{"pageNumber":"4635","pageRowStart":"115850","pageSize":"25","recordCount":184553,"records":[{"id":39781,"text":"pp1469 - 1988 - Surficial geology and geomorphology of the Mountain Lake area, Giles County, Virginia, including sedimentological studies of colluvium and boulder streams","interactions":[],"lastModifiedDate":"2012-02-02T00:10:15","indexId":"pp1469","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"1469","title":"Surficial geology and geomorphology of the Mountain Lake area, Giles County, Virginia, including sedimentological studies of colluvium and boulder streams","language":"ENGLISH","doi":"10.3133/pp1469","usgsCitation":"Mills, H.H., 1988, Surficial geology and geomorphology of the Mountain Lake area, Giles County, Virginia, including sedimentological studies of colluvium and boulder streams: U.S. Geological Survey Professional Paper 1469, 57 p., https://doi.org/10.3133/pp1469.","productDescription":"57 p.","costCenters":[],"links":[{"id":113793,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1469/report.pdf","size":"20323","linkFileType":{"id":1,"text":"pdf"}},{"id":169458,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1469/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688c30","contributors":{"authors":[{"text":"Mills, H. H.","contributorId":18384,"corporation":false,"usgs":true,"family":"Mills","given":"H.","middleInitial":"H.","affiliations":[],"preferred":false,"id":222151,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4658,"text":"twri05A4_1988 - 1988 - Methods for collection and analysis of aquatic biological and microbiological samples","interactions":[],"lastModifiedDate":"2013-11-19T16:16:02","indexId":"twri05A4_1988","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"05-A4","title":"Methods for collection and analysis of aquatic biological and microbiological samples","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/twri05A4_1988","usgsCitation":"Britton, L.J., 1988, Methods for collection and analysis of aquatic biological and microbiological samples (1988 Revision): U.S. Geological Survey Techniques of Water-Resources Investigations 05-A4, xv, 685 p., https://doi.org/10.3133/twri05A4_1988.","productDescription":"xv, 685 p.","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":139329,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"1988 Revision","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a16f","contributors":{"authors":[{"text":"Britton, Linda J.","contributorId":72780,"corporation":false,"usgs":true,"family":"Britton","given":"Linda","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":149569,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2327,"text":"wsp2265 - 1988 - The Spokane aquifer, Washington: its geologic origin and water-bearing and water-quality characteristics","interactions":[],"lastModifiedDate":"2012-02-02T00:05:19","indexId":"wsp2265","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"2265","title":"The Spokane aquifer, Washington: its geologic origin and water-bearing and water-quality characteristics","docAbstract":"The Spokane aquifer is an unconfined aquifer consisting of coarse sand, gravel, cobbles, and boulders deposited during several catastrophic glacial outburst floods--known as the Spokane Floods---of Pleistocene time. The aquifer is one of the most productive in the United States, and, as the only significant source of good-quality water supply in the Spokane Valley, it has been designated as a 'Sole Source Aquifer' by the U.S. Environmental Protection Agency. \r\n\r\nThe Spokane aquifer underlies an area of about 135 square miles in the Spokane Valley and varies in saturated thickness from a few feet to 500 feet or more. The aquifer is recharged by ground-water underflow from the Rathdrum Prairie aquifer in Idaho on the east, by ground-water underflow and surface-water seepage from small drainage areas along the Spokane Valley margins, and by percolation from various sources--from rainfall and snowmelt, from some reaches of the Spokane and Little Spokane Rivers, and from septic-tank drain fields, cesspools, and irrigation water. Discharge from the aquifer occurs by ground-water underflow from the lowermost end of the valley, by leakage to the Spokane and the Little Spokane Rivers, by evapotranspiration, and by ground-water withdrawal by pumping. The transmissivity of the aquifer ranges from less than 0.05 to 70 feet squared per second, and its specific yield ranges from less than 5 to 20 percent of the aquifer volume. Seasonal water-level fluctuations in wells tapping the aquifer are generally less than 10 feet. The annual pumpage from the aquifer in 1977 was about 164,000 acre-feet, of which about 70 percent was for municipal supplies, which included some industrial and commercial supplies. \r\n\r\nLand use over the aquifer includes predominantly agricultural activities in the eastern one-third of the valley and urban and residential developments in most of the remaining area. Potential sources of contamination of the aquifer include percolation from cesspools, septic-tank drain fields, and municipal and industrial waste-disposal sites. In general, the high rate of ground-water movement through the highly permeable aquifer materials has resulted in the ground-water quality being little affected by the overlying land use activities. Some local degradation of water quality has occurred due to industrial waste-disposal practices, however. During the water-quality study period of May 1977 to May 1978, average specific conductance of the ground water ranged from less than 100 to about 500 micromhos per centimeter at 25 degrees Celsius, average chloride concentration ranged from less than 2 to about 12 milligrams per liter (equivalent to parts per million}, and average nitrate nitrogen concentrations ranged from less than 1 to about 8 milligrams per liter. \r\n\r\nThe streamflow and water quality of the Spokane River, which are related to the flow and quality of water in the Spokane aquifer, indicate that, during the period 1913 to 1978 inclusive, the river at Post Falls, Idaho, had an average annual discharge of 6,307 cubic feet per second, a maximum discharge of 50,100 cubic feet per second, and a minimum discharge of 65 cubic feet per second. The quality of the river water along its course through the study area is affected to some extent by inflows of industrial wastewater and treated municipal sewered water. In the 30-mile reach between the State line and Riverside State Park, during the 1975 to 1978 water years inclusive, concentrations of nearly all the constituents analyzed increased, and concentrations of dissolved oxygen correspondingly decreased from 1968 to 1977 inclusive; coliform bacteria also showed notable increases in the downstream direction.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2265","usgsCitation":"Molenaar, D., 1988, The Spokane aquifer, Washington: its geologic origin and water-bearing and water-quality characteristics: U.S. Geological Survey Water Supply Paper 2265, vii, 74 p. :ill., (some col.), col. maps ;28 cm., https://doi.org/10.3133/wsp2265.","productDescription":"vii, 74 p. :ill., (some col.), col. maps ;28 cm.","costCenters":[],"links":[{"id":137598,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2265/report-thumb.jpg"},{"id":28170,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2265/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a85f","contributors":{"authors":[{"text":"Molenaar, Dee","contributorId":34485,"corporation":false,"usgs":true,"family":"Molenaar","given":"Dee","email":"","affiliations":[],"preferred":false,"id":145019,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":237,"text":"wsp2330 - 1988 - Selected papers in the hydrologic sciences, 1987","interactions":[],"lastModifiedDate":"2024-01-24T19:25:26.608273","indexId":"wsp2330","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"2330","title":"Selected papers in the hydrologic sciences, 1987","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2330","usgsCitation":"1988, Selected papers in the hydrologic sciences, 1987: U.S. Geological Survey Water Supply Paper 2330, v, 129 p., https://doi.org/10.3133/wsp2330.","productDescription":"v, 129 p.","costCenters":[],"links":[{"id":424767,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25552.htm","text":"Use of aeromagnetic data to define boundaries of a carbonate-rock aquifer in east-central Nevada","linkFileType":{"id":5,"text":"html"},"description":"25552"},{"id":424766,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25406.htm","text":"Potential for saltwater intrusion into the Upper Floridan aquifer, Hernando County, Florida","linkFileType":{"id":5,"text":"html"},"description":"25406"},{"id":424765,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25285.htm","text":"Base flow as an indicator of drought occurrence","linkFileType":{"id":5,"text":"html"},"description":"25285"},{"id":421281,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25259.htm","text":"Fire-related debris flows in the Beaver Creek drainage, Lewis and Clark County, Montana","linkFileType":{"id":5,"text":"html"},"description":"25259"},{"id":24846,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2330/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":136529,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2330/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a03e4b07f02db5f838e","contributors":{"editors":[{"text":"Subitzky, Seymour","contributorId":35710,"corporation":false,"usgs":true,"family":"Subitzky","given":"Seymour","affiliations":[],"preferred":false,"id":884410,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":63588,"text":"gp987Z - 1988 - The magnetic field of the earth— 1985: Vertical intensity chart","interactions":[],"lastModifiedDate":"2025-07-18T20:11:34.989856","indexId":"gp987Z","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"987","chapter":"Z","title":"The magnetic field of the earth— 1985: Vertical intensity chart","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp987Z","usgsCitation":"Peddie, N., and Zunde, A., 1988, The magnetic field of the earth— 1985: Vertical intensity chart: U.S. Geological Survey Geophysical Investigations Map 987, 1 Plate: 48.29 × 34.00 inches, https://doi.org/10.3133/gp987Z.","productDescription":"1 Plate: 48.29 × 34.00 inches","costCenters":[],"links":[{"id":186921,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":260503,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0987z/plate-1.pdf"},{"id":391701,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6336.htm"}],"scale":"40053700","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b995","contributors":{"authors":[{"text":"Peddie, N.W.","contributorId":75911,"corporation":false,"usgs":true,"family":"Peddie","given":"N.W.","affiliations":[],"preferred":false,"id":269187,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zunde, A.K.","contributorId":21946,"corporation":false,"usgs":true,"family":"Zunde","given":"A.K.","affiliations":[],"preferred":false,"id":269186,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28468,"text":"wri884109 - 1988 - Quality-assurance data for routine water analysis in the laboratories of the US Geological Survey for water-year 1985","interactions":[],"lastModifiedDate":"2012-02-02T00:08:50","indexId":"wri884109","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"88-4109","title":"Quality-assurance data for routine water analysis in the laboratories of the US Geological Survey for water-year 1985","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884109","usgsCitation":"Lucey, K., and Peart, D., 1988, Quality-assurance data for routine water analysis in the laboratories of the US Geological Survey for water-year 1985: U.S. Geological Survey Water-Resources Investigations Report 88-4109, vii, 121 p. :chiefly ill. ;28 cm., https://doi.org/10.3133/wri884109.","productDescription":"vii, 121 p. :chiefly ill. ;28 cm.","costCenters":[],"links":[{"id":159312,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4109/report-thumb.jpg"},{"id":57270,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4109/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8ae4b07f02db6514f7","contributors":{"authors":[{"text":"Lucey, K.J.","contributorId":70002,"corporation":false,"usgs":true,"family":"Lucey","given":"K.J.","email":"","affiliations":[],"preferred":false,"id":199855,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peart, D.B.","contributorId":45304,"corporation":false,"usgs":true,"family":"Peart","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":199854,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38409,"text":"pp1476 - 1988 - Geology of the Farmington Canyon complex, Wasatch Mountains, Utah","interactions":[],"lastModifiedDate":"2025-09-23T16:48:42.146165","indexId":"pp1476","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"1476","title":"Geology of the Farmington Canyon complex, Wasatch Mountains, Utah","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1476","usgsCitation":"Bryant, B., 1988, Geology of the Farmington Canyon complex, Wasatch Mountains, Utah: U.S. Geological Survey Professional Paper 1476, Report: iv, 54 p., 1 Plate: 33.00 x 41.00 inches, https://doi.org/10.3133/pp1476.","productDescription":"Report: iv, 54 p., 1 Plate: 33.00 x 41.00 inches","costCenters":[],"links":[{"id":119326,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1476/report-thumb.jpg"},{"id":64789,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1476/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64788,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1476/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":495912,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4897.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Utah","otherGeospatial":"Farmington Canyon complex, Wasatch Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -111.9394,\n              41.25\n            ],\n            [\n              -111.9394,\n              40.8275\n            ],\n            [\n              -111.6858,\n              40.8275\n            ],\n            [\n              -111.6858,\n              41.25\n            ],\n            [\n              -111.9394,\n              41.25\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae4af","contributors":{"authors":[{"text":"Bryant, Bruce bbryant@usgs.gov","contributorId":1355,"corporation":false,"usgs":true,"family":"Bryant","given":"Bruce","email":"bbryant@usgs.gov","affiliations":[],"preferred":false,"id":219771,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68091,"text":"ha694A - 1988 - Hydrogeology of the Great Basin region of Nevada, Utah, and adjacent states","interactions":[],"lastModifiedDate":"2017-02-21T10:46:55","indexId":"ha694A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"694","chapter":"A","title":"Hydrogeology of the Great Basin region of Nevada, Utah, and adjacent states","docAbstract":"<p>This atlas is a product of the Great Basin Regional Aquifer-System Analysis (RASA), a study that began in 1981. The study is part of a U.S. Geological Survey program for evaluating regional aquifer systems nationwide. A regional aquifer system is defined as “an areally extensive set of aquifers which are linked in some way, such as hydraulically or economically” (Harrill and others, 1983, p. 2). The purpose of the Great Basin RASA is to evaluate aquifer system in the Great Basin by developing a better understanding of recharge and discharge processes, delineating individual ground-water flow systems, and developing mathematical models of representative flow systems. Harrill and others (1983) provide a more complete background of both the national RASA program and the Great Basin RASA.</p><p>The purpose of this atlas is to delineate and describe the major hydrogeologic units in the Great Basin region and to identify those units that (1) constitute regional aquifers or (2) act as barriers to the movement of ground water. The scope of this atlas, however, is limited to a brief geologic overview of the Great Basin: lithology and areal extent of units, major structural features, and influence of tectonic events. In addition, the water-bearing characteristics of each unit are briefly summarized.</p><p>This atlas is Chapter A of the three-part Hydrologic Atlas series. Chapter B shows ground-water levels in the Great Basin region, and Chapter C shows inferred directions of ground-water flow and individual flow systems.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ha694A","usgsCitation":"Plume, R.W., and Carlton, S.M., 1988, Hydrogeology of the Great Basin region of Nevada, Utah, and adjacent states: U.S. Geological Survey Hydrologic Atlas 694, 1 Sheet: 33.00 x 43.57 inches, https://doi.org/10.3133/ha694A.","productDescription":"1 Sheet: 33.00 x 43.57 inches","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":186302,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":335841,"rank":4,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/ha694C","text":"HA-694-C","linkHelpText":"Major ground-water flow systems in the Great Basin region of Nevada, Utah, and adjacent states"},{"id":335842,"rank":2,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/ha694B","text":"HA-694-B","linkHelpText":"Ground-water levels in the Great Basin region of Nevada, Utah, and adjacent states"},{"id":89349,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/694a/plate-1.pdf","text":"Hydrologic Atlas HA-694-A","size":"16.14 MB","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","country":"United States","state":"Nevada, Utah","otherGeospatial":"Great Basin region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120.32226562500001,\n              42.24478535602799\n            ],\n            [\n              -120.32226562500001,\n              38.77121637244273\n            ],\n            [\n              -114.86206054687499,\n              34.867904962568716\n            ],\n            [\n              -113.983154296875,\n              37.01132594307015\n            ],\n            [\n              -111.24755859375,\n              40.136890695345905\n            ],\n            [\n              -111.060791015625,\n              42.293564192170095\n            ],\n            [\n              -120.32226562500001,\n              42.24478535602799\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ee4b07f02db6150f4","contributors":{"authors":[{"text":"Plume, Russell W. rwplume@usgs.gov","contributorId":2303,"corporation":false,"usgs":true,"family":"Plume","given":"Russell","email":"rwplume@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":277625,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carlton, Stephen M.","contributorId":56309,"corporation":false,"usgs":true,"family":"Carlton","given":"Stephen","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":277626,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38541,"text":"pp1330 - 1988 - A seismic-stratigraphic investigation of the Madison and associated aquifers; application to ground-water exploration, Powder River basin, Montana-Wyoming","interactions":[],"lastModifiedDate":"2025-08-22T18:53:36.890323","indexId":"pp1330","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"1330","title":"A seismic-stratigraphic investigation of the Madison and associated aquifers; application to ground-water exploration, Powder River basin, Montana-Wyoming","docAbstract":"<p>This seismic-stratigraphic investigation is part of a larger 5-year project the \"Madison Project\" undertaken by the Water Resources Division of the U.S. Geological Survey to study the hydrology of the Madison and associated aquifers. The objectives and methods of investigation of the Madison Project are described by the U.S. Geological Survey (1975). </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1330","usgsCitation":"1988, A seismic-stratigraphic investigation of the Madison and associated aquifers; application to ground-water exploration, Powder River basin, Montana-Wyoming: U.S. Geological Survey Professional Paper 1330, Report: iii, 99 p.; 1 Plate: 58.00 × 41.00 inches, https://doi.org/10.3133/pp1330.","productDescription":"Report: iii, 99 p.; 1 Plate: 58.00 × 41.00 inches","costCenters":[],"links":[{"id":120241,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1330/report-thumb.jpg"},{"id":65308,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1330/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65309,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1330/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":402077,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74254.htm","text":"Introduction to seismic-stratigraphic study of the Madison and associated aquifers","linkFileType":{"id":5,"text":"html"}},{"id":494548,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74255.htm","text":"Regional stratigraphic framework and genesis of the Madison and associated aquifers","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Montana, Wyoming","otherGeospatial":"Powder River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -104.04052734375,\n              43.27720532212024\n            ],\n            [\n              -104.1064453125,\n              46.7549166192819\n            ],\n            [\n              -108.47900390625,\n              46.649436163350245\n            ],\n            [\n              -107.75390625,\n              44.308126684886126\n            ],\n            [\n              -106.23779296875,\n              43.229195113965005\n            ],\n            [\n              -104.04052734375,\n              43.27720532212024\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b18e4b07f02db6a7042","contributors":{"editors":[{"text":"Balch, A. H.","contributorId":104892,"corporation":false,"usgs":true,"family":"Balch","given":"A.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":726041,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":61709,"text":"gq1619 - 1988 - Geologic map of the Rustic quadrangle, Larimer County, Colorado","interactions":[],"lastModifiedDate":"2012-02-10T00:10:30","indexId":"gq1619","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1619","title":"Geologic map of the Rustic quadrangle, Larimer County, Colorado","language":"ENGLISH","doi":"10.3133/gq1619","usgsCitation":"Shaver, K.C., Neese, W.D., and Braddock, W.A., 1988, Geologic map of the Rustic quadrangle, Larimer County, Colorado: U.S. Geological Survey Geologic Quadrangle 1619, 1 map :col. ;58 x 44 cm., on sheet 74 x 93 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/gq1619.","productDescription":"1 map :col. ;58 x 44 cm., on sheet 74 x 93 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":102693,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1143.htm","linkFileType":{"id":5,"text":"html"},"description":"1143"},{"id":248009,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1619/report.pdf","size":"68","linkFileType":{"id":1,"text":"pdf"}},{"id":252586,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1619/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.61749999999999,40.6175 ], [ -105.61749999999999,40.75 ], [ -105.5,40.75 ], [ -105.5,40.6175 ], [ -105.61749999999999,40.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db61153e","contributors":{"authors":[{"text":"Shaver, Kenneth Charles","contributorId":10098,"corporation":false,"usgs":true,"family":"Shaver","given":"Kenneth","email":"","middleInitial":"Charles","affiliations":[],"preferred":false,"id":266264,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Neese, William D.","contributorId":30293,"corporation":false,"usgs":true,"family":"Neese","given":"William","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":266265,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Braddock, William A.","contributorId":61010,"corporation":false,"usgs":true,"family":"Braddock","given":"William","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":266266,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":49075,"text":"ofr88593D - 1988 - PCCONTUR VERSION 1.0 : a microcomputer general purpose contouring program, Part D - Plot system source code and library disk","interactions":[],"lastModifiedDate":"2012-02-02T00:10:44","indexId":"ofr88593D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-593","chapter":"D","title":"PCCONTUR VERSION 1.0 : a microcomputer general purpose contouring program, Part D - Plot system source code and library disk","language":"ENGLISH","doi":"10.3133/ofr88593D","usgsCitation":"Godson, R.H., Bracken, R.E., and Webring, M.W., 1988, PCCONTUR VERSION 1.0 : a microcomputer general purpose contouring program, Part D - Plot system source code and library disk: U.S. Geological Survey Open-File Report 88-593, 1 computer diskette (5 1/4 in.), https://doi.org/10.3133/ofr88593D.","productDescription":"1 computer diskette (5 1/4 in.)","costCenters":[],"links":[{"id":172032,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689ef1","contributors":{"authors":[{"text":"Godson, Richard H.","contributorId":11190,"corporation":false,"usgs":true,"family":"Godson","given":"Richard","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":238969,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bracken, Robert E. 0000-0001-7759-2743 rbracken@usgs.gov","orcid":"https://orcid.org/0000-0001-7759-2743","contributorId":2640,"corporation":false,"usgs":true,"family":"Bracken","given":"Robert","email":"rbracken@usgs.gov","middleInitial":"E.","affiliations":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":238968,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Webring, Michael W. mwebring@usgs.gov","contributorId":1221,"corporation":false,"usgs":true,"family":"Webring","given":"Michael","email":"mwebring@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":238967,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":28799,"text":"wri874174 - 1988 - Dye tracing techniques used to determine ground-water flow in a carbonate aquifer system near Elizabethtown, Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:08:44","indexId":"wri874174","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4174","title":"Dye tracing techniques used to determine ground-water flow in a carbonate aquifer system near Elizabethtown, Kentucky","docAbstract":"Because of the vulnerability of karst aquifers to contamination and the need for water managers to know recharge areas and groundwater flow characteristics for springs and wells used for public water supply, qualitative and quantitative dye tracing techniques were used during a groundwater investigation in the Elizabethtown area, Hardin County, in north-central Kentucky. The principal aquifer in the Elizabethtown area is thick, nearly horizontal beds of limestone, and thin beds of shale of Mississippi age. As much as 65% of all water pumped for the city water supply is obtained from two springs and two wells that obtain water from these rocks. Sinkholes were classified according to their ability to funnel runoff directly into the groundwater flow system, based primarily on the nature of the swallet draining the sinkhole. The presence of bedrock in the sinkhole nearly always ensured a well defined swallet leading to the subsurface. Qualitative and quantitative dye tracing techniques and equipment are discussed in detail. Qualitative dye tracing with fluorescein dye and passive dye detectors, consisting of activated coconut charcoal identified point to point connection between representative sinkholes, sinking streams, and karst windows and the city springs and wells. Qualitative tracing confirmed the presence of infiltrated surface water from a perennial stream, Valley Creek, in water from city wells and generally confirmed the direction of groundwater flow as shown by a water level contour map. Quantitative dye tracing with rhodamin WT, automatic samplers, discharge measurements, and fluorometric analyses were used to determine flow characteristics such as traveltime for arrival of the leading edge, peak concentration, trailing edge, and persistence of the dye cloud at the spring resurgence. Analyses of the dye recovery curves for quantitative dye traces completed between the same sinkholes and a city spring, and during different flow conditions showed that the arrival time of the leading edge of the dye cloud ranged from 5 to 24 hours and that the traveltime of the centroid of the dye cloud ranged from 6 to 31 hours when discharge was 4.6 and 0.53 cu ft/second, respectively. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874174","usgsCitation":"Mull, D.S., Smoot, J.L., and Liebermann, T., 1988, Dye tracing techniques used to determine ground-water flow in a carbonate aquifer system near Elizabethtown, Kentucky: U.S. Geological Survey Water-Resources Investigations Report 87-4174, vii, 102 p. :ill., map ;28 cm., https://doi.org/10.3133/wri874174.","productDescription":"vii, 102 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":110247,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_46832.htm","linkFileType":{"id":5,"text":"html"},"description":"46832"},{"id":123375,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4174/report-thumb.jpg"},{"id":57666,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4174/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57667,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4174/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a59e4b07f02db62fa03","contributors":{"authors":[{"text":"Mull, D. S.","contributorId":43331,"corporation":false,"usgs":true,"family":"Mull","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":200412,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smoot, J. L.","contributorId":59794,"corporation":false,"usgs":true,"family":"Smoot","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":200413,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Liebermann, T.D.","contributorId":23569,"corporation":false,"usgs":true,"family":"Liebermann","given":"T.D.","email":"","affiliations":[],"preferred":false,"id":200411,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":38401,"text":"pp1466A - 1988 - Geology and tectonic history of the lower Cape Fear River valley, southeastern North Carolina","interactions":[],"lastModifiedDate":"2022-03-31T18:32:18.257183","indexId":"pp1466A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"1466","chapter":"A","title":"Geology and tectonic history of the lower Cape Fear River valley, southeastern North Carolina","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1466A","usgsCitation":"Soller, D.R., 1988, Geology and tectonic history of the lower Cape Fear River valley, southeastern North Carolina: U.S. Geological Survey Professional Paper 1466, Report: iv, 60 p.; 1 Plate: 17.50 × 22.00 inches, https://doi.org/10.3133/pp1466A.","productDescription":"Report: iv, 60 p.; 1 Plate: 17.50 × 22.00 inches","costCenters":[],"links":[{"id":64768,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1466a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":397943,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4891.htm"},{"id":64769,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1466a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119817,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1466a/report-thumb.jpg"}],"scale":"250000","country":"United States","state":"North Carolina","otherGeospatial":"lower Cape Fear River valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -79.1381,\n              34\n            ],\n            [\n              -78,\n              34\n            ],\n            [\n              -78,\n              35\n            ],\n            [\n              -79.1381,\n              35\n            ],\n            [\n              -79.1381,\n              34\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db684258","contributors":{"authors":[{"text":"Soller, D. R.","contributorId":25923,"corporation":false,"usgs":true,"family":"Soller","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":219755,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28455,"text":"wri884045 - 1988 - Streamflows in Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:08:52","indexId":"wri884045","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"88-4045","title":"Streamflows in Wyoming","docAbstract":"A description of the occurrence and availability of surface waters in Wyoming is presented along with explanations of both streamflow-data collection and methods for estimating streamflow characteristics at gaged and ungaged sites. Mountain ranges separate the major drainage basins and have a significant effect on the quantity of precipitation and the volume of runoff that occurs in Wyoming. Perennial streams that originate in the mountains provide the most dependable source of runoff; streams that originate in the plains and deserts generally are intermittent or ephemeral and have extended periods of no flow. Streamflow data for several hundred gaged sites in the State are available for engineering and management purposes. When gaged data are not available, methods for estimating streamflow characteristics are needed. Methods presented in this report for estimating streamflow characteristics have been improved over previous methods through the use of refined analytical techniques and an updated data base. Peak-flow characteristics and mean annual runoff at ungaged sites can be estimated by using regression equations, with either basin characteristics or channel width being independent variables. Log-linear regression equations are used for estimating streamflow characteristics in the mountains; whereas, curvilinear equations of double-exponential form were determined to be more appropriate than log-linear relations for depicting peak flows in the plains and deserts. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884045","usgsCitation":"Lowham, H., 1988, Streamflows in Wyoming: U.S. Geological Survey Water-Resources Investigations Report 88-4045, vi, 84 p. :ill., maps (some col.) ;28 cm., https://doi.org/10.3133/wri884045.","productDescription":"vi, 84 p. :ill., maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":159574,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4045/report-thumb.jpg"},{"id":57256,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4045/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57257,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4045/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4c9b","contributors":{"authors":[{"text":"Lowham, H. W.","contributorId":8111,"corporation":false,"usgs":true,"family":"Lowham","given":"H. W.","affiliations":[],"preferred":false,"id":199828,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20442,"text":"ofr87450N - 1988 - Geologic summary and hydrocarbon plays, Williston Basin, Montana, North and South Dakota, and Sioux Arch, South Dakota and Nebraska, U.S.","interactions":[],"lastModifiedDate":"2012-02-02T00:07:34","indexId":"ofr87450N","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"87-450","chapter":"N","title":"Geologic summary and hydrocarbon plays, Williston Basin, Montana, North and South Dakota, and Sioux Arch, South Dakota and Nebraska, U.S.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87450N","usgsCitation":"Peterson, J.A., 1988, Geologic summary and hydrocarbon plays, Williston Basin, Montana, North and South Dakota, and Sioux Arch, South Dakota and Nebraska, U.S.: U.S. Geological Survey Open-File Report 87-450, ii, 43 leaves :ill., map ;28 cm., https://doi.org/10.3133/ofr87450N.","productDescription":"ii, 43 leaves :ill., map ;28 cm.","costCenters":[],"links":[{"id":152737,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0450n/report-thumb.jpg"},{"id":49983,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0450n/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db68819d","contributors":{"authors":[{"text":"Peterson, James A.","contributorId":106872,"corporation":false,"usgs":true,"family":"Peterson","given":"James","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":182662,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26743,"text":"wri884003 - 1988 - Preliminary evaluation of the hydrogeologic system in Owens Valley, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:38","indexId":"wri884003","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"88-4003","title":"Preliminary evaluation of the hydrogeologic system in Owens Valley, California","docAbstract":"A preliminary, two-layer, steady-state, groundwater flow model was used to evaluate present data and hydrologic concepts of Owens Valley, California. Simulations of the groundwater system indicate that areas where water levels are most affected by changes in recharge and discharge are near toes of alluvial fans and along the edge of permeable volcanic deposits. Sensitivity analysis for each model parameter shows that steady state simulations are most sensitive to uncertainties in evapotranspiration rates. Tungsten Hills, Poverty Hills, and Alabama Hills were found to act as virtually impermeable barriers to groundwater flow. Accurate simulation of the groundwater system between Bishop and Lone Pine appears to be possible without simulating the groundwater system in Round Valley, near Owens Lake, or in aquifer materials more than 1,000 ft below land surface. Although vast amounts of geologic and hydrologic data have been collected for Owens Valley, many parts of the hydrogeologic system have not been defined with sufficient detail to answer present water management questions. Location and extent of geologic materials that impede the vertical movement of water are poorly documented. The likely range of aquifer characteristics, except vertical hydraulic conductivity, is well known, but spatial distribution of these characteristics is not well documented. A set of consistent water budgets is needed, including one for surface water, groundwater, and the entire valley. The largest component of previous water budgets (evapotranspiration) is largely unverified. More definitive estimates of local gains and losses for Owens River are needed. Although groundwater pumpage from each well is measured, the quantity of withdrawal from different zones of permeable material has not been defined. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884003","usgsCitation":"Danskin, W., 1988, Preliminary evaluation of the hydrogeologic system in Owens Valley, California: U.S. Geological Survey Water-Resources Investigations Report 88-4003, v, 76 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri884003.","productDescription":"v, 76 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":158543,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4003/report-thumb.jpg"},{"id":55620,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4003/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c40a","contributors":{"authors":[{"text":"Danskin, W.R. 0000-0001-8672-5501","orcid":"https://orcid.org/0000-0001-8672-5501","contributorId":22713,"corporation":false,"usgs":true,"family":"Danskin","given":"W.R.","affiliations":[],"preferred":false,"id":196923,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26667,"text":"wri844252 - 1988 - Ground-water resources of the Lamprey River basin, southeastern New Hampshire","interactions":[],"lastModifiedDate":"2012-02-02T00:08:30","indexId":"wri844252","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4252","title":"Ground-water resources of the Lamprey River basin, southeastern New Hampshire","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844252","usgsCitation":"Cotton, J.E., 1988, Ground-water resources of the Lamprey River basin, southeastern New Hampshire: U.S. Geological Survey Water-Resources Investigations Report 84-4252, 46 p. :ill., maps (1 col.) ;28 cm., https://doi.org/10.3133/wri844252.","productDescription":"46 p. :ill., maps (1 col.) ;28 cm.","costCenters":[],"links":[{"id":121944,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4252/report-thumb.jpg"},{"id":55533,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4252/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55534,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4252/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a81e","contributors":{"authors":[{"text":"Cotton, J. E.","contributorId":52976,"corporation":false,"usgs":true,"family":"Cotton","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":196798,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3967,"text":"cir1018 - 1988 - Proceedings of the 1987 Exclusive Economic Zone symposium on mapping and research; planning for the next 10 years","interactions":[],"lastModifiedDate":"2012-02-02T00:05:29","indexId":"cir1018","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"1018","title":"Proceedings of the 1987 Exclusive Economic Zone symposium on mapping and research; planning for the next 10 years","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/cir1018","usgsCitation":"Lockwood, M., and McGregor, B.A., 1988, Proceedings of the 1987 Exclusive Economic Zone symposium on mapping and research; planning for the next 10 years: U.S. Geological Survey Circular 1018, iii, 175 p. :ill., maps ;28 cm., https://doi.org/10.3133/cir1018.","productDescription":"iii, 175 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":117580,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1988/1018/report-thumb.jpg"},{"id":31053,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1988/1018/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db6605ab","contributors":{"authors":[{"text":"Lockwood, Millington","contributorId":91843,"corporation":false,"usgs":true,"family":"Lockwood","given":"Millington","email":"","affiliations":[],"preferred":false,"id":147916,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McGregor, Bonnie A.","contributorId":61022,"corporation":false,"usgs":true,"family":"McGregor","given":"Bonnie","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":147915,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4032,"text":"cir996 - 1988 - A modification of the U.S. Geological Survey one-sixth order semiquantitative spectrographic method for the analysis of geologic materials that improves limits of determination of some volatile to moderately volatile elements","interactions":[],"lastModifiedDate":"2012-02-02T00:05:21","indexId":"cir996","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"996","title":"A modification of the U.S. Geological Survey one-sixth order semiquantitative spectrographic method for the analysis of geologic materials that improves limits of determination of some volatile to moderately volatile elements","docAbstract":"A modification of the one-sixth order semi-quantitative emission spectrographic method for the analysis of 30 elements in geologic materials (Grimes and Marranzino 1968) improves the limits of determination of some volatile to moderately volatile elements. The modification uses a compound-pendulum-mounted filter to regulate the amount of emitted light passing into the spectrograph. One hundred percent transmission of emitted light is allowed during the initial 20 seconds of the burn, then continually reduced to 40 percent over the next 32 seconds using the pendulum-mounted filter, and followed by an additional 68 seconds of burn time. The reduction of light transmission during the latter part of the burn decreases spectral background and the line emission of less volatile elements commonly responsible for problem-causing interferences. The sensitivity of the method for some geochemically important trace elements commonly determined in mineral exploration (Ag, As, Au, Be, Bi, Cd, Cr, Cu, Pb, Sb, Sn, and Zn) is improved up to five-fold under ideal conditions without compromising precision or accuracy","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir996","usgsCitation":"Detra, D., and Cooley, E.F., 1988, A modification of the U.S. Geological Survey one-sixth order semiquantitative spectrographic method for the analysis of geologic materials that improves limits of determination of some volatile to moderately volatile elements: U.S. Geological Survey Circular 996, iii, 22 p. :ill. ;26 cm., https://doi.org/10.3133/cir996.","productDescription":"iii, 22 p. :ill. ;26 cm.","costCenters":[],"links":[{"id":124729,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1988/0996/report-thumb.jpg"},{"id":31124,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1988/0996/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adeb8","contributors":{"authors":[{"text":"Detra, D.E.","contributorId":72358,"corporation":false,"usgs":true,"family":"Detra","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":148035,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cooley, Elmo F.","contributorId":71950,"corporation":false,"usgs":true,"family":"Cooley","given":"Elmo","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":148034,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":43344,"text":"ofr88664 - 1988 - Isostatic gravity map of the Nevada Test Site and vicinity, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:04:53","indexId":"ofr88664","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-664","title":"Isostatic gravity map of the Nevada Test Site and vicinity, Nevada","language":"ENGLISH","doi":"10.3133/ofr88664","usgsCitation":"Ponce, D.A., Harris, R., and Oliver, H., 1988, Isostatic gravity map of the Nevada Test Site and vicinity, Nevada: U.S. Geological Survey Open-File Report 88-664, 1 map ;83 x 67 cm., on sheet 107 x 97 cm., folded in envelope 31 x 24 cm., https://doi.org/10.3133/ofr88664.","productDescription":"1 map ;83 x 67 cm., on sheet 107 x 97 cm., folded in envelope 31 x 24 cm.","costCenters":[],"links":[{"id":134947,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81093,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1988/0664/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db6670be","contributors":{"authors":[{"text":"Ponce, David A. 0000-0003-4785-7354 ponce@usgs.gov","orcid":"https://orcid.org/0000-0003-4785-7354","contributorId":1049,"corporation":false,"usgs":true,"family":"Ponce","given":"David","email":"ponce@usgs.gov","middleInitial":"A.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":228070,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harris, Reid N.","contributorId":54568,"corporation":false,"usgs":true,"family":"Harris","given":"Reid N.","affiliations":[],"preferred":false,"id":228071,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Oliver, Howard W.","contributorId":78704,"corporation":false,"usgs":true,"family":"Oliver","given":"Howard W.","affiliations":[],"preferred":false,"id":228072,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":63602,"text":"gp991 - 1988 - Map showing global distribution of moment-tensor focal mechanisms, 1981-1985, prepared by National Earthquake Information Center, World Data Center A for Seismology","interactions":[],"lastModifiedDate":"2022-06-14T19:34:49.582489","indexId":"gp991","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"991","title":"Map showing global distribution of moment-tensor focal mechanisms, 1981-1985, prepared by National Earthquake Information Center, World Data Center A for Seismology","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp991","usgsCitation":"Goter, S., 1988, Map showing global distribution of moment-tensor focal mechanisms, 1981-1985, prepared by National Earthquake Information Center, World Data Center A for Seismology: U.S. Geological Survey Geophysical Investigations Map 991, Report: 1 p.; 1 Plate: 44.51 × 27.42 inches, https://doi.org/10.3133/gp991.","productDescription":"Report: 1 p.; 1 Plate: 44.51 × 27.42 inches","costCenters":[],"links":[{"id":249793,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0991/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":402166,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6340.htm"},{"id":253303,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0991/report-thumb.jpg"},{"id":249794,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0991/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"40000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688040","contributors":{"authors":[{"text":"Goter, S.K.","contributorId":70856,"corporation":false,"usgs":true,"family":"Goter","given":"S.K.","affiliations":[],"preferred":false,"id":269206,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28944,"text":"wri884041 - 1988 - Estimating flood hydrographs and volumes for Alabama streams","interactions":[],"lastModifiedDate":"2012-02-02T00:08:37","indexId":"wri884041","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"88-4041","title":"Estimating flood hydrographs and volumes for Alabama streams","docAbstract":"The hydraulic design of highway drainage structures involves an evaluation of the effect of the proposed highway structures on lives, property, and stream stability. Flood hydrographs and associated flood volumes are useful tools in evaluating these effects. For design purposes, the Alabama Highway Department needs information on flood hydrographs and volumes associated with flood peaks of specific recurrence intervals (design floods) at proposed or existing bridge crossings. This report will provide the engineer with a method to estimate flood hydrographs, volumes, and lagtimes for rural and urban streams in Alabama with drainage areas less than 500 sq mi. Existing computer programs and methods to estimate flood hydrographs and volumes for ungaged streams have been developed in Georgia. These computer programs and methods were applied to streams in Alabama. The report gives detailed instructions on how to estimate flood hydrographs for ungaged rural or urban streams in Alabama with drainage areas less than 500 sq mi, without significant in-channel storage or regulations. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884041","usgsCitation":"Olin, D., and Atkins, J., 1988, Estimating flood hydrographs and volumes for Alabama streams: U.S. Geological Survey Water-Resources Investigations Report 88-4041, v, 25 p. :ill., map ;28 cm., https://doi.org/10.3133/wri884041.","productDescription":"v, 25 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":120141,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4041/report-thumb.jpg"},{"id":57820,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4041/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc98d","contributors":{"authors":[{"text":"Olin, D.A.","contributorId":106905,"corporation":false,"usgs":true,"family":"Olin","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":200658,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Atkins, J.B.","contributorId":63842,"corporation":false,"usgs":true,"family":"Atkins","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":200657,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26750,"text":"wri874268 - 1988 - Geohydrology and digital simulation of the ground-water flow system in the Umatilla Plateau and Horse Heaven Hills area, Oregon and Washington","interactions":[],"lastModifiedDate":"2017-02-07T08:20:36","indexId":"wri874268","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4268","title":"Geohydrology and digital simulation of the ground-water flow system in the Umatilla Plateau and Horse Heaven Hills area, Oregon and Washington","docAbstract":"The Columbia Plateau is underlain by massive basalt flows, with a composite thickness of about 10,000 ft. Structural features within the study area include a series of anticline-syncline pairs. The main avenues of groundwater movement in the basalt are the interflow zone between basalt flows. Individual interflow zones may be rather extensive in the lateral direction and are largely isolated from overlying and underlying interflows by poorly permeable basalt flow centers. Four aquifers were defined for this study. The uppermost aquifer (layer 1) consists of unconsolidated deposits of gravel, sand, silt, and clay that overlie the basalt: layer 2 consists of the Saddle Mountains Basalt, layer 3 the Wanapum Basalt, and layer 4 consists of the upper thousand ft of Grande Ronde Basalt. Recharge to the groundwater system is from precipitation, leakage from streams, and seepage from surface water irrigation. Natural discharge of aquifers is principally to streams. Discharge by groundwater pumpage from the study area ranged from approximately 2,000 acre-ft in 1950 to 144,000 acre-ft in 1980. About 85% of the total pumpage in 1980 was from the Oregon part of the study area. Water level declines of over 300 ft occur locally in parts of the study area. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874268","usgsCitation":"Davies-Smith, A., Bolke, E., and Collins, C.A., 1988, Geohydrology and digital simulation of the ground-water flow system in the Umatilla Plateau and Horse Heaven Hills area, Oregon and Washington: U.S. Geological Survey Water-Resources Investigations Report 87-4268, v, 72 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874268.","productDescription":"v, 72 p. :ill., maps ;28 cm.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":123773,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4268/report-thumb.jpg"},{"id":55626,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4268/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8d63","contributors":{"authors":[{"text":"Davies-Smith, A.","contributorId":23180,"corporation":false,"usgs":true,"family":"Davies-Smith","given":"A.","email":"","affiliations":[],"preferred":false,"id":196935,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bolke, E.L.","contributorId":52151,"corporation":false,"usgs":true,"family":"Bolke","given":"E.L.","affiliations":[],"preferred":false,"id":196937,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Collins, C. A.","contributorId":43731,"corporation":false,"usgs":true,"family":"Collins","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":196936,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":3808,"text":"cir1021 - 1988 - Concepts for a National Water-Quality Assessment Program","interactions":[],"lastModifiedDate":"2012-02-02T00:05:41","indexId":"cir1021","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"1021","title":"Concepts for a National Water-Quality Assessment Program","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/cir1021","usgsCitation":"Hirsch, R.M., Alley, W., and Wilber, W.G., 1988, Concepts for a National Water-Quality Assessment Program: U.S. Geological Survey Circular 1021, vii, 42 p. :ill., maps ;28 cm., https://doi.org/10.3133/cir1021.","productDescription":"vii, 42 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":118100,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1988/1021/report-thumb.jpg"},{"id":30878,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1988/1021/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a488c","contributors":{"authors":[{"text":"Hirsch, Robert M. 0000-0002-4534-075X rhirsch@usgs.gov","orcid":"https://orcid.org/0000-0002-4534-075X","contributorId":2005,"corporation":false,"usgs":true,"family":"Hirsch","given":"Robert","email":"rhirsch@usgs.gov","middleInitial":"M.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":502,"text":"Office of Surface Water","active":true,"usgs":true},{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true},{"id":37316,"text":"WMA - Integrated Information Dissemination Division","active":true,"usgs":true}],"preferred":true,"id":147643,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Alley, William M.","contributorId":93030,"corporation":false,"usgs":true,"family":"Alley","given":"William M.","affiliations":[],"preferred":false,"id":147644,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wilber, William G. wgwilber@usgs.gov","contributorId":297,"corporation":false,"usgs":true,"family":"Wilber","given":"William","email":"wgwilber@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":147642,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":3422,"text":"cir1004 - 1988 - Estimated Use of Water in the United States in 1985","interactions":[],"lastModifiedDate":"2012-02-02T00:05:38","indexId":"cir1004","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"1004","title":"Estimated Use of Water in the United States in 1985","docAbstract":"Water withdrawals in the United States during 1985 were estimated to average 399,000 million gallons per day (Mgal/d) of freshwater and saline water for offstream uses--10 percent less than the 1980 estimate. Average per-capita use for all offstream uses was 1,650 gallons per day (gal/d) of freshwater and saline water combined and 1,400 gal/d of freshwater alone. \r\n\r\nOffstream water-use categories are classified in this report as public supply, domestic, commercial, irrigation, livestock, industrial, mining, and thermoelectric power. During 1985, public-supply withdrawals were estimated to be 36,500 Mgal/d, and self-supplied withdrawals were estimated as follows: domestic, 3,320 Mgal/d: commercial, 1,230 Mgal/d; irrigation, 137,000 Mgal/d: livestock, 4,470 Mgal/d; industrial, 25,800 Mgal/d; mining, 3,440 Mgal/d; and thermoelectric power, 187,000 Mgal/d. \r\n\r\nWater use for hydroelectric power generation, the only instream use compiled in this report, was estimated to be 3,050,000 Mgal/d during 1985, or 7 percent less than during 1980. This is in contrast to an increasing trend that persisted from 1950 to 1980. \r\n\r\nEstimates of withdrawals by source indicate that, during 1985, total surface-water withdrawals were 325,000 Mgal/d, or 10 percent less than during 1980, and total ground-water withdrawals were 74,000 Mgal/d, or 12 percent less than during 1980. Total saline-water withdrawals during 1985 were 60,300 Mgal/d, or 16 percent less than during 1980; most was saline surface water. Reclaimed sewage averaged about 579 Mgal/d during 1985, or 22 percent more than during 1980. \r\n\r\nTotal freshwater consumptive use was estimated to be 92,300 Mgal/d during 1985, or 9 percent less than during 1980. Consumptive use by irrigation accounted for the largest part of consumptive use during 1985 and was estimated to be 73,800 Mgal/d. \r\n\r\nA comparison of total withdrawals (fresh and saline) by State indicates that 37 States and Puerto Rico had less water withdrawn for offstream uses during 1985 than during 1980. California accounted for the most water withdrawn for offstream use, 49,700 Mgal/d, more than double the water withdrawn in either Texas or Idaho, the next largest users. A similar comparison by water-resources regions indicates that the California and the South Atlantic-Gulf regions accounted for nearly one-quarter of the total water withdrawn in the United States. Total withdrawals for offstream use in the eastern water-resources regions, which include the Mississippi and Souris Rivers, accounted for 53 percent of the Nation's total withdrawals, compared to 55 percent during 1980. Freshwater consumptive use in the East was about 11 percent of the freshwater withdrawn in the East and accounted for only 21 percent of the Nation's total freshwater consumptive use. By comparison, freshwater consumptive use in the West was about 41 percent of the freshwater withdrawn in the West. \r\n\r\nThe 1985 estimates of total water withdrawals and consumptive use were less than the 1980 estimates; this apparently further confirms a general trend indicated by a slackening in the rate of increase of total withdrawals from 1970 to 1975 and again from 1975 to 1980. Public-supply withdrawals during 1985 were 7 percent more than during 1980, \r\nself-supplied domestic withdrawals were 4 percent less, irrigation withdrawals were 6 \r\npercent less, livestock withdrawals were 108 percent more, and thermoelectric power \r\nWithdrawals were 13 percent less. The combined total for self-supplied industrial, commercial, and mining withdrawals (excluding thermoelectric power) was 30,500 Mgal/d \r\nduring 1985, or 33 percent less than withdrawals listed for 'other' industries during \r\n1980, which also included commercial and mining uses.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/cir1004","usgsCitation":"Solley, W.B., Merk, C.F., and Pierce, R.R., 1988, Estimated Use of Water in the United States in 1985: U.S. Geological Survey Circular 1004, viii, 82 p., https://doi.org/10.3133/cir1004.","productDescription":"viii, 82 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":124374,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1988/1004/report-thumb.jpg"},{"id":30437,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1988/1004/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b31e4b07f02db6b41a8","contributors":{"authors":[{"text":"Solley, Wayne B.","contributorId":61409,"corporation":false,"usgs":true,"family":"Solley","given":"Wayne","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":146876,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Merk, Charles F.","contributorId":44503,"corporation":false,"usgs":true,"family":"Merk","given":"Charles","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":146875,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pierce, Robert R.","contributorId":62578,"corporation":false,"usgs":true,"family":"Pierce","given":"Robert","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":146877,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
]}