{"pageNumber":"330","pageRowStart":"8225","pageSize":"25","recordCount":11004,"records":[{"id":16239,"text":"ofr88195 - 1988 - Selected hydrologic data for Pahvant Valley and adjacent areas, Millard County, Utah, 1987","interactions":[],"lastModifiedDate":"2017-08-31T16:02:47","indexId":"ofr88195","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":"88-195","title":"Selected hydrologic data for Pahvant Valley and adjacent areas, Millard County, Utah, 1987","docAbstract":"<p>This report contains hydrologic data collected in Pahvant Valley and adjacent areas from 1909 to 1987. The report area is mainly comprised of Pahvant Valley on the east and the southern part of the Sevier Desert on the west (plate 1). The area is in west-central Utah, within the Basin and Range physiographic province, and includes about 1,600 square miles. </p><p>Most of the data in this report were collected by the U.S. Geological Survey in cooperation with the Utah Department of Natural Resources, Division of Water Rights, from 1985 to 1987. Some of the earlier data were previously published by Enright and Holmes (1982), Meinzer (1911), Mower (1963 and 1967), and Mundorff (1970). </p><p>The purpose of this report is to provide hydrologic data for use by the general public and by officials managing the area's water resources, and to supplement interpretive reports for the area. Tables 1 to 6 contain information about wells including well completions, drillers' logs, water levels, flowing-well discharges, and chemical quality. Spring and surfacewater site data are listed in tables 7 to 9. Hydrologic-data sites are shown on plate 1. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/ofr88195","collaboration":"Prepared in cooperation with the Utah Department of Natural Resources","usgsCitation":"Thiros, S.A., 1988, Selected hydrologic data for Pahvant Valley and adjacent areas, Millard County, Utah, 1987: U.S. Geological Survey Open-File Report 88-195, Report: iv, 151 p.; Plate: 23.06 in. x 23.37 in., https://doi.org/10.3133/ofr88195.","productDescription":"Report: iv, 151 p.; Plate: 23.06 in. x 23.37 in.","numberOfPages":"154","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":148918,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0195/report-thumb.jpg"},{"id":45160,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1988/0195/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45161,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0195/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","county":"Millard County","otherGeospatial":"Pahvant 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Susan A. 0000-0002-8544-553X sthiros@usgs.gov","orcid":"https://orcid.org/0000-0002-8544-553X","contributorId":965,"corporation":false,"usgs":true,"family":"Thiros","given":"Susan","email":"sthiros@usgs.gov","middleInitial":"A.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":172472,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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}]}}
,{"id":59598,"text":"mf1818 - 1988 - Interpretive aeromagnetic map of the Eagle Mountains Wilderness Study Area, Riverside County, California","interactions":[],"lastModifiedDate":"2016-08-22T10:47:29","indexId":"mf1818","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1818","title":"Interpretive aeromagnetic map of the Eagle Mountains Wilderness Study Area, Riverside County, California","docAbstract":"<p>This report describes the interpretation of aeromagnetic surveys of the Eagle Mountains area, concentrating on the Eagle Mountains Wilderness Study Area (WSA). The interpretations are based on correlations with mapped surface geology by R. E. Powell, reproduced here from Powell and others (1984), as a base for the aeromagnetic data.</p>\n<p>The Eagle Mountains Wilderness Study Area consists of about 49,723 acres in the southeastern and east-central part of the Eagle Mountains, Riverside County, California, just north of Interstate 10 about 170 mi east-southeast of Los Angeles. The western boundary of the WSA abuts Joshua Tree National Monument, the northern boundary skirts the Eagle Mountains mining district, and parts of the southern and eastern boundaries follow the Colorado River aqueduct. Principal access to the interior of the WSA is provided by jeep trails in Big Wash and an unnamed, major north-draining wash in the western part of the study area.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1818","usgsCitation":"Grauch, V.J., 1988, Interpretive aeromagnetic map of the Eagle Mountains Wilderness Study Area, Riverside County, California: U.S. Geological Survey Miscellaneous Field Studies Map 1818, Plate: 31.75 x 39.66 inches, https://doi.org/10.3133/mf1818.","productDescription":"Plate: 31.75 x 39.66 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":326178,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1818.JPG"},{"id":327236,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1818/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"California","county":"Riverside County","otherGeospatial":"Eagle Mountains Wilderness Study Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -115.75,33.666666666666664 ], [ -115.75,33.916666666666664 ], [ -115.41666666666667,33.916666666666664 ], [ -115.41666666666667,33.666666666666664 ], [ -115.75,33.666666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d9e4b07f02db5dfe2e","contributors":{"authors":[{"text":"Grauch, V. J. S. 0000-0002-0761-3489","orcid":"https://orcid.org/0000-0002-0761-3489","contributorId":34125,"corporation":false,"usgs":true,"family":"Grauch","given":"V.","email":"","middleInitial":"J. S.","affiliations":[],"preferred":false,"id":262292,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61564,"text":"mf1594E - 1988 - Mines, prospects, and mineral sites, wilderness and RARE II areas, White Mountain National Forest, New Hampshire","interactions":[],"lastModifiedDate":"2016-08-23T10:41:18","indexId":"mf1594E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1594-E","title":"Mines, prospects, and mineral sites, wilderness and RARE II areas, White Mountain National Forest, New Hampshire","docAbstract":"<p><span>The Wilderness Act (Public Law 88-577, September 3, 1964) and related acts require the U.S. Geological Survey and the U.S. Bureau of Mines to survey certain areas on Federal lands to determine their mineral value, if any, that may be present. Results must be made available to the public and be submitted to the President&nbsp;and the Congress. This report presents the results of investigations of mines, prospects, and mineral sites in the Great Gulf and Presidential Range-Dry River Wilderness Areas; the Dartmouth Range, Wild River, Pemigewasset, Kinsman Mountain, Mount Wolf-Gordon Pond, Jobildunk, and Carr Mountain Roadless Areas; and the intervening and immediately surrounding areas in the White Mountain National Forest, Coos, Grafton, and Carroll Counties, New Hampshire. The Great Gulf Wilderness&nbsp;was established when the Wilderness Act was passed in 1964, and the Presidential Range-Dry River Wilderness was established by Public Law 93-622, January 3, 1975. The&nbsp;Dartmouth Range, Wild River, Pemigewasset, Kinsman Mountain, Mount Wolf-Gordon Pond,&nbsp;Carr Mountain, and Jobildunk areas were classified&nbsp;as a further planning area during the Second Roadless Area Review and Evaluation (RARE II) by the U.S. Forest Service, January 1979.</span></p>\n<p>The areas investigated are located in the&nbsp;White Mountain National Forest in Coos, Grafton, and Carroll Counties, New Hampshire. Personnel from the U.S. Bureau of Mines conducted field reconnaissance of the westernmost areas, Kinsman Mountain, Mt. Wolf-Gordon Pond, Jobildunk, and Carr Mountain, in the fall of 1980. Field reconnaissance of the eastern areas, Great Gulf, Presidential Range-Dry River, Dartmouth Range, Pemigewasset and Wild River was conducted in the spring of 1981. A total of 237 rock and 103 panned-concentrate samples were collected during the investigations. Reconnaissance radiometric ground surveys were conducted at selected locations.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1594E","usgsCitation":"Gazdik, G.C., Harris, G., Welsh, R.A., and Girol, V.P., 1988, Mines, prospects, and mineral sites, wilderness and RARE II areas, White Mountain National Forest, New Hampshire: U.S. Geological Survey Miscellaneous Field Studies Map 1594-E, 2 Plates: 54.42 x 39.82 inches and 22.71 x 28.02 inches, https://doi.org/10.3133/mf1594E.","productDescription":"2 Plates: 54.42 x 39.82 inches and 22.71 x 28.02 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":326382,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1594E.PNG"},{"id":327604,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1594-E/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":327605,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1594-E/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"125000","country":"United States","state":"New Hampshire","county":"Carroll County, Coos County, Grafton County","otherGeospatial":"White Mountain National Forest","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -72,\n              43.75\n            ],\n            [\n              -72,\n              44.75\n            ],\n            [\n              -70.75,\n              44.75\n            ],\n            [\n              -70.75,\n              43.75\n            ],\n            [\n              -72,\n              43.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699d5f","contributors":{"authors":[{"text":"Gazdik, G. 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,{"id":27106,"text":"wri874034 - 1988 - Hydrogeology, aquifer characteristics, and ground-water flow of the surficial aquifer system, Broward County, Florida","interactions":[],"lastModifiedDate":"2022-01-10T12:39:00.489015","indexId":"wri874034","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":"87-4034","title":"Hydrogeology, aquifer characteristics, and ground-water flow of the surficial aquifer system, Broward County, Florida","docAbstract":"The surficial aquifer system, in which an unconfined groundwater flow system exists, comprises the sediments from land surface to the intermediate confining unit (formerly called the Floridan aquiclude) in Broward County, Florida. These sediments have hydraulic conductivities that range more than seven orders of magnitude from about 0.001 ft/d to more than 10,000 ft/d. The sediments are grouped into (1) the Biscayne aquifer, (2) a semiconfining unit, (3) a gray limestone aquifer in west Broward County, and (4) basal sand or clayey sand. The system is about 160 ft thick in west Broward County and more than 350 ft thick in east Broward. Transmissivities, locally variable, show a clear areal trend from greater than 300,000 sq ft/day in southeast Broward County to less than 75,000 sq ft/day in the northwest part of the county. Very high transmissivity is associated with the Biscayne aquifer. Transmissivity of the gray limestone aquifer ranged from about 20,000 to 88,000 sq ft/day. Topography, water levels, geologic framework, and water quality in west Broward County suggest past and present groundwater movement is south or southeast. Drainage and urban development have greatly altered circulation patterns in east Broward County , eliminating the original coastal groundwater ridge, causing rapid surface runoff and short groundwater flow paths, and saltwater intrusion. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri874034","collaboration":"Prepared in cooperation with the South Florida Water Management District","usgsCitation":"Fish, J., 1988, Hydrogeology, aquifer characteristics, and ground-water flow of the surficial aquifer system, Broward County, Florida: U.S. Geological Survey Water-Resources Investigations Report 87-4034, vi, 92 p., https://doi.org/10.3133/wri874034.","productDescription":"vi, 92 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science 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href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db6148c9","contributors":{"authors":[{"text":"Fish, J.E.","contributorId":101658,"corporation":false,"usgs":true,"family":"Fish","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":197561,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":59059,"text":"mf1999 - 1988 - Mineral resources and resource potential map of the Pyramid Peak Roadless Area, Riverside County, California","interactions":[],"lastModifiedDate":"2025-05-28T16:41:49.055241","indexId":"mf1999","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1999","title":"Mineral resources and resource potential map of the Pyramid Peak Roadless Area, Riverside County, California","docAbstract":"<p>The Pyramid Peak Roadless Area is underlain by mid-Cretaceous plutonic rocks (granite, granodiorite, and tonalite) that intrude metasedimentary rocks of the Desert Divide Group. The granodiorite grades eastward into strongly deformed mylonitic rocks mapped as part of the Santa Rosa mylonite zone. Metasedimentary rocks, orthogneiss, and anatexites of the Palm Canyon Complex were displaced westward over the Santa Rosa mylonite zone along low-angle thrust faults that are nearly synchronous with the mylonite zone. The Pliocene and (or) Pleistocene Bautista Formation unconformably overlies the mid-Cretaceous plutonic rocks.</p>\n<p>Geologic and geochemical data indicate that the study area has high resource potential for marble, and moderate resource potential for epithermal gold deposits and tungsten skarns. The Desert Divide Group and the Palm Canyon Complex contain large resources of marble quarried for Portland cement and for construction applications. Gold occurs in quartz veins and pegmatites in the Desert Divide Group and the Penrod Quartz Monzonite. Skarns in the Desert Divide Group contain scheelite and anomalous concentrations of arsenic and beryllium. Thin layers of tremolite asbestos along low-angle thrust faults occur outside of the study area.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1999","usgsCitation":"Calzia, J., 1988, Mineral resources and resource potential map of the Pyramid Peak Roadless Area, Riverside County, California: U.S. Geological Survey Miscellaneous Field Studies Map 1999, 1 Plate: 28.18 x 25.27 inches, https://doi.org/10.3133/mf1999.","productDescription":"1 Plate: 28.18 x 25.27 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":486650,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5592.htm","linkFileType":{"id":5,"text":"html"}},{"id":327173,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1999/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":182642,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1999.PNG"}],"country":"United States","state":"California","county":"Riverside County","otherGeospatial":"Pyramid Peak Roadless Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.61666666666666,33.55 ], [ -116.61666666666666,33.71666666666667 ], [ -116.41666666666667,33.71666666666667 ], [ -116.41666666666667,33.55 ], [ -116.61666666666666,33.55 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b08e4b07f02db69b9ab","contributors":{"authors":[{"text":"Calzia, J.P.","contributorId":58614,"corporation":false,"usgs":true,"family":"Calzia","given":"J.P.","affiliations":[],"preferred":false,"id":261344,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57329,"text":"wdrVA871 - 1988 - Water resources data for Virginia, water year 1987","interactions":[],"lastModifiedDate":"2020-11-25T19:44:50.732637","indexId":"wdrVA871","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"VA-87-1","title":"Water resources data for Virginia, water year 1987","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrVA871","usgsCitation":"Prugh, B., Easton, F., and Lynch, D.D., 1988, Water resources data for Virginia, water year 1987: U.S. Geological Survey Water Data Report VA-87-1, xiv, 441 p., https://doi.org/10.3133/wdrVA871.","productDescription":"xiv, 441 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc80d","contributors":{"authors":[{"text":"Prugh, B.J.","contributorId":88811,"corporation":false,"usgs":true,"family":"Prugh","given":"B.J.","affiliations":[],"preferred":false,"id":256726,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Easton, F.J.","contributorId":61096,"corporation":false,"usgs":true,"family":"Easton","given":"F.J.","email":"","affiliations":[],"preferred":false,"id":256725,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lynch, D. D.","contributorId":12075,"corporation":false,"usgs":true,"family":"Lynch","given":"D.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":256724,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"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":34107,"text":"b1762 - 1988 - Geochemistry of mineralized quartzite beds in the Spokane Formation (Belt Supergroup), Rogers Pass area, Lewis and Clark County, Montana","interactions":[],"lastModifiedDate":"2022-11-03T18:49:58.4724","indexId":"b1762","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"1762","title":"Geochemistry of mineralized quartzite beds in the Spokane Formation (Belt Supergroup), Rogers Pass area, Lewis and Clark County, Montana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1762","usgsCitation":"Connor, J.J., and McNeal, J.M., 1988, Geochemistry of mineralized quartzite beds in the Spokane Formation (Belt Supergroup), Rogers Pass area, Lewis and Clark County, Montana: U.S. Geological Survey Bulletin 1762, iii, 17 p., https://doi.org/10.3133/b1762.","productDescription":"iii, 17 p.","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":409124,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21893.htm","linkFileType":{"id":5,"text":"html"}},{"id":164132,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1762/report-thumb.jpg"},{"id":62029,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1762/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Montana","county":"Lewis and Clark County","otherGeospatial":"Rogers Pass area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -112.475,\n              47.8\n            ],\n            [\n              -112.475,\n              47.02\n            ],\n            [\n              -112.361,\n              47.02\n            ],\n            [\n              -112.361,\n              47.8\n            ],\n            [\n              -112.475,\n              47.8\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6aab45","contributors":{"authors":[{"text":"Connor, Jon J.","contributorId":21948,"corporation":false,"usgs":true,"family":"Connor","given":"Jon","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":212465,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McNeal, James M. jmcneal@usgs.gov","contributorId":2810,"corporation":false,"usgs":true,"family":"McNeal","given":"James","email":"jmcneal@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":212464,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":12138,"text":"ofr88344 - 1988 - Location maps and list of U.S. Geological Survey reports on water resources in Alaska, 1950 to 1988","interactions":[{"subject":{"id":12138,"text":"ofr88344 - 1988 - Location maps and list of U.S. Geological Survey reports on water resources in Alaska, 1950 to 1988","indexId":"ofr88344","publicationYear":"1988","noYear":false,"title":"Location maps and list of U.S. Geological Survey reports on water resources in Alaska, 1950 to 1988"},"predicate":"SUPERSEDED_BY","object":{"id":17308,"text":"ofr9160 - 1991 - Location maps and list of U.S. Geological Survey reports on water resources in Alaska 1950 to 1990","indexId":"ofr9160","publicationYear":"1991","noYear":false,"title":"Location maps and list of U.S. Geological Survey reports on water resources in Alaska 1950 to 1990"},"id":1}],"supersededBy":{"id":17308,"text":"ofr9160 - 1991 - Location maps and list of U.S. Geological Survey reports on water resources in Alaska 1950 to 1990","indexId":"ofr9160","publicationYear":"1991","noYear":false,"title":"Location maps and list of U.S. Geological Survey reports on water resources in Alaska 1950 to 1990"},"lastModifiedDate":"2023-08-08T22:12:55.946273","indexId":"ofr88344","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":"88-344","title":"Location maps and list of U.S. Geological Survey reports on water resources in Alaska, 1950 to 1988","docAbstract":"<p>The objective of this compilation is to provide a listing of water-resources reports in Alaska by location. For the purposes of this report, Alaska has been divided into six geographic sections: Arctic Slope, West, Southwest, East-Central, Southcentral, and Southeast. In addition, reports are cited in the following categories: Statewide and Topical, Trans-Alaska Pipeline System, and Glaciers. The Statewide and Topical reports are not located on maps. The index to the location maps is on the facing page. The numbers on the location maps refer to the bibliographic citations. (Gaps have been left in the numbering system for additional reports in future editions of this compilation.)</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr88344","usgsCitation":"1988, Location maps and list of U.S. Geological Survey reports on water resources in Alaska, 1950 to 1988: U.S. Geological Survey Open-File Report 88-344, iv, 35 p., https://doi.org/10.3133/ofr88344.","productDescription":"iv, 35 p.","costCenters":[],"links":[{"id":419620,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0344/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":146524,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0344/report-thumb.jpg"}],"country":"United 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,{"id":39793,"text":"b1713D - 1988 - Mineral resources of the Whipple Mountains and Whipple Mountains Addition Wilderness Study Areas, San Bernardino County, California","interactions":[{"subject":{"id":7331,"text":"ofr82956 - 1982 - Mineral-resource potential of the Whipple Mountains Wilderness Study Area(CDCA-312), San Bernardino County, California","indexId":"ofr82956","publicationYear":"1982","noYear":false,"title":"Mineral-resource potential of the Whipple Mountains Wilderness Study Area(CDCA-312), San Bernardino County, California"},"predicate":"SUPERSEDED_BY","object":{"id":39793,"text":"b1713D - 1988 - Mineral resources of the Whipple Mountains and Whipple Mountains Addition Wilderness Study Areas, San Bernardino County, California","indexId":"b1713D","publicationYear":"1988","noYear":false,"chapter":"D","title":"Mineral resources of the Whipple Mountains and Whipple Mountains Addition Wilderness Study Areas, San Bernardino County, California"},"id":1}],"lastModifiedDate":"2017-07-05T12:49:41","indexId":"b1713D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"1713","chapter":"D","title":"Mineral resources of the Whipple Mountains and Whipple Mountains Addition Wilderness Study Areas, San Bernardino County, California","docAbstract":"<p>At the request of the U.S. Bureau of Land Management, approximately 85,100 acres of the Whipple Mountains Wilderness Study Area (CDCA-312) and 1,380 acres of the Whipple Mountains Addition Wilderness Study Area (AZ-050-010) were evaluated for identified mineral resources (known) and mineral resource potential (undiscovered). In this report, the Whipple Mountains and Whipple Mountains Addition Wilderness Study Areas are referred to as simply \"the study area.\" </p><p>Most of the mines and prospects with identified resources in the Whipple Mountains Wilderness Study Area are within areas designated as having mineral resource potential. The area in and around the Turk Silver mine and the Lucky Green group and the area near the northwest boundary of the study area have high mineral resource potential for copper, lead, zinc, gold, and silver. An area along the west boundary of the study area has moderate resource potential for copper lead, zinc, gold, and silver. An area in the east adjacent to the Whipple Mountains Addition Wilderness Study Area has moderate resource potential for copper, gold, and silver resources. One area on the north boundary and one on the southeast boundary of the study area have low mineral resource potential for copper, lead, zinc, gold, and silver. Two areas, one on the north boundary and one inside the east boundary of the study area, have moderate resource potential for manganese. A small area inside the south boundary of the study area has high resource potential for decorative building stone, and the entire study area has low resource potential for&nbsp;sand and gravel and other rock products suitable for construction. Two areas in the eastern part of the study area have low resource potential for uranium. There is no resource potential for oil and gas or geothermal resources in the Whipple Mountains Wilderness Study Area. </p><p>Sites within the Whipple Mountains Wilderness Study Area with identified resources of copper, gold, silver, manganese and (or) decorative building stone are located at the Stewart mine, New American Eagle mine, Turk Silver mine, Twin Lode mine, decorative stone property, Lucky Green group, Blue Cloud mine, Nickel Plate mine, Crescent mine, Quadrangle Copper group, and the Copper Basin mine. </p><p>The Whipple Mountains Addition Wilderness Study Area has moderate resource potential for copper, gold, and silver resources and low resource potential for sand and gravel and other rock products. There is no resource potential for oil and gas or for geothermal energy in the Whipple Mountains Addition Wilderness Study Area. </p><p>Although there are no identified resources in the Whipple Mountains Addition Wilderness Study Area, sites within and immediately adjacent warrant further study because of gold assays from widespread, numerous samples.</p>","largerWorkTitle":"Mineral resources of Wilderness Study Areas: Eastern California Desert Conservation Area","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/b1713D","usgsCitation":"Marsh, S.P., Raines, G.L., Diggles, M.F., Howard, K.A., Simpson, R.W., Hoover, D.B., Ridenour, J., Moyle, P.R., and Willett, S.L., 1988, Mineral resources of the Whipple Mountains and Whipple Mountains Addition Wilderness Study Areas, San Bernardino County, California: U.S. Geological Survey Bulletin 1713, Report: vi, 36 p.; Plate: 36.50 x 25.00 inches, https://doi.org/10.3133/b1713D.","productDescription":"Report: vi, 36 p.; Plate: 36.50 x 25.00 inches","startPage":"D1","endPage":"D36","costCenters":[],"links":[{"id":67672,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1713d/report.pdf","text":"Report","size":"2.02 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":173394,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1713d/report-thumb.jpg"},{"id":67671,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1713d/plate-1.pdf","text":"Plate","size":"5.14 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate"}],"country":"United States","state":"California","county":"San Bernardino County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.378662109375,\n              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P.","contributorId":42950,"corporation":false,"usgs":true,"family":"Marsh","given":"Sherman","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":222190,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Raines, Gary L.","contributorId":48162,"corporation":false,"usgs":true,"family":"Raines","given":"Gary","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":222194,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Diggles, Michael F. 0000-0002-9946-0247 mdiggles@usgs.gov","orcid":"https://orcid.org/0000-0002-9946-0247","contributorId":810,"corporation":false,"usgs":true,"family":"Diggles","given":"Michael","email":"mdiggles@usgs.gov","middleInitial":"F.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":501,"text":"Office of Science Quality and Integrity","active":true,"usgs":true},{"id":5053,"text":"IPDS Training","active":true,"usgs":true},{"id":5066,"text":"Office of the Director USGS","active":true,"usgs":true}],"preferred":true,"id":222189,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Howard, Keith A. 0000-0002-6462-2947 khoward@usgs.gov","orcid":"https://orcid.org/0000-0002-6462-2947","contributorId":3439,"corporation":false,"usgs":true,"family":"Howard","given":"Keith","email":"khoward@usgs.gov","middleInitial":"A.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":222191,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Simpson, Robert W. simpson@usgs.gov","contributorId":1053,"corporation":false,"usgs":true,"family":"Simpson","given":"Robert","email":"simpson@usgs.gov","middleInitial":"W.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":222192,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hoover, Donald B.","contributorId":89877,"corporation":false,"usgs":true,"family":"Hoover","given":"Donald","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":222188,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Ridenour, James","contributorId":87540,"corporation":false,"usgs":true,"family":"Ridenour","given":"James","email":"","affiliations":[],"preferred":false,"id":222193,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Moyle, Phillip R.","contributorId":100898,"corporation":false,"usgs":true,"family":"Moyle","given":"Phillip","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":222187,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Willett, Spencee L.","contributorId":48621,"corporation":false,"usgs":true,"family":"Willett","given":"Spencee","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":222195,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":13327,"text":"ofr88119 - 1988 - U.S. Geological Survey ground-water studies in Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:06:52","indexId":"ofr88119","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":"88-119","title":"U.S. Geological Survey ground-water studies in Nevada","docAbstract":"Groundwater is an important natural resource in Nevada. In 1985, groundwater provided 24% of the total water withdrawn, and supplied about 40% of the State 's population. Public supply and self-supplied domestic use accounted for about 12% of the groundwater withdrawn, and self-supplied industrial and mining use was about 3%. The major issues related to groundwater in Nevada are: groundwater availability; natural and artificial groundwater recharge; underground storage of hazardous wastes; organic and inorganic trace constituents in groundwater; and geothermal groundwater systems. The U.S. Geological Survey (USGS) is actively conducting 30 hydrologic investigations in Nevada, of which 18 are related to groundwater quantity and quality. Three examples of ongoing groundwater studies by the USGS that are designed to address specific groundwater issues in Nevada are discussed: carbonate-rock aquifers in eastern and southern Nevada; groundwater quality in the Carson River basin, Nevada-California; and groundwater in Honey Lake Valley, Nevada-California. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88119","usgsCitation":"Dettinger, M.D., and Van Denburgh, A.S., 1988, U.S. Geological Survey ground-water studies in Nevada: U.S. Geological Survey Open-File Report 88-119, 2 p. :map ;28 cm., https://doi.org/10.3133/ofr88119.","productDescription":"2 p. :map ;28 cm.","costCenters":[],"links":[{"id":147395,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0119/report-thumb.jpg"},{"id":41753,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0119/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ae4b07f02db612817","contributors":{"authors":[{"text":"Dettinger, M. D. 0000-0002-7509-7332","orcid":"https://orcid.org/0000-0002-7509-7332","contributorId":93069,"corporation":false,"usgs":false,"family":"Dettinger","given":"M.","middleInitial":"D.","affiliations":[{"id":16196,"text":"Scripps Institution of Oceanography, La Jolla, CA","active":true,"usgs":false}],"preferred":false,"id":167626,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Van Denburgh, A. S.","contributorId":23928,"corporation":false,"usgs":true,"family":"Van Denburgh","given":"A.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":167625,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38436,"text":"pp1404C - 1988 - Hydrogeologic framework of the Virginia coastal plain","interactions":[{"subject":{"id":10306,"text":"ofr84728 - 1984 - Hydrogeologic framework of the Virginia coastal plain","indexId":"ofr84728","publicationYear":"1984","noYear":false,"title":"Hydrogeologic framework of the Virginia coastal plain"},"predicate":"SUPERSEDED_BY","object":{"id":38436,"text":"pp1404C - 1988 - Hydrogeologic framework of the Virginia coastal plain","indexId":"pp1404C","publicationYear":"1988","noYear":false,"chapter":"C","title":"Hydrogeologic framework of the Virginia coastal plain"},"id":1}],"lastModifiedDate":"2025-04-17T19:12:46.556498","indexId":"pp1404C","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":"1404","chapter":"C","title":"Hydrogeologic framework of the Virginia coastal plain","docAbstract":"<p>This report defines the hydrogeologic framework of the Virginia Coastal Plain and is a product of a comprehensive regional study to define the geology, hydrology, and geochemistry of the northern Atlantic Coastal Plain aquifer system extending from North Carolina to Long Island, New York. </p><p>The Virginia Coastal Plain consists of an eastward-thickening wedge of generally unconsolidated, interbedded sands and clays, ranging in age from Early Cretaceous to Holocene. These sediments range in thickness from more than 6,000 feet beneath the northeastern part of the Eastern Shore Peninsula to nearly 0 feet along the Fall Line. Eight confined aquifers, eight confining units, and an uppermost water table aquifer are delineated as the hydrogeologic framework of the Coastal Plain sediments in Virginia. The nine regional aquifers, from oldest to youngest, are lower, middle, and upper Potomac, Brightseat, Aquia, Chickahominy-Piney Point, St. Marys-Choptank, Yorktown-Eastover, and Columbia. The Brightseat is a newly identified and correlated aquifer of early Paleoceneage. This study is one of other, similar studies of the Coastal Plain areas in North Carolina, Maryland-Delaware, New Jersey, and Long Island, New York. These combined studies provide a system of hydrogeologic units that can be identified and correlated throughout the northern Atlantic Coastal Plain. </p><p>Data for this study were collected and analyzed from October 1979 to May 1983. The nine aquifers and eight confining units are identified and delineated by use of geophysical logs, drillers' information, and stratigraphic and paleontologic data. By correlating geophysical logs with hydrologic, stratigraphic, and paleontologic data throughout the Coastal Plain, a comprehensive multilayered framework of aquifers and confining units, each with distinct lithologic properties, was developed. Cross sections show the stratigraphic relationships of aquifers and confining units in the hydrogeologic framework of the Virginia Coastal Plain. Maps show confining-unit thicknesses and altitudes of aquifer tops, provide the basis for assigning aquifers to screened intervals of observation and production wells, and are used for the development of a comprehensive observation-well network in the Virginia Coastal Plain.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1404C","usgsCitation":"Meng, A.A., and Harsh, J.F., 1988, Hydrogeologic framework of the Virginia coastal plain: U.S. Geological Survey Professional Paper 1404, Report: iv, 82 p.: 4 Plates: 49.25 x 31.7 inches or smaller, https://doi.org/10.3133/pp1404C.","productDescription":"Report: iv, 82 p.: 4 Plates: 49.25 x 31.7 inches or smaller","costCenters":[],"links":[{"id":484735,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4843.htm","linkFileType":{"id":5,"text":"html"}},{"id":3447,"rank":7,"type":{"id":15,"text":"Index 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,{"id":15655,"text":"ofr87558 - 1988 - Distribution and variability of precipitation chemistry in the conterminous United States, January through December 1983","interactions":[],"lastModifiedDate":"2012-02-02T00:06:47","indexId":"ofr87558","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":"87-558","title":"Distribution and variability of precipitation chemistry in the conterminous United States, January through December 1983","docAbstract":"Analysis of atmospheric precipitation samples, collected during the 1983 calendar year from 109 National Trends Network sites in the United States, are presented in this report. The sites were grouped into six geographical regions based on the chemical composition of the samples. Precipitation chemistry in these regions was influenced by proximity to (1) oceans, (2) major industrial and fossil-fuel consuming areas, and (3) major agricultural and livestock areas. Frequency distributions of ionic composition, determined on 10 chemical constituents and on precipitation quantities for each site, showed wide variations in chemical concentrations and precipitation quantities from site to site. Of the 109 sites, 55 had data coverage for the year sufficient to characterize precipitation quality patterns on a nationwide basis. Except for ammonium and calcium, both of which showed largest concentrations in the agricultural midwest and plains states, the largest concentrations and loads generally were in areas that include the heavily industrialized population center of the eastern United States. Except for hydrogen, all chemical ions are inversely related to the quantity of precipitation depth. Precipitation quantities generally account for less than 30% of chemical variation in precipitation samples. However, precipitation quantities account for 30 to 65% of the variations of calcium concentrations in precipitation. In regions where precipitation has a large ionic proportion of hydrogen-ion equivalents, much of the hydrogen-ion concentration could be balanced by sulfate equivalents and partly balanced by nitrite-plus-nitrate equivalents. In the regions where hydrogen-ion equivalents in precipitation were smaller, ammonion-and calcium-ion equivalents were necessary, along with the hydrogen-ion equivalents, to balance the sulfate plus nitrite-plus-nitrate equivalent. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87558","usgsCitation":"Rinella, J.F., and Miller, T.L., 1988, Distribution and variability of precipitation chemistry in the conterminous United States, January through December 1983: U.S. Geological Survey Open-File Report 87-558, vii, 241 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr87558.","productDescription":"vii, 241 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":146494,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0558/report-thumb.jpg"},{"id":44620,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0558/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db6491fe","contributors":{"authors":[{"text":"Rinella, J. F.","contributorId":86777,"corporation":false,"usgs":true,"family":"Rinella","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":171502,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, T. L.","contributorId":54557,"corporation":false,"usgs":true,"family":"Miller","given":"T.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":171501,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":14872,"text":"ofr88681 - 1988 - Catalog of heat-flow and other pertinent data for the eastern United States and selected adjacent areas","interactions":[],"lastModifiedDate":"2012-02-02T00:06:52","indexId":"ofr88681","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":"88-681","title":"Catalog of heat-flow and other pertinent data for the eastern United States and selected adjacent areas","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88681","usgsCitation":"McCartan, L., and Architzel, R.J., 1988, Catalog of heat-flow and other pertinent data for the eastern United States and selected adjacent areas: U.S. Geological Survey Open-File Report 88-681, 5 p.  ;28 cm.; also in ASCII on IBM-compatible diskette; supplement to MF-2057, https://doi.org/10.3133/ofr88681.","productDescription":"5 p.  ;28 cm.; also in ASCII on IBM-compatible diskette; supplement to MF-2057","costCenters":[],"links":[{"id":147100,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0681/report-thumb.jpg"},{"id":43681,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0681/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f3e4b07f02db5ef8c3","contributors":{"authors":[{"text":"McCartan, Lucy","contributorId":87960,"corporation":false,"usgs":true,"family":"McCartan","given":"Lucy","affiliations":[],"preferred":false,"id":170158,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Architzel, Rebecca J.","contributorId":107706,"corporation":false,"usgs":true,"family":"Architzel","given":"Rebecca","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":170159,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44853,"text":"wri884052 - 1988 - Ground-water levels in the Lower Paleozoic and Precambrian crystalline rocks, of East Bradford and West Bradford Townships, Chester County, Pennsylvania, July and August 1987","interactions":[],"lastModifiedDate":"2022-01-10T20:21:50.472625","indexId":"wri884052","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":"88-4052","title":"Ground-water levels in the Lower Paleozoic and Precambrian crystalline rocks, of East Bradford and West Bradford Townships, Chester County, Pennsylvania, July and August 1987","docAbstract":"<p>No abstract available</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri884052","usgsCitation":"Garges, J.A., 1988, Ground-water levels in the Lower Paleozoic and Precambrian crystalline rocks, of East Bradford and West Bradford Townships, Chester County, Pennsylvania, July and August 1987: U.S. Geological Survey Water-Resources Investigations Report 88-4052, 1 Plate: 30.07 × 29.75 inches, https://doi.org/10.3133/wri884052.","productDescription":"1 Plate: 30.07 × 29.75 inches","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":161713,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":394127,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_46975.htm"},{"id":82213,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4052/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Pennsylvania","county":"Chester County","otherGeospatial":"East Bradford and West Bradford Townships","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -75.7781,\n              39.9147\n            ],\n            [\n              -75.5981,\n              39.9147\n            ],\n            [\n              -75.5981,\n              40.0111\n            ],\n            [\n              -75.7781,\n              40.0111\n            ],\n            [\n              -75.7781,\n              39.9147\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667545","contributors":{"authors":[{"text":"Garges, John A.","contributorId":74428,"corporation":false,"usgs":true,"family":"Garges","given":"John","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":230555,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38450,"text":"pp1408E - 1988 - Water use on the Snake River plain, Idaho and eastern Oregon","interactions":[{"subject":{"id":13849,"text":"ofr85559 - 1986 - Water use on the Snake River plain, Idaho and eastern Oregon","indexId":"ofr85559","publicationYear":"1986","noYear":false,"title":"Water use on the Snake River plain, Idaho and eastern Oregon"},"predicate":"SUPERSEDED_BY","object":{"id":38450,"text":"pp1408E - 1988 - Water use on the Snake River plain, Idaho and eastern Oregon","indexId":"pp1408E","publicationYear":"1988","noYear":false,"chapter":"E","title":"Water use on the Snake River plain, Idaho and eastern Oregon"},"id":1}],"lastModifiedDate":"2013-11-19T15:49:31","indexId":"pp1408E","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":"1408","chapter":"E","title":"Water use on the Snake River plain, Idaho and eastern Oregon","docAbstract":"Amounts of water withdrawn and consumptively used for irrigation \nand other uses on the Snake River Plain were estimated to help deter- \nmine hydrologic effects of ground- and surface-water use. Irrigation is \nthe largest off stream use of water on the plain. Surface-water irriga- \ntion began in the 1840's and increased rapidly through the early 1900's. \nUse of ground water for irrigation accelerated after World War II. In \n1980, about 3.1 million acres were irrigated: 1.0 million acres were \nirrigated with about 2.3 million acre-feet of ground water; 2.0 million \nacres were irrigated with about 12.7 million acre-feet of surface water; \n0.1 million acres were irrigated with combined surface and ground water. \nHistorical changes in aquifer storage and spring discharge are closely \nrelated to changes in irrigation practices.\nIndustries, including aquaculture, withdrew an estimated 1.97 million \nacre-feet of water. Withdrawals for other offstream uses, including public \nand rural supplies, totaled 132,000 acre-feet. Hydroelectric power \ngeneration is an economically important instream use of water. In \n1980, about 52 million acre-feet of surface water was used to generate \n2.6 million megawatt-hours of electricity. Native vegetation evapo- \ntranspired an estimated 3.7 million acre-feet, and 900,000 acre-feet \nevaporated from bare ground and open water.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp1408E","usgsCitation":"Goodell, S.A., 1988, Water use on the Snake River plain, Idaho and eastern Oregon: U.S. Geological Survey Professional Paper 1408, vi, 51 p., https://doi.org/10.3133/pp1408E.","productDescription":"vi, 51 p.","numberOfPages":"63","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":122089,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1408e/report-thumb.jpg"},{"id":64930,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1408e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho;Oregon","otherGeospatial":"Snake River Plain","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.0,42.0 ], [ -117.0,45.0 ], [ -111.0,45.0 ], [ -111.0,42.0 ], [ -117.0,42.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5eff26","contributors":{"authors":[{"text":"Goodell, S. A.","contributorId":38168,"corporation":false,"usgs":true,"family":"Goodell","given":"S.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":219844,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":60361,"text":"mf1921A - 1988 - Mineral resource potential map of the Pecos Wilderness, Santa Fe, San Miguel, Mora, Rio Arriba, and Taos Counties, New Mexico","interactions":[],"lastModifiedDate":"2025-05-23T18:51:56.04573","indexId":"mf1921A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1921","chapter":"A","title":"Mineral resource potential map of the Pecos Wilderness, Santa Fe, San Miguel, Mora, Rio Arriba, and Taos Counties, New Mexico","docAbstract":"<p>The Pecos Wilderness covers approximately 348 sq mi in the Santa Fe and Carson National Forests, north-central New Mexico. The area investigated includes the wilderness and approximately 150 sq mi of adjacent territory. The additional area covers several RARE II Road less Areas that were classified by the U.S. Forest Service in 1979 as Proposed Wilderness and Further Planning Areas, but were not incorporated in the Pecos Wilderness by the New Mexico Wilderness Bill. For the purpose of this report the entire area is called the study area.</p>\n<p>The study area is at the southern end of the Sangre de Cristo Range. It is characterized by an axial line of alpine peaks that rise to more than 13,000 ft, flanked on the west and north by heavily wooded ridges and canyons that drain to the Rio Grande Valley, and on the southeast by a high dissected plateau of meadows and forest. The plateau is dissected by deep canyons of the Pecos River and its tributaries, and is bounded on the east by a scarp of about 3,000 ft. Partly forested ranch land lies below the base of the scarp to the east, and beyond that is prai-rie of the Great Plains.</p>\n<p>This map is based on geologic and geochemical studies and mine and prospect investigations that were done principally in 1977 and 1979-80 (U.S. Geological Survey, U.S. Bureau of Mines, and New Mexico Bureau of Mines and Mineral Resources, 1980; Lane, 1980; Moench and Robertson, 1980; Moench, Robertson, and Sutley, 1980; Moench and Erickson, 1980; Moench, Grambling, and Robertson, 1988; Moench, Sutley, and Erickson, 1988; Erickson, Sutley, and Moench, 1986). An aeromagnetic survey covering almost all of the Pecos Wilderness was flown in 1970. The resulting aeromagnetic map was published by Moench and others (1980) and interpreted in that report by Lindreth Cordell. Cordell found no correlation between magnetic features and geologic terraines having mineral resource potential.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1921A","usgsCitation":"Moench, R.H., and Lane, M.E., 1988, Mineral resource potential map of the Pecos Wilderness, Santa Fe, San Miguel, Mora, Rio Arriba, and Taos Counties, New Mexico: U.S. Geological Survey Miscellaneous Field Studies Map 1921, Report: 15 p.; 1 Plate: 39.17 x 56.44 inches, https://doi.org/10.3133/mf1921A.","productDescription":"Report: 15 p.; 1 Plate: 39.17 x 56.44 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":327363,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1921-A/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":88790,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1988/1921a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":183202,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1988/1921a/report-thumb.jpg"},{"id":407322,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5486.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"New Mexico","county":"Mora County, Rio Arriba County, San Miguel County, Santa Fe County, Taos County","otherGeospatial":"Pecos Wilderness","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.875,\n              35.6008\n            ],\n            [\n              -105.3906,\n              35.6008\n            ],\n            [\n              -105.3906,\n              36.1039\n            ],\n            [\n              -105.875,\n              36.1039\n            ],\n            [\n              -105.875,\n              35.6008\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f4132","contributors":{"authors":[{"text":"Moench, R. H.","contributorId":8853,"corporation":false,"usgs":true,"family":"Moench","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":263607,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lane, M. E.","contributorId":9262,"corporation":false,"usgs":true,"family":"Lane","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":263608,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":34934,"text":"b1594 - 1988 - Natural aggregates of the conterminous United States","interactions":[],"lastModifiedDate":"2025-05-07T18:37:36.576465","indexId":"b1594","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"1594","title":"Natural aggregates of the conterminous United States","docAbstract":"Crushed stone and sand and gravel are the two main sources of natural aggregates. These materials are commonly used construction materials and frequently can be interchanged with one another. They are widely used throughout the United States, with every State except two producing crushed stone. Together they amount to about half the mining volume in the United States. Approximately 96 percent of sand and gravel and 77 percent of the crushed stone produced in the United States are used in the construction industry. \r\nNatural aggregates are widely distributed throughout the United States in a variety of geologic environments. Sand and gravel deposits commonly are the results of the weathering of bedrock and subsequent transportation and deposition of the material by water or ice (glaciers). As such, they commonly occur as river or stream deposits or in glaciated areas as glaciofluvial and other deposits. Crushed stone aggregates are derived from a wide variety of parent bedrock materials. Limestone and other carbonates account for approximately three quarters of the rocks used for crushed stone, with granite and other igneous rocks making up the bulk of the remainder. Limestone deposits are widespread throughout the Central and Eastern United States and are scattered in the West. Granites are widely distributed in the Eastern and Western United States, with few exposures in the Midwest. Igneous rocks (excluding granites) are largely concentrated in the Western United States and in a few isolated localities in the East. \r\nEven though natural aggregates are widely distributed throughout the United States, they are not universally available for consumptive use. Some areas are devoid of sand and gravel, and potential sources of crushed stone may be covered with sufficient unconsolidated material to make surface mining impractical. In some areas many aggregates do not meet the physical property requirements for certain uses, or they may contain mineral constituents that react adversely when used as concrete aggregate. \r\nIn areas where suitable natural aggregate is not available or accessible, it may become necessary to improve the quality of existing aggregate, to import aggregate from outside the area, or to substitute artificial aggregate for natural aggregate. In most cases, all of these alternatives add substantially to the cost of the final product. Even though an area may be blessed with an abundance of aggregate suitable for the intended purpose, existing land uses, zoning, or regulations may preclude commercial exploitation of the aggregate. \r\nThis report also discusses the aggregate industry in general terms, including exploration, mining, and processing, as well as aggregate production rates. Proper long-range planning based on an understanding of the aggregate industry can help assure adequate supplies of aggregate.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1594","usgsCitation":"Langer, W.H., 1988, Natural aggregates of the conterminous United States (Version 1.0): U.S. Geological Survey Bulletin 1594, Report: 33 p.; 2 Plates: 42.50 x 31.00 inches, https://doi.org/10.3133/b1594.","productDescription":"Report: 33 p.; 2 Plates: 42.50 x 31.00 inches","costCenters":[],"links":[{"id":110407,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21810.htm","linkFileType":{"id":5,"text":"html"}},{"id":3382,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/bul/b1594/","linkFileType":{"id":5,"text":"html"}},{"id":164349,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","otherGeospatial":"conterminous United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"geometry\": {\n        \"type\": \"MultiPolygon\",\n        \"coordinates\": [\n          [\n            [\n              [\n                -94.81758,\n                49.38905\n              ],\n              [\n                -94.64,\n                48.84\n              ],\n              [\n                -94.32914,\n                48.67074\n              ],\n              [\n                -93.63087,\n                48.60926\n              ],\n              [\n                -92.61,\n                48.45\n              ],\n              [\n                -91.64,\n                48.14\n              ],\n              [\n                -90.83,\n                48.27\n              ],\n              [\n                -89.6,\n                48.01\n              ],\n              [\n                -89.27292,\n                48.01981\n              ],\n              [\n                -88.37811,\n                48.30292\n              ],\n              [\n                -87.43979,\n                47.94\n              ],\n              [\n                -86.46199,\n                47.55334\n              ],\n              [\n                -85.65236,\n                47.22022\n              ],\n              [\n                -84.87608,\n                46.90008\n              ],\n              [\n                -84.77924,\n                46.6371\n              ],\n              [\n                -84.54375,\n                46.53868\n              ],\n              [\n                -84.6049,\n                46.4396\n              ],\n              [\n                -84.3367,\n                46.40877\n              ],\n              [\n                -84.14212,\n                46.51223\n              ],\n              [\n                -84.09185,\n                46.27542\n              ],\n             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blanger@usgs.gov","contributorId":1241,"corporation":false,"usgs":true,"family":"Langer","given":"William","email":"blanger@usgs.gov","middleInitial":"H.","affiliations":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"preferred":false,"id":213834,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29498,"text":"wri874248 - 1988 - Hydrogeology and predevelopment flow in the Texas Gulf Coast aquifer systems","interactions":[],"lastModifiedDate":"2016-08-10T15:19:13","indexId":"wri874248","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":"87-4248","title":"Hydrogeology and predevelopment flow in the Texas Gulf Coast aquifer systems","docAbstract":"<p>A multilayered ground-water flow system exists in the Coastal Plain sediments of Texas. The Tertiary and Quaternary clastic deposits have an area! extent of 128,000 square miles onshore and in the Gulf of Mexico. Two distinct aquifer systems are recognized for the sediments, which range in thickness from a few feet to more than 12,000 feet. The older system the Texas coastal uplands aquifer system consists of four aquifers and two confining units in the Wilcox and Claiborne Groups. It is bounded from below by the practically impermeable Midway confining unit or by the top of the geopressured zone. It is bounded from above by the poorly permeable Vicksburg-Jackson confining unit, which separates it from the younger coastal lowlands aquifer system. The coastal lowlands aquifer system consists of five permeable zones and two confining units that range in age from Oligocene to Holocene. The hydrogeologic units of both systems are exposed in bands that parallel the coastline. The units dip and thicken toward the Gulf.</p>\n<p>Quality of water in the aquifer systems varies greatly, with dissolved solids ranging from a few hundred to more than 200,000 milligrams per liter.</p>\n<p>A three-dimensional, variable-density digital model was developed to simulate predevelopment flow in the aquifer systems, for which steady-state conditions were assumed. Horizontal hydraulic conductivities of the aquifers and permeable zones in the calibrated model range from 15 feet per day for the middle Wilcox aquifer, to 170 feet per day for the Holocene-upper Pleistocene aquifer. Vertical hydraulic conductivities range from 1 x 10<sup>-5</sup> foot per day for the Vicksburg-Jackson confining unit, to 1 x 10<sup>-2</sup> foot per day for four of the aquifers and permeable zones. The simulated values of transmissivity and leakance are functions of the percent of sand that is present in each model grid block.</p>\n<p>There is a large range in precipitation across the study area, from about 21 inches per year in the west to about 56 inches per year in the east. Eastward from a line through Corpus Christi and San Antonio, average annual precipitation ranges from about 30 to about 56 inches. A few inches per year reaches the saturated zone in topographically high areas and is discharged in low areas as evapotranspiration, seepage, springflow, and stream base flow. A smaller amount of water flows through the aquifers and permeable zones downdip from the outcrop areas. This flow results in upward or downward leakage into adjacent hydrogeologic units, but is generally upward into overlying units.</p>\n<p>Westward from the line through Corpus Christi and San Antonio, average annual precipitation ranges from about 30 to about 21 inches. The general pattern of flow in the aquifers and permeable zones is similar to that in the east, but rates of flow are somewhat smaller. In contrast to the east, ground-water discharge in the west is generally not visible. Evapotranspiration is the main mechanism for ground-water discharge, with most ground water being discharged through evapotranspiration by phreatophytes.</p>\n<p>Simulated discharge and recharge rates in the combined outcrop areas of all units do not exceed 6 inches per year. The large rates occur in small, local topographically low and high areas. The average discharge rate simulated in the outcrops of the units is 0.45 inch per year. The recharge area is considerably smaller than the discharge area, and the average recharge rate over this smaller area is 0.74 inch per year.</p>\n<p>Total simulated recharge in the outcrop areas is 269 million cubic feet per day, which is offset by an equal amount of discharge in the outcrop areas. The smallest rates of leakage are across the Vicksburg-Jackson confining unit, with downward and upward rates of less than one million cubic feet per day. The greatest rate of leakage is 47 million cubic feet per day upward into the Holocene-upper Pleistocene permeable zone.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri874248","usgsCitation":"Ryder, P.D., 1988, Hydrogeology and predevelopment flow in the Texas Gulf Coast aquifer systems: U.S. Geological Survey Water-Resources Investigations Report 87-4248, vii, 109 p., https://doi.org/10.3133/wri874248.","productDescription":"vii, 109 p.","numberOfPages":"116","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":58346,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4248/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":126794,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4248/report-thumb.jpg"}],"country":"United States","state":"Texas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -94.1748046875,\n              33.578014746143985\n            ],\n            [\n              -95.20751953125,\n              33.063924198120645\n            ],\n            [\n              -99.16259765625,\n              28.07198030177986\n            ],\n            [\n              -99.580078125,\n              27.60567082646547\n            ],\n            [\n              -99.11865234374999,\n              26.43122806450644\n            ],\n            [\n              -98.1298828125,\n              26.03704188651584\n            ],\n            [\n              -97.18505859374999,\n              25.997549919572112\n            ],\n            [\n              -97.36083984375,\n              27.527758206861886\n            ],\n            [\n              -96.328125,\n              28.51696944040106\n            ],\n            [\n              -95.361328125,\n              28.92163128242129\n            ],\n            [\n              -94.482421875,\n              29.53522956294847\n            ],\n            [\n              -93.91113281249999,\n              29.7453016622136\n            ],\n            [\n              -93.515625,\n              31.16580958786196\n            ],\n            [\n              -94.02099609375,\n              32.02670629333614\n            ],\n            [\n              -94.04296874999999,\n              33.578014746143985\n            ],\n            [\n              -94.1748046875,\n              33.578014746143985\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db625321","contributors":{"authors":[{"text":"Ryder, Paul D.","contributorId":60188,"corporation":false,"usgs":true,"family":"Ryder","given":"Paul","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":201611,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56219,"text":"wdrNY871 - 1988 - Water resources data, New York, water year 1987, volume 1, eastern New York, excluding Long Island","interactions":[],"lastModifiedDate":"2020-11-20T20:00:17.578896","indexId":"wdrNY871","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"NY-87-1","title":"Water resources data, New York, water year 1987, volume 1, eastern New York, excluding Long Island","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNY871","usgsCitation":"Firda, G., Lumia, R., and Burke, P.M., 1988, Water resources data, New York, water year 1987, volume 1, eastern New York, excluding Long Island: U.S. Geological Survey Water Data Report NY-87-1, ix, 267 p., https://doi.org/10.3133/wdrNY871.","productDescription":"ix, 267 p.","costCenters":[],"links":[{"id":380654,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1987/ny-87-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":175024,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1987/ny-87-1/report-thumb.jpg"}],"country":"United States","state":"New 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York\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f0d9c","contributors":{"authors":[{"text":"Firda, G.D.","contributorId":99622,"corporation":false,"usgs":true,"family":"Firda","given":"G.D.","affiliations":[],"preferred":false,"id":254977,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lumia, Richard rlumia@usgs.gov","contributorId":4579,"corporation":false,"usgs":true,"family":"Lumia","given":"Richard","email":"rlumia@usgs.gov","affiliations":[],"preferred":true,"id":254975,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Burke, P. M.","contributorId":8478,"corporation":false,"usgs":true,"family":"Burke","given":"P.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":254976,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2191,"text":"wsp2336A - 1988 - Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts","interactions":[{"subject":{"id":14775,"text":"ofr86532 - 1987 - Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts","indexId":"ofr86532","publicationYear":"1987","noYear":false,"title":"Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts"},"predicate":"SUPERSEDED_BY","object":{"id":2191,"text":"wsp2336A - 1988 - Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts","indexId":"wsp2336A","publicationYear":"1988","noYear":false,"chapter":"A","title":"Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts"},"id":1}],"lastModifiedDate":"2016-08-05T11:55:09","indexId":"wsp2336A","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":"2336","chapter":"A","title":"Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts","docAbstract":"<p>The Edwards aquifer is a complexly faulted, carbonate aquifer lying within the Balcones fault zone of south-central Texas. The aquifer consists of thin- to massive-bedded limestone and dolomite, most of which is in the form of mudstones and wackestones. Well-developed secondary porosity has formed in association with former erosional surfaces within the carbonate rocks, within dolomitized-burrowed tidal and evaporitic deposits, and along inclined fractures to produce an aquifer with transmissivities greater than 100 ft2/s. The aquifer is recharged mainly by streamflow losses in the outcrop area of the Edwards aquifer and is discharged by major springs located at considerable distances, as much as 150 mi, from the areas of recharge and by wells. Ground-water flow within the Edwards aquifer of the San Antonio region was simulated to investigate concepts relating to the storage and flow characteristics. The concepts of major interest were the effects of barrier faults on flow direction, water levels, springflow, and storage within the aquifer. A general-purpose, finite-difference model, modified to provide the capability of representing barrier faults, was used to simulate ground-water flow and storage in the aquifer. The approach in model development was to conduct a series of simulations beginning with a simple representation of the aquifer framework and then proceeding to subsequent representations of increasing complexity. The simulations investigated the effects of complex geologic structures and of significant changes in transmissivity, anisotropy, and storage coefficient. Initial values of transmissivity, anisotropy, and storage coefficient were estimated based on concepts developed in previous studies. Results of the simulations confirmed the original estimates of transmissivity values (greater than 100 square feet/s) in the confined zone of the aquifer between San Antonio and Comal Springs. A storage coefficient of 0.05 in the unconfined zone of the aquifer produced the best simulation of water levels and springflow. A major interpretation resulting from the simulations is that two essentially independent areas of regional flow were identified in the west and central part of the study area. Flows from the two areas converge at Comal Springs. The directions of computed flux vectors reflected the presence of major barrier faults, which locally deflect patterns of ground-water movement. The most noticeable deflection is the convergence of flow through a geologic structural opening, the Knippa gap, in eastern Uvalde County. A second significant interpretation is that ground-water flow in northeastern Bexar, Comal, and Hays Counties is diverted by barrier faults toward San Marcos Springs, a regional discharge point. Simulations showed that several barrier faults in the northwestern part of the San Antonio area had a significant effect on storage, water levels, and springflow within the Edwards aquifer.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp2336A","usgsCitation":"Maclay, R.W., and Land, L.F., 1988, Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts: U.S. Geological Survey Water Supply Paper 2336, iv, 48 p., https://doi.org/10.3133/wsp2336A.","productDescription":"iv, 48 p.","endPage":"54","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":27832,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2336a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138266,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2336a/report-thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"Edwards Aquifer","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f2e45","contributors":{"authors":[{"text":"Maclay, Robert W.","contributorId":13210,"corporation":false,"usgs":true,"family":"Maclay","given":"Robert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":144799,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Land, Larry F.","contributorId":60612,"corporation":false,"usgs":true,"family":"Land","given":"Larry","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":144800,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26983,"text":"wri874082 - 1988 - A digital simulation of the glacial-aquifer system in Sanborn and parts of Beadle, Miner, Hanson, Davison, and Jerauld counties, South Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:08:44","indexId":"wri874082","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":"87-4082","title":"A digital simulation of the glacial-aquifer system in Sanborn and parts of Beadle, Miner, Hanson, Davison, and Jerauld counties, South Dakota","docAbstract":"The drought in South Dakota from 1974-76 and the near drought conditions in 1980-81 have resulted in increased demands on the groundwater resources within many of the irrigated areas of the James River basin in eastern South Dakota. These increases in demand for irrigation water from the glacial aquifer system, and continued requests to the State for additional irrigation well permits, have created a need for a systematic water management program to avoid over-development of this system in the James River basin. An equally spaced grid containing 56 rows and 52 columns used to simulate the glacial aquifer system, was calibrated using water level data collected before significant groundwater development (before 1973). The aquifer was also simulated in 11 annual transient stress periods from 1973 through 1983 and in 12 monthly transient stress periods for 1976. The simulated pre-development potentiometric heads were compared to average water levels from 32 observation wells to check the accuracy of the simulate potentiometric surface. The average arithmetic difference between the simulated and observed water levels was 1.68 ft and the average absolute difference was 4.38 ft. The non-pumping steady-state simulated water budget indicates that recharge from precipitation accounts for 97.1% of the water entering the aquifer and evapotranspiration accounts for 98.2% of the water leaving the aquifer. The sensitivity analysis of the steady-state model indicates that the model is most sensitive to reductions in recharge and least to changes in hydraulic conductivity. The maximum annual recharge varied from 0.10 inch in 1976 to 8.14 inches in 1977. The potential annual evapotranspiration varied from 29.9 inches in 1982 to 48.9 inches in 1976. Withdrawals from the glacial aquifer system increased 2.6 times between 1975 and 1976. The average annual arithmetic difference between the simulated and observed water levels ranged from 3.88 ft in 1974 to 2.23 ft in 1982; the average absolute difference ranged from 4.70 ft in 1973 to 11.70 ft in 1982. In the 1976 monthly transient simulation, the maximum annual recharge rate 0.10 inch was distributed over the months of March, April, and September. The potential monthly evapotranspiration rate ranged from 12.50 inches in August to 0.00 inch during the winter when the ground was frozen. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874082","usgsCitation":"Emmons, P., 1988, A digital simulation of the glacial-aquifer system in Sanborn and parts of Beadle, Miner, Hanson, Davison, and Jerauld counties, South Dakota: U.S. Geological Survey Water-Resources Investigations Report 87-4082, v, 59 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874082.","productDescription":"v, 59 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124046,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4082/report-thumb.jpg"},{"id":55870,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4082/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6aed4d","contributors":{"authors":[{"text":"Emmons, P.J.","contributorId":60630,"corporation":false,"usgs":true,"family":"Emmons","given":"P.J.","email":"","affiliations":[],"preferred":false,"id":197359,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":64935,"text":"i1773 - 1988 - Metallogenic map of zinc, lead, and barium deposits and occurrences in Paleozoic sedimentary rocks, east-central United States","interactions":[],"lastModifiedDate":"2012-02-10T00:11:07","indexId":"i1773","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"1773","subseriesTitle":"NONE","title":"Metallogenic map of zinc, lead, and barium deposits and occurrences in Paleozoic sedimentary rocks, east-central United States","language":"ENGLISH","doi":"10.3133/i1773","usgsCitation":"Clark, S.H., 1988, Metallogenic map of zinc, lead, and barium deposits and occurrences in Paleozoic sedimentary rocks, east-central United States: U.S. Geological Survey IMAP 1773, 1 map :col. ;120 x 97 cm., on sheet 127 x 102 cm., folded in envelope 30 x 24 cm. +1 pamphlet (77 p. : tables ; 28 cm.), https://doi.org/10.3133/i1773.","productDescription":"1 map :col. ;120 x 97 cm., on sheet 127 x 102 cm., folded in envelope 30 x 24 cm. +1 pamphlet (77 p. : tables ; 28 cm.)","costCenters":[],"links":[{"id":107119,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9906.htm","linkFileType":{"id":5,"text":"html"},"description":"9906"},{"id":190061,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1773/report-thumb.jpg"},{"id":91465,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1773/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"2500000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -93,31 ], [ -93,44 ], [ -78.5,44 ], [ -78.5,31 ], [ -93,31 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4fe4b07f02db628700","contributors":{"authors":[{"text":"Clark, S. H. B.","contributorId":95052,"corporation":false,"usgs":true,"family":"Clark","given":"S.","email":"","middleInitial":"H. B.","affiliations":[],"preferred":false,"id":272392,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14851,"text":"ofr87765 - 1988 - Simulated changes in ground-water flow caused by hypothetical pumping in east Carson Valley, Douglas County, Nevada","interactions":[],"lastModifiedDate":"2021-11-09T20:07:05.790302","indexId":"ofr87765","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":"87-765","title":"Simulated changes in ground-water flow caused by hypothetical pumping in east Carson Valley, Douglas County, Nevada","docAbstract":"An existing groundwater model of Carson Valley was used to simulate changes in groundwater flow on the east side of Carson Valley, Nevada, in response to hypothetical increases in groundwater pumpage. Pumpage scenarios that reflect State groundwater permits and pending applications were used in four different simulations to estimate the effect of hypothetical development on groundwater levels and storage, groundwater flow to the Carson River, and groundwater levels and storage, groundwater flow to the Carson River, and groundwater consumed by evapotranspiration over a 45-yr period. The four simulations were based on pumpage rates ranging from 0.13 to 6.4 cu ft/sec (92 to 4,590 acre-ft/year). Changes in groundwater flow and water levels caused by the lowest rate were minimal and at the limit of accuracy of the groundwater model. The highest pumping rate caused water level declines as much as 15 ft, decreased groundwater storage by 27,000 acre/ft, decreased groundwater to the Carson River by 4.3 cu ft/sec (3,100 acre-ft/year), and reduced evapotranspiration losses by about 1,200 acre-ft/year. (Author 's abstract)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr87765","usgsCitation":"Maurer, D.K., 1988, Simulated changes in ground-water flow caused by hypothetical pumping in east Carson Valley, Douglas County, Nevada: U.S. Geological Survey Open-File Report 87-765, Report: iv, 6 p.; 5 Plates: 12.68 × 18.25 inches or smaller, https://doi.org/10.3133/ofr87765.","productDescription":"Report: iv, 6 p.; 5 Plates: 12.68 × 18.25 inches or smaller","costCenters":[],"links":[{"id":391523,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17326.htm"},{"id":43642,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0765/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":43641,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0765/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":43640,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0765/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":43639,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0765/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":43638,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0765/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":43637,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0765/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":146677,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0765/report-thumb.jpg"}],"country":"United States","state":"Nevada","county":"Douglas County","otherGeospatial":"east Carson Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.7680,\n              38.898\n            ],\n            [\n              -119.5830,\n              38.898\n            ],\n            [\n              -119.5830,\n              39.108\n            ],\n            [\n              -119.7680,\n              39.108\n            ],\n            [\n              -119.7680,\n              38.898\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f9e4b07f02db5f38a2","contributors":{"authors":[{"text":"Maurer, D. K.","contributorId":37757,"corporation":false,"usgs":true,"family":"Maurer","given":"D.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":170123,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}