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No abstract available.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrTX902","usgsCitation":"Buckner, H., and Shelby, W., 1991, Water resources data Texas, water year 1990, volume 2. San Jacinto River basin, Brazos River basin, San Bernard River basin, and intervening coastal basins: U.S. Geological Survey Water Data Report TX-90-2, viii, 267 p., https://doi.org/10.3133/wdrTX902.","productDescription":"viii, 267 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":181262,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1990/tx-90-2/report-thumb.jpg"},{"id":381457,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1990/tx-90-2/report.pdf"}],"country":"United States","state":"Texas","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -103.0517578125,\n 35.003003395276714\n ],\n [\n -103.0517578125,\n 34.06176136129718\n ],\n [\n -102.667236328125,\n 33.797408767572485\n ],\n [\n -101.84326171875,\n 33.4955977448657\n ],\n [\n -101.1181640625,\n 33.073130945006625\n ],\n [\n -100.118408203125,\n 32.602361666817515\n ],\n [\n -98.96484375,\n 31.840232667909365\n ],\n [\n -97.767333984375,\n 30.968189296794247\n ],\n [\n -97.14111328125,\n 30.44867367928756\n ],\n [\n -96.52587890625,\n 29.707139348134145\n ],\n [\n -96.21826171874999,\n 29.219302076779456\n ],\n [\n -95.95458984375,\n 28.545925723233477\n ],\n [\n -95.526123046875,\n 28.70986084394286\n ],\n [\n -95.00976562499999,\n 28.8831596093235\n ],\n [\n -94.757080078125,\n 29.248063243796576\n ],\n [\n -94.85595703125,\n 29.649868677972304\n ],\n [\n -95.03173828125,\n 29.983486718474694\n ],\n [\n -95.614013671875,\n 30.80791068136646\n ],\n [\n -96.35009765625,\n 31.5504526754715\n ],\n [\n -97.086181640625,\n 32.045332838858506\n ],\n [\n -98.06396484375,\n 32.861132322810946\n ],\n [\n -99.2724609375,\n 33.65120829920497\n ],\n [\n -100.72265625,\n 34.243594729697406\n ],\n [\n -101.458740234375,\n 34.615126683462194\n ],\n [\n -103.0517578125,\n 35.003003395276714\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5faa5a","contributors":{"authors":[{"text":"Buckner, H.D.","contributorId":49783,"corporation":false,"usgs":true,"family":"Buckner","given":"H.D.","email":"","affiliations":[],"preferred":false,"id":252300,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shelby, W.J.","contributorId":15248,"corporation":false,"usgs":true,"family":"Shelby","given":"W.J.","email":"","affiliations":[],"preferred":false,"id":252299,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":19458,"text":"ofr9166 - 1991 - Regional stratigraphy and subsurface geology of Cenozoic deposits, Gulf Coastal Plain, south-central United States","interactions":[{"subject":{"id":19458,"text":"ofr9166 - 1991 - Regional stratigraphy and subsurface geology of Cenozoic deposits, Gulf Coastal Plain, south-central United States","indexId":"ofr9166","publicationYear":"1991","noYear":false,"title":"Regional stratigraphy and subsurface geology of Cenozoic deposits, Gulf Coastal Plain, south-central United States"},"predicate":"SUPERSEDED_BY","object":{"id":38232,"text":"pp1416G - 1996 - Regional stratigraphy and subsurface geology of Cenozoic deposits, Gulf Coastal Plain, south-central United States","indexId":"pp1416G","publicationYear":"1996","noYear":false,"chapter":"G","title":"Regional stratigraphy and subsurface geology of Cenozoic deposits, Gulf Coastal Plain, south-central United States"},"id":1}],"supersededBy":{"id":38232,"text":"pp1416G - 1996 - Regional stratigraphy and subsurface geology of Cenozoic deposits, Gulf Coastal Plain, south-central United States","indexId":"pp1416G","publicationYear":"1996","noYear":false,"title":"Regional stratigraphy and subsurface geology of Cenozoic deposits, Gulf Coastal Plain, south-central United States"},"lastModifiedDate":"2015-11-02T11:48:46","indexId":"ofr9166","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-66","title":"Regional stratigraphy and subsurface geology of Cenozoic deposits, Gulf Coastal Plain, south-central United States","docAbstract":"

The Gulf Coast Regional Aquifer-System Analysis includes all major aquifer systems in Cenozoic deposits in the Gulf Coastal Plain in the States of Arkansas, Illinois, Kentucky, Louisiana, Mississippi, Missouri, Tennessee, Texas, and small areas in Alabama and Florida (western panhandle area), an area of about 290,000 square miles. The Gulf Coast geosyncline and the Mississippi embayment were the major depocenters for the Tertiary and Quaternary deposits that form the framework for the aquifer systems.

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FoiiDation of the Gulf Coast geosyncline and the Mississippi embayment began with downwarping and downfaulting at the end of the Paleozoic Era. Sedimentation caused the geosyncline to continue to subside throughout Mesozoic and Cenozoic time. During the Late Cretaceous, at the close of the Mesozoic Era, the sea advanced northward and eventually inundated the Mississippi embayment. Marine cycles persisted throughout the Paleocene and Eocene Epochs of the Tertiary Period, as the sea alternately advanced and retreated over the Mississippi embayment. The resulting sediments form a series of dense marine clays separated by terrigenous sands. The Gulf Coast geosyncline remained submerged during marine regressions in the embayment. After withdrawal of the last Tertiary sea from the Mississippi embayment at the end of the Eocene Epoch, deposition continued along the Gulf Coastal Plain under a shifting variety of nonmarine, marine, near-marine, and deltaic environments. Deposition resumed in the Mississippi embayment during the Quaternary with glacially related terraces and aggradation of streams. Fluvial deposition continues.

\n

Structural features in the Gulf Coastal Plain and Mississippi embayment significantly affected Cenozoic deposition. The Desha basin, for example, is a pronounced Tertiary synclinal depocenter in southeastern Arkansas. Three large uplifts are approximately aligned along the latitude of the northern boundary of Louisiana. These are, from west to east, the Sabine, Monroe, and Jackson uplifts. A belt of three major fault zones, the Luling-Mexia-Talco, Arkansas, and Pickens-Gilbertown, generally follows the strike of sediments across the Coastal Plain and more or less forms the northern updip extent of the Gulf Coast geosyncline. An alternating series of gentle synclines and anticlines is oriented perpendicular to the coastline along the Gulf Coast in Texas. Beginning at the southwestern end, these are the Rio Grande embayment, San Marcos arch, Houston embayment, and Sabine arch. The Wiggins anticline is oriented approximately along strike of the sediments in southern Mississippi. Salt domes are numerous in the Gulf Coastal Plain and may penetrate thousands of feet of sediments. Although the degree of salt intrusion can be very great, disruption of adjacent strata is limited to the vicinity of the dome.

\n

The physiography of the Gulf Coastal Plain is a direct result of the nature of the strata at land surface and physical forces that act upon them. Different terrains typify the lithologies that underlie them. The sands and clays that are the predominant rock types each produce characteristic geomorphologic patterns; sands tend to produce ridges, and clays produce topographic lows.

\n

Although Cenozoic deposits are not uniformly differentiated, interstate correlations of major Paleocene and Eocene units are generally established throughout the area. Younger deposits are not as well differentiated. Some stratigraphic designations made at surface exposures cannot be extended into the sub-surface, and the scarcity of distinct geologic horizons has hampered differentiation on a regional scale. The complexities of facies development in Oligocene and younger coastal deposits preclude the development of extensive recognizable horizons needed for stratigraphic applications. Coastal deposits are a heterogeneous assemblage of deltaic, lagoonal, lacustrine, palustrine, eolian, and fluvial clastic facies and local calcareous reef facies. Even major time boundaries, as between geologic series, are not fully resolved. Surficial Quaternary deposits overlie the truncated subcrops of Tertiary strata and generally are distinguishable, although some contacts between Pleistocene and underlying Pliocene deposits have been a ?lstoncal source of controversy. Glacially related terraces are characteristic of the Pleistocene Epoch, and alluvium of aggrading streams typifies the Holocene. 

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An approach was developed to obtain a consistent, regional distribution of herbicide and nitrate data from near-surface aquifers in the corn and soybean producing region of the mid-continent. Near-surface aquifers are defined as those with the top of aquifer material within 50 feet of land surface, regardless of whether the material is saturated or unsaturated. Three hundred wells will be selected for sampling from 12 states. These States include Illinois, Indiana, Iowa, Kansas, Michigan, Minnesota, Missouri, Nebraska, North Dakota, Ohio, South Dakota, and Wisconsin. The reconnaissance data obtained will be used to determine the spatial and seasonal distribution of selected herbicides, two atrazine metabolites, and nitrate in near-surface aquifers in the study region. Hydrologic, geologic, and land-use data will be collected for use in an exploratory statistical analysis to help explain the herbicide distribution.

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R.","contributorId":42190,"corporation":false,"usgs":true,"family":"Burkart","given":"M.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":181353,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":19481,"text":"ofr9155 - 1991 - Ground-water data for Michigan 1989","interactions":[],"lastModifiedDate":"2016-12-29T10:40:13","indexId":"ofr9155","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-55","title":"Ground-water data for Michigan 1989","docAbstract":"

Water levels, locations, depths, and aquifers tapped are given for 108 observation wells. Tabulated data include a listing of ground-water reports in Michigan, extremes of water levels for calendar year 1989 and for the period of record, pumpage of most major ground-water users in the State, and water-quality data from selected wells. In 1989, the two largest municipal users of ground water were Lansing and Kalamazoo. Lansing pumped 7.2 billion gallons from the Saginaw Formation and glacial deposits; Kalamazoo pumped 6.7 billion gallons from glacial deposits only.

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Our map was made by digital image-processing, a technical specialty related to the broader fields of computer graphics and machine vision (Dawson, 1987; Kennie and McLaren, 1988). The technology includes the many spacially based operations first brought together and developed systematically to manipulate Ranger, Mariner, Landsat, and other images that are reassembled from spacecraft telemetry in a raster or scan-line arrangement of square-grid elements (Nathan, 1966; Castleman, 1979; Sheldon, 1987). These computer procedures have been successfully transferred to landform analysis from remote-sensing applications by substituting terrain heights or sea-floor depths for the customary values of electromagnetic radiation obtained from satellites an stored in digital arrays of pixels (Batson and others, 1975).

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1987","interactions":[],"lastModifiedDate":"2012-02-02T00:07:43","indexId":"ofr91212","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-212","title":"Reported water use in Kansas, 1987","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/ofr91212","usgsCitation":"Kenny, J.F., 1991, Reported water use in Kansas, 1987: U.S. Geological Survey Open-File Report 91-212, vi, 39 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr91212.","productDescription":"vi, 39 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":153466,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1991/0212/report-thumb.jpg"},{"id":49098,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1991/0212/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a56e4b07f02db62d638","contributors":{"authors":[{"text":"Kenny, J. F.","contributorId":100378,"corporation":false,"usgs":true,"family":"Kenny","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":181231,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":49488,"text":"ofr91256A - 1991 - Principal facts for 133 gravity stations, with color maps of Bouguer and isostatic residual gravity anomalies on the Winnemucca 1° x 2° quadrangle, Nevada","interactions":[],"lastModifiedDate":"2021-12-23T20:19:22.878103","indexId":"ofr91256A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-256","chapter":"A","title":"Principal facts for 133 gravity stations, with color maps of Bouguer and isostatic residual gravity anomalies on the Winnemucca 1° x 2° quadrangle, Nevada","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr91256A","usgsCitation":"Sikora, R., 1991, Principal facts for 133 gravity stations, with color maps of Bouguer and isostatic residual gravity anomalies on the Winnemucca 1° x 2° quadrangle, Nevada: U.S. Geological Survey Open-File Report 91-256, 40 p., https://doi.org/10.3133/ofr91256A.","productDescription":"40 p.","costCenters":[],"links":[{"id":86082,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1991/0256a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":389438,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18099.htm"},{"id":178517,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1991/0256a/report-thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Winnemucca 1°X 2° quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -118,\n 40\n ],\n [\n -116,\n 40\n ],\n [\n -116,\n 41\n ],\n [\n -118,\n 41\n ],\n [\n -118,\n 40\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668b7a","contributors":{"authors":[{"text":"Sikora, Robert","contributorId":60239,"corporation":false,"usgs":true,"family":"Sikora","given":"Robert","email":"","affiliations":[],"preferred":false,"id":239733,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":39613,"text":"pp1501 - 1991 - The Cenozoic evolution of the San Joaquin Valley, California","interactions":[],"lastModifiedDate":"2012-02-02T00:10:34","indexId":"pp1501","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"1501","title":"The Cenozoic evolution of the San Joaquin Valley, California","docAbstract":"The San Joaquin Valley, which is the southern part of the 700-km-long Great Valley of California, is an asymmetric structural trough that is filled with a prism of upper Mesozoic and Cenozoic sediments up to 9 km thick; these sediments rest on crystalline basement rocks of the southwestward-tilted Sierran block. The San Joaquin sedimentary basin is separated from the Sacramento basin to the north by the buried Stockton arch and associated Stockton fault. The buried Bakersfield arch near the south end of the valley separates the small Maricopa-Tejon subbasin at the south end of the San Joaquin basin from the remainder of the basin. Cenozoic strata in the San Joaquin basin thicken southeastward from about 800 m in the north to over 9,000 m in the south. \r\n\r\nThe San Joaquin Valley can be subdivided into five regions on the basis of differing structural style. They are the northern Sierran block, the southern Sierran block, the northern Diablo homocline, the westside fold belt, and the combined Maricopa-Tejon subbasin and southmargin deformed belt. Considerable facies variation existed within the sedimentary basin, particularly in the Neogene when a thick section of marine sediment accumulated in the southern part of the basin, while a relatively thin and entirely nonmarine section was deposited in the northern part. The northern Sierran block, the stable east limb of the valley syncline between the Stockton fault and the San Joaquin River, is the least deformed region of the valley. Deformation consists mostly of a southwest tilt and only minor late Cenozoic normal faulting. The southern Sierran block, the stable east limb of the valley syncline between the San Joaquin River and the Bakersfield arch, is similar in style to the northern part of the block, but it has a higher degree of deformation. Miocene or older normal faults trend mostly north to northwest and have a net down-to-the-west displacement with individual offsets of as much as 600 m. The northern Diablo homocline, the western limb of the valley syncline between the Stockton arch and Panoche Creek, consists of a locally faulted homocline with northeast dips. Deformation is mostly late Cenozoic, is complex in its history, and has included up-to-the-southwest reverse faulting. The west-side fold belt, the southwestern part of the valley syncline between Panoche Creek and Elk Hills and including the southern Diablo and Temblor Ranges, is characterized by a series of folds and faults trending slightly oblique to the San Andreas fault. Paleogene folding took place in the northern part of the belt; however, most folding took place in Neogene time, during which the intensity of deformation increased southeastward along the belt and southwestward toward the San Andreas fault. The Maricopa-Tejon subbasin and the south-margin deformed belt are structurally distinct, but genetically related, regions bounded by the Bakersfield arch on the north, the San Emigdio Mountains on the south, the Tehachapi Mountains on the east, and the southeast end of the fold belt on the west. This combined region, which is the most deformed part of the basin, has undergone significant late Cenozoic shortening through north-directed thrust faulting at the south margin, as well as extreme Neogene basin subsidence north of the thrust belt. \r\n\r\nThe sedimentary history of the San Joaquin basin, recorded in terms of unconformity-bounded depositional sequences, has been controlled principally by tectonism, but it has also been controlled by eustatic sea-level changes and, to a lesser degree, by climate. Plate tectonic events that had an influence on the basin include (1) subduction during the early Tertiary that changed from oblique to normal convergence in the later part of the Eocene, (2) the mid-Oligocene encounter of the Pacific-Farallon spreading ridge with the trench, and the consequent establishment of the San Andreas transform, (3) the northwestward migration of the Mendocino triple junction that in","language":"ENGLISH","doi":"10.3133/pp1501","usgsCitation":"Bartow, J.A., 1991, The Cenozoic evolution of the San Joaquin Valley, California: U.S. Geological Survey Professional Paper 1501, 40 p.; 2 plates in pocket, https://doi.org/10.3133/pp1501.","productDescription":"40 p.; 2 plates in pocket","costCenters":[],"links":[{"id":104667,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4910.htm","linkFileType":{"id":5,"text":"html"},"description":"4910"},{"id":122041,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1501/report-thumb.jpg"},{"id":67207,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1501/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":67208,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1501/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":67209,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1501/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad2e4b07f02db681b73","contributors":{"authors":[{"text":"Bartow, J. Alan","contributorId":84373,"corporation":false,"usgs":true,"family":"Bartow","given":"J.","email":"","middleInitial":"Alan","affiliations":[],"preferred":false,"id":221807,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":66800,"text":"i2011 - 1991 - Stratigraphic cross section showing upper Paleocene coal-bearing rocks of the Tongue River member of the Fort Union Formation in the Piney Canyon NE and Piney Canyon NW quadrangles, Campbell and Weston counties, southeastern Powder River basin, Wyoming","interactions":[],"lastModifiedDate":"2012-02-10T00:11:15","indexId":"i2011","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":"2011","subseriesTitle":"NONE","title":"Stratigraphic cross section showing upper Paleocene coal-bearing rocks of the Tongue River member of the Fort Union Formation in the Piney Canyon NE and Piney Canyon NW quadrangles, Campbell and Weston counties, southeastern Powder River basin, Wyoming","language":"ENGLISH","doi":"10.3133/i2011","isbn":"0607791713","usgsCitation":"Pierce, F.W., and Johnson, E.A., 1991, Stratigraphic cross section showing upper Paleocene coal-bearing rocks of the Tongue River member of the Fort Union Formation in the Piney Canyon NE and Piney Canyon NW quadrangles, Campbell and Weston counties, southeastern Powder River basin, Wyoming: U.S. Geological Survey IMAP 2011, 1 section ;sheet 81 x 109 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i2011.","productDescription":"1 section ;sheet 81 x 109 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":256074,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2011/plate-1.pdf","size":"10543","linkFileType":{"id":1,"text":"pdf"}},{"id":256075,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/2011/report.pdf","size":"32","linkFileType":{"id":1,"text":"pdf"}},{"id":256076,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/2011/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.11749999999999,43.666666666666664 ], [ -105.11749999999999,43.700833333333335 ], [ -105.08333333333333,43.700833333333335 ], [ -105.08333333333333,43.666666666666664 ], [ -105.11749999999999,43.666666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6af790","contributors":{"authors":[{"text":"Pierce, F. W.","contributorId":55085,"corporation":false,"usgs":true,"family":"Pierce","given":"F.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":275103,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, E. A.","contributorId":87893,"corporation":false,"usgs":true,"family":"Johnson","given":"E.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":275104,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":66940,"text":"i2226 - 1991 - Correlation and depositional analysis of oil shale and associated rocks in the Eocene Green River Formation, greater Green River basin, southwest Wyoming","interactions":[],"lastModifiedDate":"2019-12-23T11:32:13","indexId":"i2226","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":"2226","title":"Correlation and depositional analysis of oil shale and associated rocks in the Eocene Green River Formation, greater Green River basin, southwest Wyoming","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i2226","usgsCitation":"Roehler, H.W., 1991, Correlation and depositional analysis of oil shale and associated rocks in the Eocene Green River Formation, greater Green River basin, southwest Wyoming: U.S. Geological Survey IMAP 2226, 2 Sheets: 52.42 x 42.14 inches and 45.86 x 42.47 inches, https://doi.org/10.3133/i2226.","productDescription":"2 Sheets: 52.42 x 42.14 inches and 45.86 x 42.47 inches","costCenters":[],"links":[{"id":107347,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10195.htm","linkFileType":{"id":5,"text":"html"},"description":"10195"},{"id":190446,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"62500","country":"United States","state":"Wyoming","otherGeospatial":"Green River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.0333251953125,\n 41.000629848685385\n ],\n [\n -108.270263671875,\n 41.000629848685385\n ],\n [\n -108.270263671875,\n 42.92827401776912\n ],\n [\n -111.0333251953125,\n 42.92827401776912\n ],\n [\n -111.0333251953125,\n 41.000629848685385\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db684763","contributors":{"authors":[{"text":"Roehler, H. W.","contributorId":16072,"corporation":false,"usgs":true,"family":"Roehler","given":"H.","middleInitial":"W.","affiliations":[],"preferred":false,"id":275339,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":19491,"text":"ofr90709 - 1991 - Assessment of hydrogeologic conditions with emphasis on water quality and wastewater injection, Southwest Sarasota and West Charlotte counties, Florida","interactions":[{"subject":{"id":19491,"text":"ofr90709 - 1991 - Assessment of hydrogeologic conditions with emphasis on water quality and wastewater injection, Southwest Sarasota and West Charlotte counties, Florida","indexId":"ofr90709","publicationYear":"1991","noYear":false,"title":"Assessment of hydrogeologic conditions with emphasis on water quality and wastewater injection, Southwest Sarasota and West Charlotte counties, Florida"},"predicate":"SUPERSEDED_BY","object":{"id":1955,"text":"wsp2371 - 1992 - Assessment of hydrogeologic conditions with emphasis on water quality and wastewater injection, southwest Sarasota and West Charlotte counties, Florida","indexId":"wsp2371","publicationYear":"1992","noYear":false,"title":"Assessment of hydrogeologic conditions with emphasis on water quality and wastewater injection, southwest Sarasota and West Charlotte counties, Florida"},"id":1}],"supersededBy":{"id":1955,"text":"wsp2371 - 1992 - Assessment of hydrogeologic conditions with emphasis on water quality and wastewater injection, southwest Sarasota and West Charlotte counties, Florida","indexId":"wsp2371","publicationYear":"1992","noYear":false,"title":"Assessment of hydrogeologic conditions with emphasis on water quality and wastewater injection, southwest Sarasota and West Charlotte counties, Florida"},"lastModifiedDate":"2020-01-02T06:41:42","indexId":"ofr90709","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"90-709","title":"Assessment of hydrogeologic conditions with emphasis on water quality and wastewater injection, Southwest Sarasota and West Charlotte counties, Florida","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr90709","usgsCitation":"Hutchinson, C.B., 1991, Assessment of hydrogeologic conditions with emphasis on water quality and wastewater injection, Southwest Sarasota and West Charlotte counties, Florida: U.S. Geological Survey Open-File Report 90-709, vi, 103 p., https://doi.org/10.3133/ofr90709.","productDescription":"vi, 103 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":151906,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Florida","county":"Sarasota County, West Charlotte County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -82.7490234375,\n 27.508271413876017\n ],\n [\n -82.353515625,\n 26.765230565697482\n ],\n [\n -81.990966796875,\n 26.765230565697482\n ],\n [\n -81.990966796875,\n 27.6251403350933\n ],\n [\n -82.353515625,\n 27.6251403350933\n ],\n [\n -82.7490234375,\n 27.508271413876017\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db671f7c","contributors":{"authors":[{"text":"Hutchinson, C. B.","contributorId":94655,"corporation":false,"usgs":true,"family":"Hutchinson","given":"C.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":180999,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":40280,"text":"ofr91554 - 1991 - Complete Bouguer gravity anomaly and isostatic residual gravity maps of the Bakersfield 1° x 2° quadrangle, California","interactions":[],"lastModifiedDate":"2021-11-19T20:11:07.241918","indexId":"ofr91554","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-554","title":"Complete Bouguer gravity anomaly and isostatic residual gravity maps of the Bakersfield 1° x 2° quadrangle, California","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr91554","usgsCitation":"Langenheim, V., and Plescia, J.B., 1991, Complete Bouguer gravity anomaly and isostatic residual gravity maps of the Bakersfield 1° x 2° quadrangle, California: U.S. Geological Survey Open-File Report 91-554, 2 Plates: 40.83 × 27.26 inches and 40.24 × 26.83 inches, https://doi.org/10.3133/ofr91554.","productDescription":"2 Plates: 40.83 × 27.26 inches and 40.24 × 26.83 inches","costCenters":[],"links":[{"id":172949,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":391944,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18160.htm"},{"id":71862,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1991/0554/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":71861,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1991/0554/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Bakersfield 1° x 2° quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120,\n 36\n ],\n [\n -118,\n 36\n ],\n [\n -118,\n 35\n ],\n [\n -120,\n 35\n ],\n [\n -120,\n 36\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8a6f","contributors":{"authors":[{"text":"Langenheim, Victoria E. 0000-0003-2170-5213 zulanger@usgs.gov","orcid":"https://orcid.org/0000-0003-2170-5213","contributorId":1526,"corporation":false,"usgs":true,"family":"Langenheim","given":"Victoria E.","email":"zulanger@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":223216,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Plescia, Jeffrey B.","contributorId":48995,"corporation":false,"usgs":true,"family":"Plescia","given":"Jeffrey","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":223217,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":19615,"text":"ofr91280 - 1991 - The Putnam thrust; northern Portneuf Range, southeastern Idaho: Structural complexities caused by upper-plate Imbricate thrusting and Neogene block rotation","interactions":[],"lastModifiedDate":"2024-12-18T23:00:26.226513","indexId":"ofr91280","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-280","title":"The Putnam thrust; northern Portneuf Range, southeastern Idaho: Structural complexities caused by upper-plate Imbricate thrusting and Neogene block rotation","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr91280","usgsCitation":"Kellogg, K., 1991, The Putnam thrust; northern Portneuf Range, southeastern Idaho: Structural complexities caused by upper-plate Imbricate thrusting and Neogene block rotation: U.S. Geological Survey Open-File Report 91-280, 37 p., https://doi.org/10.3133/ofr91280.","productDescription":"37 p.","costCenters":[],"links":[{"id":152589,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1991/0280/report-thumb.jpg"},{"id":49084,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1991/0280/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":390301,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18107.htm","text":"northern Portneuf Range","linkFileType":{"id":5,"text":"html"}},{"id":465305,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18108.htm","text":"western part of northern Portneuf Range, Pocatello Range, and northern Bannock Range","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Idaho","otherGeospatial":"northern Portneuf Range","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -112.551,\n 42.75\n ],\n [\n -111.938,\n 42.75\n ],\n [\n -111.938,\n 43.29\n ],\n [\n -112.551,\n 43.29\n ],\n [\n -112.551,\n 42.75\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67ad1c","contributors":{"authors":[{"text":"Kellogg, K.S.","contributorId":99145,"corporation":false,"usgs":true,"family":"Kellogg","given":"K.S.","email":"","affiliations":[],"preferred":false,"id":181219,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":66525,"text":"i1959E - 1991 - Cross section showing the reconstructed stratigraphic framework of Paleocene rocks and coal beds in the central Powder River basin from Decker to Bear Skull Mountain, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:13:24","indexId":"i1959E","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":"1959","subseriesTitle":"NONE","chapter":"E","title":"Cross section showing the reconstructed stratigraphic framework of Paleocene rocks and coal beds in the central Powder River basin from Decker to Bear Skull Mountain, Montana","language":"ENGLISH","doi":"10.3133/i1959E","usgsCitation":"McLellan, M., 1991, Cross section showing the reconstructed stratigraphic framework of Paleocene rocks and coal beds in the central Powder River basin from Decker to Bear Skull Mountain, Montana: U.S. Geological Survey IMAP 1959, 1 section :col. ;sheet 61 x 72 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1959E.","productDescription":"1 section :col. ;sheet 61 x 72 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":107217,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10039.htm","linkFileType":{"id":5,"text":"html"},"description":"10039"},{"id":189690,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad0e4b07f02db680b74","contributors":{"authors":[{"text":"McLellan, M.W.","contributorId":38643,"corporation":false,"usgs":true,"family":"McLellan","given":"M.W.","email":"","affiliations":[],"preferred":false,"id":274656,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":20148,"text":"ofr91456 - 1991 - Water-quality data for Sauk Lake and tributaries near Sauk Centre, Minnesota, 1988-89","interactions":[],"lastModifiedDate":"2018-03-19T10:24:03","indexId":"ofr91456","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-456","title":"Water-quality data for Sauk Lake and tributaries near Sauk Centre, Minnesota, 1988-89","docAbstract":"

The U.S. Army Corps of Engineers is planning to reduce aquatic growth and siltation in Sauk Lake in west-central Minnesota in order to improve recreation. A detailed water-quality survey of the lake and surrounding watershed was needed to plan remedial activities.

\n

Water-quality data were collected at 11 sites on Sauk Lake, at sites on 3 major tributaries to the lake, and at the outflow from the lake from September 1988 through August 1989. Data collected from five selected lake sites comprise alkalinity, dissolved-solids concentration, concentrations of nutrients, plankton counts, and chlorophyll a and b. Vertical profiles of specific conductance, pH, temperature, and dissolved oxygen, as well as transparency depths were measured at all lake sites. Discharge, specific conductance, pH, temperature, and dissolved oxygen were measured at the stream sites. Water samples were collected to determine alkalinity and concentrations of suspended solids and nutrients.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/ofr91456","collaboration":"Prepared in cooperation with the U.S. Army Corps of Engineers","usgsCitation":"Mitton, G.B., 1991, Water-quality data for Sauk Lake and tributaries near Sauk Centre, Minnesota, 1988-89: U.S. Geological Survey Open-File Report 91-456, iv, 57 p, https://doi.org/10.3133/ofr91456.","productDescription":"iv, 57 p","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":49688,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1991/0456/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":152831,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1991/0456/report-thumb.jpg"}],"country":"United States","state":"Minnesota","city":"Sauk Centre","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -95.0042724609375,\n 45.69802700880466\n ],\n [\n -95.0042724609375,\n 45.874234183868346\n ],\n [\n -94.87380981445312,\n 45.874234183868346\n ],\n [\n -94.87380981445312,\n 45.69802700880466\n ],\n [\n -95.0042724609375,\n 45.69802700880466\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e59aa","contributors":{"authors":[{"text":"Mitton, Gregory B.","contributorId":76769,"corporation":false,"usgs":true,"family":"Mitton","given":"Gregory","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":182149,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":54412,"text":"wdrCA901 - 1991 - Water Resources Data, California, Water Year 1990. Volume 1. Southern Great Basin from Mexican Border to Mono Lake Basin; and Pacific Slope Basins from Tijuana River to Santa Maria River","interactions":[],"lastModifiedDate":"2012-09-01T01:01:51","indexId":"wdrCA901","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":"CA-90-1","title":"Water Resources Data, California, Water Year 1990. Volume 1. Southern Great Basin from Mexican Border to Mono Lake Basin; and Pacific Slope Basins from Tijuana River to Santa Maria River","docAbstract":"Water resources data for the 1990 water year for California consist of records of stage, discharge, and water quality of streams; stage and contents in lakes and reservoirs; and water levels and water quality in wells. Volume 1 contains discharge records for 157 streamflow-gaging stations, 16 crest-stage partial-record streamflow stations, and 2miscellaneous measurement stations; stage and contents records for 16 lakes and reservoirs; water-quality records for 19 streamflow-gaging stations, 2 partial-record stations; and precipitation records for 13 stations. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in California.","language":"English","publisher":"U.S. Geological Survey, Water Resources Division","publisherLocation":"Sacramento, CA","doi":"10.3133/wdrCA901","collaboration":"Prepared in cooperation with the California Department of 'vater Resources and with other agencies","usgsCitation":"Bowers, J.C., Jensen, R., and Hoffman, E., 1991, Water Resources Data, California, Water Year 1990. Volume 1. Southern Great Basin from Mexican Border to Mono Lake Basin; and Pacific Slope Basins from Tijuana River to Santa Maria River (Legacy Report): U.S. Geological Survey Water Data Report CA-90-1, xi, 300 p., https://doi.org/10.3133/wdrCA901.","productDescription":"xi, 300 p.","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":181924,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wdr_CA_90_1.jpg"},{"id":260081,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1990/ca-90/WDR-1990-vol1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.75,32.5 ], [ -120.75,38.166666666666664 ], [ -114.13333333333334,38.166666666666664 ], [ -114.13333333333334,32.5 ], [ -120.75,32.5 ] ] ] } } ] }","edition":"Legacy Report","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fc04d","contributors":{"authors":[{"text":"Bowers, J. C.","contributorId":57106,"corporation":false,"usgs":true,"family":"Bowers","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":250277,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jensen, R.M.","contributorId":39053,"corporation":false,"usgs":true,"family":"Jensen","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":250275,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hoffman, E.B.","contributorId":47379,"corporation":false,"usgs":true,"family":"Hoffman","given":"E.B.","email":"","affiliations":[],"preferred":false,"id":250276,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":20145,"text":"ofr91482 - 1991 - Documentation of model input and output values for the geohydrology and ground-water-flow simulation of the Surprise Spring basin aquifer system, San Bernardino County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:07:44","indexId":"ofr91482","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-482","title":"Documentation of model input and output values for the geohydrology and ground-water-flow simulation of the Surprise Spring basin aquifer system, San Bernardino County, California","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/ofr91482","usgsCitation":"Mitten, H., and Londquist, C., 1991, Documentation of model input and output values for the geohydrology and ground-water-flow simulation of the Surprise Spring basin aquifer system, San Bernardino County, California: U.S. Geological Survey Open-File Report 91-482, iii, 5 p. ;28 cm. +1 computer disk (5 1/4 in.), https://doi.org/10.3133/ofr91482.","productDescription":"iii, 5 p. ;28 cm. +1 computer disk (5 1/4 in.)","costCenters":[],"links":[{"id":152828,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1991/0482/report-thumb.jpg"},{"id":49685,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1991/0482/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db636198","contributors":{"authors":[{"text":"Mitten, H. 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