{"pageNumber":"6678","pageRowStart":"166925","pageSize":"25","recordCount":184900,"records":[{"id":1999,"text":"wsp1651 - 1964 - Chemical quality of surface waters and sedimentation in the Saline River basin, Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:05:22","indexId":"wsp1651","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1651","title":"Chemical quality of surface waters and sedimentation in the Saline River basin, Kansas","docAbstract":"This report gives the results of an investigation of the sediment and dissolved minerals that are transported by the Saline River and its tributaries. The Saline River basin is in western and central Kansas; it is long and narrow and covers 3,420 square miles of rolling plains, which is broken in some places by escarpments and small areas of badlands. In the western part the uppermost bedrock consists predominantly of calcareous elastic sedimentary rocks of continental origin of Pliocene age and in most places is covered by eolian deposits of Pleistocene and Recent age. In the central part the ex posed bedrock consists predominantly of calcareous marine sedimentary rocks of Late Cretaceous age. In the eastern part the exposed bedrock consists mainly of noncalcareous continental and littoral elastic sedimentary rocks of Early Cretaceous and Permian age. Fluvial deposits are in the valleys, and eolian materials are present over much of the uplands. \r\n\r\nAverage precipitation increases rather uniformly from about 18 inches per year in the west to almost 28 inches per year in the east. Runoff is not affected by irrigation nor regulated by large structures, but it is closely related to precipitation. Average runoff increases from less than 0.2 inch per year in the west to more than 1.5 inches per year in the east. Aquifers of the flood-plain and terrace deposits and of the Cretaceous Dakota Sandstone are the major sources of ground-water accretion to the streams. In the upper reaches of the Saline River, the water is only slightly mineralized; during the period of record the specific conductance near Wakeeney never exceeded 750 micromhos per centimeter. In the lower reaches, however, the water is slightly mineralized during periods of high flow and is highly mineralized during periods of low flow; the specific conductance near Russell exceeded 1,500 micromhos per centimeter more than 80 percent of the time. Near Russell, near Wilson, and at Tescott the water is of the calcium bicarbonate type when the specific conductance is less than about 1,000 micromhos per centimeter, but it is of the sodium chloride type when the specific conductance is more than about 1,500 micromhos per centimeter. The water is off the calcium bicarbonate, sodium bicarbonate, or sodium chloride type when the conductance is between 1,000 and 1,500 micromhos per centimeter. Most of the increase in mineralization of the water is caused by inflow of highly mineralized ground water. The ground-water inflow was estimated to be 22 percent of the total streamflow at Tescott in 1948 and 60 percent in 1952. Mineralization increases and water quality deteriorates progressively downstream along nearly the entire Saline River, especially in the part of the area directly underlain by the Dakota Sandstone between the vicinities of Fairport and Wilson: sodium and chloride are the principal constituents of water contributed by the Dakota. The total percentage of the salt in the Saline River that comes from oil-field brines is considered to be small. The water in the upper Saline River is of good quality for domestic use except that it is hard; the water in the lower Saline River is of poor quality for domestic use because most of the time it is highly mineralized, is hard, and contains high concentrations of chloride and sulfate. In the upper reaches of the river, the water is of good quality for irrigation. In the lower reaches, if the water were impounded in a reservoir, it would be of good quality for irrigation during years of high flow and of very poor quality during years of low flow. The water in the lower reaches is of poor quality for industrial use because it is highly mineralized most of the tinge. Relations of suspended-sediment discharge to water discharge were used with the long-term streamflow duration curves to compute the long-term aver age suspended-sediment discharges and concentrations at five indications. Sediment discharge is closely related to runoff. S","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1651","usgsCitation":"Jordan, P.R., Jones, B., and Petri, L., 1964, Chemical quality of surface waters and sedimentation in the Saline River basin, Kansas: U.S. Geological Survey Water Supply Paper 1651, v, 90 p. :ill., maps ;23 cm., https://doi.org/10.3133/wsp1651.","productDescription":"v, 90 p. :ill., maps ;23 cm.","costCenters":[],"links":[{"id":110000,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24844.htm","linkFileType":{"id":5,"text":"html"},"description":"24844"},{"id":138366,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1651/report-thumb.jpg"},{"id":27438,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1651/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27439,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1651/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27440,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1651/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27441,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1651/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27442,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1651/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27443,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1651/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4827e4b07f02db4e55e1","contributors":{"authors":[{"text":"Jordan, Paul Robert","contributorId":57819,"corporation":false,"usgs":true,"family":"Jordan","given":"Paul","email":"","middleInitial":"Robert","affiliations":[],"preferred":false,"id":144506,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, B.F.","contributorId":52156,"corporation":false,"usgs":true,"family":"Jones","given":"B.F.","email":"","affiliations":[],"preferred":false,"id":144505,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Petri, Lester R.","contributorId":19534,"corporation":false,"usgs":true,"family":"Petri","given":"Lester R.","affiliations":[],"preferred":false,"id":144504,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1122,"text":"wsp1773 - 1964 - Geology and ground-water resources of the Anchorage area, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:05:17","indexId":"wsp1773","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1773","title":"Geology and ground-water resources of the Anchorage area, Alaska","docAbstract":"The Anchorage area, at the head of Cook Inlet in south-central Alaska, \r\noccupies 150 square miles of a glaciated lowland and lies between two estuaries and the Chugach Mountains. Two military bases are in the area; \r\nAnchorage is the largest city in Alaska and the chief transportation center \r\nfor this part of the State. \r\nThe bedrock in the Anchorage area is chiefly Tertiary shale in the lowland \r\nand metamorphic rocks of Mesozoic age beneath the adjacent mountain \r\nslopes. Glacial drift which underlies nearly the entire area has an average \r\nthickness of several hundred feet and appears to include at least five sheets \r\nof deposits, two of which are exposed. The drift consists of till, outwash stream and lake deposits (sand and gravel), and estuarine (and lake) deposits \r\n(clay and silt). The stratigraphy and lateral distribution of the deposits are \r\ncomplex, but data at hand s, how that the thickest deposits, including all the \r\nestuarine and lake sediment and most of the stream-deposited sediment, \r\nare beneath the lowland away from the mountain wall, and that the deposits \r\nnear the mountains are till and subordinate outwash sediments. \r\nDeposits of sand and gravel laid down by outwash streams in channels and \r\non outwash plains are the most important aquifers, and the only \r\nones which yield large quantities of ground water from single beds. Thin \r\nlayers of sandy or gravelly material in till are also important aquifers although they yield relatively small quantities of water. Bedded sand and \r\nsilt associated with the estuarine and lake(?) clay commonly becomes unstable during drilling and pumping, and has been successfully developed in \r\nonly a few wells. Unconfined aquifers are extensive, but permeable saturated \r\nmaterial is thin in many places and water supplies available from them are \r\nsmall or undependable in those places. The most important aquifers are confined or artesian. Clay and till form the confining beds: the till is somewhat 'leaky' in many places. Near Anchorage the buried water-bearing \r\nbeds appear to be interconnected and to form a single artesian system. The \r\nwater table and piezometric surface slope from the mountain wall of the \r\nlowland toward the estuaries, and the flow of the ground water is in that \r\ndirection. The aquifers are recharged by the infiltration of precipitation \r\nat the land surface and of surface water through stream beds: near the mountains the artesian aquifers are probably recharged in part by percolation from \r\nthe water-table aquifer, and far from the mountains the water-table aquifer \r\nis probably recharged in part by upward flow from the underlying artesian \r\naquifers. In several valleys and in a few other places, in the lowland, artesian wells flow at the land surface. \r\nThe outwash sand and gravel are moderately to very permeable; most \r\nof the other water-bearing material are much less permeable. The co- efficient of transmissibility for some single beds of sandy gravel is as high \r\nas 60,000 to I00,000 gpd per ft (gallons per day per foot); for the entire \r\nsection of glacial drift at and near Anchorage it is believed to be of the \r\norder of 200,000 gpd per ft. Calculations based on this value for the total \r\nsection and on the slope of the piezometric surface indicate that in the \r\nimmediate vicinity of Anchorage about 5 million gpd flows through each \r\nmile-wide section of the drift (measured in a northeast-southwest direction, perpendicular to the direction of flow), under normal (nonpumping) conditions. Under conditions of continuous heavy pumping the slope of the piezometric surface is steepened, flow is increased, and additional recharge is induced. \r\n\r\nThe highest yield reported from a well in this area is 2.600 gpm (gallons per minute) with 35 feet of drawdown: the highest reported specific capacity is 180 gpm per ft of drawdown, for a well pumped at. 270 gpm. \r\n\r\nOnly a few wells in the area have been developed for high yields. Well screens have been used ","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1773","usgsCitation":"Cederstrom, D.J., Trainer, F.W., and Waller, R.M., 1964, Geology and ground-water resources of the Anchorage area, Alaska: U.S. Geological Survey Water Supply Paper 1773, vi, 108 p. :illus., maps (1 col.) diagrs., tables. ;24 cm., https://doi.org/10.3133/wsp1773.","productDescription":"vi, 108 p. :illus., maps (1 col.) diagrs., tables. ;24 cm.","costCenters":[],"links":[{"id":138014,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1773/report-thumb.jpg"},{"id":25887,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1773/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25888,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1773/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25889,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1773/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25890,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1773/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25891,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1773/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db6855f4","contributors":{"authors":[{"text":"Cederstrom, Dagfin John","contributorId":90287,"corporation":false,"usgs":true,"family":"Cederstrom","given":"Dagfin","email":"","middleInitial":"John","affiliations":[],"preferred":false,"id":143212,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trainer, Frank W.","contributorId":103655,"corporation":false,"usgs":true,"family":"Trainer","given":"Frank","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":143213,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Waller, Roger Milton","contributorId":22320,"corporation":false,"usgs":true,"family":"Waller","given":"Roger","email":"","middleInitial":"Milton","affiliations":[],"preferred":false,"id":143211,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1106,"text":"wsp1669W - 1964 - The yield of sedimentary aquifers of the coastal plain, southeast river basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:16","indexId":"wsp1669W","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"W","title":"The yield of sedimentary aquifers of the coastal plain, southeast river basins","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/wsp1669W","usgsCitation":"Callahan, J.T., 1964, The yield of sedimentary aquifers of the coastal plain, southeast river basins: U.S. Geological Survey Water Supply Paper 1669, iv, 56 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1669W.","productDescription":"iv, 56 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":137882,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1669w/report-thumb.jpg"},{"id":25841,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669w/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25842,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1669w/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a57e4b07f02db62e816","contributors":{"authors":[{"text":"Callahan, Joseph Thomas","contributorId":45689,"corporation":false,"usgs":true,"family":"Callahan","given":"Joseph","email":"","middleInitial":"Thomas","affiliations":[],"preferred":false,"id":143186,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":63663,"text":"gp424 - 1964 - Aeromagnetic and geologic map of part of the Silver City mining region, Grant County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-10T00:11:11","indexId":"gp424","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"424","title":"Aeromagnetic and geologic map of part of the Silver City mining region, Grant County, New Mexico","language":"ENGLISH","doi":"10.3133/gp424","usgsCitation":"Jones, W.R., Case, J.E., and Pratt, W., 1964, Aeromagnetic and geologic map of part of the Silver City mining region, Grant County, New Mexico: U.S. Geological Survey Geophysical Investigations Map 424, 1 map., https://doi.org/10.3133/gp424.","productDescription":"1 map.","costCenters":[],"links":[{"id":249881,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0424/report.pdf","size":"581","linkFileType":{"id":1,"text":"pdf"}},{"id":249882,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0424/plate-1.pdf","size":"2911","linkFileType":{"id":1,"text":"pdf"}},{"id":253429,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0424/report-thumb.jpg"}],"scale":"63360","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.25,32.666666666666664 ], [ -108.25,32.8675 ], [ -108,32.8675 ], [ -108,32.666666666666664 ], [ -108.25,32.666666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db6989a7","contributors":{"authors":[{"text":"Jones, W. R.","contributorId":62975,"corporation":false,"usgs":true,"family":"Jones","given":"W.","middleInitial":"R.","affiliations":[],"preferred":false,"id":269333,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Case, J. E.","contributorId":56625,"corporation":false,"usgs":true,"family":"Case","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":269332,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pratt, W. P.","contributorId":14838,"corporation":false,"usgs":true,"family":"Pratt","given":"W. P.","affiliations":[],"preferred":false,"id":269331,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":35276,"text":"b1142L - 1964 - Geology of the Tintic Junction quadrangle, Tooele, Juab, and Utah Counties, Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:09:43","indexId":"b1142L","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1142","chapter":"L","title":"Geology of the Tintic Junction quadrangle, Tooele, Juab, and Utah Counties, Utah","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/b1142L","usgsCitation":"Morris, H.T., 1964, Geology of the Tintic Junction quadrangle, Tooele, Juab, and Utah Counties, Utah: U.S. Geological Survey Bulletin 1142, p. L1-L23, :fold. col. map (in pocket) ;24 cm., https://doi.org/10.3133/b1142L.","productDescription":"p. L1-L23, :fold. col. map (in pocket) ;24 cm.","costCenters":[],"links":[{"id":109414,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20885.htm","linkFileType":{"id":5,"text":"html"},"description":"20885"},{"id":166972,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1142l/report-thumb.jpg"},{"id":63135,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1142l/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63136,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1142l/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67cab4","contributors":{"authors":[{"text":"Morris, H. T.","contributorId":15585,"corporation":false,"usgs":true,"family":"Morris","given":"H.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":214362,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2874,"text":"wsp1779Q - 1964 - Ground water in the Midvale and Council areas, Upper Weiser River basin, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:05:35","indexId":"wsp1779Q","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1779","chapter":"Q","title":"Ground water in the Midvale and Council areas, Upper Weiser River basin, Idaho","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1779Q","usgsCitation":"Walker, E.H., and Sisco, H., 1964, Ground water in the Midvale and Council areas, Upper Weiser River basin, Idaho: U.S. Geological Survey Water Supply Paper 1779, iv, 26 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1779Q.","productDescription":"iv, 26 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":138977,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1779q/report-thumb.jpg"},{"id":29502,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1779q/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d960","contributors":{"authors":[{"text":"Walker, Eugene H.","contributorId":24761,"corporation":false,"usgs":true,"family":"Walker","given":"Eugene","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":145941,"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":145942,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":97,"text":"wsp1781 - 1964 - Ground-water levels in the United States, 1957-61, North-central states","interactions":[],"lastModifiedDate":"2012-02-02T00:05:10","indexId":"wsp1781","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1781","title":"Ground-water levels in the United States, 1957-61, North-central states","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1781","usgsCitation":"Hackett, O.M., 1964, Ground-water levels in the United States, 1957-61, North-central states: U.S. Geological Survey Water Supply Paper 1781, v, 148 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1781.","productDescription":"v, 148 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":136215,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1781/report-thumb.jpg"},{"id":24703,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1781/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6675b6","contributors":{"authors":[{"text":"Hackett, O. M.","contributorId":38527,"corporation":false,"usgs":true,"family":"Hackett","given":"O.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":141925,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":62504,"text":"gq307 - 1964 - Geology of the Kelly quadrangle, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:11:00","indexId":"gq307","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"307","title":"Geology of the Kelly quadrangle, Kentucky","language":"ENGLISH","doi":"10.3133/gq307","usgsCitation":"Miller, T.P., 1964, Geology of the Kelly quadrangle, Kentucky: U.S. Geological Survey Geologic Quadrangle 307, 1 map :col. ;81 x 89 cm., https://doi.org/10.3133/gq307.","productDescription":"1 map :col. ;81 x 89 cm.","costCenters":[],"links":[{"id":102318,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_767.htm","linkFileType":{"id":5,"text":"html"},"description":"767"},{"id":248667,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0307/report.pdf","size":"32","linkFileType":{"id":1,"text":"pdf"}},{"id":253894,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0307/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87.5,36.8675 ], [ -87.5,37 ], [ -87.36749999999999,37 ], [ -87.36749999999999,36.8675 ], [ -87.5,36.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67fbfc","contributors":{"authors":[{"text":"Miller, Thomas P. tmiller@usgs.gov","contributorId":4183,"corporation":false,"usgs":true,"family":"Miller","given":"Thomas","email":"tmiller@usgs.gov","middleInitial":"P.","affiliations":[{"id":121,"text":"Alaska Volcano Observatory","active":false,"usgs":true}],"preferred":false,"id":267468,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":14077,"text":"ofr6476 - 1964 - Polar charts for calculating aeromagnetic anomalies of three-dimensional bodies","interactions":[],"lastModifiedDate":"2017-05-19T18:32:38","indexId":"ofr6476","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"64-76","title":"Polar charts for calculating aeromagnetic anomalies of three-dimensional bodies","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6476","usgsCitation":"Henderson, R.G., and Wilson, A., 1964, Polar charts for calculating aeromagnetic anomalies of three-dimensional bodies: U.S. Geological Survey Open-File Report 64-76, 13 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr6476.","productDescription":"13 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":42714,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0076/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42715,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0076/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42716,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0076/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42717,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0076/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42718,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0076/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42719,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0076/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42720,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0076/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42721,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1964/0076/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":146688,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1964/0076/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db684a33","contributors":{"authors":[{"text":"Henderson, Roland George","contributorId":43787,"corporation":false,"usgs":true,"family":"Henderson","given":"Roland","email":"","middleInitial":"George","affiliations":[],"preferred":false,"id":168892,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilson, Alphonso","contributorId":57467,"corporation":false,"usgs":true,"family":"Wilson","given":"Alphonso","email":"","affiliations":[],"preferred":false,"id":168893,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":43404,"text":"ofr64111 - 1964 - Geology of the Jackass Flats quadrangle, Nevada Test Site, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:04:56","indexId":"ofr64111","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"64-111","title":"Geology of the Jackass Flats quadrangle, Nevada Test Site, Nevada","language":"ENGLISH","doi":"10.3133/ofr64111","usgsCitation":"McKay, E.J., and Williams, W.P., 1964, Geology of the Jackass Flats quadrangle, Nevada Test Site, Nevada: U.S. Geological Survey Open-File Report 64-111, 1 map., https://doi.org/10.3133/ofr64111.","productDescription":"1 map.","costCenters":[],"links":[{"id":134881,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67fe82","contributors":{"authors":[{"text":"McKay, E. J.","contributorId":57040,"corporation":false,"usgs":true,"family":"McKay","given":"E.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":228164,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, William P.","contributorId":84723,"corporation":false,"usgs":true,"family":"Williams","given":"William","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":228165,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":63534,"text":"gp448 - 1964 - Aeromagnetic map of the Beckett quadrangle, Berkshire, Hampshire, and Hampden Counties, Massachusetts","interactions":[],"lastModifiedDate":"2022-08-17T21:56:10.085185","indexId":"gp448","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"448","title":"Aeromagnetic map of the Beckett quadrangle, Berkshire, Hampshire, and Hampden Counties, Massachusetts","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp448","usgsCitation":"Popenoe, P., Boynton, G.R., and Zandle, G.L., 1964, Aeromagnetic map of the Beckett quadrangle, Berkshire, Hampshire, and Hampden Counties, Massachusetts: U.S. Geological Survey Geophysical Investigations Map 448, 1 Plate: 21.75 × 27.74 inches, https://doi.org/10.3133/gp448.","productDescription":"1 Plate: 21.75 × 27.74 inches","costCenters":[],"links":[{"id":405290,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3392.htm","linkFileType":{"id":5,"text":"html"}},{"id":253172,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0448/report-thumb.jpg"},{"id":249681,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0448/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":249680,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0448/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Massachusetts","county":"Berkshire County, Hampshire County, Hampden County","otherGeospatial":"Beckett quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73.125,\n              42.25\n            ],\n            [\n              -73,\n              42.25\n            ],\n            [\n              -73,\n              42.375\n            ],\n            [\n              -73.125,\n              42.375\n            ],\n            [\n              -73.125,\n              42.25\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697245","contributors":{"authors":[{"text":"Popenoe, Peter","contributorId":62206,"corporation":false,"usgs":true,"family":"Popenoe","given":"Peter","email":"","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":269072,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boynton, G. R.","contributorId":82276,"corporation":false,"usgs":true,"family":"Boynton","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":269073,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zandle, G. L.","contributorId":39863,"corporation":false,"usgs":true,"family":"Zandle","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":269071,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2173,"text":"wsp1944 - 1964 - Quality of surface waters of the United States, 1962, Parts 7 and 8, Lower Mississippi River basin and western Gulf of Mexico basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:23","indexId":"wsp1944","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1944","title":"Quality of surface waters of the United States, 1962, Parts 7 and 8, Lower Mississippi River basin and western Gulf of Mexico basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1944","usgsCitation":"Love, S.K., 1964, Quality of surface waters of the United States, 1962, Parts 7 and 8, Lower Mississippi River basin and western Gulf of Mexico basins: U.S. Geological Survey Water Supply Paper 1944, xii, 645 p. :ill. ;25 cm., https://doi.org/10.3133/wsp1944.","productDescription":"xii, 645 p. :ill. ;25 cm.","costCenters":[],"links":[{"id":138311,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1944/report-thumb.jpg"},{"id":27784,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1944/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651abe","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":144768,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2733,"text":"wsp1673 - 1964 - Magnitude and frequency of floods in the United States; part 2-A. South Atlantic slope basins, James River to Savannah River","interactions":[],"lastModifiedDate":"2022-01-07T20:41:08.645519","indexId":"wsp1673","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1673","title":"Magnitude and frequency of floods in the United States; part 2-A. South Atlantic slope basins, James River to Savannah River","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1673","usgsCitation":"Speer, P.R., and Gamble, C.R., 1964, Magnitude and frequency of floods in the United States; part 2-A. South Atlantic slope basins, James River to Savannah River: U.S. Geological Survey Water Supply Paper 1673, Report: x, 329 p.; 3 Plates: 26.00 × 25.50 inches or smaller, https://doi.org/10.3133/wsp1673.","productDescription":"Report: x, 329 p.; 3 Plates: 26.00 × 25.50 inches or smaller","costCenters":[],"links":[{"id":29152,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1673/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29151,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1673/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29150,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1673/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29149,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1673/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138895,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1673/report-thumb.jpg"},{"id":110007,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24882.htm","linkFileType":{"id":5,"text":"html"},"description":"24882"}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.5,\n              32.05\n            ],\n            [\n              -75.667,\n              32.05\n            ],\n            [\n              -75.667,\n              38.333\n            ],\n            [\n              -83.5,\n              38.333\n            ],\n            [\n              -83.5,\n              32.05\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6495ce","contributors":{"authors":[{"text":"Speer, Paul R.","contributorId":24768,"corporation":false,"usgs":true,"family":"Speer","given":"Paul","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":145684,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gamble, Charles R.","contributorId":6822,"corporation":false,"usgs":true,"family":"Gamble","given":"Charles","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":145683,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1669,"text":"wsp1779F - 1964 - Hydrologic studies of small watersheds, Honey Creek basin, Collin and Grayson Counties, Texas, 1953-1959","interactions":[],"lastModifiedDate":"2016-08-23T14:27:54","indexId":"wsp1779F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1779","chapter":"F","title":"Hydrologic studies of small watersheds, Honey Creek basin, Collin and Grayson Counties, Texas, 1953-1959","docAbstract":"<p>This report presents the results of an investigation into the effects of floodwaterretarding structures in the 39 square miles of the Honey Creek basin above the stream-gaging station near McKinney, during the period October 1952 to September 1959. The number of such structures in the study area was increased from 2 to 12 during the investigation.</p>\n<p>Data were collected which permit computation of basin and watershed precipitation, inflow to and outflow from each floodwater-retarding structure, evaporation and seepage from each pool, and a continuous record of discharge from the entire study area. Transpiration was not evaluated, but in the water-budget summary it is included in the item \"pool consumption\", together with evaporation and seepage.</p>\n<p>During the 7-year study period, the annual inflow to the gaged pools ranged from 1.34 to 26.50 inches and averaged 7.39 inches, of which 0.73 inch was direct rainfall on the pool surface. The annual pool consumption ranged only from 1.33 to 1.85 inches, and averaged 1.62 inches. These results indicate that in a year of substantial runoff the floodwater-retarding structures would have only a minor effect on downstream water yield, but in a year of low runoff the structures would have a marked effect on downstream water yield.</p>\n<p>The effect on the flood regimen at a downstream point because of floodwaterretarding structures in the headwaters will vary with the amount and intensity of the precipitation and with antecedent conditions. The beneficial effects of the structures on Honey Creek during the floods of April and May 1957 is illustrative. During the period April 19 to May 31, 1957, the total volume of inflow to the floodwater-retarding structures was equivalent to 4.3 times the combined capacities of the pools from an average basin rainfall of 30.31 inches. The retarding effects of the structures limited the flooding on Honey Creek at the gage to minor flooding on only five occasions during that period.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1779F","collaboration":"Prepared in cooperation with the U.S. Soil Conservation Service and the Texas Water Commission","usgsCitation":"Gilbert, C.R., Commons, G., Koberg, G.E., and Kennon, F., 1964, Hydrologic studies of small watersheds, Honey Creek basin, Collin and Grayson Counties, Texas, 1953-1959: U.S. Geological Survey Water Supply Paper 1779, Report: v, 98 p.; 3 Plates: 24.00 x 7.00 inches or smaller, https://doi.org/10.3133/wsp1779F.","productDescription":"Report: v, 98 p.; 3 Plates: 24.00 x 7.00 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":138232,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1779f/report-thumb.jpg"},{"id":26741,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779f/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26742,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779f/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26743,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779f/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26744,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1779f/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","county":"Collin County, Grayson County","otherGeospatial":"Honey Creek 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Clarence R.","contributorId":30965,"corporation":false,"usgs":true,"family":"Gilbert","given":"Clarence","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":143947,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Commons, G.G.","contributorId":52951,"corporation":false,"usgs":true,"family":"Commons","given":"G.G.","email":"","affiliations":[],"preferred":false,"id":143948,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Koberg, G. E.","contributorId":30212,"corporation":false,"usgs":true,"family":"Koberg","given":"G.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":143946,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kennon, F.W.","contributorId":88332,"corporation":false,"usgs":true,"family":"Kennon","given":"F.W.","affiliations":[],"preferred":false,"id":143949,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":2203,"text":"wsp1764 - 1964 - Ground-water geology of the Dickson, Lawrenceburg, and Waverly areas in the western Highland Rim, Tennessee","interactions":[],"lastModifiedDate":"2024-01-31T20:36:24.280058","indexId":"wsp1764","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1764","title":"Ground-water geology of the Dickson, Lawrenceburg, and Waverly areas in the western Highland Rim, Tennessee","docAbstract":"Ground-water supplies in the Dickson, Lawrenceburg, and Waverly areas are obtained from wells and springs in limestone and chert formations of Missisippian age. In the Dickson area most of the wells and springs are in Warsaw Limestone. In the Lawrenceburg and Waverly areas, ground-water supplies are obtained from Fort Payne Chert and from residuum. In all three areas a few wells obtain small amounts of water from gravel stringers in the residuum. \r\n\r\nYields of well range from a few to 300 gpm (gallons per minute). Wells having the largest yields obtain water from residual material (colluvium) in the valley of Trace Creek in the Waverly area. Fewer than 10 percent of all wells inventoried yield more than 25 gpm. Springs are common in all the areas studied and yield as much as 1,000 gpm. \r\n\r\nThe quality of water from wells and springs iv the areas studied generally is good. The water is of the calcium bicarbonate type, and most of it is moderately hard to hard. The constituents in water from springs and from wells are about the same, although water from springs tends to be softer and slightly lower in dissolved-solids content. \r\n\r\nSprings constitute the largest potential source of water in the three areas. Twenty-one of the large springs discharge approximately 12 million gallons per day, or about 8,000 gpm. Another potential source of water is residuum underlying the valley of Trace Creek in the Waverly area. Wells yielding as much as 500 gpm probably could be developed in this aquifer.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1764","usgsCitation":"Marcher, M.V., Bingham, R.H., and Lounsbury, R., 1964, Ground-water geology of the Dickson, Lawrenceburg, and Waverly areas in the western Highland Rim, Tennessee: U.S. Geological Survey Water Supply Paper 1764, Report: iv, 50 p.; 7 Plates: 19.68 × 38.83 inches or smaller, https://doi.org/10.3133/wsp1764.","productDescription":"Report: iv, 50 p.; 7 Plates: 19.68 × 38.83 inches or smaller","costCenters":[],"links":[{"id":27871,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1764/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":397419,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24942.htm","text":"Lawrenceburg 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Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24941.htm","text":"Dickson area"},{"id":397420,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24943.htm","text":"Waverly area"}],"scale":"31680","country":"United States","state":"Tennessee","city":"Dickson, Lawrenceburg, Waverly","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -87.5,\n              36\n            ],\n            [\n              -87.25,\n              36\n            ],\n            [\n              -87.25,\n              36.125\n            ],\n            [\n              -87.5,\n              36.125\n            ],\n            [\n              -87.5,\n              36\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      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   36.125\n            ],\n            [\n              -87.875,\n              36\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d966","contributors":{"authors":[{"text":"Marcher, Melvin V.","contributorId":11590,"corporation":false,"usgs":true,"family":"Marcher","given":"Melvin","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":144819,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bingham, Roy H.","contributorId":56632,"corporation":false,"usgs":true,"family":"Bingham","given":"Roy","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":144820,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lounsbury, Richard Edwin","contributorId":102054,"corporation":false,"usgs":true,"family":"Lounsbury","given":"Richard Edwin","affiliations":[],"preferred":false,"id":144821,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2797,"text":"wsp1608B - 1964 - Ground water in folded Cretaceous sandstone of the Bhachau area, Kutch, India, with reference to the Kandla Port water supply","interactions":[],"lastModifiedDate":"2012-02-02T00:05:28","indexId":"wsp1608B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"B","title":"Ground water in folded Cretaceous sandstone of the Bhachau area, Kutch, India, with reference to the Kandla Port water supply","docAbstract":"This report is based on an investigation of the availability of ground-water supplies in the Bhachau area for the nearby Kandla Port and township development undertaken by the Government of India. This seaport lies on an estuary of the Gulf of Kutch in western India and in the eastern part of the State of Kutch. The fieldwork on the investigation was carried on from November 1952 through April 1953 with continuing hydrologic observations through 1954-55. The fieldwork included: geologic mapping and delimitation of the principal aquifers of the region; preparation of water-table maps; a detailed inventory of existing wells and springs; observations of significant water table fluctuations; preparation of isobicarb, isochlor and isosulf maps to show the areal distribution of ground-water salinity. \r\n\r\nThe Bhachau area includes about 116 square miles in eastern Kutch and lies in a belt of semiarid low-latitude steppes. The mean annual rainfall is about 15 inches, most of which falls from late June to late September during the southwest monsoon. The area includes a central sandy upland ranging from about 100 to 250 feet above sea level ; a northern lowland of between about 50 to 125 feet altitude that slopes north to the Great Rann of Kutch; a belt of low buttes and discontinuous ridges ranging from about 200 to 275 feet above sea level; and southern lowland which slopes in a southerly to southeasterly direction from an altitude of about 125 feet to 25 feet or less near the Gulf of Kutch. The principal streams are Kageshwar Vokra and Kara Vokra which drain north to the Great Rann and Kotwala Vokra and Dalwala Vokra which drain south toward the Gulf of Kutch. \r\n\r\nThe rocks of the Bhachau area include nonmarine and marine sediments of Mesozoic, Tertiary, and Quaternary age and volcanic rocks of late Mesozoic to early Tertiary age. The oldest rocks in the area are medium- to coarse-grained white to buff current-bedded friable sandstone with occasional partings of white silty shale of the Upper Bhuj series that has been assigned to the Early Cretaceous. The soft friable sandstone of the Upper Bhuj series constitutes the most productive ground-water reservoir in the Bhachau area. At present (1955) there are nine irrigated tracts for which water is obtained from dug wells less than 90 feet deep in the Upper Bhuj. These wells are worked by bullocks and 'motes' (leather bags) at withdrawal rates ranging from about 6,000 to 24,000imperial gallons per day; however, many existing individual wells if equipped with mechanical pumps are capable of yielding 100,000 gallons per day. The Deccan trap of Late Cretaceous to Eocene age occurs in a sequence of basaltic lava flows in the Bhachau area, but trap dikes, sills and plugs that are common in other parts of Kutch have not been observed in the area. Laterite of probable Eocene age is extensive at the top of the Deccan trap, and in places where the lava flows are thin the parent rock has been almost completely lateritized. The Deccan lava flows or the laterite, where the trap is absent, rest disconformably on the Upper Bhuj. No wells have been observed in the Deccan trap of the Bhachau area, but it is possible that locally small supplies of good water may be obtained from these rocks. \r\n\r\nThe Tertiary sediments, which are assigned to the Manchhar series of Pliocene age, generally rest on the laterite or the Deccan trap ; but where both are absent, the Manchhar rests directly on the Upper Bhuj. The Manchhar series includes massive reddish-brown gypseous clay shales, laminated gray siltstones, some limestone, mottled sandstone, and laterite trap gravel. Only meager supplies of brackish water are obtained from wells in these sediments. \r\n\r\nAlong the channels of Kotwala, Dalwala, Kageshwar, and Kara Vokras are narrow bands of unconsolidated coarse sand with fine gravel of Quaternary age. 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