The investigation of the ground-water resources of Oklahoma by the U.S. Geological Survey in cooperation with the Oklahoma Water Resources Board includes a continuing program to collect on a systematic basis records of water levels in selected observation wells. These water-level records: (1) provide an index to available ground-water supplies; (2) facilitate the prediction of trends in water levels that will indicate likely changes in storage; (3) aid in the prediction of the base flow of streams; (4) provide information for use in basic research; and (5) provide long-time continuous records of fluctuations of water levels in representative wells, These selected records also serve as a framework to which other types of hydrologic data may be related.
Prior to 1956, measurements of water levels in observation wells in Oklahoma were included in water-supply papers published annually by the U.S. Geological Survey (table 1). Beginning with the 1956 calendar year, however, Federal water-level reports will contain only records of a selected network of observation wells, and will be published by the U.S. Geological Survey at 5-year intervals. The first of this series, for the 1956-59 period has recently been published.
This report has been prepared primarily to present water-level records of wells not included in the Federal network. However, for the sake of completeness it includes water-level records of Federal wells that either have been or will be published in Water-Supply Papers since 1955. This report, which contains water-level records for the 5-year period (1956-60), is the first of a series presenting water-level records for all permanent observation wells in Oklahoma. It is planned that future water-level reports will be published at 2-year intervals.
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Ray","contributorId":20722,"corporation":false,"usgs":true,"family":"Cummings","given":"T.","email":"","middleInitial":"Ray","affiliations":[],"preferred":false,"id":257650,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":14,"text":"wsp1734 - 1963 - Compilation of records of surface waters of the United States, October 1950 to September 1960: Part 10. The Great Basin","interactions":[],"lastModifiedDate":"2024-03-05T22:41:00.563745","indexId":"wsp1734","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1734","title":"Compilation of records of surface waters of the United States, October 1950 to September 1960: Part 10. The Great Basin","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1734","usgsCitation":"Hendricks, E.L., Hofmann, W., Phillips, K.N., Travis, W.I., Wilson, M.T., Harris, E., and Jibson, W., 1963, Compilation of records of surface waters of the United States, October 1950 to September 1960: Part 10. The Great Basin: U.S. Geological Survey Water Supply Paper 1734, Report: ix, 318 p.; 1 Plate: 24.00 x 34.60 inches, https://doi.org/10.3133/wsp1734.","productDescription":"Report: ix, 318 p.; 1 Plate: 24.00 x 34.60 inches","costCenters":[],"links":[{"id":110010,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24918.htm","linkFileType":{"id":5,"text":"html"},"description":"24918"},{"id":24619,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1734/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24618,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1734/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":136023,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1734/report-thumb.jpg"}],"country":"United States","state":"Arizona, Idaho, Nevada, New Mexico, Oregon, Utah","otherGeospatial":"Great Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -110.667,\n 44.25\n ],\n [\n -121.5,\n 44.25\n ],\n [\n -121.5,\n 32.617\n ],\n [\n -110.667,\n 32.617\n ],\n [\n -110.667,\n 44.25\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1de4b07f02db6a9a09","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":141817,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hofmann, Walter","contributorId":30604,"corporation":false,"usgs":true,"family":"Hofmann","given":"Walter","email":"","affiliations":[],"preferred":false,"id":896006,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Phillips, K. N.","contributorId":36806,"corporation":false,"usgs":true,"family":"Phillips","given":"K.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":896007,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Travis, W. I.","contributorId":47445,"corporation":false,"usgs":true,"family":"Travis","given":"W.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":896008,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wilson, M. T.","contributorId":102116,"corporation":false,"usgs":true,"family":"Wilson","given":"M.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":896009,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Harris, E. E.","contributorId":24328,"corporation":false,"usgs":true,"family":"Harris","given":"E. E.","affiliations":[],"preferred":false,"id":896010,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Jibson, W.N.","contributorId":27928,"corporation":false,"usgs":true,"family":"Jibson","given":"W.N.","email":"","affiliations":[],"preferred":false,"id":896011,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":2058,"text":"wsp1475O - 1963 - Hydrologic and geologic reconnaissance of Pinto Basin, Joshua Tree National Monument, Riverside County, California","interactions":[{"subject":{"id":23112,"text":"ofr5672 - 1956 - A brief hydrologic and geologic reconnaissance of Pinto Basin, Joshua Tree National Monument, Riverside County, California","indexId":"ofr5672","publicationYear":"1956","noYear":false,"title":"A brief hydrologic and geologic reconnaissance of Pinto Basin, Joshua Tree National Monument, Riverside County, California"},"predicate":"SUPERSEDED_BY","object":{"id":2058,"text":"wsp1475O - 1963 - Hydrologic and geologic reconnaissance of Pinto Basin, Joshua Tree National Monument, Riverside County, California","indexId":"wsp1475O","publicationYear":"1963","noYear":false,"chapter":"O","title":"Hydrologic and geologic reconnaissance of Pinto Basin, Joshua Tree National Monument, Riverside County, California"},"id":1},{"subject":{"id":52115,"text":"ofr6090 - 1960 - Summary of hydrologic conditions at Joshua Tree National Monument, Riverside County, California, 1956-1959","indexId":"ofr6090","publicationYear":"1960","noYear":false,"title":"Summary of hydrologic conditions at Joshua Tree National Monument, Riverside County, California, 1956-1959"},"predicate":"SUPERSEDED_BY","object":{"id":2058,"text":"wsp1475O - 1963 - Hydrologic and geologic reconnaissance of Pinto Basin, Joshua Tree National Monument, Riverside County, California","indexId":"wsp1475O","publicationYear":"1963","noYear":false,"chapter":"O","title":"Hydrologic and geologic reconnaissance of Pinto Basin, Joshua Tree National Monument, Riverside County, California"},"id":2}],"lastModifiedDate":"2023-01-06T22:49:59.861671","indexId":"wsp1475O","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1475","chapter":"O","displayTitle":"Hydrologic and Geologic Reconnaissance of Pinto Basin, Joshua Tree National Monument, Riverside County, California","title":"Hydrologic and geologic reconnaissance of Pinto Basin, Joshua Tree National Monument, Riverside County, California","docAbstract":"Pinto basin, in the north-central part of Riverside County, Calif., is a typical desert valley formed by downfaulting along several major fault zones. The valley is filled with alluvium, and ground water in the alluvium discharges as subsurface outflow through an alluvium-filled gap at the east end of the valley. Occasionally surface water from cloudburst floods also discharges in a wash through the gap at the east end of the valley.\r\n\r\nA northeastward extension of the major fault along the south side of the valley acts as a barrier to the discharge of ground water from the valley. The average ground-water gradient is less than 1 foot per mile across the main part of the valley above this barrier, but the water level drops abruptly across the fault. The ground-water storage capacity of the uppermost 100 feet of saturated alluvium beneath the central valley area is estimated to be about 230,000 acre-feet. All this water in storage occurs at depths greater than 95 feet below the land surface and cannot be reached by plants or animals. During 1959 virtually all the water pumped in the area was withdrawn from storage. However, the quantity of water pumped is small in relation to the total quantity in storage. Except for a small decline in head, no evidence indicates that the pumping will greatly impair the yield for many years or cause the water to deteriorate in quality.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Hydrology of the Public Domain","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1475O","usgsCitation":"Kunkel, F., 1963, Hydrologic and geologic reconnaissance of Pinto Basin, Joshua Tree National Monument, Riverside County, California: U.S. Geological Survey Water Supply Paper 1475, Report: iii, 24 p.; 1 Plate: 30.90 x 20.80 inches, https://doi.org/10.3133/wsp1475O.","productDescription":"Report: iii, 24 p.; 1 Plate: 30.90 x 20.80 inches","startPage":"537","endPage":"561","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":27600,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1475o/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27599,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1475o/plate-28.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138561,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1475o/report-thumb.jpg"}],"scale":"62500","country":"United States","state":"California","county":"Riverside County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -115.733,\n 33.9\n ],\n [\n -115.733,\n 34\n ],\n [\n -115.333,\n 34\n ],\n [\n -115.333,\n 33.9\n ],\n [\n -115.733,\n 33.9\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db6118db","contributors":{"authors":[{"text":"Kunkel, Fred","contributorId":47766,"corporation":false,"usgs":true,"family":"Kunkel","given":"Fred","email":"","affiliations":[],"preferred":false,"id":144611,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":44061,"text":"ofr63106 - 1963 - Water-resources investigations and reports in the Susquehanna River basin; conducted by the United States Geological Survey, Water Resources Division","interactions":[{"subject":{"id":44061,"text":"ofr63106 - 1963 - Water-resources investigations and reports in the Susquehanna River basin; conducted by the United States Geological Survey, Water Resources Division","indexId":"ofr63106","publicationYear":"1963","noYear":false,"title":"Water-resources investigations and reports in the Susquehanna River basin; conducted by the United States Geological Survey, Water Resources Division"},"predicate":"SUPERSEDED_BY","object":{"id":70046297,"text":"70046297 - 1963 - Water resources investigations in the Susquehanna River basin","indexId":"70046297","publicationYear":"1963","noYear":false,"title":"Water resources investigations in the Susquehanna River basin"},"id":1}],"supersededBy":{"id":70046297,"text":"70046297 - 1963 - Water resources investigations in the Susquehanna River basin","indexId":"70046297","publicationYear":"1963","noYear":false,"title":"Water resources investigations in the Susquehanna River basin"},"lastModifiedDate":"2013-06-05T14:14:02","indexId":"ofr63106","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"63-106","title":"Water-resources investigations and reports in the Susquehanna River basin; conducted by the United States Geological Survey, Water Resources Division","language":"ENGLISH","doi":"10.3133/ofr63106","issn":"ma","usgsCitation":"Page, L.V., Water Resources Division, U.S. Geological Survey, and Seaber, P.R., 1963, Water-resources investigations and reports in the Susquehanna River basin; conducted by the United States Geological Survey, Water Resources Division: U.S. Geological Survey Open-File Report 63-106, 1 map, https://doi.org/10.3133/ofr63106.","productDescription":"1 map","costCenters":[],"links":[{"id":173570,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9cfb","contributors":{"authors":[{"text":"Page, Leland Vernon","contributorId":95450,"corporation":false,"usgs":true,"family":"Page","given":"Leland","email":"","middleInitial":"Vernon","affiliations":[],"preferred":false,"id":229082,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531520,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Seaber, Paul R.","contributorId":67492,"corporation":false,"usgs":true,"family":"Seaber","given":"Paul","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":229081,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1793,"text":"wsp1539K - 1963 - Ground water in the coastal dune area near Florence, Oregon","interactions":[],"lastModifiedDate":"2017-02-03T13:32:03","indexId":"wsp1539K","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1539","chapter":"K","title":"Ground water in the coastal dune area near Florence, Oregon","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1539K","usgsCitation":"Hampton, E.R., 1963, Ground water in the coastal dune area near Florence, Oregon: U.S. Geological Survey Water Supply Paper 1539, iv, 36 p. :charts, maps (1 fold. in pocket) ;24 cm., https://doi.org/10.3133/wsp1539K.","productDescription":"iv, 36 p. :charts, maps (1 fold. in pocket) ;24 cm.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":109978,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24733.htm","linkFileType":{"id":5,"text":"html"},"description":"24733"},{"id":26937,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539k/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26938,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1539k/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":136933,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1539k/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d7b9","contributors":{"authors":[{"text":"Hampton, E. R.","contributorId":57038,"corporation":false,"usgs":true,"family":"Hampton","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":144164,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1762,"text":"wsp1475P - 1963 - Hydrology of stock-water development in southeastern Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:05:15","indexId":"wsp1475P","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1475","chapter":"P","title":"Hydrology of stock-water development in southeastern Idaho","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Hydrology of the Public Domain","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. Govt. 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Off.,","doi":"10.3133/wsp1475P","usgsCitation":"Hadley, R.F., 1963, Hydrology of stock-water development in southeastern Idaho: U.S. Geological Survey Water Supply Paper 1475, iv, 563-599 p. :maps ;24 cm., https://doi.org/10.3133/wsp1475P.","productDescription":"iv, 563-599 p. :maps ;24 cm.","costCenters":[],"links":[{"id":137114,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1475p/report-thumb.jpg"},{"id":26875,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1475p/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26876,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1475p/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26877,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1475p/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601f16","contributors":{"authors":[{"text":"Hadley, R. F.","contributorId":27028,"corporation":false,"usgs":true,"family":"Hadley","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":144102,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2357,"text":"wsp1539Q - 1963 - Reconnaissance of the hydrology of the Little Lost River basin, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:05:20","indexId":"wsp1539Q","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1539","chapter":"Q","title":"Reconnaissance of the hydrology of the Little Lost River basin, Idaho","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1539Q","usgsCitation":"Mundorff, M.J., Broom, H.C., and Kilburn, C., 1963, Reconnaissance of the hydrology of the Little Lost River basin, Idaho: U.S. Geological Survey Water Supply Paper 1539, iv, 51 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1539Q.","productDescription":"iv, 51 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":109984,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24739.htm","linkFileType":{"id":5,"text":"html"},"description":"24739"},{"id":137785,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1539q/report-thumb.jpg"},{"id":28292,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539q/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28293,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539q/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28294,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539q/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28295,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1539q/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db636c6b","contributors":{"authors":[{"text":"Mundorff, Maurice John","contributorId":41404,"corporation":false,"usgs":true,"family":"Mundorff","given":"Maurice","email":"","middleInitial":"John","affiliations":[],"preferred":false,"id":145073,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Broom, H. C.","contributorId":93024,"corporation":false,"usgs":true,"family":"Broom","given":"H.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":145075,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kilburn, Chabot","contributorId":83499,"corporation":false,"usgs":true,"family":"Kilburn","given":"Chabot","email":"","affiliations":[],"preferred":false,"id":145074,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":947,"text":"wsp1779B - 1963 - Variations in the chemical character of the Susquehanna River at Harrisburg, Pennsylvania","interactions":[],"lastModifiedDate":"2017-07-07T09:17:39","indexId":"wsp1779B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1779","chapter":"B","title":"Variations in the chemical character of the Susquehanna River at Harrisburg, Pennsylvania","docAbstract":"The chemical quality of the Susquehanna River at Harrisburg is influenced by three major factors: streamflow, anthracite and bituminous coal-mine drainage, and geology. Water samples collected at Harrisburg near the west bank of the Susquehanna River and those of western tributaries that drain limestone terranes are similar in chemical quality. The water is alkaline and contains calcium, magnesium, and bicarbonate-ion concentrations typical of water drained from limestone. The chemical quality of water samples collected in the center of the river resembles the quality of the West Branch Susquehanna River, which has a dissolved-solids content of about 200 parts per million, and a sulfate-ion concentration that generally exceeds the bicarbonate-ion concentration. Samples collected near the east or Harrisburg bank show the effect of anthracite coalmine drainage from the river's eastern tributaries. The pH of these samples ranges from 5.7 to 7.5, and sulfate is the predominate ion. \r\n\r\nThe dissolved-solids content of the river at the Harrisburg cross-section stations is inversely proportional to the streamflow. During periods of low riverflow, the dissolved-solids content approaches a maximum; during periods of high flow, the content is low. \r\n\r\nThe chemical composition of the river at the Harrisburg cross section indicates that water from the principal tributaries above Harrisburg does not mix sufficiently to lose its chemical-quality identity before reaching Harrisburg irrespective of the long distance involved, the many islands and bridge piers, and the rough streambed. This lack of lateral mixing is probably due to the small depth-width ratio and the extreme width of the river.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp1779B","usgsCitation":"Anderson, P.W., 1963, Variations in the chemical character of the Susquehanna River at Harrisburg, Pennsylvania: U.S. Geological Survey Water Supply Paper 1779, iii, 17 p. :illus., map ;24 cm., https://doi.org/10.3133/wsp1779B.","productDescription":"iii, 17 p. :illus., map ;24 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":25447,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1779b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":136964,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1779b/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48e3e4b07f02db54f199","contributors":{"authors":[{"text":"Anderson, Peter W.","contributorId":10400,"corporation":false,"usgs":true,"family":"Anderson","given":"Peter","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":142902,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":42579,"text":"ofr6340 - 1963 - Preliminary map of Block Island, Rhode Island, showing availability of ground water","interactions":[{"subject":{"id":42579,"text":"ofr6340 - 1963 - Preliminary map of Block Island, Rhode Island, showing availability of ground water","indexId":"ofr6340","publicationYear":"1963","noYear":false,"title":"Preliminary map of Block Island, Rhode Island, showing availability of ground water"},"predicate":"SUPERSEDED_BY","object":{"id":70047668,"text":"70047668 - 1964 - Ground-water resources of Block Island, Rhode Island","indexId":"70047668","publicationYear":"1964","noYear":false,"title":"Ground-water resources of Block Island, Rhode Island"},"id":1}],"supersededBy":{"id":70047668,"text":"70047668 - 1964 - Ground-water resources of Block Island, Rhode Island","indexId":"70047668","publicationYear":"1964","noYear":false,"title":"Ground-water resources of Block Island, Rhode Island"},"lastModifiedDate":"2013-08-16T16:00:53","indexId":"ofr6340","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"63-40","title":"Preliminary map of Block Island, Rhode Island, showing availability of ground water","language":"ENGLISH","doi":"10.3133/ofr6340","usgsCitation":"Hansen, A.J., 1963, Preliminary map of Block Island, Rhode Island, showing availability of ground water: U.S. Geological Survey Open-File Report 63-40, 1 map., https://doi.org/10.3133/ofr6340.","productDescription":"1 map.","costCenters":[],"links":[{"id":169341,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d8bc","contributors":{"authors":[{"text":"Hansen, Arnold J. Jr.","contributorId":84336,"corporation":false,"usgs":true,"family":"Hansen","given":"Arnold","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":226749,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":95,"text":"wsp1770 - 1963 - Ground-water levels in the United States, 1956-60, southwestern states","interactions":[{"subject":{"id":23879,"text":"ofr6196 - 1961 - Water levels in observation wells in Santa Barbara County, California, in 1960","indexId":"ofr6196","publicationYear":"1961","noYear":false,"title":"Water levels in observation wells in Santa Barbara County, California, in 1960"},"predicate":"SUPERSEDED_BY","object":{"id":95,"text":"wsp1770 - 1963 - Ground-water levels in the United States, 1956-60, southwestern states","indexId":"wsp1770","publicationYear":"1963","noYear":false,"title":"Ground-water levels in the United States, 1956-60, southwestern states"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:10","indexId":"wsp1770","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1770","title":"Ground-water levels in the United States, 1956-60, southwestern states","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1770","usgsCitation":"Hackett, O.M., 1963, Ground-water levels in the United States, 1956-60, southwestern states: U.S. Geological Survey Water Supply Paper 1770, v, 160 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1770.","productDescription":"v, 160 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":136059,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1770/report-thumb.jpg"},{"id":24701,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1770/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6675b0","contributors":{"authors":[{"text":"Hackett, O. M.","contributorId":38527,"corporation":false,"usgs":true,"family":"Hackett","given":"O.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":141923,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1295,"text":"wsp1619W - 1963 - Chemical quality of surface waters in Pennsylvania","interactions":[],"lastModifiedDate":"2017-07-07T09:16:55","indexId":"wsp1619W","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1619","chapter":"W","title":"Chemical quality of surface waters in Pennsylvania","docAbstract":"Pennsylvania has an abundant supply of surface water of good quality. The average rainfall over the 45,300 square miles in the State is about 42 inches per year. Of this amount, about 50 percent appears in the streams as runoff. The combined mean annual runoff of the Delaware, Ohio, and Susquehanna Rivers, at their farthest downstream measuring points in the State, is in excess of 81,000 cubic feet per second. Variations in the chemical quality of the surface waters in Pennsylvania are caused by areal differences in geology, urban and industrial development, mining, quarrying, land use, and runoff. Waters having the least dissolved solids are found in the glaciated northeastern and northwestern parts of the State; waters having higher values of hardness are found in the limestone terranes in the southeastern and south-central parts. In the anthracite coal fields in the northeast and in the bituminous coal fields in the southwest, many streams receive acid mine drainage, which lowers the alkalinity and increases the sulfate content of the waters. The chemical quality of surface waters in Pennsylvania is discussed in general terms. Introductory sections of the report cover the main causative factors which influence chemical quality.
","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp1619W","usgsCitation":"Durfor, C.N., and Anderson, P.W., 1963, Chemical quality of surface waters in Pennsylvania: U.S. Geological Survey Water Supply Paper 1619, iv, 50 p. :ill., maps ;23 cm., https://doi.org/10.3133/wsp1619W.","productDescription":"iv, 50 p. :ill., maps ;23 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":26289,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1619w/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137035,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1619w/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e3845","contributors":{"authors":[{"text":"Durfor, Charles N.","contributorId":50881,"corporation":false,"usgs":true,"family":"Durfor","given":"Charles","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":143517,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, Peter W.","contributorId":10400,"corporation":false,"usgs":true,"family":"Anderson","given":"Peter","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":143516,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":39,"text":"wsp1692 - 1963 - Evaporation control research, 1959-60","interactions":[],"lastModifiedDate":"2012-02-02T00:05:11","indexId":"wsp1692","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1692","title":"Evaporation control research, 1959-60","docAbstract":"Two hundred and forty-five dispersions of long-chain alkanols were formulated by using various emulsifiers and alkanols. The dispensing and spreading ability of each of these formulations was tested. The most promising emulsifier that could be used with any of the alkanols was glyceryl monostearate (self-emulsifying). However, the concentration of the alkanol in the dispersion form varied somewhat: with the length of the carbon chain. A maximum concentration of 16 percent was obtained using the longer chain alkanols in the dispersion form without losing any of the properties of a fluid. \r\n\r\nNine field tests were undertaken on small stock tanks. The retardant materials used in these tests were dodecanol, hexadecanol, and octadecanol. These materials were applied in either liquid or dispersion form. Four types of dispensing equipment were tested. The first type used a pressure system which sprayed a liquid onto the surface of the water. An anemometer and wind-controlled vane, operated by an electrical system, determined the length End frequency of application. The second type was similar to the first except that gravity was utilized to force the liquid onto the surface. The third type. used a drip system with rates of about 10 drops per minute. The fourth type used a gravity feed and a wind-controlled valve which allowed the dispersion material to flow onto the surface of the water when the wind was in the proper direction. In the field tests, the best reduction in evaporation was obtained using octadecanol in dispersion form and dispensed with the wind-controlled valve and gravity feed system. The maximum reduction in evaporation for a 2-week period was 27 percent. However, the economics of suppressing evaporation from stock tanks is questionable because of the short travel time across the tank by the film. \r\n\r\nThere are still many problems unsolved. Some of these can be resolved in the laboratory whereas others can be resolved only in the field. Some of the more serious problems are the effect of impurities in the alkanols; the rate of cooling of the alkanol from a liquid to a solid state ; the effect of the film on the exchange of water molecules between the air and water; whether the film remains effective in suppressing evaporation for any rate of movement downwind; and the possible use of dodecanol and eicosanol as suppressants.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1692","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1963, Evaporation control research, 1959-60: U.S. Geological Survey Water Supply Paper 1692, 2 v. :illus. ;24 cm., https://doi.org/10.3133/wsp1692.","productDescription":"2 v. :illus. ;24 cm.","costCenters":[],"links":[{"id":137354,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1692/report-thumb.jpg"},{"id":24655,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1692/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47c1e4b07f02db4a6f10","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":527157,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1009,"text":"wsp1579 - 1963 - Progress report on the ground-water resources of the Louisville area, Kentucky, 1949-55","interactions":[],"lastModifiedDate":"2012-02-02T00:05:16","indexId":"wsp1579","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1579","title":"Progress report on the ground-water resources of the Louisville area, Kentucky, 1949-55","docAbstract":"In the Louisville area, the principal water-bearing formations are the glacial-outwash sand and gravel and, in places, the underlying limestone. During the period 1949 through 1955 pumpage from the two aquifers averaged about 30 mgd (million gallons per day). The pumpage was approximately in balance with the normal net recharge to the area but was only about 8 percent of the estimated potential supply of ground water, including induced infiltration from the river. In the Louisville area, ground water is used chiefly for air conditioning and for industrial cooling. In the part of the area southwest of the city, ground water is used also for public supply. \r\n\r\nHigh ground-water levels in 1937 resulted from the greatest flood of record. Subsequently, water levels generally declined in the entire Louisville area. In downtown Louisville, where ground water is used for air conditioning, the water level fluctuates seasonally in response to variations in the rate of pumping. In the heavily pumped industrial areas, where ground water is used for cooling, water-level fluctuations correlate with changes in rates of pumping caused by variations in production schedules. Levels were lowest during the years of World War II. During the period 1952-55, relatively low levels throughout the area reflected the effects of less than normal rainfall, summer drought, and sustained pumping. \r\n\r\nGround water in the Louisville area is very hard and generally of the calcium bicarbonate or calcium sulfate type. It is high in iron and sulfate content but is moderately low in chloride content. In water of the sand and gravel aquifer, the concentration of sulfate has increased gradually during the period 1949-54.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1579","usgsCitation":"Bell, E., Kellogg, R.W., and Kulp, W.K., 1963, Progress report on the ground-water resources of the Louisville area, Kentucky, 1949-55: U.S. Geological Survey Water Supply Paper 1579, iv, 47 p. :ill., maps ;24 cm. + separate portfolio with plates., https://doi.org/10.3133/wsp1579.","productDescription":"iv, 47 p. :ill., maps ;24 cm. + separate portfolio with plates.","costCenters":[],"links":[{"id":137977,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1579/report-thumb.jpg"},{"id":25589,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1579/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25590,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1579/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25591,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1579/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25592,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1579/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25593,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1579/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25594,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1579/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25595,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1579/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25596,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1579/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25597,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1579/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25598,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1579/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25599,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1579/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25600,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1579/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25601,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1579/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25602,"rank":413,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1579/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25603,"rank":414,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1579/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25604,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1579/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65dbab","contributors":{"authors":[{"text":"Bell, Edwin A.","contributorId":96660,"corporation":false,"usgs":true,"family":"Bell","given":"Edwin A.","affiliations":[],"preferred":false,"id":143018,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kellogg, Robert W.","contributorId":61793,"corporation":false,"usgs":true,"family":"Kellogg","given":"Robert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":143017,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kulp, Willis K.","contributorId":8076,"corporation":false,"usgs":true,"family":"Kulp","given":"Willis","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":143016,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1216,"text":"wsp1619FF - 1963 - Geology and ground-water resources of Bartow County, 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685c81","contributors":{"authors":[{"text":"Croft, M.G.","contributorId":55413,"corporation":false,"usgs":true,"family":"Croft","given":"M.G.","email":"","affiliations":[],"preferred":false,"id":143383,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1207,"text":"wsp1619GG - 1963 - Geology and ground-water resources of the town of Southold, Suffolk County, New York","interactions":[],"lastModifiedDate":"2022-03-22T18:33:48.468611","indexId":"wsp1619GG","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1619","chapter":"GG","title":"Geology and ground-water resources of the town of Southold, Suffolk County, New York","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1619GG","usgsCitation":"Crandell, H., 1963, Geology and ground-water resources of the town of Southold, Suffolk County, New York: U.S. Geological Survey Water Supply Paper 1619, Report: iv, 36 p.; 3 Plate: 36.00 × 17.00 inches or smaller, https://doi.org/10.3133/wsp1619GG.","productDescription":"Report: iv, 36 p.; 3 Plate: 36.00 × 17.00 inches or smaller","costCenters":[],"links":[{"id":397410,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24824.htm"},{"id":26093,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1619gg/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26092,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619gg/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26091,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619gg/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26090,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619gg/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138062,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1619gg/report-thumb.jpg"}],"scale":"48000","country":"United States","state":"New York","county":"Suffolk County","otherGeospatial":"Town of Southold","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -72.625,\n 40.95\n ],\n [\n -72.242,\n 40.95\n ],\n [\n -72.242,\n 41.167\n ],\n [\n -72.625,\n 41.167\n ],\n [\n -72.625,\n 40.95\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4448","contributors":{"authors":[{"text":"Crandell, Herbert C.","contributorId":15591,"corporation":false,"usgs":true,"family":"Crandell","given":"Herbert C.","affiliations":[],"preferred":false,"id":143366,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1095,"text":"wsp1539O - 1963 - Hydrogeologic reconnaissance of San Nicolas Island, California","interactions":[],"lastModifiedDate":"2023-01-06T19:37:28.561983","indexId":"wsp1539O","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1539","chapter":"O","title":"Hydrogeologic reconnaissance of San Nicolas Island, California","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1539O","usgsCitation":"Burnhan, W.L., Kunkel, F., Hofmann, W., and Peterson, W.C., 1963, Hydrogeologic reconnaissance of San Nicolas Island, California: U.S. Geological Survey Water Supply Paper 1539, Report: iv, 43 p.; 1 Plate: 32.78 x 37.00 inches, https://doi.org/10.3133/wsp1539O.","productDescription":"Report: iv, 43 p.; 1 Plate: 32.78 x 37.00 inches","costCenters":[],"links":[{"id":25825,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1539o/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25824,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539o/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137915,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1539o/report-thumb.jpg"},{"id":109982,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24737.htm","linkFileType":{"id":5,"text":"html"},"description":"24737"}],"country":"United States","state":"California","otherGeospatial":"San Nicolas Island","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -119.58645965805519,\n 33.289640846680385\n ],\n [\n -119.58645965805519,\n 33.210206200976145\n ],\n [\n -119.42590136313942,\n 33.210206200976145\n ],\n [\n -119.42590136313942,\n 33.289640846680385\n ],\n [\n -119.58645965805519,\n 33.289640846680385\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627906","contributors":{"authors":[{"text":"Burnhan, W. L.","contributorId":21136,"corporation":false,"usgs":true,"family":"Burnhan","given":"W.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":143167,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kunkel, Fred","contributorId":47766,"corporation":false,"usgs":true,"family":"Kunkel","given":"Fred","email":"","affiliations":[],"preferred":false,"id":143169,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hofmann, Walter","contributorId":30604,"corporation":false,"usgs":true,"family":"Hofmann","given":"Walter","email":"","affiliations":[],"preferred":false,"id":143168,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Peterson, W. C.","contributorId":57051,"corporation":false,"usgs":true,"family":"Peterson","given":"W.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":143170,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":951,"text":"wsp1539G - 1963 - Ground-water geology of Karnes County, Texas","interactions":[],"lastModifiedDate":"2016-08-19T14:41:27","indexId":"wsp1539G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1539","chapter":"G","title":"Ground-water geology of Karnes County, Texas","docAbstract":"The exposed rocks and those underlying Karnes County dip toward the Gulf of Mexico at average rates ranging from 20 to more than 200 feet per mile. The oil fields are on structures associated with faulting; the effect of faulting on the occurrence of ground water has not been determined.
\nThe principal water-bearing formations, from oldest to youngest, underlying the county are the Carrizo sand, Yegua formation, Jackson group, Catahoula tuff, Oakville sandstone, and Lagarto clay. They range in age from Eocene to Miocene and all are of sedimentary origin. About 40 million acre-feet of usable water (water containing less than 3,000 ppm) is stored more then 2,500 feet below land surface in the Carrizo sand; 30 million acre-feet is stored in the younger formations at depths less than 1,000 feet.
\nGround-water withdrawals for municipal, industrial, and domestic use averaged about 1.7 million gpd in 1957. Irrigation and stock supplies were derived from both ground- and surface-water sources. In general, water levels from 1936 through 1957 were not affected appreciably by withdrawals.
\nRecharge to the ground-water reservoir from precipitation, although only a small percentage of total precipitation, exceeded withdrawals of ground water by wells in 1957.
\nMost of the usable ground water in Karnes County is of substandard quality; whereas water from the San Antonio River, although hard, is of excellent quality. Wells tapping the Carrizo may yield as much as 1,000 gpm in the northwestern part of the county; wells in the shallower formations may yield as much as 600 gpm in the most favorable areas, but in some places may yield only a few gallons per minute of water suitable only for stock.
","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp1539G","usgsCitation":"Anders, R.B., 1963, Ground-water geology of Karnes County, Texas: U.S. Geological Survey Water Supply Paper 1539, Report: v, 40 p.; 10 Plates, https://doi.org/10.3133/wsp1539G.","productDescription":"Report: v, 40 p.; 10 Plates","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":25472,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1539g/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":109976,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24730.htm","linkFileType":{"id":5,"text":"html"},"description":"24730"},{"id":25471,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539g/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25465,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539g/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25466,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539g/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25467,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539g/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25468,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539g/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25469,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539g/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138059,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1539g/report-thumb.jpg"},{"id":25462,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539g/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25463,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539g/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25464,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539g/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25470,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539g/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db6741a5","contributors":{"authors":[{"text":"Anders, Robert B.","contributorId":44125,"corporation":false,"usgs":true,"family":"Anders","given":"Robert","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":142907,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":33821,"text":"b1063G - 1963 - Geology of the Jewel Cave SW Quadrangle, Custer County, South Dakota","interactions":[{"subject":{"id":12752,"text":"ofr5910 - 1959 - The geology of the Jewel Cave SW quadrangle, South Dakota, and its bearing on the origin of the uranium deposits in the southern Black Hills","indexId":"ofr5910","publicationYear":"1959","noYear":false,"title":"The geology of the Jewel Cave SW quadrangle, South Dakota, and its bearing on the origin of the uranium deposits in the southern Black Hills"},"predicate":"SUPERSEDED_BY","object":{"id":33821,"text":"b1063G - 1963 - Geology of the Jewel Cave SW Quadrangle, Custer County, South Dakota","indexId":"b1063G","publicationYear":"1963","noYear":false,"chapter":"G","title":"Geology of the Jewel Cave SW Quadrangle, Custer County, South Dakota"},"id":1}],"lastModifiedDate":"2018-03-07T14:23:16","indexId":"b1063G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1063","chapter":"G","title":"Geology of the Jewel Cave SW Quadrangle, Custer County, South Dakota","docAbstract":"The Jewel Cave SW quadrangle is in the southwestern part of the Black Hills in Custer County, S. Dak., about midway between Edgemont, S. Dak., and Newcastle, Wyo. All the rocks that crop out within the quadrangle are of sedimentary origin and range in age from Pennsylvanian to Early Cretaceous.\r\n\r\nThe Minnesota Formation of Pennsylvania and Permian age, which is about 1,000 feet thick, was studied in outcrop and from two diamond-drill cores. In the subsurface the upper part of the formation consists of gray sandstone, very fine grained dolomite, and anhydrite. The anhydrite has been leached from the formation near the outcrop, perhaps in the early part of the Cenozoic Era, and the resulting subsidence has produced collapse breccias in the Minnelusa and milder deformation in the overlying units. In the collapse breccias the rocks have been oxidized and are red, whereas in the subsurface they are gray. The anhydrite cement of the subsurface sandstone has been replaced by calcite, and the dolomite beds have been partially converted to limestone.\r\n\r\nThe Opeche Formation of Permian age consists of 75 to 115 feet of red siltstone and shale and two thin gypsum beds. The Minnekahta Limestone of Permian age is about 40 feet thick.\r\n\r\nThe Spearfish Formation of Permian and Triassic age is about 550 feet thick and consists of red siltstone red sandstone, dolomite, and gypsum. The dolomite and gypsum beds are restricted to the lower half of the formation. In the northeast corner of the quadrangle the gypsum beds have been dissolved by ground water. The Sundance Formation of Late Jurassic age is divided into five members that have a total thickness of about 360 feet. The Morrison Formation of Late Jurassic age ranges in thickness from 60 to 120 feet. It consists of blocky weathering noncarbonaceous mudstone and subordinate beds of limestone and sandstone.\r\n\r\nThe Inyan Kara Group of Early Cretaceous age has been subdivided into the Lakota Formation and the Fall River Formation. The Lakota Formation consists of 200 to 300 feet of carbonaceous siltstone blocky-weathering claystone, and fine-grained to conglomeratic sandstone. These rocks were deposited in stream channels, flood plains, and ponds. The Fall River Formation is about 110 to 130 feet thick. Along the northeast side of the outcrop the formation consists of fine- to medium-grained sandstone, which forms an elongate body at least 1-1/2 miles wide and more than 25 miles long. To the southwest the formation consists of thinly stratified interbedded sandstone, carbonaceous siltstone, and varicolored mudstone. The Skull Creek and Mowry Shales of Early Cretaceous age consist of black fissile shale. The Mowry contains abundant fish scales and weathers to a silver gray.\r\n\r\nAlluvium fills the bottom of many intermittent streams, and small gravel-covered terraces mark the former high levels of these streams. Gravel, which caps hills at altitudes of 4,460 to 4,620 feet, is believed to have been deposited by a Pleistocene stream that drained southeastward toward the town of Minnekahta. Many landslides are present along the northward- and eastward-facing scarp of the Inyan Kara hogback.\r\n\r\nThe Dewey fault, trending N. 75 deg E., crosses the quadrangle. It is probably a vertical dip-slip fault, and has an apparent displacement of 250 to 440 feet. Two northwest-trending anticlines are in the quadrangle - one extends from the Edgemont NE quadrangle to near the center of the Jewel Cave SW quadrangle, and the other is limited to the center of the Jewel Cave SW quadrangle.\r\n\r\nCollapse structures, which were produced by the solution of anhydrite, are (a) breccias in the Minnelusa Formation, (b) limestone-dolomite breccias in the Spearfish Formation, (c) undulations and normal faults in the formations overlying the Minnelusa and (d) breccia pipes that extend upward from the Minnelusa to at least as high as the Lakota Formation. The leaching probably occurred in early Cenozoic time.\r\n\r\nMinor deformationa","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1063G","collaboration":"Prepared on behalf of the U.S. Atomic Energy Commission","usgsCitation":"Braddock, W.A., 1963, Geology of the Jewel Cave SW Quadrangle, Custer County, South Dakota: U.S. Geological Survey Bulletin 1063, 52 p., https://doi.org/10.3133/b1063G.","productDescription":"52 p.","startPage":"217","endPage":"268","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":109263,"rank":699,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20699.htm","linkFileType":{"id":5,"text":"html"},"description":"20699"},{"id":96110,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1063g/plate-21.pdf","size":"252","linkFileType":{"id":1,"text":"pdf"}},{"id":96109,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1063g/plate-20.pdf","size":"7111","linkFileType":{"id":1,"text":"pdf"}},{"id":96111,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1063g/plate-22.pdf","size":"401","linkFileType":{"id":1,"text":"pdf"}},{"id":96108,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1063g/report.pdf","size":"5115","linkFileType":{"id":1,"text":"pdf"}},{"id":166670,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1063g/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae2a7","contributors":{"authors":[{"text":"Braddock, William A.","contributorId":61010,"corporation":false,"usgs":true,"family":"Braddock","given":"William","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":211990,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":65274,"text":"i270B2 - 1963 - Arabian Peninsula","interactions":[],"lastModifiedDate":"2025-03-24T13:33:39.943151","indexId":"i270B2","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"270-B-2","title":"Arabian Peninsula","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i270B2","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1963, Arabian Peninsula: U.S. Geological Survey IMAP 270-B-2, 1 Plate: 55.26 x 47.93 inches, https://doi.org/10.3133/i270B2.","productDescription":"1 Plate: 55.26 x 47.93 inches","costCenters":[],"links":[{"id":189291,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0270b-2/report-thumb.jpg"},{"id":483629,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0270b-2/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"2000000","otherGeospatial":"Arabian Peninsula","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 34,12 ], [ 34,32.5 ], [ 61,32.5 ], [ 61,12 ], [ 34,12 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db679e82","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":533663,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1975,"text":"wsp1662A - 1963 - Specific Yield--Column drainage and centrifuge moisture content","interactions":[],"lastModifiedDate":"2012-02-02T00:05:24","indexId":"wsp1662A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1662","chapter":"A","title":"Specific Yield--Column drainage and centrifuge moisture content","docAbstract":"The specific yield of a rock or soil, with respect to water, is the ratio of (1) the volume of water which, after being saturated, it will yield by gravity to (2) its own volume. Specific retention represents the water retained against gravity drainage. The specific yield and retention when added together are equal to the total interconnected porosity of the rock or soil. Because specific retention is more easily determined than specific yield, most methods for obtaining yield first require the determination of specific retention. Recognizing the great need for developing improved methods of determining the specific yield of water-bearing materials, the U.S. Geological Survey and the California Department of Water Resources initiated a cooperative investigation of this subject. The major objectives of this research are (1) to review pertinent literature on specific yield and related subjects, (2) to increase basic knowledge of specific yield and rate of drainage and to determine the most practical methods of obtaining them, (3) to compare and to attempt to correlate the principal laboratory and field methods now commonly used to obtain specific yield, and (4) to obtain improved estimates of specific yield of water-bearing deposits in California. An open-file report, 'Specific yield of porous media, an annotated bibliography,' by A. I. Johnson, D. A. Morris, and R. C. Prill, was released in 1960 in partial fulfillment of the first objective. This report describes the second phase of the specific-yield study by the U.S. Geological Survey Hydrologic Laboratory at Denver, Colo. Laboratory research on column drainage and centrifuge moisture equivalent, two methods for estimating specific retention of porous media, is summarized. In the column-drainage study, a wide variety of materials was packed into plastic columns of 1- to 8-inch diameter, wetted with Denver tap water, and drained under controlled conditions of temperature and humidity. The effects of cleaning the porous media; of different column diameters; of dye and time on drainage; and of different methods of drainage, wetting, and packing were all determined. To insure repeatability of porosity in duplicate columns, a mechanical technique of packing was developed. \r\n\r\nIn the centrifuge moisture-content study, the centrifuge moisture-equivalent (the moisture content retained by a soil that has been first saturated and then subjected to a force equal to 1,000 times the force of gravity for 1 hour) test was first reviewed and evaluated. It was determined that for reproducible moisture-retention results the temperature and humidity should be controlled by use of a controlled-temperature centrifuge. In addition to refining this standard test, the study determined the effect of length of period of centrifuging and of applied tension on the drainage results. \r\n\r\nThe plans for future work require the continuation of the laboratory standardization study qith emphasis on investigation of soil-moisture tension and unsaturated-permeability techniques. A detailed study in the field then will be followed by correlation and evaluation of laboratory and field methods.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1662A","usgsCitation":"Johnson, A., Prill, R., and Morris, D.A., 1963, Specific Yield--Column drainage and centrifuge moisture content: U.S. Geological Survey Water Supply Paper 1662, v, 60 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1662A.","productDescription":"v, 60 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":138314,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1662a/report-thumb.jpg"},{"id":27351,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1662a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db648529","contributors":{"authors":[{"text":"Johnson, A.I.","contributorId":82676,"corporation":false,"usgs":true,"family":"Johnson","given":"A.I.","email":"","affiliations":[],"preferred":false,"id":144464,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Prill, R.C.","contributorId":27034,"corporation":false,"usgs":true,"family":"Prill","given":"R.C.","affiliations":[],"preferred":false,"id":144462,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Morris, D. 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The area lies between Hamilton, Ohio, and the Ohio River and includes a preglacial valley now occupied by portions of the Miami River, Whitewater River, and Mill Creek. The valley is partially filled with glacial debris which yields large quantities of good-quality water. The object of the study was to determine the thickness of these glacial deposits and the shape of the preglacial valley.
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