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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp351","usgsCitation":"MacKallor, J., 1963, Natural gamma aeroradioactivity of the Georgia Nuclear Laboratory area, Georgia: U.S. Geological Survey Geophysical Investigations Map 351, 1 Plate: 55.24 × 33.44 inches, https://doi.org/10.3133/gp351.","productDescription":"1 Plate: 55.24 × 33.44 inches","costCenters":[],"links":[{"id":253335,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0351/report-thumb.jpg"},{"id":249859,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0351/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":249858,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0351/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":392125,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3286.htm"}],"scale":"250000","country":"United States","state":"Georgia","otherGeospatial":"Georgia Nuclear Laboratory area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -85.5,\n 33.3833\n ],\n [\n -82.9667,\n 33.3833\n ],\n [\n -82.9667,\n 35\n ],\n [\n -85.5,\n 35\n ],\n [\n -85.5,\n 33.3833\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db69820c","contributors":{"authors":[{"text":"MacKallor, J. 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F.","affiliations":[],"preferred":false,"id":268433,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1111,"text":"wsp1577 - 1963 - Ground-water geology and pump irrigation in Frenchman Creek Basin above Palisade, Nebraska","interactions":[],"lastModifiedDate":"2012-02-02T00:05:17","indexId":"wsp1577","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":"1577","title":"Ground-water geology and pump irrigation in Frenchman Creek Basin above Palisade, Nebraska","docAbstract":"This report describes the geography, geology, and ground-water resources of that part of the Frenchman Creek basin upstream from Palisade, Nebr., an area of about 4,900 square miles. The basin includes all of Phillips County, Colo., and Chase County, Nebr., and parts of Logan, Sedgwick, Washington, and Yuma Counties, Colo., and Dundy, Hayes, Hitchcock, and Perkins Counties, Nebr. The land surface ranges from nearly flat to rolling; choppy hills and interdune saddles are common in the areas of dune sand, and steep bluffs and gullies cut the edges of the relatively flat loess plateaus. Most of the basin is drained by tributaries of Frenchman Creek, but parts of the sandhills are undrained. Farming and livestock raising are the principal industries. Irrigation with ground water has expanded rapidly since 1934. \r\n\r\nThe rocks exposed in the basin are largely unconsolidated and range in age from Pliocene to Recent. They comprise the Ogallala formation (Pliocene), the Sanborn formation (Pleistocene and Recent?), dune sand (Pleistocene and Recent), and alluvium (Recent). The rocks underlying the Ogallala are the Pierre shale (Late Cretaceous) and the White River group (Oligocene). The Pierre shale is relatively impermeable and yields little or no water to wells. The White River group also is relatively impermeable and yields little or no water to wells; however, small to moderate quantities of water possibly may be obtained from wells that penetrate fractured or 'porous' zones in the upper part of the White River group or permeable channel deposits within the group. The Ogallala formation is the main aquifer in the basin and yields moderate to large quantities of water to wells. The Sanborn formation and the dune sand generally lie above the water table, but in areas of high water table the dune sand yields small quantities of water to wells for domestic and stock supplies. The alluvium, which includes the low terrace deposits bordering the major streams, yields small to large quantities of water to wells. \r\n\r\nThe ground-water reservoir is recharged only from precipitation on the basin. Of the average annual precipitation of 19.5 inches, about 0.9 inch infiltrates to the water table, thereby contributing about 220,000 acre-feet of water annually to the ground-water reservoir. About 81 million acre-feet of water that could drain under gravity, and thus theoretically is available to wells, is held in groundwater storage in the basin. Water is discharged from the ground-water reservoir by wells, evaporation and transpiration, springs, seepage into streams, and movement into adjacent areas to the east and southeast. Most of the domestic, stock, and irrigation water supplies and all the public supplies are pumped from wells.\r\n\r\nDuring 1953, 96 wells were used to irrigate 10,000 acres of land with 19,000 acre-feet of water. About 34,000 acre-feet of water is evaporated and transpired annually in the valleys of the main streams and in areas of shallow water table in the sandhills. \r\n\r\nFrom the projection of base-flow measurements made during 1952, it was estimated that the average annual flow of Frenchman Creek into the reservoir above Enders Dam is about 57,000 acre-feet. By similar determinations, the average annual flow of Frenchman Creek at the gaging station at Palisade, Nebr., about 22 miles downstream from Enders Dam, is about 76,000 acre-feet, and the flow of Stinking Water Creek at the gaging station near Palisade is about 22,000 acre-feet. The combined flow of Frenchman and Stinking Water Creeks at their confluence near Palisade thus is about 98,000 acre-feet per year. About 90,000 acre-feet of ground water is estimated to move eastward each year across the Colorado-Nebraska State line within the basin. \r\n\r\nAdditional irrigation wells that will tap the Ogallala formation and the alluvium in the major valleys undoubtedly will be drilled. On the basis of current estimates of future irrigation.withdrawals, it is concluded that by the ","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1577","usgsCitation":"Cardwell, W.D., and Jenkins, E., 1963, Ground-water geology and pump irrigation in Frenchman Creek Basin above Palisade, Nebraska: U.S. Geological Survey Water Supply Paper 1577, vii, 472 p. :illus., diagrs., maps ;24 cm., https://doi.org/10.3133/wsp1577.","productDescription":"vii, 472 p. :illus., diagrs., maps ;24 cm.","costCenters":[],"links":[{"id":109991,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24763.htm","linkFileType":{"id":5,"text":"html"},"description":"24763"},{"id":138010,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1577/report-thumb.jpg"},{"id":25858,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1577/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25859,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1577/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25860,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1577/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25861,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1577/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25862,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1577/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25863,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1577/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25864,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1577/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25865,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1577/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25866,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1577/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25867,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1577/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25868,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1577/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668e74","contributors":{"authors":[{"text":"Cardwell, W. D. E.","contributorId":69120,"corporation":false,"usgs":true,"family":"Cardwell","given":"W.","email":"","middleInitial":"D. E.","affiliations":[],"preferred":false,"id":143195,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jenkins, Edward D.","contributorId":17972,"corporation":false,"usgs":true,"family":"Jenkins","given":"Edward D.","affiliations":[],"preferred":false,"id":143194,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":62331,"text":"gq268 - 1963 - Geology of the Lynn Grove quadrangle in Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:12:51","indexId":"gq268","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"268","title":"Geology of the Lynn Grove quadrangle in Kentucky","language":"ENGLISH","doi":"10.3133/gq268","usgsCitation":"Olive, W.W., 1963, Geology of the Lynn Grove quadrangle in Kentucky: U.S. Geological Survey Geologic Quadrangle 268, 1 map :col. ;on sheet 76 x 82 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/gq268.","productDescription":"1 map :col. ;on sheet 76 x 82 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":102274,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_723.htm","linkFileType":{"id":5,"text":"html"},"description":"723"},{"id":248510,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0268/report.pdf","size":"35","linkFileType":{"id":1,"text":"pdf"}},{"id":253571,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0268/report-thumb.jpg"}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67ea84","contributors":{"authors":[{"text":"Olive, Wilds W.","contributorId":51302,"corporation":false,"usgs":true,"family":"Olive","given":"Wilds","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":267238,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68454,"text":"ha51 - 1963 - Floods at Warren, Ohio","interactions":[],"lastModifiedDate":"2012-02-10T00:11:26","indexId":"ha51","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"51","title":"Floods at Warren, Ohio","language":"ENGLISH","doi":"10.3133/ha51","usgsCitation":"Edelen, G.W., Ruggles, F.H., and Cross, W.P., 1963, Floods at Warren, Ohio: U.S. Geological Survey Hydrologic Atlas 51, 1 map :col. ;74 x 82 cm. folded in envelope 30 x 24 cm. (Contour interval 10 feet. 29 by 33 inches), https://doi.org/10.3133/ha51.","productDescription":"1 map :col. ;74 x 82 cm. folded in envelope 30 x 24 cm. (Contour interval 10 feet. 29 by 33 inches)","costCenters":[],"links":[{"id":186276,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89991,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/051/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -80.88388888888889,41.168055555555554 ], [ -80.88388888888889,41.28333333333333 ], [ -80.75,41.28333333333333 ], [ -80.75,41.168055555555554 ], [ -80.88388888888889,41.168055555555554 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4bae","contributors":{"authors":[{"text":"Edelen, George W. 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Jr.","contributorId":40628,"corporation":false,"usgs":true,"family":"Ruggles","given":"Frederick","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":278253,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cross, William Perry","contributorId":21137,"corporation":false,"usgs":true,"family":"Cross","given":"William","email":"","middleInitial":"Perry","affiliations":[],"preferred":false,"id":278252,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":61801,"text":"gq229 - 1963 - Geology of the Flaherty quadrangle, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:50","indexId":"gq229","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"229","title":"Geology of the Flaherty quadrangle, Kentucky","language":"ENGLISH","doi":"10.3133/gq229","usgsCitation":"Swadley, W.C., 1963, Geology of the Flaherty quadrangle, Kentucky: U.S. Geological Survey Geologic Quadrangle 229, 1 map :col. ;57 x 46 cm., on sheet 81 x 83 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/gq229.","productDescription":"1 map :col. ;57 x 46 cm., on sheet 81 x 83 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":102233,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_682.htm","linkFileType":{"id":5,"text":"html"},"description":"682"},{"id":248093,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0229/report.pdf","size":"36","linkFileType":{"id":1,"text":"pdf"}},{"id":252753,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0229/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -86.11749999999999,37.75 ], [ -86.11749999999999,37.8675 ], [ -86,37.8675 ], [ -86,37.75 ], [ -86.11749999999999,37.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acfe4b07f02db6805a2","contributors":{"authors":[{"text":"Swadley, W. C.","contributorId":46940,"corporation":false,"usgs":true,"family":"Swadley","given":"W.","middleInitial":"C.","affiliations":[],"preferred":false,"id":266382,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":64953,"text":"i365 - 1963 - Geologic map of the Hay Creek quadrangle, Roosevelt County, Montana","interactions":[],"lastModifiedDate":"2012-02-10T00:11:09","indexId":"i365","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":"365","subseriesTitle":"NONE","title":"Geologic map of the Hay Creek quadrangle, Roosevelt County, Montana","language":"ENGLISH","doi":"10.3133/i365","usgsCitation":"Colton, R.B., 1963, Geologic map of the Hay Creek quadrangle, Roosevelt County, Montana: U.S. Geological Survey IMAP 365, 1 map :col. ;on sheet 63 x 81 cm. in folder 30 x 24 cm., https://doi.org/10.3133/i365.","productDescription":"1 map :col. ;on sheet 63 x 81 cm. in folder 30 x 24 cm.","costCenters":[],"links":[{"id":102853,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1319.htm","linkFileType":{"id":5,"text":"html"},"description":"1319"},{"id":190381,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":91467,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0365/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.25,48.25 ], [ -105.25,48.5 ], [ -105,48.5 ], [ -105,48.25 ], [ -105.25,48.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db6983c7","contributors":{"authors":[{"text":"Colton, R. 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W. Jr.","contributorId":18331,"corporation":false,"usgs":true,"family":"Johnson","given":"R.","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":269337,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"King, E. R.","contributorId":93482,"corporation":false,"usgs":true,"family":"King","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":269338,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Long, C. L.","contributorId":98699,"corporation":false,"usgs":true,"family":"Long","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":269339,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":35330,"text":"b1121J - 1963 - Geology of the Duck Creek Pass quadrangle, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:09:35","indexId":"b1121J","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":"1121","chapter":"J","title":"Geology of the Duck Creek Pass quadrangle, Montana","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1121J","usgsCitation":"Nelson, W.H., 1963, Geology of the Duck Creek Pass quadrangle, Montana: U.S. Geological Survey Bulletin 1121, p. J1-J56, ill., maps ;23 cm., https://doi.org/10.3133/b1121J.","productDescription":"p. J1-J56, ill., maps ;23 cm.","costCenters":[],"links":[{"id":109356,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20818.htm","linkFileType":{"id":5,"text":"html"},"description":"20818"},{"id":166067,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1121j/report-thumb.jpg"},{"id":63188,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1121j/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63189,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1121j/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682fdf","contributors":{"authors":[{"text":"Nelson, Willis H.","contributorId":84777,"corporation":false,"usgs":true,"family":"Nelson","given":"Willis","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":214462,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68922,"text":"om212 - 1963 - Preliminary geologic map of the Fort Hill quadrangle, Lincoln County, Wyoming","interactions":[],"lastModifiedDate":"2020-01-13T17:28:37","indexId":"om212","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":329,"text":"Oil and Gas Investigation Map","code":"OM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"212","title":"Preliminary geologic map of the Fort Hill quadrangle, Lincoln County, Wyoming","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/om212","usgsCitation":"Oriel, S.S., 1963, Preliminary geologic map of the Fort Hill quadrangle, Lincoln County, Wyoming: U.S. Geological Survey Oil and Gas Investigation Map 212, 1 map. , https://doi.org/10.3133/om212.","productDescription":"1 map. ","costCenters":[],"links":[{"id":104993,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5367.htm","linkFileType":{"id":5,"text":"html"},"description":"5367"},{"id":188693,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"48000","country":"United States ","state":"Wyoming ","county":"Lincoln ","otherGeospatial":"Fort Hill quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -110.2500,\n 42.2500\n ],\n [\n -110.5000,\n 42.2500\n ],\n [\n -110.5000,\n 42.0000\n ],\n [\n -110.2500,\n 42.0000\n ],\n [\n -110.2500,\n 42.2500\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b43e","contributors":{"authors":[{"text":"Oriel, Steven S.","contributorId":108079,"corporation":false,"usgs":true,"family":"Oriel","given":"Steven","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":279225,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2478,"text":"wsp1613A - 1963 - Geology and ground-water conditions in southern Nassau and southeastern Queens Counties, Long Island, N.Y.","interactions":[{"subject":{"id":51254,"text":"ofr5377 - 1953 - Water-level and chloride-content data at outpost observation wells in southwestern Nassau County, Long Island, New York","indexId":"ofr5377","publicationYear":"1953","noYear":false,"title":"Water-level and chloride-content data at outpost observation wells in southwestern Nassau County, Long Island, New York"},"predicate":"SUPERSEDED_BY","object":{"id":2478,"text":"wsp1613A - 1963 - Geology and ground-water conditions in southern Nassau and southeastern Queens Counties, Long Island, N.Y.","indexId":"wsp1613A","publicationYear":"1963","noYear":false,"chapter":"A","title":"Geology and ground-water conditions in southern Nassau and southeastern Queens Counties, Long Island, N.Y."},"id":1},{"subject":{"id":51661,"text":"ofr5498 - 1954 - Supplementary data on water levels and chloride concentrations at outpost observation wells in southern Nassau County, Long Island, New York","indexId":"ofr5498","publicationYear":"1954","noYear":false,"title":"Supplementary data on water levels and chloride concentrations at outpost observation wells in southern Nassau County, Long Island, New York"},"predicate":"SUPERSEDED_BY","object":{"id":2478,"text":"wsp1613A - 1963 - Geology and ground-water conditions in southern Nassau and southeastern Queens Counties, Long Island, N.Y.","indexId":"wsp1613A","publicationYear":"1963","noYear":false,"chapter":"A","title":"Geology and ground-water conditions in southern Nassau and southeastern Queens Counties, Long Island, N.Y."},"id":2}],"lastModifiedDate":"2022-03-22T19:47:50.062941","indexId":"wsp1613A","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":"1613","chapter":"A","title":"Geology and ground-water conditions in southern Nassau and southeastern Queens Counties, Long Island, N.Y.","docAbstract":"Test drilling, electrical logging, and water sampling of 'outpost' and other \r\nwells have revealed the existence of a deep confined body of salt water in the \r\nMagothy(?) formation beneath southwestern Nassau and southeastern Queens \r\nCounties, Long Island, N.Y. In connection with a test-drilling program, cooperatively sponsored by the U.S. Geological Survey, the Nassau County Department \r\nof Public Works, and the New York State Water Resources Commission (formerly \r\nWater Power and Control Commission), 13 wells ranging in depth from about \r\n130 to 800 feet were drilled during 1952 and 1953 and screened at various depths \r\nin the Magothy(?) formation and Jameco gravel. On the basis of the preliminary \r\ngeologic, hydrologic, and chemical data from these wells, a detailed investigation \r\nof ground-water conditions from the water table to the bedrock was begun in a \r\n200-square-mile area in southern Nassau and southeastern Queens Counties. \r\nThe Inain purposes of the investigation were to delineate the bodies of fresh and \r\nsalty ground water in the project area, to relate their occurrence and movement \r\nto geologic and hydrologic conditions, to estimate the rate of encroachment, if \r\nany, of the salty water, and to evaluate the effectiveness of the existing network \r\nof outpost wells as detectors of salt-water encroachment. \r\nAbout a million people in the report area, residing mainly in southern Nassau \r\nCounty, are completely dependent on ground water as a source of supply. Fortunately, precipitation averages about 44 inches per year, of which approximately \r\nhalf is estimated to percolate into the ground-water reservoir. \r\nThe ground water is contained in and moves through eight differentiated geologic units composed of unconsolidated gravel, sand, and clay, of Late Cretaceous, \r\nPleistocene, and Recent age, having a maximum total thickness of about 1,700 \r\nfeet. The underlying metamorphic and igneous crystalline basement rocks are \r\nof Precambrian age and are not water bearing. \r\nThe water-yielding units from the surface down are (1) the upper Pleistocene \r\ndeposits, (2) the principal artesian aquifer, composed of the Jameco gravel and \r\nMagothy(?) formation, and (3) the Lloyd sand member of the Raritar formation. \r\nThe confining units are the '20-foot' clay, the Gardiners clay, and the clay member of the Raritan formation. The upper Pleistocene deposits contain an extensive unconfined body of fresh water. Fresh water under artesian conditions is \r\ncontained in the principal artesian aquifer and the Lloyd sand member. The \r\npiezometric surface of the principal artesian aquifer is similar in shape to the south-ward-sloping water table; it ranges in altitude from about sea level to 55 feet \r\nabove. \r\nThe chemical quality of the fresh ground water in most of the area in all aquifers \r\nis good to excellent, and concentrations of dissolved solids and of chloride generally \r\nare below 100 ppm (parts per million) and 10 ppm, respectively. Analyses of \r\nwater samples from selected wells show no progressive increase in concentration of \r\nchloride in most of the area. The data on quality of water have been used to \r\ndelineate one major and several minor bodies of salty ground water. The wedgeshaped main confined salt-water body, in which the concentration of chloride \r\nreaches about 17,000 ppm, is in the Magothy(?) formation and Jameco gravel in \r\nextreme southwestern Nassau County and southeastern Queens County. The \r\nbase of the salt-water wedge is about at the top of the clay member of the Raritan \r\nformation. Beneath the barrier beach in south-central and southeastern Nassau County a shallow extension of the main confined salt-water body contains as much as 4,000 ppm of chloride and is separated from the lower main salt-water body by fresh ground water. Shallow, thin bodies of unconfined salty ground water are common in the upper Pleistocene and Recent deposits adjacent to salty surface water in tidal creeks, bays, and the Atlantic","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1613A","usgsCitation":"Perlmutter, N.M., and Geraghty, J.J., 1963, Geology and ground-water conditions in southern Nassau and southeastern Queens Counties, Long Island, N.Y.: U.S. Geological Survey Water Supply Paper 1613, Report: vi, 205 p.; 7 Plates: 27.00 × 40.00 inches or smaller, https://doi.org/10.3133/wsp1613A.","productDescription":"Report: vi, 205 p.; 7 Plates: 27.00 × 40.00 inches or smaller","costCenters":[],"links":[{"id":28560,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1613a/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28559,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1613a/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28557,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1613a/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28556,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1613a/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28555,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1613a/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138751,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1613a/report-thumb.jpg"},{"id":28558,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1613a/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28561,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1613a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":394230,"rank":10,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24803.htm"},{"id":28554,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1613a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"96200","country":"United States","state":"New York","county":"Nassau County, Queens County","otherGeospatial":"Long Island","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -73.812,\n 40.583\n ],\n [\n -73.417,\n 40.583\n ],\n [\n -73.417,\n 40.727\n ],\n [\n -73.812,\n 40.727\n ],\n [\n -73.812,\n 40.583\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685f9f","contributors":{"authors":[{"text":"Perlmutter, N. 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J.","contributorId":74738,"corporation":false,"usgs":true,"family":"Geraghty","given":"J.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":145261,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2485,"text":"wsp1475I - 1963 - Hydrology of small watersheds in western states","interactions":[],"lastModifiedDate":"2024-02-01T20:08:52.68234","indexId":"wsp1475I","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":"I","title":"Hydrology of small watersheds in western states","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1475I","usgsCitation":"Peterson, H.V., 1963, Hydrology of small watersheds in western states: U.S. Geological Survey Water Supply Paper 1475, Report: iii, 140 p.; 2 Plates: 20.00 x 15.45 inches and 20.00 x 15.35 inches, https://doi.org/10.3133/wsp1475I.","productDescription":"Report: iii, 140 p.; 2 Plates: 20.00 x 15.45 inches and 20.00 x 15.35 inches","costCenters":[],"links":[{"id":425241,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24412.htm","text":"Wind River basin area","linkFileType":{"id":5,"text":"html"}},{"id":28581,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1475i/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28580,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1475i/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28579,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1475i/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138778,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1475i/report-thumb.jpg"},{"id":425240,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24411.htm","text":"Cheyenne River basin area","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Nebraska, South Dakota, Wyoming","otherGeospatial":"Cheyenne River basin, Wind River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -109.05,\n 43.5\n ],\n [\n -109.05,\n 42.733\n ],\n [\n -107.5,\n 42.733\n ],\n [\n -107.5,\n 43.5\n ],\n [\n -109.05,\n 43.5\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -106,\n 44.167\n ],\n [\n -106,\n 42.683\n ],\n [\n -103.227,\n 42.683\n ],\n [\n -103.227,\n 44.167\n ],\n [\n -106,\n 44.167\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601f10","contributors":{"authors":[{"text":"Peterson, Harold V.","contributorId":9630,"corporation":false,"usgs":true,"family":"Peterson","given":"Harold","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":145272,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1917,"text":"wsp1528 - 1963 - Geology and ground-water resources of the Scottsville area, Kentucky","interactions":[],"lastModifiedDate":"2022-02-01T22:49:59.33899","indexId":"wsp1528","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":"1528","title":"Geology and ground-water resources of the Scottsville area, Kentucky","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1528","usgsCitation":"Hopkins, W.B., 1963, Geology and ground-water resources of the Scottsville area, Kentucky: U.S. Geological Survey Water Supply Paper 1528, Report: vi, 333 p.; 3 Plates: 33.68 × 37.03 inches or smaller, https://doi.org/10.3133/wsp1528.","productDescription":"Report: vi, 333 p.; 3 Plates: 33.68 × 37.03 inches or smaller","costCenters":[],"links":[{"id":27243,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1528/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":109966,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24704.htm","linkFileType":{"id":5,"text":"html"},"description":"24704"},{"id":27242,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1528/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27241,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1528/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27240,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1528/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137701,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1528/report-thumb.jpg"}],"country":"United States","state":"Kentucky","otherGeospatial":"Scottsville area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -86.25,\n 36.629\n ],\n [\n -86,\n 36.629\n ],\n [\n -86,\n 36.875\n ],\n [\n -86.25,\n 36.875\n ],\n [\n -86.25,\n 36.629\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db68600c","contributors":{"authors":[{"text":"Hopkins, William B.","contributorId":54574,"corporation":false,"usgs":true,"family":"Hopkins","given":"William","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":144362,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2966,"text":"wsp1576D - 1963 - Ground water for irrigation in part of the Fort Hall Indian Reservation, Idaho","interactions":[],"lastModifiedDate":"2024-07-31T21:57:05.62565","indexId":"wsp1576D","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":"1576","chapter":"D","title":"Ground water for irrigation in part of the Fort Hall Indian Reservation, Idaho","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1576D","usgsCitation":"West, S.W., and Kilburn, C., 1963, Ground water for irrigation in part of the Fort Hall Indian Reservation, Idaho: U.S. Geological Survey Water Supply Paper 1576, Report: iv, 33 p.; 3 Plates: 32.00 x 31.00 inches or smaller, https://doi.org/10.3133/wsp1576D.","productDescription":"Report: iv, 33 p.; 3 Plates: 32.00 x 31.00 inches or smaller","costCenters":[],"links":[{"id":431768,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24756.htm","linkFileType":{"id":5,"text":"html"}},{"id":29697,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1576d/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29696,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1576d/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29695,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1576d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139270,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1576d/report-thumb.jpg"},{"id":29698,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1576d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","otherGeospatial":"Fort Hall Indian Reservation","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -112.056,\n 43.25\n ],\n [\n -112.666,\n 43.25\n ],\n [\n -112.666,\n 42.848\n ],\n [\n -112.056,\n 42.848\n ],\n [\n -112.056,\n 43.25\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66dd62","contributors":{"authors":[{"text":"West, Sam W.","contributorId":64234,"corporation":false,"usgs":true,"family":"West","given":"Sam","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":146059,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kilburn, Chabot","contributorId":83499,"corporation":false,"usgs":true,"family":"Kilburn","given":"Chabot","email":"","affiliations":[],"preferred":false,"id":146060,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2042,"text":"wsp1669O - 1963 - Ground-water conditions at Argonne National Laboratory, Illinois, 1948-60","interactions":[],"lastModifiedDate":"2012-02-02T00:05:19","indexId":"wsp1669O","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":"1669","chapter":"O","title":"Ground-water conditions at Argonne National Laboratory, Illinois, 1948-60","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1962","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1669O","usgsCitation":"Knowles, D., Drescher, W., and LeRoux, E.F., 1963, Ground-water conditions at Argonne National Laboratory, Illinois, 1948-60: U.S. Geological Survey Water Supply Paper 1669, iv, 40 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1669O.","productDescription":"iv, 40 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":137709,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1669o/report-thumb.jpg"},{"id":27531,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1669o/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d2e9","contributors":{"authors":[{"text":"Knowles, Doyle B.","contributorId":85566,"corporation":false,"usgs":true,"family":"Knowles","given":"Doyle B.","affiliations":[],"preferred":false,"id":144578,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Drescher, W.J.","contributorId":35713,"corporation":false,"usgs":true,"family":"Drescher","given":"W.J.","email":"","affiliations":[],"preferred":false,"id":144577,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"LeRoux, E. F.","contributorId":29795,"corporation":false,"usgs":true,"family":"LeRoux","given":"E.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":144576,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":2355,"text":"wsp1619CC - 1963 - Ground water in the Raft River Basin, Idaho, with special reference to irrigation use, 1956-60","interactions":[],"lastModifiedDate":"2013-11-26T14:46:59","indexId":"wsp1619CC","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":"CC","title":"Ground water in the Raft River Basin, Idaho, with special reference to irrigation use, 1956-60","docAbstract":"In the Raft River basin in south-central Idaho, ground-water withdrawals \nfor irrigation have more than doubled since 1955, when data were compiled \nfor a comprehensive report on the area. The present report summerizes data \non the ground-water use and changes in the water regimen during the intervening \n5 years. Water levels have declined 10 to 20 feet in the areas of heaviest pumping \nand 3 to 5 feet throughout the remainder of the area. These water-level declines \nare related to increased ground-water pumpage and below-normal precipitation \nin the basin. The total pumpage during the 1960 irrigation season is estimated \nto be about 127,000 acre-feet, of which about half was consumed by crops or \nevaporated. The remainder returned to the aquifer.
\nIrrigation development is acting to reduce the amount of underflow out of the \nbasin. The water table can be lowered considerably more before underflow from \nthe basin would be reduced substantially.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1619CC","usgsCitation":"Mundorff, M.J., and Sisco, H., 1963, Ground water in the Raft River Basin, Idaho, with special reference to irrigation use, 1956-60: U.S. Geological Survey Water Supply Paper 1619, iii, 23 p., https://doi.org/10.3133/wsp1619CC.","productDescription":"iii, 23 p.","numberOfPages":"29","temporalStart":"1956-01-01","temporalEnd":"1960-12-31","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":137783,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1619cc/report-thumb.jpg"},{"id":28284,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619cc/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28285,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1619cc/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"125000","country":"United States","state":"Idaho","otherGeospatial":"Raft River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -113.6014,41.9942 ], [ -113.6014,42.6996 ], [ -113.1303,42.6996 ], [ -113.1303,41.9942 ], [ -113.6014,41.9942 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d9b8","contributors":{"authors":[{"text":"Mundorff, Maurice John","contributorId":41404,"corporation":false,"usgs":true,"family":"Mundorff","given":"Maurice","email":"","middleInitial":"John","affiliations":[],"preferred":false,"id":145070,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sisco, H.G.","contributorId":54185,"corporation":false,"usgs":true,"family":"Sisco","given":"H.G.","email":"","affiliations":[],"preferred":false,"id":145071,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2044,"text":"wsp1606 - 1963 - Geology and ground-water resources of Montgomery County, Alabama","interactions":[],"lastModifiedDate":"2022-02-02T15:02:35.456462","indexId":"wsp1606","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":"1606","title":"Geology and ground-water resources of Montgomery County, Alabama","docAbstract":"Montgomery County includes an area of 790 square miles in east-central Alabama. The economy of Montgomery County is related primarily to the growing and processing of agricultural products.
The county is in the northern part of the Coastal Plain. It consists of parts of four divisions of the Coastal Plain: the terraces, the Black Prairie, the Chunnennuggee Hills, and the flood plains. The county drains north and northwest into the Alabama and Tallapoosa Rivers, except for a small area in the southern part of the county that is drained by tributaries of the Conecuh River.
Sedimentary rocks of Late Cretaceous age underlie Montgomery County. They are divided, in ascending order, into the following: Coker and Gordo formations of the Tuscaloosa group; Eutaw formation; and Mooreville and Demopolis chalks, Ripley formation, Prairie Bluff chalk, and Providence sand of the Selma group. The Clayton formation of Tertiary age crops out in a small area in the southern part of the county. Pleistocene terrace deposits of the ancestral Alabama River overlie the older rocks in the northern part of the county. Recent alluvium underlies the flood plains of the larger streams. The Cretaceous and younger rocks consist chiefly of clay, chalk, sandstone, sand, and gravel, and a few thin beds of limestone. These deposits are underlain by a basement complex of pre-Cretaceous crystalline rocks.
Large-scale withdrawals of water began in the Montgomery area about 1885. Pumpage by the city of Montgomery in 1958 averaged about 15 million gallons per day. It is estimated that an additional 10 to 15 million gallons per day was pumped in the county for industrial, irrigation, domestic, and stock use.
The principal aquifer in the country is the Eutaw formation. It supplies water to the city of Montgomery municipal wells, to industrial wells in the Montgomery area, and to most domestic and stock wells in the northern two-thirds of the county. Irrigation wells also tap the Eutaw. Yields from wells range from 350 to 600 gallons per minute.
The Gordo formation, the upper part of the Coker formation, and the Pleistocene terrace deposits in the Montgomery area also yield moderate to large quantities of water to municipal and industrial wells. The lower part of the Coker formation is not developed as a source of water supply, but information obtained during the investigation rthat led to this report indicates that it may be a potential source of water to wells of large capacity. Sand beds in the Ripley formation, Providence sand, and Recent alluvium in -the southern part of the county yield adequate amounts of water to domestic and stock wells.
Most of the ground water used in Montgomery County occurs under artesian conditions, although water-table conditions occur in the Pleistocene terrace deposits and Recent alluvium, and in the outcrop areas of the Eutaw and Eipley formations and the Providence sand.
Most of the water recharging the Ooker, Gordo, and Eutaw formations in their areas of outcrop also is discharged in these areas; only a small quantity of water moves downdip beneath the overlying chalk beds. The natural discharge, and hence the natural recharge, is estimated to be 0.2 to 0.3 million gallons per day per square mile of outcrop.
All ground water in the county is of chemical quality that is satisfactory for most uses, although locally it is high in iron or chloride content and is hard. Water from the Eutaw formation a few miles southwest of Montgomery's West well field is very high in chloride content. This water moves toward the cone of depression in the piezometric surface produced by pumping in the West well field.
Much additional ground water could be pumped from the Eutaw formation, especially south of Montgomery's West well field. Additional water also is available from the upper part of the Coker formation. Before large groundwater developments are planned, however, the problems of well spacing and pumping rates should be studied in order to determine the maximum development permitted by the supply. Observation wells should be installed in the Eutaw formation southwest of Montgomery's West well field to detect encroachment of water of high chloride content from adjacent Lowndes County.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1606","collaboration":"Prepared in cooperation with the Water Works and Sanitary Sewer Board of the City of Montgomery and the Geological Survey of Alabama","usgsCitation":"Knowles, D.B., Reade, H., and Scott, J.C., 1963, Geology and ground-water resources of Montgomery County, Alabama: U.S. Geological Survey Water Supply Paper 1606, Report: v, 76 p.; 15 Plates: 45.58 x 25.01 inches or smaller, https://doi.org/10.3133/wsp1606.","productDescription":"Report: v, 76 p.; 15 Plates: 45.58 x 25.01 inches or smaller","costCenters":[],"links":[{"id":27553,"rank":414,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1606/plate-15.pdf","text":"Plate 15","size":"544.75 kB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 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