{"pageNumber":"5354","pageRowStart":"133825","pageSize":"25","recordCount":184769,"records":[{"id":4301,"text":"cir861 - 1982 - Geological studies of the COST nos. G-1 and G-2 wells, United States North Atlantic outer continental shelf","interactions":[],"lastModifiedDate":"2018-10-23T17:49:36","indexId":"cir861","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"861","title":"Geological studies of the COST nos. G-1 and G-2 wells, United States North Atlantic outer continental shelf","docAbstract":"The COST Nos. G-1 and G-2 wells (fig. 1) are the second and third deep stratigraphic test wells drilled in the North Atlantic Outer Continental Shelf of the United States. COST No. G-1 was drilled in the Georges Bank basin to a total depth of 16,071 ft (4,898 m). G-1 bottomed in phyllite, slate, and metaquartzite overlain by weakly metamorphosed dolomite, all of Cambrian age. From approximately 15,600 to 12,400 ft (4,755 to 3,780 m) the strata are Upper Triassic(?), Lower Jurassic(?), and Middle Jurassic, predominantly red shales, sandstones, and conglomerates. Thin, gray Middle Jurassic beds of shale, sandstone, limestone, and dolomite occur from 12,400 to 9,900 ft (3,780 to 3,018 m). From 9,900 to 1,030 ft (3,018 to 314 m) are coarse-grained unconsolidated sands and loosely cemented sandstones, with beds of gray shale, lignite, and coal. The microfossils indicate the rocks are Upper Jurassic from 10,100 ft (3,078 m) up to 5,400 ft (1,646 m) and Cretaceous from that depth to 1,030 ft (314 m). No younger or shallower rocks were recovered in the drilling at the COST No. G-1 site, but an Eocene limestone is inferred to be disconformable over Santonian strata. The Jurassic strata of the COST No. G-1 well were deposited in shallow marine, marginal marine, and nonmarine environments, which changed to a dominantly shallow marine but still nearshore environment in the Cretaceous. \r\n\r\nThe COST No. G-2 well was drilled 42 statute miles {68 km) east of the G-1 site, still within the Georges Bank basin, to a depth of 21,874 ft (6,667 m). The bottom 40 ft (12 m) of salt and anhydrite is overlain by approximately 7,000 ft {2,134 m) of Upper Triassic{?), Lower Jurassic{?) and Middle Jurassic dolomite, limestone, and interbedded anhydrite from 21,830 to 13,615 ft (6,654 to 4,153 m). From 13,500 to 9,700 ft (4,115 to 2,957 m) are Middle Jurassic limestones with interbedded sandstone. From 9,700 to 4,000 ft (2,957 to 1,219 m) are Upper Jurassic and Cretaceous interbedded sandstones and limestones overlain by Upper Cretaceous unconsolidated sands, sandstones, and calcareous shales. Pliocene, Miocene, Eocene, and Paleocene strata are disconformable over Santonian rocks; uppermost Cretaceous rocks are missing at this site, as at G-1. The sedimentary rocks in the COST No. G-2 well were deposited in somewhat deeper water, farther away from sources of terrigenous material than those at G-l, but still in marginal marine to shallow marine environments. \r\n\r\nData from geophysical logs and examination of conventional cores, wellcuttings, and sidewall cores show that below 10,000 ft {3,048 m), the strata in both wells have moderate porosities {< 20 percent) and low to moderate permeabilities {< 100 mD) and are thus considered adequate to poor reservoir rocks. Above 10,000 ft (3,000 m) the porosities range from 16 to 39 percent, and the permeabilities are highly variable, ranging from 0.01 to 7,100 mD. \r\n\r\nMeasurements of vitrinite reflectance, color alteration of visible organic matter, and various organic geochemical properties suggest that the Tertiary and Cretaceous strata of the COST Nos. G-1 and G-2 are not prospective for oil and gas. These sediments have not been buried deeply enough for hydrocarbon generation, and the kerogen and extractable organic matter in them are thermally immature. However, the Jurassic rocks at the G-1 site do contain small amounts of thermally mature gas-prone kerogens. The Jurassic rocks at COST No. G-2 are also gas-prone and are slightly richer in organic carbon and total extractable hydrocarbons than the G-1 rocks, but both sites have only poor to fair oil and gas source-rock potential.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir861","usgsCitation":"Wenkam, C.R., 1982, Geological studies of the COST nos. G-1 and G-2 wells, United States North Atlantic outer continental shelf: U.S. Geological Survey Circular 861, vi, 193 p. :ill., maps ;26 cm., https://doi.org/10.3133/cir861.","productDescription":"vi, 193 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":31412,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1982/0861/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124681,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1982/0861/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db687461","contributors":{"editors":[{"text":"Scholle, Peter A.","contributorId":60194,"corporation":false,"usgs":true,"family":"Scholle","given":"Peter A.","affiliations":[],"preferred":false,"id":749517,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Wenkam, Chiye R.","contributorId":105286,"corporation":false,"usgs":true,"family":"Wenkam","given":"Chiye","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":148769,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10700,"text":"ofr82815 - 1982 - Test of airborne radar for mapping two types of land cover; forested wetland and perennial snow and ice","interactions":[],"lastModifiedDate":"2012-02-02T00:06:24","indexId":"ofr82815","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-815","title":"Test of airborne radar for mapping two types of land cover; forested wetland and perennial snow and ice","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82815","usgsCitation":"Place, J.L., 1982, Test of airborne radar for mapping two types of land cover; forested wetland and perennial snow and ice: U.S. Geological Survey Open-File Report 82-815, 15 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82815.","productDescription":"15 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":143330,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0815/report-thumb.jpg"},{"id":38519,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0815/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684bfe","contributors":{"authors":[{"text":"Place, John L.","contributorId":83145,"corporation":false,"usgs":true,"family":"Place","given":"John","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":161821,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7302,"text":"ofr82974 - 1982 - Marine geological investigations in the Beaufort Sea in 1981 and preliminary interpretations for regions from the Canning River to the Canadian border","interactions":[],"lastModifiedDate":"2012-02-02T00:06:08","indexId":"ofr82974","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-974","title":"Marine geological investigations in the Beaufort Sea in 1981 and preliminary interpretations for regions from the Canning River to the Canadian border","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82974","usgsCitation":"Reimnitz, E., Barnes, P.W., Rearic, D., Minkler, P., Kempema, E., and Reiss, T.E., 1982, Marine geological investigations in the Beaufort Sea in 1981 and preliminary interpretations for regions from the Canning River to the Canadian border: U.S. Geological Survey Open-File Report 82-974, 67 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82974.","productDescription":"67 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":141472,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0974/report-thumb.jpg"},{"id":34693,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0974/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606b83","contributors":{"authors":[{"text":"Reimnitz, Erk","contributorId":17963,"corporation":false,"usgs":true,"family":"Reimnitz","given":"Erk","email":"","affiliations":[],"preferred":false,"id":155135,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barnes, P. W.","contributorId":8819,"corporation":false,"usgs":true,"family":"Barnes","given":"P.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":155134,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rearic, D.M.","contributorId":65463,"corporation":false,"usgs":true,"family":"Rearic","given":"D.M.","affiliations":[],"preferred":false,"id":155137,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Minkler, P.W.","contributorId":87933,"corporation":false,"usgs":true,"family":"Minkler","given":"P.W.","affiliations":[],"preferred":false,"id":155138,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kempema, E. W.","contributorId":105314,"corporation":false,"usgs":false,"family":"Kempema","given":"E. W.","affiliations":[],"preferred":false,"id":155139,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Reiss, T. E.","contributorId":36940,"corporation":false,"usgs":true,"family":"Reiss","given":"T.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":155136,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":2714,"text":"wsp2190 - 1982 - A study of trends in total phosphorus measurements at NASQAN stations","interactions":[],"lastModifiedDate":"2012-02-02T00:05:34","indexId":"wsp2190","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2190","title":"A study of trends in total phosphorus measurements at NASQAN stations","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2190","usgsCitation":"Smith, R.A., Hirsch, R.M., and Slack, J.R., 1982, A study of trends in total phosphorus measurements at NASQAN stations: U.S. Geological Survey Water Supply Paper 2190, iv, 34 p. **Missing p. 24-25 and 28-29**, https://doi.org/10.3133/wsp2190.","productDescription":"iv, 34 p. **Missing p. 24-25 and 28-29**","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":139000,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2190/report-thumb.jpg"},{"id":29098,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2190/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a6125","contributors":{"authors":[{"text":"Smith, Richard A. 0000-0003-2117-2269 rsmith1@usgs.gov","orcid":"https://orcid.org/0000-0003-2117-2269","contributorId":580,"corporation":false,"usgs":true,"family":"Smith","given":"Richard","email":"rsmith1@usgs.gov","middleInitial":"A.","affiliations":[{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true}],"preferred":true,"id":145652,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hirsch, Robert M. 0000-0002-4534-075X rhirsch@usgs.gov","orcid":"https://orcid.org/0000-0002-4534-075X","contributorId":2005,"corporation":false,"usgs":true,"family":"Hirsch","given":"Robert","email":"rhirsch@usgs.gov","middleInitial":"M.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":37316,"text":"WMA - Integrated Information Dissemination Division","active":true,"usgs":true},{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true},{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"preferred":true,"id":145653,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Slack, James Richard","contributorId":83905,"corporation":false,"usgs":true,"family":"Slack","given":"James","email":"","middleInitial":"Richard","affiliations":[],"preferred":false,"id":145654,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":67087,"text":"i1378 - 1982 - Paleovalley and geologic map of northeastern Colorado","interactions":[],"lastModifiedDate":"2012-02-10T00:11:17","indexId":"i1378","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"1378","subseriesTitle":"NONE","title":"Paleovalley and geologic map of northeastern Colorado","language":"ENGLISH","doi":"10.3133/i1378","usgsCitation":"Scott, G., 1982, Paleovalley and geologic map of northeastern Colorado: U.S. Geological Survey IMAP 1378, 1 map :col. ;45 x 68 cm. +1 text (12 p. : maps ; 28 cm.) folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1378.","productDescription":"1 map :col. ;45 x 68 cm. +1 text (12 p. : maps ; 28 cm.) folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":256448,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1378/plate-1.pdf","size":"5780","linkFileType":{"id":1,"text":"pdf"}},{"id":256449,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1378/report.pdf","size":"1336","linkFileType":{"id":1,"text":"pdf"}},{"id":256450,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1378/report-thumb.jpg"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104,40 ], [ -104,41 ], [ -102,41 ], [ -102,40 ], [ -104,40 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689ac0","contributors":{"authors":[{"text":"Scott, G. R.","contributorId":61398,"corporation":false,"usgs":true,"family":"Scott","given":"G. R.","affiliations":[],"preferred":false,"id":275581,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":65212,"text":"i1544 - 1982 - Petroleum potential of wilderness lands, Oregon","interactions":[],"lastModifiedDate":"2012-02-10T00:11:02","indexId":"i1544","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"1544","subseriesTitle":"NONE","title":"Petroleum potential of wilderness lands, Oregon","language":"ENGLISH","doi":"10.3133/i1544","usgsCitation":"Fouch, T.D., and Miller, B.M., 1982, Petroleum potential of wilderness lands, Oregon: U.S. Geological Survey IMAP 1544, 1 map :col. ;50 x 66 cm., folded in envelope 30 x 24 cm. +1 pamphlet (5 p. : map ; 26 cm.), https://doi.org/10.3133/i1544.","productDescription":"1 map :col. ;50 x 66 cm., folded in envelope 30 x 24 cm. +1 pamphlet (5 p. : map ; 26 cm.)","costCenters":[],"links":[{"id":106800,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9308.htm","linkFileType":{"id":5,"text":"html"},"description":"9308"},{"id":100828,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1544/report.pdf","size":"520","linkFileType":{"id":1,"text":"pdf"}},{"id":189195,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1544/report-thumb.jpg"},{"id":91476,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1544/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.83333333333333,42 ], [ -124.83333333333333,46.166666666666664 ], [ -116.5,46.166666666666664 ], [ -116.5,42 ], [ -124.83333333333333,42 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687d9a","contributors":{"authors":[{"text":"Fouch, T. D.","contributorId":68333,"corporation":false,"usgs":true,"family":"Fouch","given":"T.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":272852,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, B. M.","contributorId":27142,"corporation":false,"usgs":true,"family":"Miller","given":"B.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":272851,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9354,"text":"ofr811113 - 1982 - Hydrology of Area 24, Eastern Coal Province, Alabama and Georgia","interactions":[],"lastModifiedDate":"2016-12-14T12:01:54","indexId":"ofr811113","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"81-1113","title":"Hydrology of Area 24, Eastern Coal Province, Alabama and Georgia","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811113","usgsCitation":"Harkins, J.R., and and others, 1982, Hydrology of Area 24, Eastern Coal Province, Alabama and Georgia: U.S. Geological Survey Open-File Report 81-1113, v, 81 p. :ill., col. maps ;28 cm., https://doi.org/10.3133/ofr811113.","productDescription":"v, 81 p. :ill., col. 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,{"id":28064,"text":"wri822 - 1982 - Quality of streams in the Bull Mountains region, south-central Montana","interactions":[],"lastModifiedDate":"2019-09-26T12:39:17","indexId":"wri822","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-2","title":"Quality of streams in the Bull Mountains region, south-central Montana","docAbstract":"In October 1977, water-quality monitoring stations were established on five small streams that drain the Bull Mountains and also on the Musselshell River to document present water-quality conditions in a coal area of south-central Montana. Relatively static water-quality conditions exist throughout the annual flow cycle on the small streams but water quality varies with time on the Musselshell River. The near absence of surface runoff in the Bull Mountains during the study and the dominance by the base-flow component account for stability of water quality in the small streams. High-mountain runoff coupled with storms and prairie runoff impact the base flow of the Musselshell River. Bicarbonate and sulfate were the principal anions and are present in nearly equal proportions in all small streams. Except for West Parrot Creek, magnesium was the most dominant cation. West Parrot Creek, which consistently contained the smallest levels of dissolved solids, had sodium rather than magnesium as the principal cation. Fattig Creek was highest in dissolved solids with an approximate concentration range of 900 to 2,100 milligrams per liter. Suspended-sediment discharge in the streams was relatively small; no stream exceeded 0.32 ton per day. The Musselshell River had dissolved solids concentrations that ranged from about 450 milligrams per liter during spring runoff to 1,800 milligrams per liter during periods of base flow. The sodium sulfate-type water, which is common during base flow, is diluted during runoff with water having principal ions of calcium, magnesium, and bicarbonate. Suspended-sediment loads ranged from 0.56 to 37,300 tons per day and correlated directly to stream discharge. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri822","usgsCitation":"Knapton, J.R., 1982, Quality of streams in the Bull Mountains region, south-central Montana: U.S. Geological Survey Water-Resources Investigations Report 82-2, iv, 50 p., https://doi.org/10.3133/wri822.","productDescription":"iv, 50 p.","costCenters":[],"links":[{"id":157994,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Montana","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"id\":\"29\",\"properties\":{\"name\":\"Montana\",\"nation\":\"USA  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J. 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,{"id":3869,"text":"cir863 - 1982 - Water-data program of the U.S. Geological Survey","interactions":[],"lastModifiedDate":"2012-02-02T00:05:36","indexId":"cir863","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"863","title":"Water-data program of the U.S. Geological Survey","docAbstract":"The U.S. Geological Survey is the principal Federal agency responsible for the collection of hydrologic data needed for the planning, development, use, and management of the Nation 's water resources. These data are the foundation necessary for conducting analytical and interpretive appraisals describing the occurrence and availability of surface and ground waters, and their physical, chemical, and biological characteristics. The data are likewise required for basic and problem-oriented research in hydraulics, hydrology, and related fields. Hydrologic data collection by the Geological Survey began in 1894. Current operations include about 17,000 stations for collection of river, lake, and reservoir data; about 27,000 wells for collection of ground-water data; and almost 17,000 stations for collection of water-quality information. These activities are described as well as the means by which the data are made available, and how the program is coordinated with other agencies. (USGS)","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir863","usgsCitation":"Gilbert, B.K., and Buchanan, T.J., 1982, Water-data program of the U.S. Geological Survey: U.S. Geological Survey Circular 863, iii, 16 p. :ill., maps ;27 cm., https://doi.org/10.3133/cir863.","productDescription":"iii, 16 p. :ill., maps ;27 cm.","costCenters":[],"links":[{"id":126650,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1982/0863/report-thumb.jpg"},{"id":30961,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1982/0863/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f1e4b07f02db5ee2c2","contributors":{"authors":[{"text":"Gilbert, Bruce K.","contributorId":60198,"corporation":false,"usgs":true,"family":"Gilbert","given":"Bruce","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":147761,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buchanan, Thomas J.","contributorId":6842,"corporation":false,"usgs":true,"family":"Buchanan","given":"Thomas","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":147760,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10636,"text":"ofr82712 - 1982 - Slides showing geology and mineral resources of the eastern Pioneer Mountains, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:06:29","indexId":"ofr82712","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-712","title":"Slides showing geology and mineral resources of the eastern Pioneer Mountains, Montana","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82712","usgsCitation":"Pearson, R.C., Zen, E., and Berger, B.R., 1982, Slides showing geology and mineral resources of the eastern Pioneer Mountains, Montana: U.S. Geological Survey Open-File Report 82-712, 2 p., col. maps ;28 cm., https://doi.org/10.3133/ofr82712.","productDescription":"2 p., col. maps ;28 cm.","costCenters":[],"links":[{"id":144200,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0712/report-thumb.jpg"},{"id":38469,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0712/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f1e4b07f02db5ee3d0","contributors":{"authors":[{"text":"Pearson, R. C.","contributorId":30978,"corporation":false,"usgs":true,"family":"Pearson","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":161720,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zen, E-an","contributorId":38564,"corporation":false,"usgs":true,"family":"Zen","given":"E-an","affiliations":[],"preferred":false,"id":161721,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Berger, B. R.","contributorId":77914,"corporation":false,"usgs":true,"family":"Berger","given":"B.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":161722,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":10482,"text":"ofr82936 - 1982 - Progress report on geologic studies of the Ranger orebodies, Northern Territory, Australia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:33","indexId":"ofr82936","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-936","title":"Progress report on geologic studies of the Ranger orebodies, Northern Territory, Australia","docAbstract":"The Ranger No. 1 and No. 3 orebodies contain about 124,000 tonnes U3O8 in highly chloritized metasediments of the lower Proterozoic Cahill Formation within about 500 m of the projected sub-Kombolgie Formation unconformity. In both orebodies, oxidized and reduced uranium minerals occur chiefly in quartzose schists that have highly variable amounts of muscovite, sericite, and chlorite. The effects of several periods of alteration are pervasive in the vicinity of orebodies where biotite and garnet are altered to chlorite, and feldspars to white mica or chlorite. Oxidized uranium minerals, associated with earthy iron oxides, occur from the surface to a depth of about 60 m. Below the oxidized zone, uranium occurs chiefly as uraninite and pitchblende disseminated through thick sections of quartz-chlorite-muscovite schist and has no apparent association with graphite or sulfides. In fact, graphite is rare and sulfides are generally low in abundance (<0.5 percent). Higher ore grades occur in disrupted zones a few centimeters thick and in some quartz-chlorite vein-like zones of uncertain origin. Uranium correlates strongly with chlorite, but not all of the many ages of chlorite have associated uranium. At least five textural varieties of chlorite are present and represent at least 3 ages. Preliminary microprobe analyses suggest that Mg-Fe-Al contents are relatively uniform. Apatite commonly occurs with chlorite. Uranium is not common in carbonate rocks and seems to occur only in disrupted zones that have chlorite alteration. Chloritization and silicification are more widespread and intense in the No. 1 orebody than in the No. 3. In both orebodies, hematite occurs tens to hundreds of meters below the weathered zone, in both altered and largely unaltered rocks, with and without uranium. \r\n\r\nThe structure of the orebodies is outwardly simple, particularly in No. 3; dips are less than 40? on most lithologic contacts. The No. 1 orebody is in a basin-like structure about 400 m wide that probably formed in part by progressive removal of carbonate rocks that are as much as 200 m thick adjacent to the No. 1 orebody and below the No. 3 orebody. Quartz-chlorite breccias have formed in the zone of carbonate thinning; uranium is spotty and low grade in these breccias. Chloritized and uraniferous broken and sheared zones, a few centimeters to a few meters thick, have an unknown attitude but must have small displacement. Blocks of altered Kombolgie sandstone are downfaulted into the No. 3 orebody and locally contain reduced uranium minerals. One or more shear zones 5-30 m thick of crushed and smeared fine to coarse rock fragments occur below the orebodies, and other low-angle shears probably occur in the orebodies. The shear zone dips about 40 o and displacement on it is not known. The footwall rocks generally are less retrograded than those in the hanging wall (orebody) and consist of quartz-biotite-feldspar schists and gneisses flanking the Nanambu Complex. A few scattered fractures in the footwall sequence contain pitchblende of unknown age and origin. \r\n\r\nMajor element chemical analyses confirm the lithologic observations of large changes in composition during multiple stages of alteration. Granitic dikes and pelitic schists have gained Fe and Mg and lost Si, Ca, Na, and K during chloritization. Marbles have gained Si, Al, Fe, and P, and lost Mg, Ca, and K during jasperoid-chlorite alteration. Total net chemical gains and losses in the Ranger No. 1 orebody were huge: equal to about 37 percent of the mass of the ore-bearing rock that will be mined. There were net gains in Si and P and net losses in Al, Fe, Mg, Ca, K, and Na. \r\n\r\nThe geologic age(s) of uranium emplacement are obscure because there are few age criteria. Reduced uranium minerals are younger than 1.8-b.y.-old granite dikes, and some occur locally in 1.65-b.y.-old Kombolgie Formation. Diabase dikes (age not known) are thoroughly chloritized and contain sparse ore minerals. Oxidized ura","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82936","usgsCitation":"Nash, J., and Frishman, D., 1982, Progress report on geologic studies of the Ranger orebodies, Northern Territory, Australia: U.S. Geological Survey Open-File Report 82-936, 31 p., ill., map ;28 cm., https://doi.org/10.3133/ofr82936.","productDescription":"31 p., ill., map ;28 cm.","costCenters":[],"links":[{"id":144007,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0936/report-thumb.jpg"},{"id":38347,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0936/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65debf","contributors":{"authors":[{"text":"Nash, J. T.","contributorId":31751,"corporation":false,"usgs":true,"family":"Nash","given":"J. T.","affiliations":[],"preferred":false,"id":161473,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frishman, David","contributorId":40214,"corporation":false,"usgs":true,"family":"Frishman","given":"David","email":"","affiliations":[],"preferred":false,"id":161474,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28040,"text":"wri8172 - 1982 - Sediment transport and source areas of sediment and runoff, Big Sandy River basin, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:08:25","indexId":"wri8172","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"81-72","title":"Sediment transport and source areas of sediment and runoff, Big Sandy River basin, Wyoming","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri8172","usgsCitation":"Kircher, J.E., 1982, Sediment transport and source areas of sediment and runoff, Big Sandy River basin, Wyoming: U.S. Geological Survey Water-Resources Investigations Report 81-72, vi, 51 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri8172.","productDescription":"vi, 51 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":157948,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0072/report-thumb.jpg"},{"id":56878,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0072/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbf33","contributors":{"authors":[{"text":"Kircher, J. E.","contributorId":11207,"corporation":false,"usgs":true,"family":"Kircher","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":199112,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61453,"text":"mf1367 - 1982 - Reconnaissance geologic map and mineral resource potential of the Gearhart Mountain Wilderness and Roadless Area (6225), Lake and Klamath counties, Oregon","interactions":[],"lastModifiedDate":"2025-09-24T16:53:30.56769","indexId":"mf1367","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1367","title":"Reconnaissance geologic map and mineral resource potential of the Gearhart Mountain Wilderness and Roadless Area (6225), Lake and Klamath counties, Oregon","docAbstract":"The Gearhart Mountain Wilderness, Lake and Klamath Counties, Oreg., is devoid of mines and mineral prospects and there are no known mining claims within the area. Furthermore, the results of this mineral appraisal indicate that there is little likelihood that commercial deposits of metallic minerals will be found in the area. Commercial uranium deposits, like those at the White King and Lucky Lass mines about 16 mi (~25 km) to the southeast of the wilderness, and deposits of mercury, like those south-southeast of the wilderness, are not likely to be found within the wilderness, even though all of these areas are characterized by middle and late Cenozoic intrusive and extrusive volcanic rocks. Rock of low commercial value for construction purposes is present, but better and more accessible deposits are present in adjacent regions. There is no evidence to indicate that mineral fuels are present in the area. Higher than normal heat floe characterizes the region containing Gerheart Mountain, indicating that it may have some, as yet undefined, potential for the development of geothermal energy. Data are not available to determine whether this higher than normal heat flow is meaningful in terms of a potential energy source or as a guide to possible future exploration; lack of thermal springs or other evidence of localized geothermal anomalies within the Gerhart Mountain suggest, however, that the potential for the development of geothermal energy is probably low.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1367","usgsCitation":"Walker, G.W., and Ridenour, J., 1982, Reconnaissance geologic map and mineral resource potential of the Gearhart Mountain Wilderness and Roadless Area (6225), Lake and Klamath counties, Oregon: U.S. Geological Survey Miscellaneous Field Studies Map 1367, Report: 3 p.; 1 Plate: 28.60 x 25.20 inches, https://doi.org/10.3133/mf1367.","productDescription":"Report: 3 p.; 1 Plate: 28.60 x 25.20 inches","numberOfPages":"4","costCenters":[],"links":[{"id":496035,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_7048.htm","linkFileType":{"id":5,"text":"html"}},{"id":284428,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1367/report.pdf"},{"id":284427,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1367/plate-1.pdf"},{"id":182580,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1367.jpg"}],"scale":"48000","country":"United States","state":"Oregon","county":"Klamath County, Lake County","otherGeospatial":"Gearhart Mountain","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.913889,42.478333 ], [ -120.913889,42.543056 ], [ -120.715,42.543056 ], [ -120.715,42.478333 ], [ -120.913889,42.478333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd6f73e4b0b290851066be","contributors":{"authors":[{"text":"Walker, George W.","contributorId":101308,"corporation":false,"usgs":true,"family":"Walker","given":"George","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":265672,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ridenour, James","contributorId":87540,"corporation":false,"usgs":true,"family":"Ridenour","given":"James","email":"","affiliations":[],"preferred":false,"id":265671,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28039,"text":"wri824046 - 1982 - Evaluation of sediment yield and sediment data-collection network in the Piceance basin, northwestern Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:25","indexId":"wri824046","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-4046","title":"Evaluation of sediment yield and sediment data-collection network in the Piceance basin, northwestern Colorado","docAbstract":"Statistical relationships were developed between suspended-sediment discharge and several regional factors of climate, physiography, and land use in the Piceance basin, northwestern Colorado. The purpose of the study was to evaluate the existing sediment collection network, especially in regard to detecting changes in suspended-sediment discharge due to the development in the basin. Spatial- and time variability were examined using multiple linear regression techniques. Because of the short period of record, monthly mean sediment loads were used to determine shifts or changes in trends due to mining and related activities in the basin. Dummy variable analysis was used to detect these premining and postmining differences in the regression lines and also to detect seasonal differences in the sediment discharge. Differences did exist in the sediment discharge from season to season and before and after mining; however, due to the variability and short period of record the cause of these differences could not be adequately determined. Part of the high variability in sediment discharge was due to variability in the water discharge. Therefore, if the network is to be improved, the emphasis needs to be on improvement of the water-discharge. The results of the monthly mean regression analysis were used in the mean monthly and mean annual analysis for determination of initial network design equations. These were only preliminary in nature and could be improved with additional data. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824046","usgsCitation":"Kircher, J.E., and Von Guerard, P., 1982, Evaluation of sediment yield and sediment data-collection network in the Piceance basin, northwestern Colorado: U.S. Geological Survey Water-Resources Investigations Report 82-4046, vi, 25 p. :ill., map ;28 cm., https://doi.org/10.3133/wri824046.","productDescription":"vi, 25 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":123891,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4046/report-thumb.jpg"},{"id":56877,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4046/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db673e0e","contributors":{"authors":[{"text":"Kircher, J. E.","contributorId":11207,"corporation":false,"usgs":true,"family":"Kircher","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":199110,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Von Guerard, Paul","contributorId":40620,"corporation":false,"usgs":true,"family":"Von Guerard","given":"Paul","affiliations":[],"preferred":false,"id":199111,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61394,"text":"mf1455 - 1982 - Map showing relationship of historic to prehistoric landslides, Pacific Palisades area, city of Los Angeles, California","interactions":[],"lastModifiedDate":"2012-02-10T00:10:29","indexId":"mf1455","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1455","title":"Map showing relationship of historic to prehistoric landslides, Pacific Palisades area, city of Los Angeles, California","language":"ENGLISH","doi":"10.3133/mf1455","usgsCitation":"McGill, J., 1982, Map showing relationship of historic to prehistoric landslides, Pacific Palisades area, city of Los Angeles, California: U.S. Geological Survey Miscellaneous Field Studies Map 1455, 1 map ;77 x 134 cm. folded in envelope 25 x 32 cm., https://doi.org/10.3133/mf1455.","productDescription":"1 map ;77 x 134 cm. folded in envelope 25 x 32 cm.","costCenters":[],"links":[{"id":105882,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_7209.htm","linkFileType":{"id":5,"text":"html"},"description":"7209"},{"id":183467,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.66666666666667,34 ], [ -118.66666666666667,34.083333333333336 ], [ -118.5,34.083333333333336 ], [ -118.5,34 ], [ -118.66666666666667,34 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605cdd","contributors":{"authors":[{"text":"McGill, J.T.","contributorId":32988,"corporation":false,"usgs":true,"family":"McGill","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":265571,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61537,"text":"mf1381A - 1982 - Geologic map of the Wild Rogue Wilderness, Coos, Curry, and Douglas counties, Oregon","interactions":[],"lastModifiedDate":"2012-02-10T00:10:51","indexId":"mf1381A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1381","chapter":"A","title":"Geologic map of the Wild Rogue Wilderness, Coos, Curry, and Douglas counties, Oregon","language":"ENGLISH","doi":"10.3133/mf1381A","usgsCitation":"Gray, F., Ramp, L., Moring, B., Douglas, I., and Donahoe, J., 1982, Geologic map of the Wild Rogue Wilderness, Coos, Curry, and Douglas counties, Oregon: U.S. Geological Survey Miscellaneous Field Studies Map 1381, 1 map ;58 x 49 cm. folded in envelope 25 x 32 cm., https://doi.org/10.3133/mf1381A.","productDescription":"1 map ;58 x 49 cm. folded in envelope 25 x 32 cm.","costCenters":[],"links":[{"id":105801,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_7070.htm","linkFileType":{"id":5,"text":"html"},"description":"7070"},{"id":187073,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.08333333333333,42.583333333333336 ], [ -124.08333333333333,42.833333333333336 ], [ -123.83333333333333,42.833333333333336 ], [ -123.83333333333333,42.583333333333336 ], [ -124.08333333333333,42.583333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db689841","contributors":{"authors":[{"text":"Gray, Floyd 0000-0002-0223-8966 fgray@usgs.gov","orcid":"https://orcid.org/0000-0002-0223-8966","contributorId":603,"corporation":false,"usgs":true,"family":"Gray","given":"Floyd","email":"fgray@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":662,"text":"Western Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":265919,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ramp, Len","contributorId":64333,"corporation":false,"usgs":true,"family":"Ramp","given":"Len","email":"","affiliations":[],"preferred":false,"id":265922,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moring, Barry","contributorId":80692,"corporation":false,"usgs":true,"family":"Moring","given":"Barry","affiliations":[],"preferred":false,"id":265923,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Douglas, Ian","contributorId":35815,"corporation":false,"usgs":true,"family":"Douglas","given":"Ian","email":"","affiliations":[],"preferred":false,"id":265920,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Donahoe, James","contributorId":37827,"corporation":false,"usgs":true,"family":"Donahoe","given":"James","affiliations":[],"preferred":false,"id":265921,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":9308,"text":"ofr82643 - 1982 - Water-resources studies in Utah, July 1, 1981 to June 30, 1982","interactions":[],"lastModifiedDate":"2017-09-01T15:02:14","indexId":"ofr82643","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-643","title":"Water-resources studies in Utah, July 1, 1981 to June 30, 1982","docAbstract":"<p>This report summarizes the progress on water-resources studies in Utah by the U.S. Geological Survey during the period July 1, 1981, to June 30, 1982. Much of the work was done in cooperation with the State of Utah or local agencies. Additional supporting funds were transferred from other Federal agencies or appropriated directly to the Geological Survey.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/ofr82643","usgsCitation":"1982, Water-resources studies in Utah, July 1, 1981 to June 30, 1982: U.S. Geological Survey Open-File Report 82-643, iv, 44 p., https://doi.org/10.3133/ofr82643.","productDescription":"iv, 44 p.","numberOfPages":"48","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":140918,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0643/report-thumb.jpg"},{"id":37023,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0643/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9bbe","contributors":{"compilers":[{"text":"Hamblin, Linda S.","contributorId":52202,"corporation":false,"usgs":true,"family":"Hamblin","given":"Linda","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":659126,"contributorType":{"id":3,"text":"Compilers"},"rank":1}]}}
,{"id":9364,"text":"ofr82434 - 1982 - Flood data in West Windsor Township, Mercer County, New Jersey, through 1981 water year","interactions":[],"lastModifiedDate":"2012-02-02T00:06:00","indexId":"ofr82434","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-434","title":"Flood data in West Windsor Township, Mercer County, New Jersey, through 1981 water year","docAbstract":"Flood stages and peak discharges are described for 13 sites on streams in West Windsor Township, Mercer County, New Jersey, and surrounding areas, collected by the U.S. Geological Survey through the 1981 water year. Included are descriptions and elevations of floodmarks at 30 sites located by the West Windsor Township Environmental Commission after the September 25-27, 1975 flood. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82434","usgsCitation":"Harriman, D., and Velnich, A., 1982, Flood data in West Windsor Township, Mercer County, New Jersey, through 1981 water year: U.S. Geological Survey Open-File Report 82-434, 27 p., map ;28 cm., https://doi.org/10.3133/ofr82434.","productDescription":"27 p., map ;28 cm.","costCenters":[],"links":[{"id":140861,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0434/report-thumb.jpg"},{"id":37074,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0434/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49b7e4b07f02db5cc5ac","contributors":{"authors":[{"text":"Harriman, D.A.","contributorId":27860,"corporation":false,"usgs":true,"family":"Harriman","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":159548,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Velnich, A. J.","contributorId":25149,"corporation":false,"usgs":true,"family":"Velnich","given":"A. J.","affiliations":[],"preferred":false,"id":159547,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28341,"text":"wri8225 - 1982 - Evaluation of a predictive ground-water solute-transport model at the Idaho National Engineering Laboratory, Idaho","interactions":[],"lastModifiedDate":"2019-11-27T09:32:01","indexId":"wri8225","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-25","title":"Evaluation of a predictive ground-water solute-transport model at the Idaho National Engineering Laboratory, Idaho","docAbstract":"<p>Aqueous chemical and radioactive wastes discharged to shallow ponds and to shallow or deep wells on the Idaho National Engineering Laboratory (INEL) since 1952 have affected the quality of the ground water in the underlying Snake River Plain aquifer. The aqueous wastes have created large and laterally dispersed concentration plumes within the aquifer. The waste plumes with the largest areal distribution are those of chloride, tritium, and with high specific conductance values. The data from eight wells drilled near the southern INEL boundary during the summer of 1980 were used to evaluate the accuracy of a predictive modeling study completed in 1973, and to simulate 1980 positions of chloride and tritium plumes. Data interpretation from the drilling program indicates that the hydrogeologic characteristics of the subsurface rocks have marked effects on the regional ground-water flow regimen and, therefore, the movement of aqueous wastes. As expected, the waste plumes projected by the computer model for 1980, extended somewhat further downgradient than indicated by well data due to conservative worst-case assumptions in the model input and inaccurate approximations of subsequent waste discharge and aquifer recharge conditions. (USGS)</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8225","usgsCitation":"Lewis, B.D., and Goldstein, F.J., 1982, Evaluation of a predictive ground-water solute-transport model at the Idaho National Engineering Laboratory, Idaho: U.S. Geological Survey Water-Resources Investigations Report 82-25, vi, 71 p. , https://doi.org/10.3133/wri8225.","productDescription":"vi, 71 p. ","costCenters":[],"links":[{"id":369705,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0025/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158474,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0025/report-thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"Idaho National Engineering Laboratory","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.04681396484375,\n              43.51916261057404\n            ],\n            [\n              -112.04477548599242,\n              43.51916261057404\n            ],\n            [\n              -112.04477548599242,\n              43.51984724248989\n            ],\n            [\n              -112.04681396484375,\n              43.51984724248989\n            ],\n            [\n              -112.04681396484375,\n              43.51916261057404\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5faf18","contributors":{"authors":[{"text":"Lewis, Barney D.","contributorId":93873,"corporation":false,"usgs":true,"family":"Lewis","given":"Barney","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":199625,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goldstein, Flora J.","contributorId":89573,"corporation":false,"usgs":true,"family":"Goldstein","given":"Flora","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":199624,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9287,"text":"ofr82287 - 1982 - Reconnaissance geology of the Wadi Amq Quadrangle, sheet 18/41 C, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:09","indexId":"ofr82287","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-287","title":"Reconnaissance geology of the Wadi Amq Quadrangle, sheet 18/41 C, Kingdom of Saudi Arabia","docAbstract":"The Wadi Amq quadrangle (sheet 18/41 C) lies between lat 18?00' and 18?30' N. and long 41?00' and 41?30' E. and encompasses an area of 2,937 km2, of which only about 150 km2 is land; the remainder is covered by the Red Sea. The only geologic formations exposed in the quadrangle are Quaternary volcanic rocks and surficial deposits. Most of the volcanic rocks are basalt that was extruded during a continuation of the opening of the Red Sea rift. The Quaternary surficial deposits include those of shallow bank and coral reefs, carbonate sand, sabkhahs, pediment and plains, and alluvial sand and gravel. The coral reefs could possibly provide raw material for a cement industry if required, and the sabkhahs might yield useful salts; otherwise the quadrangle has no economic mineral potential.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82287","usgsCitation":"Hadley, D., 1982, Reconnaissance geology of the Wadi Amq Quadrangle, sheet 18/41 C, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 82-287, 8 p., 1 over-size sheet, ill., maps ;28 cm., https://doi.org/10.3133/ofr82287.","productDescription":"8 p., 1 over-size sheet, ill., maps ;28 cm.","costCenters":[],"links":[{"id":140936,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0287/report-thumb.jpg"},{"id":37004,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0287/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37005,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0287/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db6277d5","contributors":{"authors":[{"text":"Hadley, D.G.","contributorId":32527,"corporation":false,"usgs":true,"family":"Hadley","given":"D.G.","affiliations":[],"preferred":false,"id":159423,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":67558,"text":"i1300 - 1982 - Geologic and structure map of the Choteau 1° x 2° quadrangle, western Montana: A digital database","interactions":[{"subject":{"id":23983,"text":"ofr8024 - 1980 - Hydrocarbon evaluation and structure contour map of part of the Choteau 1° x 2° quadrangle, Lewis and Clark, Teton, Powell, Missoula, Lake, Flathead and Cascade Counties, Montana","indexId":"ofr8024","publicationYear":"1980","noYear":false,"title":"Hydrocarbon evaluation and structure contour map of part of the Choteau 1° x 2° quadrangle, Lewis and Clark, Teton, Powell, Missoula, Lake, Flathead and Cascade Counties, Montana"},"predicate":"SUPERSEDED_BY","object":{"id":67558,"text":"i1300 - 1982 - Geologic and structure map of the Choteau 1° x 2° quadrangle, western Montana: A digital database","indexId":"i1300","publicationYear":"1982","noYear":false,"title":"Geologic and structure map of the Choteau 1° x 2° quadrangle, western Montana: A digital database"},"id":1},{"subject":{"id":46736,"text":"ofr78524 - 1978 - Geologic map of part of the Choteau 1 degree by 2 degrees Quadrangle, Lewis and Clark, Teton, Powell, Missoula, Lake, Flathead, and Cascade counties, Montana","indexId":"ofr78524","publicationYear":"1978","noYear":false,"title":"Geologic map of part of the Choteau 1 degree by 2 degrees Quadrangle, Lewis and Clark, Teton, Powell, Missoula, Lake, Flathead, and Cascade counties, Montana"},"predicate":"SUPERSEDED_BY","object":{"id":67558,"text":"i1300 - 1982 - Geologic and structure map of the Choteau 1° x 2° quadrangle, western Montana: A digital database","indexId":"i1300","publicationYear":"1982","noYear":false,"title":"Geologic and structure map of the Choteau 1° x 2° quadrangle, western Montana: A digital database"},"id":2},{"subject":{"id":47106,"text":"ofr79280 - 1979 - Geologic map of the Choteau 1 degree by 2 degrees Quadrangle, Lewis and Clark, Teton, Powell, Missoula, Lake, Hathead, and Cascade counties, Montana","indexId":"ofr79280","publicationYear":"1979","noYear":false,"title":"Geologic map of the Choteau 1 degree by 2 degrees Quadrangle, Lewis and Clark, Teton, Powell, Missoula, Lake, Hathead, and Cascade counties, Montana"},"predicate":"SUPERSEDED_BY","object":{"id":67558,"text":"i1300 - 1982 - Geologic and structure map of the Choteau 1° x 2° quadrangle, western Montana: A digital database","indexId":"i1300","publicationYear":"1982","noYear":false,"title":"Geologic and structure map of the Choteau 1° x 2° quadrangle, western Montana: A digital database"},"id":3}],"lastModifiedDate":"2021-10-22T20:57:18.411894","indexId":"i1300","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"1300","title":"Geologic and structure map of the Choteau 1° x 2° quadrangle, western Montana: A digital database","docAbstract":"The geologic and structure map of Choteau 1 x 2 degree quadrangle (Mudge and others, 1982) was originally converted to a digital format by Jeff Silkwood (U.S.  Forest Service and completed by the U.S. Geological Survey staff and contractor at the Spokane Field Office (WA) in 2000 for input into a geographic information system (GIS).  The resulting digital geologic map (GIS) database can be queried in many ways to produce a variey of geologic maps.  Digital base map data files (topography, roads, towns, rivers and lakes, etc.) are not included: they may be obtained from a variety of commercial and government sources.  This database is not meant to be used or displayed at any scale larger than 1:250,000 (e.g.  1:100,000 or 1:24,000.  The digital geologic map graphics and plot files (chot250k.gra/.hp/.eps and chot-map.pdf) that are provided in the digital package are representations of the digital database.  They are not designed to be cartographic products.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i1300","usgsCitation":"Mudge, M., Earhart, R.L., Whipple, J., and Harrison, J.E., 1982, Geologic and structure map of the Choteau 1° x 2° quadrangle, western Montana: A digital database (Digital Database version 1.0): U.S. Geological Survey IMAP 1300, HTML Document, https://doi.org/10.3133/i1300.","productDescription":"HTML Document","costCenters":[],"links":[{"id":438958,"rank":701,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P93PTFDV","text":"USGS data release","linkHelpText":"GIS Data for Geologic and Structure Map of the Choteau 1 x 2 Degree Quadrangle, Western Montana"},{"id":106683,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9123.htm","linkFileType":{"id":5,"text":"html"},"description":"9123"},{"id":190206,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6139,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/imap/i1300/","linkFileType":{"id":5,"text":"html"}}],"scale":"250000","country":"United States","state":"Montana","otherGeospatial":"Choteau 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114,47 ], [ -114,48 ], [ -112,48 ], [ -112,47 ], [ -114,47 ] ] ] } } ] }","edition":"Digital Database version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a6471","contributors":{"authors":[{"text":"Mudge, Melville R.","contributorId":72370,"corporation":false,"usgs":true,"family":"Mudge","given":"Melville R.","affiliations":[],"preferred":false,"id":276685,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Earhart, Robert L.","contributorId":74729,"corporation":false,"usgs":true,"family":"Earhart","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":276686,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Whipple, James W.","contributorId":90736,"corporation":false,"usgs":true,"family":"Whipple","given":"James W.","affiliations":[],"preferred":false,"id":276687,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Harrison, Jack E.","contributorId":52639,"corporation":false,"usgs":true,"family":"Harrison","given":"Jack","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":276684,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":28353,"text":"wri824006 - 1982 - Thermal springs in the Boise River basin, south-central Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:08:35","indexId":"wri824006","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-4006","title":"Thermal springs in the Boise River basin, south-central Idaho","docAbstract":"The Boise River Basin, characterized by steep, rugged mountains and narrow river valleys, drains an area of about 2,680 square miles in south-central Idaho. Granitic rocks of the Idaho batholith predominate in the basin. Temperature of waters from thermal springs in the basin range from 33 degrees to 87 degrees Celsius, are sodium carbonate type and are slightly alkaline. Dissolved-solids concentrations are less than 280 milligrams per liter. Estimated reservoir temperatures determined by the silica and sodium-potassium-calcium geothermometers range from 50 degrees to 98 degrees Celsius. Tritium concentrations in sampled thermal springs are near zero and indicate these waters were recharged prior to 1954. Stable-isotope data are not conclusive insofar as indicating a source area of recharge for the thermal springs in the basin. Thermal springs discharged at least 4,900 acre-feet of water in 1981, and the associated convective heat flux is 11,000,000 calories per second. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri824006","usgsCitation":"Lewis, R., and Young, H., 1982, Thermal springs in the Boise River basin, south-central Idaho: U.S. Geological Survey Water-Resources Investigations Report 82-4006, iii, 28 p. :ill., map ;28 cm., https://doi.org/10.3133/wri824006.","productDescription":"iii, 28 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":158330,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4006/report-thumb.jpg"},{"id":57158,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4006/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a55e4b07f02db62c686","contributors":{"authors":[{"text":"Lewis, R.E.","contributorId":31735,"corporation":false,"usgs":true,"family":"Lewis","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":199649,"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":199650,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10394,"text":"ofr82240 - 1982 - Ground-water applications of remote sensing","interactions":[],"lastModifiedDate":"2017-03-28T13:17:48","indexId":"ofr82240","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-240","title":"Ground-water applications of remote sensing","docAbstract":"<p>Remote sensing can be used as a tool to inventory springs and seeps and to interpret lithology, structure, and ground-water occurrence and quality. Thermograms are the best images for inventory of seeps and springs. The steps in aquifer mapping are image analysis and interpretation and ground-water interpretation. A ground-water interpretation is derived from a conceptual geologic model by inferring aquifer characteristics and water salinity. The image selection process is very important for obtaining maximum geologic and hydrologic information from remotely sensed data. Remote sensing can contribute an image base map or geologic and hydrologic parameters, derived from the image, to the multiple data sets in a hydrologic information system. Various merging and integration techniques may then be used to obtain information from these data sets.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82240","usgsCitation":"Moore, G.K., 1982, Ground-water applications of remote sensing: U.S. Geological Survey Open-File Report 82-240, iv, 55 p., https://doi.org/10.3133/ofr82240.","productDescription":"iv, 55 p.","numberOfPages":"61","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":38226,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0240/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143926,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0240/report-thumb.jpg"}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d3dc","contributors":{"authors":[{"text":"Moore, Gerald K.","contributorId":14377,"corporation":false,"usgs":true,"family":"Moore","given":"Gerald","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":161314,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":65414,"text":"i1467 - 1982 - Controlled photomosaic of the Arabia Northwest Quadrangle of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:13","indexId":"i1467","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"1467","subseriesTitle":"NONE","title":"Controlled photomosaic of the Arabia Northwest Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i1467","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Controlled photomosaic of the Arabia Northwest Quadrangle of Mars: U.S. Geological Survey IMAP 1467, 1 photomosaic ;40 x 60 cm., sheet 86 x 67 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1467.","productDescription":"1 photomosaic ;40 x 60 cm., sheet 86 x 67 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":114909,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1467/report.pdf","size":"27","linkFileType":{"id":1,"text":"pdf"}},{"id":114910,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1467/plate-1.pdf","size":"8402","linkFileType":{"id":1,"text":"pdf"}},{"id":189725,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1467/report-thumb.jpg"}],"scale":"2000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688cc0","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":533801,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":66466,"text":"i1417 - 1982 - Geologic map of the La Place and Tuskegee quadrangles, Macon, Tallapoosa, and Elmore counties, Alabama","interactions":[],"lastModifiedDate":"2012-02-10T00:11:20","indexId":"i1417","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"1417","subseriesTitle":"NONE","title":"Geologic map of the La Place and Tuskegee quadrangles, Macon, Tallapoosa, and Elmore counties, Alabama","language":"ENGLISH","doi":"10.3133/i1417","usgsCitation":"Markewich, H.W., and Christopher, R.A., 1982, Geologic map of the La Place and Tuskegee quadrangles, Macon, Tallapoosa, and Elmore counties, Alabama: U.S. Geological Survey IMAP 1417, 1 map :col. ;29 x 49 cm., on sheet 71 x 93 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1417.","productDescription":"1 map :col. ;29 x 49 cm., on sheet 71 x 93 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":106720,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9194.htm","linkFileType":{"id":5,"text":"html"},"description":"9194"},{"id":188766,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"48000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -85.86749999999999,32.3675 ], [ -85.86749999999999,32.5 ], [ -85.61749999999999,32.5 ], [ -85.61749999999999,32.3675 ], [ -85.86749999999999,32.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696fd3","contributors":{"authors":[{"text":"Markewich, H. W.","contributorId":31426,"corporation":false,"usgs":true,"family":"Markewich","given":"H.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":274577,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Christopher, R. A.","contributorId":53775,"corporation":false,"usgs":true,"family":"Christopher","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":274578,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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