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Strike Dam and Bruneau quadrangles, southwestern Idaho","language":"ENGLISH","doi":"10.3133/mf2063E","usgsCitation":"Malde, H., 1989, Geologic map of the Bruneau Formation in the C.J. Strike Dam and Bruneau quadrangles, southwestern Idaho: U.S. Geological Survey Miscellaneous Field Studies Map 2063, 1 map ;58 x 86 cm. on sheet 74 x 104 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/mf2063E.","productDescription":"1 map ;58 x 86 cm. on sheet 74 x 104 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":105220,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5665.htm","linkFileType":{"id":5,"text":"html"},"description":"5665"},{"id":180072,"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\": [ [ [ -116,42.8675 ], [ -116,43 ], [ -115.75,43 ], [ -115.75,42.8675 ], [ -116,42.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0be4b07f02db69d76a","contributors":{"authors":[{"text":"Malde, H.E.","contributorId":65863,"corporation":false,"usgs":true,"family":"Malde","given":"H.E.","affiliations":[],"preferred":false,"id":263278,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":44833,"text":"wri884202 - 1989 - Hydrogeology of the western part of the Salt River Valley area, Maricopa County, Arizona","interactions":[],"lastModifiedDate":"2013-12-13T14:03:39","indexId":"wri884202","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"88-4202","title":"Hydrogeology of the western part of the Salt River Valley area, Maricopa County, Arizona","docAbstract":"The Salt River Valley is a major population and agricultural center of more than 3,000 mi2 in central Arizona (fig. 1). The western part of the Salt River Valley area (area of this report) covers about 1,500 mi2. The Phoenix metropolitan area with a population of more than 1.6 million in 1985 (Valley National Bank, 1987) is located within the valley. The watersheds of the Salt, Verde, and Agua Fria Rivers provide the valley with a reliable but limited surface-water supply that must be augmented with ground water even in years of plentiful rainfall. Large-scale ground-water withdrawals began in the Salt River Valley in the early part of the 20th century; between 1915 and 1983, the total estimated ground-water pumpage was 81 million acre-ft (U.S. Geological Survey, 1984). Because of the low average annual rainfall and high potential evapotranspiration, the principal sources of ground-water recharge are urban runoff, excess irrigation, canal seepage and surface-water flows during years of higher-than-normal rainfall. Withdrawals greatly exceed recharge and, in some area, ground-water levels have declines as much as 350 ft (Laney and other, 1978; Ross, 1978). In the study area, ground-water declines of more than 300 ft have occurred in Deer Valley and from Luke Air Force Base north to Beardsley. As a result, a large depression of the water table has developed west of Luke Air Force Base (fig. 2). Ground-water use has decreased in recent years because precipitation and surface-water supplies have been greater than normal. Increased precipitation also caused large quantities of runoff to be released into the normally dry Salt and Gila River channels. From February 1978 to June 1980, streamflow losses of at least 90,000 acre-ft occurred between Jointhead Dam near the east boundary of the study area and Gillespie Dam several miles southwest of the west edge of the study area (Mann and Rhone, 1983). Consequently, ground-water declines in a large part of the basin have slowed, and ground-water levels in some sarea have risen significantly. In many areas along the Salt River and northeast of the confluence of the Salt and Agua Fria River, ground-water levels rose more than 25 ft between 1978 and 1984 (Reeter and Remick, 1986).","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri884202","collaboration":"Prepared in cooperation with the Arizona Department of Water Resources, Salt River Project, and Arizona Municipal Water Users' Association","usgsCitation":"Brown, J.G., and Pool, D.R., 1989, Hydrogeology of the western part of the Salt River Valley area, Maricopa County, Arizona: U.S. Geological Survey Water-Resources Investigations Report 88-4202, 4 Plates: 45.81 x 39.54 inches and smaller, https://doi.org/10.3133/wri884202.","productDescription":"4 Plates: 45.81 x 39.54 inches and smaller","costCenters":[],"links":[{"id":171262,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri884202.PNG"},{"id":279489,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4202/plate-3.pdf"},{"id":279490,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4202/plate-4.pdf"},{"id":279487,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4202/plate-1.pdf"},{"id":279488,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4202/plate-2.pdf"}],"country":"United States","state":"Arizona","county":"Maricopa County","otherGeospatial":"Salt River Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -113.0,33.25 ], [ -113.0,34.0 ], [ -112.0,34.0 ], [ -112.0,33.25 ], [ -113.0,33.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db614b2d","contributors":{"authors":[{"text":"Brown, James G.","contributorId":81094,"corporation":false,"usgs":true,"family":"Brown","given":"James","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":230517,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pool, D. R.","contributorId":75581,"corporation":false,"usgs":true,"family":"Pool","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":230516,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":21287,"text":"ofr89399 - 1989 - Ground-water, surface-water, and bottom-sediment contamination in the O-Field area, Aberdeen Proving Ground, Maryland, and the possible effects of selected remedial actions on ground water","interactions":[],"lastModifiedDate":"2012-02-02T00:07:59","indexId":"ofr89399","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-399","title":"Ground-water, surface-water, and bottom-sediment contamination in the O-Field area, Aberdeen Proving Ground, Maryland, and the possible effects of selected remedial actions on ground water","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/ofr89399","usgsCitation":"Vroblesky, D.A., Lorah, M.M., and Oliveros, J.P., 1989, Ground-water, surface-water, and bottom-sediment contamination in the O-Field area, Aberdeen Proving Ground, Maryland, and the possible effects of selected remedial actions on ground water: U.S. Geological Survey Open-File Report 89-399, x, 162 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr89399.","productDescription":"x, 162 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":155288,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0399/report-thumb.jpg"},{"id":50839,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0399/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6965fe","contributors":{"authors":[{"text":"Vroblesky, Don A. vroblesk@usgs.gov","contributorId":413,"corporation":false,"usgs":true,"family":"Vroblesky","given":"Don","email":"vroblesk@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":184150,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lorah, Michelle M. 0000-0002-9236-587X mmlorah@usgs.gov","orcid":"https://orcid.org/0000-0002-9236-587X","contributorId":1437,"corporation":false,"usgs":true,"family":"Lorah","given":"Michelle","email":"mmlorah@usgs.gov","middleInitial":"M.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":184151,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Oliveros, James P.","contributorId":72367,"corporation":false,"usgs":true,"family":"Oliveros","given":"James","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":184152,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":13109,"text":"ofr8968 - 1989 - Ground-water level data for North Carolina, 1987","interactions":[],"lastModifiedDate":"2016-12-16T09:03:56","indexId":"ofr8968","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-68","title":"Ground-water level data for North Carolina, 1987","docAbstract":"Continuous and periodic measurements in 54 key wells and water-level measurements emplaced in Coastal Plain aquifers across North Carolina in 193 supplemental wells are presented in this report. Hydrographs of selected wells show changes in ground-water storage in the State. The water table in the shallow aquifers was higher throughout most of the State in 1987 than in 1986, indicating that rain had recharged these aquifers sufficiently to replenish the deficit in ground water storage that accumulated in the western and central parts of the State during 1986. Water levels in the heavily pumped Coastal Plain aquifers show a general downward trend for the year, indicating ground water is being withdrawn from aquifer storage. Record low water levels were measured in 4 of 13 wells in the Castle Hayne aquifer; the greatest decline measured during 1987 was 0.3 ft. Water levels in wells in the Peedee, Black Creek, upper Cape Fear, and lower Cape Fear aquifers generally show downward trends. Record low water levels were measured in 4 of 8 wells in the Peedee aquifer; the maximum decline measured during 1987 was 1.5 ft. All wells in the Black Creek, upper Cape Fear, and lower Cape Fear aquifers had record low water levels for 1987, with maximum measured declines in 1987 of 8.6, 3.1, and 3.1 ft., respectively. Record high water levels were measured in two wells, one each in the Castle Hayne and Peedee aquifers. Potentiometric surface maps show the effects of major centers of pumping for the Castle Hayne, Black Creek, and lower Cape Fear aquifers of the Coastal Plain.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8968","usgsCitation":"Coble, R.W., Strickland, A., and Bailey, M.C., 1989, Ground-water level data for North Carolina, 1987: U.S. Geological Survey Open-File Report 89-68, x, 152 p. :chiefly ill. ;28 cm., https://doi.org/10.3133/ofr8968.","productDescription":"x, 152 p. :chiefly ill. ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":41508,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0068/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144539,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0068/report-thumb.jpg"}],"country":"United States","state":"North 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","language":"English","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr89319","usgsCitation":"Colton, R.B., Whitaker, S.T., and Ehler, W., 1989, Geologic map of the Opheim 1° x 30' quadrangle, Valley and Daniels counties, Montana: U.S. Geological Survey Open-File Report 89-319, Report: 10 p.; 1 Plate: 32.69 × 28.74 inches, https://doi.org/10.3133/ofr89319.","productDescription":"Report: 10 p.; 1 Plate: 32.69 × 28.74 inches","costCenters":[],"links":[{"id":41530,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0319/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41531,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0319/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144442,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0319/report-thumb.jpg"},{"id":108795,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17633.htm","linkFileType":{"id":5,"text":"html"},"description":"17633"}],"country":"United States","state":"Montana","county":"Daniels County, Valley County","otherGeospatial":"Opheim 1° x 30' quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -106,\n 48.5\n ],\n [\n -107.0,\n 48.5\n ],\n [\n -107.0,\n 49.0\n ],\n [\n -106,\n 49.0\n ],\n [\n -106,\n 48.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af6e4b07f02db692b65","contributors":{"authors":[{"text":"Colton, R. B.","contributorId":40186,"corporation":false,"usgs":true,"family":"Colton","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":167289,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Whitaker, S. T.","contributorId":38124,"corporation":false,"usgs":true,"family":"Whitaker","given":"S.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":167288,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ehler, W. C.","contributorId":50875,"corporation":false,"usgs":true,"family":"Ehler","given":"W. C.","affiliations":[],"preferred":false,"id":167290,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":33611,"text":"b1857B - 1989 - United States gold terranes — Part I","interactions":[{"subject":{"id":33611,"text":"b1857B - 1989 - United States gold terranes — Part I","indexId":"b1857B","publicationYear":"1989","noYear":false,"chapter":"B","title":"United States gold terranes — Part I"},"predicate":"IS_PART_OF","object":{"id":33277,"text":"b1857 - 1988 - Geology and resources of gold in the United States","indexId":"b1857","publicationYear":"1988","noYear":false,"title":"Geology and resources of gold in the United States"},"id":1}],"isPartOf":{"id":33277,"text":"b1857 - 1988 - Geology and resources of gold in the United States","indexId":"b1857","publicationYear":"1988","noYear":false,"title":"Geology and resources of gold in the United States"},"lastModifiedDate":"2025-03-06T19:55:35.830362","indexId":"b1857B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1857","chapter":"B","title":"United States gold terranes — Part I","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1857B","usgsCitation":"Tooker, E.W., Bagby, W.C., Kiilsgaard, T.H., Fisher, F.S., Bennett, E.H., Redden, J., and French, G.M., 1989, United States gold terranes — Part I: U.S. Geological Survey Bulletin 1857, vi, 74 p., https://doi.org/10.3133/b1857B.","productDescription":"vi, 74 p.","costCenters":[],"links":[{"id":61492,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1857b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":165905,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1857b/report-thumb.jpg"},{"id":403680,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_22002.htm","text":"Geologic setting and potential exploration guides for gold deposits, Black Hills, South Dakota","linkFileType":{"id":5,"text":"html"}},{"id":483005,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_22003.htm","text":"Gold-silver deposits associated with the Trans-Challis fault system, Idaho","linkFileType":{"id":5,"text":"html"}},{"id":483006,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_22004.htm","text":"Patterns of gold mineralization in Nevada and Utah","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699892","contributors":{"authors":[{"text":"Tooker, Edwin W.","contributorId":26345,"corporation":false,"usgs":true,"family":"Tooker","given":"Edwin","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":211660,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bagby, William C.","contributorId":75604,"corporation":false,"usgs":true,"family":"Bagby","given":"William","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":211662,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kiilsgaard, Thor H.","contributorId":68738,"corporation":false,"usgs":true,"family":"Kiilsgaard","given":"Thor","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":211661,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fisher, Frederick S.","contributorId":17979,"corporation":false,"usgs":true,"family":"Fisher","given":"Frederick","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":211658,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bennett, Earl H.","contributorId":97093,"corporation":false,"usgs":true,"family":"Bennett","given":"Earl","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":211663,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Redden, Jack A.","contributorId":107347,"corporation":false,"usgs":true,"family":"Redden","given":"Jack A.","affiliations":[],"preferred":false,"id":211664,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"French, Gregory McN","contributorId":25620,"corporation":false,"usgs":true,"family":"French","given":"Gregory","email":"","middleInitial":"McN","affiliations":[],"preferred":false,"id":211659,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":13226,"text":"ofr89259 - 1989 - Natural ground-water quality in Michigan, 1974-87","interactions":[],"lastModifiedDate":"2016-09-16T11:43:33","indexId":"ofr89259","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-259","title":"Natural ground-water quality in Michigan, 1974-87","docAbstract":"Wide variations occur in the chemical and physical characteristics of natural groundwaters in Michigan. Dissolved-solids concentrations range from 20 to 76,000 mg/L. Waters having low dissolved-solids concentrations are calcium bicarbonate-type waters. Sodium, sulfate, and chloride increase as mineralization increases. Iron, aluminum, and titanium concentrations are higher at some locations than is common in most natural waters. Lead concentrations exceed U.S. Environmental Protection Agency 's primary drinking-water regulations at some locations in the northern part of the lower Peninsula. Generalized areal patterns of water-quality variability indicate that geology is a primary cause of differences across the State. Examples of chemical associations in water indicate that chemical analyses may be valuable in tracing and identifying mineral deposits.
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a symposium highlighting research on the causes, effects, and prediction of geologic and hydrologic hazards; program abstracts","interactions":[],"lastModifiedDate":"2018-10-01T19:09:58","indexId":"cir1038","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"1038","title":"Geohazards '88; a symposium highlighting research on the causes, effects, and prediction of geologic and hydrologic hazards; program abstracts","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/cir1038","usgsCitation":"1989, Geohazards '88; a symposium highlighting research on the causes, effects, and prediction of geologic and hydrologic hazards; program abstracts: U.S. Geological Survey Circular 1038, iv, 29 p., https://doi.org/10.3133/cir1038.","productDescription":"iv, 29 p.","costCenters":[],"links":[{"id":31404,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1989/1038/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117204,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1989/1038/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8f81","contributors":{"editors":[{"text":"Hodges, Carroll Ann","contributorId":99144,"corporation":false,"usgs":true,"family":"Hodges","given":"Carroll","email":"","middleInitial":"Ann","affiliations":[],"preferred":false,"id":747034,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}} ,{"id":21190,"text":"ofr89626 - 1989 - A study of Bacillus cereus distributions and ten water extractable ions from soils on St. John, U.S. Virgin Islands","interactions":[],"lastModifiedDate":"2012-02-02T00:07:46","indexId":"ofr89626","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-626","title":"A study of Bacillus cereus distributions and ten water extractable ions from soils on St. John, U.S. Virgin Islands","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr89626","usgsCitation":"Tucker, R.E., McHugh, J.B., and Alminas, H.V., 1989, A study of Bacillus cereus distributions and ten water extractable ions from soils on St. John, U.S. Virgin Islands: U.S. Geological Survey Open-File Report 89-626, 44 p. :ill. ;28 cm., https://doi.org/10.3133/ofr89626.","productDescription":"44 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":153075,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0626/report-thumb.jpg"},{"id":50777,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0626/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a6251","contributors":{"authors":[{"text":"Tucker, R. E.","contributorId":50520,"corporation":false,"usgs":true,"family":"Tucker","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":184000,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McHugh, J. B.","contributorId":79462,"corporation":false,"usgs":true,"family":"McHugh","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":184001,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Alminas, H. V.","contributorId":83926,"corporation":false,"usgs":true,"family":"Alminas","given":"H.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":184002,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":44164,"text":"ofr89226 - 1989 - Summary of hydrologic data for the San Gabriel River basin and Edwards Aquifer, Georgetown area, Texas, water year 1988","interactions":[],"lastModifiedDate":"2016-08-15T09:09:29","indexId":"ofr89226","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-226","title":"Summary of hydrologic data for the San Gabriel River basin and Edwards Aquifer, Georgetown area, Texas, water year 1988","docAbstract":"The Edwards aquifer is the principle source of freshwater for municipal, domestic, and industrial users in the Georgetown area. Other sources of freshwater are the streams draining the San Gabriel River basin and Lake Georgetown. Lake Georgetown, located on the North Fork San Gabriel River west of Georgetown, is a freshwater supply for some municipalities in the area, water in the San Gabriel River basin also supplies a variety of needs east of Georgetown. Because of the importance of the Edwards aquifer and the surface waters in the area, the U.S. Geological Survey, in cooperation with the city of Georgetown, conducted a monitoring program of the Edwards Aquifer and principal streams during water year 1988. The study area centered on Georgetown and encompassed an area of about 150 square miles (fig. 1).
\nThe freshwater resources in the Georgetown area have been the subject of three recent reports. Baker and others (1986) described the Edwards aquifer and the relation between recharge and discharge. Krietier and others (1987) provided fracture analysis, geologic mapping, ground-water chemistry, and the relation between rainfall and recharge in the study area. Land and Dorsey (1988) conducted an investigation to reassess the inclusion of the Georgetown Limestone as one of the geologic units comprising the Edwards aquifer. In addition, the Geological Survey publishes streamflow and water-quality data in the Water Resources Data for Texas report on an annual basis.
\nThe primary purpose of this report is to present a summary of the hydrologic data collected from the streams draining the San Gabriel River basin and from the Edwards aquifer during the 1988 water year (October 1987–September 1988). A secondary purpose is to add perspective to the 1988 data by including data from the previous 2 years (1986 and 1987) when available. The scope of the report is limited to the Georgetown area (fig. 1) and to data collected by the Geological Survey.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr89226","collaboration":"Prepared in cooperation with the City of Georgetown","usgsCitation":"Land, L.F., and Dorsey, M., 1989, Summary of hydrologic data for the San Gabriel River basin and Edwards Aquifer, Georgetown area, Texas, water year 1988: U.S. Geological Survey Open-File Report 89-226, Plate: 34.68 x 28.33 inches, https://doi.org/10.3133/ofr89226.","productDescription":"Plate: 34.68 x 28.33 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326473,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr89226.JPG"},{"id":81561,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0226/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","otherGeospatial":"San Gabriel River basin and Edwards Aquifer","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -97.75,\n 30.75\n ],\n [\n -97.5625,\n 30.75\n ],\n [\n -97.5625,\n 30.625\n ],\n [\n -97.625,\n 30.625\n ],\n [\n -97.625,\n 30.5\n ],\n [\n -97.75,\n 30.5\n ],\n [\n -97.75,\n 30.75\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699146","contributors":{"authors":[{"text":"Land, Larry F.","contributorId":60612,"corporation":false,"usgs":true,"family":"Land","given":"Larry","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":229265,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dorsey, M.E.","contributorId":73997,"corporation":false,"usgs":true,"family":"Dorsey","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":229266,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":47308,"text":"ofr899 - 1989 - Geologic map of the Greenville 1 x 2 degree quadrangle, GA, SC, and NC","interactions":[],"lastModifiedDate":"2022-04-06T21:50:01.099884","indexId":"ofr899","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-9","title":"Geologic map of the Greenville 1 x 2 degree quadrangle, GA, SC, and NC","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr899","usgsCitation":"Nelson, A.E., Horton, J., and Clarke, J.W., 1989, Geologic map of the Greenville 1 x 2 degree quadrangle, GA, SC, and NC: U.S. Geological Survey Open-File Report 89-9, Report: 10 p.; 1 Plate: 31.35 × 22.99 inches, https://doi.org/10.3133/ofr899.","productDescription":"Report: 10 p.; 1 Plate: 31.35 × 22.99 inches","costCenters":[],"links":[{"id":84255,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0009/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84256,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0009/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":388177,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18948.htm"},{"id":172611,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0009/report-thumb.jpg"}],"scale":"250000","country":"United States","state":"Georgia, South Carolina","otherGeospatial":"Greenville 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 -84.00,\n 34.00\n ],\n [\n -82.00,\n 34.00\n ],\n [\n -82.00,\n 35.00\n ],\n [\n -84.00,\n 35.00\n ],\n [\n -84.00,\n 34.00\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a313e","contributors":{"authors":[{"text":"Nelson, Arthur E.","contributorId":6035,"corporation":false,"usgs":true,"family":"Nelson","given":"Arthur","email":"","middleInitial":"E.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":235018,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Horton, J. Wright Jr. 0000-0001-6756-6365 whorton@usgs.gov","orcid":"https://orcid.org/0000-0001-6756-6365","contributorId":423,"corporation":false,"usgs":true,"family":"Horton","given":"J. Wright","suffix":"Jr.","email":"whorton@usgs.gov","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":false,"id":235017,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Clarke, James W.","contributorId":35297,"corporation":false,"usgs":true,"family":"Clarke","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":235019,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":27553,"text":"wri884130 - 1989 - The hydrogeologic framework and a reconnaissance of ground-water quality in the Piedmont Province of North Carolina, with a design for future study","interactions":[],"lastModifiedDate":"2017-01-25T09:01:37","indexId":"wri884130","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"88-4130","title":"The hydrogeologic framework and a reconnaissance of ground-water quality in the Piedmont Province of North Carolina, with a design for future study","docAbstract":"The U.S. Geological Survey is investigating the relation of ground- water quality and land use in the regolith and fractured rock ground-water system of the North Carolina Piedmont. The initial phase of this study provides a description of the ground-water flow system and a review of available ground-water data and formulates hypotheses that guide the design of a water-quality monitoring network for study of selected areas. \r\n\r\nIn the Piedmont, the solid igneous and metamorphic bedrock grades upward into unweathered fractured rock that is covered by a transition zone of highly-fractured, partially weathered rock, clay-rich saprolite, and the soil. The fractured bedrock, transition zone, saprolite, and soil make up a complex flow system. \r\n\r\nA review of available ground-water quality data shows a lack of information about organic compounds and trace metals and changes in ground- water quality with depth. Land use, soils, and geology significantly influence ground-water quality. \r\n\r\nThe hypotheses that need to be tested in the next study phase are: (1) that ground-water contamination can be related to land use, and (2) that the transition zone between bedrock and regolith serves as a primary transmitter of contaminants. \r\n\r\nMonitoring of basins containing industrial, urban, residential, and agricultural land uses in future studies will help define the relation of ground-water quality to land use. Water quality at different depths in the flow system and in streams during base flow needs to be identified.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884130","usgsCitation":"Harned, D., 1989, The hydrogeologic framework and a reconnaissance of ground-water quality in the Piedmont Province of North Carolina, with a design for future study: U.S. Geological Survey Water-Resources Investigations Report 88-4130, vi, 55 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri884130.","productDescription":"vi, 55 p. :ill., maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":158977,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4130/report-thumb.jpg"},{"id":56411,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4130/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North 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