No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrKS792","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Water resources data for Kansas, water year 1979; Volume 2, Arkansas River basin: U.S. Geological Survey Water Data Report KS-79-2, 373 p., https://doi.org/10.3133/wdrKS792.","productDescription":"373 p.","costCenters":[],"links":[{"id":181148,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f49ee","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":533006,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":56921,"text":"wdrWV791 - 1980 - Water resources data for West Virginia, water year 1979","interactions":[],"lastModifiedDate":"2025-02-25T14:56:53.408946","indexId":"wdrWV791","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"WV-79-1","title":"Water resources data for West Virginia, water year 1979","docAbstract":"Water resources data for the 1979 water year for West Virginia consist of records of stage, discharge, and water quality of streams and springs; stage and contents of lakes and reservoirs; and water levels in wells. This report contains discharge records for 117 gaging stations; stage only records for 8 gaging stations; stage and contents for 7 lakes and reservoirs; contents for 1 reservoir; change in contents for 1 reservoir; water quality for 92 gaging stations; and water levels for 34 observation wells. Also included are 2 crest-stage partial-record stations, and 1 low-flow partial record station. Additional water data were collected at various sites, not part of the systematic data collections program, and are published as miscellaneous measurements and analyses. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in West Virginia.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrWV791","collaboration":"Prepared in cooperation with the State of West Virginia and other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Water resources data for West Virginia, water year 1979: U.S. Geological Survey Water Data Report WV-79-1, viii, 417 p., https://doi.org/10.3133/wdrWV791.","productDescription":"viii, 417 p.","costCenters":[],"links":[{"id":482435,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1979/wv-79-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":181150,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1979/wv-79-1/report-thumb.jpg"}],"country":"United States","state":"West 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Only three wells were being used in 1979, two by the community of St. Paul and one by the Coast Guard Loran facility. All wells are in the southeastern part of the island. The island has no established surface drainage, and no springs were found on the eastern part of the island during the survey. Drainage of ground-water from the island is assumed to be by seepage through the sandy deposits along the east coast and possibly by undersea discharge elsewhere on the island. On the basis of present well yields, amount of freshwater inferred to be present below the water table, and potential recharge from precipitation, it is concluded that it should be possible to design a well field in the southeastern part of the island that could yield more than a million gallons per day without danger of inducing saline water into the well field. The water is of good chemical quality. 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Pleistocene","interactions":[],"lastModifiedDate":"2012-02-02T00:08:20","indexId":"ofr80569","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-569","title":"Paleohydrology of the southern Great Basin, with special reference to water table fluctuations beneath the Nevada Test Site during the late(?) Pleistocene","docAbstract":"Knowledge of the magnitude of water-table rise during Pleistocene pluvial climates, and of the resultant shortening of groundwater flow path and reduction in unsaturated zone thickness, is mandatory for a technical evaluation of the Nevada Test Site (NTS) or other arid zone sites as repositories for high-level or transuranic radioactive wastes. The distribution of calcitic veins filling fractures in alluvium, and of tufa deposits between the Ash Meadows spring discharge area and the Nevada Test Site indicates that discharge from the regional Paleozoic carbonate aquifer during the Late( ) Pleistocene pluvial periods may have occurred at an altitude about 50 meters higher than at present and 14 kilometers northeast of Ash Meadows. Use of the underflow equation (relating discharge to transmissivity, aquifer width, and hydraulic gradient), and various assumptions regarding pluvial recharge, transmissivity, and altitude of groundwater base level, suggest possible rises in potentiometric level in the carbonate aquifer of about -90 meters beneath central Frenchman Flat. During Wisconsin time the rise probably did not exceed 30 meters. Water-level rises beneath Frenchman Flat during future pluvials are unlikely to exceed 30 meters and might even be 10 meters lower than modern levels. Neither the cited rise in potentiometric level in the regional carbonate aquifer, nor the shortened flow path during the Late( ) Pleistocene preclude utilization of the NTS as a repository for high-level or transuranic-element radioactive wastes provided other requisite conditions are met as this site. Deep water tables, attendant thick (up to several hundred meter) unsaturated zones, and long groundwater flow paths characterized the region during the Wisconsin Stage and probably throughout the Pleistocene Epoch and are likely to so characterize it during future glacial periods. (USGS)","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey ; Open-file Services Section, U.S. Geological Survey [distributor],","doi":"10.3133/ofr80569","issn":"0094-9140","usgsCitation":"Winograd, I.J., and Doty, G.C., 1980, Paleohydrology of the southern Great Basin, with special reference to water table fluctuations beneath the Nevada Test Site during the late(?) Pleistocene: U.S. Geological Survey Open-File Report 80-569, iv, 97 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr80569.","productDescription":"iv, 97 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":157228,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0569/report-thumb.jpg"},{"id":53875,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0569/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689d2c","contributors":{"authors":[{"text":"Winograd, Isaac Judah","contributorId":9233,"corporation":false,"usgs":true,"family":"Winograd","given":"Isaac","email":"","middleInitial":"Judah","affiliations":[],"preferred":false,"id":192744,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Doty, Gene C.","contributorId":96272,"corporation":false,"usgs":true,"family":"Doty","given":"Gene","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":192745,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":36671,"text":"fwsobs80_34 - 1980 - Strategy for assessing impacts of power plants on fish and shellfish populations","interactions":[],"lastModifiedDate":"2012-02-02T00:10:00","indexId":"fwsobs80_34","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"80/34","title":"Strategy for assessing impacts of power plants on fish and shellfish populations","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Fritz, E.S., Rago, P.J., and Murarka, I.P., 1980, Strategy for assessing impacts of power plants on fish and shellfish populations: FWS/OBS 80/34, xii, 68 p. : ill.; 28 cm.","productDescription":"xii, 68 p. : ill.; 28 cm.","costCenters":[],"links":[{"id":161834,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b1102","contributors":{"authors":[{"text":"Fritz, Eugene S.","contributorId":32207,"corporation":false,"usgs":true,"family":"Fritz","given":"Eugene","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":216766,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rago, Paul J.","contributorId":91153,"corporation":false,"usgs":true,"family":"Rago","given":"Paul","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":216768,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Murarka, Ishwar P.","contributorId":47000,"corporation":false,"usgs":true,"family":"Murarka","given":"Ishwar","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":216767,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ]}