{"pageNumber":"334","pageRowStart":"8325","pageSize":"25","recordCount":11004,"records":[{"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":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":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":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":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":12146,"text":"ofr87106 - 1987 - Maps of runoff in the northeastern region and the southern Blue Ridge Province of the United States during selected periods in 1983-85","interactions":[],"lastModifiedDate":"2024-11-27T22:29:05.831365","indexId":"ofr87106","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":"87-106","title":"Maps of runoff in the northeastern region and the southern Blue Ridge Province of the United States during selected periods in 1983-85","docAbstract":"<p>Maps of annual runoff for two regions in the eastern United States were prepared by the U.S. Geological Survey for the Direct/Delayed Response Project being conducted by the U.S. EPA. These maps show annual runoff during water year 1984 in the northeastern region and in the Southern Blue Ridge Province.</p>\n<p>Runoff from the northeastern region during the 1984 water yr ranged from 12 to 55 in.; this was 25 to 55% &gt; average runoff for the 1951-80 period. Runoff from the Southern Blue Ridge Province during the 1984 water year ranged from 14 to 60 in.; this was 10 to 30% &gt; the average runoff for the 1951-80 period.</p>\n<p>A split sample analysis of the data for New York was conducted to evaluate the accuracy of the runoff mapping procedure used in this report. A runoff map was prepared using one-half of the data base. The map was then used to estimate runoff at the gaging stations that were not used to develop the map. The values estimated from the split-sample map were found to differ from the actual recorded values by 9.9%.</p>\n<p>The runoff maps are most accurate in areas with a relatively large concentration of gaging stations and little topographic variability. Conversely, the maps are least accurate in areas with few gaging stations and high topographic variability. Based on these criteria, those parts of the maps covering Connecticut, Massachusetts, New Jersey, and Rhode Island, are the most reliable. The least reliable parts of the maps are those along the North Carolina-Tennessee border and in parts of Maine.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr87106","collaboration":"Prepared in cooperation with the U.S. Environmental Protection Agency Environmental Research Laboratory Corvallis, Oregon","usgsCitation":"Graczyk, D., Gebert, W., Krug, W., and Allord, G., 1987, Maps of runoff in the northeastern region and the southern Blue Ridge Province of the United States during selected periods in 1983-85: U.S. Geological Survey Open-File Report 87-106, Report: iv, 8 p.; 3 Plates: 18.49 x 18.85 inches or smaller, https://doi.org/10.3133/ofr87106.","productDescription":"Report: iv, 8 p.; 3 Plates: 18.49 x 18.85 inches or smaller","numberOfPages":"12","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":464575,"rank":7,"type":{"id":36,"text":"NGMDB 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,{"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":15445,"text":"ofr87545 - 1987 - Ground-water levels in the alluvial aquifer in eastern Arkansas, 1986","interactions":[],"lastModifiedDate":"2012-02-02T00:07:04","indexId":"ofr87545","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":"87-545","title":"Ground-water levels in the alluvial aquifer in eastern Arkansas, 1986","docAbstract":"This report, prepared by the U.S. Geological Survey in cooperation with the Arkansas Soil and Water Conservation Commission, the U.S. Soil Conservation Service, and local Conservation Districts, contains groundwater level measurements of 512 wells tapping the Mississippi River Valley alluvial aquifer of eastern Arkansas. The measurements were made by district Soil Conservation Service personnel during 1986. The purpose of this report is to provide these data to other State and Federal agencies as well as to private landowners. The shallowest pre-pumping water levels occurred in Clay, Independence, Mississippi, and Randolph Counties where the average depth to water was 15 feet or less. The deepest water levels occurred in interstream areas where groundwater withdrawals were the greatest. Water levels of 100 feet or greater below land surface were measured in Arkansas, Cross, Lonoke, Poinsett, and Prairie Counties. Water level measurements made during the post-pumping (recovery) season averaged about 3 feet less than those made during the pre-pumping season. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87545","usgsCitation":"Plafcan, M., 1987, Ground-water levels in the alluvial aquifer in eastern Arkansas, 1986: U.S. Geological Survey Open-File Report 87-545, iv, 31 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr87545.","productDescription":"iv, 31 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":148754,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0545/report-thumb.jpg"},{"id":44415,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0545/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6674f6","contributors":{"authors":[{"text":"Plafcan, Maria","contributorId":20338,"corporation":false,"usgs":true,"family":"Plafcan","given":"Maria","email":"","affiliations":[],"preferred":false,"id":171148,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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":57328,"text":"wdrVA861 - 1987 - Water resources data for Virginia, water year 1986","interactions":[],"lastModifiedDate":"2020-12-14T23:42:38.298284","indexId":"wdrVA861","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"VA-86-1","title":"Water resources data for Virginia, water year 1986","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrVA861","usgsCitation":"Prugh, B., Easton, F., and Lynch, D.D., 1987, Water resources data for Virginia, water year 1986: U.S. Geological Survey Water Data Report VA-86-1, xii, 395 p., https://doi.org/10.3133/wdrVA861.","productDescription":"xii, 395 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,{"id":16515,"text":"ofr87107 - 1987 - Geohydrologic framework of the Snake River plain regional aquifer system, Idaho and eastern Oregon","interactions":[],"lastModifiedDate":"2022-08-17T19:02:14.613053","indexId":"ofr87107","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":"87-107","title":"Geohydrologic framework of the Snake River plain regional aquifer system, Idaho and eastern Oregon","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr87107","usgsCitation":"Whitehead, R., 1987, Geohydrologic framework of the Snake River plain regional aquifer system, Idaho and eastern Oregon: U.S. Geological Survey Open-File Report 87-107, Report: vii, 60 p.; 6 Plates: 41.04 × 23.81 inches or smaller, https://doi.org/10.3133/ofr87107.","productDescription":"Report: vii, 60 p.; 6 Plates: 41.04 × 23.81 inches or smaller","costCenters":[],"links":[{"id":45498,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0107/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45492,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0107/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":405269,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17139.htm","linkFileType":{"id":5,"text":"html"}},{"id":45495,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0107/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45494,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0107/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45493,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0107/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45497,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0107/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45496,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0107/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148385,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0107/report-thumb.jpg"}],"country":"United States","state":"Idaho, Oregon","otherGeospatial":"Snake River plain regional aquifer system","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.83837890625,\n              42.06560675405716\n            ],\n            [\n              -111.75,\n              42.06560675405716\n            ],\n            [\n              -111.75,\n              45.3521452458518\n            ],\n            [\n              -121.83837890625,\n              45.3521452458518\n            ],\n            [\n              -121.83837890625,\n              42.06560675405716\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8ea2","contributors":{"authors":[{"text":"Whitehead, R.L.","contributorId":34891,"corporation":false,"usgs":true,"family":"Whitehead","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":172979,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":67575,"text":"i1797A - 1987 - Chart showing lithology, mineralogy, and paleontology of the nonmarine North Horn Formation and Flagstaff Member of the Green River Formation, Price Canyon, central Utah: a principal reference section","interactions":[],"lastModifiedDate":"2025-08-14T16:30:00.294686","indexId":"i1797A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1797","chapter":"A","title":"Chart showing lithology, mineralogy, and paleontology of the nonmarine North Horn Formation and Flagstaff Member of the Green River Formation, Price Canyon, central Utah: a principal reference section","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i1797A","usgsCitation":"Fouch, T.D., Hanley, J., Forester, R.M., Keighin, C.W., Pitman, J.K., and Nichols, D.J., 1987, Chart showing lithology, mineralogy, and paleontology of the nonmarine North Horn Formation and Flagstaff Member of the Green River Formation, Price Canyon, central Utah: a principal reference section: U.S. Geological Survey IMAP 1797, Report: 8 p.; 1 Plate: 55.32 × 37.51 inches, https://doi.org/10.3133/i1797A.","productDescription":"Report: 8 p.; 1 Plate: 55.32 × 37.51 inches","costCenters":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":256572,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1797a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":91701,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1797a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":186145,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1797a/report-thumb.jpg"},{"id":395024,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9917.htm"}],"scale":"37500","country":"United States","state":"Utah","otherGeospatial":"Price Canyon","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111,\n              39.667\n            ],\n            [\n              -110.75,\n              39.667\n            ],\n            [\n              -110.75,\n              39.917\n            ],\n            [\n              -111,\n              39.917\n            ],\n            [\n              -111,\n              39.667\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4c6d","contributors":{"authors":[{"text":"Fouch, T. D.","contributorId":68333,"corporation":false,"usgs":true,"family":"Fouch","given":"T.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":276762,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hanley, J.H.","contributorId":35011,"corporation":false,"usgs":true,"family":"Hanley","given":"J.H.","affiliations":[],"preferred":false,"id":276760,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Forester, R. M.","contributorId":76332,"corporation":false,"usgs":true,"family":"Forester","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":276763,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Keighin, C. W.","contributorId":79887,"corporation":false,"usgs":true,"family":"Keighin","given":"C.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":276764,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Pitman, Janet K. 0000-0002-0441-779X jpitman@usgs.gov","orcid":"https://orcid.org/0000-0002-0441-779X","contributorId":767,"corporation":false,"usgs":true,"family":"Pitman","given":"Janet","email":"jpitman@usgs.gov","middleInitial":"K.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true},{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":276765,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Nichols, D. J.","contributorId":55466,"corporation":false,"usgs":true,"family":"Nichols","given":"D.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":276761,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":27485,"text":"wri874164 - 1987 - Evaluation of the potential for artificial ground-water recharge in eastern San Joaquin County, California — Phase 3","interactions":[],"lastModifiedDate":"2022-01-18T22:43:49.45933","indexId":"wri874164","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4164","title":"Evaluation of the potential for artificial ground-water recharge in eastern San Joaquin County, California — Phase 3","docAbstract":"<p>Infiltration tests were used to evaluate the potential of basin spreading surface water as a means of artificially recharging the aquifer system in eastern San Joaquin County, California. Two infiltration sites near Lockeford and Linden were selected on the basis of information collected during the first two phases of the study. Data from the infiltration tests indicate that the two sites are acceptable for recharge by the basin-spreading method. Infiltration rates ranged between 6.7 and 10.5 ft/day near Lockeford and between 2.6 and 11.2 ft/day near Linden. Interpretation of these data is limited by lack of information on the response of the saturated zone during testing and by the inherent difficulty in extrapolating the results of small-scale tests to larger long-term operations. Lithology is a major factor that controls infiltration rates at the test sites. The unsaturated zone is characterized by heterogeneous layers of coarse- and fine- grained materials. Clay layers of low hydraulic conductivity commonly form discontinuous lenses that may cause a transient perched water table to develop during recharge. Water level measurements from wells screened in the unsaturated zone indicate that the perched water table could reach the land surface after 2 and 5 months of recharge near Lockeford and Linden, respectively. These figures probably represent the minimum time necessary for saturation of the land. Another major factor that affects infiltration rates is the quality of the recharge water, particularly the suspended sediment content. The clogging action of suspended sediment may be minimized by: (1) pretreatment of recharge water in a settling pond, (2) adherence to a routine program of monitoring and maintenance, and (3) proper design of the recharge facility. Other factors that affect infiltration rates include basin excavation technique, basin shape, and maintenance procedures. Efficient operation of the recharge facility requires careful attention to the relation between subsurface water levels and infiltration rates.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri874164","usgsCitation":"Hamlin, S.N., 1987, Evaluation of the potential for artificial ground-water recharge in eastern San Joaquin County, California — Phase 3: U.S. Geological Survey Water-Resources Investigations Report 87-4164, iv, 17 p., https://doi.org/10.3133/wri874164.","productDescription":"iv, 17 p.","costCenters":[],"links":[{"id":56336,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4164/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":394485,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_46823.htm"},{"id":124290,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4164/report-thumb.jpg"}],"country":"United States","state":"California","county":"San Joaquin County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.2992,\n              37.8292\n            ],\n            [\n              -120.933,\n              37.8292\n            ],\n            [\n              -120.933,\n              38.25\n            ],\n            [\n              -121.2992,\n              38.25\n            ],\n            [\n              -121.2992,\n              37.8292\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa1ac","contributors":{"authors":[{"text":"Hamlin, S. N.","contributorId":46560,"corporation":false,"usgs":true,"family":"Hamlin","given":"S.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":198199,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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":59728,"text":"mf1982 - 1987 - Median-porosity contour maps of the J Sandstone, Dakota Group, in the Denver Basin, Colorado, Nebraska, and Wyoming","interactions":[],"lastModifiedDate":"2025-05-27T18:34:31.463601","indexId":"mf1982","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":"1982","title":"Median-porosity contour maps of the J Sandstone, Dakota Group, in the Denver Basin, Colorado, Nebraska, and Wyoming","docAbstract":"<p>The Lower Cretaceous J sandstone of the Dakota Group is present in the Denver basin in eastern Colorado, southeastern Wyoming, and southwestern Nebraska. Deposited during a regression of the Cretaceous epicontinental sea, this informally named unit is composed primarily of sandstone and shale of deltaic and near shore-marine origin. The J sandstone can be divided into an upper transgressive sand, a middle marginal-marine and deltaic facies, and a lower prodelta sequence (Clark, 1978). The depth from the surface to the top of the J sandstone increases from about 4,000 ft on the gently-dipping eastern flank of the basin to more than 8,000 ft at the basin ax is near the steeply-dipping western flank.</p>\n<p>Porosity data compiled in this study were determined from J sandstone cores from 134 widely spaced boreholes. Porosity in areas of poor core coverage was determined from neutron density logs from an additional 20 boreholes ( corrected to core average grain density). Median, rather than average, porosity was used in order to minimize the statistical effect of anomalously high and low porosity values. Thirty-five oil companies and independent operators supplied core porosity data. Core porosities were determined by means of helium porosimetry, primarily by Core Laboratories of Denver, Colo.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1982","usgsCitation":"Higley, D., and Gautier, D.L., 1987, Median-porosity contour maps of the J Sandstone, Dakota Group, in the Denver Basin, Colorado, Nebraska, and Wyoming: U.S. Geological Survey Miscellaneous Field Studies Map 1982, 1 Plate: 37.30 x 38.73 inches, https://doi.org/10.3133/mf1982.","productDescription":"1 Plate: 37.30 x 38.73 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":327248,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1982/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":486612,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5567.htm","linkFileType":{"id":5,"text":"html"}},{"id":182300,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1982.PNG"}],"country":"United States","state":"Colorado, Nebraska, Wyoming","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -103,\n              39\n            ],\n            [\n              -103,\n              41.5\n            ],\n            [\n              -105,\n              41.5\n            ],\n            [\n              -105,\n              39\n            ],\n            [\n              -103,\n              39\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db61006c","contributors":{"authors":[{"text":"Higley, D.K. 0000-0001-8024-9954","orcid":"https://orcid.org/0000-0001-8024-9954","contributorId":90261,"corporation":false,"usgs":true,"family":"Higley","given":"D.K.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":262491,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gautier, D. L.","contributorId":69996,"corporation":false,"usgs":true,"family":"Gautier","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":262490,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"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":29745,"text":"wri824010 - 1987 - Ground-water hydrology of the Toppenish Creek basin, Yakima Indian Reservation, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:08:59","indexId":"wri824010","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":"82-4010","title":"Ground-water hydrology of the Toppenish Creek basin, Yakima Indian Reservation, Washington","docAbstract":"A groundwater flow model was constructed for the Toppenish Creek basin aquifer system in eastern Washington. Flow was simulated in three aquifer units: (1) the confined old valley fill and shallow basalt (unit 2); (2) the underlying primary basalt (unit 3); and (3) the deep basalt (unit 4). Water levels in the overlying unconfined alluvial aquifer (unit 1) were held fixed. Calibrated transmissivities ranged from 0.01 to 0.48 foot squared per second. Calibrated storage coefficients were 0.0004 to 0.006. The confining-bed leakance ranged from 2.0 x 10 to the minus 11th power to 2.5 x 10 to the minus 10th power feet per second per foot. Under steady-state conditions (1954) annual natural recharge was about 29,000 acre-ft underflow from adjacent basins. Annual pumpage increased from less than 500 acre-ft in 1954 to an average of 19,600 acre-ft for 1971 and 1972. Pumpage caused simulated declines in unit 3 of up to 95 ft for 1955-72. Projected annual declines from 1973-77 using 1971-72 pumpage were about 0.5-1.5 ft in unit 2 and 0.2-1.5 ft in unit 3. The corresponding declines from 1978-82 were 0.2-1.2 ft and 0.2-0.8 ft, respectively. Using 1971-72 pumpage plus 12 ,400 acre-ft per year from unit 3, the calculated annual declines from 1978-82 were 1-36 ft in unit 2 and 4-20 ft in unit 3. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824010","usgsCitation":"Skrivan, J., 1987, Ground-water hydrology of the Toppenish Creek basin, Yakima Indian Reservation, Washington: U.S. Geological Survey Water-Resources Investigations Report 82-4010, vi, 47 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824010.","productDescription":"vi, 47 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":122648,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4010/report-thumb.jpg"},{"id":58544,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4010/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db6986b6","contributors":{"authors":[{"text":"Skrivan, J.A.","contributorId":107743,"corporation":false,"usgs":true,"family":"Skrivan","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":202047,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14775,"text":"ofr86532 - 1987 - Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts","interactions":[{"subject":{"id":14775,"text":"ofr86532 - 1987 - Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts","indexId":"ofr86532","publicationYear":"1987","noYear":false,"title":"Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts"},"predicate":"SUPERSEDED_BY","object":{"id":2191,"text":"wsp2336A - 1988 - Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts","indexId":"wsp2336A","publicationYear":"1988","noYear":false,"chapter":"A","title":"Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts"},"id":1}],"supersededBy":{"id":2191,"text":"wsp2336A - 1988 - Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts","indexId":"wsp2336A","publicationYear":"1988","noYear":false,"title":"Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts"},"lastModifiedDate":"2020-05-13T16:47:03.039489","indexId":"ofr86532","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":"86-532","title":"Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts","docAbstract":"<p>The Edwards aquifer is a complexly faulted, carbonate aquifer lying within the Balcones fault zone of south-central Texas. The aquifer is recharged mainly by streamflow losses in the outcrop area of the Edwards aquifer and is discharged by major springs located at considerable distances, as much as 150 mi, from the areas of recharge, and by wells. Groundwater flow within the Edwards aquifer of the San Antonio region was simulated to investigate concepts relating to the storage and flow characteristics. A general purpose, finite difference model, modified to provide the capability of representing barrier faults, was used to simulate groundwater flow and storage in the aquifer. The simulations investigated the effects of complex geologic structures and significant changes in transmissivity, anisotropy, and storage coefficient, with initial values based on concepts developed in previous studies. Results of the simulations confirmed the original estimates of transmissivity values (&gt; 100 sq ft/sec) in the confined zone of the aquifer between San Antonio and Comal Springs. A storage coefficient of 0.05 in the unconfined zone of the aquifer produced the best simulation of water levels and springflow. A major interpretation resulting from the simulations is that two essentially independent areas of regional flow were identified in the west and central part of the study area. Flow from the two areas converges at Comal Springs. The directions of computed flux vectors reflected the presence of major barrier faults which locally deflect patterns of groundwater movement. The most noticeable deflection is the convergence of flow through the geologic structural opening, the Knippa gap, in eastern Uvalde County. A second significant interpretation is that groundwater flow in northeastern Bexar, Comal, and Hays Counties is diverted by barrier faults toward San Marcos Springs, a regional discharge point. (Lantz-PTT)</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr86532","usgsCitation":"Maclay, R., and Land, L.F., 1987, Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts: U.S. Geological Survey Open-File Report 86-532, vii, 86 p., https://doi.org/10.3133/ofr86532.","productDescription":"vii, 86 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":374776,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0532/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148809,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0532/report-thumb.jpg"}],"country":"United States","state":"Texas","city":"San Antonio","otherGeospatial":"Edwards 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R.W.","contributorId":72804,"corporation":false,"usgs":true,"family":"Maclay","given":"R.W.","affiliations":[],"preferred":false,"id":169983,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Land, L. F.","contributorId":17253,"corporation":false,"usgs":true,"family":"Land","given":"L.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":169982,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":60284,"text":"mf1461 - 1987 - Subsurface stratigraphy of the eastern Hollister Valley, California","interactions":[],"lastModifiedDate":"2016-08-22T15:44:24","indexId":"mf1461","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":"1461","title":"Subsurface stratigraphy of the eastern Hollister Valley, California","docAbstract":"<p>In September 1977, four cores were recovered by shallow auger drilling from Hollister Valley, California, near the Calaveras fault. The wells were drilled to search for evidence that Hollister Valley may have been occupied by a large lake during the late Pleistocene or Holocene. This small valley, near Monterey Bay, may have been dammed by a large landslide on the San Andreas fault (Jenkins, 1973; Herd and Helley, 1977). The cores sampled the first 38 m of sediment below the valley floor, but no lacustrine deposits were found at these sites; a very detailed record to Holocene alluviation in a tectonically subsiding basin.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1461","usgsCitation":"McMasters, C.R., Herd, D.G., Throckmorton, C.K., and Heusser, L., 1987, Subsurface stratigraphy of the eastern Hollister Valley, California: U.S. Geological Survey Miscellaneous Field Studies Map 1461, 3 plates: 41.99 x 35.50 inches or smaller, https://doi.org/10.3133/mf1461.","productDescription":"3 plates: 41.99 x 35.50 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":183011,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1461.PNG"},{"id":327348,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1461/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":327349,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1461/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":327350,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1461/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"California","otherGeospatial":"Hollister Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -121.66666666666667,36.75 ], [ -121.66666666666667,37 ], [ -121.33333333333333,37 ], [ -121.33333333333333,36.75 ], [ -121.66666666666667,36.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db6999f4","contributors":{"authors":[{"text":"McMasters, Catherine R.","contributorId":173570,"corporation":false,"usgs":false,"family":"McMasters","given":"Catherine","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":263447,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Herd, Darrell G.","contributorId":72363,"corporation":false,"usgs":true,"family":"Herd","given":"Darrell","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":263450,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Throckmorton, Constance K.","contributorId":36935,"corporation":false,"usgs":true,"family":"Throckmorton","given":"Constance","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":263448,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Heusser, Linda E.","contributorId":54203,"corporation":false,"usgs":true,"family":"Heusser","given":"Linda E.","affiliations":[],"preferred":false,"id":263449,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":29919,"text":"wri864317 - 1987 - Geology and hydrology of the Onondaga aquifer in eastern Erie County, New York, with emphasis on ground-water-level declines since 1982","interactions":[],"lastModifiedDate":"2022-02-02T19:34:07.04247","indexId":"wri864317","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":"86-4317","title":"Geology and hydrology of the Onondaga aquifer in eastern Erie County, New York, with emphasis on ground-water-level declines since 1982","docAbstract":"<p>The Onondaga aquifer is a nearly flat-lying, 25- to 110-foot-thick, cherty limestone with moderately developed karst features such as sinkholes, disappearing streams, and solution-widened joints. Most groundwater moves through solution-widened bedding planes, although some moves through vertical joints. The yield of water from 42 wells ranges from 3 to 100 gal/min, averaging 20 gal/min. Groundwater levels in the Onondaga aquifer declined during the fall of 1981 and summer and fall of 1982-85, near a 2.2-mile-long and 800-foot-wide land surface depression in the eastern part of Erie County. More than 60 wells and several wetlands went dry and at least three sinkholes developed. Groundwater levels were measured in 150 wells during a high water level period in April 1984 and a low water period in October 1984. Water levels fluctuated 20 to 50 ft near the depression and near the quarries but fluctuated only 5 to 10 ft elsewhere. The water level decline was caused by the combined effect of groundwater removal by pumpage from a quarry (the water is then discharged to Dorsch Creek) and by the swallets in the 2.2-mile-long depression area, which are recharge points for the aquifer. In 1982, sinkholes formed in a surface depression area in Harris Hill. The enlargement of these sinkholes seems to be unrelated to the water level decline in the eastern part of the county and is probably caused by local drainage alterations.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864317","usgsCitation":"Staubitz, W., and Miller, T.S., 1987, Geology and hydrology of the Onondaga aquifer in eastern Erie County, New York, with emphasis on ground-water-level declines since 1982: U.S. Geological Survey Water-Resources Investigations Report 86-4317, Report: vi, 44 p.; 4 Plates: 33.74 × 23.81 inches or smaller, https://doi.org/10.3133/wri864317.","productDescription":"Report: vi, 44 p.; 4 Plates: 33.74 × 23.81 inches or smaller","costCenters":[],"links":[{"id":395295,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36637.htm"},{"id":58740,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4317/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58739,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4317/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58738,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4317/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58737,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4317/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58736,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4317/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123337,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4317/report-thumb.jpg"}],"country":"United States","state":"New York","county":"Erie County","otherGeospatial":"Onondaga aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -78.7,\n              42.933\n            ],\n            [\n              -78.463,\n              42.933\n            ],\n            [\n              -78.463,\n              43.033\n            ],\n            [\n              -78.7,\n              43.033\n            ],\n            [\n              -78.7,\n              42.933\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b468a","contributors":{"authors":[{"text":"Staubitz, W. W.","contributorId":73209,"corporation":false,"usgs":true,"family":"Staubitz","given":"W. W.","affiliations":[],"preferred":false,"id":202359,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, Todd S.","contributorId":85623,"corporation":false,"usgs":true,"family":"Miller","given":"Todd","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":202360,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3603,"text":"cir968 - 1987 - Development of sinkholes resulting from man's activities in the Eastern United States","interactions":[],"lastModifiedDate":"2016-01-25T10:39:26","indexId":"cir968","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":"968","title":"Development of sinkholes resulting from man's activities in the Eastern United States","docAbstract":"<p>Development of induced sinkholes in carbonate terranes in the Eastern United States has resulted in costly damage and water pollution. Previously, detailed investigations of sinkholes were limited to Alabama and Missouri, with the most comprehensive being in Alabama. An investigation of the remainder of the area was made in 1981 to regionalize previous findings. More than 850 sites of sinkhole development have been identified in 19 States. It is estimated that more than 6,500 sinkholes or related features have formed at these sites. Most have occurred since 1950. Based on information available, States most impacted are Alabama, Florida, Georgia, Missouri, Pennsylvania, and Tennessee.</p>\n<p>The total cost of damage and associated protective measures resulting from induced sinkholes is unknown. Costs reported for a limited number of sites were about $170 million--expended almost entirely after 1970. About $140 million were expended at five dams in four States and to repair or protect highways in two States.</p>\n<p>Sinkholes are of two types, natural and induced {accelerated or caused by man}. The sudden development of both types results from the collapse of the roof of a cavity or cavern in rock, or from the downward migration of unconsolidated deposits into solutionally enlarged openings in the top of bedrock. The occurrence of sinkholes resulting from bedrock roof collapses, in comparison with the occurrence of sinkholes resulting from downward migration of unconsolidated deposits, is rare.</p>\n<p>Induced sinkholes are of two types: those resulting from a decline in water level due to ground-water withdrawals and those resulting from construction. Sinkholes resulting from water-level declines are caused by loss of buoyant support, increase in velocity of water movement, water-level fluctuations, and induced recharge. Most induced sinkholes resulting from construction are caused by the diversion or impoundment of surface drainage over unconsolidated deposits resting on openings in the top of bedrock. Collapse mechanisms include loading, saturation, and piping.</p>\n<p>Assessment of existing or potential sinkhole problems at a site requires recognition of features associated with sinkhole development and knowledge of triggering mechanisms that cause sinkholes. Natural sinkhole development is generally not predictable. Induced sinkhole development is predictable in some instances, but is predictable only in the sense that it will occur in a particular area. The most predictable development results from dewatering by wells, quarries, and mines.</p>\n<p>Alternatives that allow avoiding or minimizing sinkhole hazards are most numerous when a problem or potential problem is recognized during site evaluation. The number of alternatives declines after the beginning of site development. Where sinkhole development is predictable, zoning of land use can minimize hazards.</p>","language":"English","publisher":"U.S. Government Print Office","doi":"10.3133/cir968","usgsCitation":"Newton, J.G., 1987, Development of sinkholes resulting from man's activities in the Eastern United States: U.S. Geological Survey Circular 968, iv, 54 p., https://doi.org/10.3133/cir968.","productDescription":"iv, 54 p.","numberOfPages":"62","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":30638,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1987/0968/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124742,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1987/0968/report-thumb.jpg"}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": 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,{"id":61333,"text":"mf1981 - 1987 - Oblique map of the northern Sierra Nevada, California, showing location of gold-bearing areas","interactions":[],"lastModifiedDate":"2025-05-27T18:29:42.950442","indexId":"mf1981","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":"1981","title":"Oblique map of the northern Sierra Nevada, California, showing location of gold-bearing areas","docAbstract":"<p>More than a third of the gold produced by the United States was mined in California. The bulk of this gold was recovered from the western slope of the northern half of the Sierra Nevada between the Merced River in the south and the Feather River to the north, a distance of about 170 mi. Gold was first discovered, in this region, on the American River at Coloma in 1848, triggering the famed California gold rush. Mining was continuously active, somewhere in the area, from the discovery of gold until World War II when mining was legally prohibited. Dramatic increases in gold prices in the past decade coupled with recent advances in extractive techniques have revitalized prospecting, and major deposits are currently being explored and developed.</p>\n<p>Gold has been found in a variety of geologic environments in the region. In addition to production from the complex vein systems of the historically famous Mother Lode and associated East Gold Belt and West Gold Belt, large amounts of gold have also been recovered from the Grass Valley-Nevada City and other isolated lode districts and from Tertiary river channels and Quaternary alluvium.</p>\n<p>This oblique map illustrates the relation of the different gold-bearing environments&nbsp;to each other and to the general terrain of the northern Sierra Nevada. The map was derived from the 1970 U.S. Geological Survey 1:500,000-scale topographic map of&nbsp;California and the 1976 U.S. Geological Survey 1:500,000-scale topographic map of Nevada, using an isometrograph, a mechanical instrument that produces an oblique framework by tracing individual contours. Form lines sketched over this framework graphically portray the physiographic configuration of the region. Relief on the oblique map has a 3:1 vertical exaggeration and appears as if viewed from a 30&deg; angle above the horizon.</p>\n<p>Locations of lode gold prospects and mines shown on the map were obtained from the U.S. Geological Survey's Mineral Resource Data System (MRDS), a computerized mineral-resource information file, and plotted in their respective locations (D.F. Huber, written commun., 1986). Some locations from two northern counties, missing from the MRDS retrival, were added. The twenty lode mines believed to be the most productive are cited in table 1. A total of nearly 4,000 sites, including both prospects and mines, were initially plotted, but about a third of those were obscured by topography on the oblique map. Locations of Tertiary river channels and gold-dredging fields were taken from published general references modified by examining specific sources and by cursory field examination. Seven of the major dredge fields are identified in table 2.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1981","usgsCitation":"Alpha, T.R., Dodge, F.C., and Bliss, J.D., 1987, Oblique map of the northern Sierra Nevada, California, showing location of gold-bearing areas: U.S. Geological Survey Miscellaneous Field Studies Map 1981, 1 Plate: 47.11 x 31.51 inches, https://doi.org/10.3133/mf1981.","productDescription":"1 Plate: 47.11 x 31.51 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":179871,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1981.PNG"},{"id":486611,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5566.htm","linkFileType":{"id":5,"text":"html"}},{"id":327579,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1981/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"northern Sierra Nevada","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -122,\n              40\n            ],\n            [\n              -122,\n              36.6833\n            ],\n            [\n              -118.5583,\n              36.683\n            ],\n            [\n              -118.5583,\n              40\n            ],\n            [\n              -122,\n              40\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db69659d","contributors":{"authors":[{"text":"Alpha, T. 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,{"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. 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,{"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, 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