/wsp1950.","productDescription":"xii, 635 p. ;23 cm.","costCenters":[],"links":[{"id":136096,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1950/report-thumb.jpg"},{"id":24802,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1950/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651a8a","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":142062,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":65693,"text":"i512 - 1966 - Geologic map of California","interactions":[],"lastModifiedDate":"2012-02-02T00:13:03","indexId":"i512","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"512","subseriesTitle":"NONE","title":"Geologic map of California","language":"ENGLISH","doi":"10.3133/i512","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1966, Geologic map of California: U.S. Geological Survey IMAP 512, 1 map :col. ;on sheet 53 x 43 cm., https://doi.org/10.3133/i512.","productDescription":"1 map :col. ;on sheet 53 x 43 cm.","costCenters":[],"links":[{"id":102076,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_508.htm","linkFileType":{"id":5,"text":"html"},"description":"508"},{"id":187153,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"2500000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a31ca","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":534078,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32717,"text":"pp448G - 1966 - Low-flow characteristics of streams in the Mississippi embayment in southern Arkansas, northern Louisiana and northeastern Texas with a section on quality of the water","interactions":[{"subject":{"id":52133,"text":"ofr60129 - 1960 - Lowest mean discharge and flow duration data by years at selected gaging stations in the Mississippi Embayment area","indexId":"ofr60129","publicationYear":"1960","noYear":false,"title":"Lowest mean discharge and flow duration data by years at selected gaging stations in the Mississippi Embayment area"},"predicate":"SUPERSEDED_BY","object":{"id":32717,"text":"pp448G - 1966 - Low-flow characteristics of streams in the Mississippi embayment in southern Arkansas, northern Louisiana and northeastern Texas with a section on quality of the water","indexId":"pp448G","publicationYear":"1966","noYear":false,"chapter":"G","title":"Low-flow characteristics of streams in the Mississippi embayment in southern Arkansas, northern Louisiana and northeastern Texas with a section on quality of the water"},"id":1}],"lastModifiedDate":"2021-09-02T19:24:37.416257","indexId":"pp448G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"448","chapter":"G","title":"Low-flow characteristics of streams in the Mississippi embayment in southern Arkansas, northern Louisiana and northeastern Texas with a section on quality of the water","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Water resources of the Mississippi embayment","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp448G","usgsCitation":"Speer, P.R., Hines, M.S., Calandro, A., and Jeffery, H., 1966, Low-flow characteristics of streams in the Mississippi embayment in southern Arkansas, northern Louisiana and northeastern Texas with a section on quality of the water: U.S. Geological Survey Professional Paper 448, Report: iii, 40 p.; 2 Plates: 43.12 × 36.00 inches and 43.54 × 36.00 inches, https://doi.org/10.3133/pp448G.","productDescription":"Report: iii, 40 p.; 2 Plates: 43.12 × 36.00 inches and 43.54 × 36.00 inches","costCenters":[],"links":[{"id":60631,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0448g/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60633,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0448g/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":388463,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4450.htm"},{"id":124231,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0448g/report-thumb.jpg"},{"id":60632,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0448g/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arkansas, Louisiana, Texas","otherGeospatial":"Mississippi embayment","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -94.7470,\n              32.0\n            ],\n            [\n              -90.0833,\n              32.0\n            ],\n            [\n              -90.0833,\n              35.2261\n            ],\n            [\n              -94.7470,\n              35.2261\n            ],\n            [\n              -94.7470,\n              32.0\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f043b","contributors":{"authors":[{"text":"Speer, P. R.","contributorId":104948,"corporation":false,"usgs":true,"family":"Speer","given":"P.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":209015,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hines, M. S.","contributorId":100444,"corporation":false,"usgs":true,"family":"Hines","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":209014,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Calandro, A. J.","contributorId":92668,"corporation":false,"usgs":true,"family":"Calandro","given":"A. J.","affiliations":[],"preferred":false,"id":209013,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jeffery, H. G.","contributorId":74353,"corporation":false,"usgs":true,"family":"Jeffery","given":"H. G.","affiliations":[],"preferred":false,"id":209012,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":13341,"text":"ofr6624 - 1966 - Geology of the Cerro Summit quadrangle, Montrose County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:07:02","indexId":"ofr6624","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"66-24","title":"Geology of the Cerro Summit quadrangle, Montrose County, Colorado","docAbstract":"The Cerro Summit quadrangle covers 58 square miles of dissected plateau on the south flank of the Gunnison uplift in southwestern Colorado. It lies east of the Uncompahgre River valley and south of the Black Canyon of the Gunnison River. Rocks dip gently in most of the quadrangle, but they are locally upturned and faulted on the margin of the Gunnison uplift and are intensely deformed in the core of the uplift. The rocks exposed are of Precambrian, late Mesozoic, and Cenozoic age. \r\n\r\nPrecambrian rocks include metasedimentary schist and gneiss, granitic pegmatite, and olivine gabbro. The oldest Mesozoic rocks exposed are continental, fresh-water, and lagoonal deposits in the Late Jurassic Entrada Sandstone, Wanakah Formation, and Morrison Formation. Channel-fill deposits that unconformably overlie the Jurassic rocks are possibly the Burro Canyon Formation of Early Cretaceous age. Upper Cretaceous rocks include marine and nearshore deposits of the Dakota \r\n\r\nSandstone, Mancos Shale, and Pictured Cliffs Sandstone, and the fresh- and brackish-water sandstone, shale, and coal of the Fruitland Formation. Rocks of Late Cretaceous age that crop out in the adjacent Cimarron Ridge area may also have been deposited in this quadrangle but are now eroded; these rocks include the nonmarine Kirtland Shale and an unnamed volcanic conglomerate and tuff breccia. Nine faunal zones in the Mancos Shale help to establish the correct correlation of units in the Upper Cretaceous. The Pictured Cliffs Sandstone, Fruitland Formation, and Kirtland Shale of the Cerro Summit area have been mapped by some geologists as the Mesaverde Formation. Fossils indicate that the rocks are younger than the type Mesaverde. The unnamed volcanic rocks represent major volcanism in nearby areas. A Late Cretaceous (Maestrichtian) age for the volcanism is indicated by palynological evidence and an isotopic age of approximately 66 million years. Middle Tertiary rocks are conglomerate and tuff breccia. Upper Tertiary or lower Quaternary rocks include gravel along Pool Gulch and older landslide debris on Waterdog Peak. Pleistocene and Recent deposits consist of the older stream gravel of Shinn Park, valley-fill deposits of Bostwick-Shinn Park, and pediment, landslide, eolian, alluvial, and colluvial deposits. P1elstocene valley-fill deposits of Bostwick-Shinn Park were deposited during the Cedar Ridge, or Kansan, to Pinedale or late Wisconsin times. The valley-fill deposits are divided into five units that are separated by strong Interglacial or Interstadial soils and that contain three volcanic ash beds. Chemical and petrographic data suggest that the middle ash bed may correlate with the Pearlette Ash Member (late Kansan) of the Sappa Formation in Nebraska. Alluvium on two pediment surfaces seems to be of Sacagawea Ridge or Illinoian age. Landslide deposits, of Pleistocene and Recent age, cover about 85 percent of the quadrangle; most of the deposits were formerly mapped as till. The name Cerro Till was abandoned because till does not occur in the type area.\r\n\r\nThe dominant tectonic structures are the high-angle Cimarron fault of a few thousand feet displacement and the broad Montrose syncline. Evidence in the Cimarron Ridge area suggests that these structures formed in Late Cretaceous (Maestrichtian) time. Much of the strata near the surface of the quadrangle has been involved in landsliding that has continued from late Tertiary to the present.","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr6624","usgsCitation":"Dickinson, R.G., 1966, Geology of the Cerro Summit quadrangle, Montrose County, Colorado: U.S. Geological Survey Open-File Report 66-24, 117 p. ill., 2 maps (1 col.) ;30 cm., https://doi.org/10.3133/ofr6624.","productDescription":"117 p. ill., 2 maps (1 col.) ;30 cm.","costCenters":[],"links":[{"id":147751,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1966/0024/report-thumb.jpg"},{"id":41765,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0024/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41766,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1966/0024/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae884","contributors":{"authors":[{"text":"Dickinson, Robert G.","contributorId":79489,"corporation":false,"usgs":true,"family":"Dickinson","given":"Robert","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":167651,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42923,"text":"ofr66151 - 1966 - Progress report on salt-water intrusion studies, Sunset and Bolsa Gaps, Orange County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:10:27","indexId":"ofr66151","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"66-151","title":"Progress report on salt-water intrusion studies, Sunset and Bolsa Gaps, Orange County, California","language":"ENGLISH","doi":"10.3133/ofr66151","usgsCitation":"Wall, J.R., Cordes, E.H., and Moreland, J.A., 1966, Progress report on salt-water intrusion studies, Sunset and Bolsa Gaps, Orange County, California: U.S. Geological Survey Open-File Report 66-151, 44 p., https://doi.org/10.3133/ofr66151.","productDescription":"44 p.","costCenters":[],"links":[{"id":173080,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65dead","contributors":{"authors":[{"text":"Wall, J. R.","contributorId":59863,"corporation":false,"usgs":true,"family":"Wall","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":227414,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cordes, E. H.","contributorId":49002,"corporation":false,"usgs":true,"family":"Cordes","given":"E.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":227413,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moreland, J. A.","contributorId":71994,"corporation":false,"usgs":true,"family":"Moreland","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":227415,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1092,"text":"wsp1831 - 1966 - Hydrology of Cornfield Wash area and effects of land-treatment practices, Sandoval County, New Mexico, 1951-60","interactions":[],"lastModifiedDate":"2024-09-24T18:14:18.610113","indexId":"wsp1831","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1831","title":"Hydrology of Cornfield Wash area and effects of land-treatment practices, Sandoval County, New Mexico, 1951-60","docAbstract":"The collection of runoff and sediment data was the primary objective of the 10-year (1951-60) study in the Cornfield Wash basin, which has an area of 21.3 square miles. However, reconnaissance investigations also were made of (1) precipitation; (2) the effects of reservoirs on runoff, erosion, and sediment yield; (3) the effects of range pitting on runoff, sediment, and vegetation yields; and (4) the effects of wire sediment barriers on sediment accumulations. \r\n\r\nPrecipitation averaged 6.07 inches for the warm season (May 1 through October 31). From 1951 to 1955 much of the precipitation came in short torrential downpours. Since 1955, precipitation usually has been of lower intensity, resulting in a low runoff-precipitation ratio. \r\n\r\nThe total composite inflow to the 19 reservoirs in the Cornfield Wash basin--12 constructed in 1950 and 7 constructed from 1953 to 1956--was 5,720 acre-feet. The reservoirs permanently retained 1,370 acre-feet of water, 43 percent of which was apparently lost by evaporation. \r\n\r\nThe average seasonal runoff (1951-59) from the ephemeral streams of the Cornfield Wash basin and nearby watersheds can be expressed, with a high coefficient of correlation, by the equation: runoff = 29.4 (area) 0.82 acre-feet. This relation suggests that there is a good correlation between the size of the drainage basin and the basin characteristics that most influence travel time of runoff. Comparisons of readily measurable basin characteristics that influence travel time indicate: 1. Land slope is proportional to (area) .0.035; 2. Length of longest watercourse is proportional to (area) 0.52; 3. Distance along the longest watercourse from gaging station to a point opposite the center of drainage basin is proportional to (area)0.52; and 4. Equivalent channel slope is proportional to (area)- 0.027. Except for land slope, the coefficients of correlation for each of the basin characteristics-area relations were relatively high. The correlation between seasonal runoff (1951-60) from the small watersheds of the Cornfield Wash basin and the size of the drainage basin was improved after correcting for the influence of land slope.\r\n\r\nThe original total storage capacity of the 19 reservoirs was reduced from 845 to 455 acre-feet as a result of the impoundment of 390 acre-feet of sediment. Backwater from the reservoirs influenced the deposition of an additional 20 acre-feet of sediment. \r\n\r\nThe average annual accretion of sediment (1951-60) in the reservoirs of the Cornfield Wash basin can be expressed by the equation: sediment - 0.0119 (seasonal runoff) 1.3 (incised channel density) 0.71. By removing seasonal runoff as a variable, the average annual sediment accretion is proportional to (area) 1.19 (incised channel density) 1.3. \r\n\r\nConservation and rehabilitation of damaged land were successful in some instances and only partly successful in others. The reservoirs are effective in inducing sediment accretion upstream; also, they stop the advance of abrupt headcuts below the reservoirs, but only as long as the spillage is not great and the spillway stays intact. In addition, the reservoirs are effective in reducing flood peaks. A longer period of study is necessary to define adequately the effectiveness of the wire sediment barriers. The data collected on range-pitting effects were not complete enough to. define the magnitude of the changes, if any, in runoff, sediment, and vegetation yields.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1831","usgsCitation":"Burkham, D., 1966, Hydrology of Cornfield Wash area and effects of land-treatment practices, Sandoval County, New Mexico, 1951-60: U.S. Geological Survey Water Supply Paper 1831, Report: v, 87 p.; 1 Plate: 22.00 x 24.26 inches, https://doi.org/10.3133/wsp1831.","productDescription":"Report: v, 87 p.; 1 Plate: 22.00 x 24.26 inches","costCenters":[],"links":[{"id":25821,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1831/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25822,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1831/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":462211,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25036.htm","linkFileType":{"id":5,"text":"html"}},{"id":137933,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1831/report-thumb.jpg"}],"country":"United States","state":"New Mexico","county":"Sandoval County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-107.6208,36.2208],[-107.5854,36.2203],[-107.5501,36.2203],[-107.5147,36.219],[-107.4964,36.2183],[-107.4782,36.2181],[-107.4605,36.2178],[-107.4428,36.2181],[-107.4251,36.2178],[-107.404,36.2172],[-106.9865,36.2159],[-106.9141,36.2155],[-106.897,36.2152],[-106.877,36.2154],[-106.8766,36.1732],[-106.8806,36.0307],[-106.8814,36.0003],[-106.6158,36.002],[-106.3947,36.0025],[-106.3099,36.0018],[-106.2445,36.0011],[-106.2438,35.9657],[-106.2529,35.9666],[-106.2632,35.967],[-106.262,35.9725],[-106.2979,35.9742],[-106.2978,35.9651],[-106.2978,35.9601],[-106.3137,35.9592],[-106.3137,35.9542],[-106.3449,35.9527],[-106.3535,35.9536],[-106.3824,35.9535],[-106.3836,35.9612],[-106.395,35.9607],[-106.3949,35.9476],[-106.3968,35.8641],[-106.3967,35.8559],[-106.3949,35.8292],[-106.4147,35.8287],[-106.4124,35.8218],[-106.4067,35.8164],[-106.3982,35.8115],[-106.384,35.8097],[-106.3664,35.8116],[-106.3619,35.812],[-106.3522,35.8107],[-106.3517,35.8157],[-106.3352,35.8094],[-106.317,35.8058],[-106.2994,35.7977],[-106.2801,35.7932],[-106.2636,35.7801],[-106.2568,35.7719],[-106.2517,35.7638],[-106.25,35.7611],[-106.2466,35.7533],[-106.2454,35.742],[-106.2463,35.6758],[-106.2462,35.6544],[-106.2465,35.5469],[-106.2464,35.5319],[-106.2474,35.4802],[-106.2467,35.4461],[-106.246,35.4071],[-106.2458,35.3495],[-106.2463,35.315],[-106.2474,35.3054],[-106.2434,35.3054],[-106.2416,35.2519],[-106.242,35.2147],[-106.3765,35.2175],[-106.3822,35.2175],[-106.4531,35.2172],[-106.479,35.2176],[-106.4964,35.2184],[-106.5645,35.2186],[-106.5955,35.2184],[-106.8622,35.2172],[-106.8808,35.2171],[-106.9337,35.2171],[-106.9416,35.217],[-107.0345,35.2185],[-107.0761,35.2186],[-107.0801,35.2186],[-107.0936,35.2189],[-107.1105,35.2188],[-107.1262,35.2186],[-107.1578,35.2192],[-107.1623,35.2192],[-107.1628,35.2192],[-107.1972,35.2197],[-107.2345,35.3024],[-107.3016,35.3021],[-107.3025,35.4247],[-107.3035,35.4787],[-107.3032,35.5277],[-107.3041,35.6139],[-107.3046,35.6439],[-107.3048,35.6552],[-107.305,35.6707],[-107.3053,35.6852],[-107.305,35.6997],[-107.3052,35.7151],[-107.3049,35.7301],[-107.3057,35.7419],[-107.3054,35.7573],[-107.3053,35.7864],[-107.3047,35.8168],[-107.3049,35.8295],[-107.3051,35.8744],[-107.3055,35.9311],[-107.3058,35.9765],[-107.3054,35.991],[-107.3056,36.0005],[-107.317,36.0008],[-107.3397,36.0006],[-107.3875,36.0009],[-107.4068,36.0007],[-107.4421,36.0008],[-107.5161,36.0026],[-107.5513,36.0026],[-107.5541,36.0025],[-107.5718,36.0027],[-107.5866,36.003],[-107.6042,36.0032],[-107.6213,36.003],[-107.6247,36.0034],[-107.6244,36.0175],[-107.6242,36.032],[-107.6231,36.0633],[-107.6226,36.0892],[-107.6223,36.1041],[-107.6218,36.135],[-107.6216,36.1491],[-107.621,36.1763],[-107.6208,36.1917],[-107.6208,36.2208]]],[[[-106.2452,35.8563],[-106.2457,35.8427],[-106.2736,35.8563],[-106.2452,35.8563]]]]},\"properties\":{\"name\":\"Sandoval\",\"state\":\"NM\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db6049e0","contributors":{"authors":[{"text":"Burkham, D. E.","contributorId":97073,"corporation":false,"usgs":true,"family":"Burkham","given":"D. E.","affiliations":[],"preferred":false,"id":143163,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1346,"text":"wsp1540C - 1966 - Methods for analysis of selected metals in water by atomic absorption","interactions":[],"lastModifiedDate":"2012-02-02T00:05:13","indexId":"wsp1540C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1540","chapter":"C","title":"Methods for analysis of selected metals in water by atomic absorption","docAbstract":"This manual describes atomic-absorption-spectroscopy methods for determining calcium, copper, lithium, magnesium, manganese, potassium, sodium, strontium and zinc in atmospheric precipitation, fresh waters, and brines. The procedures are intended to be used by water quality laboratories of the Water Resources Division of the U.S. Geological Survey. Detailed procedures, calculations, and methods for the preparation of reagents are given for each element along with data on accuracy, precision, and sensitivity. Other topics discussed briefly are the principle of atomic absorption, instrumentation used, and special analytical techniques.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1540C","usgsCitation":"Fishman, M., and Downs, S.C., 1966, Methods for analysis of selected metals in water by atomic absorption: U.S. Geological Survey Water Supply Paper 1540, iii, 23-45 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1540C.","productDescription":"iii, 23-45 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":137473,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1540c/report-thumb.jpg"},{"id":26417,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1540c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a131","contributors":{"authors":[{"text":"Fishman, Marvin J.","contributorId":87110,"corporation":false,"usgs":true,"family":"Fishman","given":"Marvin J.","affiliations":[],"preferred":false,"id":143601,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Downs, Sanford C.","contributorId":66233,"corporation":false,"usgs":true,"family":"Downs","given":"Sanford","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":143600,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":33129,"text":"b1234 - 1966 - Bibliography of North American geology, 1964","interactions":[],"lastModifiedDate":"2012-02-02T00:09:11","indexId":"b1234","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1234","title":"Bibliography of North American geology, 1964","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1234","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1966, Bibliography of North American geology, 1964: U.S. Geological Survey Bulletin 1234, 944 p, https://doi.org/10.3133/b1234.","productDescription":"944 p","costCenters":[],"links":[{"id":247374,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1234/report.pdf","size":"45083","linkFileType":{"id":1,"text":"pdf"}},{"id":251821,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1234/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629913","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":529455,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":938,"text":"wsp1821 - 1966 - Availability of ground water upper Pawcatuck River basin Rhode Island","interactions":[],"lastModifiedDate":"2022-02-14T19:48:59.03077","indexId":"wsp1821","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1821","title":"Availability of ground water upper Pawcatuck River basin Rhode Island","docAbstract":"The upper Pawcatuck River basin is a 70-square-mile area in southcentral Rhode Island consisting of broad, rolling hills and narrow valleys in the north and fiat-floored plains in the south. It is drained by the Pawcatuck River and its two major tributaries, the Usquepaug-Queen River and the Chipuxet River. \r\n\r\nAnalysis of the water budget for the basin shows that approximately 94 mgd (million gallons per day) or about 63 percent of the precipitation flows out of the basin as streamflow. Of this amount, about 66 mgd is from ground-water seepage. \r\n\r\nTwo ground-water reservoirs composed of glacial deposits of sand and gravel and capable of substantial yields are in the basin. The larger reservoir underlies the central part of the Usquepaug-Queen River valley. This reservoir ranges in width from 3,000 to 4,000 feet and is 32,000 feet long. A large part of the reservoir contains sand and gravel more than 100 feet thick, having a permeability of more than 1,000 gallons per day per square foot. The yield of this reservoir is estimated to be about 17 mgd. \r\n\r\nThe smaller ground-water reservoir is in the Chipuxet River valley. It is about 4,000 feet wide and 16,000 feet long. A large part of this reservoir contains sand and gravel more than 150 feet thick having a permeability of more than 1,000 gallons per day per square foot. The yield of the Chipuxet reservoir is estimated to be about 8.6 mgd. \r\n\r\nMineral content of water from both of the reservoirs is generally less than 200 parts per million of dissolved solids. However, in the Chipuxet groundwater reservoir the dissolved solids are somewhat higher, and the iron content is a problem. \r\n\r\nOnly about 1.5 mgd of water is used in the basin. Most of it is used for public supplies and is obtained from wells not tapping the Usquepaug-Queen or Chipuxet ground-water reservoirs. Estimates of the 25 mgd of ground water potentially available are believed to be conservative, and substantially larger quantities may actually be available when development takes place.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1821","usgsCitation":"Allen, W.B., Hahn, G.W., and Brackley, R.A., 1966, Availability of ground water upper Pawcatuck River basin Rhode Island: U.S. Geological Survey Water Supply Paper 1821, Report: v, 66 p.; 3 Plates: 23.50 × 45.32 inches or smaller, https://doi.org/10.3133/wsp1821.","productDescription":"Report: v, 66 p.; 3 Plates: 23.50 × 45.32 inches or smaller","costCenters":[],"links":[{"id":25415,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1821/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25414,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1821/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25413,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1821/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25412,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1821/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137202,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1821/report-thumb.jpg"},{"id":395917,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25029.htm"}],"country":"United States","state":"Rhode Island","otherGeospatial":"upper Pawcatuck River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.633,\n              41.408\n            ],\n            [\n              -71.488,\n              41.408\n            ],\n            [\n              -71.488,\n              41.625\n            ],\n            [\n              -71.633,\n              41.625\n            ],\n            [\n              -71.633,\n              41.408\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d5ce","contributors":{"authors":[{"text":"Allen, William Burrows","contributorId":13596,"corporation":false,"usgs":true,"family":"Allen","given":"William","email":"","middleInitial":"Burrows","affiliations":[],"preferred":false,"id":142886,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hahn, Glenn Walter","contributorId":75899,"corporation":false,"usgs":true,"family":"Hahn","given":"Glenn","email":"","middleInitial":"Walter","affiliations":[],"preferred":false,"id":142888,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brackley, Richard A.","contributorId":61792,"corporation":false,"usgs":true,"family":"Brackley","given":"Richard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":142887,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1011,"text":"wsp1819C - 1966 - Summary of hydrologic conditions of the Louisville area, Kentucky","interactions":[],"lastModifiedDate":"2021-12-01T19:30:30.603416","indexId":"wsp1819C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1819","chapter":"C","title":"Summary of hydrologic conditions of the Louisville area, Kentucky","docAbstract":"Water problems and their solutions have been associated with the growth and development of the Louisville area for more than a century. Many hydrologic data that aided water users in the past can be applied to present water problems and will be helpful for solving many similar problems in the future. Most of the water problems of Louisville, a water-rich area, concern management and are associated with the distribution of supplies, the quality of water, drainage, and waste disposal. \r\n\r\nThe local hydrologic system at Louisville is dominated by the Ohio River and the glacial-outwash deposits beneath its flood plain. The water-bearing limestones in the uplands are ,secondary sources of water. The average flow of the Ohio River at Louisville, 73 billion gallons per day, and the potential availability of 370 million gallons per day of ground water suitable for industrial cooling purposes minimize the chance of acute water shortage in the area. Under current development, use of water averages about 211 million gallons per day, excluding about 392 million gallons of Ohio River water circulated daily through steampower plants and returned directly to the river. Optimum use and control of the water resources will be dependent on solving several water problems. The principal sources of water are in the Ohio River bottom land, whereas the new and potential centers of use are in the uplands. Either water must be piped to these new centers from the present sources or new supplies must be developed. Available data on streamflow and ground water are adequate to plan for the development of small local supplies. \r\n\r\nSince the completion of floodwalls and levees in 1953, widespread damage from flooding is a thing of the past in the Louisville area. Some local flooding of unprotected areas and of lowlands along tributary streams still takes place. The analyses of streamflow data are useful in planning for protection of these areas, but additional streamflow records and flood-area mapping are needed to best solve the problem. Droughts are a problem only to users of small water supplies in the uplands, where additional water either can be imported or developed locally. \r\n\r\nPollution and undesirable chemical quality of water for some uses are the most serious drawbacks to the optimum development of the water resources in Louisville and Jefferson County. Available chemical analyses of ground water are useful for determining its suitability for various uses, but additional data are needed to guide management decisions. Sources of contamination should be inventoried and water samples analyzed periodically to monitor changes in quality.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1965","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1819C","usgsCitation":"Bell, E.A., 1966, Summary of hydrologic conditions of the Louisville area, Kentucky: U.S. Geological Survey Water Supply Paper 1819, Report: iv, 36 p.; 6 Plates: 37.50 × 19.00 inches or smaller, https://doi.org/10.3133/wsp1819C.","productDescription":"Report: iv, 36 p.; 6 Plates: 37.50 × 19.00 inches or smaller","costCenters":[],"links":[{"id":392337,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25021.htm"},{"id":25615,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1819c/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25614,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1819c/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25616,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1819c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25613,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1819c/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25612,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1819c/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25611,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1819c/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25610,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1819c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137994,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1819c/report-thumb.jpg"}],"country":"United States","state":"Kentucky","city":"Louisville","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -85.87188720703125,\n              38.005902055387054\n            ],\n            [\n              -85.51071166992188,\n              38.005902055387054\n            ],\n            [\n              -85.51071166992188,\n              38.35350340353833\n            ],\n            [\n              -85.87188720703125,\n              38.35350340353833\n            ],\n            [\n              -85.87188720703125,\n              38.005902055387054\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db69905c","contributors":{"authors":[{"text":"Bell, Edwin Allen","contributorId":84340,"corporation":false,"usgs":true,"family":"Bell","given":"Edwin","email":"","middleInitial":"Allen","affiliations":[],"preferred":false,"id":143021,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1077,"text":"wsp1837 - 1966 - Hydrology of the cavernous limestones of the Mammoth Cave area, Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1837","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1837","title":"Hydrology of the cavernous limestones of the Mammoth Cave area, Kentucky","docAbstract":"The Mammoth Cave National Park in central Kentucky offers a unique opportunity to study the occurrence of ground water in limestone under natural conditions. Ground water occurs as perched and semiperched bodies in alternate sandstone, shale, and limestone formations and under water-table conditions at the approximate level of the Green River in thick soluble limestone. Three continuous recorders that operated for 5 years indicate that precipitation on the Mammoth Cave plateau recharges the underlying sandstone rapidly. Ground water from the sandstone discharges horizontally to the edges of the plateau and vertically to underlying formations. Some of the precipitation recharges underlying formations almost immediately through overland flow to sinkholes and free fall through open shafts to pools at the water table. \r\n\r\nMuch of the precipitation on the Pennyroyal plain flows overland into sinkholes and then through solution openings to the Green River. Water from the Green River flows into limestone solution channels under Mammoth Cave plateau at some stages, and this water discharges again to the Green River downstream. The presence of salt water, high in chloride in the Green River, makes it possible to trace the movement of the river water through the underground streams. Graphs show relationships of chloride concentration, stage of the Green River, time, precipitation, ground-water levels, and stratigraphy.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1837","usgsCitation":"Brown, R., 1966, Hydrology of the cavernous limestones of the Mammoth Cave area, Kentucky: U.S. Geological Survey Water Supply Paper 1837, v, 64 p. :illus, maps. ;24 cm., https://doi.org/10.3133/wsp1837.","productDescription":"v, 64 p. :illus, maps. ;24 cm.","costCenters":[],"links":[{"id":138041,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1837/report-thumb.jpg"},{"id":25784,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1837/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4828e4b07f02db4e6015","contributors":{"authors":[{"text":"Brown, Richmond F.","contributorId":40577,"corporation":false,"usgs":true,"family":"Brown","given":"Richmond F.","affiliations":[],"preferred":false,"id":143139,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1081,"text":"wsp1819D - 1966 - Water resources of Fort Huachuca Military Reservation, southeastern Arizona","interactions":[],"lastModifiedDate":"2023-02-07T20:29:25.76919","indexId":"wsp1819D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1819","chapter":"D","title":"Water resources of Fort Huachuca Military Reservation, southeastern Arizona","docAbstract":"<p>The Fort Huachuca Military Reservation, on the northeast flank of the Huachuca Mountains, is in the southern part of the San Pedro River drainage in the Basin and Range physiographic province in Arizona. The main sources of water available in the reservation area are ground water stored in two unconsolidated sedimentary deposits filling the San Pedro basin, and spring flow in Garden &middot;and Huachuca Canyons in the Huachuca Mountains.</p>\n<p>The unconsolidated deposits are divided into the upper and lower units of basin flu. These units yield the major part of the fort's water supply, and pumping from them has caused the water level in the Fort Huachuca well field to decline 3 feet per year. All the upper unit and 40 feet of the 220-foot-thick lower unit have seen dewatered in post wells 1 and 2. In Garden Canyon, spring flow is derived from solution channels and &nbsp;fractures in carbonate rocks; and in Huachuca Canyon, from fractures in mudstone, sandstone, carbonate rocks, &middot;and granite. The flow from springs generally is not used by the fort, but it is sufficient to supply the entire water demand during some periods.</p>\n<p>Spring flow, if used to supplement the ground-water supply, will decrease the draft on the ground-water reservoir in the two basin-fill units; or it could be used for artificial recharge to these aquifers. A second well field, if developed in the North Gate-Libby Field area, would partly accomplish the same result by decreasing the heavily concentrated draft on the ground-water reservoir of the Fort Huachuca well field, and by utilizing ground water that now moves unused northeastward to the San Pedro River.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, DC","doi":"10.3133/wsp1819D","usgsCitation":"Brown, S., Davidson, E., Kister, L., and Thomsen, B.W., 1966, Water resources of Fort Huachuca Military Reservation, southeastern Arizona: U.S. Geological Survey Water Supply Paper 1819, Report: v, 57 p.; 2 Plates: 33.50 x 39.00 inches and 16.00 x 9.50 inches, https://doi.org/10.3133/wsp1819D.","productDescription":"Report: v, 57 p.; 2 Plates: 33.50 x 39.00 inches and 16.00 x 9.50 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":25795,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1819d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":278836,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1819d/report.pdf"},{"id":137099,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1819d/report-thumb.jpg"},{"id":25796,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1819d/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":412823,"rank":5,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25022.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Arizona","otherGeospatial":"Fort Huachuca Military Reservation","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.5,\n              31.4\n            ],\n            [\n              -110.5,\n              31.75\n            ],\n            [\n              -110.117,\n              31.75\n            ],\n            [\n              -110.117,\n              31.4\n            ],\n            [\n              -110.5,\n              31.4\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0821","contributors":{"authors":[{"text":"Brown, S. G.","contributorId":46914,"corporation":false,"usgs":true,"family":"Brown","given":"S. G.","affiliations":[],"preferred":false,"id":143145,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davidson, E. S.","contributorId":57910,"corporation":false,"usgs":true,"family":"Davidson","given":"E. S.","affiliations":[],"preferred":false,"id":143147,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kister, L. R.","contributorId":54187,"corporation":false,"usgs":true,"family":"Kister","given":"L. R.","affiliations":[],"preferred":false,"id":143146,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Thomsen, B. W.","contributorId":39768,"corporation":false,"usgs":true,"family":"Thomsen","given":"B.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":143148,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":42918,"text":"ofr66120 - 1966 - Summer base-flow recession curves for Iowa streams","interactions":[],"lastModifiedDate":"2016-02-22T10:25:58","indexId":"ofr66120","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"66-120","title":"Summer base-flow recession curves for Iowa streams","docAbstract":"<p>Base-flow recession. curves for the summer months (June through September) were developed in this study for gaging stations on interior Iowa streams having five or more years of record. The tabulated data enables the user, starting with a known base flow at a gage, to estimate base flows for up to 20 days in the future. Rainfall during the period o&pound; the forecast will require that a new estimate be made after the stream again reaches base flow.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Iowa City","doi":"10.3133/ofr66120","collaboration":"Prepared in cooperation with the Iowa Natural Resources Council","usgsCitation":"Saboe, C., 1966, Summer base-flow recession curves for Iowa streams: U.S. Geological Survey Open-File Report 66-120, 27 p., https://doi.org/10.3133/ofr66120.","productDescription":"27 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":264294,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1966/0120/report.pdf","size":"1885","linkFileType":{"id":1,"text":"pdf"}},{"id":264295,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1966/0120/report-thumb.jpg"}],"country":"United 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,{"id":3841,"text":"cir527 - 1966 - Ground-water research in the United States","interactions":[],"lastModifiedDate":"2012-02-02T00:05:40","indexId":"cir527","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"527","title":"Ground-water research in the United States","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/cir527","usgsCitation":"Hackett, O.M., 1966, Ground-water research in the United States: U.S. Geological Survey Circular 527, 8 p. ;27 cm., https://doi.org/10.3133/cir527.","productDescription":"8 p. ;27 cm.","costCenters":[],"links":[{"id":118395,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1966/0527/report-thumb.jpg"},{"id":30914,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1966/0527/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db666ffd","contributors":{"authors":[{"text":"Hackett, O. M.","contributorId":38527,"corporation":false,"usgs":true,"family":"Hackett","given":"O.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":147706,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52522,"text":"ofr662 - 1966 - Extent and frequency of inundation of Schuylkill River flood plain from Conshohocken to Philadelphia, Pennsylvania","interactions":[{"subject":{"id":52522,"text":"ofr662 - 1966 - Extent and frequency of inundation of Schuylkill River flood plain from Conshohocken to Philadelphia, Pennsylvania","indexId":"ofr662","publicationYear":"1966","noYear":false,"title":"Extent and frequency of inundation of Schuylkill River flood plain from Conshohocken to Philadelphia, Pennsylvania"},"predicate":"SUPERSEDED_BY","object":{"id":68598,"text":"ha248 - 1967 - Floods on Schuylkill River from Conshohocken to Philadelphia, Pennsylvania","indexId":"ha248","publicationYear":"1967","noYear":false,"title":"Floods on Schuylkill River from Conshohocken to Philadelphia, Pennsylvania"},"id":1}],"supersededBy":{"id":68598,"text":"ha248 - 1967 - Floods on Schuylkill River from Conshohocken to Philadelphia, Pennsylvania","indexId":"ha248","publicationYear":"1967","noYear":false,"title":"Floods on Schuylkill River from Conshohocken to Philadelphia, Pennsylvania"},"lastModifiedDate":"2016-10-21T10:53:44","indexId":"ofr662","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"66-2","title":"Extent and frequency of inundation of Schuylkill River flood plain from Conshohocken to Philadelphia, Pennsylvania","docAbstract":"<p>Information on flood conditions plays an important part in the development and use of river valleys. This report presents maps, profiles, and flood-frequency relations developed from past flood experience on the Schuylkill River from Conshohocken to Philadelphia, Pa. The maps and profiles are used to define the areal extent and depth of flooding of the August 24, 1933, and August 19, 1955, floods. The flood of October 4, 1869, which is the greatest flood known on the lower Schuylkill River, is presented on the flood profile and on the ten cross sections. The area inundated by the 1869 flood is not defined because insufficient data are available and because hydrologic and hydraulic conditions have undoubtedly changed to such an extent that such a definition would have little present significance. The basic flood data were prepared to aid individuals, organizations, and governmental agencies in making sound decisions for the safe and economical development of the lower Schuylkill River valley. Recommendations for land use, or suggestions for limitations of land use, are not made in this report.</p><p>The responsibility for planning for the optimum land use in the flood plain and the implementation of flood-plain regulations to achieve such optimum use rests with the State and local interests. The preparation of this report was undertaken after consultation with representatives of the Philadelphia City Planning Commission and the Montgomery County Planning Commission who expressed the need for flood-plain information and their willingness to consider floodplain regulations.</p><p>The area covered by this report extends downstream along the Schuylkill River from Plymouth Dam in Conshohocken to the mouth of Wissahickon Creek in Philadelphia. Flooding along Wissahickon Creek is not included in the report. The reach studied extends from 13.0 miles to 21.0 miles upstream from the river mouth. All river distances used in the report are river miles upstream from the mouth of the Schuylkill River as used by the Corps of Engineer, U.S. Army and by the U.S. Geological Survey (Bogart, 1960, p. 194). For the convenience of users a tabulation of river miles of selected points upstream from the mouth of the Schuylkill River is included at the end of this report (table 1).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr662","usgsCitation":"Alter, A.T., 1966, Extent and frequency of inundation of Schuylkill River flood plain from Conshohocken to Philadelphia, Pennsylvania: U.S. Geological Survey Open-File Report 66-2, vii, 49 p., https://doi.org/10.3133/ofr662.","productDescription":"vii, 49 p.","numberOfPages":"61","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":177744,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":330310,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1966/0002/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Pennsylvania","city":"Conshohocken, Philadelphia","otherGeospatial":"Schuylkill River","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8b05","contributors":{"authors":[{"text":"Alter, A. T.","contributorId":60711,"corporation":false,"usgs":true,"family":"Alter","given":"A.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":245489,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52521,"text":"ofr661 - 1966 - Domestic water supply for the Hopland Indian Rancheria, Mendocino County, California","interactions":[],"lastModifiedDate":"2018-06-04T12:06:11","indexId":"ofr661","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"66-1","title":"Domestic water supply for the Hopland Indian Rancheria, Mendocino County, California","docAbstract":"<p>No abstract available.</p>","language":"English","doi":"10.3133/ofr661","usgsCitation":"Akers, J.P., 1966, Domestic water supply for the Hopland Indian Rancheria, Mendocino County, California: U.S. Geological Survey Open-File Report 66-1, 10 p., https://doi.org/10.3133/ofr661.","productDescription":"10 p.","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":177743,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"California","county":"Mendocino County","otherGeospatial":"Hopland Indian Rancheria","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db63606d","contributors":{"authors":[{"text":"Akers, J. P.","contributorId":82678,"corporation":false,"usgs":true,"family":"Akers","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":245488,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2306,"text":"wsp1822 - 1966 - Selected techniques in water resources investigations, 1965","interactions":[],"lastModifiedDate":"2017-09-06T15:33:12","indexId":"wsp1822","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1822","title":"Selected techniques in water resources investigations, 1965","docAbstract":"<p>Increasing world activity in water-resources development has created an interest in techniques for conducting investigations in the field. In the United States, the Geological Survey has the responsibility for extensive and intensive hydrologic studies, and the Survey places considerable emphasis on discovering better ways to carry out its responsibility. For many years, the dominant interest in field techniques has been \"in house,\" but the emerging world interest has led to a need for published accounts of this progress. In 1963 the Geological Survey published \"Selected Techniques in Water Resources Investigations\" (Water-Supply Paper 1669-Z) as part of the series \"Contributions to the Hydrology of the United States.\"</p><p>The report was so favorably received that successive volumes are planned, of which this is the first. The present report contains 25 papers that represent new ideas being tested or applied in the hydrologic field program of the Geological Survey. These ideas range from a proposed system for monitoring fluvial sediment to how to construct stream-gaging wells from steel oil drums. The original papers have been revised and edited by the compilers, but the ideas presented are those of the authors. The general description of the bubble gage on page 2 has been given by the compilers as supplementary information.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1822","usgsCitation":"1966, Selected techniques in water resources investigations, 1965: U.S. Geological Survey Water Supply Paper 1822, iii, 117 p., https://doi.org/10.3133/wsp1822.","productDescription":"iii, 117 p.","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":137715,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1822/report-thumb.jpg"},{"id":28129,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1822/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a03e4b07f02db5f830d","contributors":{"compilers":[{"text":"Mesnier, Glennon N.","contributorId":67488,"corporation":false,"usgs":true,"family":"Mesnier","given":"Glennon","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":709724,"contributorType":{"id":3,"text":"Compilers"},"rank":1},{"text":"Chase, Edith B.","contributorId":11192,"corporation":false,"usgs":true,"family":"Chase","given":"Edith","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":709725,"contributorType":{"id":3,"text":"Compilers"},"rank":2}]}}
,{"id":2261,"text":"wsp1805 - 1966 - Ground water in Huerfano County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:05:20","indexId":"wsp1805","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1805","title":"Ground water in Huerfano County, Colorado","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/wsp1805","usgsCitation":"McLaughlin, T.G., 1966, Ground water in Huerfano County, Colorado: U.S. Geological Survey Water Supply Paper 1805, v, 91 p. :illus., maps (8 fold. (3 col.)) ;24 cm., https://doi.org/10.3133/wsp1805.","productDescription":"v, 91 p. :illus., maps (8 fold. (3 col.)) ;24 cm.","costCenters":[],"links":[{"id":137571,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1805/report-thumb.jpg"},{"id":247196,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1805/plate-1_sheet_1.pdf","size":"11698","linkFileType":{"id":1,"text":"pdf"}},{"id":247197,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1805/plate-1_sheet_2.pdf","size":"10035","linkFileType":{"id":1,"text":"pdf"}},{"id":28046,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1805/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28047,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1805/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28048,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1805/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28049,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1805/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28050,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1805/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28051,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1805/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28052,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1805/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66db6e","contributors":{"authors":[{"text":"McLaughlin, Thad Gerald","contributorId":48941,"corporation":false,"usgs":true,"family":"McLaughlin","given":"Thad","email":"","middleInitial":"Gerald","affiliations":[],"preferred":false,"id":144913,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":37497,"text":"ssrw99 - 1966 - Waterfowl status report, 1966","interactions":[],"lastModifiedDate":"2012-02-02T00:09:51","indexId":"ssrw99","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":83,"text":"Special Scientific Report  - Wildlife","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"99","title":"Waterfowl status report, 1966","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Hansen, H.A., and Hudgins, M.R., 1966, Waterfowl status report, 1966 (Updates and revises Special Scientific Report-Wildlife 61 (1961).): Special Scientific Report  - Wildlife 99, 96 p.","productDescription":"96 p.","costCenters":[],"links":[{"id":94676,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/mdp.39015018209950?urlappend=%3Bseq=5"},{"id":165842,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Updates and revises Special Scientific Report-Wildlife 61 (1961).","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4b8c","contributors":{"authors":[{"text":"Hansen, Henry A. (compiler)","contributorId":101723,"corporation":false,"usgs":true,"family":"Hansen","given":"Henry","suffix":"(compiler)","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":218176,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hudgins, Mildred R.","contributorId":52632,"corporation":false,"usgs":true,"family":"Hudgins","given":"Mildred","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":218175,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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