{"pageNumber":"1730","pageRowStart":"43225","pageSize":"25","recordCount":68937,"records":[{"id":65819,"text":"i2276 - 1992 - Shaded relief and surface markings map of the Lunar near side","interactions":[],"lastModifiedDate":"2019-12-23T11:48:34","indexId":"i2276","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"2276","title":"Shaded relief and surface markings map of the Lunar near side","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i2276","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1992, Shaded relief and surface markings map of the Lunar near side: U.S. Geological Survey IMAP 2276, 2 Plates: 41.74 x 30.33 inches and 41.77 x 30.17 inches, https://doi.org/10.3133/i2276.","productDescription":"2 Plates: 41.74 x 30.33 inches and 41.77 x 30.17 inches","costCenters":[],"links":[{"id":189758,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":260795,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2276/plate-1.pdf"},{"id":260796,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2276/plate-2.pdf"}],"scale":"5000000","otherGeospatial":"Moon","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f49c3","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":534174,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":65820,"text":"i2331 - 1992 - Shaded relief and surface markings maps of the polar regions of Ganymede","interactions":[],"lastModifiedDate":"2012-02-02T00:13:18","indexId":"i2331","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"2331","subseriesTitle":"NONE","title":"Shaded relief and surface markings maps of the polar regions of Ganymede","language":"ENGLISH","doi":"10.3133/i2331","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1992, Shaded relief and surface markings maps of the polar regions of Ganymede: U.S. Geological Survey IMAP 2331, 4 remote-sensing images on 3 sheets ;43 x 55 cm. or smaller, sheets 66 x 81 cm. or smaller, folded in envelope 30 x 24 cm., https://doi.org/10.3133/i2331.","productDescription":"4 remote-sensing images on 3 sheets ;43 x 55 cm. or smaller, sheets 66 x 81 cm. or smaller, folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":189759,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":101172,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2331/plate-1.pdf","size":"4858","linkFileType":{"id":1,"text":"pdf"}},{"id":101173,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2331/plate-2.pdf","size":"7769","linkFileType":{"id":1,"text":"pdf"}},{"id":101174,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2331/plate-3.pdf","size":"7453","linkFileType":{"id":1,"text":"pdf"}}],"scale":"888000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f49c9","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":534175,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":65526,"text":"i2247 - 1992 - Controlled photomosaic of the MTM 10047 Quadrangle, Ganges Chasma region of Mars","interactions":[],"lastModifiedDate":"2012-02-10T00:11:08","indexId":"i2247","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"2247","subseriesTitle":"NONE","title":"Controlled photomosaic of the MTM 10047 Quadrangle, Ganges Chasma region of Mars","language":"ENGLISH","doi":"10.3133/i2247","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1992, Controlled photomosaic of the MTM 10047 Quadrangle, Ganges Chasma region of Mars: U.S. Geological Survey IMAP 2247, 1 remote-sensing image ;61 x 59 cm., on sheet 94 x 66 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i2247.","productDescription":"1 remote-sensing image ;61 x 59 cm., on sheet 94 x 66 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":189156,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":100983,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2247/plate-1.pdf","size":"17044","linkFileType":{"id":1,"text":"pdf"}}],"scale":"502000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 45,-12.5 ], [ 45,-7.5 ], [ 50,-7.5 ], [ 50,-12.5 ], [ 45,-12.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688b1c","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533913,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":64512,"text":"i2090C - 1992 - Map showing bottom topography of the Pacific Continental Margin, Cape Mendocino to Point Conception","interactions":[],"lastModifiedDate":"2012-02-10T00:10:52","indexId":"i2090C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"2090","subseriesTitle":"NONE","chapter":"C","title":"Map showing bottom topography of the Pacific Continental Margin, Cape Mendocino to Point Conception","docAbstract":"All contours, geographic outlines, and political boundaries shown on this map of the bottom topography, or bathymetry, of the Pacific continental margin between 34? and 41? N. latitudes were plotted from digital data bases in the library of the U.S. Geological Survey (USGS)-National Oceanic and Atmospheric Administration (NOAA) Joint Office for Mapping and Research (JOMAR). These digital data were obtained and compiled from many sources; consequently, data quality varies within particular data bases as well as from one data base to another.\nBathymetric contours were digitized from a map compiled by Chase and others (1981) and from the unpublished large scale versions of that map (T.E. Chase, unpub. maps, 1981). Data for the area seaward of the continental slope (~2000 m depth) were obtained primarily from the U.S. Coast and Geodetic Survey (C&GS) 1955 Pacific Exploratory Survey, a systematic and detailed (~8 -nmi trackline spacing) survey between Mexico and Canada. The USGS provided data from cruises S3-78-NC, S15-79-NC, L2-77-NC, Ll0-76-NC, and Bartlett 72. Data were also obtained from Scripps Institution of Oceanography cruises Merazine, Blue Flash, Kayak B, Scan I, and Seven Tow (Chase and Menard, 1971; Chase and others, 1975; Wilde and others, 1976; Wilde and others, 1978). The 200-m contour was derived from the National Ocean Survey charts 1306N-20 (1975), 1307N-l1B (1974a), 1307N-18B (1974b), and C&GS chart 1308N-12 (1969). Sea-floor depths were corrected for sound velocity in sea water using Matthew's (1939) tables.\nOnshore topographic contours were generated by computer from a modified version of 3-arc-second elevation data provided by the Defense Mapping Agency.\nThe United States digital shoreline was obtained from the NOAA, NOS, Nautical Charting Division, National Atlas files. The coastline of Canada was digitized from Canadian Hydrographic Service bathymetric maps. The primary source of names of the sea floor features was the \"Gazetteer of Undersea Features\" (Defense Mapping Agency, 1990).\nAcknowledgments\nChristopher Hines assisted in the construction and verification of the digital data bases. Reviews and suggestions by Edward C. Escowitz and Florence Wong and advice provided by Will Stettner regarding the cartographic design substantially improved the quality of this map.\nReferences Cited\nChase, T.E., and Menard, H.W., 1971, Bathymetric atlas of the northeastern Pacific Ocean: U.S. Naval Oceanographic Office Publication 1303, scale 1:2,000,000 at 33&deg; latitude, 48 p.\nChase, T.E., Wilde, Pat, and Normark, W.R., 1975, Oceanographic data of the Monterey Deep Sea Fan: San Diego, University of California, Institute of Marine Resources Publication TR 58, scale 1:898,524 at 35&deg; latitude.\nChase, T.E., Wilde, Pat, Normark, W.R., Miller, C.P., Seekins, B.A., and Young, J.D., 1981, Offshore topography of the Western United States between 32&deg; and 49&deg; North latitudes: U.S. Geological Survey Open-File Report 81-443, scale 1:864,518 at 38&deg; latitude, 2 sheets.\nCoast and Geodetic Survey, 1969, Point St. George to Point Delgada: Coast and Geodetic Survey Bathymetric Map 1308N-12, scale 1:250,000.\nDefense Mapping Agency, 1990, Gazetteer of undersea features (4th ed.): Washington, D.C., Defense Mapping Agency.\nMatthews, D.J., 1939, Tables of the velocity of sound in pure water and sea water (2d ed.): London, Admiralty, Hydrographic Department, H.D. 282, 52 p.\nNational Ocean Survey, 1974a, Vicinity Pt. Sur to Pt. Reyes: National Ocean Survey Bathymetric Map 1307N-11B, scale 1:250,000.\nNational Ocean Survey, 1974b, Pt. Reyes to Tolo Bank: National Ocean Survey Bathymetric Map 1307N-18B, scale 1:250,000.\nNational Ocean Survey, 1975, Cape San Martin to Point Conception: National Ocean Survey Bathymetric Map 1306N-20, scale 1:250,000.\nWilde, Pat, Normark, W.R., and Chase, T.E., 1976, Oceanographic data off central California 37&deg; to 40&deg; North including the Delgada Deep Sea Fan: Berkeley, University of California, Lawrence Berkeley Laboratory Publication 92, scale 1 :864,581 at 38&deg; latitude.\nWilde, Pat, Chase, T.E., Holmes, M.L., Normark, W.R., Thomas, J.A., McCulloch, D.S., and Kulm, L.D., 1978, Oceanographic data off northern California-southern Oregon 40&deg; to 43&deg; North including the Gorda Deep Sea Fan: Berkeley, University of California, Lawrence Berkeley Laboratory Publication 251, scale 1:815,482 at 42&deg; latitude.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/i2090C","usgsCitation":"Chase, T.E., Wilde, P., Normark, W.R., Evenden, G., Miller, C.P., Seekins, B.A., Young, J.D., Grim, M.S., and Lief, C.J., 1992, Map showing bottom topography of the Pacific Continental Margin, Cape Mendocino to Point Conception: U.S. Geological Survey IMAP 2090, PDF: 52.64 inches x 36.93 inches; 1 map :col. ;78 x 106 cm., on sheet 93 x 133 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i2090C.","productDescription":"PDF: 52.64 inches x 36.93 inches; 1 map :col. ;78 x 106 cm., on sheet 93 x 133 cm., folded in envelope 30 x 24 cm.","additionalOnlineFiles":"Y","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":122454,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/i_2090_C.jpg"},{"id":94399,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/imap/2090/c/","linkFileType":{"id":5,"text":"html"}}],"scale":"1000000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -129,34 ], [ -129,41 ], [ -117,41 ], [ -117,34 ], [ -129,34 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a95e4b07f02db659a64","contributors":{"authors":[{"text":"Chase, T. E.","contributorId":14784,"corporation":false,"usgs":true,"family":"Chase","given":"T.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":271145,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilde, Pat","contributorId":28981,"corporation":false,"usgs":true,"family":"Wilde","given":"Pat","email":"","affiliations":[],"preferred":false,"id":271146,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Normark, W. R.","contributorId":87137,"corporation":false,"usgs":true,"family":"Normark","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":271150,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Evenden, G. I.","contributorId":52960,"corporation":false,"usgs":true,"family":"Evenden","given":"G. I.","affiliations":[],"preferred":false,"id":271148,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Miller, C. P.","contributorId":106855,"corporation":false,"usgs":true,"family":"Miller","given":"C.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":271152,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Seekins, B. A.","contributorId":32130,"corporation":false,"usgs":true,"family":"Seekins","given":"B.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":271147,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Young, J. D.","contributorId":83087,"corporation":false,"usgs":true,"family":"Young","given":"J.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":271149,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Grim, M. S.","contributorId":102884,"corporation":false,"usgs":true,"family":"Grim","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":271151,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Lief, C. J.","contributorId":107784,"corporation":false,"usgs":true,"family":"Lief","given":"C.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":271153,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":65573,"text":"i2262 - 1992 - Controlled photomosaic of the MTM 35102 Quadrangle (revised), Alba Patera region of Mars","interactions":[],"lastModifiedDate":"2012-02-10T00:11:03","indexId":"i2262","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"2262","subseriesTitle":"NONE","title":"Controlled photomosaic of the MTM 35102 Quadrangle (revised), Alba Patera region of Mars","language":"ENGLISH","doi":"10.3133/i2262","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1992, Controlled photomosaic of the MTM 35102 Quadrangle (revised), Alba Patera region of Mars: U.S. Geological Survey IMAP 2262, 1 remote-sensing image ;62 x 52 cm., on sheet 94 x 61 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i2262.","productDescription":"1 remote-sensing image ;62 x 52 cm., on sheet 94 x 61 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":101025,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2262/plate-1.pdf","size":"11698","linkFileType":{"id":1,"text":"pdf"}},{"id":255408,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/2262/report.pdf","size":"25","linkFileType":{"id":1,"text":"pdf"}},{"id":255409,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/2262/report-thumb.jpg"}],"scale":"502000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 100,32.5 ], [ 100,37.5 ], [ 105,37.5 ], [ 105,32.5 ], [ 100,32.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db68830e","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533960,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30225,"text":"wri904041 - 1992 - Potential effects of dredging the South Fork Obion River on ground-water levels near Sidonia, Weakley County, Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:08:54","indexId":"wri904041","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"90-4041","title":"Potential effects of dredging the South Fork Obion River on ground-water levels near Sidonia, Weakley County, Tennessee","docAbstract":"The U.S. Army Corps of Engineers has proposed dredging an approximate 7-mile reach of the South Fork Obion River near Sidonia, Tennessee. This dredging will have an effect on ground-water levels in a wetland area near the river. The river cuts into a sandy aquifer that is confined by an overlying clay layer. Ground water in the confined aquifer flows from a ridge on the north side of the study area toward the river, Estimates of aquifer transmissivity range from 3,300 to 18,800 feet squared per day.\r\n\r\nAssuming a 3-foot decline in stream stage due to dredging, the maximum decline in ground-water levels would be about 2.4 feet at low flow. Ground-water levels in the aquifer would decline by at least 2 feet at a distance of 0.5 mile from the river within 60 days after the change in stream stage, regardless of the assumed transmissivity value. Water-level declines in the upper clay layer probably would be much smaller. The time required for a specified change in ground-water level is dependent on the aquifer properties and distance from the river.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri904041","usgsCitation":"Tucci, P., and Hileman, G.E., 1992, Potential effects of dredging the South Fork Obion River on ground-water levels near Sidonia, Weakley County, Tennessee: U.S. Geological Survey Water-Resources Investigations Report 90-4041, iii, 12 p. :ill. ;28 cm., https://doi.org/10.3133/wri904041.","productDescription":"iii, 12 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":2416,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri904041/","linkFileType":{"id":5,"text":"html"}},{"id":126543,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_90_4041.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c8d1","contributors":{"authors":[{"text":"Tucci, Patrick ptucci@usgs.gov","contributorId":926,"corporation":false,"usgs":true,"family":"Tucci","given":"Patrick","email":"ptucci@usgs.gov","affiliations":[],"preferred":true,"id":202890,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hileman, G. E.","contributorId":11639,"corporation":false,"usgs":true,"family":"Hileman","given":"G.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":202891,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29618,"text":"wri904056 - 1992 - Simulation of the effects of proposed construction of twelfth street extension and of flood-plain reforestation on flood elevations, Congaree River near Columbia, South Carolina","interactions":[],"lastModifiedDate":"2017-01-25T11:49:04","indexId":"wri904056","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"90-4056","title":"Simulation of the effects of proposed construction of twelfth street extension and of flood-plain reforestation on flood elevations, Congaree River near Columbia, South Carolina","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri904056","usgsCitation":"Schuck-Kolben, R.E., and Benedict, S., 1992, Simulation of the effects of proposed construction of twelfth street extension and of flood-plain reforestation on flood elevations, Congaree River near Columbia, South Carolina: U.S. Geological Survey Water-Resources Investigations Report 90-4056, vi, 37 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri904056.","productDescription":"vi, 37 p. :ill., maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":160122,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4056/report-thumb.jpg"},{"id":58441,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4056/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"South Carolina","city":"Columbia","otherGeospatial":"Congaree River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.419677734375,\n              33.44977658311846\n            ],\n            [\n              -81.419677734375,\n              34.379712580462204\n            ],\n            [\n              -80.22216796875,\n              34.379712580462204\n            ],\n            [\n              -80.22216796875,\n              33.44977658311846\n            ],\n            [\n              -81.419677734375,\n              33.44977658311846\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f7e4b07f02db5f1df4","contributors":{"authors":[{"text":"Schuck-Kolben, R. E.","contributorId":14841,"corporation":false,"usgs":true,"family":"Schuck-Kolben","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":201823,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Benedict, S.T.","contributorId":97155,"corporation":false,"usgs":true,"family":"Benedict","given":"S.T.","email":"","affiliations":[],"preferred":false,"id":201824,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30223,"text":"wri924131 - 1992 - Hydrology of Melton Valley at Oak Ridge National Laboratory, Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:08:50","indexId":"wri924131","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-4131","title":"Hydrology of Melton Valley at Oak Ridge National Laboratory, Tennessee","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-file Reports Section [distributor],","doi":"10.3133/wri924131","usgsCitation":"Tucci, P., 1992, Hydrology of Melton Valley at Oak Ridge National Laboratory, Tennessee: U.S. Geological Survey Water-Resources Investigations Report 92-4131, vi, 76 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri924131.","productDescription":"vi, 76 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":119401,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1992/4131/report-thumb.jpg"},{"id":59006,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1992/4131/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604866","contributors":{"authors":[{"text":"Tucci, Patrick ptucci@usgs.gov","contributorId":926,"corporation":false,"usgs":true,"family":"Tucci","given":"Patrick","email":"ptucci@usgs.gov","affiliations":[],"preferred":true,"id":202887,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20353,"text":"ofr9283 - 1992 - Accounting System for Water Use by Vegetation in the Lower Colorado River Valley","interactions":[],"lastModifiedDate":"2012-03-02T17:16:06","indexId":"ofr9283","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-83","title":"Accounting System for Water Use by Vegetation in the Lower Colorado River Valley","docAbstract":"The Colorado River is the principal source of water in the valley of the Colorado River between Hoover Dam and the international boundary with Mexico (fig. 1). Agricultural, domestic, municipal, industrial, hydroelectric-power genera-tion, and recreation are the primary uses of river water in the valley. Most of the consumptive use of water from the river occurs downstream from Davis Dam, where water is diverted to irrigate crops along the river or is exported to interior regions of California and Arizona.\r\n\r\nMost of the agricultural areas are on the alluvium of the flood plain; in a few areas, land on the alluvial terraces has been cultivated. River water is consumed mainly by vegetation (crops and phreatophytes) on the flood plain. Crops were grown on 70.3 percent of the vegetated area classified by using 1984 digital image satellite data. Phreatophytes, natural vege-tation that obtain water from the alluvial aquifer, covered the remaining vegetated areas on the uncultivated flood plain. Most of the water used for irrigation is diverted or pumped from the river. In some areas, water is pumped from wells completed in the alluvial aquifer, which is hydraulically connected to the river.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr9283","usgsCitation":"Owen-Joyce, S.J., 1992, Accounting System for Water Use by Vegetation in the Lower Colorado River Valley: U.S. Geological Survey Open-File Report 92-83, 2 p., https://doi.org/10.3133/ofr9283.","productDescription":"2 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":153094,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0083/report-thumb.jpg"},{"id":49885,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0083/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699c61","contributors":{"authors":[{"text":"Owen-Joyce, Sandra J. 0000-0002-4400-5618 sjowen@usgs.gov","orcid":"https://orcid.org/0000-0002-4400-5618","contributorId":5215,"corporation":false,"usgs":true,"family":"Owen-Joyce","given":"Sandra","email":"sjowen@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":182506,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41746,"text":"ofr9253 - 1992 - Approximate water-level changes in wells completed in the Chicot and Evangeline aquifers, 1991-92 in Fort Bend County and adjacent areas, Texas","interactions":[],"lastModifiedDate":"2021-12-08T21:13:52.057742","indexId":"ofr9253","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-53","title":"Approximate water-level changes in wells completed in the Chicot and Evangeline aquifers, 1991-92 in Fort Bend County and adjacent areas, Texas","docAbstract":"<p>This report was prepared in cooperation with the Fort Bend Subsidence District, and presents data on water-level changes during 1991-92 in the Chicot and Evangeline aquifer (fig. 1-2) in Fort Bend County. &nbsp;Water-level change maps were prepared previously by Locke (1990),and Locke and Barbie (1991), for both aquifers, and by Wesselman (1972) for the Chicot aquifer.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr9253","usgsCitation":"Locke, G.L., and Santos, H.X., 1992, Approximate water-level changes in wells completed in the Chicot and Evangeline aquifers, 1991-92 in Fort Bend County and adjacent areas, Texas: U.S. Geological Survey Open-File Report 92-53, 2 Plates: 29.78 x 26.43 inches and 29.82 x 26.38 inches, https://doi.org/10.3133/ofr9253.","productDescription":"2 Plates: 29.78 x 26.43 inches and 29.82 x 26.38 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":176675,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr9253.PNG"},{"id":392651,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18202.htm"},{"id":79464,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0053/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79463,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0053/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","county":"Fort Bend County","otherGeospatial":"Chicot and Evangeline aquifers","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -96,\n              29.336\n            ],\n            [\n              -95.392,\n              29.336\n            ],\n            [\n              -95.392,\n              29.81\n            ],\n            [\n              -96,\n              29.81\n            ],\n            [\n              -96,\n              29.336\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db67a175","contributors":{"authors":[{"text":"Locke, Glenn L. gllocke@usgs.gov","contributorId":2479,"corporation":false,"usgs":true,"family":"Locke","given":"Glenn","email":"gllocke@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":225467,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Santos, Horatio X.","contributorId":105348,"corporation":false,"usgs":true,"family":"Santos","given":"Horatio","email":"","middleInitial":"X.","affiliations":[],"preferred":false,"id":225468,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":20357,"text":"ofr92137 - 1992 - Earthquake induced water-level fluctuations at Yucca Mountain, Nevada, April 1992","interactions":[],"lastModifiedDate":"2012-02-02T00:07:46","indexId":"ofr92137","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-137","title":"Earthquake induced water-level fluctuations at Yucca Mountain, Nevada, April 1992","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey :\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/ofr92137","usgsCitation":"O’Brien, G.M., 1992, Earthquake induced water-level fluctuations at Yucca Mountain, Nevada, April 1992: U.S. Geological Survey Open-File Report 92-137, iii, 7 p. ill. ;28 cm., https://doi.org/10.3133/ofr92137.","productDescription":"iii, 7 p. ill. ;28 cm.","costCenters":[],"links":[{"id":153116,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0137/report-thumb.jpg"},{"id":49889,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0137/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db6297de","contributors":{"authors":[{"text":"O’Brien, Grady M.","contributorId":71197,"corporation":false,"usgs":true,"family":"O’Brien","given":"Grady","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":182511,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20393,"text":"ofr92175 - 1992 - Compilation of selected data for thermal-water wells and springs in Idaho, 1921 through 1991","interactions":[],"lastModifiedDate":"2012-02-02T00:07:50","indexId":"ofr92175","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-175","title":"Compilation of selected data for thermal-water wells and springs in Idaho, 1921 through 1991","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nU.S. Geological Survey, Books and Open-File Reports Section [distributor],","doi":"10.3133/ofr92175","usgsCitation":"Parliman, D., and Young, H., 1992, Compilation of selected data for thermal-water wells and springs in Idaho, 1921 through 1991: U.S. Geological Survey Open-File Report 92-175, iii, 201 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr92175.","productDescription":"iii, 201 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":153665,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0175/report-thumb.jpg"},{"id":49940,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0175/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a9071","contributors":{"authors":[{"text":"Parliman, D. J.","contributorId":64220,"corporation":false,"usgs":true,"family":"Parliman","given":"D. J.","affiliations":[],"preferred":false,"id":182576,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Young, H.W.","contributorId":68278,"corporation":false,"usgs":true,"family":"Young","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":182577,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29850,"text":"wri924008 - 1992 - Results of ground-water, surface-water, and water-quality monitoring, Black Mesa area, northeastern Arizona; 1989-90","interactions":[],"lastModifiedDate":"2022-09-21T19:19:17.683494","indexId":"wri924008","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-4008","title":"Results of ground-water, surface-water, and water-quality monitoring, Black Mesa area, northeastern Arizona; 1989-90","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri924008","usgsCitation":"Sottilare, J.P., Bills, D.J., and Brown, J.G., 1992, Results of ground-water, surface-water, and water-quality monitoring, Black Mesa area, northeastern Arizona; 1989-90: U.S. Geological Survey Water-Resources Investigations Report 92-4008, iv, 38 p., https://doi.org/10.3133/wri924008.","productDescription":"iv, 38 p.","costCenters":[],"links":[{"id":407161,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47591.htm","linkFileType":{"id":5,"text":"html"}},{"id":160305,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1992/4008/report-thumb.jpg"},{"id":58659,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1992/4008/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona","otherGeospatial":"Black Mesa area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.375,\n              35.75\n            ],\n            [\n              -109.625,\n              35.75\n            ],\n            [\n              -109.625,\n              36.9167\n            ],\n            [\n              -111.375,\n              36.9167\n            ],\n            [\n              -111.375,\n              35.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611afa","contributors":{"authors":[{"text":"Sottilare, J. P.","contributorId":106504,"corporation":false,"usgs":true,"family":"Sottilare","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":202241,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bills, D. J.","contributorId":17610,"corporation":false,"usgs":true,"family":"Bills","given":"D.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":202239,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, J. G.","contributorId":28263,"corporation":false,"usgs":true,"family":"Brown","given":"J.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":202240,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":64534,"text":"i2089A - 1992 - Map showing sediment isopachs in the deep-sea basins of the Pacific continental margin, Point Conception to Point Loma","interactions":[],"lastModifiedDate":"2012-02-10T00:10:58","indexId":"i2089A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"2089","subseriesTitle":"NONE","chapter":"A","title":"Map showing sediment isopachs in the deep-sea basins of the Pacific continental margin, Point Conception to Point Loma","docAbstract":"The U.S. Geological Survey conducted a series of cruises, EEZSCAN 84 (EEZ-SCAN 84 Scientific Staff, 1986), to collect reconnaissance data on the newly proclaimed Exclusive Economic Zone (EEZ), the area out to 200 nautical miles from the coastline of the United States. The cruises systematically surveyed the entire conterminous United States west coast EEZ using the Geological Long-Range Inclined Asdic (GLORIA) side-scan sonar, a 160-in<sup>3</sup> airgun seismic-reflection profiler, a 3.5-kHz high-resolution seismic-reflection profiler, a 10-kHz echo sounder, and a proton-precession magnetometer. The nominal trackline spacing throughout the survey was 30 km.\nDerivative maps of sediment thickness (I-2089-A, I-2090-A, I-2091-A) and depth to basement (I-2089-B, I-2090-B, I-2091-B) in the basins of the west coast EEZ were compiled from both the sonar-image dala and the deep-penetration seismic data obtained on these cruises. Only EEZ-SCAN 84 data were used for the map compilations because available data from other cruises in this region are sparsely located, have poor navigational control, or were obtained with seismic systems that were not powerful enough to resolve oceanic basement. For this map series, sediment thickness and depth to basement were determined only in the deep-ocean basin regions because the seismic system used on the EEZ-SCAN 84 cruises could not resolve oceanic basement beneath the thick sediments of the continental slope. All the data used to compile the maps are presented in the \"Atlas of the Exclusive Economic Zone, Western Conterminous United States\" (EEZ-SCAN 84 Scientific Staff, 1986).\nBasement Outcrops\nGLORIA imagery was used to locate areas of basement outcrop throughout the region. Where possible, sediment thickness on and immediately adjacent to basement outcrops was measured from seismic data. Where there was no bathymetric or seismic control, a seamount peak was assumed to have no sediment cover. A pattern is used on the map to indicate all basement outcrops.\nData Reduction\nAcoustic basement in the basins, invariably oceanic Layer 2, was observed on all of the seismic records. One-way traveltime was measured from the sea floor to acoustic basement. Because the trackline spacing of about 30 km is relatively large compared to the data density along track, we chose to measure the sediment thickness every 0.5 hour or at an interval of approximately 7.5 km. Water depth was measured with a 10-kHz profiler. Depth to basement was calculated using the sea surface as the zero datum and adding the corrected water depth (Carter, 1980) to the sediment thickness. Acoustic travel times were converted to depths by first calculating a regression equation from the interval velocity versus depth data of Connard and others (1984). Their data base comprises a compilation of all available Deep Sea Drilling Project data plus wide-angle refraction data, which were collected in Cascadia Basin west of Oregon and represents the best data set available for the United States west coast EEZ. The regression equation was integrated to determine sediment thickness as a function of one-way traveltime . The resulting equation is\nz = 1400t + 0 .5t<sup>2</sup>\nwhere z is sediment thickness in meters, and t is one-way traveltime in seconds. Sediment thicknesses calculated using this equation were compared to values calculated from the general equation of Carlson and others (1986). Values for sediment thickness calculated by the two equations differed by no greater than 10 percent throughout the range of travel times.\nBathymetry\nThe bathymetry is from Chase and others (1981). The bathymetric data were compiled from a variety of sources, and data quality is inconsistent. Because of differences in navigational precision and density of coverage, the bathymetric contours of a feature may be at a different location than the corresponding isopleths derived from the EEZ-SCAN 84 data, or a feature may not be indicated on the bathymetry at all. These situations occur because either the feature is poorly located in the bathymetric data set or, especially in the outer EEZ, the bathymetric data are too sparse to have defined the existence of a feature.\nAcknowledgments\nTopographic digital data bases were corrected and verified by Christina Lief. Gerald Evenden developed the computer software system MAPGEN, used to compose this map. Reviews, suggestions, and technical contributions from Edward C. Escowitz and Florence Wong and advice about cartographic design from Will Stettner substantially improved the quality of this map.\nReferences Cited\nCarlson, R.L., Gangi, A.F., and Snow, K.R., 1986, Empirical reflection-traveltime/ depth and velocity/depth functions for the deep-sea sediment column: Journal of Geophysical Research, v. 91, no. B8, p. 8249-8266.\nCarter, D.J.T., 1980, Echo-sounding correction tables: Taunton, United Kingdom, Hydrographic Department, Ministry of Defence, 150 p.\nChase, T.E., Wilde, Pat, Normark, W.R, Miller, C.P., Seekins, B.A., and Young, J.D., 1981, Offshore topography of the Western United States between 32&deg; and 49&deg; North latitudes: U.S. Geological Survey Open-File Report 81-443, scale 1:864,518 at 38&deg; latitude, 2 sheets.\nConnard, G., Couch, R., Keeling , K., Roy, J., and Troseth, S., 1984, Abyssal plain and continental net-objective sedimentary thicknesses, in Kulm, L.D., and others, eds., Western North America continental margin and adjacent ocean floor off Oregon and Washington, Atlas 1 of Regional Atlas Series, Ocean Margin Drilling Program: Woods Hole, Mass., Marine Science International, sheet 7.\n\nEEZ-SCAN 84 Scientific Staff, 1986, Atlas of the Exclusive Economic Zone, Western Conterminous United States: U.S. Geological Survey Miscellaneous Investigations Series I-1792, scale 1:500,000, 152 p.\n\nindex map for I-2089-A\nSee Also\n\n\"U.S. Pacific West Coast Field Activities\" (Paskevich and others, 2011; http://pubs.usgs.gov/of/2010/1332/htmldocs/pc/pc_overview.html).\n\nPaskevich, V.F., Wong, F.L., O?Malley, J.J., Stevenson, A.J., and Gutmacher, C.E., 2011, GLORIA sidescan-sonar imagery for parts of the U.S. Exclusive Economic Zone and adjacent areas: U.S. Geological Survey Open-File Report 2010?1332, available at http://pubs.usgs.gov/of/2010/1332/.","language":"ENGLISH","doi":"10.3133/i2089A","usgsCitation":"Gardner, J., Cacchione, D., Drake, D., Edwards, B.D., Field, M., Hampton, M.A., Karl, H.A., Kenyon, N.H., Masson, D., McCulloch, D.S., and Grim, M.S., 1992, Map showing sediment isopachs in the deep-sea basins of the Pacific continental margin, Point Conception to Point Loma: U.S. Geological Survey IMAP 2089, PDF: 47.34 inches x 27.21 inches; 1 map :col. ;56 x 86 cm., on sheet 71 x 119 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i2089A.","productDescription":"PDF: 47.34 inches x 27.21 inches; 1 map :col. ;56 x 86 cm., on sheet 71 x 119 cm., folded in envelope 30 x 24 cm.","additionalOnlineFiles":"Y","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":126714,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/i_2089_a.gif"},{"id":94392,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/imap/2089/a/","linkFileType":{"id":5,"text":"html"}}],"scale":"1000000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -126,30 ], [ -126,35 ], [ -117,35 ], [ -117,30 ], [ -126,30 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a2537","contributors":{"authors":[{"text":"Gardner, J.V.","contributorId":76705,"corporation":false,"usgs":true,"family":"Gardner","given":"J.V.","affiliations":[],"preferred":false,"id":271265,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cacchione, D.A.","contributorId":65448,"corporation":false,"usgs":true,"family":"Cacchione","given":"D.A.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":271264,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Drake, D.E.","contributorId":48150,"corporation":false,"usgs":true,"family":"Drake","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":271263,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Edwards, B. D.","contributorId":27056,"corporation":false,"usgs":true,"family":"Edwards","given":"B.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":271261,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Field, M.E.","contributorId":27052,"corporation":false,"usgs":true,"family":"Field","given":"M.E.","affiliations":[],"preferred":false,"id":271260,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hampton, M. A.","contributorId":103271,"corporation":false,"usgs":true,"family":"Hampton","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":271270,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Karl, Herman A.","contributorId":80649,"corporation":false,"usgs":true,"family":"Karl","given":"Herman","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":271267,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Kenyon, Neil H.","contributorId":89535,"corporation":false,"usgs":false,"family":"Kenyon","given":"Neil","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":271268,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Masson, D.G.","contributorId":44160,"corporation":false,"usgs":true,"family":"Masson","given":"D.G.","email":"","affiliations":[],"preferred":false,"id":271262,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"McCulloch, D. S.","contributorId":78315,"corporation":false,"usgs":true,"family":"McCulloch","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":271266,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Grim, M. S.","contributorId":102884,"corporation":false,"usgs":true,"family":"Grim","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":271269,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}}
,{"id":42004,"text":"ofr9286 - 1992 - Altitude of the water table in the surficial aquifer system, shallow zone, in eastern Palm Beach County, Florida, May 1-5, 1989","interactions":[],"lastModifiedDate":"2022-12-13T21:54:53.248848","indexId":"ofr9286","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-86","title":"Altitude of the water table in the surficial aquifer system, shallow zone, in eastern Palm Beach County, Florida, May 1-5, 1989","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr9286","usgsCitation":"Kane, R.L., 1992, Altitude of the water table in the surficial aquifer system, shallow zone, in eastern Palm Beach County, Florida, May 1-5, 1989: U.S. Geological Survey Open-File Report 92-86, 1 Plate: 18.03 × 27.10 inches, https://doi.org/10.3133/ofr9286.","productDescription":"1 Plate: 18.03 × 27.10 inches","costCenters":[],"links":[{"id":169652,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":410411,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18210.htm","linkFileType":{"id":5,"text":"html"}},{"id":79759,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1992/0086/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","county":"Palm Beach County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -80.43496271623788,\n              26.957535710727228\n            ],\n            [\n              -80.43496271623788,\n              26.28980493099533\n            ],\n            [\n              -79.97551737014285,\n              26.28980493099533\n            ],\n            [\n              -79.97551737014285,\n              26.957535710727228\n            ],\n            [\n              -80.43496271623788,\n              26.957535710727228\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db6869e3","contributors":{"authors":[{"text":"Kane, Richard L. rkane@usgs.gov","contributorId":2034,"corporation":false,"usgs":true,"family":"Kane","given":"Richard","email":"rkane@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":225829,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":65564,"text":"i2261 - 1992 - Controlled photomosaic of the MTM 25182 Quadrangle, Ma'Adim Vallis region of Mars","interactions":[],"lastModifiedDate":"2019-12-23T11:42:58","indexId":"i2261","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"2261","title":"Controlled photomosaic of the MTM 25182 Quadrangle, Ma'Adim Vallis region of Mars","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i2261","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1992, Controlled photomosaic of the MTM 25182 Quadrangle, Ma'Adim Vallis region of Mars: U.S. Geological Survey IMAP 2261, Plate: 26 x 37 inches, https://doi.org/10.3133/i2261.","productDescription":"Plate: 26 x 37 inches","costCenters":[],"links":[{"id":190123,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":101016,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2261/plate-1.pdf","size":"11960","linkFileType":{"id":1,"text":"pdf"}}],"scale":"502000","otherGeospatial":"Mars","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688364","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533951,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20407,"text":"ofr92146 - 1992 - Methods of analysis by the U.S. Geological Survey National Water Quality Laboratory-Determination of the total phosphorus by a Kjeldahl digestion method and an automated colorimetric finish that includes dialysis","interactions":[],"lastModifiedDate":"2021-05-28T18:15:20.780159","indexId":"ofr92146","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-146","title":"Methods of analysis by the U.S. Geological Survey National Water Quality Laboratory-Determination of the total phosphorus by a Kjeldahl digestion method and an automated colorimetric finish that includes dialysis","docAbstract":"A method to determine total phosphorus (TP) in the same digests prepared for total Kjeldahl nitrogen (TKN) determinations is desribed.  The batch, high-temperature (block digester), HG(II)-catalyzed digestion step is similar to U.S. Geological Survey methods I-2552-85/I-4552-85 and U.S. Environmental Protection Agency method 365.4 except that sample and reagent volumes are halved.  Prepared digests are desolvated at 220 degrees Celsius and digested at 370 degrees Celsius in separate block digesters set at these temperatures, rather than in a single, temperature-programmed block digester.  This approach is used in the method escribed here, which permits 40 calibrants, reference waters, and smaples to be digested and resolvated in about an hour.  Orthophosphate ions originally present in samples, along with those released during the digestion step, are determined colorimetrically at a rate of 90 tests per hour by an automated version of the phosphoantimonylmolybdenum blue procedure.  About 100 microliters of digest are required per determination.  The upper concentration limit is 2 milligrams per liter (mg/L) with a method detection limt of 0.01 mg/L.  Repeatability for a sample containing approximately 1.6 mg/L of TP in a high suspended-solids matrix is 0.7 percent.  Between-day precision for the same sample is 5.0 percent.  A dialyzer in the air-segmented continuous flow analyzer provides on-line digest cleanup, eliminated particulates that otherwise would interfere in the colorimetric finish.  An single-channel analyzer can process the resolvated digests from two pairs of block digesters each hour.  Paired t-test analysis of TP concentrations for approximately 1,600 samples determined by the new method (U.S. Geologial Survey methods I-2610-91 and I-4610-91) and the old method (U.S. Geological Survey methods I-2600-85 and I-4600-85) revealed positive bias in the former of 0.02 to 0.04 mg/L for surface-water samples in agreement with previous studies.  Concentrations of total phosphorus detemrined for ground-water samples by both methods were statistically equivalent.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr92146","usgsCitation":"Patton, C.J., and Truitt, E.P., 1992, Methods of analysis by the U.S. Geological Survey National Water Quality Laboratory-Determination of the total phosphorus by a Kjeldahl digestion method and an automated colorimetric finish that includes dialysis: U.S. Geological Survey Open-File Report 92-146, vii, 39 p., https://doi.org/10.3133/ofr92146.","productDescription":"vii, 39 p.","costCenters":[{"id":452,"text":"National Water Quality Laboratory","active":true,"usgs":true}],"links":[{"id":153001,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0146/report-thumb.jpg"},{"id":49947,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0146/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62bc0c","contributors":{"authors":[{"text":"Patton, Charles J. cjpatton@usgs.gov","contributorId":809,"corporation":false,"usgs":true,"family":"Patton","given":"Charles","email":"cjpatton@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":182594,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Truitt, Earl P.","contributorId":65877,"corporation":false,"usgs":true,"family":"Truitt","given":"Earl","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":182595,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29856,"text":"wri924007 - 1992 - Flood of May 19-20, 1990, in the vicinity of Hot Springs, Arkansas","interactions":[],"lastModifiedDate":"2012-02-02T00:08:58","indexId":"wri924007","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-4007","title":"Flood of May 19-20, 1990, in the vicinity of Hot Springs, Arkansas","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri924007","usgsCitation":"Southard, R.E., 1992, Flood of May 19-20, 1990, in the vicinity of Hot Springs, Arkansas: U.S. Geological Survey Water-Resources Investigations Report 92-4007, 1 v. (various pagings) :ill., maps ;28 cm. [PGS - 48 p.], https://doi.org/10.3133/wri924007.","productDescription":"1 v. (various pagings) :ill., maps ;28 cm. [PGS - 48 p.]","costCenters":[],"links":[{"id":119534,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1992/4007/report-thumb.jpg"},{"id":58667,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1992/4007/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eecf7","contributors":{"authors":[{"text":"Southard, R. E.","contributorId":49831,"corporation":false,"usgs":true,"family":"Southard","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":202250,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29857,"text":"wri924126 - 1992 - Scour around bridge piers on streams in Arkansas","interactions":[],"lastModifiedDate":"2012-02-02T00:08:58","indexId":"wri924126","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-4126","title":"Scour around bridge piers on streams in Arkansas","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri924126","usgsCitation":"Southard, R.E., 1992, Scour around bridge piers on streams in Arkansas: U.S. Geological Survey Water-Resources Investigations Report 92-4126, v, 29 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri924126.","productDescription":"v, 29 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":160088,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1992/4126/report-thumb.jpg"},{"id":58668,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1992/4126/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd1ca","contributors":{"authors":[{"text":"Southard, R. E.","contributorId":49831,"corporation":false,"usgs":true,"family":"Southard","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":202251,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29278,"text":"wri924057 - 1992 - Trihalomethane formation potential of Kentucky River water","interactions":[],"lastModifiedDate":"2019-12-28T10:12:15","indexId":"wri924057","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-4057","title":"Trihalomethane formation potential of Kentucky River water","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri924057","usgsCitation":"Rathbun, R.E., White, K.D., and Evaldi, R., 1992, Trihalomethane formation potential of Kentucky River water: U.S. Geological Survey Water-Resources Investigations Report 92-4057, iv, 16 p., https://doi.org/10.3133/wri924057.","productDescription":"iv, 16 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,{"id":29890,"text":"wri914191 - 1992 - Ground-water hydrology and simulation of saltwater encroachment, shallow aquifer system of southern Cape May County, New Jersey","interactions":[],"lastModifiedDate":"2012-02-02T00:08:54","indexId":"wri914191","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"91-4191","title":"Ground-water hydrology and simulation of saltwater encroachment, shallow aquifer system of southern Cape May County, New Jersey","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri914191","usgsCitation":"Spitz, F., and Barringer, T.H., 1992, Ground-water hydrology and simulation of saltwater encroachment, shallow aquifer system of southern Cape May County, New Jersey: U.S. Geological Survey Water-Resources Investigations Report 91-4191, vii, 87 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri914191.","productDescription":"vii, 87 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":119457,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4191/report-thumb.jpg"},{"id":58707,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4191/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668c6b","contributors":{"authors":[{"text":"Spitz, F. J.","contributorId":56682,"corporation":false,"usgs":true,"family":"Spitz","given":"F. J.","affiliations":[],"preferred":false,"id":202308,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barringer, T. H.","contributorId":29468,"corporation":false,"usgs":true,"family":"Barringer","given":"T.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":202307,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":19170,"text":"ofr92116 - 1992 - Ground-water quality of the central Oklahoma (Garber-Wellington) Aquifer conference; proceedings, February 20, 1992","interactions":[],"lastModifiedDate":"2012-02-02T00:07:33","indexId":"ofr92116","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"92-116","title":"Ground-water quality of the central Oklahoma (Garber-Wellington) Aquifer conference; proceedings, February 20, 1992","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/ofr92116","usgsCitation":"Christenson, S.C., and Carpenter, L.K., 1992, Ground-water quality of the central Oklahoma (Garber-Wellington) Aquifer conference; proceedings, February 20, 1992: U.S. Geological Survey Open-File Report 92-116, iv, 24 p. :map ;28 cm., https://doi.org/10.3133/ofr92116.","productDescription":"iv, 24 p. :map ;28 cm.","costCenters":[],"links":[{"id":151417,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0116/report-thumb.jpg"},{"id":48638,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0116/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697863","contributors":{"authors":[{"text":"Christenson, Scott C. schris@usgs.gov","contributorId":980,"corporation":false,"usgs":true,"family":"Christenson","given":"Scott","email":"schris@usgs.gov","middleInitial":"C.","affiliations":[{"id":516,"text":"Oklahoma Water Science Center","active":true,"usgs":true}],"preferred":true,"id":180435,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carpenter, Lyn K.","contributorId":67907,"corporation":false,"usgs":true,"family":"Carpenter","given":"Lyn","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":180436,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4848,"text":"ds4 - 1992 - 1:2,000,000-scale digital line graph (DLG) data","interactions":[],"lastModifiedDate":"2012-02-02T00:05:48","indexId":"ds4","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"4","title":"1:2,000,000-scale digital line graph (DLG) data","language":"ENGLISH","publisher":"Earth Science Information Office,","doi":"10.3133/ds4","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1992, 1:2,000,000-scale digital line graph (DLG) data: U.S. Geological Survey Data Series 4, 1 computer laser optical disc :col. ;4 3/4 in., https://doi.org/10.3133/ds4.","productDescription":"1 computer laser optical disc :col. ;4 3/4 in.","costCenters":[],"links":[{"id":139840,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd491ae4b0b290850eee44","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528388,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27823,"text":"wri914195 - 1992 - Public water-supply systems and water use in Tennessee, 1988","interactions":[],"lastModifiedDate":"2012-02-02T00:08:40","indexId":"wri914195","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"91-4195","title":"Public water-supply systems and water use in Tennessee, 1988","docAbstract":"This report summarizes the results of a study conducted by the U.S. Geological Survey, in cooperation with the Tennessee Department of Environment and Conservation (TDEC), Division of Water Supply in 1988. Data gathered during an inventory by the TDEC were collated to determine water use, supply sources, population served, and design and storage capacities of the systems. The inventory was limited to systems that were active on June 30, 1988. Results of a survey of the systems conducted by the Tennessee Department of Health and Environment during 1988 were a primary source of data for this report. Data from computer and manual files maintained by the Tennessee Department of Health and Environment and the U.S. Geological Survey also were used.\r\n\r\nThe Division of Water Supply, TDEC, surveyed 541 public water-supply systems. These systems served 81 percent of the population of the State, or 3.95 million people. The gross per capita use statewide for public-supplied water was 179 gallons per day. Total water withdrawals for public supply increased about 39 percent from 510 million gallons per day (Mgal/d) in 1980, to 708 Mgalld in 1988. During the same period, the population increased about 7 percent. Surface-water withdrawals accounted for 63 percent (446 Mgal/d) of the total water withdrawn in the State. All of these withdrawals occurred in the Tennessee (56 percent or 249 Mgal/d) and the Ohio (44 percent or 197 Mgalld) hydrologic regions. Ground water supplied 262 Mgal/d or 37 percent of the total water withdrawn by public-supply systems statewide. Of that amount, 79 percent, or 208 Mgalld, was used in western Tennessee.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri914195","usgsCitation":"Hutson, S.S., and Morris, A.J., 1992, Public water-supply systems and water use in Tennessee, 1988: U.S. Geological Survey Water-Resources Investigations Report 91-4195, iii, 74 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri914195.","productDescription":"iii, 74 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":2157,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri914195/","linkFileType":{"id":5,"text":"html"}},{"id":158869,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af3e4b07f02db691b8a","contributors":{"authors":[{"text":"Hutson, Susan S. sshutson@usgs.gov","contributorId":2040,"corporation":false,"usgs":true,"family":"Hutson","given":"Susan","email":"sshutson@usgs.gov","middleInitial":"S.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":198739,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morris, A. Jannine","contributorId":81147,"corporation":false,"usgs":true,"family":"Morris","given":"A.","email":"","middleInitial":"Jannine","affiliations":[],"preferred":false,"id":198740,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38445,"text":"pp1405C - 1992 - Simulation of regional ground-water flow in the Cambrian-Ordovician aquifer system in the northern Midwest, United States: in <i>Regional aquifer-system analysis</i>","interactions":[],"lastModifiedDate":"2015-10-06T09:49:22","indexId":"pp1405C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1992","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":"1405","chapter":"C","title":"Simulation of regional ground-water flow in the Cambrian-Ordovician aquifer system in the northern Midwest, United States: in <i>Regional aquifer-system analysis</i>","docAbstract":"<p>A six-State area in the northern Midwest of the United States has become increasingly dependent on ground water from the Cambrian-Ordovician aquifer system, which consists of a sequence of sandstones, carbonate rocks, and shales. Ground-water withdrawals from the aquifer system began in the late 1800's and increased to approximately 684 million gallons per day (1,058 cubic feet per second) by 1980. This withdrawal has caused more than 900 feet of decline in the potentiometric surface of the aquifer system in parts of the Chicago, Ill., area. Pumping in Minneapolis-St. Paul, Minn., Milwaukee, Wis., and central Iowa has produced a few hundreds of feet of water-level decline.</p>\n<p>A quasi-three-dimensional ground-water flow model was developed to improve understanding of the regional ground-water flow system by simulating the aquifer system under the conditions that existed before and during ground-water development. The Cambrian-Ordovician aquifer system and the overlying rocks were incorporated in the conceptual model as five aquifer layers with four intervening confining layers. The aquifer layers, from top to bottom, are as follows: Quaternary deposits and Cretaceous rocks (aquifer layer 5); basal Devonian carbonate rocks and underlying Silurian carbonate rocks (aquifer layer 4); Middle Ordovician St. Peter Sandstone, Lower Ordovician Prairie du Chien Group, and Upper Cambrian Jordan Sandstone (aquifer layer 3); Upper Cambrian Ironton and Galesville Sandstones (aquifer layer 2); and Upper Cambrian Mount Simon Sandstone and Precambrian Hinckley Sandstone (aquifer layer 1).</p>\n<p>The effects on the flow system of ground water having variable density and the individual aquifer layer contribution of flow to wells open to several aquifer layers were simulated by incorporating appropriate terms in the ground-water flow equation and corresponding modifications in the ground-water flow model.</p>\n<p>Results of steady-state simulations are shown as maps of freshwater head and as flow-rate vectors. A comparison was made of available predevelopment head data and simulated predevelopment heads for the Mount Simon, St. Peter-Prairie du Chien-Jordan, and Silurian-Devonian aquifers. The root mean square of the differences between observed and simulated heads for these aquifers was 53, 36, and 44 feet, respectively.</p>\n<p>Steady-state model simulation indicates that regional recharge areas are located in northwestern Iowa, southeastern Minnesota, much of Wisconsin, northern Illinois, and central Missouri. Regional discharge areas are located near the Mississippi River and its tributaries, the Missouri River, Lake Michigan, and the Illinois basin.</p>\n<p>Results of a transient simulation of the period 1861 to 1980 are shown as maps of freshwater head and freshwater-head decline. The root mean square of the differences between observed and simulated heads for the St. Peter-Prairie du Chien-Jordan aquifer was 63 feet. In addition, hydrographs of simulated hydraulic head were compared with hydrographs of observed head in wells open to various combinations of aquifers. The numerous head measurements within a model node display a wide range in magnitude; however, their historical trend generally follows the trend of the simulated heads.</p>\n<p>The simulated recharge from the glacial drift to the immediately underlying bedrock aquifers averages 0.03, 0.06, 0.24, and 0.02 inch per year, respectively, to the Mount Simon, Ironton-Galesville, St. Peter- Prairie du Chien-Jordan, and Silurian-Devonian aquifers for predevelopment conditions and 0.03, 0.07, 0.45, and 0.07 inch per year, respectively, to the same aquifers for 1976-80. These recharge rates are less than 1.5 percent of average annual precipitation of about 30 inches per year. Most of the recharge from precipitation discharges to streams as base flow through local and intermediate ground-water flow systems. Only a small fraction of the precipitation recharges the deeper, regional flow system. The simulated predevelopment recharge of 571 cubic feet per second is balanced by an equivalent discharge. For the period 1976-80, simulated recharge increased to 1,398 cubic feet per second. Total discharge, including pumpage from the four bedrock aquifers, increased to 1,619 cubic feet per second. The difference in recharge and discharge during this period is from aquifer storage.</p>\n<p>Results of variable-density simulations indicate that the rate of ground-water movement is small in areas where ground water is highly mineralized. The rates and directions are controlled by the intrinsic permeability of the rock, freshwater head gradients, and gravitational force.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Regional aquifer-system analysis","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1405C","usgsCitation":"Mandle, R., and Kontis, A., 1992, Simulation of regional ground-water flow in the Cambrian-Ordovician aquifer system in the northern Midwest, United States: in <i>Regional aquifer-system analysis</i>: U.S. Geological Survey Professional Paper 1405, viii, 97 p., https://doi.org/10.3133/pp1405C.","productDescription":"viii, 97 p.","numberOfPages":"111","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":64920,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1405c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122070,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1405c/report-thumb.jpg"}],"country":"United States","state":"Iowa, Illinois, Indiana, Michigan, Minnesota, Missouri, Wisconsin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -86.044921875,\n              45.9511496866914\n            ],\n            [\n              -88.330078125,\n              46.042735653846506\n            ],\n            [\n              -90.3955078125,\n              46.31658418182218\n            ],\n            [\n              -92.59277343749999,\n              46.34692761055676\n            ],\n            [\n              -93.603515625,\n              46.13417004624326\n            ],\n            [\n              -94.7021484375,\n              45.24395342262324\n            ],\n            [\n              -95.8447265625,\n              43.644025847699496\n            ],\n            [\n              -96.6796875,\n              42.553080288955826\n            ],\n            [\n              -96.7236328125,\n              41.83682786072714\n            ],\n            [\n              -96.328125,\n              40.78054143186031\n            ],\n            [\n              -95.2734375,\n              39.16414104768742\n            ],\n            [\n              -94.8779296875,\n              38.37611542403604\n            ],\n            [\n              -93.8232421875,\n              37.996162679728116\n            ],\n            [\n              -90.7470703125,\n              37.54457732085582\n            ],\n            [\n              -89.69238281249999,\n              37.71859032558816\n            ],\n            [\n              -88.1982421875,\n              38.03078569382294\n            ],\n            [\n              -87.01171875,\n              38.685509760012\n            ],\n            [\n              -85.78125,\n              39.16414104768742\n            ],\n            [\n              -86.4404296875,\n              42.45588764197166\n            ],\n            [\n              -86.8798828125,\n              43.29320031385282\n            ],\n            [\n              -87.099609375,\n              44.15068115978091\n            ],\n            [\n              -86.044921875,\n              45.9511496866914\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648697","contributors":{"authors":[{"text":"Mandle, R.J.","contributorId":27090,"corporation":false,"usgs":true,"family":"Mandle","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":219835,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kontis, A.L.","contributorId":69542,"corporation":false,"usgs":true,"family":"Kontis","given":"A.L.","affiliations":[],"preferred":false,"id":219836,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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