A map of the water table in the Solomon River valley from Waconda Lake to Solomon presents current (1980) data on water levels in the unconsolidated deposits. The study was made, in cooperation with the U.S. Bureau of Reclamation, to obtain information for use in a water-management study of the Soloman River Basin.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81334","usgsCitation":"Reed, T., 1983, Map of water table in Solomon River valley, Waconda Lake to Solomon, north-central Kansas, May 1980: U.S. Geological Survey Open-File Report 81-334, 27.82 x 27.38 inches, https://doi.org/10.3133/ofr81334.","productDescription":"27.82 x 27.38 inches","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":134662,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0334/report-thumb.jpg"},{"id":346211,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0334/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Kansas","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -98.32763671875,\n 38.832219591146746\n ],\n [\n -97.37182617187499,\n 38.832219591146746\n ],\n [\n -97.37182617187499,\n 39.51675478434244\n ],\n [\n -98.32763671875,\n 39.51675478434244\n ],\n [\n -98.32763671875,\n 38.832219591146746\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a93e4b07f02db6586cb","contributors":{"authors":[{"text":"Reed, Thomas B.","contributorId":76704,"corporation":false,"usgs":true,"family":"Reed","given":"Thomas B.","affiliations":[],"preferred":false,"id":233304,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":41863,"text":"ofr83611 - 1983 - Aeromagnetic map of south-central Alabama","interactions":[],"lastModifiedDate":"2021-11-16T21:51:27.917459","indexId":"ofr83611","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-611","title":"Aeromagnetic map of south-central Alabama","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83611","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, Aeromagnetic map of south-central Alabama: U.S. Geological Survey Open-File Report 83-611, 9 Plates:32.24 × 22.31 inches or smaller, https://doi.org/10.3133/ofr83611.","productDescription":"9 Plates:32.24 × 22.31 inches or smaller","costCenters":[],"links":[{"id":172723,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79594,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79593,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79592,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79591,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79590,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79589,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79588,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79587,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79586,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":391774,"rank":11,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14133.htm"}],"country":"United States","state":"Alabama","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -86,\n 31.5\n ],\n [\n -87,\n 31.5\n ],\n [\n -87,\n 32.833\n ],\n [\n -86,\n 32.833\n ],\n [\n -86,\n 31.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691cc3","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530667,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":26368,"text":"wri8174 - 1983 - Water resources of Manatee County, Florida","interactions":[],"lastModifiedDate":"2013-08-12T12:12:40","indexId":"wri8174","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"81-74","title":"Water resources of Manatee County, Florida","docAbstract":"Rapid development of Manatee County in southwest Florida is creating water-resource problems. This report presents an evaluation of the water resources and potential effects of water-resource developments. Most streams in the county have small drainage basins and minimal flow. Streamflow is variable with the base flow occurring from November to May. The Manattee River and its largest tributary, the Braden River, are the principal sources of public supplies. Surface water is generally of good quality and less mineralized than ground water except in the tidally affected and coastal area. The principal aquifers in the county are the surficial, minor artesian, and the Floridan. The Floridan aquifer is the major source of irrigation water in the county. The minor artesian aquifer is a highly developed source of water for small rural supplies. Withdrawals of 20 to 50 million gallons per fay from the Floridan aquifer since the 1950 's have caused declines in the potentiometric surface of about 20 to 50 feet. The quality of ground water is good except in the coastal and southern parts of the county. Water in the Floridan aquifer is generally more mineralized than the other aquifers, generally increasing in mineral content with depth and from the northeast towards the southwest. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri8174","usgsCitation":"Brown, D., 1983, Water resources of Manatee County, Florida: U.S. Geological Survey Water-Resources Investigations Report 81-74, vii, 112 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri8174.","productDescription":"vii, 112 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":158404,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0074/report-thumb.jpg"},{"id":276460,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0074/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4804e4b07f02db4ceb99","contributors":{"authors":[{"text":"Brown, David P.","contributorId":85590,"corporation":false,"usgs":true,"family":"Brown","given":"David P.","affiliations":[],"preferred":false,"id":196267,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":54343,"text":"wdrIL822 - 1983 - Water Resources Data, Illinois, Water Year 1982, Vol. 2","interactions":[],"lastModifiedDate":"2012-02-02T00:11:36","indexId":"wdrIL822","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"IL-82-2","title":"Water Resources Data, Illinois, Water Year 1982, Vol. 2","language":"ENGLISH","doi":"10.3133/wdrIL822","usgsCitation":"Richards, T., Hayes, P., Stahl, R., and Fitzgerald, K.K., 1983, Water Resources Data, Illinois, Water Year 1982, Vol. 2: U.S. Geological Survey Water Data Report IL-82-2, NA, https://doi.org/10.3133/wdrIL822.","productDescription":"NA","costCenters":[],"links":[{"id":177018,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb988","contributors":{"authors":[{"text":"Richards, T.E.","contributorId":64718,"corporation":false,"usgs":true,"family":"Richards","given":"T.E.","email":"","affiliations":[],"preferred":false,"id":249976,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hayes, P.D.","contributorId":52644,"corporation":false,"usgs":true,"family":"Hayes","given":"P.D.","email":"","affiliations":[],"preferred":false,"id":249975,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stahl, R.L.","contributorId":35798,"corporation":false,"usgs":true,"family":"Stahl","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":249974,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fitzgerald, K. K.","contributorId":34501,"corporation":false,"usgs":true,"family":"Fitzgerald","given":"K.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":249973,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":54342,"text":"wdrIL821 - 1983 - Water Resources Data, Illinois, Water Year 1982, Vol. 1","interactions":[],"lastModifiedDate":"2012-02-02T00:11:36","indexId":"wdrIL821","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"IL-82-1","title":"Water Resources Data, Illinois, Water Year 1982, Vol. 1","language":"ENGLISH","doi":"10.3133/wdrIL821","usgsCitation":"Stahl, R., Fitzgerald, K.K., Richards, T., and Hayes, P., 1983, Water Resources Data, Illinois, Water Year 1982, Vol. 1: U.S. Geological Survey Water Data Report IL-82-1, NA, https://doi.org/10.3133/wdrIL821.","productDescription":"NA","costCenters":[],"links":[{"id":177017,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb97d","contributors":{"authors":[{"text":"Stahl, R.L.","contributorId":35798,"corporation":false,"usgs":true,"family":"Stahl","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":249970,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fitzgerald, K. K.","contributorId":34501,"corporation":false,"usgs":true,"family":"Fitzgerald","given":"K.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":249969,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Richards, T.E.","contributorId":64718,"corporation":false,"usgs":true,"family":"Richards","given":"T.E.","email":"","affiliations":[],"preferred":false,"id":249972,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hayes, P.D.","contributorId":52644,"corporation":false,"usgs":true,"family":"Hayes","given":"P.D.","email":"","affiliations":[],"preferred":false,"id":249971,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":46850,"text":"ofr82634 - 1983 - Drainage divides, Massachusetts; Housatonic River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:11:00","indexId":"ofr82634","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-634","title":"Drainage divides, Massachusetts; Housatonic River basin","docAbstract":"Drainage boundaries for selected subbasins in Berkshire County, Massachusetts, are delineated on 12 topographic quadrangle maps at a scale of 1:24,000. Drainage basins are shown for all U.S. Geological Survey data-collection sites and for mouths of major rivers. Drainage basins are shown for the outlets of lakes or ponds and for streams where the drainage area is greater than 3 square miles. Successive sites along watercourses are indicated where the intervening area is at least 6 square miles on tributary streams or 15 square miles along the Housatonic River. (USGS)","language":"ENGLISH","doi":"10.3133/ofr82634","usgsCitation":"Gadoury, R.A., and Wandle, S.W., 1983, Drainage divides, Massachusetts; Housatonic River basin: U.S. Geological Survey Open-File Report 82-634, 12 maps ;58 x 43 cm., https://doi.org/10.3133/ofr82634.","productDescription":"12 maps ;58 x 43 cm.","costCenters":[],"links":[{"id":168315,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635e1f","contributors":{"authors":[{"text":"Gadoury, Russell A.","contributorId":99542,"corporation":false,"usgs":true,"family":"Gadoury","given":"Russell","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":234193,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wandle, S. William Jr.","contributorId":99562,"corporation":false,"usgs":true,"family":"Wandle","given":"S.","suffix":"Jr.","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":234194,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":18111,"text":"ofr83740 - 1983 - A hydrochemical reconnaissance study of the Walker River basin, California and Nevada","interactions":[],"lastModifiedDate":"2022-08-25T18:42:56.446527","indexId":"ofr83740","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-740","title":"A hydrochemical reconnaissance study of the Walker River basin, California and Nevada","docAbstract":"During 1975 and 1976, a large number of water and sediment samples were collected from the Walker River Basin. Additional surface water samples were collected during 1980 and 1981. Data are given herein for chemical analyses of snowmelt, tributary, river, spring, well, lake, reservoir, lake sediment pore fluid, tufa, lake and river sediment samples. These data provide the basis for consideration of processes which govern the chemical evolution of large closed basin hydrologic systems in the Basin and Range Province of the Southwestern United States.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83740","usgsCitation":"Benson, L.V., and Spencer, R.J., 1983, A hydrochemical reconnaissance study of the Walker River basin, California and Nevada: U.S. Geological Survey Open-File Report 83-740, iii, 57 p., https://doi.org/10.3133/ofr83740.","productDescription":"iii, 57 p.","costCenters":[],"links":[{"id":405615,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75702.htm","linkFileType":{"id":5,"text":"html"}},{"id":47466,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0740/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":149290,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0740/report-thumb.jpg"}],"country":"United States","state":"California, Nevada","otherGeospatial":"Walker River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -119.9167,\n 38.0667\n ],\n [\n -118.5,\n 38.0667\n ],\n [\n -118.5,\n 39.1833\n ],\n [\n -119.9167,\n 39.1833\n ],\n [\n -119.9167,\n 38.0667\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae3ed","contributors":{"authors":[{"text":"Benson, L. V.","contributorId":50159,"corporation":false,"usgs":true,"family":"Benson","given":"L.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":178567,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spencer, R. J.","contributorId":56664,"corporation":false,"usgs":true,"family":"Spencer","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":178568,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":60611,"text":"mf1322B - 1983 - Aeromagnetic and gravity maps of the Freel and Dardanelles Roadless Areas, Alpine and El Dorado counties, California","interactions":[],"lastModifiedDate":"2016-08-23T08:59:44","indexId":"mf1322B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1322","chapter":"B","title":"Aeromagnetic and gravity maps of the Freel and Dardanelles Roadless Areas, Alpine and El Dorado counties, California","docAbstract":"The Freel and Dardanelles Roadless Areas comprise 51 mi2 (132 km2) in the central Sierra Nevada south of Lake Tahoe. The Sierra Nevada crest passes through the eastern part of the area. Prominent mountains include Stevens Peak (elev 10,061 ft), Waterhouse Peak (elev 9,497 ft), and Freel Peak (elev 10,881 ft).
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1322B","usgsCitation":"Plouff, D., 1983, Aeromagnetic and gravity maps of the Freel and Dardanelles Roadless Areas, Alpine and El Dorado counties, California: U.S. Geological Survey Miscellaneous Field Studies Map 1322, 41.79 x 23.48 inches, https://doi.org/10.3133/mf1322B.","productDescription":"41.79 x 23.48 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":183043,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1322B.PNG"},{"id":327422,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1322-B/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"California","county":"Alpine County, El Dorado County","otherGeospatial":"Freel and Dardaneel Roadless Areas","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.16666666666667,38.666666666666664 ], [ -120.16666666666667,38.916666666666664 ], [ -119.83333333333333,38.916666666666664 ], [ -119.83333333333333,38.666666666666664 ], [ -120.16666666666667,38.666666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db6984c8","contributors":{"authors":[{"text":"Plouff, Donald","contributorId":94657,"corporation":false,"usgs":true,"family":"Plouff","given":"Donald","email":"","affiliations":[],"preferred":false,"id":264077,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":18886,"text":"ofr83831 - 1983 - Analytical results for 544 water samples collected in the Attean Quartz Monzonite in the vicinity of Jackman, Maine","interactions":[],"lastModifiedDate":"2012-02-02T00:07:25","indexId":"ofr83831","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-831","title":"Analytical results for 544 water samples collected in the Attean Quartz Monzonite in the vicinity of Jackman, Maine","docAbstract":"Water samples were collected in the vicinity of Jackman, Maine as a part of the study of the relationship of dissolved constituents in water to the sediments subjacent to the water. Each sample was analyzed for specific conductance, alkalinity, acidity, pH, fluoride, chloride, sulfate, phosphate, nitrate, sodium, potassium, calcium, magnesium, and silica. Trace elements determined were copper, zinc, molybdenum, lead, iron, manganese, arsenic, cobalt, nickel, and strontium. The longitude and latitude of each sample location and a sample site map are included in the report as well as a table of the analytical results.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83831","usgsCitation":"Ficklin, W.H., Nowlan, G., and Preston, D.J., 1983, Analytical results for 544 water samples collected in the Attean Quartz Monzonite in the vicinity of Jackman, Maine: U.S. Geological Survey Open-File Report 83-831, 48 p. :map ;28 cm., https://doi.org/10.3133/ofr83831.","productDescription":"48 p. :map ;28 cm.","costCenters":[],"links":[{"id":150813,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0831/report-thumb.jpg"},{"id":48283,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0831/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":48284,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0831/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67cc04","contributors":{"authors":[{"text":"Ficklin, W. H.","contributorId":89517,"corporation":false,"usgs":true,"family":"Ficklin","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":179921,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nowlan, G.A.","contributorId":99131,"corporation":false,"usgs":true,"family":"Nowlan","given":"G.A.","affiliations":[],"preferred":false,"id":179922,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Preston, D. J.","contributorId":22759,"corporation":false,"usgs":false,"family":"Preston","given":"D.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":179920,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":25786,"text":"wri834214 - 1983 - Subsurface storage of freshwater in south Florida: A prospectus","interactions":[],"lastModifiedDate":"2021-12-21T22:10:20.198858","indexId":"wri834214","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4214","title":"Subsurface storage of freshwater in south Florida: A prospectus","docAbstract":"A method of increasing storage capacity for freshwater in south Florida is to use brackish artesian aquifers as reservoirs. In this way, water deficiencies occurring during the annual dry season can be offset by surplus water obtained during the wet season and injected underground. Most of south Florida is underlain by several deep, confined, carbonate waterbearing zones which might be suitable for freshwater storage. These zones are in the Avon Park, Ocala, Suwannee, Tampa, and Hawthorn Formations. Experimental freshwater injection systems have been operated at five locations with promising, but not fully definitive, results. A determination of the feasibility of freshwater injection at a selected site begins with an assessment of the local geologic suitability. Verification of feasibility, however, requires injection and recovery tests to be performed at the site. Recovery efficiency, a measure of the success of the operation, is the amount of potable water, expressed as a percentage of the volume injected, which can be recovered before its salinity, or the concentration of other chemical constituents present in the native aquifer water, increases to the point that the recovered water is no longer useable.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834214","usgsCitation":"Merritt, M.L., Meyer, F., Sonntag, W.H., and Fitzpatrick, D., 1983, Subsurface storage of freshwater in south Florida: A prospectus: U.S. Geological Survey Water-Resources Investigations Report 83-4214, iv, 69 p., https://doi.org/10.3133/wri834214.","productDescription":"iv, 69 p.","costCenters":[],"links":[{"id":393273,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35857.htm"},{"id":54535,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4214/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158858,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4214/report-thumb.jpg"}],"country":"United States","state":"Florida","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -82.705078125,\n 24.966140159912975\n ],\n [\n -79.6728515625,\n 24.966140159912975\n ],\n [\n -79.6728515625,\n 27.15692045688088\n ],\n [\n -82.705078125,\n 27.15692045688088\n ],\n [\n -82.705078125,\n 24.966140159912975\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db6999b3","contributors":{"authors":[{"text":"Merritt, M. L.","contributorId":47401,"corporation":false,"usgs":true,"family":"Merritt","given":"M.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":195069,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meyer, F.W.","contributorId":25150,"corporation":false,"usgs":true,"family":"Meyer","given":"F.W.","email":"","affiliations":[],"preferred":false,"id":195067,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sonntag, W. H.","contributorId":106127,"corporation":false,"usgs":true,"family":"Sonntag","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":195070,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fitzpatrick, D. J.","contributorId":33313,"corporation":false,"usgs":true,"family":"Fitzpatrick","given":"D. J.","affiliations":[],"preferred":false,"id":195068,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":43359,"text":"ofr83555 - 1983 - Land use and land cover and associated maps for Austin, Texas","interactions":[],"lastModifiedDate":"2012-02-02T00:10:09","indexId":"ofr83555","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-555","title":"Land use and land cover and associated maps for Austin, Texas","language":"ENGLISH","doi":"10.3133/ofr83555","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, Land use and land cover and associated maps for Austin, Texas: U.S. Geological Survey Open-File Report 83-555, maps :photocopy ;44 x 77 cm., https://doi.org/10.3133/ofr83555.","productDescription":"maps :photocopy ;44 x 77 cm.","costCenters":[],"links":[{"id":162513,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b1728","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531135,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":18741,"text":"ofr82648 - 1983 - Water resources of the Tulalip Indian Reservation, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:07:24","indexId":"ofr82648","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-648","title":"Water resources of the Tulalip Indian Reservation, Washington","docAbstract":"Water will play a significant role in the future development of the Tulalip Indian Reservation. Ground-water resources are sufficient to supply several times the 1978 population. Potential problems associated with increased ground-water development are saltwater encroachment in the coastal areas and septic-tank contamination of shallow aquifers. There are sufficient good-quality surface-water resources to allow for significant expansion of the tribe)s fisheries activities. \r\n\r\nThe tribal well field is the only place where the ground-water system has been stressed) resulting in declining water levels (1,5 feet per year), The well field has a useful life of at least 1.5-20 years, This can be increased by drilling additional wells to expand the present well field, \r\n\r\nInflow of water to the reservation is in the form of precipitation (103 cubic feet per second) ft3/s)) surface-water inflow (13 ft3/s)) and ground-water inflow (4 ft3/s), Outflow is as evapotranspiration (62 ft3/s)) surface-water outflow (40 ft3/s)) and ground-water outflow (18 ft3/s), Total inflow and outflow are equal (120 ft3/s). \r\n\r\nGround water is generally suitable for domestic use without treatment) but a serious quality problem is the presence of coliform bacteria in some shallow wells, High values of turbidity and color and large concentrations of iron and manganese are common problems regarding the esthetic quality of the water, In a few places, large concentrations of chloride and dissolved solids indicate the possibility of saltwater encroachment, but no ongoing trend has been identified, \r\n\r\nSurface waters have been observed to contain undesirably high concentrations of total phosphorus and total and fecal-coliform bacteria) and to have temperatures too high for fish-rearing. The concentration of nutrients appears to be related to flow conditions. Nitrate and total nitrogen are greater in wet-season runoff than during low-flow periods) and total phosphorus shows an inverse relationship. Total phosphorus and ammonia concentrations are greatest in dry-season storm runoff. Generally) surface-water quality is adequate for fish-rearing and (with treatment) for public supply,","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82648","usgsCitation":"Drost, B., 1983, Water resources of the Tulalip Indian Reservation, Washington: U.S. Geological Survey Open-File Report 82-648, vii, 106 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82648.","productDescription":"vii, 106 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":150951,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0648/report-thumb.jpg"},{"id":48100,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0648/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":48101,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0648/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f1e4b07f02db5ee3e2","contributors":{"authors":[{"text":"Drost, B. W.","contributorId":38526,"corporation":false,"usgs":true,"family":"Drost","given":"B. W.","affiliations":[],"preferred":false,"id":179657,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29911,"text":"wri834002 - 1983 - Ground-water contamination at Wurtsmith Air Force Base, Michigan","interactions":[],"lastModifiedDate":"2017-01-25T14:09:18","indexId":"wri834002","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4002","title":"Ground-water contamination at Wurtsmith Air Force Base, Michigan","docAbstract":"A sand and gravel aquifer of glacial origin underlies Wurtsmith Air Force Base in northeastern lower Michigan. The aquifer overlies a thick clay layer at an average depth of 65 feet. The water table is about 10 feet below land surface in the western part of the Base and about 25 feet below land surface in the eastern part. A ground-water divide cuts diagonally across the Base from northwest to southeast. South of the divide, ground water flows to the Au Sable River; north of the divide, it flows to Van Etten Creek and Van Etten Lake. Mathematical models were used to aid in calculating rates of groundwater flow. Rates range from about 0.8 feet per day in the eastern part of the Base to about 0.3 feet per day in the western part. Models also were used as an aid in making decisions regarding purging of contaminated water from the aquifer.
In 1977, trichloroethylene was detected in the Air Force Base water-supply system. It had leaked from a buried storage tank near Building 43 in the southeastern part of the Base and moved northeastward under the influence of the natural ground-water gradient and the pumping of Base water-supply wells. In the most highly contaminated part of the plume, concentrations are greater than 1,000 micrograms per liter. Current purge pumping is removing some of the trichloroethylene, and seems to have arrested its eastward movement. Pumping of additional purge wells could increase the rate of removal.
Trichloroethylene has also been detected in ground water in the vicinity of the Base alert apron, where a plume from an unknown source extends northeastward off Base. A smaller, less well-defined area of contamination also occurs just north of the larger plume. Trichloroethylene, identified near the waste-treatment plant, seepage lagoons, and the northern landfill area, is related to activities and operations in these areas. Dichloroethylene and trichloroethylene occur in significant quantities westward of Building 43, upgradient from the major spill site. Benzene, indicative of ground-water contamination by a fuel substance, occurs in an area northeast of the bulk-fuel storage area. Analysis of a variety of chemical, physical, and biologic characteristics of water on the Base indicate that there is a measurable affect on ground-water quality from landfills, the seepage lagoon, and the waste-treatment plant.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/wri834002","collaboration":"Prepared in cooperation with the U.S. Air Force","usgsCitation":"Stark, J., Cummings, T., and Twenter, F.R., 1983, Ground-water contamination at Wurtsmith Air Force Base, Michigan: U.S. Geological Survey Water-Resources Investigations Report 83-4002, Document: ix, 93 p.; Plate: 41.58 x 35.42 inches, https://doi.org/10.3133/wri834002.","productDescription":"Document: ix, 93 p.; Plate: 41.58 x 35.42 inches","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":58728,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4002/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58729,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4002/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119514,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4002/report-thumb.jpg"}],"country":"United States","state":"Michigan","otherGeospatial":"Wurtsmith Air Force Base","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -83.416667,\n 44.483333\n ],\n [\n -83.416667,\n 44.425\n ],\n [\n -83.325,\n 44.425\n ],\n [\n -83.325,\n 44.483333\n ],\n [\n -83.416667,\n 44.483333\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d05d","contributors":{"authors":[{"text":"Stark, J. R.","contributorId":100406,"corporation":false,"usgs":true,"family":"Stark","given":"J. R.","affiliations":[],"preferred":false,"id":202340,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cummings, T. R.","contributorId":104082,"corporation":false,"usgs":true,"family":"Cummings","given":"T. R.","affiliations":[],"preferred":false,"id":202341,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Twenter, F. R.","contributorId":81080,"corporation":false,"usgs":true,"family":"Twenter","given":"F.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":202339,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":18478,"text":"ofr83542 - 1983 - Sources and mechanisms of recharge for ground water in the west-central Amargosa Desert, Nevada– A geochemical interpretation","interactions":[{"subject":{"id":18478,"text":"ofr83542 - 1983 - Sources and mechanisms of recharge for ground water in the west-central Amargosa Desert, Nevada– A geochemical interpretation","indexId":"ofr83542","publicationYear":"1983","noYear":false,"title":"Sources and mechanisms of recharge for ground water in the west-central Amargosa Desert, Nevada– A geochemical interpretation"},"predicate":"SUPERSEDED_BY","object":{"id":5784,"text":"pp712F - 1985 - Sources and mechanisms of recharge for ground water in the west-central Amargosa Desert, Nevada; a geochemical interpretation","indexId":"pp712F","publicationYear":"1985","noYear":false,"chapter":"F","title":"Sources and mechanisms of recharge for ground water in the west-central Amargosa Desert, Nevada; a geochemical interpretation"},"id":1}],"supersededBy":{"id":5784,"text":"pp712F - 1985 - Sources and mechanisms of recharge for ground water in the west-central Amargosa Desert, Nevada; a geochemical interpretation","indexId":"pp712F","publicationYear":"1985","noYear":false,"title":"Sources and mechanisms of recharge for ground water in the west-central Amargosa Desert, Nevada; a geochemical interpretation"},"lastModifiedDate":"2021-12-09T21:45:56.659916","indexId":"ofr83542","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-542","title":"Sources and mechanisms of recharge for ground water in the west-central Amargosa Desert, Nevada– A geochemical interpretation","docAbstract":"Ground water in the west-central Amargosa Desert, Nevada, was recharged primarily by overland flow of snowmelt in or near the present-day stream channels, rather than by subsurface flow from highland recharge areas to the north. Geochemical arguments, including reaction mechanisms, are used to support these findings. Carbon-, hydrogen-, and oxygen-isotope data show that much of the recharge in the area occurred during late Wisconsin time. Absence of ground-water recharge prior to late Pleistocene is considered to indicate that either climatic conditions were unfavorable for recharge or that ground-water velocities were such that they transported this earlier recharge away from the study aea. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83542","usgsCitation":"Claassen, H., 1983, Sources and mechanisms of recharge for ground water in the west-central Amargosa Desert, Nevada– A geochemical interpretation: U.S. Geological Survey Open-File Report 83-542, vi, 66 p., https://doi.org/10.3133/ofr83542.","productDescription":"vi, 66 p.","costCenters":[],"links":[{"id":392702,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14096.htm"},{"id":47833,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0542/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":153097,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0542/report-thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Amargosa Desert","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -116.682,\n 36.25\n ],\n [\n -116.318,\n 36.25\n ],\n [\n -116.318,\n 36.872\n ],\n [\n -116.682,\n 36.872\n ],\n [\n -116.682,\n 36.25\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e76bc","contributors":{"authors":[{"text":"Claassen, H.C.","contributorId":74028,"corporation":false,"usgs":true,"family":"Claassen","given":"H.C.","affiliations":[],"preferred":false,"id":179203,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":20547,"text":"ofr8460 - 1983 - Flood-flow characteristics of Lullwater Creek from Ponce de Leon Avenue to proposed Presidential Parkway, Atlanta, Georgia","interactions":[],"lastModifiedDate":"2016-12-14T13:52:13","indexId":"ofr8460","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"84-60","title":"Flood-flow characteristics of Lullwater Creek from Ponce de Leon Avenue to proposed Presidential Parkway, Atlanta, Georgia","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8460","usgsCitation":"Price, M., 1983, Flood-flow characteristics of Lullwater Creek from Ponce de Leon Avenue to proposed Presidential Parkway, Atlanta, Georgia: U.S. Geological Survey Open-File Report 84-60, v, 22 p. :ill., map ;29 cm., https://doi.org/10.3133/ofr8460.","productDescription":"v, 22 p. :ill., map ;29 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":50066,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0060/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":153213,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0060/report-thumb.jpg"},{"id":50065,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0060/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Georgia","city":"Atlanta","otherGeospatial":"Lullwater Creek","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -84.34513092041016,\n 33.75445967067027\n ],\n [\n -84.34513092041016,\n 33.807964383611484\n ],\n [\n -84.30951118469238,\n 33.807964383611484\n ],\n [\n -84.30951118469238,\n 33.75445967067027\n ],\n [\n -84.34513092041016,\n 33.75445967067027\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df79e","contributors":{"authors":[{"text":"Price, McGlone","contributorId":42964,"corporation":false,"usgs":true,"family":"Price","given":"McGlone","email":"","affiliations":[],"preferred":false,"id":182825,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":30331,"text":"wri824077 - 1983 - Evaluation of water levels in major aquifers of the New Jersey coastal plain, 1978","interactions":[],"lastModifiedDate":"2012-02-02T00:08:51","indexId":"wri824077","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-4077","title":"Evaluation of water levels in major aquifers of the New Jersey coastal plain, 1978","docAbstract":"Increased withdrawals from the major artesian aquifers that underlie the New Jersey Coastal Plain have caused water-level declines and large regional cones of depression. These cones of depression are delineated on detailed potentiometric surface maps produced from water-level data collected in the field in 1978. Water levels for 1978 are compared with those from 1970 or 1973, and water-level changes are evaluated and compared with hydrographs from observation wells. The Potomac-Raritan-Magothy aquifer system is divided into regionally extensive lower and upper aquifers. These aquifers have large cones of depression centered in Camden, Middlesex, and Monmouth Counties. Water levels declined 5 to 20 feet in these areas between 1973 and 1978. Deep cones of depression in coastal Monmouth and Ocean Counties in the Englishtown and Wenonah-Mount Laurel aquifers are similar in location and shape, due to a good hydraulic connection between these aquifers. Water levels declined 2 to 31 feet in the Englishtown aquifer and 12 to 26 feet in the Wenonah-Mount Laurel aquifer between 1973 and 1978. Water levels in the Atlantic City 800-foot sand of the Kirkwood Formation define an extensive elongated cone of depression centered near Margate, Atlantic County. Head changes ranged from a decline of 4 feet to a recovery of 9 feet during 1970-78. The lowest heads in the Cohansey Sand were about 26 feet below sea level at Cape May, Cape May County, and less than 0.5 miles from salty ground water. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824077","usgsCitation":"Walker, R., 1983, Evaluation of water levels in major aquifers of the New Jersey coastal plain, 1978: U.S. Geological Survey Water-Resources Investigations Report 82-4077, vi, 62 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824077.","productDescription":"vi, 62 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123582,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4077/report-thumb.jpg"},{"id":59124,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4077/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59125,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4077/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59126,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4077/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59127,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4077/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59128,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4077/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59129,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4077/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db667295","contributors":{"authors":[{"text":"Walker, R.L.","contributorId":27009,"corporation":false,"usgs":true,"family":"Walker","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":203073,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8051,"text":"ofr80594 - 1983 - Quality of rivers of the United States, 1976 water year--based on the National Stream Quality Accounting Network (NASQAN)","interactions":[],"lastModifiedDate":"2012-02-02T00:06:04","indexId":"ofr80594","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"80-594","title":"Quality of rivers of the United States, 1976 water year--based on the National Stream Quality Accounting Network (NASQAN)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr80594","usgsCitation":"Britton, L.J., Goddard, K.E., and Briggs, J.C., 1983, Quality of rivers of the United States, 1976 water year--based on the National Stream Quality Accounting Network (NASQAN): U.S. Geological Survey Open-File Report 80-594, vi, 423 p. :ill., maps (some col.) ;28 cm., https://doi.org/10.3133/ofr80594.","productDescription":"vi, 423 p. :ill., maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":140578,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0594/report-thumb.jpg"},{"id":35625,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0594/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db654a3f","contributors":{"authors":[{"text":"Britton, Linda J.","contributorId":72780,"corporation":false,"usgs":true,"family":"Britton","given":"Linda","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":157057,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goddard, Kimball E.","contributorId":24348,"corporation":false,"usgs":true,"family":"Goddard","given":"Kimball","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":157055,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Briggs, John C.","contributorId":24349,"corporation":false,"usgs":true,"family":"Briggs","given":"John","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":157056,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":9184,"text":"ofr80678 - 1983 - Groundwater resources of the Dallas-Monmouth area, Polk, Benton, and Marion Counties, Oregon","interactions":[],"lastModifiedDate":"2022-08-10T14:00:53.89564","indexId":"ofr80678","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"80-678","title":"Groundwater resources of the Dallas-Monmouth area, Polk, Benton, and Marion Counties, Oregon","docAbstract":"The Dallas-Monmouth area is in the west-central Willamette Valley of western Oregon. It comprises a total of about 400 square miles in Polk, Benton, and Marion Counties. Tertiary consolidated rocks underlie the entire area. These rocks include marine sandstone, siltstone, shale, tuff, basalt, and gabbro. In the lowlands, the consolidated rocks are overlain by unconsolidated deposits of clay, silt, sand, and gravel which reach a maximum thickness of about 125 feet locally. The consolidated rocks generally are poor water-bearing formations and yield only small quantities of ground water to wells. From 1956 to 1976, about 6 percent of all wells completed in basalt and 14 percent of those completed in marine sedimentary rocks were reported to be \"dry holes.\" The median yield of wells completed in the consolidated rocks was less than 10 gallons per minute, and the maximum reported yield was 200 gallons per minute. Shallow ground water in the consolidated rocks is generally of good quality, but with increasing depth in these rocks the water contains increasing concentrations of dissolved minerals. It is estimated that about 5 percent of all the wells completed in the consolidated rocks yield poor-quality water. The best water-bearing units are sand-and-gravel beds in the unconsolidated deposits. Near Independence, the sand-and-gravel beds are hydraulically continuous and exceed a saturated thickness of 10 feet over an area covering several tens of square miles chiefly within the Willamette River flood plain. Properly constructed wells in these deposits can generally obtain yields of 100 to 500 gallons per minute, and large quantities of additional ground water can be developed from this source. Outside the above area, sand-and-gravel beds generally are less than 10 feet thick, lenticular in shape, local in extent, and generally yield less than 30 gallons per minute to wells. Sand-and-gravel beds probably are absent in the Baskett Slough drainage basin, in the E. E. Wilson Wildlife Management area, and in the Luckiamute and Little Luckiamute River valleys upstream from the U.S. Highway 99W bridge.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80678","collaboration":"Prepared in cooperation with The United States Department of the Interior, Geological Survey","usgsCitation":"Gonthier, J.B., 1983, Groundwater resources of the Dallas-Monmouth area, Polk, Benton, and Marion Counties, Oregon: U.S. Geological Survey Open-File Report 80-678, Report: vi, 50 p.; 2 Plates: 23.18 x 34.68 inches and 18.78 x 12.85 inches, https://doi.org/10.3133/ofr80678.","productDescription":"Report: vi, 50 p.; 2 Plates: 23.18 x 34.68 inches and 18.78 x 12.85 inches","costCenters":[],"links":[{"id":405072,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11734.htm","linkFileType":{"id":5,"text":"html"}},{"id":405018,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0678/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":405017,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0678/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141630,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0678/report-thumb.jpg"},{"id":405016,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0678/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon","county":"Benton County, Marion County, Polk County","otherGeospatial":"Dallas-Monmouth area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -123.35998535156249,\n 44.79937794671695\n ],\n [\n -123.12927246093751,\n 44.79937794671695\n ],\n [\n -123.12927246093751,\n 44.97451370563983\n ],\n [\n -123.35998535156249,\n 44.97451370563983\n ],\n [\n -123.35998535156249,\n 44.79937794671695\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a94e4b07f02db6589aa","contributors":{"authors":[{"text":"Gonthier, Joseph B.","contributorId":74350,"corporation":false,"usgs":true,"family":"Gonthier","given":"Joseph","email":"","middleInitial":"B.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":159240,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7223,"text":"ofr83274 - 1983 - Hydrogeologic data from parts of the Denver basin, Colorado","interactions":[],"lastModifiedDate":"2022-08-18T18:13:45.798042","indexId":"ofr83274","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-274","title":"Hydrogeologic data from parts of the Denver basin, Colorado","docAbstract":"This report presents hydrogeologic data collected and compiled during 1956-81 as part of a comprehensive hydrogeologic data collected and compiled during 1956-81 as part of a comprehensive hdryogeologic investigation of the Denver basin, Colorado, by the U.S. Geological Survey in cooperation with the Colorado Department of Natural Resources, Division of Water Resources, Office of the State Engineer. The data, in tabular and graphic form, consist of records for 870 wells which include water-level data for 158 wells and water-quality analyses for 561 wells; geophysical logs from three wells which include resistivity, self potential, and natural gamma logs; and gain-and-loss data of streamflow measured at 54 sites.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83274","usgsCitation":"Major, T.J., Robson, S.G., Romero, J.C., and Zawistowski, S., 1983, Hydrogeologic data from parts of the Denver basin, Colorado: U.S. Geological Survey Open-File Report 83-274, Report: iv, 425 p.; 3 Plates: 23.94 × 36.08 inches or smaller, https://doi.org/10.3133/ofr83274.","productDescription":"Report: iv, 425 p.; 3 Plates: 23.94 × 36.08 inches or smaller","costCenters":[],"links":[{"id":140680,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0274/report-thumb.jpg"},{"id":34617,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0274/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34618,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0274/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34619,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0274/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34620,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0274/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":405315,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13959.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Colorado","otherGeospatial":"Denver basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -105.281,\n 38.639\n ],\n [\n -103.719,\n 38.639\n ],\n [\n -103.719,\n 40.432\n ],\n [\n -105.281,\n 40.432\n ],\n [\n -105.281,\n 38.639\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4fe4b07f02db628a04","contributors":{"authors":[{"text":"Major, T. J.","contributorId":18762,"corporation":false,"usgs":true,"family":"Major","given":"T.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":154820,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robson, S. G.","contributorId":97102,"corporation":false,"usgs":true,"family":"Robson","given":"S.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":154823,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Romero, J. C.","contributorId":58635,"corporation":false,"usgs":false,"family":"Romero","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":154822,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Zawistowski, Stanley","contributorId":52959,"corporation":false,"usgs":true,"family":"Zawistowski","given":"Stanley","email":"","affiliations":[],"preferred":false,"id":154821,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":65659,"text":"i1555 - 1983 - Controlled photomosaic of the Phaethontis North-central Quadrangle of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:18","indexId":"i1555","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"1555","subseriesTitle":"NONE","title":"Controlled photomosaic of the Phaethontis North-central Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i1555","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, Controlled photomosaic of the Phaethontis North-central Quadrangle of Mars (Revised in April 1983): U.S. Geological Survey IMAP 1555, 1 photomosaic ;53 x 59 cm., on sheet 86 x 67 cm., https://doi.org/10.3133/i1555.","productDescription":"1 photomosaic ;53 x 59 cm., on sheet 86 x 67 cm.","costCenters":[],"links":[{"id":251387,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1555/report.pdf","size":"24","linkFileType":{"id":1,"text":"pdf"}},{"id":251388,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1555/plate-1.pdf","size":"11093","linkFileType":{"id":1,"text":"pdf"}},{"id":252248,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1555/report-thumb.jpg"}],"scale":"2000000","edition":"Revised in April 1983","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adde4b07f02db686da4","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":534047,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29860,"text":"wri834066 - 1983 - Exploratory drilling and aquifer testing at the Kipahulu District, Haleakala National Park, Maui, Hawaii","interactions":[],"lastModifiedDate":"2023-01-09T20:45:17.860682","indexId":"wri834066","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4066","title":"Exploratory drilling and aquifer testing at the Kipahulu District, Haleakala National Park, Maui, Hawaii","docAbstract":"An exploratory well, located at 388 feet above sea level in Kipahulu Valley on Maui, Hawaii, was completed and tested in October 1980. The 410-foot well penetrates a series of very dense basaltic lava flows of the Hana Formation. At an elevation of 10 feet above mean sea level, the well penetrated a water-bearing zone of permeable basaltic rock. Water from this zone had a head of about 76 feet above sea level. In October of 1980, the well was pump tested for 9 hours at various discharge rates up to 350 gallons per minute with a maximum drawdown of about 12 feet. Based on the test data, the well should produce water at a rate of 200 gallons per minute with a drawdown of less than 3 feet. The water level in the well was continuously monitored from October 1980 to mid-November 1981, during which period a maximum decline of 20 feet was recorded. Water level fluctuations in the well can be correlated to the flow in nearby Palikea Stream. The long-term water level in the well should stabilize at about 75 feet above sea level. Water quality was excellent. The total dissolved-solids content was 49 milligrams per liter and the chloride content was 4.2 milligrams per liter.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834066","usgsCitation":"Souza, W.R., 1983, Exploratory drilling and aquifer testing at the Kipahulu District, Haleakala National Park, Maui, Hawaii: U.S. Geological Survey Water-Resources Investigations Report 83-4066, v, 26 p., https://doi.org/10.3133/wri834066.","productDescription":"v, 26 p.","costCenters":[],"links":[{"id":58671,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4066/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123551,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4066/report-thumb.jpg"},{"id":411586,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35701.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Hawaii","otherGeospatial":"Haleakala National Park","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -156.25717163085938,\n 20.580081709180345\n ],\n [\n -156.01547241210938,\n 20.580081709180345\n ],\n [\n -156.01547241210938,\n 20.78693059257028\n ],\n [\n -156.25717163085938,\n 20.78693059257028\n ],\n [\n -156.25717163085938,\n 20.580081709180345\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f78f4","contributors":{"authors":[{"text":"Souza, W. R.","contributorId":102114,"corporation":false,"usgs":true,"family":"Souza","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":202254,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":41747,"text":"ofr83150 - 1983 - Approximate water-level changes in wells in the Chicot and Evangeline aquifers, 1977-83 and 1982-83 and measured compaction, 1973-83 in Harris and Galvestan counties, Texas","interactions":[],"lastModifiedDate":"2016-08-11T15:37:32","indexId":"ofr83150","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-150","title":"Approximate water-level changes in wells in the Chicot and Evangeline aquifers, 1977-83 and 1982-83 and measured compaction, 1973-83 in Harris and Galvestan counties, Texas","docAbstract":"This report, which was prepared in cooperation with the City of Hoston, the Harris-Galveston Coastal Subsidence District, and the Texas Department of Water Resources, presents data on water-level changes in the Chicot and Evangeline aquifers.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83150","usgsCitation":"Strause, J.L., and Ranzau, C., 1983, Approximate water-level changes in wells in the Chicot and Evangeline aquifers, 1977-83 and 1982-83 and measured compaction, 1973-83 in Harris and Galvestan counties, Texas: U.S. Geological Survey Open-File Report 83-150, 7 p., https://doi.org/10.3133/ofr83150.","productDescription":"7 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":176676,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0150/report-thumb.jpg"},{"id":79465,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0150/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db67a152","contributors":{"authors":[{"text":"Strause, Jeffrey L.","contributorId":61420,"corporation":false,"usgs":true,"family":"Strause","given":"Jeffrey","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":225470,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ranzau, C.E. Jr.","contributorId":41831,"corporation":false,"usgs":true,"family":"Ranzau","given":"C.E.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":225469,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":18624,"text":"ofr8334 - 1983 - Selected ground-water data in parts of Gilliam, Morrow, and Umatilla counties, Oregon","interactions":[],"lastModifiedDate":"2017-02-07T09:29:21","indexId":"ofr8334","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-34","title":"Selected ground-water data in parts of Gilliam, Morrow, and Umatilla counties, Oregon","docAbstract":"Over the last 20 years there has been a shift from dryland to irrigated agriculture in parts of Gilliam, Morrow, and Umatilla Counties in northeastern Oregon. Some irrigation water used in this area obtained from surface sources, but a significant amount is obtained from wells. The principal aquifer in the area is the Columbia River Basalt Group. Wells in the basalt are commonly drilled to depths of 500 to 1,200 ft and many produce more than 1,000 gal/min. A cooperative ground-water modeling study by the U.S. Geological Survey and Oregon Water Resources Department has resulted in the compilation of data from drillers logs and well inspections for wells completed in the basalt aquifer. Water-level measurements have been made in some wells in the area since the 1950's. The wells with longest periods of record are those that are part of a Statewide network of observation wells measured by the U. S. Geological Survey and Oregon Water Resources Department. This report includes a table of well information, representative hydrographs, and well location maps. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8334","usgsCitation":"Smith, P., Collins, C.A., and Olson, L., 1983, Selected ground-water data in parts of Gilliam, Morrow, and Umatilla counties, Oregon: U.S. Geological Survey Open-File Report 83-34, iv, 48 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr8334.","productDescription":"iv, 48 p. :ill., maps ;28 cm.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":47964,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0034/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":47966,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0034/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":151651,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0034/report-thumb.jpg"},{"id":47965,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0034/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9687","contributors":{"authors":[{"text":"Smith, P.A.","contributorId":86795,"corporation":false,"usgs":true,"family":"Smith","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":179449,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Collins, C. A.","contributorId":43731,"corporation":false,"usgs":true,"family":"Collins","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":179448,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Olson, L.J.","contributorId":16436,"corporation":false,"usgs":true,"family":"Olson","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":179447,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":8116,"text":"ofr83139 - 1983 - Hydrologic data from the Tamarack Wildlife Area and vicinity, Logan County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:05","indexId":"ofr83139","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-139","title":"Hydrologic data from the Tamarack Wildlife Area and vicinity, Logan County, Colorado","docAbstract":"Hydrologic data were collected from the Tamarack Ranch Wildlife area and vicinity near Crook, Colo., during the period September 1979 to August 1981. These data will aid in the analysis of the effects of proposed water-development projects on the hydrologic system of the wildlife area. The data collected included a reconnaissance evaluation of specific conductance, a 24-hour sampling of air and water temperature at 6 sites, and periodic measurements of water levels, temperature, and specific conductance at 57 sites.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83139","usgsCitation":"Burns, A.W., 1983, Hydrologic data from the Tamarack Wildlife Area and vicinity, Logan County, Colorado: U.S. Geological Survey Open-File Report 83-139, 126 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83139.","productDescription":"126 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":140649,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0139/report-thumb.jpg"},{"id":35719,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0139/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35720,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0139/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35721,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0139/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db6076dc","contributors":{"authors":[{"text":"Burns, Alan W.","contributorId":41419,"corporation":false,"usgs":true,"family":"Burns","given":"Alan","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":157177,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}