No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6765","usgsCitation":"Colton, R.B., 1967, Sand and gravel pit data sheets and location map for the Torrington quadrangle, Connecticut: U.S. Geological Survey Open-File Report 67-65, Report: 46 p.; 1 Plate: 20.83 x 27.16 inches, https://doi.org/10.3133/ofr6765.","productDescription":"Report: 46 p.; 1 Plate: 20.83 x 27.16 inches","costCenters":[],"links":[{"id":490873,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1967/0065/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145300,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1967/0065/report-thumb.jpg"},{"id":492931,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8237.htm","linkFileType":{"id":5,"text":"html"}},{"id":490874,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0065/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Connecticut","otherGeospatial":"Torrington quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -71.86019897460938,\n 41.32242759476505\n ],\n [\n -71.83101654052734,\n 41.34176252711261\n ],\n [\n -71.83067321777344,\n 41.35104125623227\n ],\n [\n -71.83685302734375,\n 41.355680124938715\n ],\n [\n -71.83856964111328,\n 41.365987538503056\n ],\n [\n -71.83273315429688,\n 41.3698523976995\n ],\n [\n -71.83273315429688,\n 41.38865810163064\n ],\n [\n -71.84200286865234,\n 41.39664244054911\n ],\n [\n -71.84234619140625,\n 41.41157824719922\n ],\n 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]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdd13","contributors":{"authors":[{"text":"Colton, Roger B.","contributorId":17967,"corporation":false,"usgs":true,"family":"Colton","given":"Roger","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":167300,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1984,"text":"wsp1696E - 1967 - Determination of Strontium-90 in water","interactions":[],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1696E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"1696","chapter":"E","title":"Determination of Strontium-90 in water","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1696E","usgsCitation":"Johnson, J.O., and Edwards, K., 1967, Determination of Strontium-90 in water: U.S. Geological Survey Water Supply Paper 1696, iii, 10 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1696E.","productDescription":"iii, 10 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":137682,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1696e/report-thumb.jpg"},{"id":27368,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1696e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db66794d","contributors":{"authors":[{"text":"Johnson, J. O.","contributorId":97480,"corporation":false,"usgs":true,"family":"Johnson","given":"J.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":144477,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Edwards, K.W.","contributorId":14375,"corporation":false,"usgs":true,"family":"Edwards","given":"K.W.","email":"","affiliations":[],"preferred":false,"id":144476,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1112,"text":"wsp1836 - 1967 - Ground-water conditions and geologic reconnaissance of the Upper Sevier River basin, Utah","interactions":[],"lastModifiedDate":"2017-09-04T17:41:05","indexId":"wsp1836","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"1836","title":"Ground-water conditions and geologic reconnaissance of the Upper Sevier River basin, Utah","docAbstract":"The upper Sevier River basin is in south-central Utah and includes an area of about 2,400 .square miles of high plateaus and valleys. It comprises the entire Sevier River drainage basin above Kingston, including the East Fork Sevier River and its tributaries. The basin was investigated to determine general ground-water conditions, the interrelation of ground water and surface water, the effects of increasing the pumping of ground water, and the amount of ground water in storage.
The basin includes four main valleys - Panguitch Valley, Circle Valley, East Fork Valley, and Grass Valley - which are drained by the Sevier River, the East Fork Sevier River, and Otter Creek. The plateaus surrounding the valleys consist of sedimentary and igneous rocks that range in age from Triassic to Quaternary. The valley fill, which is predominantly alluvial gravel, sand, silt, and clay, has a maximum thickness of more than 800 feet.
The four main valleys constitute separate ground-water basins. East Fork Valley basin is divided into Emery Valley, Johns Valley, and Antimony subbasins, and Grass Valley basin is divided into Koosharem and Angle subbasins. Ground water occurs under both artesian and water-table conditions in all the basins and subbasins except Johns Valley, Emery Valley, and Angle subbasins, where water is only under water-table conditions. The water is under artesian pressure in beds of gravel and sand confined by overlying beds of silt and clay in the downstream parts of Panguitch Valley basin, Circle Valley basin, and Antimony subbasin, and in most of Koosharem subbasin. Along the sides and upstream ends of these basins, water is usually under water-table conditions.
About 1 million acre-feet of ground water that is readily available to wells is stored in the gravel and sand of the upper 200 feet of saturated valley fill. About 570,000 acre-feet is stored in Panguitch Valley basin, about 210,000 in Circle Valley basin, about 6,000 in Emery Valley subbasin, about 90,000 in Johns Valley subbasin, about 36,000 in Antimony subbasin, about 90,000 in Koosharem subbasin, and about 60,000 in Angle subbasin. Additional water, although it is not readily available to wells, is stored in beds of silt and clay. Some ground water also is available in the bedrock underlying and surrounding the basins, although the bedrock formations generally are poor aquifers.
The principal source of recharge to the valley fill in the upper Sevier River basin is infiltration from streams, canals, and irrigated fields. Some ground water also miles into the valley till from the bedrock surrounding the basins.
The basin contains about 300 wells, most of which are less than 4 inches in diameter, are less than 250 feet deep, and are used for domestic purposes and stock watering. More than half the wells are flowing wells in Koosharem subbasin.
Approximately 82,000 acre-feet of ground water was discharged in 1962 from the valley till. Springs discharged about 33,000 acre-feet, wells about 3,000, and drains about 3,000; and evapotranspiration from phreatophyte areas about 43,000 acre-feet. Springs in bedrock discharged an additional 75,000 acre-feet. Most of the water discharged by springs, wells, and drains was used for irrigation.
The ground water in the basin generally is of good chemical quality. The water is excellent for irrigation and stock but is not as desirable for most domestic and industrial uses because of its hardness. The dissolved-solids content of the ground water generally increases slightly from the upstream end of the individual ground-water basins to. the downstream end owing mostly to repeated use of the water for irrigation.
Surface water and ground water in the upper Sevier River basin are inter- connected, and the base flows of streams are affected by changes in ground- water levels. Increased pumping of ground water would result in (1) an increase in the recharge to the aquifers from surface-water sources or (2) a decrease in the discharge from streams, springs, flowing wells, and areas of phreatophytes or (3) a combination of these.
About 43,000 acre-feet of ground water is now discharged annually by evapotranspiration from phreatophyte areas, and perhaps one-third of this loss, or about 14,000 acre-feet, could be salvaged by eliminating wet areas and phreatophytes. The areas where water could be salvaged are at the downstream ends of Panguitch Valley basin, Circle Valley basin, and Antimony subbasin. Most of the 14,000 acre-feet 'of water could be pumped from large-diameter wells or developed by properly designed drains without greatly affecting stream- flow and with only moderate effect on 'spring discharge. If the wells were properly located, the pumping would lower water levels and dry up wet areas where phreatophytes grow. Conjunctive use of ground water and surface water would facilitate the more efficient use of all water resources in the basin
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1836","collaboration":"Prepared in cooperation with the Utah State Engineer","usgsCitation":"Carpenter, C.H., Robinson, G., and Bjorklund, L.J., 1967, Ground-water conditions and geologic reconnaissance of the Upper Sevier River basin, Utah: U.S. Geological Survey Water Supply Paper 1836, Report: vi, 91 p.; 3 Plates: 35.00 in. x 49.87 in. or smaller, https://doi.org/10.3133/wsp1836.","productDescription":"Report: vi, 91 p.; 3 Plates: 35.00 in. x 49.87 in. or smaller","numberOfPages":"98","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":138011,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1836/report-thumb.jpg"},{"id":25869,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1836/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Reconnaissance geologic map and sections of the Upper Sevier River Basin, Utah"},{"id":25870,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1836/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing hydrologic data and phreatophyte areas in the Upper Sevier River Basin, Utah"},{"id":25871,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1836/plate-3.pdf","text":"Plate 3","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Graphs of water levels in selected wells and selected analyses of ground and surface water in the Upper Sevier River Basin, Utah"},{"id":25872,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1836/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","otherGeospatial":"Upper Sevier River Basin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d2be","contributors":{"authors":[{"text":"Carpenter, Carl H.","contributorId":46074,"corporation":false,"usgs":true,"family":"Carpenter","given":"Carl","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":143197,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robinson, Gerald B.","contributorId":46497,"corporation":false,"usgs":true,"family":"Robinson","given":"Gerald B.","affiliations":[],"preferred":false,"id":143198,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bjorklund, Louis Jay","contributorId":21138,"corporation":false,"usgs":true,"family":"Bjorklund","given":"Louis","email":"","middleInitial":"Jay","affiliations":[],"preferred":false,"id":143196,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1344,"text":"wsp1535M - 1967 - Annual variations in chemical composition of atmospheric precipitation, eastern North Carolina and southeastern Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:05:13","indexId":"wsp1535M","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"1535","chapter":"M","title":"Annual variations in chemical composition of atmospheric precipitation, eastern North Carolina and southeastern Virginia","docAbstract":"A 2-year study of precipitation composition over eastern North Carolina and southeastern Virginia has been completed. Chemical analyses were made of the major ions in monthly rainfall samples from each of 12 sampling locations. Areal and seasonal distributions were determined for chloride, calcium, magnesium, sodium, potassium, sulfate, and nitrate. \r\n\r\nAnnual changes in loads and in geographical distribution of sulfate and of nitrate are small. Yearly rainfall sulfate loads amount to approximately 7 tons per square mile, whereas deposition of nitrate is about 2 tons per square mile per year in the interior of the network and less near the coast. Areal patterns of chloride content are consistent with the assumption that the ocean is the only major source of rainfall chloride in the area. Chloride loads were 2.1 and 1.8 tons per square mile per year; the difference can be attributed to meteorological conditions. \r\n\r\nCation concentrations in network precipitation appear to depend on localized sources, probably soil dust. Annual loads of the major cations are approximately 2 tons per square mile of calcium, 1.8 tons per square mile of sodium, 0.5 ton per square mile of magnesium, and 0.3 ton per square mile of potassium; considerable year-to-year differences were noted in these values. \r\n\r\nBicarbonate and hydrogen ion in network rainfall are closely related to the relative concentrations of sulfate and calcium. Apparently, reaction of an acidic sulfur-containing aerosol with an alkaline calcium source is one of the principal controls on precipitation alkalinity and pH. \r\n\r\nIons in precipitation contribute substantially to the quality of surface water in the network area. Comparisons between precipitation input and stream export of ions for four North Carolina rivers show that rainfall sulfate is equal to sulfate discharged, whereas nitrate in rain slightly exceeds stream nitrate. Contributions of cations to the streams by way of precipitation range from about 20 percent for potassium to almost 50 percent for calcium. \r\n\r\nChloride deposited by precipitation amounts to about one-fourth of the stream load. Additions of manufactured salt may account for much of the remainder of the surface-water load.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1535M","usgsCitation":"Fisher, D.W., 1967, Annual variations in chemical composition of atmospheric precipitation, eastern North Carolina and southeastern Virginia: U.S. Geological Survey Water Supply Paper 1535, iv, 21 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1535M.","productDescription":"iv, 21 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":137452,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1535m/report-thumb.jpg"},{"id":26415,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1535m/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b7b9","contributors":{"authors":[{"text":"Fisher, Donald W.","contributorId":106468,"corporation":false,"usgs":true,"family":"Fisher","given":"Donald","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":143597,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":977,"text":"wsp1576H - 1967 - Ground-water resources of the southern part of Jicarilla Apache Indian Reservation and adjacent areas, New Mexico","interactions":[{"subject":{"id":52217,"text":"ofr626 - 1962 - Geology and ground-water resources of the southern part of the Jicarilla Apache Indian Reservation and adjacent region to the south and east, New Mexico","indexId":"ofr626","publicationYear":"1962","noYear":false,"title":"Geology and ground-water resources of the southern part of the Jicarilla Apache Indian Reservation and adjacent region to the south and east, New Mexico"},"predicate":"SUPERSEDED_BY","object":{"id":977,"text":"wsp1576H - 1967 - Ground-water resources of the southern part of Jicarilla Apache Indian Reservation and adjacent areas, New Mexico","indexId":"wsp1576H","publicationYear":"1967","noYear":false,"chapter":"H","title":"Ground-water resources of the southern part of Jicarilla Apache Indian Reservation and adjacent areas, New Mexico"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:16","indexId":"wsp1576H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"H","title":"Ground-water resources of the southern part of Jicarilla Apache Indian Reservation and adjacent areas, New Mexico","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1576H","usgsCitation":"Baltz, E.H., and West, S.W., 1967, Ground-water resources of the southern part of Jicarilla Apache Indian Reservation and adjacent areas, New Mexico: U.S. Geological Survey Water Supply Paper 1576, iv, 89 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1576H.","productDescription":"iv, 89 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":137076,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1576h/report-thumb.jpg"},{"id":25543,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1576h/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25544,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1576h/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25545,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1576h/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25546,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1576h/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25547,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1576h/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25548,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1576h/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a47f","contributors":{"authors":[{"text":"Baltz, Elmer Harold","contributorId":22313,"corporation":false,"usgs":true,"family":"Baltz","given":"Elmer","email":"","middleInitial":"Harold","affiliations":[],"preferred":false,"id":142955,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"West, Samuel Wilson","contributorId":24763,"corporation":false,"usgs":true,"family":"West","given":"Samuel","email":"","middleInitial":"Wilson","affiliations":[],"preferred":false,"id":142956,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":985,"text":"wsp1849 - 1967 - Roughness characteristics of natural channels","interactions":[],"lastModifiedDate":"2017-06-21T09:54:47","indexId":"wsp1849","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"1849","title":"Roughness characteristics of natural channels","docAbstract":"Color photographs and descriptive data are presented for 50 stream channels for which roughness coefficients have been determined. \r\n\r\nAll hydraulic computations involving flow in open channels require an evaluation of the roughness characteristics of the channel. In the absence of a satisfactory quantitative procedure this evaluation remains chiefly an art. The ability to evaluate roughness coefficients must be developed through experience. One means of gaining this experience is by examining and becoming acquainted with the appearance of some typical channels whose roughness coefficients are known. \r\n\r\nThe photographs and data contained in this report represent a wide range of channel conditions. Familiarity with the appearance, geometry, and roughness characteristics of these channels will improve the engineer's ability to select roughness coefficients for other channels .","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1849","usgsCitation":"Barnes, H.H., 1967, Roughness characteristics of natural channels: U.S. Geological Survey Water Supply Paper 1849, vi, 213 p. :illus. (part col.) ;24 cm., https://doi.org/10.3133/wsp1849.","productDescription":"vi, 213 p. :illus. (part col.) ;24 cm.","costCenters":[],"links":[{"id":136116,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":342703,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/wsp_1849/pdf/wsp_1849.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":8,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wsp1849/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fe1e9","contributors":{"authors":[{"text":"Barnes, Harry Hawthorne","contributorId":64630,"corporation":false,"usgs":true,"family":"Barnes","given":"Harry","email":"","middleInitial":"Hawthorne","affiliations":[],"preferred":false,"id":142968,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68350,"text":"ha176 - 1967 - Availability of ground water in parts of the Olmsted and Bandana quadrangles, in Jackson Purchase region, Kentucky","interactions":[],"lastModifiedDate":"2021-10-26T19:49:29.531192","indexId":"ha176","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"176","title":"Availability of ground water in parts of the Olmsted and Bandana quadrangles, in Jackson Purchase region, Kentucky","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha176","usgsCitation":"Hansen, A., 1967, Availability of ground water in parts of the Olmsted and Bandana quadrangles, in Jackson Purchase region, Kentucky: U.S. Geological Survey Hydrologic Atlas 176, 1 Plate: 39.50 × 55.00 inches, https://doi.org/10.3133/ha176.","productDescription":"1 Plate: 39.50 × 55.00 inches","costCenters":[],"links":[{"id":188897,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":390983,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15538.htm"},{"id":89826,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/176/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Kentucky","otherGeospatial":"Olmsted and Bandana quadrangles","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -89.1,37.125 ], [ -89.1,37.217 ], [ -88.875,37.217 ], [ -88.875,37.125 ], [ -89.1,37.125 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d8c2","contributors":{"authors":[{"text":"Hansen, Arnold J.","contributorId":33316,"corporation":false,"usgs":true,"family":"Hansen","given":"Arnold J.","affiliations":[],"preferred":false,"id":278073,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":32573,"text":"pp560C - 1967 - Geology of the Arabian Peninsula; Aden Protectorate","interactions":[],"lastModifiedDate":"2012-02-02T00:09:09","indexId":"pp560C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"560","chapter":"C","title":"Geology of the Arabian Peninsula; Aden Protectorate","language":"ENGLISH","doi":"10.3133/pp560C","usgsCitation":"Greenwood, J., and Bleackley, D., 1967, Geology of the Arabian Peninsula; Aden Protectorate: U.S. Geological Survey Professional Paper 560, p. C1-C96; 2 plates in pocket, https://doi.org/10.3133/pp560C.","productDescription":"p. C1-C96; 2 plates in pocket","costCenters":[],"links":[{"id":121418,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0560c/report-thumb.jpg"},{"id":60397,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0560c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60398,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0560c/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60399,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0560c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6835bc","contributors":{"authors":[{"text":"Greenwood, J.E.","contributorId":21593,"corporation":false,"usgs":true,"family":"Greenwood","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":208707,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bleackley, D.","contributorId":61080,"corporation":false,"usgs":true,"family":"Bleackley","given":"D.","email":"","affiliations":[],"preferred":false,"id":208708,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":13827,"text":"ofr6794 - 1967 - Geology of the Coama area, Puerto Rico: with comments on Greater Antillean volcanic island arc-trench phenomena","interactions":[{"subject":{"id":13827,"text":"ofr6794 - 1967 - Geology of the Coama area, Puerto Rico: with comments on Greater Antillean volcanic island arc-trench phenomena","indexId":"ofr6794","publicationYear":"1967","noYear":false,"title":"Geology of the Coama area, Puerto Rico: with comments on Greater Antillean volcanic island arc-trench phenomena"},"predicate":"SUPERSEDED_BY","object":{"id":5950,"text":"pp636 - 1971 - Geology of the Coamo area, Puerto Rico, and its relation to the volcanic arc-trench association","indexId":"pp636","publicationYear":"1971","noYear":false,"title":"Geology of the Coamo area, Puerto Rico, and its relation to the volcanic arc-trench association"},"id":1}],"supersededBy":{"id":5950,"text":"pp636 - 1971 - Geology of the Coamo area, Puerto Rico, and its relation to the volcanic arc-trench association","indexId":"pp636","publicationYear":"1971","noYear":false,"title":"Geology of the Coamo area, Puerto Rico, and its relation to the volcanic arc-trench association"},"lastModifiedDate":"2012-02-02T00:06:43","indexId":"ofr6794","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"67-94","title":"Geology of the Coama area, Puerto Rico: with comments on Greater Antillean volcanic island arc-trench phenomena","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr6794","usgsCitation":"Glover, L., 1967, Geology of the Coama area, Puerto Rico: with comments on Greater Antillean volcanic island arc-trench phenomena: U.S. Geological Survey Open-File Report 67-94, 329 p. ill., maps ;29 cm. +portfolio (ill., maps, mounted photos.), 38 cm., https://doi.org/10.3133/ofr6794.","productDescription":"329 p. ill., maps ;29 cm. +portfolio (ill., maps, mounted photos.), 38 cm.","costCenters":[],"links":[{"id":145199,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad1e4b07f02db680e61","contributors":{"authors":[{"text":"Glover, Lynn","contributorId":6046,"corporation":false,"usgs":true,"family":"Glover","given":"Lynn","affiliations":[],"preferred":false,"id":168465,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":34792,"text":"b1215AB - 1967 - Geology of Shawnee County, Kansas","interactions":[],"lastModifiedDate":"2021-08-23T12:14:20.609672","indexId":"b1215AB","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"1215","chapter":"A-B","title":"Geology of Shawnee County, Kansas","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/b1215AB","usgsCitation":"Johnson, W.D., Adkison, W.L., and Wagner, H.C., 1967, Geology of Shawnee County, Kansas: U.S. Geological Survey Bulletin 1215, Report: viii, 254 p.; 1 Table; 4 Plates: 31.50 × 41.50 inches or smaller, https://doi.org/10.3133/b1215AB.","productDescription":"Report: viii, 254 p.; 1 Table; 4 Plates: 31.50 × 41.50 inches or smaller","costCenters":[],"links":[{"id":109514,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21008.htm","linkFileType":{"id":5,"text":"html"},"description":"21008"},{"id":109513,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21007.htm","linkFileType":{"id":5,"text":"html"},"description":"21007"},{"id":166277,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1215a-b/report-thumb.jpg"},{"id":62690,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1215a-b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62691,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1215a-b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62692,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1215a-b/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62693,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1215a-b/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62694,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1215a-b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":247498,"rank":405,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/bul/1215a-b/plate-table_1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Kansas","county":"Shawnee County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-95.5901,39.2166],[-95.5872,39.1417],[-95.5887,39.1331],[-95.59,39.1305],[-95.5931,39.1273],[-95.5938,39.1246],[-95.5951,39.121],[-95.5964,39.1179],[-95.5961,39.112],[-95.5971,39.1016],[-95.5975,39.0767],[-95.5973,39.0658],[-95.5893,39.0583],[-95.5858,39.0564],[-95.5751,39.0575],[-95.5583,39.063],[-95.5524,39.0638],[-95.5405,39.0635],[-95.5266,39.0695],[-95.5195,39.0703],[-95.5118,39.0687],[-95.5049,39.064],[-95.504,39.0586],[-95.5021,38.9175],[-95.502,38.9039],[-95.5016,38.8703],[-95.9468,38.8712],[-95.9427,39.0892],[-95.9456,39.0925],[-95.9514,39.0967],[-95.9566,39.0995],[-95.9624,39.1023],[-95.9671,39.1056],[-95.9729,39.1094],[-95.977,39.1094],[-95.9829,39.1105],[-95.9865,39.111],[-95.99,39.1115],[-95.9929,39.1129],[-95.9951,39.1171],[-95.9932,39.122],[-95.9925,39.1234],[-95.9937,39.1252],[-95.9936,39.1261],[-95.9948,39.1261],[-95.9984,39.1257],[-96.0051,39.1218],[-96.0129,39.1174],[-96.0153,39.117],[-96.0195,39.1166],[-96.0259,39.1181],[-96.0277,39.1186],[-96.0359,39.1233],[-96.0338,39.2185],[-95.5901,39.2166]]]},\"properties\":{\"name\":\"Shawnee\",\"state\":\"KS\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683a00","contributors":{"authors":[{"text":"Johnson, William D. Jr.","contributorId":60294,"corporation":false,"usgs":true,"family":"Johnson","given":"William","suffix":"Jr.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":213594,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Adkison, Windsor Lester","contributorId":12846,"corporation":false,"usgs":true,"family":"Adkison","given":"Windsor","email":"","middleInitial":"Lester","affiliations":[],"preferred":false,"id":213593,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wagner, Holly Clyde","contributorId":96238,"corporation":false,"usgs":true,"family":"Wagner","given":"Holly","email":"","middleInitial":"Clyde","affiliations":[],"preferred":false,"id":213595,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":63483,"text":"gp597 - 1967 - Aeromagnetic and gravity profiles of the United States along the 37th parallel: A contribution to the upper mantle project","interactions":[],"lastModifiedDate":"2022-07-07T21:19:34.816372","indexId":"gp597","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"597","title":"Aeromagnetic and gravity profiles of the United States along the 37th parallel: A contribution to the upper mantle project","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp597","usgsCitation":"Zietz, I., and Kirby, J., 1967, Aeromagnetic and gravity profiles of the United States along the 37th parallel: A contribution to the upper mantle project: U.S. Geological Survey Geophysical Investigations Map 597, Report: 1 p.; 1 Plate: 43.69 × 30.54 inches, https://doi.org/10.3133/gp597.","productDescription":"Report: 1 p.; 1 Plate: 43.69 × 30.54 inches","costCenters":[],"links":[{"id":403239,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5964.htm"},{"id":253130,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0597/report-thumb.jpg"},{"id":249588,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0597/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":249587,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0597/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"2500000","country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -125,35 ], [ -125,39 ], [ -70,39 ], [ -70,35 ], [ -125,35 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db69849d","contributors":{"authors":[{"text":"Zietz, Isidore","contributorId":76708,"corporation":false,"usgs":true,"family":"Zietz","given":"Isidore","affiliations":[],"preferred":false,"id":268955,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kirby, J.R.","contributorId":6428,"corporation":false,"usgs":true,"family":"Kirby","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":268954,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":52573,"text":"ofr6771 - 1967 - Ground-water aspects of the lower Henrys Fork region, Idaho","interactions":[],"lastModifiedDate":"2013-11-19T10:29:25","indexId":"ofr6771","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"67-71","title":"Ground-water aspects of the lower Henrys Fork region, Idaho","docAbstract":"The lower Henrys Fork region includes the plains and low benches between Ashton and the junction of Henrys Fork and Snake River in eastern Idaho. The northwestern and western parts of the area are part of the Snake River lava plain. The central part of the area is occupied by alluvial plains of the Snake, Teton, and Falls Rivers, and Henrys Fork. The southeastern part of the area is a bench (Rexburg Bench), chiefly on silicic and basaltic volcanic rocks, which rises gradually to mountain peaks southeast of the area. The basalt, and the sand and gravel under the alluvial plains are good aquifers and yield large amounts of water with small drawdowns. The silicic volcanic rocks and the interbedded ash, pyroclastics, and sedimentary deposits generally yield much less water than the basalt and alluvium. The regional water table slopes southward beneath the basalt and alluvial plains. Seepage from stream channels and irrigated tracts has resulted in an extensive body of ground water perched above the regional water table. The perched water in part moves vertically down to the regional water table and in part laterally to the streams. Ground water beneath the Rexburg Bench moves generally northwestward to join the regional ground-water body beneath the alluvial plain. The regional water table is below the level of the streams in the area and ground water in the main aquifer, therefore is not tributary to the streams. Recharge to the regional water table is estimated to average 725,000 acre-feet annually. Pumping from the regional ground-water reservoir for irrigation or other uses would have no effect on streamflow or surface-water rights within the study area. However, depletion of the underflow would eventually reduce the inflow to American Falls Reservoir unless the depletion was offset by additional recharge. Total withdrawals of ground water for irrigation in 1962 were estimated to be 25,000 acre-feet and caused no significant decline in the water table. In the Ashton area surface-water irrigation has cause water to be perched in basalt above the silicic volcanic rocks and much of this perched water contributed to streamflow. The flow of Henrys Fork would be decreased by the amount of pumped ground water consumed by crops. 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