{"pageNumber":"4310","pageRowStart":"107725","pageSize":"25","recordCount":165901,"records":[{"id":26824,"text":"wri864173 - 1987 - Geohydrologic reconnaissance of a ground-water contamination problem in the Argonne Road area near Spokane, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:08:30","indexId":"wri864173","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"86-4173","title":"Geohydrologic reconnaissance of a ground-water contamination problem in the Argonne Road area near Spokane, Washington","docAbstract":"Three domestic wells that withdraw groundwater from an alluvium-filled trough cut into granite were found to be contaminated with the organic solvents tetrachloroethene, trichloroethene, 1,1,1-trichloroethane, and 1 ,2-trans-dichloroethene. The suspected source of contamination is a nearby septic-tank sludge disposal area. There is concern that the affected aquifer is tributary to the Spokane aquifer, which has been accorded ' sole source ' status by the U.S. Environmental Protection Agency. Preliminary estimates suggest that groundwater in the area is moving toward the Spokane aquifer and that the transit time may range from 2.5 to 25 years. Because of longitudinal dispersion, however, the plume of contaminants may move at a faster rate than the ambient groundwater and may arrive at given destinations more quickly than calculated above. A literature search has indicated that the dissolved solute phase of the contaminants will not be significantly affected by sorption, volatilization, chemical activity, or biodegradation. Because of the preliminary nature of the investigation, many questions relating to the extent of contamination remain unanswered. A list of suggested additional studies to answer those questions and to refine and confirm the findings of this investigation is presented. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri864173","usgsCitation":"Dion, N.P., 1987, Geohydrologic reconnaissance of a ground-water contamination problem in the Argonne Road area near Spokane, Washington: U.S. Geological Survey Water-Resources Investigations Report 86-4173, v, 37 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri864173.","productDescription":"v, 37 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124095,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4173/report-thumb.jpg"},{"id":55705,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4173/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8e23","contributors":{"authors":[{"text":"Dion, N. P.","contributorId":33302,"corporation":false,"usgs":true,"family":"Dion","given":"N.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":197069,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26801,"text":"wri874007 - 1987 - Ground-water quality and geochemistry of Las Vegas Valley, Clark County, Nevada, 1981-83: Implementation of a monitoring network","interactions":[],"lastModifiedDate":"2022-02-02T21:59:20.341167","indexId":"wri874007","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-4007","title":"Ground-water quality and geochemistry of Las Vegas Valley, Clark County, Nevada, 1981-83: Implementation of a monitoring network","docAbstract":"<p>As a result of rapid urban growth in Las Vegas Valley, rates of water use and wastewater disposal have grown rapidly during the last 25 years. Concern has developed over the potential water quality effects of this growth. The deep percolation of wastewater and irrigation return flow (much of which originates as imported water from Lake Mead), along with severe overdraft conditions in the principal aquifers of the valley, could combine to pose a long-term threat to groundwater quality. The quantitative investigations of groundwater quality and geochemical conditions in the valley necessary to address these concerns would include the establishment of data collection networks on a valley-wide scale that differ substantially from existing networks. The valley-wide networks would have a uniform areal distribution of sampling sites, would sample from all major depth zones, and would entail repeated sampling from each site. With these criteria in mind, 40 wells were chosen for inclusion in a demonstration monitoring network. Groundwater in the northern half of the valley generally contains 200 to 400 mg/L of dissolved solids, and is dominated by calcium, magnesium , and bicarbonate ions, reflecting a chemical equilibrium between the groundwater and the dominantly carbonate rocks in the aquifers of this area. The intermediate to deep groundwater in the southern half of the valley is of poorer quality (containing 700 to 1,500 mg/L of dissolved solids) and is dominated by calcium, magnesium, sulfate, and bicarbonate ions, reflecting the occurrence of other rock types including evaporite minerals among the still-dominant carbonate rocks in the aquifers of this part of the valley. The poorest quality groundwater in the valley is generally in the lowland parts of the valley in the first few feet beneath the water table, where dissolved solids concentrations range from 2,000 to &gt; 7,000 mg/L , and probably reflects the effects of evaporite dissolution, secondary recharge, and evapotranspiration. The most common water quality constraint on potential groundwater use is the high salinity. No evidence of large-scale contamination of deep groundwater was found in this study.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri874007","usgsCitation":"Dettinger, M.D., 1987, Ground-water quality and geochemistry of Las Vegas Valley, Clark County, Nevada, 1981-83: Implementation of a monitoring network: U.S. Geological Survey Water-Resources Investigations Report 87-4007, v, 69 p., https://doi.org/10.3133/wri874007.","productDescription":"v, 69 p.","costCenters":[],"links":[{"id":395317,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_46696.htm"},{"id":55689,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4007/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124197,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4007/report-thumb.jpg"}],"country":"United States","state":"Nevada","county":"Clark County","otherGeospatial":"Las Vegas Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -115.2883,\n              35.95\n            ],\n            [\n              -114.9231,\n              35.95\n            ],\n            [\n              -114.9231,\n              36.3444\n            ],\n            [\n              -115.2883,\n              36.3444\n            ],\n            [\n              -115.2883,\n              35.95\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6673c0","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":197027,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":40175,"text":"ofr87525 - 1987 - Composite magnetic anomaly map of the Greenville 1 degree x 2 degree Quadrangle, Georgia and South Carolina","interactions":[],"lastModifiedDate":"2012-02-02T00:10:52","indexId":"ofr87525","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-525","title":"Composite magnetic anomaly map of the Greenville 1 degree x 2 degree Quadrangle, Georgia and South Carolina","language":"ENGLISH","doi":"10.3133/ofr87525","usgsCitation":"Bond, K.R., 1987, Composite magnetic anomaly map of the Greenville 1 degree x 2 degree Quadrangle, Georgia and South Carolina: U.S. Geological Survey Open-File Report 87-525, 1 map :photocopy ;46 x 75 cm., on sheet 61 x 111 cm., https://doi.org/10.3133/ofr87525.","productDescription":"1 map :photocopy ;46 x 75 cm., on sheet 61 x 111 cm.","costCenters":[],"links":[{"id":171774,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":70138,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0525/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8219","contributors":{"authors":[{"text":"Bond, Kevin R.","contributorId":44937,"corporation":false,"usgs":true,"family":"Bond","given":"Kevin","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":223076,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26440,"text":"wri874116 - 1987 - Relation of water chemistry of the Edwards aquifer to hydrogeology and land use, San Antonio Region, Texas","interactions":[],"lastModifiedDate":"2016-08-10T11:49:14","indexId":"wri874116","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-4116","title":"Relation of water chemistry of the Edwards aquifer to hydrogeology and land use, San Antonio Region, Texas","docAbstract":"<p>Water-chemistry data from the Edwards aquifer for 1976-85, consisting of nearly 1,500 chemical analyses from 280 wells and 3 springs, were used to statistically evaluate relations among ground-water chemistry, hydrogeology, and land use. Five land uses associated with sampled wells were classified on the basis of published information and field surveys. Four major subareas of the aquifer were defined to reflect the relative susceptibility of ground water to contamination originating from human activities using hydrogeologic and tritium data.</p>\n<p>Water from an agricultural area over the unconfined zone of the aquifer had the largest median concentration of nitrite plus nitrate. Large nitrite plus nitrate concentrations were spatially associated with large tritium concentrations and nitrogen isotopic ratios characteristic of streamflow recharge. Detections of fecal-coliform bacteria were associated mainly with water from wells completed in the unconfined zone.</p>\n<p>Most of the occurrences of tetrachloroethylene, l,2-(trans)-dichloroethylene, trichlorofluoromethane, 1,1,1-trichloroethane, and 2,4-D in ground water were associated with wells completed in the unconfined zone of the aquifer. Fatty acids detected in water from some wells may commonly be present naturally in ground water.</p>\n<p>The percentage of samples in which arsenic, barium, lead, and zinc were detected was similar among subareas; the samples were from the freshwater parts of the aquifer. Large lead and zinc concentrations were associated with volumes of pumpage less than 1,000 gallons.</p>\n<p>In general, the quality of ground water in the freshwater parts of the aquifer (north of the \"bad-water\" line) is suitable for all uses including human consumption. Two areas that are exceptions are: (1) Northeast of Garner Field in Uvalde, Texas, where PCE (tetrachloroethylene) has been detected in groundwater samples, and (2) north-central Bexar County near the former West Avenue landfill where PCE and benzene have been detected in ground-water samples. Concentrations of these organic compounds in water from many wells in the two areas exceed the maximum contaminant level for human consumption set by the U.S. Environmental Protection Agency.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri874116","usgsCitation":"Buszka, P.M., 1987, Relation of water chemistry of the Edwards aquifer to hydrogeology and land use, San Antonio Region, Texas: U.S. Geological Survey Water-Resources Investigations Report 87-4116, Report: vi, 100 p.; 16 Plates, https://doi.org/10.3133/wri874116.","productDescription":"Report: vi, 100 p.; 16 Plates","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":55255,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4116/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55258,"rank":413,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4116/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55259,"rank":414,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4116/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55260,"rank":415,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4116/plate-16.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55257,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4116/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158130,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4116/report-thumb.jpg"},{"id":110243,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_46783.htm","linkFileType":{"id":5,"text":"html"},"description":"46783"},{"id":55261,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4116/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55245,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4116/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55246,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4116/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55247,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4116/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55248,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4116/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55249,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4116/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55250,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4116/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55251,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4116/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55252,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4116/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55253,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4116/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55254,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4116/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55256,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4116/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db6349f6","contributors":{"authors":[{"text":"Buszka, Paul M. 0000-0001-8218-826X pmbuszka@usgs.gov","orcid":"https://orcid.org/0000-0001-8218-826X","contributorId":1786,"corporation":false,"usgs":true,"family":"Buszka","given":"Paul","email":"pmbuszka@usgs.gov","middleInitial":"M.","affiliations":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true},{"id":27231,"text":"Indiana-Kentucky Water Science Center","active":true,"usgs":true}],"preferred":true,"id":196396,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":12115,"text":"ofr84734 - 1987 - Hydrology of area 51, northern Great Plains and Rocky Mountain coal provinces, Wyoming and Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:06:35","indexId":"ofr84734","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"84-734","title":"Hydrology of area 51, northern Great Plains and Rocky Mountain coal provinces, Wyoming and Montana","docAbstract":"This report is one of a series designed to characterize the hydrology of drainage basins within coal provinces, nationwide. Area 51 (in the Rocky Mountain Coal Province) includes all or part of the Shoshone, Bighorn, Greybull, Wind, and Popo Agie River drainage basins - a total of 11,800 sq mi. Area 51 contains more than 18 million tons of strippable bituminous coal and extensive deposits of subbituminous coal, in the arid and semiarid basins. The report represents a summary of results of water resources investigations of the U.S. Geological Survey, some of which were conducted in cooperation with State and other Federal agencies. More than 30 individual topics are discussed in brief texts that are accompanied by maps, graphs, photographs , and illustrations. Primary topics in the reports are physiography, resources and economy, surface-water quantity and quality, and groundwater. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84734","usgsCitation":"Peterson, D.A., Mora, K.L., Lowry, M.E., Rankl, J.G., Wilson, J.F., Lowham, H., and Ringen, B.H., 1987, Hydrology of area 51, northern Great Plains and Rocky Mountain coal provinces, Wyoming and Montana (WRI/OFR): U.S. Geological Survey Open-File Report 84-734, v, 73 p. :ill. (some col.), maps (some col.) ;28 cm., https://doi.org/10.3133/ofr84734.","productDescription":"v, 73 p. :ill. (some col.), maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":144783,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0734/report-thumb.jpg"},{"id":40143,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0734/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601fa8","contributors":{"authors":[{"text":"Peterson, David A. davep@usgs.gov","contributorId":1742,"corporation":false,"usgs":true,"family":"Peterson","given":"David","email":"davep@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":165124,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mora, K. L.","contributorId":55008,"corporation":false,"usgs":true,"family":"Mora","given":"K.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":165128,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lowry, Marlin E.","contributorId":52552,"corporation":false,"usgs":true,"family":"Lowry","given":"Marlin","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":165127,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rankl, James G.","contributorId":93026,"corporation":false,"usgs":true,"family":"Rankl","given":"James","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":165130,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wilson, James F. Jr.","contributorId":23546,"corporation":false,"usgs":true,"family":"Wilson","given":"James","suffix":"Jr.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":165126,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Lowham, H. W.","contributorId":8111,"corporation":false,"usgs":true,"family":"Lowham","given":"H. W.","affiliations":[],"preferred":false,"id":165125,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Ringen, Bruce H.","contributorId":73612,"corporation":false,"usgs":true,"family":"Ringen","given":"Bruce","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":165129,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":64273,"text":"gp953B - 1987 - Digital colored Bouguer gravity, free-air gravity, station location, and terrain maps for the conterminous United States","interactions":[],"lastModifiedDate":"2022-12-23T22:29:26.707245","indexId":"gp953B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"953","chapter":"B","title":"Digital colored Bouguer gravity, free-air gravity, station location, and terrain maps for the conterminous United States","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp953B","usgsCitation":"Simpson, R., Hildenbrand, T., Godson, R.H., and Kane, M.F., 1987, Digital colored Bouguer gravity, free-air gravity, station location, and terrain maps for the conterminous United States: U.S. Geological Survey Geophysical Investigations Map 953, Report: 1 p.; 2 Plates: 31.75 x 43.51 inches and 30.16 x 43.61 inches, https://doi.org/10.3133/gp953B.","productDescription":"Report: 1 p.; 2 Plates: 31.75 x 43.51 inches and 30.16 x 43.61 inches","costCenters":[],"links":[{"id":254308,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0953b/report-thumb.jpg"},{"id":250880,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0953b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":250879,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0953b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":250878,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0953b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":411034,"rank":5,"type":{"id":36,"text":"NGMDB Index 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 -76.35,\n                39.15\n              ],\n              [\n                -76.54272,\n                38.71762\n              ],\n              [\n                -76.32933,\n                38.08326\n              ],\n              [\n                -76.99,\n                38.23999\n              ],\n              [\n                -76.30162,\n                37.91794\n              ],\n              [\n                -76.25874,\n                36.9664\n              ],\n              [\n                -75.9718,\n                36.89726\n              ],\n              [\n                -75.86804,\n                36.55125\n              ],\n              [\n                -75.72749,\n                35.55074\n              ],\n              [\n                -76.36318,\n                34.80854\n              ],\n              [\n                -77.39763,\n                34.51201\n              ],\n              [\n                -78.05496,\n                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           29.48\n              ],\n              [\n                -95.60026,\n                28.73863\n              ],\n              [\n                -96.59404,\n                28.30748\n              ],\n              [\n                -97.14,\n                27.83\n              ],\n              [\n                -97.37,\n                27.38\n              ],\n              [\n                -97.38,\n                26.69\n              ],\n              [\n                -97.33,\n                26.21\n              ],\n              [\n                -97.14,\n                25.87\n              ],\n              [\n                -97.53,\n                25.84\n              ],\n              [\n                -98.24,\n                26.06\n              ],\n              [\n                -99.02,\n                26.37\n              ],\n              [\n                -99.3,\n                26.84\n              ],\n              [\n                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        -122.51201,\n                37.78339\n              ],\n              [\n                -122.95319,\n                38.11371\n              ],\n              [\n                -123.7272,\n                38.95166\n              ],\n              [\n                -123.86517,\n                39.76699\n              ],\n              [\n                -124.39807,\n                40.3132\n              ],\n              [\n                -124.17886,\n                41.14202\n              ],\n              [\n                -124.2137,\n                41.99964\n              ],\n              [\n                -124.53284,\n                42.76599\n              ],\n              [\n                -124.14214,\n                43.70838\n              ],\n              [\n                -124.02053,\n                44.6159\n              ],\n              [\n                -123.89893,\n                45.52341\n              ],\n              [\n                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     [\n                -113,\n                49\n              ],\n              [\n                -110.05,\n                49\n              ],\n              [\n                -107.05,\n                49\n              ],\n              [\n                -104.04826,\n                48.99986\n              ],\n              [\n                -100.65,\n                49\n              ],\n              [\n                -97.22872,\n                49.0007\n              ],\n              [\n                -95.15907,\n                49\n              ],\n              [\n                -95.15609,\n                49.38425\n              ],\n              [\n                -94.81758,\n                49.38905\n              ]\n            ]\n          ]\n        ]\n      },\n      \"properties\": {\n        \"name\": \"United States\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d580","contributors":{"authors":[{"text":"Simpson, R.W.","contributorId":76738,"corporation":false,"usgs":true,"family":"Simpson","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":270393,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hildenbrand, T.G.","contributorId":83892,"corporation":false,"usgs":true,"family":"Hildenbrand","given":"T.G.","email":"","affiliations":[],"preferred":false,"id":270394,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Godson, R. H.","contributorId":98719,"corporation":false,"usgs":true,"family":"Godson","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":270395,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kane, M. F.","contributorId":45708,"corporation":false,"usgs":true,"family":"Kane","given":"M.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":270392,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":42384,"text":"ofr87114 - 1987 - Selected ground-water data in the upper Mongaup River basin, Sullivan County, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:05:04","indexId":"ofr87114","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-114","title":"Selected ground-water data in the upper Mongaup River basin, Sullivan County, New York","docAbstract":"A set of four adjoining 7.5-minute quadrangle sheets that together depict the upper Mongaup River Basin in Sullivan County , N.Y., at 1:24,000 scale show the location, well yield, depth, water use, ownership, and date of ownership of wells, test holes , and springs. Most wells that tap stratified-drift deposits have high yields (50 to 300 gal/min) and are used for public supply. Bedrock wells have smaller yields and are generally used for domestic supply. The data were compiled from a previous U.S. Geological Survey, countywide, groundwater resources report and from unpublished data. (USGS)","language":"ENGLISH","doi":"10.3133/ofr87114","usgsCitation":"Wolcott, S.W., 1987, Selected ground-water data in the upper Mongaup River basin, Sullivan County, New York: U.S. Geological Survey Open-File Report 87-114, 4 maps ;58 x 44 cm., on sheet 69 x 48 cm., folded in envelope 34 x 25 cm., https://doi.org/10.3133/ofr87114.","productDescription":"4 maps ;58 x 44 cm., on sheet 69 x 48 cm., folded in envelope 34 x 25 cm.","costCenters":[],"links":[{"id":136518,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":80149,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0114/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80150,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0114/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80151,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0114/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80152,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0114/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f96da","contributors":{"authors":[{"text":"Wolcott, Stephen W.","contributorId":93458,"corporation":false,"usgs":true,"family":"Wolcott","given":"Stephen","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":226379,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14088,"text":"ofr8720 - 1987 - Determination of organic content from formation-density logs, Devonian-Mississippian Woodford Shale, Anadarko Basin, Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:06:53","indexId":"ofr8720","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-20","title":"Determination of organic content from formation-density logs, Devonian-Mississippian Woodford Shale, Anadarko Basin, Oklahoma","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8720","usgsCitation":"Hester, T., and Schmoker, J., 1987, Determination of organic content from formation-density logs, Devonian-Mississippian Woodford Shale, Anadarko Basin, Oklahoma: U.S. Geological Survey Open-File Report 87-20, i, 11 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr8720.","productDescription":"i, 11 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":147137,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0020/report-thumb.jpg"},{"id":42732,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0020/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6676f2","contributors":{"authors":[{"text":"Hester, T.C.","contributorId":93054,"corporation":false,"usgs":true,"family":"Hester","given":"T.C.","email":"","affiliations":[],"preferred":false,"id":168907,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schmoker, J. W.","contributorId":69964,"corporation":false,"usgs":true,"family":"Schmoker","given":"J. W.","affiliations":[],"preferred":false,"id":168906,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26719,"text":"wri874207 - 1987 - Technique for estimating flood-peak discharges and frequencies on rural streams in Illinois","interactions":[],"lastModifiedDate":"2012-02-02T00:08:30","indexId":"wri874207","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-4207","title":"Technique for estimating flood-peak discharges and frequencies on rural streams in Illinois","docAbstract":"Flood-peak discharges and frequencies are presented for 394 gaged sites in Illinois, Indiana, and Wisconsin for recurrence intervals ranging from 2 to 100 years. A technique is presented for estimating flood-peak discharges at recurrence intervals ranging from 2 to 500 years for nonregulated streams in Illinois with drainage areas ranging from 0.02 to 10,000 square miles. Multiple-regression analyses, using basin characteristics and peak streamflow data from 268 of the 394 gaged sites, were used to define the flood-frequency relation. The most significant independent variables for estimating flood-peak discharge are drainage area, slope, rainfall intensity and a regional factor. Examples are given to show a step-by-step procedure in calculating a 50-year flood for a site on an ungaged stream, a site at a gaged location, and a site near a gaged location. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874207","usgsCitation":"Curtis, G., 1987, Technique for estimating flood-peak discharges and frequencies on rural streams in Illinois: U.S. Geological Survey Water-Resources Investigations Report 87-4207, v, 79 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874207.","productDescription":"v, 79 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":2054,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://il.water.usgs.gov/pubsearch/reports.cgi/view?series=WRIR&number=87-4207","linkFileType":{"id":5,"text":"html"}},{"id":158251,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4207/report-thumb.jpg"},{"id":55593,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4207/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db6862d3","contributors":{"authors":[{"text":"Curtis, G.W.","contributorId":69159,"corporation":false,"usgs":true,"family":"Curtis","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":196884,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26829,"text":"wri854237 - 1987 - Water resources of the Rio Grande de  Añasco-lower valley, Puerto Rico","interactions":[],"lastModifiedDate":"2022-01-26T20:38:32.978974","indexId":"wri854237","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"85-4237","title":"Water resources of the Rio Grande de  Añasco-lower valley, Puerto Rico","docAbstract":"<p>A large amount of water suitable for most uses is available in the lower Rio Grande de Anasco Valley, the major source of which is the Rio Grande de Anasco which contributes about 95% of the surface water inflow to the lower valley. River flow at El Espino exceeds 100 cu ft/sec about 85% of the time and 200 cu ft/sec 50% of the time. Average daily flow for the driest months of the year (February, March, and April), is almost always &lt;100 cu ft/sec. In contrast, the average daily flow for the wettest, months of the year (September, October, and November), is &gt; 120 cu ft/sec. During the study period, flows of the Rio Canas averaged about 5 cu ft/sec. The lower valley is underlain by igneous rocks that have been eroded to depths of 350 ft or more below sea level. The valley is filled with 250 ft or more of limestone and clay, that in turn is overlain by as much as 100 ft of alluvium. The amount of groundwater available is unknown. There are large volumes of water in the saturated mostly fine-grained alluvium of Zone II, but as a whole the alluvium does not yield water readily to wells. Sand and gravel deposits associated with former river channels yield an estimated 100 to 150 gal/min to wells. The principal source of groundwater is the limestone of Zone III, that reportedly yields as much as 500 gal/min to wells. The quality of surface water especially that of Rio Grande de Anasco was very good. Specific conductance seldom exceeds 250 microsiemens/cm, even at low flows. Both salinity and sodium are low, falling in the Cl-S1 irrigation water classification. Water quality in the lower 5,000 ft or so of the river was affected by saltwater encroachment from the sea. The water quality of the other streams and canals in the lower valley was variable depending on susceptibility of saltwater encroachment, contamination from man-made sources, and concentration of minerals by evapotranspiration. Specific conductance however seldom exceeded 500 microsiemens/cm and the water usually falls in the C1-S2 classification. The quality of groundwater in the alluvial aquifer was about the same as that of the water of the Rio Grande de Anasco except where encroached by saltwater or contaminated. The water from the limestone was more mineralized than that of the alluvium (about 600 to 700 microsiemens/cm), and was somewhat similar to that of the smaller streams and canals in the valley.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854237","usgsCitation":"Diaz, J.R., and Jordan, D., 1987, Water resources of the Rio Grande de  Añasco-lower valley, Puerto Rico: U.S. Geological Survey Water-Resources Investigations Report 85-4237, vii, 48 p., https://doi.org/10.3133/wri854237.","productDescription":"vii, 48 p.","costCenters":[],"links":[{"id":394913,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36385.htm"},{"id":55720,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4237/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123315,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4237/report-thumb.jpg"}],"country":"United States","state":"Puerto Rico","otherGeospatial":"Rio Grande de Anasco - lower valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -67.23770141601562,\n              18.248915760544524\n            ],\n            [\n              -67.06878662109375,\n              18.248915760544524\n            ],\n            [\n              -67.06878662109375,\n              18.293253626696984\n            ],\n            [\n              -67.23770141601562,\n              18.293253626696984\n            ],\n            [\n              -67.23770141601562,\n              18.248915760544524\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f03b4","contributors":{"authors":[{"text":"Diaz, Jose Raul","contributorId":18363,"corporation":false,"usgs":true,"family":"Diaz","given":"Jose","email":"","middleInitial":"Raul","affiliations":[],"preferred":false,"id":197081,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jordan, Donald G.","contributorId":9519,"corporation":false,"usgs":true,"family":"Jordan","given":"Donald G.","affiliations":[],"preferred":false,"id":197080,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44035,"text":"ofr87340S - 1987 - Thickness of Jurassic rocks, Powder River basin, Wyoming and Montana","interactions":[],"lastModifiedDate":"2018-01-08T13:27:50","indexId":"ofr87340S","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-340","chapter":"S","title":"Thickness of Jurassic rocks, Powder River basin, Wyoming and Montana","language":"ENGLISH","doi":"10.3133/ofr87340S","issn":"ma","usgsCitation":"Fox, J.E., and Higley, D.K., 1987, Thickness of Jurassic rocks, Powder River basin, Wyoming and Montana: U.S. Geological Survey Open-File Report 87-340, 1 map :photocopy ;55 x 55 cm., on sheet 78 x 79 cm., https://doi.org/10.3133/ofr87340S.","productDescription":"1 map :photocopy ;55 x 55 cm., on sheet 78 x 79 cm.","costCenters":[],"links":[{"id":173360,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81451,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0340s/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a55e4b07f02db62ce90","contributors":{"authors":[{"text":"Fox, J. E.","contributorId":79080,"corporation":false,"usgs":true,"family":"Fox","given":"J.","middleInitial":"E.","affiliations":[],"preferred":false,"id":229032,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Higley, Debra K. 0000-0001-8024-9954 higley@usgs.gov","orcid":"https://orcid.org/0000-0001-8024-9954","contributorId":152663,"corporation":false,"usgs":true,"family":"Higley","given":"Debra","email":"higley@usgs.gov","middleInitial":"K.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":229031,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1903,"text":"wsp2248 - 1987 - Ground water in the southeastern Uinta Basin, Utah and Colorado","interactions":[{"subject":{"id":9549,"text":"ofr83271 - 1983 - Ground water in the southeastern Uinta Basin, Utah and Colorado","indexId":"ofr83271","publicationYear":"1983","noYear":false,"title":"Ground water in the southeastern Uinta Basin, Utah and Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":1903,"text":"wsp2248 - 1987 - Ground water in the southeastern Uinta Basin, Utah and Colorado","indexId":"wsp2248","publicationYear":"1987","noYear":false,"title":"Ground water in the southeastern Uinta Basin, Utah and Colorado"},"id":1}],"lastModifiedDate":"2017-08-31T16:24:02","indexId":"wsp2248","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"2248","title":"Ground water in the southeastern Uinta Basin, Utah and Colorado","docAbstract":"<p>The potential for developing oil-shale resources in the southeastern Uinta Basin of Utah and Colorado has created the need for information on the quantity and quality of water available in the area. This report describes the availability and chemical quality of ground water, which might provide a source or supplement of water supply for an oil-shale industry. </p><p>Ground water in the southeastern Uinta Basin occurs in three major aquifers. Alluvial aquifers of small areal extent are present i n val ley-f i 11 deposits of six major drainages. Consolidated-rock aquifers include the birds's-nest aquifer i n the Parachute Creek Member of the G reen River Formation, which is limited to the central part of the study area; and the Douglas Creek aquifer, which includes parts of the Douglas Creek Member of the Green River Formation and parts of the intertonguing Renegade Tongue of the Wasatch Formation; this aquifer underlies most of the study area.</p><p>The alluvial aquifers are recharged by infiltration of streamflow and leakage from consolidated-rock aquifers. Recharge is estimated to average about 32,000 acre-feet per year. Discharge from alluvial aquifers, primarily by evapotranspiration, also averages about 32,000 acre-feet per year. The estimated volume of recoverable water in storage in alluvial aquifers is about 200,000 acre-feet. Maximum yields to individual wells are less than 1,000 gallons per minute.</p><p>Recharge to the bird's-nest aquifer, primarily from stream infiltration and downward leakage from the overlying Uinta Formation, is estimated to average 670 acre-feet per year. Discharge from the bird's-nest aquifer, which is primarily by seepage to Bitter Creek and the White River, is estimated to be at 670 acre-feet per year. The estimated volume of recoverable water in storage in the bird's-nest aquifer is 1.9 million acre-feet. Maximum yields to individual wells in some areas may be as much as 5,000 gallons per minute. </p><p>A digital-computer model of the flow system was used to evaluate the effects of oil-shale development on the bird's-nest aquifer at the Federal lease tracts Ua and Ub. Results of model simulations indicate that during construction of a vertical access shaft, a pumping rate of about 900 gallons per minute would be required to dewaterthe aquifer. The model also indicates that the construction of a proposed reservoir on the White River may raise water levels in the bird's-nest aquifer near the reservoir site by as much as 45 feet.</p><p>The flow model was used to evaluate the potential ground-water supply available for oil-shale development in the vicinity of the Federal lease tracts Ua and Ub. The results of the simulation indicate that bird's-nest aquifer could supply about 10,000 acre-feet of water per year at that site, for a period of 20 years. Downdraw after 20 years of pumping would exceed 250 feet near the simulated well field. Based on the results of the model simulation, it is estimated that the aquifer could simultaneously supply another 10,000 acre-feet of water per year in the northern part of the study area, but some interference between well fields could be expected.</p><p>The Douglas Creek aquifer is recharged by precipitation and stream infiltration at an average rate of about 20.000 acre-feet per year. Discharge is estimated to be about the same and is primarily through springs and diffuse seepage. The estimated volume of recoverable water in storage is 16 million acre-feet. Maximum yields to individual wells are estimated to be less than 500 gallons per minute.</p><p>A model of the flow system in the Douglas Creek aquifer indicates that the aquifer could supply about 700 acre-feet of water per year for oil-shale development at Federal lease tracts Ua and Ub and at the TOSCO Corp. site. After 20 years of pumping, water levels in production wells would be near the base of the aquifer. Based on the results of the model simulation, it is estimated that the aquifer could supply another 700 acre-feet of water per year in the southern part of the modeled area, but some interference between wells could be expected. </p><p>Chemical quality of the ground water in the southeastern Uinta Basin varies considerably. Water from alluvial wells ranges from about 440 to 27,800 milligrams per liter of dissolved solids. Water from two consolidated-rock aquifers has dissolved-solids concentrations ranging from 870 to 5,810 milligrams per liter in the bird's-nest aquifer, and from 640 to 6,100 milligrams per liter in the Douglas Creek aquifer. Water from alluvial wells generally is a sodium sulfate type, whereas water in both the consolidated-rock aquifers generally changes from a sodium sulfate type to a sodium bicarbonate type. All ground water is very alkaline, and the alluvial aquifers contain very hard water. None of the water is suitable for public supply, but all the water could be used for industrial purposes such as washing and cooling.</p><p>Changes in chemical composition of the ground water can be attributed to several physiochemical processes, including mineral precipitation and dissolution, oxidation and reduction, mixing, ion exchange, and evaporative concentration. Mass-transfer modeling of these processes shows how they can account for the variability in the ground-water quality. The mass-transfer model of the Bitter Creek alluvial aquifer shows that evaporative concentration, combined with precipitation of calcite, dolomite, gypsum, and release of carbon dioxide to the atmosphere results in the documented changes in the pH and dissolved solids in the water. The water-quality changes in the consolidated-rock aquifers are a result of precipitation of calcium carbonate and perhaps dolomite (calcium magnesium carbonate) with the reduction of sulfate by organic carbon, as well as ion exchange of magnesium for sodium. These processes result in large values of pH and alkalinity in the water. </p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp2248","usgsCitation":"Holmes, W.F., and Kimball, B.A., 1987, Ground water in the southeastern Uinta Basin, Utah and Colorado: U.S. Geological Survey Water Supply Paper 2248, Report: vi, 47 p.; Plate: 20.50 in. x 25.00 in., https://doi.org/10.3133/wsp2248.","productDescription":"Report: vi, 47 p.; Plate: 20.50 in. x 25.00 in.","numberOfPages":"55","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":27200,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2248/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138548,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2248/report-thumb.jpg"},{"id":27199,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2248/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado, Utah","otherGeospatial":"Uinta Basin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d745","contributors":{"authors":[{"text":"Holmes, Walter F.","contributorId":31737,"corporation":false,"usgs":true,"family":"Holmes","given":"Walter","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":144340,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kimball, Briant A. bkimball@usgs.gov","contributorId":533,"corporation":false,"usgs":true,"family":"Kimball","given":"Briant","email":"bkimball@usgs.gov","middleInitial":"A.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":144339,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29757,"text":"wri874002 - 1987 - Water quality of Lake Tuscaloosa and streamflow and water quality of selected tributaries to Lake Tuscaloosa, Alabama, 1982-86","interactions":[],"lastModifiedDate":"2012-02-02T00:08:51","indexId":"wri874002","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-4002","title":"Water quality of Lake Tuscaloosa and streamflow and water quality of selected tributaries to Lake Tuscaloosa, Alabama, 1982-86","docAbstract":"Lake Tuscaloosa, created in 1969 by the impoundment of North River, provides the primary water supply for Tuscaloosa, Alabama , and surrounding areas. This report describes the percent contribution of major tributaries to the mean inflow to the lake; water quality; and changes in water quality in the lake and selected tributaries. During base flow, about 60% of the total flow into Lake Tuscaloosa is contributed by Binion and Carroll Creeks, which drain only 22% of the Lake Tuscaloosa basin. Binion and Carroll Creek basins are underlain primarily by sand and gravel deposits of the Coker Formation. Mean inflow to the lake was 1,150 cu ft/sec during 1983, a wet year, and 450 cu ft/sec during 1985, a relatively dry year. More than 80% of the total inflow during both years was contributed by North River and Binion, Cripple, and Carroll Creeks. About 59% was contributed by North River during those years. Except for pH, sulfate, and dissolved and total recoverable iron and manganese, the water quality of the tributaries is generally within drinking water limits and acceptable for most uses. The water quality of Lake Tuscaloosa is generally within drinking water limits and acceptable for most uses. The maximum and median concentrations of sulfate increased every year at the dam from 1979 to 1985 (7.2 to 18 mg/L and 6.2 to 14 mg/L, respectively). The dissolved solids concentrations for water at the dam have varied (1979-86) from 27 to 43 mg/L; the sulfate, 5.2 to 18 mg/L; and the dissolved iron, 10 to 250 micrograms/L--all within the recommended drinking water limits. However, concentrations of dissolved manganese and total recoverable iron and manganese at the dam commonly exceeded the recommended drinking water limits. In November 1985, after the summer warmup and increase in biological activity, the water quality at five depth profiles sites on Lake Tuscaloosa was acceptable for most uses, generally. However, a dissolved oxygen concentration of 1 mg/L or less was observed within 5 to 10 ft of the bottom for several depth profiles. At depths &gt; 35 to 40 ft (out of a total depth of about 50 to 100 ft) the dissolved oxygen concentration was &lt; 5 mg/L at several sites. By mid-January 1986, the temperature and dissolved oxygen depth profiles were virtually constant from top to bottom of the lake at all five sites; this indicated that lake turnover was complete. However, significant variation existed in pH depth profiles. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874002","usgsCitation":"Slack, L.J., 1987, Water quality of Lake Tuscaloosa and streamflow and water quality of selected tributaries to Lake Tuscaloosa, Alabama, 1982-86: U.S. Geological Survey Water-Resources Investigations Report 87-4002, vi, 64 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874002.","productDescription":"vi, 64 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159320,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4002/report-thumb.jpg"},{"id":58552,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4002/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cfe4b07f02db546249","contributors":{"authors":[{"text":"Slack, L. J.","contributorId":44157,"corporation":false,"usgs":true,"family":"Slack","given":"L.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":202067,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":43801,"text":"ofr87157 - 1987 - Geologic map of the Wind Gap Quadrangle, Northampton and Monroe counties, Pennsylvania","interactions":[],"lastModifiedDate":"2012-02-02T00:04:55","indexId":"ofr87157","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-157","title":"Geologic map of the Wind Gap Quadrangle, Northampton and Monroe counties, Pennsylvania","language":"ENGLISH","doi":"10.3133/ofr87157","usgsCitation":"Epstein, J., 1987, Geologic map of the Wind Gap Quadrangle, Northampton and Monroe counties, Pennsylvania: U.S. Geological Survey Open-File Report 87-157, 1 map :photocopy ;58 x 44 cm., on sheet 77 x 111 cm. +1 pamphlet (9 p. ; 28 cm.), https://doi.org/10.3133/ofr87157.","productDescription":"1 map :photocopy ;58 x 44 cm., on sheet 77 x 111 cm. +1 pamphlet (9 p. ; 28 cm.)","costCenters":[],"links":[{"id":134583,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db68929e","contributors":{"authors":[{"text":"Epstein, Jack Burton","contributorId":64625,"corporation":false,"usgs":true,"family":"Epstein","given":"Jack Burton","affiliations":[],"preferred":false,"id":228705,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44419,"text":"wri864067 - 1987 - Lithology and base of the surficial aquifer system, Palm Beach County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:10:31","indexId":"wri864067","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"86-4067","title":"Lithology and base of the surficial aquifer system, Palm Beach County, Florida","docAbstract":"The surficial aquifer system is a major source of freshwater in Palm Beach County. In 1982, public supply withdrawals from the aquifer system totaled 33,543 million gallons, 77.5% of total public supply withdrawals. To evaluate the aquifer system and its geologic framework, a cooperative study with Palm Beach County was begun in 1982 by the U.S. Geological Survey. The surficial aquifer system in Palm Beach County is composed primarily of sand, sandstone, shell, silt, calcareous clay (marl), and limestone deposited during the Pleistocene and Pliocene epochs. In the western two-thirds of Palm Beach County, sediments in the aquifer system are poorly consolidated sand, shell, and sandy limestone. Owing to interspersed calcareous clays and silt and very poorly sorted materials, permeabilities in this zone of the aquifer system are relatively low. Two other zones of the aquifer system are found in the eastern one-third of the county where the sediments are appreciably more permeable than in the west due to better sorting and less silt and clay content. The location of more detailed lithologic logs for wells in these sections, along with data from nearby wells, allowed enhanced interpretation and depiction of the lithology which had previously been generalized. The most permeable zone of the aquifer system in this area is characterized by highly developed secondary porosity where infiltrating rainwater and solution by groundwater have removed calcitic-cementing materials from the sediments to produce interconnected cavities. Increased permeability in the aquifer system is generally coincident with the eastern boundary of the overlying organic soils and Lake Flirt Marl. Lithologic logs of wells in Palm Beach County indicate that sediments forming the aquifer system were deposited directly on the erosional surface of the Hawthorn Formation in some areas. In other locations in the county, lithologic logs indicate that the base of the aquifer system was formed by fluvial deposits containing erosional materials from the Tamiami and Hawthorn Formations and Caloosahatchee Marl. (Lantz-PTT)","language":"ENGLISH","doi":"10.3133/wri864067","usgsCitation":"Miller, W.L., 1987, Lithology and base of the surficial aquifer system, Palm Beach County, Florida: U.S. Geological Survey Water-Resources Investigations Report 86-4067, 1 map : col. ; 32 x 37 cm., on sheet 62 x 89 cm., folded in envelope 31 x 23 cm., https://doi.org/10.3133/wri864067.","productDescription":"1 map : col. ; 32 x 37 cm., on sheet 62 x 89 cm., folded in envelope 31 x 23 cm.","costCenters":[],"links":[{"id":173112,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81717,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4067/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635c14","contributors":{"authors":[{"text":"Miller, Wesley L.","contributorId":91859,"corporation":false,"usgs":true,"family":"Miller","given":"Wesley","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":229732,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44408,"text":"wri864185 - 1987 - Streamflow gain and loss of selected streams in northern Arkansas","interactions":[],"lastModifiedDate":"2019-08-20T09:48:20","indexId":"wri864185","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"86-4185","title":"Streamflow gain and loss of selected streams in northern Arkansas","docAbstract":"This map shows streamflow gain and loss measurements (seepage runs) on the Crooked, Osage, and Spavinaw Creeks, and Illinois, Kings, Mulberry, Spring, and Strawberry Rivers during the low-flow conditions from September 1982 to October 1984. Data indicated that streamflow gains and losses resulted from differences in lithology of the predominately carbonate rocks and from the presence of faults. The Kings and Strawberry Rivers and Osage Creek were gaining streams throughout their length, however wastewater discharges precluded an accurate determination on Osage Creek. Crooked and Spavinaw Creeks and the Illinois, Spring, and Mulberry Rivers generally were gaining streams throughout most of their lengths although short losing reaches were identified. The largest gains in streamflow generally occurred were Mississippian formation predominated near the streams. Faults that intersected the stream channels primarily were responsible for streamflow losses. The specific conductance of water increased in the stream reaches that had the most significant streamflow gains. The specific conductance of water in tributaries was generally higher than that in larger streams. (Author 's abstract)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri864185","usgsCitation":"Freiwald, D.A., 1987, Streamflow gain and loss of selected streams in northern Arkansas: U.S. Geological Survey Water-Resources Investigations Report 86-4185, 8 Plates: 39.87 x 39.18 inches or smaller, https://doi.org/10.3133/wri864185.","productDescription":"8 Plates: 39.87 x 39.18 inches or smaller","costCenters":[],"links":[{"id":173026,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4185/report-thumb.jpg"},{"id":366691,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4185/plate-1-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":366684,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4185/plate-4-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":366685,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4185/plate-4-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":366686,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4185/plate-3-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":366687,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4185/plate-3-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":366688,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4185/plate-2-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":366689,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4185/plate-2-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":366690,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4185/plate-1-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arkansas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -94.6142578125,\n              35.28150065789119\n            ],\n            [\n              -89.69238281249999,\n              35.28150065789119\n            ],\n            [\n              -89.69238281249999,\n              36.527294814546245\n            ],\n            [\n              -94.6142578125,\n              36.527294814546245\n            ],\n            [\n              -94.6142578125,\n              35.28150065789119\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4e09","contributors":{"authors":[{"text":"Freiwald, David A. freiwald@usgs.gov","contributorId":226,"corporation":false,"usgs":true,"family":"Freiwald","given":"David","email":"freiwald@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":229717,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20731,"text":"ofr87450Y - 1987 - Oil and gas resources of the Cincinnati arch, Ohio, Indiana, Kentucky, and Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:07:48","indexId":"ofr87450Y","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"87-450","chapter":"Y","title":"Oil and gas resources of the Cincinnati arch, Ohio, Indiana, Kentucky, and Tennessee","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87450Y","usgsCitation":"Ryder, R.T., 1987, Oil and gas resources of the Cincinnati arch, Ohio, Indiana, Kentucky, and Tennessee: U.S. Geological Survey Open-File Report 87-450, i, 30 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr87450Y.","productDescription":"i, 30 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":153963,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0450y/report-thumb.jpg"},{"id":50285,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0450y/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691d97","contributors":{"authors":[{"text":"Ryder, R. T.","contributorId":96673,"corporation":false,"usgs":true,"family":"Ryder","given":"R.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":183145,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44405,"text":"wri864178 - 1987 - Water-level maps of the alluvial aquifer in eastern Arkansas, 1985","interactions":[],"lastModifiedDate":"2019-08-20T09:50:07","indexId":"wri864178","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"86-4178","title":"Water-level maps of the alluvial aquifer in eastern Arkansas, 1985","docAbstract":"Maps shown in this report show the potentiometric surface of the alluvial aquifer before and after the pumping season of 1985, the depth-to-water in the spring of 1985, and the change in water levels between the spring of 1980 and the spring of 1985. Hydrographs showing long-term water-level changes in the alluvial aquifer are also included. (Rubinstein-PTT)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri864178","usgsCitation":"Plafcan, M., and Fugitt, D., 1987, Water-level maps of the alluvial aquifer in eastern Arkansas, 1985: U.S. Geological Survey Water-Resources Investigations Report 86-4178, 1 Plate: 58.14 x 38.46 inches, https://doi.org/10.3133/wri864178.","productDescription":"1 Plate: 58.14 x 38.46 inches","costCenters":[],"links":[{"id":172929,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4178/report-thumb.jpg"},{"id":366692,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4178/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arkansas","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cee4b07f02db54538d","contributors":{"authors":[{"text":"Plafcan, Maria","contributorId":20338,"corporation":false,"usgs":true,"family":"Plafcan","given":"Maria","email":"","affiliations":[],"preferred":false,"id":229711,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fugitt, D.T.","contributorId":9334,"corporation":false,"usgs":true,"family":"Fugitt","given":"D.T.","email":"","affiliations":[],"preferred":false,"id":229710,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44409,"text":"wri864189 - 1987 - Potentiometric-surface of the water-table, Magothy, and Lloyd aquifers on Long Island, New York, in 1984","interactions":[],"lastModifiedDate":"2022-12-27T22:56:37.235028","indexId":"wri864189","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"86-4189","title":"Potentiometric-surface of the water-table, Magothy, and Lloyd aquifers on Long Island, New York, in 1984","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864189","usgsCitation":"Doriski, T.P., 1987, Potentiometric-surface of the water-table, Magothy, and Lloyd aquifers on Long Island, New York, in 1984: U.S. Geological Survey Water-Resources Investigations Report 86-4189, 8 Plates: 36.59 x 22.39 inches or smaller, https://doi.org/10.3133/wri864189.","productDescription":"8 Plates: 36.59 x 22.39 inches or smaller","costCenters":[],"links":[{"id":411103,"rank":10,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36611.htm","linkFileType":{"id":5,"text":"html"}},{"id":81703,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4189/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81702,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4189/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81701,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4189/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81700,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4189/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81696,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4189/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81699,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4189/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81697,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4189/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81698,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4189/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":173585,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"New York","otherGeospatial":"Long Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -73.9402237135873,\n              40.535165012909374\n            ],\n            [\n              -73.32737821143094,\n              40.585714917518914\n            ],\n            [\n              -72.20674643605918,\n              40.85113756952231\n            ],\n            [\n              -71.84254110906322,\n              41.08647309372546\n            ],\n            [\n              -72.28028789631803,\n              41.17615490662308\n            ],\n            [\n              -72.64799519761131,\n              40.9913822898217\n            ],\n            [\n              -73.16278541942312,\n              41.00459756051177\n            ],\n            [\n              -73.19780516240344,\n              40.94114010013382\n            ],\n            [\n              -73.36589992870944,\n              40.951720582036614\n            ],\n            [\n              -73.54800259220742,\n              40.94378537953705\n            ],\n            [\n              -73.7336072300036,\n              40.88291715045801\n            ],\n            [\n              -73.89119607341503,\n              40.78488113258558\n            ],\n            [\n              -73.99625530235596,\n              40.72652073479111\n            ],\n            [\n              -74.05929083972103,\n              40.64951285822099\n            ],\n            [\n              -74.01726714814431,\n              40.58305534791833\n            ],\n            [\n              -73.9402237135873,\n              40.535165012909374\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad3e4b07f02db68202b","contributors":{"authors":[{"text":"Doriski, Thomas P.","contributorId":20301,"corporation":false,"usgs":true,"family":"Doriski","given":"Thomas","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":229718,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44402,"text":"wri874162 - 1987 - Potentiometric surface of the alluvial aquifer and hydrologic conditions in the Guayama quadrangle, Puerto Rico, March 1986","interactions":[],"lastModifiedDate":"2019-08-20T09:53:27","indexId":"wri874162","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-4162","title":"Potentiometric surface of the alluvial aquifer and hydrologic conditions in the Guayama quadrangle, Puerto Rico, March 1986","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri874162","usgsCitation":"Dacosta, R., and Gómez-Gómez, F., 1987, Potentiometric surface of the alluvial aquifer and hydrologic conditions in the Guayama quadrangle, Puerto Rico, March 1986: U.S. Geological Survey Water-Resources Investigations Report 87-4162, 1 Plate: 28.69 x 21.54 inches, https://doi.org/10.3133/wri874162.","productDescription":"1 Plate: 28.69 x 21.54 inches","costCenters":[],"links":[{"id":168555,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4162/report-thumb.jpg"},{"id":366693,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4162/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","otherGeospatial":"Puerto Rico","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -66.21768951416016,\n              17.92157608317564\n            ],\n            [\n              -66.07624053955078,\n              17.92157608317564\n            ],\n            [\n              -66.07624053955078,\n              17.989835742155027\n            ],\n            [\n              -66.21768951416016,\n              17.989835742155027\n            ],\n            [\n              -66.21768951416016,\n              17.92157608317564\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682ed0","contributors":{"authors":[{"text":"Dacosta, Rafael","contributorId":93060,"corporation":false,"usgs":true,"family":"Dacosta","given":"Rafael","email":"","affiliations":[],"preferred":false,"id":229706,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gómez-Gómez, Fernando","contributorId":31366,"corporation":false,"usgs":true,"family":"Gómez-Gómez","given":"Fernando","affiliations":[],"preferred":false,"id":229705,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":50778,"text":"ofr87227 - 1987 - Selected geohydrologic characteristics of the Patapsco aquifers at Chalk Point, Prince Georges County, Maryland","interactions":[],"lastModifiedDate":"2012-02-02T00:11:35","indexId":"ofr87227","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-227","title":"Selected geohydrologic characteristics of the Patapsco aquifers at Chalk Point, Prince Georges County, Maryland","language":"ENGLISH","doi":"10.3133/ofr87227","usgsCitation":"Mack, F., 1987, Selected geohydrologic characteristics of the Patapsco aquifers at Chalk Point, Prince Georges County, Maryland: U.S. Geological Survey Open-File Report 87-227, iv, 36 p. : ill., map ; 28 cm., https://doi.org/10.3133/ofr87227.","productDescription":"iv, 36 p. : ill., map ; 28 cm.","costCenters":[],"links":[{"id":177610,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa575","contributors":{"authors":[{"text":"Mack, Frederick K.","contributorId":95858,"corporation":false,"usgs":true,"family":"Mack","given":"Frederick K.","affiliations":[],"preferred":false,"id":242287,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":50779,"text":"ofr87313 - 1987 - Issues in digital cartographic data standards; Report 9; A final bibliography for digital data standards","interactions":[],"lastModifiedDate":"2012-02-02T00:11:35","indexId":"ofr87313","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-313","title":"Issues in digital cartographic data standards; Report 9; A final bibliography for digital data standards","language":"ENGLISH","doi":"10.3133/ofr87313","usgsCitation":"Moellering, H., 1987, Issues in digital cartographic data standards; Report 9; A final bibliography for digital data standards: U.S. Geological Survey Open-File Report 87-313, 71 p.; 28 cm., https://doi.org/10.3133/ofr87313.","productDescription":"71 p.; 28 cm.","costCenters":[],"links":[{"id":177611,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0313/report-thumb.jpg"},{"id":86347,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0313/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db667010","contributors":{"authors":[{"text":"Moellering, Harold","contributorId":71626,"corporation":false,"usgs":true,"family":"Moellering","given":"Harold","email":"","affiliations":[],"preferred":false,"id":242288,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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