{"pageNumber":"316","pageRowStart":"7875","pageSize":"25","recordCount":11004,"records":[{"id":61392,"text":"mf2143 - 1991 - Map showing the relationship of selected mafic and ultramafic bodies in the crust of the eastern United States to seismically active areas","interactions":[],"lastModifiedDate":"2012-02-10T00:10:29","indexId":"mf2143","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"2143","title":"Map showing the relationship of selected mafic and ultramafic bodies in the crust of the eastern United States to seismically active areas","language":"ENGLISH","doi":"10.3133/mf2143","usgsCitation":"McCartan, L., Snyder, S.L., and Stover, C.W., 1991, Map showing the relationship of selected mafic and ultramafic bodies in the crust of the eastern United States to seismically active areas: U.S. Geological Survey Miscellaneous Field Studies Map 2143, 1 map :col. ;120 x 97 cm., on sheet 130 x 104 cm., folded in envelope 30 x 24 cm. +1 pamphlet (14 p. : tables ; 28 cm.), https://doi.org/10.3133/mf2143.","productDescription":"1 map :col. ;120 x 97 cm., on sheet 130 x 104 cm., folded in envelope 30 x 24 cm. +1 pamphlet (14 p. : tables ; 28 cm.)","costCenters":[],"links":[{"id":100728,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1991/2143/plate-1.pdf","size":"12680","linkFileType":{"id":1,"text":"pdf"}},{"id":183465,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1991/2143/report-thumb.jpg"},{"id":88961,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1991/2143/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"2500000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -96,23 ], [ -96,51 ], [ -64,51 ], [ -64,23 ], [ -96,23 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9fe4b07f02db660dfb","contributors":{"authors":[{"text":"McCartan, Lucy","contributorId":87960,"corporation":false,"usgs":true,"family":"McCartan","given":"Lucy","affiliations":[],"preferred":false,"id":265569,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Snyder, S. L.","contributorId":25132,"corporation":false,"usgs":true,"family":"Snyder","given":"S.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":265567,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stover, C. W.","contributorId":70369,"corporation":false,"usgs":true,"family":"Stover","given":"C.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":265568,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":64803,"text":"i2108 - 1991 - Geologic map of Bryce Canyon National Park and vicinity, southwestern Utah","interactions":[],"lastModifiedDate":"2022-04-11T21:48:07.605927","indexId":"i2108","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"2108","title":"Geologic map of Bryce Canyon National Park and vicinity, southwestern Utah","docAbstract":"Bryce Canyon National Park is located along the eastern escarpment of the Paunsaugunt Plateau, which along with the Markagunt Plateau to the west, form the southernmost of the High Plateaus of Utah. The park’s unique scenery has been created by forces of differential erosion acting on colorful rocks exposed along and below the rim of the plateau. Park headquarters and major scenic viewpoints that lie on or near the rim of the plateau are accessible from Utah Highway 12 mi west of the park. More remote parts of the park are located in canyons beneath the rim and are accessible only by foot, along horse trails or from a few unimproved dirt roads that approach the park boundary from the east or south.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/i2108","collaboration":"Prepared in collaboration with the U.S. National Parks Service","usgsCitation":"Bowers, W.E., 1991, Geologic map of Bryce Canyon National Park and vicinity, southwestern Utah: U.S. Geological Survey IMAP 2108, Report: iii, 15 p.; 1 Plate: 41.50 × 57.88 inches, https://doi.org/10.3133/i2108.","productDescription":"Report: iii, 15 p.; 1 Plate: 41.50 × 57.88 inches","numberOfPages":"17","costCenters":[],"links":[{"id":187338,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":398514,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10136.htm"},{"id":270132,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/2108/report.pdf"},{"id":260699,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2108/plate-1-preview.pdf"},{"id":260698,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2108/plate-1.pdf"}],"scale":"24000","country":"United States","state":"Utah","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.316,\n              37.438\n            ],\n            [\n              -112.066,\n              37.438\n            ],\n            [\n              -112.066,\n              37.706\n            ],\n            [\n              -112.316,\n              37.706\n            ],\n            [\n              -112.316,\n              37.438\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a361e","contributors":{"authors":[{"text":"Bowers, William E.","contributorId":34129,"corporation":false,"usgs":true,"family":"Bowers","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":272182,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":64968,"text":"i1947C - 1991 - Geologic map and profiles of the north wall of the Snake River Canyon, Thousand Springs and Niagara quadrangles, Idaho","interactions":[],"lastModifiedDate":"2016-08-23T10:16:56","indexId":"i1947C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"1947","chapter":"C","title":"Geologic map and profiles of the north wall of the Snake River Canyon, Thousand Springs and Niagara quadrangles, Idaho","docAbstract":"<p>The Snake River Plain is a broad, arcuate region of low relief that extends more than 300 mi across southern Idaho. The Snake River enters the plain near Idaho Falls and flows westward along the southern margin of the eastern Snake River Plain (fig. 1), a position mainly determined by the basaltic lava flows that erupted near the axis of the plain. The highly productive Snake River Plain aquifer north of the Snake River underlies most of the eastern plain. The aquifer is composed of basaltic rocks that are interbedded with fluvial and lacustrine sedimentary rocks. The top of the aquifer (water table) is typically less than 500 ft below the land surface but is deeper than 1,000 ft in a few areas. The Snake River has excavated a canyon into the nearly flat lying basaltic and sedimentary rocks of the eastern Snake River Plain aquifer, which discharges from the northern canyon wall as springs of variable size, spacing, and altitude. Geologic controls on springs are of importance because nearly 60 percent of the aquifer's discharge occurs as spring flow along the describes the geologic occurrence of springs along the northern wall of the Snake River canyon. This report is one of several that describes the geologic occurrence of springs along the northern wall of the Snake River canyon from Milner Dam to King Hill. To understand the local geologic controls on springs, the Water Resources Division of the U.S. Geological Survey initiated a geologic mapping project as part of their Snake River Plain Regional Aquifer System-Analysis Program. Objectives of the project were (1) to prepare a geologic map of a strip of land immediately north of the Snake River canyon, (2) to map the geology of the north canyon wall in profile, (3) to locate spring occurrences along the north side of the Snake River between Milner Sam and King Hill, and (4) to estimate spring discharge from the north wall of the canyon.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/i1947C","usgsCitation":"Covington, H., and Weaver, J.N., 1991, Geologic map and profiles of the north wall of the Snake River Canyon, Thousand Springs and Niagara quadrangles, Idaho: U.S. Geological Survey IMAP 1947, 45.14 x 33.69 inches, https://doi.org/10.3133/i1947C.","productDescription":"45.14 x 33.69 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":327572,"rank":701,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1947c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":107202,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10023.htm","linkFileType":{"id":5,"text":"html"},"description":"10023"},{"id":189035,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/i1947C.GIF"}],"scale":"24000","datum":"National Geodetic Vertical Datum of 1929","country":"United States","state":"Idaho","otherGeospatial":"Niagara Springs Quadrangles, Snake River Canyon, Thousand Springs Quadrangles","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.62,42.65 ], [ -114.62,42.75 ], [ -114.85,42.75 ], [ -114.85,42.65 ], [ -114.62,42.65 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a48d2","contributors":{"authors":[{"text":"Covington, H. R.","contributorId":92671,"corporation":false,"usgs":true,"family":"Covington","given":"H. R.","affiliations":[],"preferred":false,"id":272442,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weaver, Jean N.","contributorId":65099,"corporation":false,"usgs":true,"family":"Weaver","given":"Jean","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":272441,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":66167,"text":"i2151 - 1991 - Chart showing correlations of upper Cretaceous Fox Hills Sandstone and Lance Formation, and lower Tertiary Fort Union, Wasatch, and Green River formations, from the eastern flank of the Washakie Basin to the southeastern part of the Great Divide Basin, Wyoming","interactions":[],"lastModifiedDate":"2017-06-27T15:51:46","indexId":"i2151","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"2151","title":"Chart showing correlations of upper Cretaceous Fox Hills Sandstone and Lance Formation, and lower Tertiary Fort Union, Wasatch, and Green River formations, from the eastern flank of the Washakie Basin to the southeastern part of the Great Divide Basin, Wyoming","docAbstract":"<p>The stratigraphic sections show surface and subsurface correlations of some Upper Cretaceous and lower Tertiary rocks along the eastern flank of the Washakie basin and southeastern part of the Great Divide basin, Wyoming. These rock crop out from near Baggs, Wyoming, to near Creston Junction, Wyoming, 50 mi (80km) to the north. This report is a continuation of our stratigraphic investigations from south of Baggs, Wyoming to Craig, Colorado.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i2151","usgsCitation":"Hettinger, R.D., Honey, J., and Nichols, D.J., 1991, Chart showing correlations of upper Cretaceous Fox Hills Sandstone and Lance Formation, and lower Tertiary Fort Union, Wasatch, and Green River formations, from the eastern flank of the Washakie Basin to the southeastern part of the Great Divide Basin, Wyoming: U.S. Geological Survey IMAP 2151, 57.18 x 41.47 inches, https://doi.org/10.3133/i2151.","productDescription":"57.18 x 41.47 inches","costCenters":[],"links":[{"id":188682,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":107305,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10150.htm","linkFileType":{"id":5,"text":"html"},"description":"10150"}],"country":"United States","state":"Wyoming","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -107.91666666666667,41 ], [ -107.91666666666667,41.733333333333334 ], [ -107.5,41.733333333333334 ], [ -107.5,41 ], [ -107.91666666666667,41 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478ee4b07f02db489e06","contributors":{"authors":[{"text":"Hettinger, R. D.","contributorId":92283,"corporation":false,"usgs":true,"family":"Hettinger","given":"R.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":274093,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Honey, J.G.","contributorId":79915,"corporation":false,"usgs":true,"family":"Honey","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":274092,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nichols, D. J.","contributorId":55466,"corporation":false,"usgs":true,"family":"Nichols","given":"D.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":274091,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":69164,"text":"coal139A - 1991 - Subsurface cross section showing coal beds in the Sagavanirktok Formation, vicinity of Prudhoe Bay, east-central North Slope, Alaska","interactions":[],"lastModifiedDate":"2022-09-02T20:21:21.608522","indexId":"coal139A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":309,"text":"Coal Map","code":"COAL","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"139","chapter":"A","title":"Subsurface cross section showing coal beds in the Sagavanirktok Formation, vicinity of Prudhoe Bay, east-central North Slope, Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/coal139A","usgsCitation":"Roberts, S.B., 1991, Subsurface cross section showing coal beds in the Sagavanirktok Formation, vicinity of Prudhoe Bay, east-central North Slope, Alaska: U.S. Geological Survey Coal Map 139, Report: 1 p.; 1 Plate: 49.65 × 34.04 inches, https://doi.org/10.3133/coal139A.","productDescription":"Report: 1 p.; 1 Plate: 49.65 × 34.04 inches","costCenters":[],"links":[{"id":406183,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_19709.htm","linkFileType":{"id":5,"text":"html"}},{"id":191764,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/coal/139a/report-thumb.jpg"},{"id":115352,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/coal/139a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":115351,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/coal/139a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"517000","country":"United States","state":"Alaska","otherGeospatial":"Sagavanirktok Formation","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -149.367,\n              70\n            ],\n            [\n              -147.5,\n              70\n            ],\n            [\n              -147.5,\n              70.5\n            ],\n            [\n              -149.367,\n              70.5\n            ],\n            [\n              -149.367,\n              70\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699ad7","contributors":{"authors":[{"text":"Roberts, Stephen B.","contributorId":104906,"corporation":false,"usgs":true,"family":"Roberts","given":"Stephen","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":279746,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55055,"text":"wdrVA902 - 1991 - Water resources data, Virginia, water year 1990. Volume 2: Ground-water level and ground-water quality records","interactions":[],"lastModifiedDate":"2020-10-06T21:20:18.702761","indexId":"wdrVA902","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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-90-2","title":"Water resources data, Virginia, water year 1990. Volume 2: Ground-water level and ground-water quality records","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrVA902","usgsCitation":"Prugh, B., and Easton, F., 1991, Water resources data, Virginia, water year 1990. 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