No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1779Y","usgsCitation":"Pistrang, M.A., and Kunkel, F., 1964, A brief geologic and hydrologic reconnaissance of the Furnace Creek Wash area, Death Valley National Monument, California: U.S. Geological Survey Water Supply Paper 1779, Report: iv, 35 p.; 1 Plate: 24.00 x 24.73 inches, https://doi.org/10.3133/wsp1779Y.","productDescription":"Report: iv, 35 p.; 1 Plate: 24.00 x 24.73 inches","costCenters":[],"links":[{"id":411377,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24971.htm","linkFileType":{"id":5,"text":"html"}},{"id":28660,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1779y/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28659,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779y/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138708,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1779y/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Death Valley National Monument, Furnace Creek Wash area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -116.90103306234425,\n 36.52417528804904\n ],\n [\n -116.90103306234425,\n 36.4259295289059\n ],\n [\n -116.78424464238198,\n 36.4259295289059\n ],\n [\n -116.78424464238198,\n 36.52417528804904\n ],\n [\n -116.90103306234425,\n 36.52417528804904\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4979e4b0b290850ef367","contributors":{"authors":[{"text":"Pistrang, Marvin Arthur","contributorId":14803,"corporation":false,"usgs":true,"family":"Pistrang","given":"Marvin","email":"","middleInitial":"Arthur","affiliations":[],"preferred":false,"id":145311,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kunkel, Fred","contributorId":47766,"corporation":false,"usgs":true,"family":"Kunkel","given":"Fred","email":"","affiliations":[],"preferred":false,"id":145312,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":976,"text":"wsp1669CC - 1964 - Natural sources of salinity in the Brazos River, Texas with particular reference to the Croton and salt Croton Creek basins","interactions":[{"subject":{"id":976,"text":"wsp1669CC - 1964 - Natural sources of salinity in the Brazos River, Texas with particular reference to the Croton and salt Croton Creek basins","indexId":"wsp1669CC","publicationYear":"1964","noYear":false,"chapter":"CC","title":"Natural sources of salinity in the Brazos River, Texas with particular reference to the Croton and salt Croton Creek basins"},"predicate":"IS_PART_OF","object":{"id":76866,"text":"wsp1669 - 1964 - Contributions to the hydrology of the United States, 1962","indexId":"wsp1669","publicationYear":"1964","noYear":false,"title":"Contributions to the hydrology of the United States, 1962"},"id":1}],"isPartOf":{"id":76866,"text":"wsp1669 - 1964 - Contributions to the hydrology of the United States, 1962","indexId":"wsp1669","publicationYear":"1964","noYear":false,"title":"Contributions to the hydrology of the United States, 1962"},"lastModifiedDate":"2023-01-06T19:58:08.762707","indexId":"wsp1669CC","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":"CC","title":"Natural sources of salinity in the Brazos River, Texas with particular reference to the Croton and salt Croton Creek basins","docAbstract":"The average daily load of the Brazos River at Possum Kingdom Reservoir is about 2,800 tons of dissolved solids, of which 1,000 tons is chloride. More than 85 percent of the chloride load is contributed by the Salt Fork Brazos River, and more than 50 percent of the chloride load of the Brazos River originates from salt springs and seeps in Croton and Salt Crotdn Creeks, which are tributaries of Salt Fork Brazos River. The rest of the chloride is contributed from many small sources.
\nThe average daily chloride load of Croton Creek is 70 tons, much of which is carried during periods of flood runoff. The average daily chloride load of Salt Croton Creek is about 480 tons. Of this total, 330 tons is contributed by the base flow, which ranges from 0.5 to 2 cubic feet per second.
\nThe principal areas of salt springs and seeps in the Croton Creek basin are Hot Springs and Short Croton Salt Flats in northeastern Kent County. In the Salt Croton Creek basin, saline water is discharged in Dove Creek Salt Flat, Dove Creek near Dove Creek Salt Flat, and three small salt flats on Haystack Creek, all in southwestern King County and northwestern Stonewall County.
\nSalt springs and seeps discharge from the rocks of the Whitehorse Group undifferentiated in the Croton Creek basin, and from the upper part of the Dog Creek Shale of the Pease River Group in the Salt Croton Creek basin. Both groups are of Permian age. The water that is discharged by springs and seeps in the Croton Creek basin is derived from the infiltration of precipitation and seepage from streams in the Duck Creek basin. The source of the water that discharges in the Salt Croton basin is not known.
\nThe salt load contributed to the Brazos River by the springs and seeps can be reduced, although the volume of salt water for disposal probably cannot be reduced or eliminated. Collecting and disposing of the base flow of Salt Croton Creek would reduce the salt load of the Brazos River by 30 percent; disposal of the total flow of Salt Croton Creek would reduce the salt load by 45 percent.
\nThe salt water may be disposed of by impounding it in reservoirs for evaporation or by injecting it underground through oil wells, oil tests, or wells drilled for saltwater disposal. Sediments in which the salt water possibly could be injected underlie the. Dove Creek Salt Flats at depths of less than 7,000 feet.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1962 (Water Supply Paper 1669)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1669CC","usgsCitation":"Baker, R.C., Hughes, L.S., and Yost, I.D., 1964, Natural sources of salinity in the Brazos River, Texas with particular reference to the Croton and salt Croton Creek basins: U.S. Geological Survey Water Supply Paper 1669, Report: vi, 81 p. ; 4 Plates: 36.00 x 35.86 inches or smaller, https://doi.org/10.3133/wsp1669CC.","productDescription":"Report: vi, 81 p. ; 4 Plates: 36.00 x 35.86 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":411514,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24863.htm","linkFileType":{"id":5,"text":"html"}},{"id":25542,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1669cc/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25538,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669cc/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25539,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669cc/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137060,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1669cc/report-thumb.jpg"},{"id":25540,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669cc/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25541,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669cc/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","otherGeospatial":"Brazos River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -100.25,\n 33.25\n ],\n [\n -100.25,\n 32.5\n ],\n [\n -98.75,\n 32.5\n ],\n [\n -98.75,\n 33.25\n ],\n [\n -100.25,\n 33.25\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db6980df","contributors":{"authors":[{"text":"Baker, R. C.","contributorId":79084,"corporation":false,"usgs":true,"family":"Baker","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":142954,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hughes, Leon S.","contributorId":65056,"corporation":false,"usgs":true,"family":"Hughes","given":"Leon","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":142953,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Yost, I. D.","contributorId":12833,"corporation":false,"usgs":true,"family":"Yost","given":"I.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":142952,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":2656,"text":"wsp1669R - 1964 - Geology and ground-water conditions of the Redwood Falls area, Redwood County, Minnesota","interactions":[],"lastModifiedDate":"2018-04-02T10:16:10","indexId":"wsp1669R","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":"R","title":"Geology and ground-water conditions of the Redwood Falls area, Redwood County, Minnesota","docAbstract":"The Redwood Falls area includes about 80 square miles in southwestern Minnesota and is about 100 miles west of Minneapolis and St. Paul. Its surface is a gently undulating glacial-drift plain, interrupted in part by the large Minnesota River valley and the tributary Redwood River valley. The drift plain was laid down by the Des Moines lobe of the Wisconsin Glaciation and consists chiefly of ground moraine and several subdued recessional moraines. The glacial drift rests either on Precambrian gneiss or on thin patches of Cretaceous sedimentary strata that overlie the Precambrian bedrock.
\nThe glacial drift consists principally of till and some outwash and ranges in thickness from 0 to about 260 feet. It is the chief source of ground water, yielding small supplies almost anywhere in the area and large supplies in at least two places. Where the drift is absent, thin, or impermeable, small yields commonly are obtained from the Precambrian bedrock.
\nThe most notable aquifers in the area are three buried outwash deposits that are associated with a conspicuous southeastward-trending buried bedrock valley. The tops of the aquifers occur about 70,120, and 200 feet below the land surface, and their maximum known thicknesses are about 25, 55, and 45 feet, respectively. The aquifers are confined largely by relatively impermeable till; however, owing to the movement of water through the till, the drift may be regarded as a hydraulic unit.
\nThe main source of recharge to the ground-water reservoir is local precipitation, and most of the natural discharge is by evapotranspiration. The water table ranges in depth from 0 to about 30 feet below the land surface.
\nAquifer tests were made on the three outwash aquifers to determine their hydraulic characteristics. The coefficient of transmissibility (T) of the 200-foot aquifer is about 126,000 gpd (gallons per day) per ft, and the coefficient of storage (8) is about 0.0002. The T and S values of the 120-foot aquifer are about the same as for the 200-foot aquifer. For the 70-foot aquifer the value of T is about 70,000 gpd per ft, and S is about 0.0007. The data suggest that when the artesian head in the aquifers is lowered by pumping, recharge is induced by leakage from the confining beds.
\nThe 120-foot aquifer is considered the best known source of ground water In the area. The city of Redwood Falls has used this aquifer for its water supply since August 1955 and, in 1960, pumped about 106 million gallons from it. The water level in the aquifer had stabilized by late 1956; considerable additional water probably can be obtained from the aquifer. Although the 70-foot aquifer is not as extensive or as thick as the one at 120 feet, large amounts of water probably can be obtained from this aquifer also. The 200-foot aquifer is narrow, elongate, and irregular in form and appears to be very permeable only locally.
\nChemical analyses show that water from the glacial-drift aquifers is primarily of the bicarbonate type, is hard, and contains an excessive amount of iron. In places water from the Precambrian bedrock is much softer than water from the drift.
","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. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1669R","collaboration":"Prepared in cooperation wit the Division of Waters, Minnesota Department of Conservation, and the city of Redwood Falls","usgsCitation":"Schiner, G.R., and Schneider, R., 1964, Geology and ground-water conditions of the Redwood Falls area, Redwood County, Minnesota: U.S. Geological Survey Water Supply Paper 1669, Document: iv, 46 p.; 11 Plates: 37.00 x 22.43 inches or smaller, https://doi.org/10.3133/wsp1669R.","productDescription":"Document: iv, 46 p.; 11 Plates: 37.00 x 22.43 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":28979,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669r/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28986,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669r/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138209,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1669r/report-thumb.jpg"},{"id":28987,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669r/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28985,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669r/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28988,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669r/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28980,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669r/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28981,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669r/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28982,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669r/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28983,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669r/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28984,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669r/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28989,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669r/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28990,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1669r/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","county":"Redwood County","otherGeospatial":"Redwood Falls area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -95.25,\n 44.6\n ],\n [\n -95.25,\n 44.5\n ],\n [\n -95.016667,\n 44.5\n ],\n [\n -95.016667,\n 44.6\n ],\n [\n -95.25,\n 44.6\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685f8a","contributors":{"authors":[{"text":"Schiner, George R.","contributorId":22743,"corporation":false,"usgs":true,"family":"Schiner","given":"George","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":145564,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schneider, Robert","contributorId":102460,"corporation":false,"usgs":true,"family":"Schneider","given":"Robert","email":"","affiliations":[],"preferred":false,"id":145565,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":3004,"text":"wsp1786 - 1964 - Inventory of published and unpublished chemical analyses of surface waters in the continental United States and Puerto Rico, 1961","interactions":[],"lastModifiedDate":"2017-09-06T17:54:41","indexId":"wsp1786","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":"1786","title":"Inventory of published and unpublished chemical analyses of surface waters in the continental United States and Puerto Rico, 1961","docAbstract":"This inventory contains a list of published and unpublished chemical analyses obtained through September 30, 1961, by agencies associated with the Subcommittee on Hydrology. Bulletin 6 of Subcommittee on Hydrology includes references to all surface-water analyses for states east of the Mississippi River known to exist in the files of Federal agencies through September 30, 1951. Records of analyses of surface waters for states west of the Mississippi River are included in Bulletins 2 and 9 of the Subcommittee. Bulletin 2 includes the period of record prior to October 1, 1947, and Bulletin 9 includes the period from October 1, 1947, to September 30, 1955. Therefore, the earliest date for which references to data are included in this volume varies from October 1951 for states east of the Mississippi River (including Minnesota) to October 1, 1955, for states west of the Mississippi River. Analyses of water from Alaska and Puerto Rico were not reported in earlier inventories. An attempt was made to include available analyses obtained in Alaska since October 1951, but additional chemical determinations of water in Alaska that are not inventoried in this report were undoubtedly made in years prior to 1951. Requests concerning specific records not reported herein should be directed to offices having responsibility in the area.
This publication is patterned after preceding bulletins as far as practicable. The contents include a list of sampling stations and locations, drainage area above each station, period of record, number and frequency of samples collected, number of analytical values reported in each group arranged according to general types or purposes, and a list of references to the sources of basic data.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1786","collaboration":"Prepared in cooperation with the Subcommittee on Hydrology, Inter-Agency Committee on Water Resources","usgsCitation":"Woodard, T.H., and Heidel, S.G., 1964, Inventory of published and unpublished chemical analyses of surface waters in the continental United States and Puerto Rico, 1961: U.S. Geological Survey Water Supply Paper 1786, v, 490 p., https://doi.org/10.3133/wsp1786.","productDescription":"v, 490 p.","numberOfPages":"496","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":29798,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1786/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139406,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1786/report-thumb.jpg"}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66ce7f","contributors":{"authors":[{"text":"Woodard, Thomas H.","contributorId":106102,"corporation":false,"usgs":true,"family":"Woodard","given":"Thomas","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":146135,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Heidel, Sumner Griggs","contributorId":97082,"corporation":false,"usgs":true,"family":"Heidel","given":"Sumner","email":"","middleInitial":"Griggs","affiliations":[],"preferred":false,"id":146134,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":3020,"text":"wsp1608E - 1964 - Hydrogeologic reconnaissance of Poro Point and vicinity, Luzon Island, Philippines","interactions":[],"lastModifiedDate":"2013-08-12T12:26:47","indexId":"wsp1608E","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":"E","title":"Hydrogeologic reconnaissance of Poro Point and vicinity, Luzon Island, Philippines","docAbstract":"In 1961 a reconnaissance of the geology and ground-water hydrology of Poro Point, on the west coast of Luzon Island, Philippines, was made on behalf of the U.S. Department of the Navy. Poro Point, which marks the northern end of Lingayen Gulf, is about half a mile wide and projects northwestward about 2 miles into the China Sea. The point is underlain by coralline limestone of probable Pleistocene age. \n\nThe aquifer system consists of a fresh-water lens floating on salt water within the coralline limestone. Several tube wells obtain fresh water from the lens, but in May, at the end of the 6-month dry season during which rainfall totals only 40 inches, the water becomes brackish. 'Skimming wells' are considered the best method of obtaining fresh water from the lens, whose annual range in average thickness is probably 25 to 40 feet. \n\nRecharge is about 2,000-3,000 acre-feet per year and is derived wholly from precipitation during the 6-month wet season in which rainfall totals about 92 inches. The approximate amount of ground water stored in the fresh-water lens ranges from about 3,000 acre-feet at the end of the dry season to about 5,000 acre-feet at the end of the wet season. Most of the ground water is discharged through seeps and submarine springs around Poro Point; pumpage in 1961 was only about 100 acre-feet.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1608E","usgsCitation":"Worts, G., 1964, Hydrogeologic reconnaissance of Poro Point and vicinity, Luzon Island, Philippines: U.S. Geological Survey Water Supply Paper 1608, iii, 14 p. :ill., map ;24 cm. + plate folded in pocket., https://doi.org/10.3133/wsp1608E.","productDescription":"iii, 14 p. :ill., map ;24 cm. + plate folded in pocket.","costCenters":[],"links":[{"id":139461,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1608e/report-thumb.jpg"},{"id":29850,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1608e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":276481,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1608e/plate-1.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627904","contributors":{"authors":[{"text":"Worts, George Frank","contributorId":100830,"corporation":false,"usgs":true,"family":"Worts","given":"George Frank","affiliations":[],"preferred":false,"id":146158,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":38885,"text":"pp473B - 1964 - Field investigation of mine waters in the northern anthracite field, Pennsylvania","interactions":[],"lastModifiedDate":"2012-02-02T00:10:37","indexId":"pp473B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"473","chapter":"B","title":"Field investigation of mine waters in the northern anthracite field, Pennsylvania","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Mining hydrology","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp473B","usgsCitation":"Barnes, I., Stuart, W., and Fisher, D., 1964, Field investigation of mine waters in the northern anthracite field, Pennsylvania: U.S. Geological Survey Professional Paper 473, p. 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","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geological Survey research, 1963 (Professional Paper 475)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp475D","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1964, Short papers in geology and hydrology, articles 122-172: U.S. Geological Survey Professional Paper 475, vi, 223 p., https://doi.org/10.3133/pp475D.","productDescription":"vi, 223 p.","costCenters":[],"links":[{"id":421303,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28013.htm","linkFileType":{"id":5,"text":"html"}},{"id":120345,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0475d/report-thumb.jpg"},{"id":65896,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0475d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687fb1","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":529890,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70207358,"text":"70207358 - 1964 - Hidden Recharge","interactions":[],"lastModifiedDate":"2019-12-18T10:56:54","indexId":"70207358","displayToPublicDate":"1964-10-31T10:53:38","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1861,"text":"Ground Water","active":true,"publicationSubtype":{"id":10}},"title":"Hidden Recharge","docAbstract":"“Hidden recharge” is defined as subsurface percolation of water from basin‐margin mountains directly into aquifers of the valley basins. It is an important, and sometimes neglected, item in hydrologic equations. Locally, geologic conditions permit inter‐basin circulation of ground water. The concept that ground‐water basins necessarily terminate at the contact between alluvium and hardrock is not tenable. Copyright © 1964, Wiley Blackwell. All rights reserved
","language":"English","publisher":"Wiley Blackwell","doi":"10.1111/j.1745-6584.1964.tb01780.x","issn":" 0017467X","usgsCitation":"Feth, J.H., 1964, Hidden Recharge: Ground Water, v. 2, no. 4, p. 14-17 , https://doi.org/10.1111/j.1745-6584.1964.tb01780.x.","productDescription":"4 p. ","startPage":"14","endPage":"17 ","costCenters":[],"links":[{"id":370399,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"4","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Feth, J. H.","contributorId":50495,"corporation":false,"usgs":true,"family":"Feth","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":777803,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221136,"text":"70221136 - 1964 - The international hydrological decade","interactions":[],"lastModifiedDate":"2021-06-02T19:02:22.503469","indexId":"70221136","displayToPublicDate":"1964-09-01T13:59:52","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"The international hydrological decade","docAbstract":"Work toward establishing a program of international cooperative studies in scientific hydrology began about 4 years ago, and the IHD (International Hydrological Decade) will begin under international auspices in January 1965. This program will be highly important for hydrology and hydrologists, and it should contribute greatly to human welfare in the future. Fortuitously, the opening year coincides with International Cooperation Year of the United Nations Organization. American participation in the program will contribute to the purpose avowed by the President [Johnson, 1964] in a commencement address at Holy Cross early in June 1964: “to dedicate this year to finding new techniques for making Man's knowledge serve Man's welfare. Let this be a year of science.”
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR045i003p00413","usgsCitation":"Nace, R.L., 1964, The international hydrological decade: Eos, Transactions, American Geophysical Union, v. 45, no. 3, p. 413-421, https://doi.org/10.1029/TR045i003p00413.","productDescription":"9 p.","startPage":"413","endPage":"421","costCenters":[],"links":[{"id":386151,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"45","issue":"3","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Nace, R. L.","contributorId":11332,"corporation":false,"usgs":true,"family":"Nace","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":816828,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221177,"text":"70221177 - 1964 - Geohydrologic analogies between the Jordan Valleys of Utah and the holy land","interactions":[],"lastModifiedDate":"2021-06-04T17:05:35.301848","indexId":"70221177","displayToPublicDate":"1964-09-01T12:01:39","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5334,"text":"International Association of Scientific Hydrology - Bulletin ","onlineIssn":"2150-3435","printIssn":"0262-6667","active":false,"publicationSubtype":{"id":10}},"title":"Geohydrologic analogies between the Jordan Valleys of Utah and the holy land","docAbstract":"The biblical Jordan River Valley, which extends from Lake Tiberias (the Sea of Galilee) to the Dead Sea, is decidedly similar to the Jordan River Valley of Utah, which joins Lake Utah and Great Salt Lake. Both Jordan Rivers drain relatively large fresh-water lakes and also are major sources of discharge into large salty lakes that have no outlets to the ocean.The two Jordan River valleys and the highlands and mountains that surround them, have many physiographic, geologic, and hydrologic similarities as well as some noteworthy differences. For example, an hypothesis for the formation of the Dead Sea-Jordan Valley rift is that the east Jordan block slid northward with respect to the west Jordan block. The amount of displacement is estimated to be about 65 miles and took place partly in Miocene and possible Pliocène and partly in Pleistocene time. Tectonc activity has also been a major factor in the formation of the Jordan valley of Utah, but the movement here probably was along large normal faults in late Tertiary and Quaternary time. The sediments underlying both Jordan River valleys were deposited in ancestral lacustrine and fluvial environments. Abundant supplies of ground water are found under both valleys, but probably larger supplies of better quality water can be obtained in Utah. Both valleys contain numerous small nonthermal and a few large thermal springs.
","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626666409493666","usgsCitation":"Bradley, E., 1964, Geohydrologic analogies between the Jordan Valleys of Utah and the holy land: International Association of Scientific Hydrology - Bulletin , v. 9, no. 3, p. 12-23, https://doi.org/10.1080/02626666409493666.","productDescription":"12 p.","startPage":"12","endPage":"23","costCenters":[],"links":[{"id":489070,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/02626666409493666","text":"Publisher Index Page"},{"id":386209,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -114.06005859375,\n 42.00032514831621\n ],\n [\n -114.0380859375,\n 37.07271048132943\n ],\n [\n -109.05029296875,\n 37.03763967977139\n ],\n [\n -109.1162109375,\n 41.0130657870063\n ],\n [\n -111.07177734375,\n 41.02964338716638\n ],\n [\n -111.07177734375,\n 41.983994270935625\n ],\n [\n -114.06005859375,\n 42.00032514831621\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"9","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Bradley, Edward","contributorId":67071,"corporation":false,"usgs":true,"family":"Bradley","given":"Edward","email":"","affiliations":[],"preferred":false,"id":816980,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221179,"text":"70221179 - 1964 - The father of modern ground water hydrology","interactions":[],"lastModifiedDate":"2021-06-04T17:17:06.636524","indexId":"70221179","displayToPublicDate":"1964-04-01T12:14:32","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"The father of modern ground water hydrology","docAbstract":"No abstract available.
","language":"English","publisher":"Elsevier","doi":"10.1111/j.1745-6584.1964.tb01749.x","usgsCitation":"Hackett, O.M., 1964, The father of modern ground water hydrology: Groundwater, v. 2, no. 2, p. 2-5, https://doi.org/10.1111/j.1745-6584.1964.tb01749.x.","productDescription":"4 p.","startPage":"2","endPage":"5","costCenters":[],"links":[{"id":386213,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"2","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Hackett, O. M.","contributorId":38527,"corporation":false,"usgs":true,"family":"Hackett","given":"O.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":816986,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010471,"text":"70010471 - 1964 - Tritium-hydrologic research: Some results of the U.S. Geological Survey Research Program","interactions":[],"lastModifiedDate":"2026-02-13T16:21:12.862036","indexId":"70010471","displayToPublicDate":"1964-02-02T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Tritium-hydrologic research: Some results of the U.S. Geological Survey Research Program","docAbstract":"In general tritium is of limited usefulness as a tool in hydrologic studies because the tritium content of ground water, as a result of radioactive decay, becomes too low to be detectable after about 50 years. Nevertheless, a unique study was made of the hydrologic cycle of small stream basins in Wisconsin and New Jersey on the basis of measurements relative to the peak of tritium fallout in the spring of 1958. The continental and the coastal basins received approximately the same tritium fallout. Approximately 30 percent went into ground-water storage, the remainder being exported as runoff and evapotranspiration. The mean residence time for ground-water recharge for the two basins was 45 and 30 days, respectively.","language":"English","publisher":"American Association for the Advancement of Science.","doi":"10.1126/science.143.3608.804","issn":"00368075","usgsCitation":"Carlston, C., 1964, Tritium-hydrologic research: Some results of the U.S. Geological Survey Research Program: Science, v. 143, no. 3608, p. 804-806, https://doi.org/10.1126/science.143.3608.804.","productDescription":"3 p.","startPage":"804","endPage":"806","costCenters":[],"links":[{"id":219076,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Jersey, Wisconsin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -92.65443024683039,\n 47.18686471532902\n ],\n [\n -92.92337344008368,\n 44.76948314682184\n ],\n [\n -91.54422384565291,\n 43.91380985726313\n ],\n [\n -90.40331265602809,\n 42.36186629934298\n ],\n [\n -87.66640475516137,\n 42.473317234890345\n ],\n [\n -86.69378362897187,\n 45.09478563580936\n ],\n [\n -87.76789223463291,\n 45.99366780802788\n ],\n [\n -89.9402097973789,\n 46.41028342019218\n ],\n [\n -89.94150082434655,\n 47.33914537549116\n ],\n [\n -92.65443024683039,\n 47.18686471532902\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -75.03044920156037,\n 41.368918438639554\n ],\n [\n -75.21217801383332,\n 40.6314679025723\n ],\n [\n -74.81474599562263,\n 40.24767874671271\n ],\n [\n -75.6121640073091,\n 39.468177148463866\n ],\n [\n -74.80122580215662,\n 38.82749379603797\n ],\n [\n -74.0060957836949,\n 40.04453424272181\n ],\n [\n -73.96363933005574,\n 41.368918438639554\n ],\n [\n -75.03044920156037,\n 41.368918438639554\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"143","issue":"3608","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb875e4b08c986b327884","contributors":{"authors":[{"text":"Carlston, C.W.","contributorId":26062,"corporation":false,"usgs":true,"family":"Carlston","given":"C.W.","affiliations":[],"preferred":false,"id":358994,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70095523,"text":"70095523 - 1964 - Sedimentology: general introduction and definitions : fluvial sediment and channel morphology","interactions":[],"lastModifiedDate":"2014-03-25T10:35:32","indexId":"70095523","displayToPublicDate":"1964-01-01T13:52:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Sedimentology: general introduction and definitions : fluvial sediment and channel morphology","docAbstract":"Sedimentology, the study of sedimentary rocks and the \nprocesses by which they are formed, includes and is related \nto a large number of phenomena. Sedimentology includes the \nfive fundamental processes defined by the term sediaentation \n--weathering, erosion, transportation, deposition and \ndiagenesis. \nSedimentology shares with geomorphology the study of \nthe surface features of the earth. Sedimentology also \nshares with hydrology the study of river.--channels. River \nchannels are formed in part or in total as a result of \nflowing water and sediment transport, commonly called the \n\"work of the rivers.\" \nThis survey of published literature was made to aid in \narriving at definitions which would be acceptable to, and \nrepresentative of, a majority of professional personnel \nactively engaged in laboratory and field investigations \nrelated to the \"work of the river.\" The definitions in this \nlist are intended to explain the terms used in studies of \nfluvial sediment and channel morphology. No set of \ndefinitions can expect universal acceptance, however, i t is \nhoped that this compilation will be considered a summary \nand synthesis of present and past usage and that it will \nserve as a starting point for future usage. \nMultiple references are cited from textbooks, glossaries and dictionaries, scientific journals and u.s. Government \npublications. To obtain a mutual understanding and enhance \nprecision, many of the proposed definitions are a composite \nof those selected from papers or reports covering research \nstudies and field investigations. \n\nA draft of this glossary has been reviewed by a group of \ninterested personnel. The results of this review have been \ncarefully considered and the originally-suggested definitions \nhave been revised accordingly, resulting in the present \ncompilation. \nR. G. Wolff, with the help of Mrs. v. Blatcher, carried \nout the literature search and compilation of terms and the \nreview results. Paul c. Benedict approved or composed the \ndefinitions as presented in this report.","language":"English","publisher":"U.S. Geological Survey, Water Resources Division","publisherLocation":"Washington, DC","doi":"10.3133/70095523","usgsCitation":"Wolff, R.G., and Benedict, P., 1964, Sedimentology: general introduction and definitions : fluvial sediment and channel morphology: Open-File Report, iii, 132 p., https://doi.org/10.3133/70095523.","productDescription":"iii, 132 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":283310,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70095523.jpg"},{"id":284835,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70095523/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5355955fe4b0120853e8c1d4","contributors":{"authors":[{"text":"Wolff, Roger G.","contributorId":19580,"corporation":false,"usgs":true,"family":"Wolff","given":"Roger","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":491227,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Benedict, Paul C.","contributorId":72293,"corporation":false,"usgs":true,"family":"Benedict","given":"Paul C.","affiliations":[],"preferred":false,"id":491228,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70094923,"text":"70094923 - 1964 - Soil mechanics and soil physics symbols and nomenclature useful in hydrologic studies","interactions":[],"lastModifiedDate":"2014-02-25T13:59:49","indexId":"70094923","displayToPublicDate":"1964-01-01T13:50:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Soil mechanics and soil physics symbols and nomenclature useful in hydrologic studies","docAbstract":"The study of hydrology requires an interdisciplinary approach,\nincorporating knowledge from fields such as engineering, geology,\nchemistry, and agriculture. With increasing frequency, the hydrologist\nfinds it necessary to study the literature of the soil mechanics and\nsoil physics disciplines for assistance in the solution of hydrologic\nproblems. Because of the inter-relation between hydrology and soil\nmechanics and soil physics, hydrologists also are preparing an increasing\nnumber of technical papers ·for use by these two disciplines.\nTo permit the hydrologist to better understand specialized literature,\nas well as to assist him in preparing papers for these disciplines,\nthis glossary of soil mechanics and soil physics nomenclature was prepared.\nIt is a compilation from standards, dictionaries, and glossaries published\nby technical societies, and from reports by selected authorities in the\nfields of soil mechanics and soil physics. The variety of symbols and\ndefinitions presented for many of the terms demonstrates the difficulty\nthat has been encountered over the years in reaching agreement on such a\nsubject as nomenclature. Both old and new definitions and symbols are\npresented to assist the hydrologist in reading literature. Whenever\npossible the more recent symbols and nomenclature should be used by the\nhydrologist in writing papers for soil mechanics or soil physics audiences.\nWhen the hydrologist finds it necessary to use symbols or terms not included\nin the present list, he should try to select those not in conflict with the\nrecent systems presented in this report.\nSymbols are listed in alphabetical order to assist readers in finding\nthe term represented by a given symbol. Terms also are listed alphabetically,\nusually followed by recommended symbols and brief definitions.\nWhere two or more symbols or definitions are listed following a term, no\nsignificance should be placed on the order of presentation. The source is\nindicated for each symbol, term, or definition, and the sources are listed\nin the cited references.\nIt is emphasized that this report is only a compilation of nomenclature\ngenerally accepted in the soil mechanics apd soil physics disciplines.\nIt does not necessarily represent the recommendations or usage of such\nnomenclature by the Geological Survey or any part of its organization.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/70094923","usgsCitation":"Johnson, A., 1964, Soil mechanics and soil physics symbols and nomenclature useful in hydrologic studies: Open-File Report, 50 p., https://doi.org/10.3133/70094923.","productDescription":"50 p.","numberOfPages":"53","costCenters":[],"links":[{"id":282776,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70094923.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd732ce4b0b29085108c64","contributors":{"authors":[{"text":"Johnson, A.I.","contributorId":82676,"corporation":false,"usgs":true,"family":"Johnson","given":"A.I.","email":"","affiliations":[],"preferred":false,"id":490965,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221133,"text":"70221133 - 1964 - Hydrologic factors pertinent to ground‐water contamination","interactions":[],"lastModifiedDate":"2021-06-02T18:50:54.556763","indexId":"70221133","displayToPublicDate":"1964-01-01T13:47:53","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Hydrologic factors pertinent to ground‐water contamination","docAbstract":"Predictions of where and how a fluid waste may travel from disposal site to the water table require detailed information on the physical characteristics, location, and extent of all pervious and impervious materials in the unsaturated zone. Principles concerning the flow system in the unsaturated zone indicate the importance of choice of disposal technique in predicting the time required for the fluid waste to traverse the distance to the water table. With appropriate data on the location, extent, and physical properties of water‐bearing materials and on the boundaries of the saturated zone flow system, it is possible to analyze the relative merits of a variety of waste disposal techniques and to describe the probable consequences of each. Environments of consolidated rocks, such as granites, sandstones, and limestones, pose problems in addition to those related to unconsolidated or granular porous media in defining the fluid‐flow regimes that involve joint patterns, fracture patterns, solutional openings, and the rock structure. The consequences of ground‐water contamination can be just as damaging to water users as the pollution of surface streams. In fact it can be argued that the consequences are far more damaging because they persist over much longer periods of time after the contaminating source has been eliminated. It would appear prudent, therefore, to guard against contamination of the ground‐water resource in the first instance, rather than to engage in long expensive rehabilitation measures after the damage has been done. In 1960 Graham Walton presented data concerning contamination, by sewage or other man‐made wastes, of surface and underground waters. The circumstances attending the reported incidents of contamination, especially those involving ground‐water supplies, have aided materially in the choice of a few principles and ideas that will identify the role of some significant hydrologic factors in the underground movement of fluid wastes. Walton's discussion of ground‐water contamination refers often to physical settings into which fluid wastes are discharged at or near the land surface into cesspools, tile‐drain fields, and holding ponds. Furthermore, most reported instances of ground‐water contamination have taken place in relatively humid.
","language":"English","publisher":"Wiley Blackwell","doi":"10.1111/j.1745-6584.1964.tb01739.x","usgsCitation":"Brown, R., 1964, Hydrologic factors pertinent to ground‐water contamination: Groundwater, v. 2, no. 1, p. 5-12, https://doi.org/10.1111/j.1745-6584.1964.tb01739.x.","productDescription":"8 p.","startPage":"5","endPage":"12","costCenters":[],"links":[{"id":386147,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"1","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Brown, R.","contributorId":101419,"corporation":false,"usgs":true,"family":"Brown","given":"R.","affiliations":[],"preferred":false,"id":816821,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221132,"text":"70221132 - 1964 - Hydrologic factors pertinent to ground‐water contamination","interactions":[],"lastModifiedDate":"2021-06-04T12:04:08.414151","indexId":"70221132","displayToPublicDate":"1964-01-01T13:47:53","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Hydrologic factors pertinent to ground‐water contamination","docAbstract":"Predictions of where and how a fluid waste may travel from disposal site to the water table require detailed information on the physical characteristics, location, and extent of all pervious and impervious materials in the unsaturated zone. Principles concerning the flow system in the unsaturated zone indicate the importance of choice of disposal technique in predicting the time required for the fluid waste to traverse the distance to the water table. With appropriate data on the location, extent, and physical properties of water‐bearing materials and on the boundaries of the saturated zone flow system, it is possible to analyze the relative merits of a variety of waste disposal techniques and to describe the probable consequences of each. Environments of consolidated rocks, such as granites, sandstones, and limestones, pose problems in addition to those related to unconsolidated or granular porous media in defining the fluid‐flow regimes that involve joint patterns, fracture patterns, solutional openings, and the rock structure. The consequences of ground‐water contamination can be just as damaging to water users as the pollution of surface streams. In fact it can be argued that the consequences are far more damaging because they persist over much longer periods of time after the contaminating source has been eliminated. It would appear prudent, therefore, to guard against contamination of the ground‐water resource in the first instance, rather than to engage in long expensive rehabilitation measures after the damage has been done. In 1960 Graham Walton presented data concerning contamination, by sewage or other man‐made wastes, of surface and underground waters. The circumstances attending the reported incidents of contamination, especially those involving ground‐water supplies, have aided materially in the choice of a few principles and ideas that will identify the role of some significant hydrologic factors in the underground movement of fluid wastes. Walton's discussion of ground‐water contamination refers often to physical settings into which fluid wastes are discharged at or near the land surface into cesspools, tile‐drain fields, and holding ponds. Furthermore, most reported instances of ground‐water contamination have taken place in relatively humid.
","language":"English","publisher":"NGWA The Groundwater Association","doi":"10.1111/j.1745-6584.1964.tb01739.x","usgsCitation":"Brown, R., 1964, Hydrologic factors pertinent to ground‐water contamination: Groundwater, v. 2, no. 1, p. 5-12, https://doi.org/10.1111/j.1745-6584.1964.tb01739.x.","productDescription":"8 p.","startPage":"5","endPage":"12","costCenters":[],"links":[{"id":386191,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"1","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Brown, R.","contributorId":101419,"corporation":false,"usgs":true,"family":"Brown","given":"R.","affiliations":[],"preferred":false,"id":816940,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}