{"pageNumber":"333","pageRowStart":"8300","pageSize":"25","recordCount":10961,"records":[{"id":47001,"text":"ofr86537 - 1987 - Estimated water use in St. Croix, U.S. Virgin Islands, October 1983-September 1985","interactions":[],"lastModifiedDate":"2024-02-15T20:55:44.618906","indexId":"ofr86537","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":"86-537","title":"Estimated water use in St. Croix, U.S. Virgin Islands, October 1983-September 1985","docAbstract":"<p>St. Croix is the largest of the U.S. Virgin Islands, with a land area of 82 square miles. The island is located about 60 miles east-southeast of Puerto Rico and about 40 miles south of St. Thomas and St. John (fig. 1). St. Croix has experienced a dramatic increase in its population over the last 25 years, growing from about 15,000 inhabitants in 1960 to about 54,000 in 1985 (personal communication, U.S. Virgin Islands Planning Office). Tourism development has also resulted in a large transient population with demands for services and facilities. The population and economic growth of St. Croix has resulted in a significant increase in the demand and supply of water (fig. 2).</p>","conferenceTitle":"Proceedings of the Third Caribbean Islands Water-Resources Congress","conferenceDate":"July 22-25, 1986","conferenceLocation":"U.S. Virgin Islands","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr86537","collaboration":"Prepared in cooperation with the Caribbean Research Institute","usgsCitation":"Torres-Sierra, H., 1987, Estimated water use in St. Croix, U.S. Virgin Islands, October 1983-September 1985: U.S. Geological Survey Open-File Report 86-537, 1 Plate: 37.87 x 21.93 inches, https://doi.org/10.3133/ofr86537.","productDescription":"1 Plate: 37.87 x 21.93 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":156,"text":"Caribbean Water Science Center","active":true,"usgs":true}],"links":[{"id":425697,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0537/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":172103,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0537/report-thumb.jpg"}],"country":"United States","state":"Virgin Islands","otherGeospatial":"St. Croix","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -65.0348092675643,\n              17.84390563272973\n            ],\n            [\n              -65.0348092675643,\n              17.596107260870596\n            ],\n            [\n              -64.44477354748643,\n              17.596107260870596\n            ],\n            [\n              -64.44477354748643,\n              17.84390563272973\n            ],\n            [\n              -65.0348092675643,\n              17.84390563272973\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcc14","contributors":{"authors":[{"text":"Torres-Sierra, Heriberto","contributorId":97913,"corporation":false,"usgs":true,"family":"Torres-Sierra","given":"Heriberto","email":"","affiliations":[],"preferred":false,"id":234472,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":46800,"text":"ofr87674 - 1987 - Distribution, thickness, overburden, and structure contour maps of potentially recoverable lignite beds in the eastern part of the Fort Peck Indian Reservation, Montana","interactions":[],"lastModifiedDate":"2022-12-26T15:44:12.571196","indexId":"ofr87674","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":"87-674","title":"Distribution, thickness, overburden, and structure contour maps of potentially recoverable lignite beds in the eastern part of the Fort Peck Indian Reservation, Montana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr87674","usgsCitation":"Hardie, J.K., and Arndt, H.H., 1987, Distribution, thickness, overburden, and structure contour maps of potentially recoverable lignite beds in the eastern part of the Fort Peck Indian Reservation, Montana: U.S. Geological Survey Open-File Report 87-674, 21 Plates: 41.56 x 29.30 inches or smaller, https://doi.org/10.3133/ofr87674.","productDescription":"21 Plates: 41.56 x 29.30 inches or smaller","costCenters":[],"links":[{"id":171185,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":411035,"rank":23,"type":{"id":36,"text":"NGMDB Index 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States","state":"Montana","otherGeospatial":"Fort Peck Indian Reservation","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -105.583,\n              48.0833\n            ],\n            [\n              -105.583,\n              47.667\n            ],\n            [\n              -104.333,\n              47.667\n            ],\n            [\n              -104.333,\n              48.0833\n            ],\n            [\n              -105.583,\n              48.0833\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6be4b07f02db63d93a","contributors":{"authors":[{"text":"Hardie, John K.","contributorId":80281,"corporation":false,"usgs":true,"family":"Hardie","given":"John","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":234086,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Arndt, Harold H.","contributorId":14412,"corporation":false,"usgs":true,"family":"Arndt","given":"Harold","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":234085,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3025,"text":"wsp2272 - 1987 - Quality of ground water in Idaho","interactions":[{"subject":{"id":11777,"text":"ofr8350 - 1984 - Quality of ground water in Idaho","indexId":"ofr8350","publicationYear":"1984","noYear":false,"title":"Quality of ground water in Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":3025,"text":"wsp2272 - 1987 - Quality of ground water in Idaho","indexId":"wsp2272","publicationYear":"1987","noYear":false,"title":"Quality of ground water in Idaho"},"id":1},{"subject":{"id":15414,"text":"ofr8550 - 1985 - Nearshore marine geologic investigations, Point Barrow to Skull Cliff, Northeast Chukchi Sea","indexId":"ofr8550","publicationYear":"1985","noYear":false,"title":"Nearshore marine geologic investigations, Point Barrow to Skull Cliff, Northeast Chukchi Sea"},"predicate":"SUPERSEDED_BY","object":{"id":3025,"text":"wsp2272 - 1987 - Quality of ground water in Idaho","indexId":"wsp2272","publicationYear":"1987","noYear":false,"title":"Quality of ground water in Idaho"},"id":2}],"lastModifiedDate":"2012-02-02T00:05:45","indexId":"wsp2272","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":"2272","title":"Quality of ground water in Idaho","docAbstract":"The major aquifers in Idaho are categorized under two rock types, sedimentary and volcanic, and are grouped into six hydrologic basins. Areas with adequate, minimally adequate, or deficient data available for groundwater-quality evaluations are described. \r\n\r\nWide variations in chemical concentrations in the water occur within individual aquifers, as well as among the aquifers. The existing data base is not sufficient to describe fully the ground-water quality throughout the State; however, it does indicate that the water is generally suitable for most uses. In some aquifers, concentrations of fluoride, cadmium, and iron in the water exceed the U.S. Environmental Protection Agency's drinking-water standards. Dissolved solids, chloride, and sulfate may cause problems in some local areas. Water-quality data are sparse in many areas, and only general statements can be made regarding the areal distribution of chemical constituents. Few data are available to describe temporal variations of water quality in the aquifers. \r\n\r\nPrimary concerns related to special problem areas in Idaho include (1) protection of water quality in the Rathdrum Prairie aquifer, (2) potential degradation of water quality in the Boise-Nampa area, (3) effects of widespread use of drain wells overlying the eastern Snake River Plain basalt aquifer, and (4) disposal of low-level radioactive wastes at the Idaho National Engineering Laboratory. \r\n\r\nShortcomings in the ground-water-quality data base are categorized as (1) multiaquifer sample inadequacy, (2) constituent coverage limitations, (3) baseline-data deficiencies, and (4) data-base nonuniformity.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2272","usgsCitation":"Yee, J., and Souza, W.R., 1987, Quality of ground water in Idaho: U.S. Geological Survey Water Supply Paper 2272, iv, 53 p. :ill., maps ;28 cm., https://doi.org/10.3133/wsp2272.","productDescription":"iv, 53 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":139471,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2272/report-thumb.jpg"},{"id":29856,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2272/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a73e4b07f02db643973","contributors":{"authors":[{"text":"Yee, Johnson J.","contributorId":13612,"corporation":false,"usgs":true,"family":"Yee","given":"Johnson J.","affiliations":[],"preferred":false,"id":146165,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Souza, William R.","contributorId":90295,"corporation":false,"usgs":true,"family":"Souza","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":146166,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26688,"text":"wri864208 - 1987 - Streamflow and water quality of the Grand Calumet River, Lake County, Indiana, and Cook County, Illinois, October 1984","interactions":[],"lastModifiedDate":"2016-06-01T16:20:46","indexId":"wri864208","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":"86-4208","title":"Streamflow and water quality of the Grand Calumet River, Lake County, Indiana, and Cook County, Illinois, October 1984","docAbstract":"<p>A diel (24-hour) water-quality survey was done to investigate the sources of dry-weather waste inputs attributable to other than permitted point-source effluent and to evaluate the waste-load assimilative capacity of the Grand Calumet River, Lake County, Indiana, and Cook County, Illinois, in October 1984. Flow in the Grand Calumet River consists almost entirely of municipal and industrial effluents which comprised more than 90% of the 500 cu ft/sec flow observed at the confluence of the East Branch Grand Calumet River and the Indiana Harbor Ship Canal during the study. At the time of the study, virtually all of the flow in the West Branch Grand Calumet River was municipal effluent. Diel variations in streamflow of as much as 300 cu ft/sec were observed in the East Branch near the ship canal. The diel variation diminished at the upstream sampling sites in the East Branch. In the West Branch, the diel variation in flow was quite drastic; complete reversals of flow were observed at sampling stations near the ship canal. Average dissolved-oxygen concentrations at stations in the East Branch ranged from 5.7 to 8.2 mg/L and at stations in the West Branch from 0.8 to 6.6 mg/L. Concentrations of dissolved solids, suspended solids, biochemical-oxygen demand, ammonia, nitrite, nitrate, and phosphorus were substantially higher in the West Branch than in the East Branch. In the East Branch, only the Indiana Stream Pollution Control Board water-quality standards for total phosphorus and phenol were exceeded. In the West Branch, water-quality standards for total ammonia, chloride, cyanide, dissolved solids, fluoride, total phosphorus, mercury, and phenol were exceeded and dissolved oxygen was less than the minimum allowable. Three areas of significant differences between cumulative effluent and instream chemical-mass discharges were identified in the East Branch and one in the West Branch. The presence of unidentified waste inputs in the East Branch were indicated by differences in the chemical-mass discharges at three sites. Elevated suspended solids, biochemical-oxygen demand, and ammonia chemical-mass discharges at Columbia Avenue indicated the presence of a source of what may have been untreated sewage to the West Branch during the survey. (Author 's abstract)</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/wri864208","collaboration":"Prepared in cooperation with the Indiana State Board of Health","usgsCitation":"Crawford, C.G., and Wangsness, D.J., 1987, Streamflow and water quality of the Grand Calumet River, Lake County, Indiana, and Cook County, Illinois, October 1984: U.S. Geological Survey Water-Resources Investigations Report 86-4208, xi, 137 p., https://doi.org/10.3133/wri864208.","productDescription":"xi, 137 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":158852,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4208/report-thumb.jpg"},{"id":55551,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4208/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":61563,"text":"mf1648B - 1987 - Geochemical map of the Pond Mountain and Pond Mountain Addition Roadless Areas, Carter County, Tennessee","interactions":[],"lastModifiedDate":"2016-08-23T10:38:17","indexId":"mf1648B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"1648","chapter":"B","title":"Geochemical map of the Pond Mountain and Pond Mountain Addition Roadless Areas, Carter County, Tennessee","docAbstract":"<p>In the spring of 1980, K. A. Duttweiler, J. W. Whitlow, and W. R. Griffitts of the U.S. Geological Survey conducted a reconnaissance geochemical survey of the Pond Mountain and Pond Mountain Addition Roadless Areas. The purpose of the study was to determine the geochemical nature of the study area as part of the mineral resource assessment. This report presents a brief summary of the geochemistry of the study area. The evaluation of the mineral resource potential is covered in a separate report (Griffitts, Bitar, and Chatman, in press).</p>\n<p>The Pond Mountain and Pond Mountain Addition Road less Areas encompass 6,668 acres in the Cherokee National Forest in northeastern Tennessee. They are approximately 7 mi southeast of Elizabethton, and 1 mi east of Hampton, Tenn. (fig. 1).</p>\n<p>The study area is fairly accessible by U.S Highway 321 north of the area and Forest Service Route 50 along the southern boundary. Relief is moderate, but the vegetation is very thick in most places.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1648B","usgsCitation":"Duttweiler, K., Griffitts, W.R., Cooley, E., and Whitlow, J.W., 1987, Geochemical map of the Pond Mountain and Pond Mountain Addition Roadless Areas, Carter County, Tennessee: U.S. Geological Survey Miscellaneous Field Studies Map 1648, 57.34 x 38.04 inches, https://doi.org/10.3133/mf1648B.","productDescription":"57.34 x 38.04 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":179980,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1648B.JPG"},{"id":327602,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1648-B/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"Tennessee","county":"Carter County","otherGeospatial":"Pond Mountain and Pond Mountain Addition Roadless Areas","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.2,36.25 ], [ -82.2,36.3675 ], [ -82,36.3675 ], [ -82,36.25 ], [ -82.2,36.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae1c8","contributors":{"authors":[{"text":"Duttweiler, K.A.","contributorId":68310,"corporation":false,"usgs":true,"family":"Duttweiler","given":"K.A.","affiliations":[],"preferred":false,"id":266057,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Griffitts, W. R.","contributorId":10428,"corporation":false,"usgs":true,"family":"Griffitts","given":"W.","middleInitial":"R.","affiliations":[],"preferred":false,"id":266055,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cooley, E.F.","contributorId":83072,"corporation":false,"usgs":true,"family":"Cooley","given":"E.F.","email":"","affiliations":[],"preferred":false,"id":266058,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Whitlow, J. W.","contributorId":63810,"corporation":false,"usgs":true,"family":"Whitlow","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":266056,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":40066,"text":"ofr85648L - 1987 - Data on ground-water quality for the Caliente 1° x 2° quadrangle, eastern Nevada","interactions":[],"lastModifiedDate":"2022-10-17T15:26:04.864311","indexId":"ofr85648L","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":"85-648","chapter":"L","title":"Data on ground-water quality for the Caliente 1° x 2° quadrangle, eastern Nevada","docAbstract":"<p>Water quality data for groundwater has been compiled for the Caliente 1° x 2° quadrangle which covers a portion of eastern Nevada. Chemical characteristics of the water are shown on a map (at a scale of 1:250,000) and on trilinear diagrams for the major ions. The data for the area are also presented in a table.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr85648L","usgsCitation":"Welch, A., and Williams, R.P., 1987, Data on ground-water quality for the Caliente 1° x 2° quadrangle, eastern Nevada: U.S. Geological Survey Open-File Report 85-648, 2 Plates: 39.28 × 25.56 inches and 34.61 × 17.97 inches, https://doi.org/10.3133/ofr85648L.","productDescription":"2 Plates: 39.28 × 25.56 inches and 34.61 × 17.97 inches","costCenters":[],"links":[{"id":165700,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":68477,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1985/0648l/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":392475,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_16882.htm"},{"id":68478,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1985/0648l/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nevada","otherGeospatial":"Caliente 1° x 2° quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116,\n              37\n            ],\n            [\n              -114,\n              37\n            ],\n            [\n              -114,\n              38\n            ],\n            [\n              -116,\n              38\n            ],\n            [\n              -116,\n              37\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db673fdf","contributors":{"authors":[{"text":"Welch, Alan H.","contributorId":45286,"corporation":false,"usgs":true,"family":"Welch","given":"Alan H.","affiliations":[],"preferred":false,"id":222933,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, Rhea P.","contributorId":87114,"corporation":false,"usgs":true,"family":"Williams","given":"Rhea","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":222934,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":59452,"text":"mf2008A - 1987 - Cross sections showing stratigraphic framework of upper Cretaceous Dakota Sandstone, Mancos Shale, Mesaverde Group, and Mesaverde Formation, and lower Tertiary Wasatch Formation, west-central Piceance Basin, Garfield County, Colorado","interactions":[],"lastModifiedDate":"2025-05-28T16:45:03.483961","indexId":"mf2008A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"2008","chapter":"A","title":"Cross sections showing stratigraphic framework of upper Cretaceous Dakota Sandstone, Mancos Shale, Mesaverde Group, and Mesaverde Formation, and lower Tertiary Wasatch Formation, west-central Piceance Basin, Garfield County, Colorado","docAbstract":"<p>Cross sections A-A' and B-B' show the stratigraphic framework of Upper Cretaceous rocks in part of the Piceance basin, northwestern Colorado.&nbsp; This Laramide basin is asymmetric in shape and has a gently dipping western flank and a steeply dipping eastern flank.&nbsp; The basin is bounded by the Uinta uplift to the northwest, the Douglas Creek arch to the west, the Axial Basin uplift to the north, the White River uplift to the east, the Gunnison uplift and the Sawatch-Elk range to the southeast, and the Uncompahgre uplift to the southwest.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf2008A","usgsCitation":"Ellis, M.S., and Kelso, B., 1987, Cross sections showing stratigraphic framework of upper Cretaceous Dakota Sandstone, Mancos Shale, Mesaverde Group, and Mesaverde Formation, and lower Tertiary Wasatch Formation, west-central Piceance Basin, Garfield County, Colorado: U.S. Geological Survey Miscellaneous Field Studies Map 2008, 2 Plates: 48.38 x 41.93 inches and 54.47 x 36.51 inches, https://doi.org/10.3133/mf2008A.","productDescription":"2 Plates: 48.38 x 41.93 inches and 54.47 x 36.51 inches","costCenters":[],"links":[{"id":486651,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5598.htm","linkFileType":{"id":5,"text":"html"}},{"id":358740,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/2008-A/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358739,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/2008-A/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":180426,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/2008-A/report-thumb.jpg"}],"country":"United States","state":"Colorado","county":"Garfield County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109,39.25 ], [ -109,39.5 ], [ -108,39.5 ], [ -108,39.25 ], [ -109,39.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad0e4b07f02db680a95","contributors":{"authors":[{"text":"Ellis, Margaret S. mellis@usgs.gov","contributorId":198,"corporation":false,"usgs":true,"family":"Ellis","given":"Margaret","email":"mellis@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":262035,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kelso, B.S.","contributorId":56715,"corporation":false,"usgs":true,"family":"Kelso","given":"B.S.","email":"","affiliations":[],"preferred":false,"id":262034,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3497,"text":"cir981 - 1987 - Statistics of petroleum exploration in the non-Communist world outside the United States and Canada","interactions":[],"lastModifiedDate":"2018-10-19T10:45:02","indexId":"cir981","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"981","title":"Statistics of petroleum exploration in the non-Communist world outside the United States and Canada","docAbstract":"<p>The search for petroleum has expanded to include most countries in the world. From January 1, 1950, through 1980, about 160,000 crew months were spent in geologic and geophysical exploration in a study area that includes all nonCommunist countries outside the United States and Canada. By the end of 1982, almost 27,000 wildcat wells had been drilled in this study area; these and other pre-1983 wells delineated a prospective area of 1.56 million square miles in which about 836 billion barrels of ultimately recoverable crude oil has been found, 62 percent of it since 1950. The delineated prospective area is still expanding at a rate of 56,000 square miles per year (60 square miles per wildcat well) for the study area, and it is increasing in nearly every country in the study area. Maps of the delineated prospective area in each country show that in most countries, only a small part of the national territory has been explored. In spite of the expansion of the searched area, however, the rate of discovery has declined significantly from 22 million barrels per exploratory well in the 1950's to 8 million barrels per exploratory well in the 1970's. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir981","usgsCitation":"Root, D.H., Attanasi, E., and Turner, R.M., 1987, Statistics of petroleum exploration in the non-Communist world outside the United States and Canada: U.S. Geological Survey Circular 981, iv, 133 p., https://doi.org/10.3133/cir981.","productDescription":"iv, 133 p.","costCenters":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":30507,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1987/0981/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118212,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1987/0981/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e1171","contributors":{"authors":[{"text":"Root, David H.","contributorId":92232,"corporation":false,"usgs":true,"family":"Root","given":"David","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":147037,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Attanasi, Emil D. 0000-0001-6845-7160 attanasi@usgs.gov","orcid":"https://orcid.org/0000-0001-6845-7160","contributorId":198728,"corporation":false,"usgs":true,"family":"Attanasi","given":"Emil D.","email":"attanasi@usgs.gov","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":749031,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Turner, Robert M.","contributorId":96670,"corporation":false,"usgs":true,"family":"Turner","given":"Robert","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":147038,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":3956,"text":"cir994 - 1987 - Uranium resource assessment by the Geological Survey; methodology and plan to update the national resource base","interactions":[],"lastModifiedDate":"2012-02-02T00:05:29","indexId":"cir994","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"994","title":"Uranium resource assessment by the Geological Survey; methodology and plan to update the national resource base","docAbstract":"Based on the Memorandum of Understanding {MOU) of September 20, 1984, between the U.S. Geological Survey of the U.S. Department of Interior and the Energy Information Administration {EIA) of the U.S. Department of Energy {DOE), the U.S. Geological Survey began to make estimates of the undiscovered uranium endowment of selected areas of the United States in 1985. A modified NURE {National Uranium Resource Evaluation) method will be used in place of the standard NURE method of the DOE that was used for the national assessment reported in October 1980. The modified method, here named the 'deposit-size-frequency' {DSF) method, is presented for the first time, and calculations by the two methods are compared using an illustrative example based on preliminary estimates for the first area to be evaluated under the MOU. The results demonstrate that the estimate of the endowment using the DSF method is significantly larger and more uncertain than the estimate obtained by the NURE method. We believe that the DSF method produces a more realistic estimate because the principal factor estimated in the endowment equation is disaggregated into more parts and is more closely tied to specific geologic knowledge than by the NURE method. \r\n\r\nThe DSF method consists of modifying the standard NURE estimation equation, U=AxFxTxG, by replacing the factors FxT by a single factor that represents the tonnage for the total number of deposits in all size classes. Use of the DSF method requires that the size frequency of deposits in a known or control area has been established and that the relation of the size-frequency distribution of deposits to probable controlling geologic factors has been determined. Using these relations, the principal scientist {PS) first estimates the number and range of size classes and then, for each size class, estimates the lower limit, most likely value, and upper limit of the numbers of deposits in the favorable area. Once these probable estimates have been refined by elicitation of the PS, they are entered into the DSF equation, and the probability distribution of estimates of undiscovered uranium endowment is calculated using a slight modification of the program by Ford and McLaren (1980). \r\n\r\nThe EIA study of the viability of the domestic uranium industry requires an annual appraisal of the U.S. uranium resource situation. During DOE's NURE Program, which was terminated in 1983, a thorough assessment of the Nation's resources was completed. A comprehensive reevaluation of uranium resource base for the entire United States is not possible for each annual appraisal. A few areas are in need of future study, however, because of new developments in either scientific knowledge, industry exploration, or both. Four geologic environments have been selected for study by the U.S. Geological Survey in the next several years: (1) surficial uranium deposits throughout the conterminous United States, (2) uranium in collapse-breccia pipes in the Grand Canyon region of Arizona, (3) uranium in Tertiary sedimentary rocks of the Northern Great Plains, and (4) uranium in metamorphic rocks of the Piedmont province in the eastern States. \r\n\r\nIn addition to participation in the National uranium resource assessment, the U.S. Geological Survey will take part in activities of the Nuclear Energy Agency of the Organization for Economic Cooperation and Development and those of the International Atomic Energy Agency.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir994","usgsCitation":"Finch, W.I., and McCammon, R.B., 1987, Uranium resource assessment by the Geological Survey; methodology and plan to update the national resource base: U.S. Geological Survey Circular 994, iii, 31 p. :ill., maps ;26 cm., https://doi.org/10.3133/cir994.","productDescription":"iii, 31 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":124738,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1987/0994/report-thumb.jpg"},{"id":31043,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1987/0994/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db6053d3","contributors":{"authors":[{"text":"Finch, Warren Irvin","contributorId":55794,"corporation":false,"usgs":true,"family":"Finch","given":"Warren","email":"","middleInitial":"Irvin","affiliations":[],"preferred":false,"id":147891,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCammon, Richard B.","contributorId":107674,"corporation":false,"usgs":true,"family":"McCammon","given":"Richard","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":147892,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29058,"text":"wri864026 - 1987 - Relation of sediment and nutrient loads to watershed characteristics and land use in the Otisco Lake basin, Onondaga County, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:08:52","indexId":"wri864026","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":"86-4026","title":"Relation of sediment and nutrient loads to watershed characteristics and land use in the Otisco Lake basin, Onondaga County, New York","docAbstract":"Otisco Lake, the smallest and easternmost of New York State 's Finger Lakes, is the source of water supply for several villages in Onondaga County. In recent years, turbidity and algal blooms have periodically impaired the lake 's use for both water supply and recreation. Principal land uses within the Otisco Lake basin are woodland (39%) and cropland (49%). Conservation practices such as contour farming, strip cropping, and diversion ditches are applied to about 47% of the cropland in the basin. Runoff and concentrations of sediment and nutrients in the five major tributaries, which together drain about 70% of the lake 's watershed, were monitored from November 1981 through September 1983, and sediment and nutrient loads from the ungaged areas of the watershed were estimated. Otisco Lake received 10,600 tons of sediment, 20,600 lbs of phosphorus asp, 199,000 lbs of total kjeldahl nitrogen as N, and 236,000 lbs of nitrite plus nitrate as N from the five tributaries and the ungaged area during the 23-month study. Spafford Creek basin (12.0 sq mi) contributed about 72% of the annual sediment load and 46% of the annual nutrient load; the other four subbasins, which range from 2.6 to 3.7 sq mi in area, each contributed 3 to 5% of the annual sediment load and 6 to 16% of the annual nutrient load. The ungaged part of the watershed contributed 12% of the annual sediment load and 28% of the annual nutrient load. Concentrations of ammonia as N were relatively uniform through the year, although some extremely high concentrations occurred during the summer. Total Kjeldahl nitrogen concentrations were highest in the summer and lowest in the fall. Concentrations of nitrite plus nitrate were significantly lower in winter than in the rest of the year. Total phosphorus concentrations were slightly higher in the spring than at other times, and concentrations of dissolved phosphorus were slightly higher in the summer. Storms and snowmelt accounted for 70 to 90% of the runoff, 90 to 99% of the sediment load, and 70 to 98% of the nutrient loads from the tributaries. The largest nutrient loads occurred during the spring of each year, when runoff was highest. About 70% of the sediment, 60% of total Kjeldahl nitrogen, 58% of total phosphorus, and 53% of nitrite plus nitrate were transported during spring high flows. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri864026","usgsCitation":"Paschal, J., and Sherwood, D.A., 1987, Relation of sediment and nutrient loads to watershed characteristics and land use in the Otisco Lake basin, Onondaga County, New York: U.S. Geological Survey Water-Resources Investigations Report 86-4026, vi, 62 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri864026.","productDescription":"vi, 62 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159600,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4026/report-thumb.jpg"},{"id":57920,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4026/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c268","contributors":{"authors":[{"text":"Paschal, J.E.","contributorId":86816,"corporation":false,"usgs":true,"family":"Paschal","given":"J.E.","affiliations":[],"preferred":false,"id":200877,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sherwood, D. A.","contributorId":65824,"corporation":false,"usgs":true,"family":"Sherwood","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":200876,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":39649,"text":"pp1433AB - 1987 - Oligocene and Miocene volcanic rocks in the central Pioche-Marysvale igneous belt, western Utah and eastern Nevada","interactions":[],"lastModifiedDate":"2022-06-16T20:10:08.939051","indexId":"pp1433AB","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"1433","chapter":"A-B","title":"Oligocene and Miocene volcanic rocks in the central Pioche-Marysvale igneous belt, western Utah and eastern Nevada","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1433AB","usgsCitation":"Best, M., Grant, S.K., Mehnert, H.H., Keith, J.D., and Naeser, C.W., 1987, Oligocene and Miocene volcanic rocks in the central Pioche-Marysvale igneous belt, western Utah and eastern Nevada: U.S. Geological Survey Professional Paper 1433, 47 p., https://doi.org/10.3133/pp1433AB.","productDescription":"47 p.","costCenters":[],"links":[{"id":67335,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1433a-b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":164615,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1433a-b/report-thumb.jpg"},{"id":402302,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_76353.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Nevada, Utah","otherGeospatial":"central Pioche-Marysvale igneous belt","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -115.806884765625,\n              37.09900294387622\n            ],\n            [\n              -112.467041015625,\n              37.09900294387622\n            ],\n            [\n              -112.467041015625,\n              39.33429742980725\n            ],\n            [\n              -115.806884765625,\n              39.33429742980725\n            ],\n            [\n              -115.806884765625,\n              37.09900294387622\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691cb8","contributors":{"authors":[{"text":"Best, Myron G.","contributorId":50124,"corporation":false,"usgs":true,"family":"Best","given":"Myron G.","affiliations":[],"preferred":false,"id":221903,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grant, S. Kerry","contributorId":88412,"corporation":false,"usgs":true,"family":"Grant","given":"S.","email":"","middleInitial":"Kerry","affiliations":[],"preferred":false,"id":221904,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mehnert, H. H.","contributorId":16382,"corporation":false,"usgs":true,"family":"Mehnert","given":"H.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":221900,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Keith, J. D.","contributorId":32525,"corporation":false,"usgs":true,"family":"Keith","given":"J.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":221902,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Naeser, C. W.","contributorId":17582,"corporation":false,"usgs":true,"family":"Naeser","given":"C.","middleInitial":"W.","affiliations":[],"preferred":false,"id":221901,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":68212,"text":"ha696 - 1987 - Solute distribution in ground and surface water in the Snake River Basin, Idaho and eastern Oregon","interactions":[{"subject":{"id":43032,"text":"ofr85167 - 1985 - Solute distribution in waters in the Snake River basin, Idaho and eastern Oregon","indexId":"ofr85167","publicationYear":"1985","noYear":false,"title":"Solute distribution in waters in the Snake River basin, Idaho and eastern Oregon"},"predicate":"SUPERSEDED_BY","object":{"id":68212,"text":"ha696 - 1987 - Solute distribution in ground and surface water in the Snake River Basin, Idaho and eastern Oregon","indexId":"ha696","publicationYear":"1987","noYear":false,"title":"Solute distribution in ground and surface water in the Snake River Basin, Idaho and eastern Oregon"},"id":1}],"lastModifiedDate":"2020-10-05T12:54:44.455258","indexId":"ha696","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"696","title":"Solute distribution in ground and surface water in the Snake River Basin, Idaho and eastern Oregon","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha696","usgsCitation":"Low, W.H., 1987, Solute distribution in ground and surface water in the Snake River Basin, Idaho and eastern Oregon: U.S. Geological Survey Hydrologic Atlas 696, 2 Plates: 41.96 x 29.72 inches and 40.00 x 27.72 inches, https://doi.org/10.3133/ha696.","productDescription":"2 Plates: 41.96 x 29.72 inches and 40.00 x 27.72 inches","costCenters":[],"links":[{"id":185626,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89562,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/696/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89561,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/696/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","country":"United States","state":"Idaho, Oregon","otherGeospatial":"Snake River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.5,\n              42\n            ],\n            [\n              -111.5,\n              42\n            ],\n            [\n              -111.5,\n              45.1\n            ],\n            [\n              -117.5,\n              45.1\n            ],\n            [\n              -117.5,\n              42\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ece4b07f02db5eb4d0","contributors":{"authors":[{"text":"Low, Walton H.","contributorId":92672,"corporation":false,"usgs":true,"family":"Low","given":"Walton","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":277850,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":47444,"text":"b1728C - 1987 - Mineral resources of the Far South Egans Wilderness Study Area, Lincoln and Nye Counties, Nevada","interactions":[{"subject":{"id":47444,"text":"b1728C - 1987 - Mineral resources of the Far South Egans Wilderness Study Area, Lincoln and Nye Counties, Nevada","indexId":"b1728C","publicationYear":"1987","noYear":false,"chapter":"C","title":"Mineral resources of the Far South Egans Wilderness Study Area, Lincoln and Nye Counties, Nevada"},"predicate":"IS_PART_OF","object":{"id":33491,"text":"b1728 - 1986 - Mineral resources of wilderness study areas: east-central Nevada and part of adjacent Beaver County, Utah","indexId":"b1728","publicationYear":"1986","noYear":false,"title":"Mineral resources of wilderness study areas: east-central Nevada and part of adjacent Beaver County, Utah"},"id":1}],"isPartOf":{"id":33491,"text":"b1728 - 1986 - Mineral resources of wilderness study areas: east-central Nevada and part of adjacent Beaver County, Utah","indexId":"b1728","publicationYear":"1986","noYear":false,"title":"Mineral resources of wilderness study areas: east-central Nevada and part of adjacent Beaver County, Utah"},"lastModifiedDate":"2022-08-31T20:32:16.156587","indexId":"b1728C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"1728","chapter":"C","title":"Mineral resources of the Far South Egans Wilderness Study Area, Lincoln and Nye Counties, Nevada","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Mineral resources of wilderness study areas: East-central Nevada and part of adjacent Beaver County, Utah (Bulletin 1728)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1728C","usgsCitation":"Hedlund, D.C., Davies, R.C., Hovorka, D.S., Blank, H.R., and Tuftin, S., 1987, Mineral resources of the Far South Egans Wilderness Study Area, Lincoln and Nye Counties, Nevada: U.S. Geological Survey Bulletin 1728, Report: 11 p.; 1 Plate: 26.50 × 25.00 inches, https://doi.org/10.3133/b1728C.","productDescription":"Report: 11 p.; 1 Plate: 26.50 × 25.00 inches","costCenters":[],"links":[{"id":406037,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21651.htm","linkFileType":{"id":5,"text":"html"}},{"id":171470,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1728c/report-thumb.jpg"},{"id":84375,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1728c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84374,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1728c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nevada","county":"Lincoln County, Nye County","otherGeospatial":"Far South Egans Wilderness Study Area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -115.017,\n              38.375\n            ],\n            [\n              -114.792,\n              38.375\n            ],\n            [\n              -114.792,\n              38.614\n            ],\n            [\n              -115.017,\n              38.614\n            ],\n            [\n              -115.017,\n              38.375\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a3ac","contributors":{"authors":[{"text":"Hedlund, D. C.","contributorId":101624,"corporation":false,"usgs":true,"family":"Hedlund","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":235368,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davies, R. C.","contributorId":11683,"corporation":false,"usgs":true,"family":"Davies","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":235364,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hovorka, D. S.","contributorId":60210,"corporation":false,"usgs":true,"family":"Hovorka","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":235365,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Blank, H. R. Jr.","contributorId":94674,"corporation":false,"usgs":true,"family":"Blank","given":"H.","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":235367,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Tuftin, S. E.","contributorId":67561,"corporation":false,"usgs":true,"family":"Tuftin","given":"S. E.","affiliations":[],"preferred":false,"id":235366,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":68575,"text":"ha690 - 1987 - Water withdrawn for irrigation in 1980 on the Snake River Plain, Idaho and eastern Oregon","interactions":[{"subject":{"id":44010,"text":"ofr84434 - 1984 - Water withdrawn for irrigation in 1980 on the Snake River plain, Idaho and eastern Oregon","indexId":"ofr84434","publicationYear":"1984","noYear":false,"title":"Water withdrawn for irrigation in 1980 on the Snake River plain, Idaho and eastern Oregon"},"predicate":"SUPERSEDED_BY","object":{"id":68575,"text":"ha690 - 1987 - Water withdrawn for irrigation in 1980 on the Snake River Plain, Idaho and eastern Oregon","indexId":"ha690","publicationYear":"1987","noYear":false,"title":"Water withdrawn for irrigation in 1980 on the Snake River Plain, Idaho and eastern Oregon"},"id":1}],"lastModifiedDate":"2013-11-12T14:52:30","indexId":"ha690","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"690","title":"Water withdrawn for irrigation in 1980 on the Snake River Plain, Idaho and eastern Oregon","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha690","usgsCitation":"Bigelow, B.B., Goodell, S.A., and Newton, G.D., 1987, Water withdrawn for irrigation in 1980 on the Snake River Plain, Idaho and eastern Oregon: U.S. Geological Survey Hydrologic Atlas 690, 2 Plates: 49.00 x 38.00 inches, https://doi.org/10.3133/ha690.","productDescription":"2 Plates: 49.00 x 38.00 inches","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":189993,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90210,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/690/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90211,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/690/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","country":"United States","state":"Idaho;Oregon","otherGeospatial":"Snake River Plain","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.25,42.25 ], [ -117.25,44.5 ], [ -111.5,44.5 ], [ -111.5,42.25 ], [ -117.25,42.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eef61","contributors":{"authors":[{"text":"Bigelow, B. B.","contributorId":76317,"corporation":false,"usgs":true,"family":"Bigelow","given":"B.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":278500,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goodell, S. A.","contributorId":38168,"corporation":false,"usgs":true,"family":"Goodell","given":"S.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":278498,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Newton, G. D.","contributorId":43374,"corporation":false,"usgs":true,"family":"Newton","given":"G.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":278499,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":14698,"text":"ofr87454 - 1987 - Patterns of acid deposition variability in the Eastern United States, 1981-84","interactions":[],"lastModifiedDate":"2012-02-02T00:07:03","indexId":"ofr87454","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":"87-454","title":"Patterns of acid deposition variability in the Eastern United States, 1981-84","docAbstract":"An increase in pH and a decrease in sulfate concentration of precipitation were recorded at National Atmospheric Deposition Program and National Trends Network (NADP/NTN) monitoring sites in the Eastern United States between 1981 and 1984. The decline in acidity, however, was not spatially or temporally uniform. The range in acidity and sulfate concentrations decreased during the four-yr period. Variations in the area of constant pH surfaces take the general form of area reductions in both the lower (pH 4.01-4.40) and upper (pH 4.91-5.40) range of values with concomitant area increases in the middle (pH 4.41-4.90) range. The pattern for sulfate is simpler, with area increases occurring in the lower (1.0-1.9 mg/L) range, decreases in the upper (2.5-4.4 mg/L) range, with approximate stability in the middle (2.0-2.4 mg/L) range of values. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87454","usgsCitation":"Lins, H., Lanfear, K., and Schertz, T., 1987, Patterns of acid deposition variability in the Eastern United States, 1981-84: U.S. Geological Survey Open-File Report 87-454, i, 13 p. :ill. ;28 cm., https://doi.org/10.3133/ofr87454.","productDescription":"i, 13 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":147577,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0454/report-thumb.jpg"},{"id":43464,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0454/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688ad7","contributors":{"authors":[{"text":"Lins, H.F.","contributorId":81508,"corporation":false,"usgs":true,"family":"Lins","given":"H.F.","affiliations":[],"preferred":false,"id":169869,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lanfear, K.J.","contributorId":14392,"corporation":false,"usgs":true,"family":"Lanfear","given":"K.J.","affiliations":[],"preferred":false,"id":169867,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schertz, T. L.","contributorId":65841,"corporation":false,"usgs":true,"family":"Schertz","given":"T. L.","affiliations":[],"preferred":false,"id":169868,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":26176,"text":"wri854145 - 1987 - Geohydrologic conditions at the nuclear-fuels reprocessing plant and waste-management facilities at the Western New York Nuclear Service Center, Cattaraugus County, New York","interactions":[],"lastModifiedDate":"2023-04-10T20:33:26.964189","indexId":"wri854145","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":"85-4145","title":"Geohydrologic conditions at the nuclear-fuels reprocessing plant and waste-management facilities at the Western New York Nuclear Service Center, Cattaraugus County, New York","docAbstract":"<p>A nuclear-fuel reprocessing plant, a high-level radioactive liquid-waste tank complex, and related waste facilities occupy 100 hectares (ha) within the Western New York Nuclear Service Center near West Valley, N.Y. The facilities are underlain by glacial and postglacial deposits that fill an ancestrial bedrock valley. The main plant facilities are on an elevated plateau referred to as the north plateau. Groundwater on the north plateau moves laterally within a surficial sand and gravel from the main plant building to areas northeast, east, and southeast of the facilities. The sand and gravel ranges from 1 to 10 m thick and has a hydraulic conductivity ranging from 0.1 to 7.9 m/day. Two separate burial grounds, a 4-ha area for low-level radioactive waste disposal and a 2.9-ha area for disposal of higher-level waste are excavated into a clay-rich till that ranges from 22 to 28 m thick. Migration of an organic solvent from the area of higher level waste at shallow depth in the till suggests that a shallow, fractured, oxidized, and weathered till is a significant pathway for lateral movement of groundwater. Below this zone, groundwater moves vertically downward through the till to recharge a lacustrine silt and fine sand. Within the saturated parts of the lacustrine unit, groundwater moves laterally to the northeast toward Buttermilk Creek. Hydraulic conductivity of the till, based on field and laboratory analyses , ranges from 0.000018 to 0.000086 m/day.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854145","usgsCitation":"Bergeron, M.P., Kappel, W.M., and Yager, R.M., 1987, Geohydrologic conditions at the nuclear-fuels reprocessing plant and waste-management facilities at the Western New York Nuclear Service Center, Cattaraugus County, New York: U.S. Geological Survey Water-Resources Investigations Report 85-4145, Report: vi, 49 p.; 1 Plate: 39.24 x 26.71 inches, https://doi.org/10.3133/wri854145.","productDescription":"Report: vi, 49 p.; 1 Plate: 39.24 x 26.71 inches","costCenters":[],"links":[{"id":415537,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36308.htm","linkFileType":{"id":5,"text":"html"}},{"id":54977,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4145/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54976,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4145/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123559,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4145/report-thumb.jpg"}],"country":"United States","state":"New York","county":"Cattaraugus County","otherGeospatial":"Western New York Nuclear Service Center","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -78.661,\n              42.458\n            ],\n            [\n              -78.661,\n              42.442\n            ],\n            [\n              -78.643,\n              42.442\n            ],\n            [\n              -78.643,\n              42.458\n            ],\n            [\n              -78.661,\n              42.458\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b27e4b07f02db6b0f1c","contributors":{"authors":[{"text":"Bergeron, M. P.","contributorId":42969,"corporation":false,"usgs":true,"family":"Bergeron","given":"M.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":195942,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kappel, W. M.","contributorId":18754,"corporation":false,"usgs":true,"family":"Kappel","given":"W.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":195941,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Yager, R. M.","contributorId":8069,"corporation":false,"usgs":true,"family":"Yager","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":195940,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":27463,"text":"wri854108 - 1987 - Ground-penetrating radar study of the thickness and extent of sediments beneath Silver Lake, Berlin and Meriden, Connecticut","interactions":[],"lastModifiedDate":"2019-10-15T07:51:35","indexId":"wri854108","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":"85-4108","title":"Ground-penetrating radar study of the thickness and extent of sediments beneath Silver Lake, Berlin and Meriden, Connecticut","docAbstract":"A short-pulse ground-penetrating radar system was used to determine the extent and thickness of organic-rich lake-bottom sediments in Silver Lake in south-central Connecticut. Four mi of ground-penetrating radar profiles were obtained along traverses of the frozen lake during March 1984. The radar waves penetrated 6 inches of snow, 1 ft of ice, an average of 4 to 5 ft of water, and 5 ft of soft organic and inorganic deposits. A large area of the lake bottom is underlain by soft sediment exceeding 5 ft in depth. No radar reflections were obtained from the hard subbottom in these areas because the overlying sediment probably contains large proportions of silt and clay that are relatively impervious to radar. Coring along two radar profile lines confirmed the depths of soft sediment calculated from the radar data. Boring logs around the perimeter of the lake indicate that the eastern side may be underlain by till or poorly-sorted sand and gravel, and that the rest of the lake is probably underlain by fine sands and silts with some discontinuous layers of sand and gravel. 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,{"id":33388,"text":"b1707B - 1987 - Mineral resources of the East Fork High Rock Canyon Wilderness Study Area, Washoe and Humboldt counties, Nevada","interactions":[],"lastModifiedDate":"2012-08-15T01:01:59","indexId":"b1707B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"1707","chapter":"B","title":"Mineral resources of the East Fork High Rock Canyon Wilderness Study Area, Washoe and Humboldt counties, Nevada","docAbstract":"The part of the East Fork High Rock Canyon Wilderness Study Area (CA-020-914/NV-020-006A) included in this study encompasses 33,460 acres in the northwestern part of Nevada. Throughout this report, \"wilderness study area\" and \"study area\" refertothe 33,460 acres for which mineral surveys were requested. The U.S. Geological Survey and the U.S. Bureau of Mines conducted geological, geophysical, and geochemical surveys to assess the mineral resources (known) and the mineral resource potential (undiscovered) of the study area. Fieldwork for this report was carried out in 1985 and 1986. No mines, significant prospects, or mining claims are located inside the study area, and no identified resources were found. The wilderness study area has moderate mineral resource potential for gold, silver, and mercury and for zeolite minerals. A low potential also exists for geothermal energy resources, and potential for oil and gas is unknown.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/b1707B","usgsCitation":"Ach, J.A., Plouff, D., Turner, R.L., and Schmauch, S., 1987, Mineral resources of the East Fork High Rock Canyon Wilderness Study Area, Washoe and Humboldt counties, Nevada: U.S. Geological Survey Bulletin 1707, p. B1-B14, ill., map ;28 cm., https://doi.org/10.3133/b1707B.","productDescription":"p. B1-B14, ill., map ;28 cm.","costCenters":[],"links":[{"id":163323,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1707b/report-thumb.jpg"},{"id":61244,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1707b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nevada","county":"Humboldt;Washoe","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120,41 ], [ -120,42 ], [ -119,42 ], [ -119,41 ], [ -120,41 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a3e1","contributors":{"authors":[{"text":"Ach, Jay A.","contributorId":55446,"corporation":false,"usgs":true,"family":"Ach","given":"Jay","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":210808,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Plouff, Donald","contributorId":94657,"corporation":false,"usgs":true,"family":"Plouff","given":"Donald","email":"","affiliations":[],"preferred":false,"id":210810,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Turner, R. L.","contributorId":93903,"corporation":false,"usgs":true,"family":"Turner","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":210809,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Schmauch, S. W.","contributorId":53790,"corporation":false,"usgs":true,"family":"Schmauch","given":"S. W.","affiliations":[],"preferred":false,"id":210807,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":33381,"text":"b1713C - 1987 - Mineral resources of the Fort Piute Wilderness Study Area, San Bernardino County, California","interactions":[],"lastModifiedDate":"2017-07-05T12:58:51","indexId":"b1713C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"C","title":"Mineral resources of the Fort Piute Wilderness Study Area, San Bernardino County, California","docAbstract":"<p>The Fort Piute Wilderness Study Area (CDCA-267) is in northeastern San Bernardino County, California, near the boundary between California and Nevada. Mineral surveys were requested for 31,371 acres of the Fort Piute Wilderness Study Area. In this report the area studied is referred to as \"the study area\". Examination of mines and prospects in the area was accomplished by the U.S. Bureau of Mines in 1981 and 1982. Field investigations of the area were carried out by the U.S. Geological Survey in 1983 and 1985. No mines or prospects, few mining claims, and no identified resources are located within the wilderness study area. Moderate and low potential for gold resources appears limited to outcrops of gneiss and granite exposed along the eastern side of the Piute Range. Available information indicates that there is no potential for energy resources, including oil and gas, uranium, or geothermal, in the study area.</p>","largerWorkTitle":"Mineral resources of Wilderness Study Areas: Eastern California Desert Conservation Area, California","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/b1713C","usgsCitation":"Nielson, J.E., Frisken, J.G., Jachens, R.C., and McDonnell, J.R., 1987, Mineral resources of the Fort Piute Wilderness Study Area, San Bernardino County, California: U.S. Geological Survey Bulletin 1713, Report: v, 12 p.; Plate: 23.00 x 35.50 inches, https://doi.org/10.3133/b1713C.","productDescription":"Report: v, 12 p.; Plate: 23.00 x 35.50 inches","startPage":"C1","endPage":"C12","costCenters":[],"links":[{"id":61234,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1713c/plate-1.pdf","text":"Plate 1","size":"4.53 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 1"},{"id":61235,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1713c/report.pdf","text":"Report","size":"1.27 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":164232,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1713c/report-thumb.jpg"}],"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              -115.05157470703126,\n              35.337533782800946\n            ],\n            [\n              -115.13946533203124,\n              35.40024478679507\n            ],\n            [\n              -115.18890380859374,\n              35.382332329032984\n            ],\n            [\n              -115.27679443359375,\n              35.27253175660236\n            ],\n            [\n              -115.31524658203124,\n              35.11990857099681\n            ],\n            [\n              -115.3399658203125,\n              34.786739162702524\n            ],\n            [\n              -115.32623291015625,\n              34.69646117272349\n            ],\n            [\n              -115.27130126953125,\n              34.59930237746263\n            ],\n            [\n              -115.15869140624999,\n              34.55407346090554\n            ],\n            [\n              -115.02960205078125,\n              34.5020297944346\n            ],\n            [\n              -114.9169921875,\n              34.58799745550482\n            ],\n            [\n              -114.86480712890626,\n              34.70549341022544\n            ],\n            [\n              -114.84558105468749,\n              34.836349990763864\n            ],\n            [\n              -114.82635498046875,\n              35.02774729487063\n            ],\n            [\n              -114.83184814453124,\n              35.15584570226544\n            ],\n            [\n              -115.05157470703126,\n              35.337533782800946\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a320","contributors":{"authors":[{"text":"Nielson, Jane E.","contributorId":9701,"corporation":false,"usgs":true,"family":"Nielson","given":"Jane","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":210770,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frisken, James G.","contributorId":76740,"corporation":false,"usgs":true,"family":"Frisken","given":"James","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":210772,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jachens, Robert C. jachens@usgs.gov","contributorId":1180,"corporation":false,"usgs":true,"family":"Jachens","given":"Robert","email":"jachens@usgs.gov","middleInitial":"C.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":210771,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McDonnell, John R. Jr.","contributorId":32898,"corporation":false,"usgs":true,"family":"McDonnell","given":"John","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":210773,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":12329,"text":"ofr87234 - 1987 - Surface water-quality assessment of the Kentucky River basin, Kentucky: Project description","interactions":[],"lastModifiedDate":"2021-12-23T21:21:39.035116","indexId":"ofr87234","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":"87-234","title":"Surface water-quality assessment of the Kentucky River basin, Kentucky: Project description","docAbstract":"In April 1986, the U.S. Geological Survey began the National Water Quality Assessment Program, which at present (1987) is in a pilot phase in which assessment concepts and approaches are being tested and modified to prepare for full implementation of the program in the future. Seven pilot projects (four surface water projects and three groundwater projects) have been started. The preliminary plans for the surface water quality assessment of the Kentucky River basin pilot project are described. The Kentucky River basin drains an area of approximately 7,000 sq mi in east central Kentucky and is underlain by rocks that range in composition from limestone to sandstone and shale. Because greater than 95% of the basin population relies on surface water, surface water quality is of great concern. Land use practices that affect the surface water quality in the basin include agriculture, forestry, oil and gas production, coal mining, and urbanization. Water quality concerns resulting from the various land uses include the effects of: oil and gas field brine discharges; agricultural chemicals; sedimentation caused by coal mining; and trace element impacts from industrial and urban environments. Assessment activity is designed to occur over a 9-year period of time. During the first 3-year period of the cycle, concentrated data acquisition and interpretation will occur. For the next 6 years, sample collection will occur at a much lower level of intensity to document the occurrence of any gross changes in water quality. This 9-year cycle will then be repeated. Historical data will be evaluated to provide, to the extent possible, a description of existing and past trends in water quality conditions and to develop conceptual models that relate the observed conditions to the sources and causes, both natural and human-controlled. New data will be collected to verify the water quality conditions documented by historic data, to track long-term trends in water quality, to intensify temporal and spatial sampling densities, and to improve the understanding of the relations between water quality conditions and causative factors. (Lantz-PTT)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr87234","usgsCitation":"White, K.D., Smoot, J.L., Jackson, J.K., and Choquette, A., 1987, Surface water-quality assessment of the Kentucky River basin, Kentucky: Project description: U.S. Geological Survey Open-File Report 87-234, v, 39 p., https://doi.org/10.3133/ofr87234.","productDescription":"v, 39 p.","costCenters":[],"links":[{"id":393385,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17167.htm"},{"id":40559,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0234/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144047,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0234/report-thumb.jpg"}],"country":"United States","state":"Kentucky","otherGeospatial":"Kentucky River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -85.203,\n              36.862\n            ],\n            [\n              -82.638,\n              36.862\n            ],\n            [\n              -82.638,\n              38.764\n            ],\n            [\n              -85.203,\n              38.764\n            ],\n            [\n              -85.203,\n              36.862\n            ]\n          ]\n       ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aefe4b07f02db6913ff","contributors":{"authors":[{"text":"White, K. D.","contributorId":45717,"corporation":false,"usgs":true,"family":"White","given":"K.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":165907,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smoot, J. L.","contributorId":59794,"corporation":false,"usgs":true,"family":"Smoot","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":165908,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jackson, J. K.","contributorId":90312,"corporation":false,"usgs":true,"family":"Jackson","given":"J.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":165909,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Choquette, Anne F.","contributorId":98323,"corporation":false,"usgs":true,"family":"Choquette","given":"Anne F.","affiliations":[],"preferred":false,"id":165910,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":4234,"text":"cir986 - 1987 - The Alaska Mineral Resource Assessment Program: Background information to accompany folio of geologic and mineral resource maps of the Circle quadrangle, Alaska","interactions":[],"lastModifiedDate":"2025-08-22T13:53:20.564963","indexId":"cir986","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"986","title":"The Alaska Mineral Resource Assessment Program: Background information to accompany folio of geologic and mineral resource maps of the Circle quadrangle, Alaska","docAbstract":"<p>The geology, geochemistry, geophysics, and Landsat imagery of the Circle quadrangle were investigated by an interdisciplinary research team for the purpose of assessing the mineral potential of the area. The quadrangle covers approximately 15,765 km<sup>2</sup> in east-central Alaska; most of it is included in the mountainous Yukon-Tanana Upland physiographic division, but the northernmost part is in the low-lying Yukon Flats section. The Circle mining district, in the east-central part of the quadrangle, has been a major producing area of placer gold since its discovery in 1893. </p><p>For descriptive purposes, the Circle quadrangle is divided into three areas: the northwest Circle quadrangle, the area north of the Tintina fault zone, and the area south of the Tintina fault zone. The Tintina fault zone extends northwesterly through the northern part of the quadrangle. The northwest Circle quadrangle contains mostly folded and faulted, slightly metamorphosed sedimentary rocks that are intruded by Tertiary granitic plutons. In the northern part of the area north of the Tintina fault zone (Little Crazy Mountains and northern east Crazy Mountains), the rocks consist primarily of the gabbro and basalt of the Circle Volcanics and minor associated chert, graywacke, and limestone. Elsewhere in this area (south of the Circle Volcanics and in the western Crazy Mountains), the rocks are mostly slightly metamorphosed Paleozoic sedimentary rocks that have been folded and faulted. Rocks in the largest part of the quadrangle, the area south of the Tintina fault zone, consist largely of pelitic rocks that are regionally metamorphosed to greenschist and amphibolite facies. Felsic plutons, mostly Tertiary in age, occur throughout the area. The metamorphic rocks are separated from sedimentary rocks on the northwest by thrust faulting. </p><p>The aeromagnetic and gravity data show clear differences between the areas north and south of the Tintina fault zone. The metamorphic terrane to the south has low overall gravity and local gravity lows over exposed granitic plutons. It is hypothesized that magnetic chlorite schist infolded with nonmagnetic quartzite and schist account for east-northeast-trending magnetic highs that approximately parallel the regional strike of the most prominent foliation in the metamorphic rocks. North of the Tintina fault zone, the Circle Volcanics are characterized by high gravity and east-west-trending magnetic highs. The Tintina fault zone has an intense magnetic high near the western margin of the Circle quadrangle overlying the magnetic granodiorite of the Victoria Mountain pluton. A magnetic high near Circle Hot Springs is less intense, but broader, and could reflect a buried magnetic pluton similar to that of the Victoria Mountain pluton. </p><p>Computer-enhanced Landsat images of the Circle quadrangle show trends and patterns of concentrations of linear features. Features trending northeast-southwest predominate throughout the quadrangle; northwest-southeast-trending linear features are found mostly south of the Tintina fault zone. High concentrations of linear features were not found to correspond to areas of known mineralization in any consistent or significant way that could presently be used in locating areas of mineralization. Geochemical and mineralogical studies of stream sediment and heavy-mineral concentrates from the Circle quadrangle identify areas of anomalous concentrations of metallic elements, including gold, silver, tin, tungsten, lead, antimony, zinc, thorium, uranium, and beryllium. The data delineate areas of known mineral occurrences and areas that may contain undiscovered mineral resources. </p><p>To date, placer gold has been the only significant metallic mineral resource from the Circle quadrangle, but the general geologic setting, especially the presence of post-orogenic plutons, is similar to that of regions that contain tin greisen deposits, tungsten skarn deposits, lode gold deposits in metasedimentary rocks, and uranium vein deposits. Six areas or tracts were identified in which such deposits might occur, and two more tracts were delineated as possible for the occurrence of shale-hosted Lead-zinc deposits. The discovery of two diamonds in the gravels of Cooked Creek point to the slight possibility of finding placer or lode diamond deposits.&nbsp;</p><p>Although most of the past and present gold mining has taken place in four areas in the quadrangle, a sedimentary basin near the town of Central was identified as possibly containing buried placer gold deposits or sedimentary uranium deposits.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir986","usgsCitation":"Foster, H.L., Menzie, W., Cady, J.W., Simpson, S.L., Aleinikoff, J.N., Wilson, F.H., and Tripp, R.B., 1987, The Alaska Mineral Resource Assessment Program: Background information to accompany folio of geologic and mineral resource maps of the Circle quadrangle, Alaska: U.S. Geological Survey Circular 986, iii, 22 p., https://doi.org/10.3133/cir986.","productDescription":"iii, 22 p.","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":31348,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1987/0986/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139315,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1987/0986/report-thumb.jpg"},{"id":391760,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24147.htm"}],"country":"United States","state":"Alaska","otherGeospatial":"Circle quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -147,\n              65\n            ],\n            [\n              -144,\n              65\n            ],\n            [\n              -144,\n              66\n            ],\n            [\n              -147,\n              66\n            ],\n            [\n              -147,\n              65\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6834b2","contributors":{"authors":[{"text":"Foster, Helen Laura","contributorId":21936,"corporation":false,"usgs":true,"family":"Foster","given":"Helen","email":"","middleInitial":"Laura","affiliations":[],"preferred":false,"id":148511,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Menzie, W. D.","contributorId":52916,"corporation":false,"usgs":true,"family":"Menzie","given":"W. D.","affiliations":[],"preferred":false,"id":148513,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cady, J. W.","contributorId":81892,"corporation":false,"usgs":true,"family":"Cady","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":148515,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Simpson, S. L.","contributorId":46508,"corporation":false,"usgs":true,"family":"Simpson","given":"S.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":148512,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Aleinikoff, J. N. 0000-0003-3494-6841","orcid":"https://orcid.org/0000-0003-3494-6841","contributorId":75132,"corporation":false,"usgs":true,"family":"Aleinikoff","given":"J.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":148514,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Wilson, Frederic H. 0000-0003-1761-6437 fwilson@usgs.gov","orcid":"https://orcid.org/0000-0003-1761-6437","contributorId":67174,"corporation":false,"usgs":true,"family":"Wilson","given":"Frederic","email":"fwilson@usgs.gov","middleInitial":"H.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":148510,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Tripp, R. B.","contributorId":88707,"corporation":false,"usgs":true,"family":"Tripp","given":"R.","middleInitial":"B.","affiliations":[],"preferred":false,"id":148516,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":14484,"text":"ofr87140 - 1987 - Magnetotelluric study of the thickness of volcanic and sedimentary rock in the Pullman-Moscow basin of eastern Washington","interactions":[],"lastModifiedDate":"2022-09-07T18:15:00.463127","indexId":"ofr87140","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":"87-140","title":"Magnetotelluric study of the thickness of volcanic and sedimentary rock in the Pullman-Moscow basin of eastern Washington","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr87140","usgsCitation":"Klein, D.P., Sneddon, R.A., and Smoot, J.L., 1987, Magnetotelluric study of the thickness of volcanic and sedimentary rock in the Pullman-Moscow basin of eastern Washington: U.S. Geological Survey Open-File Report 87-140, iv, 30 p., https://doi.org/10.3133/ofr87140.","productDescription":"iv, 30 p.","costCenters":[],"links":[{"id":406326,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17145.htm","linkFileType":{"id":5,"text":"html"}},{"id":43178,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0140/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148884,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0140/report-thumb.jpg"}],"country":"United States","state":"Idaho, Washington","otherGeospatial":"Pullman-Moscow basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.375,\n              46.583\n            ],\n            [\n              -116.875,\n              46.583\n            ],\n            [\n              -116.875,\n              46.9\n            ],\n            [\n              -117.375,\n              46.9\n            ],\n            [\n              -117.375,\n              46.583\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649494","contributors":{"authors":[{"text":"Klein, D. P.","contributorId":36555,"corporation":false,"usgs":true,"family":"Klein","given":"D.","email":"","middleInitial":"P.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":169534,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sneddon, R. A.","contributorId":84725,"corporation":false,"usgs":true,"family":"Sneddon","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":169536,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smoot, J. L.","contributorId":59794,"corporation":false,"usgs":true,"family":"Smoot","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":169535,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"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":60616,"text":"mf1382E - 1987 - Bouguer gravity anomaly and isostatic residual gravity maps of the Walker Lake 1 degree by 2 degrees Quadrangle, California and Nevada","interactions":[],"lastModifiedDate":"2024-02-14T17:58:03.970155","indexId":"mf1382E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"1382","chapter":"E","title":"Bouguer gravity anomaly and isostatic residual gravity maps of the Walker Lake 1 degree by 2 degrees Quadrangle, California and Nevada","docAbstract":"<p>The accompanying gravity anomaly maps are part of a folio of maps of the Walker Lake 1° by 2° quadrangle, California and Nevada, prepared under the Conterminous United States Mineral Assessment Program. The quadrangle encompasses an area of about 19,500 km<sup>2</sup> along and to the east of the east flank of the Sierra Nevada (fig. 1).</p><p>The Bouguer gravity anomaly map of the Walker Lake quadrangle was prepared by interpolating gravity values among 3,447 gravity stations established in the quadrangle and additional stations from adjacent quadrangles. An isostatic residual gravity map was prepared in order to reduce the effect; of interfering gravity gradients associated with the isostatic root of the Sierra Nevada. Methods of data reduction and factors that limit the accuracy of the gravity values are discussed in the following sections of this report.</p><p>The geologic interpretation of the gravity maps is based on previous studies, sample measurements, and correlation with other maps of the folio including a geologic map (Stewart and others, 1982) and a map showing Mesozoic plutonic rocks (John, 1983). The purpose of the interpretative part of this report is to demonstrate the correlation between gravity anomalies and the mapped geology, to assess the continuation of exposed geologic units beneath the surface, and to suggest the location of concealed subsurface bodies with mineral resource potential. A three-dimensional model of the Little Walker caldera (fig. 6) is used to illustrate a possible quantitative interpretation of a gravity anomaly. A concealed 25 by 75-km Cenozoic batholith along the east flank of the Sierra Nevada with possible lateral extensions is suggested in this report. A possible magmatic mechanism is discussed to augment contemporary explanations for the extensional origin of valleys. The possibility of lower gravity anomalies indicating thinner roof rocks in the basement beneath mountain ranges also is discussed. Furthermore, interpretation of gravity anomalies was applied in discussions with W.D. Menzie (oral commun. , 1982) as one of the criteria used to identify and to delineate areas of mineral resource potential.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1382E","usgsCitation":"Plouff, D., 1987, Bouguer gravity anomaly and isostatic residual gravity maps of the Walker Lake 1 degree by 2 degrees Quadrangle, California and Nevada: U.S. Geological Survey Miscellaneous Field Studies Map 1382, Report: 16 p.; 2 Plates: 29.00 x 25.00 inches and 29.00 x 29.00 inches, https://doi.org/10.3133/mf1382E.","productDescription":"Report: 16 p.; 2 Plates: 29.00 x 25.00 inches and 29.00 x 29.00 inches","costCenters":[],"links":[{"id":88839,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1987/1382e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":88838,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1987/1382e/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":88837,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1987/1382e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":182988,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1987/1382e/report-thumb.jpg"},{"id":105804,"rank":5,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_7077.htm","linkFileType":{"id":5,"text":"html"},"description":"7077"}],"scale":"250000","country":"United States","state":"California, Nevada","otherGeospatial":"Walker Lake","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120,38 ], [ -120,39 ], [ -118,39 ], [ -118,38 ], [ -120,38 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601ff0","contributors":{"authors":[{"text":"Plouff, Donald","contributorId":94657,"corporation":false,"usgs":true,"family":"Plouff","given":"Donald","email":"","affiliations":[],"preferred":false,"id":264083,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29577,"text":"wri854323 - 1987 - Hydrologic effects of artificial-recharge experiments with reclaimed water at East Meadow, Long Island, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:08:58","indexId":"wri854323","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":"85-4323","title":"Hydrologic effects of artificial-recharge experiments with reclaimed water at East Meadow, Long Island, New York","docAbstract":"Artificial recharge experiments were conducted at East Meadow, Long Island, New York, from October 1982 through January 1984 to evaluate the degree of groundwater mounding and the chemical effects of artificially replenishing the groundwater system with tertiary-treated wastewater. More than 800 million gallons of treated effluent was returned to the upper glacial aquifer through recharge basins and injection wells in the 15-month period. Reclaimed water was provided by the Cedar Creek advanced wastewater treatment facility in Wantagh, 6 miles away. The chlorinated effluent was pumped to the recharge facility, where it was fed to basins by gravity flow and to injection wells by pumps. Observations during the recharge tests indicate that the two most significant factors in limiting the rate of infiltration through the basin floor were the recharge test duration and quality of reclaimed water. Head buildup in the aquifer beneath the basins ranged from 4.3 to 6.7 ft, depending on the quantity and duration of water application. Head buildup near the injection wells within the aquifer ranged from 0.3 to 1.2 ft. Recharge basins provided a more effective means of moving large quantities of reclaimed water into the aquifer than injection wells. Results of 3-day and 176-day ponding tests in two basins indicate that reclaimed water is relatively unchanged chemically by percolation through the unsaturated zone because: (1) the sand and gravel of the upper glacial aquifer is unreactive, (2) the water moves to the water table rapidly, and (3) the water is highly treated before recharge. The quality of water in the aquifer zones affected by recharge improved, on the whole. Groundwater concentrations of nitrate nitrogen and several low molecular weight hydrocarbons, decreased to well within drinking water standards as a direct result of recharge. Sodium and chloride concentrations increased above background levels as a result of recharge but remained well within drinking water standards and the New York State effluent standards established for this groundwater recharge study. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854323","usgsCitation":"Schneider, B., Ku, H.F., and Oaksford, E., 1987, Hydrologic effects of artificial-recharge experiments with reclaimed water at East Meadow, Long Island, New York: U.S. Geological Survey Water-Resources Investigations Report 85-4323, vii, 79 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854323.","productDescription":"vii, 79 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123565,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4323/report-thumb.jpg"},{"id":58405,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4323/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db607024","contributors":{"authors":[{"text":"Schneider, B.J.","contributorId":93539,"corporation":false,"usgs":true,"family":"Schneider","given":"B.J.","email":"","affiliations":[],"preferred":false,"id":201753,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ku, H. F.","contributorId":19976,"corporation":false,"usgs":true,"family":"Ku","given":"H.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":201751,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Oaksford, E. T.","contributorId":64284,"corporation":false,"usgs":true,"family":"Oaksford","given":"E. T.","affiliations":[],"preferred":false,"id":201752,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
]}