Ground-water resources of Marquette County are about evenly divided between bedrock aquifers and aquifers in glacial deposits. In the northern and the extreme southern parts of the county, most wells are completed in bedrock at depths less than 100 feet. In the central part, most wells are completed in glacial deposits; some of these wells are as deep as 200 feet. Yields, in some places as high as 300 gallons per minute, are generally greatest from wells completed in glacial deposits. Most well water is hard and has iron concentrations ranging from <0.1 mg/L to about 5.0 mg/L. Both ground water and surface water sources are used in municipal water systems.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/ofr82501","collaboration":"Prepared in cooperation with the Michigan Department of Natural Resources","usgsCitation":"Doonan, C.J., and Van Alstine, J.L., 1982, Ground water and geology of Marquette County, Michigan: U.S. Geological Survey Open-File Report 82-501, Document: vi, 46 p.; Plate: 27.03 x 34.96 inches, https://doi.org/10.3133/ofr82501.","productDescription":"Document: vi, 46 p.; Plate: 27.03 x 34.96 inches","costCenters":[{"id":382,"text":"Michigan Water Science 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sgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66dc6a","contributors":{"authors":[{"text":"Doonan, C. J.","contributorId":62592,"corporation":false,"usgs":true,"family":"Doonan","given":"C.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":158023,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Van Alstine, J. L.","contributorId":85962,"corporation":false,"usgs":true,"family":"Van Alstine","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":158024,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":7356,"text":"ofr821090 - 1982 - Multichannel seismic-reflection profiles collected in 1980 in the northern Bering Sea","interactions":[],"lastModifiedDate":"2012-02-02T00:06:07","indexId":"ofr821090","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":"82-1090","title":"Multichannel seismic-reflection profiles collected in 1980 in the northern Bering Sea","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr821090","usgsCitation":"Marlow, M.S., Cooper, A.K., Smith, G., and Chase, T.E., 1982, Multichannel seismic-reflection profiles collected in 1980 in the northern Bering Sea: U.S. Geological Survey Open-File Report 82-1090, 3 p. map ;28 cm., https://doi.org/10.3133/ofr821090.","productDescription":"3 p. map ;28 cm.","costCenters":[],"links":[{"id":141532,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1090/report-thumb.jpg"},{"id":34758,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1090/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4892","contributors":{"authors":[{"text":"Marlow, Michael S.","contributorId":72775,"corporation":false,"usgs":true,"family":"Marlow","given":"Michael","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":155388,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cooper, A. K.","contributorId":50149,"corporation":false,"usgs":true,"family":"Cooper","given":"A.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":155387,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, G.L.","contributorId":25569,"corporation":false,"usgs":true,"family":"Smith","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":155386,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Chase, T. E.","contributorId":14784,"corporation":false,"usgs":true,"family":"Chase","given":"T.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":155385,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":8193,"text":"ofr82681 - 1982 - Potential effects of surface coal mining on the hydrology of the Cook Creek area, Ashland coal field, southeastern Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:06:09","indexId":"ofr82681","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":"82-681","title":"Potential effects of surface coal mining on the hydrology of the Cook Creek area, Ashland coal field, southeastern Montana","docAbstract":"The Cook Creek area of the Ashland coal field contains large reserves of Federally owned coal that have been identified for potential lease sale. A hydrologic study has been conducted in the potential lease area to describe existing hydrologic systems and to assess potential impacts of surface coal mining on local water resources. Hydrogeologic data collected from wells, springs, and drill holes indicate that shallow aquifers exist within the Tongue River Member of the Fort Union Formation (Paleocene age) and within valley alluvium (Pleistocene and Holocene age). Shallow aquifers within the Tonge River Member include coal beds, clinker, and lenses of sandstone and siltstone. The Knobloch coal bed, a principal shallow aquifer used for livestock watering in the area, averages about 55 feet in thickness and is completely saturated throughout most of its extent. Coarse alluvial deposits are the most productive aquifers and are a major source of stock water in the Cook Creek basin. Surface-water resources are limited to the upstream reach part of Cook Creek, which flows intermittently. The downstream reach part of Cook Creek, plus all other small drainages that originate in the study area, are ephemeral. Mining of the Knoblock and Sawyer coal beds would remove two alluvial springs, one bedrock spring, and two wells, which are all used for watering of livestock. The potentiometric surface within the Knobloch coal aquifer and the alluvial aquifer in the downstream part of the Cook Creek basin would be lowered during mining. Lowered water levels in these aquifers might substantially affect water levels in five wells outside the mine boundary. After mining, the alluvial aquifer downgradient from the mine area might show a long-term degradation in water quality as a result of leaching of soluble salts from overburden materials used to backfill mine pits. Although mining would alter the existing hydrologic systems and remove several springs and shallow wells, alternative ground-water supplies are available that could be developed to replace those lost by mining. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82681","usgsCitation":"Cannon, M.R., 1982, Potential effects of surface coal mining on the hydrology of the Cook Creek area, Ashland coal field, southeastern Montana: U.S. Geological Survey Open-File Report 82-681, 34 p., 2 over-size sheets, ill., maps ;28 cm., https://doi.org/10.3133/ofr82681.","productDescription":"34 p., 2 over-size sheets, ill., maps ;28 cm.","costCenters":[],"links":[{"id":140982,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0681/report-thumb.jpg"},{"id":35805,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0681/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35806,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0681/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35807,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0681/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683848","contributors":{"authors":[{"text":"Cannon, M. R.","contributorId":99140,"corporation":false,"usgs":true,"family":"Cannon","given":"M.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":157321,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7202,"text":"ofr82145 - 1982 - Geophysical studies of the Syncline Ridge area, Nevada Test Site, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:06:00","indexId":"ofr82145","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":"82-145","title":"Geophysical studies of the Syncline Ridge area, Nevada Test Site, Nye County, Nevada","docAbstract":"A wide variety of geophysical methods were employed to study a proposed nuclear waste site at Syncline Ridge on the Nevada Test Site, Nev. The proposed site was believed to be a relatively undisturbed synclinal structure containing a thick argillite unit of Misslsslppian age, the Eleana Formation unit J, which would be the emplacement medium. Data acquisition for the geophysical studies was constrained because of rugged topography in a block of Tipplpah Limestone overlying the central part of the proposed site. This study employed gravity, magnetic, seismic refraction and reflection, and four distinct electrical methods to try and define the structural integrity and shape of the proposed repository medium. Detailed and regional gravity work revealed complex structure at the site. Magnetics helped only in identifying small areas of Tertiary volcanic rocks because of low magnetization of the rocks. Seismic refraction assisted in identifying near surface faulting and bedrock structure. Difficulty was experienced in obtaining good quality reflection data. This implied significant structural complexity but also revealed the principal features that were supported by other data. Electrical methods were used for fault identification and for mapping of a thick argillaceous unit of the Eleana Formation in which nuclear waste was to be emplaced. \r\n\r\nThe geophysical studies indicate that major faults along the axis of Syncline Ridge and on both margins have large vertical offsets displacing units so as not only to make mining difficult, but also providing potential paths for waste migration to underlying carbonate aquifers. The Eleana Formation appeared heterogeneous, which was inferred to be due to structural complexity. Only a small region in the northwest part of the study area was found to contain a thick and relatively undisturbed volume of host rock.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82145","usgsCitation":"Hoover, D., Hanna, W.F., Anderson, L.A., Flanigan, V.J., and Pankratz, L.W., 1982, Geophysical studies of the Syncline Ridge area, Nevada Test Site, Nye County, Nevada: U.S. Geological Survey Open-File Report 82-145, 72 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82145.","productDescription":"72 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":140180,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0145/report-thumb.jpg"},{"id":34602,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0145/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b437","contributors":{"authors":[{"text":"Hoover, D.B.","contributorId":37734,"corporation":false,"usgs":true,"family":"Hoover","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":154740,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hanna, W. F.","contributorId":6835,"corporation":false,"usgs":true,"family":"Hanna","given":"W.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":154738,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Anderson, L. A.","contributorId":22763,"corporation":false,"usgs":true,"family":"Anderson","given":"L.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":154739,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Flanigan, V. J.","contributorId":81097,"corporation":false,"usgs":true,"family":"Flanigan","given":"V.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":154742,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Pankratz, L. W.","contributorId":53375,"corporation":false,"usgs":true,"family":"Pankratz","given":"L.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":154741,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":7199,"text":"ofr82315 - 1982 - Geophysical and lithologic logs of coal test holes drilled during 1980 in the Pierce Reservoir and Bengough Hill quadrangles, Albany County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:06:00","indexId":"ofr82315","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":"82-315","title":"Geophysical and lithologic logs of coal test holes drilled during 1980 in the Pierce Reservoir and Bengough Hill quadrangles, Albany County, Wyoming","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82315","usgsCitation":"Hansen, D., Weaver, J.N., Ellis, M., and Williamson, C., 1982, Geophysical and lithologic logs of coal test holes drilled during 1980 in the Pierce Reservoir and Bengough Hill quadrangles, Albany County, Wyoming: U.S. Geological Survey Open-File Report 82-315, 53 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82315.","productDescription":"53 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":140171,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0315/report-thumb.jpg"},{"id":34591,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0315/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c269","contributors":{"authors":[{"text":"Hansen, D. 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N. 0000-0001-7068-5445 jcweaver@usgs.gov","orcid":"https://orcid.org/0000-0001-7068-5445","contributorId":9645,"corporation":false,"usgs":true,"family":"Weaver","given":"J.","email":"jcweaver@usgs.gov","middleInitial":"N.","affiliations":[],"preferred":false,"id":154725,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ellis, M.S.","contributorId":64301,"corporation":false,"usgs":true,"family":"Ellis","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":154727,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Williamson, Courteney","contributorId":39382,"corporation":false,"usgs":true,"family":"Williamson","given":"Courteney","email":"","affiliations":[],"preferred":false,"id":154726,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":8056,"text":"ofr82900 - 1982 - E-field ratio telluric survey near Medicine Lake in the Medicine Lake Highlands caldera, Siskiyou County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:13","indexId":"ofr82900","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":"82-900","title":"E-field ratio telluric survey near Medicine Lake in the Medicine Lake Highlands caldera, Siskiyou County, California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82900","usgsCitation":"Broker, M., Christopherson, K.R., and Heller, R., 1982, E-field ratio telluric survey near Medicine Lake in the Medicine Lake Highlands caldera, Siskiyou County, California: U.S. Geological Survey Open-File Report 82-900, 11 p., ill., map ;28 cm., https://doi.org/10.3133/ofr82900.","productDescription":"11 p., ill., map ;28 cm.","costCenters":[],"links":[{"id":142044,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0900/report-thumb.jpg"},{"id":35627,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0900/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a59e4b07f02db62fd5b","contributors":{"authors":[{"text":"Broker, M. M.","contributorId":63012,"corporation":false,"usgs":true,"family":"Broker","given":"M. M.","affiliations":[],"preferred":false,"id":157069,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Christopherson, K. R.","contributorId":11607,"corporation":false,"usgs":true,"family":"Christopherson","given":"K.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":157068,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Heller, Ron","contributorId":75930,"corporation":false,"usgs":true,"family":"Heller","given":"Ron","email":"","affiliations":[],"preferred":false,"id":157070,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":7347,"text":"ofr82376 - 1982 - Mineral resources of the Rawah Wilderness, Larimer County, Colorado, with a section on interpretation of aeromagnetic data","interactions":[],"lastModifiedDate":"2023-11-01T20:53:57.927985","indexId":"ofr82376","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":"82-376","title":"Mineral resources of the Rawah Wilderness, Larimer County, Colorado, with a section on interpretation of aeromagnetic data","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82376","usgsCitation":"Pearson, R.C., McCallum, M.E., Griswold, M.L., Patten, L.L., and Flanigan, V.J., 1982, Mineral resources of the Rawah Wilderness, Larimer County, Colorado, with a section on interpretation of aeromagnetic data: U.S. Geological Survey Open-File Report 82-376, Report: ii, 30 p.; 3 Plates: 23.04 x 39.55 inches or smaller, https://doi.org/10.3133/ofr82376.","productDescription":"Report: ii, 30 p.; 3 Plates: 23.04 x 39.55 inches or smaller","costCenters":[],"links":[{"id":108428,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13714.htm","linkFileType":{"id":5,"text":"html"},"description":"13714"},{"id":34752,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0376/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34751,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0376/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140149,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0376/report-thumb.jpg"},{"id":34754,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0376/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34753,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0376/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","county":"Larimer County","otherGeospatial":"Rawah Wilderness","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -105.89283158562563,\n 40.53632239113537\n ],\n [\n -105.85609994188098,\n 40.57725310085152\n ],\n [\n -105.85120238938202,\n 40.61444112016537\n ],\n [\n -105.86222188250558,\n 40.69525362840554\n ],\n [\n -105.89038280937612,\n 40.74536387569361\n ],\n [\n -105.88915842125168,\n 40.78060402668666\n ],\n [\n -105.94425588686832,\n 40.8260176904264\n ],\n [\n -105.95894854436641,\n 40.87140027627248\n ],\n [\n -106.0152703981081,\n 40.87695519153513\n ],\n [\n -106.09240684997188,\n 40.858436994807704\n ],\n [\n -106.10832389559441,\n 40.84732359113241\n ],\n [\n -106.05200204185273,\n 40.79729020788247\n ],\n [\n -106.00302651686009,\n 40.72309731188798\n ],\n [\n -105.9675192612399,\n 40.65718176786683\n ],\n [\n -105.94548027499336,\n 40.60328688631327\n ],\n [\n -105.89283158562563,\n 40.53632239113537\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a91a2","contributors":{"authors":[{"text":"Pearson, R. C.","contributorId":30978,"corporation":false,"usgs":true,"family":"Pearson","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":155353,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCallum, M. E.","contributorId":34119,"corporation":false,"usgs":true,"family":"McCallum","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":155354,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Griswold, M. L.","contributorId":63005,"corporation":false,"usgs":true,"family":"Griswold","given":"M.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":155355,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Patten, L. L.","contributorId":72374,"corporation":false,"usgs":true,"family":"Patten","given":"L.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":155356,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Flanigan, V. J.","contributorId":81097,"corporation":false,"usgs":true,"family":"Flanigan","given":"V.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":887316,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":30344,"text":"wri8234 - 1982 - Water-quality characteristics of Everglades National Park, 1959-77, with reference to the effects of water management","interactions":[],"lastModifiedDate":"2019-08-05T12:06:39","indexId":"wri8234","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":"82-34","title":"Water-quality characteristics of Everglades National Park, 1959-77, with reference to the effects of water management","docAbstract":"The U.S. Geological Survey has collected water-quality data in the Everglades National Park since 1959. Major ions, macronutrients, trace elements, and pesticides are the primary chemical groups analyzed. The period of record and frequency of sampling vary for each chemical group, with the longest record for the major ions and the shortest for the macronutrients. Within the park there are three major drainageways: Big Cypress Swamp, Shark River Slough, and Taylor Slough. Each drainageway exhibits unique hydrologic conditions, yet there is a high degree of homogeneity in water-quality characteristics among these areas. Seasonal changes in major-ion, trace-element, and macronutrient concentrations are marked in the shallow marsh. Concentrations generally increase in the dry season due to evapotranspiration, changes in chemical equilibria, and precipitation. Water-management practices in south Florida have changed the water quality in the Shark River Slough. Most major-ion, dissolved-solid, and iron concentrations and color levels have steadily increased since 1963. The water quality in the other two drainageways has not changed since sampling began. Chlorinated-hydrocarbon insecticide residues in bottom material were found in low concentration at every sampling station in the park. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8234","usgsCitation":"Waller, B.G., 1982, Water-quality characteristics of Everglades National Park, 1959-77, with reference to the effects of water management: U.S. Geological Survey Water-Resources Investigations Report 82-34, vi, 51 p. , https://doi.org/10.3133/wri8234.","productDescription":"vi, 51 p. ","costCenters":[],"links":[{"id":366265,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0034/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159310,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0034/report-thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Everglades National Park","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -81.15600585937499,\n 25.13533901613099\n ],\n [\n -80.48583984375,\n 25.13533901613099\n ],\n [\n -80.48583984375,\n 25.517657429994035\n ],\n [\n -81.15600585937499,\n 25.517657429994035\n ],\n [\n -81.15600585937499,\n 25.13533901613099\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d9f0","contributors":{"authors":[{"text":"Waller, Bradley G.","contributorId":83492,"corporation":false,"usgs":true,"family":"Waller","given":"Bradley","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":203093,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":27597,"text":"wri824110 - 1982 - Hydrology of the sand-and-gravel aquifer, southern Okaloosa and Walton Counties, northwest Florida","interactions":[],"lastModifiedDate":"2022-02-22T19:34:05.117776","indexId":"wri824110","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":"82-4110","title":"Hydrology of the sand-and-gravel aquifer, southern Okaloosa and Walton Counties, northwest Florida","docAbstract":"The sand-and-gravel aquifer in southern Okaloosa and Walton Counties, northwest Florida, extends from land surface to depth of 50 to 150 feet. Intervening layers of clay generally separate the aquifer into an unconfined surficial zone, composed principally of fine to medium sand, and a lower confined zone, consisting of variable amounts of medium to coarse sand and gravel. Well yields of 50 to 500 gallons per minute are possible in most of the area, and yields of 500 to 1,000 gallons per minute can be developed in parts of southwestern Okaloosa County.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri824110","usgsCitation":"Hayes, L.R., and Barr, D.E., 1982, Hydrology of the sand-and-gravel aquifer, southern Okaloosa and Walton Counties, northwest Florida: U.S. Geological Survey Water-Resources Investigations Report 82-4110, vi, 49 p., https://doi.org/10.3133/wri824110.","productDescription":"vi, 49 p.","costCenters":[],"links":[{"id":158870,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4110/report-thumb.jpg"},{"id":56467,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4110/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":396266,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35617.htm"}],"country":"United States","state":"Florida","county":"Okaloosa County, Walton County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -86.70135498046875,\n 30.379983796443767\n ],\n [\n -86.19873046875,\n 30.379983796443767\n ],\n [\n -86.19873046875,\n 30.590637026892917\n ],\n [\n -86.70135498046875,\n 30.590637026892917\n ],\n [\n -86.70135498046875,\n 30.379983796443767\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc79d","contributors":{"authors":[{"text":"Hayes, L. R.","contributorId":50931,"corporation":false,"usgs":true,"family":"Hayes","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":198387,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barr, D. E.","contributorId":55469,"corporation":false,"usgs":true,"family":"Barr","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":198388,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":27575,"text":"wri826 - 1982 - Methodologies for extraction of dissolved inorganic carbon for stable carbon isotope studies: Evaluation and alternatives","interactions":[],"lastModifiedDate":"2019-11-25T16:02:39","indexId":"wri826","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":"82-6","title":"Methodologies for extraction of dissolved inorganic carbon for stable carbon isotope studies: Evaluation and alternatives","docAbstract":"The gas evolution and the strontium carbonate precipitation techniques to extract dissolved inorganic carbon (DIC) for stable carbon isotope analysis were investigated. Theoretical considerations, involving thermodynamic calculations and computer simulation pointed out several possible sources of error in delta carbon-13 measurements of the DIC and demonstrated the need for experimental evaluation of the magnitude of the error. An alternative analytical technique, equilibration with out-gassed vapor phase, is proposed. The experimental studies revealed that delta carbon-13 of the DIC extracted from a 0.01 molar NaHC03 solution by both techniques agreed within 0.1 per mil with the delta carbon-13 of the DIC extracted by the precipitation technique, and an increase of only 0.27 per mil in that extracted by the gas evolution technique. The efficiency of extraction of DIC decreased with sulfate concentration in the precipitation technique but was independent of sulfate concentration in the gas evolution technique. Both the precipitation and gas evolution technique were found to be satisfactory for extraction of DIC from different kinds of natural water for stable carbon isotope analysis, provided appropriate precautions are observed in handling the samples. For example, it was found that diffusion of atmospheric carbon dioxide does alter the delta carbon-13 of the samples contained in polyethylene bottles; filtration and drying in the air change the delta carbon-13 of the samples contained in polyethylene bottles; filtration and drying in the air change the delta carbon-13 of the precipitation technique; hot manganese dioxide purification changes the delta carbon-13 of carbon dioxide. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri826","usgsCitation":"Hassan, A.A., 1982, Methodologies for extraction of dissolved inorganic carbon for stable carbon isotope studies: Evaluation and alternatives: U.S. Geological Survey Water-Resources Investigations Report 82-6, v, 51 p. , https://doi.org/10.3133/wri826.","productDescription":"v, 51 p. ","costCenters":[],"links":[{"id":158913,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0006/report-thumb.jpg"},{"id":369595,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0006/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629f7a","contributors":{"authors":[{"text":"Hassan, Afifa Afifi","contributorId":41467,"corporation":false,"usgs":true,"family":"Hassan","given":"Afifa","email":"","middleInitial":"Afifi","affiliations":[],"preferred":false,"id":198356,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":27560,"text":"wri824078 - 1982 - Magnitude and frequency of floods in eastern Oregon","interactions":[],"lastModifiedDate":"2017-02-07T10:07:45","indexId":"wri824078","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":"82-4078","title":"Magnitude and frequency of floods in eastern Oregon","docAbstract":"A method for estimating the magnitude and frequency of floods is presented for unregulated streams in eastern Oregon. Equations relating flood magnitude to basin characteristics were developed for exceedance probabilities of 0.5 to 0.01 (2- to 100-year recurrence intervals). Separate equations are presented for four regions: Southeast, Northeast, North Central, and Eastern Cascades. Also presented are values of flood discharges for selected exceedance probabilities and of basin characteristics for all gaging stations used in the analysis. Included are data for 148 stations in Oregon, 3 stations in northern California, 3 stations in western Idaho, 4 stations in northern Nevada, and 4 stations in southern Washington. Drainage areas used in the analysis range from 0.47 to 11,300 square miles. Also included are maximum discharges for all eastern Oregon stations used in the analysis. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824078","usgsCitation":"Harris, D., and Hubbard, L., 1982, Magnitude and frequency of floods in eastern Oregon: U.S. Geological Survey Water-Resources Investigations Report 82-4078, vi, 45 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824078.","productDescription":"vi, 45 p. :ill., maps ;28 cm.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":56417,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4078/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123422,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4078/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64956b","contributors":{"authors":[{"text":"Harris, D.D.","contributorId":59002,"corporation":false,"usgs":true,"family":"Harris","given":"D.D.","email":"","affiliations":[],"preferred":false,"id":198324,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hubbard, L.E.","contributorId":104945,"corporation":false,"usgs":true,"family":"Hubbard","given":"L.E.","email":"","affiliations":[],"preferred":false,"id":198325,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":27634,"text":"wri8240 - 1982 - Method for estimating historical irrigation requirements from ground water in the High Plains in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming","interactions":[],"lastModifiedDate":"2018-08-08T14:01:49","indexId":"wri8240","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":"82-40","title":"Method for estimating historical irrigation requirements from ground water in the High Plains in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming","docAbstract":"Historical information on ground-water pumpage for irrigation is required for use with a computer model of the High Plains aquifer. Available historical data on ground-water pumpage in the High Plains were inadequate for use with the computer model. Consequently, a method was developed to estimate historical pumpage data.
Two principal components were used to develop estimates of ground-water pumpage: (1) Acreage irrigated; and (2) irrigation demand. The Blaney-Criddle formula was used to calculate consumptive-use requirements for irrigated crops grown on the High Plains. The irrigation demand for each crop was estimated by subtracting precipitation available to the crop from the consumptive-use requirement of the crop. Irrigation demands were combined with irrigated acreages to estimate the volume of irrigation water required for areas in the High Plains. Estimates of irrigation water requirements were compiled for 1949, 1954, 1959, 1964, 1969, 1974, and 1978. Irrigation pumpage for use with the computer model can be estimated from the irrigation water requirements by applying a factor to account for irrigation system efficiency.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8240","usgsCitation":"Heimes, F.J., and Luckey, R.R., 1982, Method for estimating historical irrigation requirements from ground water in the High Plains in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming: U.S. Geological Survey Water-Resources Investigations Report 82-40, iii, 64 p., https://doi.org/10.3133/wri8240.","productDescription":"iii, 64 p.","numberOfPages":"71","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true},{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":356336,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0040/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158792,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0040/report-thumb.jpg"}],"country":"United States","state":"Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, Wyoming","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -106,\n 32\n ],\n [\n -96,\n 32\n ],\n [\n -96,\n 43.5\n ],\n [\n -106,\n 43.5\n ],\n [\n -106,\n 32\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629ed0","contributors":{"authors":[{"text":"Heimes, Frederick J.","contributorId":20787,"corporation":false,"usgs":true,"family":"Heimes","given":"Frederick","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":198451,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Luckey, Richard R.","contributorId":17980,"corporation":false,"usgs":true,"family":"Luckey","given":"Richard","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":198450,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"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":28286,"text":"wri824023 - 1982 - A three-dimensional ground-water-flow model modified to reduce computer-memory requirements and better simulate confining-bed and aquifer pinchouts","interactions":[],"lastModifiedDate":"2012-02-02T00:08:48","indexId":"wri824023","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":"82-4023","title":"A three-dimensional ground-water-flow model modified to reduce computer-memory requirements and better simulate confining-bed and aquifer pinchouts","docAbstract":"The Trescott computer program for modeling groundwater flow in three dimensions has been modified to (1) treat aquifer and confining bed pinchouts more realistically and (2) reduce the computer memory requirements needed for the input data. Using the original program, simulation of aquifer systems with nonrectangular external boundaries may result in a large number of nodes that are not involved in the numerical solution of the problem, but require computer storage. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824023","usgsCitation":"Leahy, P., 1982, A three-dimensional ground-water-flow model modified to reduce computer-memory requirements and better simulate confining-bed and aquifer pinchouts: U.S. Geological Survey Water-Resources Investigations Report 82-4023, iii, 62 p. :map ;28 cm., https://doi.org/10.3133/wri824023.","productDescription":"iii, 62 p. :map ;28 cm.","costCenters":[],"links":[{"id":122874,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4023/report-thumb.jpg"},{"id":57104,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4023/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a5c5c","contributors":{"authors":[{"text":"Leahy, P.P.","contributorId":104896,"corporation":false,"usgs":true,"family":"Leahy","given":"P.P.","email":"","affiliations":[],"preferred":false,"id":199530,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":66035,"text":"i1418 - 1982 - Marine geologic map of the Puerto Rico insular shelf, northwestern area, Rio Grande de Anasco to Rio Camuy","interactions":[],"lastModifiedDate":"2012-02-10T00:11:08","indexId":"i1418","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":"1418","subseriesTitle":"NONE","title":"Marine geologic map of the Puerto Rico insular shelf, northwestern area, Rio Grande de Anasco to Rio Camuy","language":"ENGLISH","doi":"10.3133/i1418","usgsCitation":"Grove, K.A., 1982, Marine geologic map of the Puerto Rico insular shelf, northwestern area, Rio Grande de Anasco to Rio Camuy: U.S. Geological Survey IMAP 1418, 1 map :col. ;93 x 116 cm., on sheet 106 x 123 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1418.","productDescription":"1 map :col. ;93 x 116 cm., on sheet 106 x 123 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":106721,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9195.htm","linkFileType":{"id":5,"text":"html"},"description":"9195"},{"id":189541,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"40000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -67.31666666666666,18.466666666666665 ], [ -67.31666666666666,18.583333333333332 ], [ -66.86749999999999,18.583333333333332 ], [ -66.86749999999999,18.466666666666665 ], [ -67.31666666666666,18.466666666666665 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db6064cf","contributors":{"authors":[{"text":"Grove, K. A.","contributorId":47459,"corporation":false,"usgs":true,"family":"Grove","given":"K.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":273890,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"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":68251,"text":"ha658 - 1982 - Dissolved solids and sodium in water from the High Plains aquifer in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:13:21","indexId":"ha658","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"658","title":"Dissolved solids and sodium in water from the High Plains aquifer in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming","docAbstract":"In 1978, the U.S. Geological Survey initiated a 5-year study of the High Plains regional aquifer to provide: (1) Hydrologic information needed to evaluate the effects of continued ground-water development; and (2) computer models to predict aquifer response to changes in ground-water development. The plan of study for the High Plains Regional Aquifer-System Analysis was described by Weeks (1978). A description of the High Plains aquifer and a map of the 1978 water table were presented by Gutentag and Weeks (1980). Maps of the bedrock geology, altitude of aquifer base, and saturated thickness of the High Plains aquifer were published by Weeks and Gutentag (1981). Water-level and saturated-thickness changes, from predevelopment to 1980, were mapped by Luckey, Gutentag, and Weeks (1981). This report describes the areal distribution of dissolved solids and sodium in the water of the High Plains aquifer. Data used in this study were provided by the U.S. Geological Survey and State agencies in each of the eight States in the High Plains. Their contribution is an integral part of this investigation.","language":"ENGLISH","doi":"10.3133/ha658","usgsCitation":"Krothe, N.C., Oliver, J.W., and Weeks, J., 1982, Dissolved solids and sodium in water from the High Plains aquifer in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming: U.S. Geological Survey Hydrologic Atlas 658, 2 maps :col. ;54 x 38 cm., on sheets 74 x 104 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/ha658.","productDescription":"2 maps :col. ;54 x 38 cm., on sheets 74 x 104 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":189677,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89636,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/658/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89637,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/658/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a250","contributors":{"authors":[{"text":"Krothe, Noel C.","contributorId":41466,"corporation":false,"usgs":true,"family":"Krothe","given":"Noel","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":277911,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Oliver, Joseph W.","contributorId":77970,"corporation":false,"usgs":true,"family":"Oliver","given":"Joseph","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":277912,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Weeks, John B.","contributorId":36123,"corporation":false,"usgs":true,"family":"Weeks","given":"John B.","affiliations":[],"preferred":false,"id":277910,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"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 - 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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. 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Warren L.","contributorId":47481,"corporation":false,"usgs":true,"family":"Coonrad","given":"Warren","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":660808,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}} ,{"id":28763,"text":"wri824 - 1982 - Appraisal of ground-water quality near wastewater-treatment facilities, Glacier National Park, Montana","interactions":[],"lastModifiedDate":"2018-11-15T12:06:35","indexId":"wri824","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":"82-4","title":"Appraisal of ground-water quality near wastewater-treatment facilities, Glacier National Park, Montana","docAbstract":"Water-level and water-quality data were collected from monitoring wells at wastewater-treatment facilities in Glacier National Park. Five additional shallow observation wells were installed at the Glacier Park Headquarters facility to monitor water quality in the shallow ground-water system.
Water-level, water-quality, and geologic information indicate that some of the initial monitoring wells are not ideally located to sample ground water most likely to be affected by waste disposal at the sites. Small differences in chemical characteristics between samples from monitor wells indicate that effluent may be affecting ground-water quality but that impacts are not significant.
Future monitoring of ground-water quality could be limited to selected wells most likely to be impacted by percolating effluent. Laboratory analyses for common ions could detect future impacts.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri824","usgsCitation":"Moreland, J.A., and Wood, W.A., 1982, Appraisal of ground-water quality near wastewater-treatment facilities, Glacier National Park, Montana: U.S. Geological Survey Water-Resources Investigations Report 82-4, iv, 27 p., https://doi.org/10.3133/wri824.","productDescription":"iv, 27 p.","costCenters":[],"links":[{"id":359459,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0004/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159429,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0004/report-thumb.jpg"}],"country":"United States","state":"Montana","otherGeospatial":"Glacier National Park","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -114.47753906249999,\n 48.23016176791893\n ],\n [\n -113.192138671875,\n 48.23016176791893\n ],\n [\n -113.192138671875,\n 49.00004203215395\n ],\n [\n -114.47753906249999,\n 49.00004203215395\n ],\n [\n -114.47753906249999,\n 48.23016176791893\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a3c4","contributors":{"authors":[{"text":"Moreland, Joe A.","contributorId":48171,"corporation":false,"usgs":true,"family":"Moreland","given":"Joe","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":200357,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wood, Wayne A.","contributorId":29417,"corporation":false,"usgs":true,"family":"Wood","given":"Wayne","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":200356,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":26400,"text":"wri8245 - 1982 - Delineation and hydrologic effects of a gasoline leak at Stovepipe Wells Hotel, Death Valley National Monument, California","interactions":[],"lastModifiedDate":"2019-08-05T11:21:19","indexId":"wri8245","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":"82-45","title":"Delineation and hydrologic effects of a gasoline leak at Stovepipe Wells Hotel, Death Valley National Monument, California","docAbstract":"Ground water is the only local source of water available to the Stovepipe Wells Hotel facilities of the Death Valley National Monument, California. A leak in a service station storage tank caused the formation of a gasoline layer overlying the water table, creating the potential for contamination of the water supply. The maximum horizontal extent of the gasoline layer was mathematically estimated to be 1,300 feet downgradient from the leaky gasoline tank. Exploratory drilling detected the gasoline layer between 900 and 1,400 feet downgradient and between 50 and 150 feet upgradient from the source. Traces of the soluble components of gasoline were also found in the aquifer 150 feet upgradient, and 250 feet distant from the source perpendicular to the direction of ground-water movement. The gasoline spill is not likely to have an effect on the supply wells located 0.4 mile south of the leak source, which is nearly perpendicular to the direction of ground-water movement and the primary direction of gasoline movement in the area. No effect on phreatophytes 2 miles downgradient from the layer is likely, but the potential effects of gasoline vapors within the unsaturated zone on local xerophytes are not known. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8245","usgsCitation":"Buono, A., and Packard, E.M., 1982, Delineation and hydrologic effects of a gasoline leak at Stovepipe Wells Hotel, Death Valley National Monument, California: U.S. Geological Survey Water-Resources Investigations Report 82-45, iv, 23 p. , https://doi.org/10.3133/wri8245.","productDescription":"iv, 23 p. 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