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Potable and near-potable water is obtained from 12 wells in this area that tap sand and gravel, and the wells are capable of yielding 1,000 gallons per minute or more. \r\n\r\nStallion Range Center, a military installation on the White Sands Missile Range, about 15 miles east of =he waterfowl refuge, needs about 100,000 gallons per day of potable water. Potable water in large quantities is not known to be available at a location closer to the Center than the refuge area.\r\n\r\nThe Fish and Wildlife Service, which operates the waterfowl refuge, gave permission to White Sands Missile Range to test drill and to develop a supply well in certain areas along the Rio Grande outside the managed lands of the refuge. The U.S. Geological Survey was then asked by White Sands Missile Range to choose locations for test drilling and to monitor drilling and testing of the wells. \r\n\r\nBetween 1963 and 1967 test wells were drilled and a suitable location for a supply well as found. 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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha288","usgsCitation":"Hickenlooper, I.J., 1968, Floods in the Mayaguez area of Puerto Rico: U.S. Geological Survey Hydrologic Atlas 288, 1 Plate: 39.50 × 35.00 inches, https://doi.org/10.3133/ha288.","productDescription":"1 Plate: 39.50 × 35.00 inches","costCenters":[],"links":[{"id":185696,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":409761,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15657.htm","linkFileType":{"id":5,"text":"html"}},{"id":89766,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/288/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"20000","country":"United States","state":"Puerto Rico","otherGeospatial":"Mayaguez area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -67.192,\n 18.125\n ],\n [\n -67.192,\n 18.25\n ],\n [\n -67.125,\n 18.25\n ],\n [\n -67.125,\n 18.125\n ],\n [\n -67.192,\n 18.125\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e09c5","contributors":{"authors":[{"text":"Hickenlooper, Irby J.","contributorId":103366,"corporation":false,"usgs":true,"family":"Hickenlooper","given":"Irby","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":278015,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68314,"text":"ha289 - 1968 - Floods in the area of Vega Alta and Vega Baja, Puerto Rico","interactions":[],"lastModifiedDate":"2012-02-10T00:11:26","indexId":"ha289","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"289","title":"Floods in the area of Vega Alta and Vega Baja, Puerto Rico","language":"ENGLISH","doi":"10.3133/ha289","usgsCitation":"Hickenlooper, I.J., 1968, Floods in the area of Vega Alta and Vega Baja, Puerto Rico: U.S. Geological Survey Hydrologic Atlas 289, 1 map., https://doi.org/10.3133/ha289.","productDescription":"1 map.","costCenters":[],"links":[{"id":185695,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89765,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/289/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"20000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -66.43333333333334,18.4 ], [ -66.43333333333334,18.5 ], [ -66.30083333333333,18.5 ], [ -66.30083333333333,18.4 ], [ -66.43333333333334,18.4 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e09a7","contributors":{"authors":[{"text":"Hickenlooper, Irby J.","contributorId":103366,"corporation":false,"usgs":true,"family":"Hickenlooper","given":"Irby","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":278014,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68305,"text":"ha297 - 1968 - Floods on Chenango River and Canasawacta Creek at Norwich, New York","interactions":[],"lastModifiedDate":"2012-02-10T00:11:30","indexId":"ha297","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"297","title":"Floods on Chenango River and Canasawacta Creek at Norwich, New York","language":"ENGLISH","doi":"10.3133/ha297","usgsCitation":"Hladio, S., 1968, Floods on Chenango River and Canasawacta Creek at Norwich, New York: U.S. Geological Survey Hydrologic Atlas 297, 1 map., https://doi.org/10.3133/ha297.","productDescription":"1 map.","costCenters":[],"links":[{"id":186690,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89745,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/297/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"2000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75.56666666666666,42.50083333333333 ], [ -75.56666666666666,42.583333333333336 ], [ -75.5,42.583333333333336 ], [ -75.5,42.50083333333333 ], [ -75.56666666666666,42.50083333333333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df8e1","contributors":{"authors":[{"text":"Hladio, Stephen","contributorId":67952,"corporation":false,"usgs":true,"family":"Hladio","given":"Stephen","email":"","affiliations":[],"preferred":false,"id":277997,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70112271,"text":"70112271 - 1968 - Color photographs for water resources studies","interactions":[],"lastModifiedDate":"2017-03-27T13:55:48","indexId":"70112271","displayToPublicDate":"1990-06-12T11:34:00","publicationYear":"1968","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3051,"text":"Photogrammetric Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Color photographs for water resources studies","docAbstract":"Air-photo interpretation is very well suited to water resources studies where limited observations of hydrologic data must be extended to regional characteristics for large areas. It is also useful in monitoring the hydrologic regimen of an area to detect possible changes. Color aerial photography is generally superior to black-and-white photography for these water resources investigations. Depth penetration through water, and excellent discrimination of water indicators, such as vegetation, are its -main assets. Meaningful interpretation of the photography depends on adequate ground control data. Experiences of the Water Resources Division, U. S. Geological Survey, indicate that the best interpretation is done by professional personnel-engineers, geologists, and water chemists intimately associated with a particular water resources project for which the photography has been obtained.
","language":"English","publisher":"American Society of Photogrammetry","publisherLocation":"Falls Church, VA","usgsCitation":"Schneider, W.J., 1968, Color photographs for water resources studies: Photogrammetric Engineering, v. 34, no. 3, p. 257-262.","productDescription":"6 p.","startPage":"257","endPage":"262","numberOfPages":"6","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288472,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"34","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"539acbebe4b0e83db6d08ed6","contributors":{"authors":[{"text":"Schneider, William J.","contributorId":47349,"corporation":false,"usgs":true,"family":"Schneider","given":"William","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":494605,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221423,"text":"70221423 - 1968 - Microcanonical ensembles of river nets","interactions":[],"lastModifiedDate":"2021-06-15T12:57:52.990625","indexId":"70221423","displayToPublicDate":"1968-12-01T07:54:33","publicationYear":"1968","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":"Microcanonical ensembles of river nets","docAbstract":"It is shown that a thermodynamic analogy can be set up for structurally cyclic as well as for noncyclic river nets that satisfy Horton's law of stream numbers. In the latter case, the microcanonical formalism of statistical thermodynamics has to be used.
","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626666809493629","usgsCitation":"Scheidegger, A.E., 1968, Microcanonical ensembles of river nets: International Association of Scientific Hydrology - Bulletin , v. 13, no. 4, p. 87-90, https://doi.org/10.1080/02626666809493629.","productDescription":"4 p.","startPage":"87","endPage":"90","costCenters":[],"links":[{"id":480332,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/02626666809493629","text":"Publisher Index Page"},{"id":386490,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Scheidegger, Adrian E.","contributorId":100370,"corporation":false,"usgs":true,"family":"Scheidegger","given":"Adrian","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":817672,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011485,"text":"70011485 - 1968 - Uranium disequilibrium in groundwater: An isotope dilution approach in hydrologic investigations","interactions":[],"lastModifiedDate":"2026-02-05T20:00:55.988607","indexId":"70011485","displayToPublicDate":"1968-11-29T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Uranium disequilibrium in groundwater: An isotope dilution approach in hydrologic investigations","docAbstract":"The distribution and environmental disequilibrium patterns of naturally occurring uranium isotopes (U234 and U238) in waters of the Floridan aquifer suggest that variations in the ratios of isotopic activity and concentrations can be used quantitatively to evaluate mixing proportions of waters from differing sources. Uranium is probably unique in its potential for this approach, which seems to have general usefulness in hydrologic investigations.
","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.162.3857.997","issn":"00368075","usgsCitation":"Osmond, J., Rydell, H., and Kaufman, M.I., 1968, Uranium disequilibrium in groundwater: An isotope dilution approach in hydrologic investigations: Science, v. 162, no. 3857, p. 997-999, https://doi.org/10.1126/science.162.3857.997.","productDescription":"3 p.","startPage":"997","endPage":"999","costCenters":[],"links":[{"id":220907,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -87.75892866886728,\n 31.143268810573844\n ],\n [\n -87.62303351734478,\n 30.238600918743856\n ],\n [\n -83.81354821489576,\n 29.00906335007337\n ],\n [\n -82.3323690353631,\n 24.615788803974226\n ],\n [\n -79.6864857441564,\n 24.55462324894998\n ],\n [\n -80.03387638676382,\n 27.87855451506119\n ],\n [\n -81.46928356514647,\n 30.78587593625049\n ],\n [\n -87.75892866886728,\n 31.143268810573844\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"162","issue":"3857","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbda6e4b08c986b32914c","contributors":{"authors":[{"text":"Osmond, J.K.","contributorId":78467,"corporation":false,"usgs":true,"family":"Osmond","given":"J.K.","email":"","affiliations":[],"preferred":false,"id":361227,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rydell, H.S.","contributorId":48704,"corporation":false,"usgs":true,"family":"Rydell","given":"H.S.","email":"","affiliations":[],"preferred":false,"id":361225,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kaufman, M. I.","contributorId":66847,"corporation":false,"usgs":true,"family":"Kaufman","given":"M.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":361226,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70171538,"text":"70171538 - 1968 - Use of dye tracers to collect hydrologic data in Oregon","interactions":[],"lastModifiedDate":"2021-06-14T12:30:37.551585","indexId":"70171538","displayToPublicDate":"1968-11-27T18:30:00","publicationYear":"1968","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3718,"text":"Water Resources Bulletin","printIssn":"0043-1370","active":true,"publicationSubtype":{"id":10}},"title":"Use of dye tracers to collect hydrologic data in Oregon","docAbstract":"Dye tracers have been used in Oregon in the Collection of hydrologic data on 2,350 miles of stream channels in the Long Tom, Umpqua, Willmette, and John Day River basins, and in the Carmen‐Smith power tunnel. These investigations demonstrated the usefulness, of dye tracers for determining: (1) estimates of traveltimes and travel rates of water, (2) discharge where standard methods of measuring are not applicable, and (3) dispersion characteristics of streams. Illustrations are used to present the results of time‐of‐travel studies in simple, concise, and readily interpreted form.
","language":"English","publisher":"Wiley","doi":"10.1111/j.1752-1688.1968.tb02937.x","issn":"1093-474X","usgsCitation":"Harris, D., and Sanderson, R., 1968, Use of dye tracers to collect hydrologic data in Oregon: Water Resources Bulletin, v. 4, no. 2, p. 51-68, https://doi.org/10.1111/j.1752-1688.1968.tb02937.x.","productDescription":"18 p.","startPage":"51","endPage":"68","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":322096,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -116.93847656250001,\n 46.13417004624326\n ],\n [\n -122.6953125,\n 45.583289756006316\n ],\n [\n -123.00292968749999,\n 46.13417004624326\n ],\n [\n -124.0576171875,\n 46.31658418182218\n ],\n [\n -124.45312499999999,\n 42.84375132629021\n ],\n [\n -124.45312499999999,\n 42.032974332441405\n ],\n [\n -117.02636718749999,\n 42.00032514831621\n ],\n [\n -116.89453125,\n 44.15068115978094\n ],\n [\n -117.24609374999999,\n 44.33956524809713\n ],\n [\n -116.4111328125,\n 45.67548217560647\n ],\n [\n -116.93847656250001,\n 46.13417004624326\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"4","issue":"2","noUsgsAuthors":false,"publicationDate":"2007-06-08","publicationStatus":"PW","scienceBaseUri":"575158bde4b053f0edd03ca2","contributors":{"authors":[{"text":"Harris, D.D.","contributorId":59002,"corporation":false,"usgs":true,"family":"Harris","given":"D.D.","email":"","affiliations":[],"preferred":false,"id":631698,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sanderson, R.B.","contributorId":169982,"corporation":false,"usgs":false,"family":"Sanderson","given":"R.B.","email":"","affiliations":[],"preferred":false,"id":631699,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70175446,"text":"70175446 - 1968 - Ground-water flow related to streamflow and water quality","interactions":[],"lastModifiedDate":"2018-04-02T12:03:05","indexId":"70175446","displayToPublicDate":"1968-08-15T13:15:00","publicationYear":"1968","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Ground-water flow related to streamflow and water quality","docAbstract":"A ground-water flow system in southwestern Minnesota illustrates water movement between geologic units and between the land surface and the subsurface. The flow patterns indicate numerous zones of ground-water recharge and discharge controlled by topography, varying thicknesses of geologic units, variation in permeabilities, and the configuration of the basement rock surface. Variations in streamflow along a reach of the Yellow Medicine River agree with the subsurface flow system. Increases and decreases in runoff per square mile correspond, apparently, to ground-water discharge and recharge zones. Ground-water quality variations between calcium sulfate waters typical of the Quaternary drift and sodium chloride waters typical of the Cretaceous rocks are caused by mixing of the two water types. The zones of mixing are in agreement with ground-water flow patterns along the hydrologic section.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR004i004p00769","usgsCitation":"Van Voast, W.A., and Novitzki, R., 1968, Ground-water flow related to streamflow and water quality: Water Resources Research, v. 4, no. 4, p. 769-775, https://doi.org/10.1029/WR004i004p00769.","productDescription":"7 p.","startPage":"769","endPage":"775","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":326403,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"4","issue":"4","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"57ada1c7e4b0f412a62dfa7a","contributors":{"authors":[{"text":"Van Voast, Wayne A.","contributorId":91846,"corporation":false,"usgs":true,"family":"Van Voast","given":"Wayne","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":645256,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Novitzki, R.P.","contributorId":73986,"corporation":false,"usgs":true,"family":"Novitzki","given":"R.P.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":645257,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70221391,"text":"70221391 - 1968 - Reforestation with conifers-its effect on streamflow in central New York","interactions":[],"lastModifiedDate":"2021-06-14T12:39:25.123987","indexId":"70221391","displayToPublicDate":"1968-06-01T07:35:29","publicationYear":"1968","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2126,"text":"JAWRA","active":true,"publicationSubtype":{"id":10}},"title":"Reforestation with conifers-its effect on streamflow in central New York","docAbstract":"During the early 1930's, more than 340,000 acres of abandoned farmland in New York State were purchased by the State Conservation Department for the planting, growing, and harvesting of trees. Since then, this land has developed from a heavy cover of weeds and brush into dense coniferous woodlands with trees averaging well over 30 feet high. Hydrologic data have been collected since 1932 in Central New York to determine the effect of the reforestation on streamflow. Data are available for three small partly reforested areas and for one non‐reforested control area. Intensive statistical analyses of the data from the four study areas were made in 1958. It was determined at that time that significant reductions in total runoff had occurred which were attributed to increases in interception and transpiration. Reductions in peak discharges during the dormant season also were indicated which were attributed to increased interception and sublimation of snowfall, and gradual desynchronization of snowmelt runoff from the wooded and open areas of partly reforested watersheds. Updating of the studies relating to peak discharges was completed in 1967 and indicated that no further changes in relative peaks had taken place since 1958. From this it is concluded that the influence exerted by the forest had become maximum by 1958 and has remained stable since then.
","language":"English","publisher":"Wiley","doi":"10.1111/j.1752-1688.1968.tb02932.x","usgsCitation":"Ayer, G.R., 1968, Reforestation with conifers-its effect on streamflow in central New York: JAWRA, v. 4, no. 2, p. 13-24, https://doi.org/10.1111/j.1752-1688.1968.tb02932.x.","productDescription":"10 p.","startPage":"13","endPage":"24","costCenters":[],"links":[{"id":386458,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","otherGeospatial":"central New York","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -78.9697265625,\n 42.342305278572816\n ],\n [\n -73.54248046875,\n 42.342305278572816\n ],\n [\n -73.54248046875,\n 43.51668853502906\n ],\n [\n -78.9697265625,\n 43.51668853502906\n ],\n [\n -78.9697265625,\n 42.342305278572816\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"4","issue":"2","noUsgsAuthors":false,"publicationDate":"2007-06-08","publicationStatus":"PW","contributors":{"authors":[{"text":"Ayer, Gordon Roundy","contributorId":52950,"corporation":false,"usgs":true,"family":"Ayer","given":"Gordon","email":"","middleInitial":"Roundy","affiliations":[],"preferred":false,"id":817497,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70270179,"text":"70270179 - 1968 - Floods in Maline Creek Basin, St. Louis County, Missouri","interactions":[],"lastModifiedDate":"2025-08-13T20:08:06.968773","indexId":"70270179","displayToPublicDate":"1968-01-01T15:52:28","publicationYear":"1968","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":"Floods in Maline Creek Basin, St. Louis County, Missouri","docAbstract":"The rapid growth of suburban St. Louis presents problems in the economic development of flood plains within the area. The U.S. Geological Survey in cooperation with the Metropolitan St. Louis Sewer District has a project to study the hydrology of five major drainage basins within the area of responsibility of the Sewer District.
This report presents hydrologic data on two flood events that can be used in evaluating the extent and depth of flooding with respect to a given stage in the Maline Creek basin. The report will aid decision making in the utilization of flood plains by providing data necessary to solve existing flood problems, and for regulating usage of flood plains to minimize the creation of new flood problems. Data are presented which will be useful in flood-plain zoning and building regulations, locating disposal facilities, locating recreational areas, designing storm and sanitary sewers, and for future bridge and culvert design.
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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Spencer, Donald W.","contributorId":27523,"corporation":false,"usgs":true,"family":"Spencer","given":"Donald","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":945674,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hauth, Leland D.","contributorId":17219,"corporation":false,"usgs":true,"family":"Hauth","given":"Leland","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":945675,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70221375,"text":"70221375 - 1968 - Well logging in ground‐water hydrology","interactions":[],"lastModifiedDate":"2021-06-11T17:14:12.52318","indexId":"70221375","displayToPublicDate":"1968-01-01T12:11:27","publicationYear":"1968","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Well logging in ground‐water hydrology","docAbstract":"In 1966 more than 50 billion gallons of water was pumped daily from an estimated 10 to 15 million water wells in the United States. This was more than one‐sixth of the national withdrawal of water. On the basis of past rates of increase, a much greater future use of ground water is suggested. Our annual investment in water wells is one‐half to three‐quarter billion dollars, not including pumps and plumbing. In 1964 approximately 436,000 new wells were drilled; however, less than 1 percent of these wells were logged by any geophysical means. The application of _ge_o.phy.sical well logging to ground‐water hydrology is comparable to its use in petroleum exploration in the 1930's; however, we can take advantage of equipment and interpretation techniques developed in the oil industry that are available now for use in ground‐water investigations. Although most petroleum well logging techniques may be utilized in hydrology; modifications in equipment and interpretation are necessary because of basic economic and environmental differences between petroleum and ground‐water evaluation. If logging is to be widely applied to ground‐water exploration and evaluation, the expense of equipment and services must be reduced. Fortunately, this can be accomplished, because most water wells are not as deep as oil wells and the temperatures and pressures are lower. The Water Resources Division of the U. S. Geological Survey is conducting research on the application of borehole geophysics to ground‐water hydrology. The following logging devices are utilized in the evaluation of ground‐water environments: spontaneous potential, resistivity, gamma, gamma‐gamma, neutron, radioactive tracer, flowmeter, caliper, fluid resistivity, gradient and differential temperature, and sonic velocity. Lightweight logging sondes and control modules are operated by one man, either on a vehicle‐mounted 6,000‐foot logger or on a suitcase‐mounted 500‐foot logger. An inexpensive magnetic tape system has been developed and is used routinely for log recording and playback. If commercial well logging service is to be widely used in ground‐water exploration and development, water well contractors, and State and municipal agencies must be educated on the advantages of obtaining more information from each hole drilled. It will be necessary also to demonstrate how well logging can provide much of this information. In addition, the well logging industry must adapt their equipment and services to the requirements of ground‐water hydrology. The need for additional logging capability in this field exists at the present time and is expected to increase. Hopefully industry will be able to fill the gap.
","language":"English","publisher":"NGWA The Groundwater Association","doi":"10.1111/j.1745-6584.1968.tb01630.x","usgsCitation":"Keys, W., 1968, Well logging in ground‐water hydrology: Groundwater, v. 6, no. 1, p. 10-18, https://doi.org/10.1111/j.1745-6584.1968.tb01630.x.","productDescription":"9 p.","startPage":"10","endPage":"18","costCenters":[],"links":[{"id":386438,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"1","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Keys, W.S.","contributorId":75126,"corporation":false,"usgs":true,"family":"Keys","given":"W.S.","email":"","affiliations":[],"preferred":false,"id":817451,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70271732,"text":"70271732 - 1968 - Water resources of the Juana Díaz area, Puerto Rico: A preliminary appraisal, 1966","interactions":[],"lastModifiedDate":"2025-09-22T19:44:14.648707","indexId":"70271732","displayToPublicDate":"1968-01-01T11:01:49","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Water resources of the Juana Díaz area, Puerto Rico: A preliminary appraisal, 1966","docAbstract":"This report is an areal study of a portion of the south coast of Puerto Rico. It follows similar studies of the Guanica, Guayanilla-Yauco, Tallaboa Valley, and Ponce areas to the west and the Jobos area to the east. It basically is an inventory of the water resources during one year. To this extent it carries no long-term information; however, as rainfall data is available for 50 years or so at some sites within the study area, we can make a qualitative estimate of the water resources under more extreme conditions. The purpose of this report, then, is to evaluate the gross hydrologic features of the area for the future management of the water resources.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70271732","collaboration":"In cooperation with the Commonwealth of Puerto Rico","usgsCitation":"Giusti, E.V., 1968, Water resources of the Juana Díaz area, Puerto Rico: A preliminary appraisal, 1966, Report: 43 p.; 1 Figure: 17.12 x 19.29 inches, https://doi.org/10.3133/70271732.","productDescription":"Report: 43 p.; 1 Figure: 17.12 x 19.29 inches","costCenters":[],"links":[{"id":495866,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70271732/figure-29.pdf","text":"Figure 29","linkFileType":{"id":1,"text":"pdf"}},{"id":495865,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70271732/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":495864,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70271732/report-thumb.jpg"}],"country":"Puerto Rico","city":"Juana Díaz","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -67.41782863900221,\n 18.61812040597721\n ],\n [\n -67.41782863900221,\n 17.80333089063508\n ],\n [\n -65.56416750050371,\n 17.80333089063508\n ],\n [\n -65.56416750050371,\n 18.61812040597721\n ],\n [\n -67.41782863900221,\n 18.61812040597721\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Giusti, Ennio V.","contributorId":35301,"corporation":false,"usgs":true,"family":"Giusti","given":"Ennio","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":949218,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70171724,"text":"70171724 - 1968 - A preliminary report of a recently discovered aquifer at Sioux Falls, South Dakota","interactions":[],"lastModifiedDate":"2017-10-15T12:48:04","indexId":"70171724","displayToPublicDate":"1968-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5088,"text":"South Dakota Academy of Science Proceedings","active":true,"publicationSubtype":{"id":10}},"title":"A preliminary report of a recently discovered aquifer at Sioux Falls, South Dakota","docAbstract":"A hydrologic study of the Big Sioux aquifer system was begun July 1, 1966, by the U.S. Geological Survey, in cooperation with the City of Sioux Falls and the East Dakota Conservancy Sub-District.
\nTest drilling being done in the search for a southern outlet to the Big Sioux aquifer has led to the discovery of the outlet and of a deeper aquifer than was previously know to exist in this area. This aquifer, herein called the Sioux Falls aquifer, was first recognized as a very clean gravel in test hole USGS #1 between the depths of 60 to 83 feet.
\nSubsequent test drilling and aquifer testing has shown the Sioux Falls aquifer to be capable of producing several hundred gallons of water per minute. THe chemical quality of this water surpasses that currently being used for the city supply.
\nFurther investigation of the aquifer is planned as a part of the continuing expansion of the water-supply facilities for Sioux Falls.
\nThis publication has been authorized by the Director of the U.S. Geological Survey and Earl McCart, Commissioner, City of Sioux Falls, South Dakota.
","language":"English","publisher":"South Dakota Academy of Science","usgsCitation":"Vaughan, K.D., and Ackroyd, E.A., 1968, A preliminary report of a recently discovered aquifer at Sioux Falls, South Dakota: South Dakota Academy of Science Proceedings, v. 47, no. 16, p. 68-74.","productDescription":"7 p.","startPage":"68","endPage":"74","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":323991,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":322193,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.sdaos.org/publications/?wpa-paged=113"}],"country":"United States","state":"South Dakota","city":"Sioux Falls","volume":"47","issue":"16","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"576913aee4b07657d19fef86","contributors":{"authors":[{"text":"Vaughan, Kenneth D.","contributorId":170160,"corporation":false,"usgs":false,"family":"Vaughan","given":"Kenneth","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":632207,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ackroyd, Earl A.","contributorId":59425,"corporation":false,"usgs":true,"family":"Ackroyd","given":"Earl","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":632208,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70175606,"text":"70175606 - 1968 - Records of wells, water levels, and chemical quality of water in the lower Santiam River basin, middle Willamette Valley, Oregon","interactions":[],"lastModifiedDate":"2020-10-09T17:48:48.446583","indexId":"70175606","displayToPublicDate":"1968-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":115,"text":"Ground Water Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"13","title":"Records of wells, water levels, and chemical quality of water in the lower Santiam River basin, middle Willamette Valley, Oregon","docAbstract":"Basic water data on the lower Santiam River basin is preliminary to a comprehensive hydrologic study of this productive and intensely irrigated area where expanding population and industry increases the demand for water. Highest yielding wells are in shallow alluvial aquifers near the main streams; yields range from several hundred to more than a thousand gpm. Wells in lacustrine and older alluvial aquifers that underlie low, flat terraces have yields from a few tens to a few hundred gpm. Wells in the Salem Hills and in the Cascade Range foothills yield moderate to small quantities of water and tap a variety of geologic units. Tabulated material includes records of representative wells, drillers' logs, and chemical and spectrographic analyses of the ground water.
","language":"English","publisher":"State of Oregon","usgsCitation":"Helm, D.C., 1968, Records of wells, water levels, and chemical quality of water in the lower Santiam River basin, middle Willamette Valley, Oregon: Ground Water Report 13, ii, 186 p.","productDescription":"ii, 186 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":326677,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":379286,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.worldcat.org/title/records-of-wells-water-levels-and-chemical-quality-of-water-in-the-lower-santiam-river-basin-middle-willamette-valley-oregon/oclc/981926200&referer=brief_results"}],"country":"United States","state":"Oregon","otherGeospatial":"Willamette Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -123.28308105468749,\n 44.07574700247845\n ],\n [\n -122.420654296875,\n 44.07574700247845\n ],\n [\n -122.420654296875,\n 45.57944511437787\n ],\n [\n -123.28308105468749,\n 45.57944511437787\n ],\n [\n -123.28308105468749,\n 44.07574700247845\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58b58e4b03bcb0104bc61","contributors":{"authors":[{"text":"Helm, Donald C.","contributorId":49792,"corporation":false,"usgs":true,"family":"Helm","given":"Donald","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":645812,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":53414,"text":"ofr6867 - 1968 - Geology, hydrology, and quality of water in the Hanford-Visalia area, San Joaquin Valley, California","interactions":[],"lastModifiedDate":"2023-03-09T23:02:14.422878","indexId":"ofr6867","displayToPublicDate":"1968-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"68-67","title":"Geology, hydrology, and quality of water in the Hanford-Visalia area, San Joaquin Valley, California","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6867","usgsCitation":"Croft, M.G., and Gordon, G.V., 1968, Geology, hydrology, and quality of water in the Hanford-Visalia area, San Joaquin Valley, California: U.S. Geological Survey Open-File Report 68-67, Report: v, 63 p.; 15 Plates: 43.83 x 23.15 inches or smaller, https://doi.org/10.3133/ofr6867.","productDescription":"Report: v, 63 p.; 15 Plates: 43.83 x 23.15 inches or smaller","costCenters":[],"links":[{"id":413936,"rank":18,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52120.htm","linkFileType":{"id":5,"text":"html"}},{"id":87299,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1968/0067/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87298,"rank":17,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0067/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87297,"rank":16,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0067/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87296,"rank":15,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0067/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87295,"rank":14,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0067/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87294,"rank":13,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0067/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87293,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0067/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87292,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0067/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87291,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0067/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87290,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0067/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87289,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0067/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87288,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0067/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87287,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0067/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87286,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0067/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87285,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0067/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87284,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0067/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":175000,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1968/0067/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Hanford-Visalia area, San Joaquin Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -120,\n 36.5\n ],\n [\n -120,\n 36\n ],\n [\n -118.8167,\n 36\n ],\n [\n -118.8167,\n 36.5\n ],\n [\n -120,\n 36.5\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8ddb","contributors":{"authors":[{"text":"Croft, Mark G.","contributorId":24426,"corporation":false,"usgs":true,"family":"Croft","given":"Mark","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":247549,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gordon, G. V.","contributorId":30254,"corporation":false,"usgs":true,"family":"Gordon","given":"G.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":247550,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70190815,"text":"70190815 - 1968 - Hydrologic and climatologic data, 1967, Salt Lake County, Utah","interactions":[],"lastModifiedDate":"2018-03-26T15:42:53","indexId":"70190815","displayToPublicDate":"1968-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5498,"text":"Utah Basic-Data Release","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"15","title":"Hydrologic and climatologic data, 1967, Salt Lake County, Utah","docAbstract":"An investigation of the water resources of Salt Lake County, Utah, was undertaken by the Water Resources Division of the U.S. Geological Survey in July 1963. This investigation is a cooperative project financed chiefly by equal contributions of the State of Utah and the Federal Government in accordance with an agreement between the Division of Water Rights, Utah Department of Natural Resources, and the Geological Survey. The investigation was financed during the period covered by this report by the following organizations: Utah Division of Water Rights (formerly State Engineer), Utah Division of Water Resources (formerly Water and Power Board), Salt Lake County, Salt Lake County Water Conservancy District, Central Utah Water Conservancy District, Metropolitan Water District of Salt Lake City, City of Murray, Granger-Hunter Improvement District, Taylorsville-Bennion Improvement District, Holladay Water Company, Magna Water and Sewer District, U.S. Bureau of Reclamation, U.S. Geological Survey.
The investigation encompasses the collection and interpretation of a large variety of climatologic, hydrologic, and geologic data in and near Salt Lake County. Utah Basic-Data Releases 11-13 contain data collected through 1966. This release contains climatologic and surfacewater data for the 1967 water year (October 1966 to September 1967) and ground-water data collected during the 1967 calendar year. A similar annual release will contain data collected during the remainder of the investigation, and interpretive reports will be prepared as the investigation proceeds. Organizations that furnished data are acknowledged in station descriptions and footnotes to tables.
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