{"pageNumber":"5834","pageRowStart":"145825","pageSize":"25","recordCount":165658,"records":[{"id":2778,"text":"wsp1608I - 1968 - Fresh and saline ground-water zones in the Punjab region, West Pakistan","interactions":[],"lastModifiedDate":"2012-02-02T00:05:29","indexId":"wsp1608I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"1608","chapter":"I","title":"Fresh and saline ground-water zones in the Punjab region, West Pakistan","docAbstract":"An extensive program of test drilling and water sampling, undertaken by the Water and Soils Investigation Division (WASID) of the West Pakistan Water and Power Development Authority (WAPDA) to evaluate hydrologic problems related to waterlogging and soil salinity, has furnished data for the delineation of fresh and saline ground-water zones in the Punjab region of West Pakistan. Fresh ground water containing generally less than 500 ppm (parts per million) of total dissolved solids is found in wide belts paralleling the major rivers and in other areas of ground-water recharge. The fresh groundwater zone of upper (northeastern) Rechna Doab, where annual precipitation in places exceeds 30 inches, is the most extensive of the Punjab region and attains a depth of 1,700 feet or more below land surface near Gujranwala. Fresh ground water adjacent to the Indus River extends locally to depths of about \r\nl,500 feet. \r\n\r\nSaline ground water occurs downgradient from sources of recharge, particularly in the central parts of the interfluvial areas. Also, available data indicate a gradual increase in mineralization with depth and distance from sources of fresh-water recharge. Thus, even extensive fresh-water zones appear to be underlain, at variable depths, by saline ground water in most of the Punjab region. The saline ground waters of the Punjab region do not constitute, however, a distinct salt-water body that can be defined in terms of stratigraphic position, sea-level datum, particular lithology, or by chemical character. \r\n\r\nThe ground waters of the Punjab region are characterized by a gradation from calcium magnesium bicarbonate types, near the sources of recharge, to waters containing a dominant proportion of sodium. Water containing from 500 to 1,000 ppm is commonly of the sodium bicarbonate type, or it may be of the mixed type, having about equal proportions of the common anions (bicarbonate, chloride, and sulfate). With increasing mineralization from about 1,000 to 3,000 ppm, ,the relative proportion of chloride and sulfate increases, and these waters are generally of the sodium chloride or sodium sulfate type. The highly mineralized waters of the Punjab region are generally of the sodium chloride type, whereas in Dera Ismail (D.I.) Khan District sodium sulfate waters predominate. The ground waters from more than 900 sampling sites have been classified into eight types, according to dominant cations and anions. These types have been further subdivided into groups containing different amounts of total dissolved solids. \r\n\r\nThe pattern of distribution of saline ground-water zones in the Punjab region and the observed gradual increase in mineral content, downgradient from sources of fresh-water recharge, can be explained best by the processes of evaporation from the water table and solution of minerals within the alluvial aquifer.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1608I","usgsCitation":"Swarzenski, W., 1968, Fresh and saline ground-water zones in the Punjab region, West Pakistan: U.S. Geological Survey Water Supply Paper 1608, iii, 24 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1608I.","productDescription":"iii, 24 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":138679,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1608i/report-thumb.jpg"},{"id":29226,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1608i/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29227,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1608i/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29228,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1608i/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29229,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1608i/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a83a7","contributors":{"authors":[{"text":"Swarzenski, W.V.","contributorId":80243,"corporation":false,"usgs":true,"family":"Swarzenski","given":"W.V.","email":"","affiliations":[],"preferred":false,"id":145772,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2614,"text":"wsp1757J - 1968 - Ground-water geology of Kordofan Province, Sudan","interactions":[],"lastModifiedDate":"2012-02-02T00:05:28","indexId":"wsp1757J","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"1757","chapter":"J","title":"Ground-water geology of Kordofan Province, Sudan","docAbstract":"For much of Kordofan Province, surface-water supplies collected and stored in hafirs, fulas, and tebeldi trees are almost completely appropriated for present needs, and water from wells must serve as the base for future economic and cultural development. This report describes the results of a reconnaissance hydrogeologic investigation of the Province and the nature and distribution of the ground-water resources with respect to their availability for development. Kordofan Province, in central Sudan, lies within the White Nile-Nile River drainage basin. The land surface is largely a plain of low relief; jebels (hills) occur sporadically, and sandy soils are common in most areas except in the south where clayey soils predominate. Seasonal rainfall, ranging from less than 100 millimeters in the north to about 800 millimeters in the south, occurs almost entirely during the summer months, but little runoff ever reaches the Nile or White Nile Rivers. \r\n\r\nThe rocks beneath the surficial depsits (Pleistocene to Recent) in the Province comprise the basement complex (Precambrian), Nawa Series (upper Paleozoic), Nubian Series (Mesozoic), laterite (lower to middle Tertiary), and the Umm Ruwaba Series (Pliocene to Pleistocene). \r\n\r\nPerennial ground-water supplies in the Province are found chiefly in five hydrologic units, each having distinct geologic or hydrologic characteristics. These units occur in Nubian or Umm Ruwaba strata or both, and the sandstone and conglomerate beds form the :principal aquifers. The water is generally under slight artesian head, and the upper surface of the zone of saturation ranges from about 50 meters to 160 meters below land surface. The surficial deposits and basement rocks are generally poor sources of ground water in most of the Province. Supplies from such sources are commonly temporary and may dissipate entirely during the dry season. Locally, however, perennial supplies are obtained from the surficial deposits and from the basement rocks. \r\n\r\nGenerally, water from Nubian aquifers is satisfactory for most uses and is of better quality than that obtained from Umm Ruwaba aquifers. The relatively high mineralization of water from the Umm Ruwaba, especially in the eastern \r\npart of the Province, makes the water unsuitable for many municipal ad industrial uses. The water is generally usable, however, for domestic and livestock purposes. \r\n\r\nSome 175 drilled wells located at 75 water yards yield an average, of about 1,000 imperial gallons .per hour per well from Nubian or Umm Ruwaba. aquifers. Generally the water yards provide sufficient water for minimum domestic and livestock requirements throughout the year. Commonly, however, the water yards are widely separated and, hence, not always properly spaced for good range management or for serving the needs of the dispersed rural population. In 1962, withdrawals from Nubian and Umm Ruwaba aquifers in the Province were approximately 600 million gallons annually. This rate of draft: could probably be continued almost indefinitely without significant depletion of the water supply. Nubian and Umm Ruwaba aquifers in the southwestern part of Kordofan offer excellent potential for future development. Nubian aquifers in northern Kordofan need extensive exploration by test drilling before their economic potential can be properly evaluated.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1757J","usgsCitation":"Rodis, H.G., Hassan, A., and Wahadan, L., 1968, Ground-water geology of Kordofan Province, Sudan: U.S. Geological Survey Water Supply Paper 1757, iv, 48 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1757J.","productDescription":"iv, 48 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":138833,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1757j/report-thumb.jpg"},{"id":28903,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1757j/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28904,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1757j/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668d8e","contributors":{"authors":[{"text":"Rodis, Harry G.","contributorId":25141,"corporation":false,"usgs":true,"family":"Rodis","given":"Harry","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":145495,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hassan, Abdulla","contributorId":102866,"corporation":false,"usgs":true,"family":"Hassan","given":"Abdulla","email":"","affiliations":[],"preferred":false,"id":145497,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wahadan, Lutfi","contributorId":64231,"corporation":false,"usgs":true,"family":"Wahadan","given":"Lutfi","email":"","affiliations":[],"preferred":false,"id":145496,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":43374,"text":"ofr6872 - 1968 - Geology of the Iliamna quadrangle, Alaska","interactions":[{"subject":{"id":43374,"text":"ofr6872 - 1968 - Geology of the Iliamna quadrangle, Alaska","indexId":"ofr6872","publicationYear":"1968","noYear":false,"title":"Geology of the Iliamna quadrangle, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":34195,"text":"b1368B - 1980 - Stratigraphy, structure, and economic geology of the Iliamna Quadrangle, Alaska","indexId":"b1368B","publicationYear":"1980","noYear":false,"chapter":"B","title":"Stratigraphy, structure, and economic geology of the Iliamna Quadrangle, Alaska"},"id":1}],"supersededBy":{"id":34195,"text":"b1368B - 1980 - Stratigraphy, structure, and economic geology of the Iliamna Quadrangle, Alaska","indexId":"b1368B","publicationYear":"1980","noYear":false,"title":"Stratigraphy, structure, and economic geology of the Iliamna Quadrangle, Alaska"},"lastModifiedDate":"2012-02-02T00:10:10","indexId":"ofr6872","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"68-72","title":"Geology of the Iliamna quadrangle, Alaska","language":"ENGLISH","doi":"10.3133/ofr6872","usgsCitation":"Detterman, R.L., and Reed, B.L., 1968, Geology of the Iliamna quadrangle, Alaska: U.S. Geological Survey Open-File Report 68-72, 1 map, https://doi.org/10.3133/ofr6872.","productDescription":"1 map","costCenters":[],"links":[{"id":106420,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8345.htm","linkFileType":{"id":5,"text":"html"},"description":"8345"},{"id":161906,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"250000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67fef9","contributors":{"authors":[{"text":"Detterman, Robert L.","contributorId":71526,"corporation":false,"usgs":true,"family":"Detterman","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":228110,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reed, Bruce L.","contributorId":19928,"corporation":false,"usgs":true,"family":"Reed","given":"Bruce","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":228109,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":23609,"text":"ofr68160 - 1968 - Applications of aerial photography and remote sensing to hydrobiological research in South Florida","interactions":[],"lastModifiedDate":"2025-04-17T14:11:35.589319","indexId":"ofr68160","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"68-160","title":"Applications of aerial photography and remote sensing to hydrobiological research in South Florida","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U. S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr68160","issn":"0094-9140","usgsCitation":"Applications of aerial photography and remote sensing to hydrobiological research in South Florida; 1968; OFR; 68-160; Kolipinski, M. C.; Higer, A. L.","productDescription":"44 p.","costCenters":[],"links":[{"id":154893,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":484406,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1968/0160/ofr68_160_flofr68_009.pdf","text":"Report","size":"2.16 MB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -81.85402279727366,\n              26.760706851407733\n            ],\n            [\n              -81.85402279727366,\n              25.017287226070962\n            ],\n            [\n              -80.07457309190833,\n              25.017287226070962\n            ],\n            [\n              -80.07457309190833,\n              26.760706851407733\n            ],\n            [\n              -81.85402279727366,\n              26.760706851407733\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","contact":"<p><a href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","publishedDate":"1969-10-01","noUsgsAuthors":false,"publicationDate":"1969-10-01","publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a4e6","contributors":{"authors":[{"text":"Kolipinski, M.C.","contributorId":68769,"corporation":false,"usgs":true,"family":"Kolipinski","given":"M.C.","affiliations":[],"preferred":false,"id":190404,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Higer, A.L.","contributorId":8501,"corporation":false,"usgs":true,"family":"Higer","given":"A.L.","affiliations":[],"preferred":false,"id":190403,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1036,"text":"wsp1848 - 1968 - Ground-water resources of the Sevier River basin between Yuba Dam and Leamington Canyon, Utah","interactions":[],"lastModifiedDate":"2017-09-04T17:03:37","indexId":"wsp1848","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"1848","title":"Ground-water resources of the Sevier River basin between Yuba Dam and Leamington Canyon, Utah","docAbstract":"<p>The area investigated is a segment of the Sevier River basin, Utah, comprising about 900 square miles and including a 19-mile reach of the Sevier River between Yuba Dam and Leamington Canyon. The larger valleys in the area are southern Juab, Round, and Scipio Valleys. The smaller valleys are Mills, Little, Dog, and Tinctic Wash Valleys.</p><p>The geology of parts of Scipio, Little, and Mills Valleys and parts of the surrounding highlands was mapped and studied to explain the occurrence of numerous sinkholes in the thre valleys and to show their relation to the large springs in Mills Valley. The sinkholes, which are formed in the alluvium, are alined along faults, which penetrate both the alluvium and the underlying bedrock, and they have been formed by collapse of solution cavities in the underlying bedrock. The bedrock is mostly sandy limestone beds of the upper part of the North Horn Formation and of the Flagstaff Limestone. The numerous faults traversing Scipio Valley in a north-northeasterly direction trend directly toward Molter and Blue Springs in Mills Valley. One fault, which can be traced directly between the springs, probably is the principal channelway for the ground water moving from Scipio and Little Valleys to the springs.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1848","usgsCitation":"Bjorklund, L.J., and Robinson, G.B., 1968, Ground-water resources of the Sevier River basin between Yuba Dam and Leamington Canyon, Utah: U.S. Geological Survey Water Supply Paper 1848, Report: v, 79 p.; 2 Plates: 16.00 in. x 18.72 in. and 24.00 in. x 19.73 in., https://doi.org/10.3133/wsp1848.","productDescription":"Report: v, 79 p.; 2 Plates: 16.00 in. x 18.72 in. and 24.00 in. x 19.73 in.","numberOfPages":"83","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":137968,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1848/report-thumb.jpg"},{"id":25675,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1848/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Reconnaissance geologic map of parts of Scipio, Little, and Mills valleys, Sevier River Basin, Utah"},{"id":25676,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1848/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing hydrology and chemical quality of water, Sevier River basin between Yuba Dam and Leamington Canyon, Utah, 1963"},{"id":25677,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1848/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","otherGeospatial":"Leamington Canyon, Sevier River basin, Yuba Dam","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a666","contributors":{"authors":[{"text":"Bjorklund, Louis Jay","contributorId":21138,"corporation":false,"usgs":true,"family":"Bjorklund","given":"Louis","email":"","middleInitial":"Jay","affiliations":[],"preferred":false,"id":143070,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robinson, Gerald B. Jr.","contributorId":91837,"corporation":false,"usgs":true,"family":"Robinson","given":"Gerald","suffix":"Jr.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":143071,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68270,"text":"ha279 - 1968 - Geology and ground water in Labette County, Kansas","interactions":[],"lastModifiedDate":"2019-11-12T09:34:30","indexId":"ha279","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"279","title":"Geology and ground water in Labette County, Kansas","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ha279","usgsCitation":"Jungmann, W.L., and Williams, C.C., 1968, Geology and ground water in Labette County, Kansas: U.S. Geological Survey Hydrologic Atlas 279, 2 Plates: 37.50 x 49.75 inches and 6.00 x 7.50 inches, https://doi.org/10.3133/ha279.","productDescription":"2 Plates: 37.50 x 49.75 inches and 6.00 x 7.50 inches","costCenters":[],"links":[{"id":188554,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89675,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/279/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89676,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/279/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"6600","country":"United States","state":"Kansas","county":"Labette ","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -95.51788330078125,\n              37.00035919622158\n            ],\n            [\n              -95.06744384765625,\n              37.00035919622158\n            ],\n            [\n              -95.06744384765625,\n              37.385435182627226\n            ],\n            [\n              -95.51788330078125,\n              37.385435182627226\n            ],\n            [\n              -95.51788330078125,\n              37.00035919622158\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db686043","contributors":{"authors":[{"text":"Jungmann, William L.","contributorId":63885,"corporation":false,"usgs":true,"family":"Jungmann","given":"William","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":277942,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, Charles C.","contributorId":107367,"corporation":false,"usgs":true,"family":"Williams","given":"Charles","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":277943,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1306,"text":"wsp1696F - 1968 - Isotopic analysis of uranium in natural waters by alpha spectrometry","interactions":[],"lastModifiedDate":"2012-02-02T00:05:17","indexId":"wsp1696F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"F","title":"Isotopic analysis of uranium in natural waters by alpha spectrometry","docAbstract":"A method is described for the determination of U234/U238 activity ratios for uranium present in natural waters. The uranium is coprecipitated from solution with aluminum phosphate, extracted into ethyl acetate, further purified by ion exchange, and finally electroplated on a titanium disc for counting. The individual isotopes are determined by measurement of the alpha-particle energy spectrum using a high resolution low-background alpha spectrometer. Overall chemical recovery of about 90 percent and a counting efficiency of 25 percent allow analyses of water samples containing as little as 0.10 ?g/l of uranium. The accuracy of the method is limited, on most samples, primarily by counting statistics.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1696F","usgsCitation":"Edwards, K., 1968, Isotopic analysis of uranium in natural waters by alpha spectrometry: U.S. Geological Survey Water Supply Paper 1696, iv, 26 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1696F.","productDescription":"iv, 26 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":137888,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1696f/report-thumb.jpg"},{"id":26339,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1696f/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db667025","contributors":{"authors":[{"text":"Edwards, K.W.","contributorId":14375,"corporation":false,"usgs":true,"family":"Edwards","given":"K.W.","email":"","affiliations":[],"preferred":false,"id":143535,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1229,"text":"wsp1586I - 1968 - Salt-water encroachment in the South Edisto River Estuary, South Carolina","interactions":[],"lastModifiedDate":"2019-12-30T09:37:26","indexId":"wsp1586I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"1586","chapter":"I","title":"Salt-water encroachment in the South Edisto River Estuary, South Carolina","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. General Printing Office","doi":"10.3133/wsp1586I","usgsCitation":"Cummings, T.R., 1968, Salt-water encroachment in the South Edisto River Estuary, South Carolina: U.S. Geological Survey Water Supply Paper 1586, iv, 19 p. , https://doi.org/10.3133/wsp1586I.","productDescription":"iv, 19 p. ","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":137925,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1586i/report-thumb.jpg"},{"id":26147,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1586i/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"South Carolina","otherGeospatial":"South Edisto River Estuary","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.9637451171875,\n              32.16166284018013\n            ],\n            [\n              -80.321044921875,\n              32.16166284018013\n            ],\n            [\n              -80.321044921875,\n              32.648625783736726\n            ],\n            [\n              -80.9637451171875,\n              32.648625783736726\n            ],\n            [\n              -80.9637451171875,\n              32.16166284018013\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdedc","contributors":{"authors":[{"text":"Cummings, T. Ray","contributorId":20722,"corporation":false,"usgs":true,"family":"Cummings","given":"T.","email":"","middleInitial":"Ray","affiliations":[],"preferred":false,"id":143406,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":53410,"text":"ofr68129 - 1968 - Hydrogeologic study of the Soquel-Aptos area, Santa Cruz County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:11:44","indexId":"ofr68129","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"68-129","title":"Hydrogeologic study of the Soquel-Aptos area, Santa Cruz County, California","language":"ENGLISH","doi":"10.3133/ofr68129","usgsCitation":"Hickey, J.J., 1968, Hydrogeologic study of the Soquel-Aptos area, Santa Cruz County, California: U.S. Geological Survey Open-File Report 68-129, 48 p. : ill., fold. plates in pocket ; 27 cm., https://doi.org/10.3133/ofr68129.","productDescription":"48 p. : ill., fold. plates in pocket ; 27 cm.","costCenters":[],"links":[{"id":174996,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1968/0129/report-thumb.jpg"},{"id":87257,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0129/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87258,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1968/0129/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db6278ab","contributors":{"authors":[{"text":"Hickey, John J.","contributorId":39763,"corporation":false,"usgs":true,"family":"Hickey","given":"John","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":247543,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68318,"text":"ha271 - 1968 - Floods at Arecibo, Puerto Rico","interactions":[],"lastModifiedDate":"2012-02-10T00:11:28","indexId":"ha271","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"271","title":"Floods at Arecibo, Puerto Rico","language":"ENGLISH","doi":"10.3133/ha271","usgsCitation":"Hickenlooper, I.J., 1968, Floods at Arecibo, Puerto Rico: U.S. Geological Survey Hydrologic Atlas 271, 1 map., https://doi.org/10.3133/ha271.","productDescription":"1 map.","costCenters":[],"links":[{"id":185888,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89771,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/271/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"20000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -66.75,18.3675 ], [ -66.75,18.5 ], [ -66.61749999999999,18.5 ], [ -66.61749999999999,18.3675 ], [ -66.75,18.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e72be","contributors":{"authors":[{"text":"Hickenlooper, Irby J.","contributorId":103366,"corporation":false,"usgs":true,"family":"Hickenlooper","given":"Irby","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":278019,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55869,"text":"ofr68249 - 1968 - Site study for water well, Fort Wingate Army Ordnance Depot, McKinley County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:12:01","indexId":"ofr68249","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"68-249","title":"Site study for water well, Fort Wingate Army Ordnance Depot, McKinley County, New Mexico","language":"ENGLISH","doi":"10.3133/ofr68249","usgsCitation":"Shomaker, J., 1968, Site study for water well, Fort Wingate Army Ordnance Depot, McKinley County, New Mexico: U.S. Geological Survey Open-File Report 68-249, 28 p., 3 figs., https://doi.org/10.3133/ofr68249.","productDescription":"28 p., 3 figs.","costCenters":[],"links":[{"id":114677,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1968/0249/report.pdf","size":"751","linkFileType":{"id":1,"text":"pdf"}},{"id":114678,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0249/plate-2.pdf","size":"1022","linkFileType":{"id":1,"text":"pdf"}},{"id":114679,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0249/plate-3.pdf","size":"1061","linkFileType":{"id":1,"text":"pdf"}},{"id":182136,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1968/0249/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f157c","contributors":{"authors":[{"text":"Shomaker, J.W.","contributorId":58347,"corporation":false,"usgs":true,"family":"Shomaker","given":"J.W.","affiliations":[],"preferred":false,"id":254395,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":47997,"text":"ofr71343 - 1968 - Geology, hydrology, and geochemistry of the Black Creek watershed near Mocanaqua, Luzerne County, Pennsylvania","interactions":[],"lastModifiedDate":"2016-06-07T16:17:20","indexId":"ofr71343","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"71-343","title":"Geology, hydrology, and geochemistry of the Black Creek watershed near Mocanaqua, Luzerne County, Pennsylvania","docAbstract":"<p>The Black Creek watershed is in the southwestern end of the Northern Anthracite field in Luzerne County, northeastern Pennsylvania. 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