{"pageNumber":"639","pageRowStart":"15950","pageSize":"25","recordCount":16495,"records":[{"id":2511,"text":"wsp1768 - 1964 - Hydrology of the Babylon-Islip area, Suffolk County, Long Island, New York","interactions":[],"lastModifiedDate":"2023-03-14T20:23:08.28216","indexId":"wsp1768","displayToPublicDate":"1964-01-01T00:00:00","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":"1768","title":"Hydrology of the Babylon-Islip area, Suffolk County, Long Island, New York","docAbstract":"The report area comprises 270 square miles, and includes most of the Towns of Babylon and Islip, and parts of the Towns of Huntington, Smithtown, and Brookhaven, in southwestern Suffolk County, New York. \r\n\r\nAlmost all the water used in the area is obtained from wells screened in permeable zones of the ground-water reservoir which consists of unconsolidated deposits of gravel, sand, silt, and clay as much as 1,800 feet thick. The ground-water reservoir contains three principal aquifers. From the surface down these are (a) surficial deposits of sand and gravel of Pleistocene age, (b) sands of the Magothy (?) Formation of Cretaceous age, and (c) the Lloyd Sand Member of the Raritan Formation of Cretaceous age. At present only the upper two aquifers are tapped by wells. Natural replenishment of the ground-water reservoir in the area takes place entirely by infiltration of precipitation and averages about 215 mgd (million gallons per day). Average ground-water runoff to streams above tidewater is 114 mgd, and it is estimated that an additional 54 mgd is discharged into tidal reaches of streams. Ground-water evapotranspiration is computed to be about 10 mgd and submarine outflow from the area is estimated to be 18 mgd. The average streamflow of the area above tidewater is 120 mgd. Because of the permeable soils and low relief, direct runoff is only about 5 percent of the average streamflow. Streams are perennial along their middle and lower reaches and exhibit well-sustained low flows. Flooding rarely occurs although continued urbanization may result in minor flooding problems as additional storm sewers are constructed. \r\n\r\nWater in most of the area is generally of good quality; however, it may be contaminated locally. Some streams and parts of the water-table aquifer contain low concentrations of synthetic detergents and other dissolved constituents from domestic and industrial wastes. Salty water occurs in parts of the water-table aquifer in the area under and bordering Great South Bay and under the barrier beaches. Present information, however, indicates that submarine outflow in the artesian aquifers is sufficient to maintain the fresh water-salt water interface some distance seaward of the barrier beaches. \r\n\r\nGround-water withdrawals in 1960 averaged 39 mgd, most of which was returned to the ground through cesspools, leaching beds, and recharge wells; pumpage did not appreciably affect the natural water balance of the groundwater reservoir. If withdrawals continue to be artificially recharged, pumpage can be increased at least fivefold before consumptive losses materially reduce ground-water levels. However, if the area were completely sewered in the future, an adequate supply of ground water for a substantially increased population could not be obtained without (a) reducing the amount of ground water in storage in the reservoir or (b) recharging treated-sewage effluent.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1768","usgsCitation":"Pluhowski, E.J., and Kantrowitz, I.H., 1964, Hydrology of the Babylon-Islip area, Suffolk County, Long Island, New York: U.S. Geological Survey Water Supply Paper 1768, Report: v, 119 p.; 8 Plates: 30.00 x 32.00 inches or smaller, https://doi.org/10.3133/wsp1768.","productDescription":"Report: v, 119 p.; 8 Plates: 30.00 x 32.00 inches or smaller","costCenters":[],"links":[{"id":28672,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1768/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28671,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1768/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28670,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1768/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28669,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1768/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28668,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1768/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28667,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1768/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28666,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1768/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28665,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1768/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28664,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1768/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138711,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1768/report-thumb.jpg"},{"id":414130,"rank":11,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24946.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"New York","county":"Suffolk County","otherGeospatial":"Babylon-Islip area, Long Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -73.479,\n              40.883\n            ],\n            [\n              -73.479,\n              40.604\n            ],\n            [\n              -73,\n              40.604\n            ],\n            [\n              -73,\n              40.883\n            ],\n            [\n              -73.479,\n              40.883\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601ef4","contributors":{"authors":[{"text":"Pluhowski, Edward J.","contributorId":87911,"corporation":false,"usgs":true,"family":"Pluhowski","given":"Edward","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":145316,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kantrowitz, Irwin H.","contributorId":93472,"corporation":false,"usgs":true,"family":"Kantrowitz","given":"Irwin","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":145317,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2176,"text":"wsp1669D - 1964 - Hydrogeology of the Huntington-Smithtown area, Suffolk County, New York","interactions":[{"subject":{"id":2176,"text":"wsp1669D - 1964 - Hydrogeology of the Huntington-Smithtown area, Suffolk County, New York","indexId":"wsp1669D","publicationYear":"1964","noYear":false,"chapter":"D","title":"Hydrogeology of the Huntington-Smithtown area, Suffolk County, New York"},"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":"2023-03-14T19:20:43.937271","indexId":"wsp1669D","displayToPublicDate":"1964-01-01T00:00:00","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":"D","title":"Hydrogeology of the Huntington-Smithtown area, Suffolk County, New York","docAbstract":"<p>No abstract available.</p>","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","doi":"10.3133/wsp1669D","usgsCitation":"Lubke, E.R., 1964, Hydrogeology of the Huntington-Smithtown area, Suffolk County, New York: U.S. Geological Survey Water Supply Paper 1669, Report: iv, 68 p.; 6 Plates: 33.00 × 21.76 inches or smaller, https://doi.org/10.3133/wsp1669D.","productDescription":"Report: iv, 68 p.; 6 Plates: 33.00 × 21.76 inches or smaller","costCenters":[],"links":[{"id":27795,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669d/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27794,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669d/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27793,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669d/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27792,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669d/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27791,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669d/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27790,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27796,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1669d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":397417,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24864.htm"},{"id":138199,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1669d/report-thumb.jpg"}],"scale":"62500","country":"United States","state":"New York","county":"Suffolk County","city":"Huntington, Smithtown","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73.5,\n              40.75\n            ],\n            [\n              -73.125,\n              40.75\n            ],\n            [\n              -73.125,\n              40.95\n            ],\n            [\n              -73.5,\n              40.95\n            ],\n            [\n              -73.5,\n              40.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ee4b07f02db615138","contributors":{"authors":[{"text":"Lubke, E. Ronald","contributorId":73572,"corporation":false,"usgs":true,"family":"Lubke","given":"E.","email":"","middleInitial":"Ronald","affiliations":[],"preferred":false,"id":144774,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68480,"text":"ha112 - 1964 - Availability of ground water in the Lynn Grove quadrangle, Kentucky-Tennessee","interactions":[],"lastModifiedDate":"2023-03-01T22:50:13.724412","indexId":"ha112","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","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":"112","title":"Availability of ground water in the Lynn Grove quadrangle, Kentucky-Tennessee","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha112","usgsCitation":"Davis, R.W., 1964, Availability of ground water in the Lynn Grove quadrangle, Kentucky-Tennessee: U.S. Geological Survey Hydrologic Atlas 112, 1 Plate: 47.50 x 32.50 inches, https://doi.org/10.3133/ha112.","productDescription":"1 Plate: 47.50 x 32.50 inches","costCenters":[],"links":[{"id":188021,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":413586,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15468.htm","linkFileType":{"id":5,"text":"html"}},{"id":90033,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/112/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Kentucky, Tennessee","otherGeospatial":"Lynn Grove quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.5,\n              36.5\n            ],\n            [\n              -88.5,\n              36.625\n            ],\n            [\n              -88.375,\n              36.625\n            ],\n            [\n              -88.375,\n              36.5\n            ],\n            [\n              -88.5,\n              36.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d936","contributors":{"authors":[{"text":"Davis, R. W.","contributorId":93459,"corporation":false,"usgs":true,"family":"Davis","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":278301,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70190800,"text":"70190800 - 1964 - Selected hydrologic data, upper Sevier River basin, Utah","interactions":[],"lastModifiedDate":"2017-09-14T12:50:52","indexId":"70190800","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5497,"text":"Utah Basic-Data Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"8","title":"Selected hydrologic data, upper Sevier River basin, Utah","docAbstract":"<p>This report is intended to serve two purposes: (1) to make available to the public basic ground-water data useful in planning and studying development of water resources, and (2) to supplement an interpretive report that will be published later.</p><p>Records were collected during 1961-63 by the U.S. Geological Survey in cooperation with the Utah State Engineer as a part of the investigation of ground-water conditions in the upper Sevier River basin, in parts of Garfield, Iron, Kane, Piute, and Sevier Counties, Utah. The interpretive material will be published in a companion report by Carl H. Carpenter, Gerald B. Robinson, Jr., and Louis J. Bjorklund.</p><p>This report is most useful in predicting conditions likely to be found in areas that are being considered as well sites. The person considering the new well can spot the proposed site on plate 1 and examine the records of nearby wells and springs as shown in the tables. From table 1 he can find information on wells, including depth, diameter, water level, yield, drawdown, use of water, temperature of water, and depth of perforations. Table 2 gives information on springs such as yield, use of water, temperature, and improvements. From tables 1 and 2 he can note the type of material that yields water in the vicinity. Table 3 shows the historic fluctuations and trends of water levels. Table 4 shows the type of material penetrated by wells. From table 5 he can note the chemical quality of water from wells and springs, and from table 6, the chemical quality of surface water. If the reader decides from his examination that conditions are favorable, he can place an application to drill a well with the State Engineer. If the State Engineer believes unappropriated water is available, the application may be approved after minimum statutory requirements have been satisfied.</p><p>The report is also useful when planning large-scale developments of water supply. This and other uses of the report will be helped by use of the interpretive report upon its release.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the Utah State Engineer","usgsCitation":"Carpenter, C.H., Robinson, G.B., and Bjorklund, L.J., 1964, Selected hydrologic data, upper Sevier River basin, Utah: Utah Basic-Data Report 8, 29 p.","productDescription":"29 p.","numberOfPages":"37","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":345770,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":345769,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/docview.exe?Folder=TP21-1-160&Title=Basic+Data+Report+8"}],"country":"United States","state":"Utah","county":"Garfield County, Iron County, Kane County, Piute County, Sevier County","otherGeospatial":"Sevier River basi","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59bb953ae4b091459a578226","contributors":{"authors":[{"text":"Carpenter, Carl H.","contributorId":46074,"corporation":false,"usgs":true,"family":"Carpenter","given":"Carl","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":710428,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robinson, Gerald B. Jr.","contributorId":91837,"corporation":false,"usgs":true,"family":"Robinson","given":"Gerald","suffix":"Jr.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":710429,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bjorklund, Louis Jay","contributorId":21138,"corporation":false,"usgs":true,"family":"Bjorklund","given":"Louis","email":"","middleInitial":"Jay","affiliations":[],"preferred":false,"id":710430,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010816,"text":"70010816 - 1964 - Ground water in North America","interactions":[],"lastModifiedDate":"2017-03-27T12:47:37","indexId":"70010816","displayToPublicDate":"1964-01-01T00:00:00","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":"Ground water in North America","docAbstract":"The fast-growing demands on this natural resource expose a need to resolve many hydrologic unknowns.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.143.3610.1001","issn":"00368075","usgsCitation":"Thomas, H.E., and Leopold, L.B., 1964, Ground water in North America: Science, v. 143, no. 3610, p. 1001-1006, https://doi.org/10.1126/science.143.3610.1001.","productDescription":"6 p.","startPage":"1001","endPage":"1006","costCenters":[],"links":[{"id":218743,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"North America","volume":"143","issue":"3610","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2ad0e4b0c8380cd5b4a7","contributors":{"authors":[{"text":"Thomas, Harold E.","contributorId":36116,"corporation":false,"usgs":true,"family":"Thomas","given":"Harold","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":359714,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":359715,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68197,"text":"ha124 - 1964 - Availability of ground water in the Hazel quadrangle, Kentucky-Tennessee","interactions":[],"lastModifiedDate":"2023-03-01T22:41:05.489714","indexId":"ha124","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","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":"124","title":"Availability of ground water in the Hazel quadrangle, Kentucky-Tennessee","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha124","usgsCitation":"MacCary, L., 1964, Availability of ground water in the Hazel quadrangle, Kentucky-Tennessee: U.S. Geological Survey Hydrologic Atlas 124, 1 Plate: 47.50 x 34.00 inches, https://doi.org/10.3133/ha124.","productDescription":"1 Plate: 47.50 x 34.00 inches","costCenters":[],"links":[{"id":186117,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89542,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/124/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":413584,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15481.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","country":"United States","state":"Kentucky, Tennessee","otherGeospatial":"Hazel quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.375,\n              36.5\n            ],\n            [\n              -88.375,\n              36.625\n            ],\n            [\n              -88.25,\n              36.625\n            ],\n            [\n              -88.25,\n              36.5\n            ],\n            [\n              -88.375,\n              36.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d952","contributors":{"authors":[{"text":"MacCary, L.M.","contributorId":13200,"corporation":false,"usgs":true,"family":"MacCary","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":277827,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70179734,"text":"70179734 - 1963 - Dissolved-mineral inflow to Great Salt Lake and chemical characteristics of the salt lake brine. Part I: Selected hydrologic data","interactions":[],"lastModifiedDate":"2017-09-06T17:19:25","indexId":"70179734","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5485,"text":"Utah Geological and Mineralogical Survey Water-Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"3-I","title":"Dissolved-mineral inflow to Great Salt Lake and chemical characteristics of the salt lake brine. Part I: Selected hydrologic data","docAbstract":"<p>This report presents the data collected for a study of the dissolved-mineral load contributed by surficial sources to Great Salt Lake, Utah. The study was conducted by the U.S. Geological Survey in cooperation with the University of Utah during the period from July 1959 through June 1962, and is part of an overall investigation of the Great Salt Lake basin by the University. Financial support for the study was provided by the U.S. Geological Survey and by the University of Utah Research Fund and Uniform School Fund. Some of the data presented in this report were obtained as part of cooperative programs between the Geological Survey and other agencies.</p>","language":"English","publisher":"Utah Geological and Minerological Society","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with The College of Mines and Mineral Industries, University of Utah, Salt Lake City, Utah","usgsCitation":"Hahl, D.C., and Mitchell, C., 1963, Dissolved-mineral inflow to Great Salt Lake and chemical characteristics of the salt lake brine. Part I: Selected hydrologic data: Utah Geological and Mineralogical Survey Water-Resources Bulletin 3-I, 39 p.","productDescription":"39 p.","numberOfPages":"51","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":345533,"rank":3,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/70179736","text":"Part II: Technical report"},{"id":345532,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://ugspub.nr.utah.gov/publications/water_resources_bulletins/WRB-3part1.pdf"},{"id":333225,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Great Salt Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.2305908203125,\n              40.59727063442024\n            ],\n            [\n              -113.2305908203125,\n              41.795888098191426\n            ],\n            [\n              -111.81884765624999,\n              41.795888098191426\n            ],\n            [\n              -111.81884765624999,\n              40.59727063442024\n            ],\n            [\n              -113.2305908203125,\n              40.59727063442024\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5879f5ade4b0847d353f44d6","contributors":{"authors":[{"text":"Hahl, D. C.","contributorId":57436,"corporation":false,"usgs":true,"family":"Hahl","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":658473,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mitchell, C.G.","contributorId":177183,"corporation":false,"usgs":true,"family":"Mitchell","given":"C.G.","email":"","affiliations":[],"preferred":false,"id":658474,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":71791,"text":"tei840 - 1963 - A summary of the ground-water hydrology of the area between the Las Vegas Valley and the Amargosa Desert, Nevada, with special reference to the effects of possible new withdrawals of ground water","interactions":[],"lastModifiedDate":"2014-07-16T14:13:44","indexId":"tei840","displayToPublicDate":"2013-07-16T14:10:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"840","title":"A summary of the ground-water hydrology of the area between the Las Vegas Valley and the Amargosa Desert, Nevada, with special reference to the effects of possible new withdrawals of ground water","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/tei840","collaboration":"Prepared on behalf of the U.S. Atomic Energy Commission.","usgsCitation":"Winograd, I.J., 1963, A summary of the ground-water hydrology of the area between the Las Vegas Valley and the Amargosa Desert, Nevada, with special reference to the effects of possible new withdrawals of ground water: U.S. Geological Survey Trace Elements Investigations 840, Report: 79 p.; 1 Map, https://doi.org/10.3133/tei840.","productDescription":"Report: 79 p.; 1 Map","costCenters":[],"links":[{"id":290305,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Nevada","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.4011,36.2803 ], [ -116.4011,36.6184 ], [ -115.2713,36.6184 ], [ -115.2713,36.2803 ], [ -116.4011,36.2803 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c79ee2e4b0194841642416","contributors":{"authors":[{"text":"Winograd, Isaac Judah","contributorId":9233,"corporation":false,"usgs":true,"family":"Winograd","given":"Isaac","email":"","middleInitial":"Judah","affiliations":[],"preferred":false,"id":284759,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70047480,"text":"70047480 - 1963 - Hydrology of Brooklyn Lake near Keystone Heights, Florida","interactions":[{"subject":{"id":52309,"text":"ofr6316 - 1963 - Hydrology of Brooklyn Lake near Keystone Heights, Florida","indexId":"ofr6316","publicationYear":"1963","noYear":false,"title":"Hydrology of Brooklyn Lake near Keystone Heights, Florida"},"predicate":"SUPERSEDED_BY","object":{"id":70047480,"text":"70047480 - 1963 - Hydrology of Brooklyn Lake near Keystone Heights, Florida","indexId":"70047480","publicationYear":"1963","noYear":false,"title":"Hydrology of Brooklyn Lake near Keystone Heights, Florida"},"id":1}],"lastModifiedDate":"2017-09-13T17:55:27","indexId":"70047480","displayToPublicDate":"2013-01-01T13:24:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5489,"text":"Florida Geological Survey Report of Investigations","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"33","title":"Hydrology of Brooklyn Lake near Keystone Heights, Florida","docAbstract":"Brooklyn Lake receded about 20 feet during 1954-58 and reached its lowest stage of record (97.2 feet) in February 1958; this was the lowest stage in the memory of longtime residents. This unusually large recession was a result of deficient rainfall during more than a 3-year period, January 1954 to May 1957. However, by October 1959, after 2 1/2 years of above normal rainfall, the lake had recovered and water was flowing through the surface outlet.","language":"English","publisher":"Florida Geological Survey","publisherLocation":"Tallahassee, FL","collaboration":"Prepared by the United States Geological Survey in cooperation with the Florida Geological Survey","usgsCitation":"Clark, W.E., Musgrove, R.H., Menke, C.G., and Cagle, J.W., 1963, Hydrology of Brooklyn Lake near Keystone Heights, Florida: Florida Geological Survey Report of Investigations 33, viii, 43 p.","productDescription":"viii, 43 p.","costCenters":[],"links":[{"id":276166,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047480.PNG"},{"id":276162,"type":{"id":11,"text":"Document"},"url":"https://ufdc.ufl.edu/UF00001220/00001/pdf?search=report+%3dinvestigations"}],"country":"United States","state":"Florida","otherGeospatial":"Brooklyn Lake","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.16,29.71 ], [ -82.16,29.86 ], [ -81.95,29.86 ], [ -81.95,29.71 ], [ -82.16,29.71 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5203a37be4b02bdb1bc63fc4","contributors":{"authors":[{"text":"Clark, William E.","contributorId":105365,"corporation":false,"usgs":true,"family":"Clark","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":482149,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Musgrove, Rufus H.","contributorId":20245,"corporation":false,"usgs":true,"family":"Musgrove","given":"Rufus","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":482146,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Menke, Clarence G.","contributorId":25450,"corporation":false,"usgs":true,"family":"Menke","given":"Clarence","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":482147,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cagle, Joseph W. Jr.","contributorId":78640,"corporation":false,"usgs":true,"family":"Cagle","given":"Joseph","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":482148,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70039573,"text":"70039573 - 1963 - Use of hydrologic models in the analysis of flood runoff","interactions":[],"lastModifiedDate":"2012-08-14T01:01:44","indexId":"70039573","displayToPublicDate":"2012-01-01T16:11:06","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":371,"text":"Monograph","active":false,"publicationSubtype":{"id":6}},"title":"Use of hydrologic models in the analysis of flood runoff","docAbstract":"The analog technique is applied to the analysis of flood runoff. A quasi-linear analog model has been developed for simulating the runoff-producing characteristics of a drainage system. Where storage is linear a unique relationship correlating the inflow and outflow peaks is derived. The technique for synthesizing flood-frequency distribution is also discussed. It is found that a linear-basin system would not modify the type of probability distribution of its inflow, whereas a nonlinear-basin system would.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70039573","usgsCitation":"Shen, J., 1963, Use of hydrologic models in the analysis of flood runoff: Monograph, vii, 52 p.; ill., https://doi.org/10.3133/70039573.","productDescription":"vii, 52 p.; ill.","numberOfPages":"87","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":261089,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039573/report.pdf"},{"id":261090,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039573/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbf28e4b08c986b3299b9","contributors":{"authors":[{"text":"Shen, John","contributorId":34109,"corporation":false,"usgs":true,"family":"Shen","given":"John","email":"","affiliations":[],"preferred":false,"id":466498,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38988,"text":"pp434B - 1963 - Autocorrelation of rainfall and streamflow minimums","interactions":[],"lastModifiedDate":"2012-02-02T00:10:14","indexId":"pp434B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"434","chapter":"B","title":"Autocorrelation of rainfall and streamflow minimums","docAbstract":"Hydrologic time series of annual minimum mean monthly rainfall and annual minimum 1-day and 7-day discharge, considered as drought indices, were used to study the distribution of droughts with respect to time. The rainfall data were found to be nearly random. The discharge data, however, were found to be nonrandomly distributed in time and generated by a first-order Markov process. The expected value of the variance for a time series generated by a first-order Markov process was compared with the expected value of the variance for a random time series. This comparison showed that the expected value of the variance for a nonrandom time series converged to the population variance with an increase in sample size at a slower rate than for a random time series.","language":"ENGLISH","doi":"10.3133/pp434B","usgsCitation":"Matalas, N., 1963, Autocorrelation of rainfall and streamflow minimums: U.S. Geological Survey Professional Paper 434, p. B1-B10, https://doi.org/10.3133/pp434B.","productDescription":"p. B1-B10","costCenters":[],"links":[{"id":124618,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0434b/report-thumb.jpg"},{"id":66094,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0434b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667811","contributors":{"authors":[{"text":"Matalas, N.C.","contributorId":25173,"corporation":false,"usgs":true,"family":"Matalas","given":"N.C.","affiliations":[],"preferred":false,"id":220773,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":35360,"text":"b1133C - 1963 - Geology and hydrology of the Elk River, Minnesota, nuclear-reactor site","interactions":[],"lastModifiedDate":"2018-03-19T10:38:39","indexId":"b1133C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1133","chapter":"C","title":"Geology and hydrology of the Elk River, Minnesota, nuclear-reactor site","docAbstract":"<p>The Elk River, Minn., nuclear-reactor site is on the east bluff of the Mississippi River about 35 miles northwest of Minneapolis and St. Paul. The area is underlain by about 70 to 180 feet of glacial drift, including at the top as much as 120 feet of outwash deposits (valley train) of the glacial Mississippi River. The underlying Cambrian bedrock consists of marine sedimentary formations including artesian sandstone aquifers. A hypothetically spilled liquid at the reactor site could follow one or both of two courses, thus: (1) It could flow over the land surface and through an artificial drainage system to the river in a matter of minutes; (2) part or nearly all of it could seep downward to the water table and then move laterally to the river. The time required might range from a few weeks to a year, or perhaps more. The St. Paul and Minneapolis water-supply intakes, 21 and 25 miles downstream, respectively, are the most critical points to be considered in the event of an accidental spill. Based on streamflow and velocity data for the Mississippi River near Anoka, the time required for the maximum concentration of a contaminant to travel from the reactor site to the St. Paul intake was computed to be about 8 hours, at the median annual maximum daily discharge. For this discharge, the maximum concentration at the intake would be about 0.0026 microcurie per cubic foot for the release of 1 curie of activity into the river near the reactor site.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/b1133C","collaboration":"Prepared in cooperation with the U.S. Atomic Energy Commission","usgsCitation":"Norvitch, R.F., Schneider, R., and Godfrey, R.G., 1963, Geology and hydrology of the Elk River, Minnesota, nuclear-reactor site: U.S. Geological Survey Bulletin 1133, Document: iv, 25 p.; 2 Plates: 18 x 16 inches, https://doi.org/10.3133/b1133C.","productDescription":"Document: iv, 25 p.; 2 Plates: 18 x 16 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":63222,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1133c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63223,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1133c/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63224,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1133c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":109385,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20849.htm","linkFileType":{"id":5,"text":"html"},"description":"20849"},{"id":165594,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1133c/report-thumb.jpg"}],"country":"United States","state":"Minnesota","city":"Elk River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -93.61209869384766,\n              45.261596972270866\n            ],\n            [\n              -93.61209869384766,\n              45.3297027614069\n            ],\n            [\n              -93.51133346557617,\n              45.3297027614069\n            ],\n            [\n              -93.51133346557617,\n              45.261596972270866\n            ],\n            [\n              -93.61209869384766,\n              45.261596972270866\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b468c","contributors":{"authors":[{"text":"Norvitch, Ralph F.","contributorId":65456,"corporation":false,"usgs":true,"family":"Norvitch","given":"Ralph","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":214511,"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":214513,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Godfrey, Richard G.","contributorId":100046,"corporation":false,"usgs":true,"family":"Godfrey","given":"Richard","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":214512,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":52309,"text":"ofr6316 - 1963 - Hydrology of Brooklyn Lake near Keystone Heights, Florida","interactions":[{"subject":{"id":52309,"text":"ofr6316 - 1963 - Hydrology of Brooklyn Lake near Keystone Heights, Florida","indexId":"ofr6316","publicationYear":"1963","noYear":false,"title":"Hydrology of Brooklyn Lake near Keystone Heights, Florida"},"predicate":"SUPERSEDED_BY","object":{"id":70047480,"text":"70047480 - 1963 - Hydrology of Brooklyn Lake near Keystone Heights, Florida","indexId":"70047480","publicationYear":"1963","noYear":false,"title":"Hydrology of Brooklyn Lake near Keystone Heights, Florida"},"id":1}],"supersededBy":{"id":70047480,"text":"70047480 - 1963 - Hydrology of Brooklyn Lake near Keystone Heights, Florida","indexId":"70047480","publicationYear":"1963","noYear":false,"title":"Hydrology of Brooklyn Lake near Keystone Heights, Florida"},"lastModifiedDate":"2013-08-07T13:22:36","indexId":"ofr6316","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"63-16","title":"Hydrology of Brooklyn Lake near Keystone Heights, Florida","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr6316","usgsCitation":"Clark, W., Musgrove, R., Menke, C., and Cagle, J., 1963, Hydrology of Brooklyn Lake near Keystone Heights, Florida: U.S. Geological Survey Open-File Report 63-16, 49 p., https://doi.org/10.3133/ofr6316.","productDescription":"49 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":177942,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604abb","contributors":{"authors":[{"text":"Clark, W.E.","contributorId":68694,"corporation":false,"usgs":true,"family":"Clark","given":"W.E.","email":"","affiliations":[],"preferred":false,"id":245122,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Musgrove, R.H.","contributorId":31051,"corporation":false,"usgs":true,"family":"Musgrove","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":245120,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Menke, C.G.","contributorId":20823,"corporation":false,"usgs":true,"family":"Menke","given":"C.G.","affiliations":[],"preferred":false,"id":245119,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cagle, J.W. Jr.","contributorId":63875,"corporation":false,"usgs":true,"family":"Cagle","given":"J.W.","suffix":"Jr.","affiliations":[],"preferred":false,"id":245121,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":71786,"text":"tei833 - 1963 - Regional Hydrology of a Part of Southern Nevada: A Reconnaissance","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"tei833","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"833","title":"Regional Hydrology of a Part of Southern Nevada: A Reconnaissance","language":"ENGLISH","doi":"10.3133/tei833","usgsCitation":"Eakin, T.E., Schoff, S.L., and Cohen, P.M., 1963, Regional Hydrology of a Part of Southern Nevada: A Reconnaissance: U.S. Geological Survey Trace Elements Investigations 833, 40 leaves : maps ; 27 cm.; Three folded maps in pocket, https://doi.org/10.3133/tei833.","productDescription":"40 leaves : maps ; 27 cm.; Three folded maps in pocket","costCenters":[],"links":[{"id":186151,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db6350f6","contributors":{"authors":[{"text":"Eakin, Thomas Emery","contributorId":49863,"corporation":false,"usgs":true,"family":"Eakin","given":"Thomas","email":"","middleInitial":"Emery","affiliations":[],"preferred":false,"id":284751,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schoff, Stuart Leeson","contributorId":57951,"corporation":false,"usgs":true,"family":"Schoff","given":"Stuart","email":"","middleInitial":"Leeson","affiliations":[],"preferred":false,"id":284752,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cohen, Philip M.","contributorId":67860,"corporation":false,"usgs":true,"family":"Cohen","given":"Philip","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":284753,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":52370,"text":"ofr63132 - 1963 - Geology and ground-water features of salt springs, seeps, and plains in the Arkansas and Red River basins of western Oklahoma and adjacent parts of Kansas and Texas","interactions":[],"lastModifiedDate":"2022-12-02T22:44:49.57593","indexId":"ofr63132","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"63-132","title":"Geology and ground-water features of salt springs, seeps, and plains in the Arkansas and Red River basins of western Oklahoma and adjacent parts of Kansas and Texas","docAbstract":"<p>The salt springs, seeps, and plains described in this report are in the Arkansas and Red River basins in western Oklahoma and adjacent areas in Kansas and Texas. The springs and seeps contribute significantly to the generally poor water quality of the rivers by bringing salt (NaCl) to the surface at an estimated daily rate of more than 8,000 tons. The region investigated is characterized by low hills and rolling plains. Many of the rivers are eroded 100 feet or more below the .surrounding upland surface and in places the valleys are bordered by steep bluffs. The alluvial plains of the major rivers are wide and the river channels are shallow and unstable. The flow of many surface streams is intermittent, especially in the western part of the area. All the natural salt-contributing areas studied are within the outcrop area of rocks of Permian age. The Permian rocks, commonly termed red beds, are composed principally of red and gray gypsiferous shale, siltstone, sandstone, gypsum, anhydrite, and dolomite. Many of the formations contain halite in the subsurface. The halite occurs mostly as discontinuous lenses in shale, although some of the thicker, more massive beds are extensive. It underlies the entire region studied at depths ranging from about 30 feet to more than 2,000 feet. The salt and associated strata show evidence of extensive removal of salt through solution by ground water. Although the salt generally occurs in relatively impervious shale small joints and fractures ,allow the passage of small quantities of water which dissolves the salt. Salt water occurs in the report area at depths ranging from less than 100 feet to more than 1,000 feet. Salt water occurs both as meteoric and connate, but the water emerging as salt springs is meteoric. Tritium analyses show that the age of the water from several springs is less than 20 years. The salt springs, seeps, and plains are confined to 13 local areas. The flow of the springs and seeps is small, but the chloride concentration in the water ranges from a few hundred parts per million to about 190,000 ppm. The wide range of concentration is believed to be due, in part, to differential dilution by fresh water. Alluvium in the vicinity of the salt springs remains saturated with salt water and evaporation from the alluvial surface causes the formation of a salt crust during dry weather. Those areas appear as salt plains that range in size from less than an acre to as much as 60 square miles. The rocks exposed at the surface in the vicinity of the salt springs are permeable enough to allow the infiltration of some precipitation. Under certain geologic and hydrologic conditions ground water percolates down and through salt-bearing rocks where it dissolves the salt. Hydrostatic pressure of ground water at higher elevations forces the salt water to emerge as salt springs at lower elevations.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr63132","usgsCitation":"Ward, P., 1963, Geology and ground-water features of salt springs, seeps, and plains in the Arkansas and Red River basins of western Oklahoma and adjacent parts of Kansas and Texas: U.S. Geological Survey Open-File Report 63-132, Report: 94 p., 7 Plates: 39.49 × 62.40 inches or smaller, https://doi.org/10.3133/ofr63132.","productDescription":"Report: 94 p., 7 Plates: 39.49 × 62.40 inches or smaller","costCenters":[],"links":[{"id":410029,"rank":10,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_54580.htm","linkFileType":{"id":5,"text":"html"}},{"id":86849,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1963/0132/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86848,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1963/0132/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86847,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1963/0132/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86846,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1963/0132/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86845,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1963/0132/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86844,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1963/0132/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86843,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1963/0132/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86842,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1963/0132/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":177602,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1963/0132/report-thumb.jpg"}],"country":"United States","state":"Kansas, Oklahoma, Texas","otherGeospatial":"Arkansas and Red River basins","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -100.5,\n              38.333\n            ],\n            [\n              -100.5,\n              33.5\n            ],\n            [\n              -98,\n              33.5\n            ],\n            [\n              -98,\n              38.333\n            ],\n            [\n              -100.5,\n              38.333\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685f64","contributors":{"authors":[{"text":"Ward, P.E.","contributorId":40267,"corporation":false,"usgs":true,"family":"Ward","given":"P.E.","email":"","affiliations":[],"preferred":false,"id":245230,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68249,"text":"ha35 - 1963 - Availability of ground water in Adair, Casey, Clinton, Cumberland, Pulaski, Russell, Taylor, and Wayne Counties, Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:13:21","indexId":"ha35","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"35","title":"Availability of ground water in Adair, Casey, Clinton, Cumberland, Pulaski, Russell, Taylor, and Wayne Counties, Kentucky","language":"ENGLISH","doi":"10.3133/ha35","usgsCitation":"Lambert, T.W., and Brown, R., 1963, Availability of ground water in Adair, Casey, Clinton, Cumberland, Pulaski, Russell, Taylor, and Wayne Counties, Kentucky: U.S. Geological Survey Hydrologic Atlas 35, 3 col. maps ;56 x 58 cm. (Two maps, scale 1:250,000, and generalized columnar section.  Sheet 1, 22 by 23 inches; sheet 2, 23 by 32 inches; sheet 3, 22 by 28 inches), https://doi.org/10.3133/ha35.","productDescription":"3 col. maps ;56 x 58 cm. (Two maps, scale 1:250,000, and generalized columnar section.  Sheet 1, 22 by 23 inches; sheet 2, 23 by 32 inches; sheet 3, 22 by 28 inches)","costCenters":[],"links":[{"id":189675,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89630,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/035/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89631,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/035/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89632,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/035/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667d25","contributors":{"authors":[{"text":"Lambert, T. William","contributorId":40574,"corporation":false,"usgs":true,"family":"Lambert","given":"T.","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":277906,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, Richmond F.","contributorId":40577,"corporation":false,"usgs":true,"family":"Brown","given":"Richmond F.","affiliations":[],"preferred":false,"id":277907,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68250,"text":"ha34 - 1963 - Availability of ground water in Caldwell, Christian, Crittenden, Livingston, Lyon, Todd, and Trigg Counties, Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:13:21","indexId":"ha34","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"34","title":"Availability of ground water in Caldwell, Christian, Crittenden, Livingston, Lyon, Todd, and Trigg Counties, Kentucky","language":"ENGLISH","doi":"10.3133/ha34","usgsCitation":"Lambert, T.W., and Brown, R., 1963, Availability of ground water in Caldwell, Christian, Crittenden, Livingston, Lyon, Todd, and Trigg Counties, Kentucky: U.S. Geological Survey Hydrologic Atlas 34, 3 col. maps ;56 x 63 cm.  (Two maps, scale 1:250,000, and generalized columnar section.  Sheet 1, 22 by 25 inches; sheet 2, 22 by 36 inches; sheet 3, 22 by 28 inches), https://doi.org/10.3133/ha34.","productDescription":"3 col. maps ;56 x 63 cm.  (Two maps, scale 1:250,000, and generalized columnar section.  Sheet 1, 22 by 25 inches; sheet 2, 22 by 36 inches; sheet 3, 22 by 28 inches)","costCenters":[],"links":[{"id":189676,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89633,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/034/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89634,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/034/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89635,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/034/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db6672c6","contributors":{"authors":[{"text":"Lambert, T. William","contributorId":40574,"corporation":false,"usgs":true,"family":"Lambert","given":"T.","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":277908,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, Richmond F.","contributorId":40577,"corporation":false,"usgs":true,"family":"Brown","given":"Richmond F.","affiliations":[],"preferred":false,"id":277909,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":52357,"text":"ofr63104 - 1963 - Reconnaissance geology and hydrology on the Nett Lake Indian Reservation, Minnesota","interactions":[],"lastModifiedDate":"2018-03-19T10:37:01","indexId":"ofr63104","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"63-104","title":"Reconnaissance geology and hydrology on the Nett Lake Indian Reservation, Minnesota","docAbstract":"The Nett Lake Indian Reservation is in northern Minnesota, about 210 miles north of Minneapolis and St. Paul. The village of Nett Lake (population about 300) is the only community on the reservation. This report is the result of an investigation made to provide a central water source for the village, at the request of the Public Health Service of the U.S. Department of Health, Education, and Welfare.\r\n\r\nThe climate of the area is continental, characterized by cool, subhumid summers and long, severe winters. The average annual precipitation is 24.2 inches.\r\n\r\nAltitudes in the area range from about 1,190 feet above mean sea level in the Little Fork River channel on the west border of the reservation to about 1,550 feet on top of the Vermilion end moraine, just south of Nett Lake. During the latter part of the Pleistocene Epoch most of the area was inundated by the waters of glacial Lake Agassiz. The area is now drained by the Little Fork River which flows north into the Rainy River, thence into Lake of the Woods, and eventually into Hudson Bay.\r\n\r\nThe geologic units in the Nett Lake area consist of unconsolidated deposits of Recent and Pleistocene age and crystalline rocks of Precambrian age.\r\n\r\nMost ground water in the Nett Lake area occurs in three different zones: 1) surficial sand and gravel deposits, 2) lake sand underlying compact lake clay, and 3) bedrock fractures. The lake sand underlying the compact clay is the best source of ground water for the village of Nett Lake. It occurs in a small channel immediately west of the village, and it ranges in depth from about 11 to 30 feet below land surface and in thickness from 0 to about 3 feet. The water level is near the surface. A test well yielded 30 gpm (gallons per minute). Two 15 gpm wells would not exceed the long-term yield of the aquifer and would be adequate for the needs of the village.","language":"ENGLISH","doi":"10.3133/ofr63104","usgsCitation":"Norvitch, R., 1963, Reconnaissance geology and hydrology on the Nett Lake Indian Reservation, Minnesota: U.S. Geological Survey Open-File Report 63-104, 36 p., https://doi.org/10.3133/ofr63104.","productDescription":"36 p.","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":86836,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1963/0104/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86837,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1963/0104/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86838,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1963/0104/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":178071,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1963/0104/report-thumb.jpg"},{"id":86839,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1963/0104/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86840,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1963/0104/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86841,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1963/0104/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db64859c","contributors":{"authors":[{"text":"Norvitch, R.F.","contributorId":107742,"corporation":false,"usgs":true,"family":"Norvitch","given":"R.F.","email":"","affiliations":[],"preferred":false,"id":245209,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52352,"text":"ofr6397 - 1963 - Geology and hydrology of the carbonate rocks of the Lebanon Valley, Pennsylvania","interactions":[{"subject":{"id":52352,"text":"ofr6397 - 1963 - Geology and hydrology of the carbonate rocks of the Lebanon Valley, Pennsylvania","indexId":"ofr6397","publicationYear":"1963","noYear":false,"title":"Geology and hydrology of the carbonate rocks of the Lebanon Valley, Pennsylvania"},"predicate":"SUPERSEDED_BY","object":{"id":70047455,"text":"70047455 - 1963 - Hydrogeology of the carbonate rocks of the Lebanon Valley, Pennsylvania","indexId":"70047455","publicationYear":"1963","noYear":false,"title":"Hydrogeology of the carbonate rocks of the Lebanon Valley, Pennsylvania"},"id":1}],"supersededBy":{"id":70047455,"text":"70047455 - 1963 - Hydrogeology of the carbonate rocks of the Lebanon Valley, Pennsylvania","indexId":"70047455","publicationYear":"1963","noYear":false,"title":"Hydrogeology of the carbonate rocks of the Lebanon Valley, Pennsylvania"},"lastModifiedDate":"2013-08-06T13:43:30","indexId":"ofr6397","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"63-97","title":"Geology and hydrology of the carbonate rocks of the Lebanon Valley, Pennsylvania","language":"ENGLISH","doi":"10.3133/ofr6397","usgsCitation":"Meisler, H., 1963, Geology and hydrology of the carbonate rocks of the Lebanon Valley, Pennsylvania: U.S. Geological Survey Open-File Report 63-97, 122 p., https://doi.org/10.3133/ofr6397.","productDescription":"122 p.","costCenters":[],"links":[{"id":179012,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4692","contributors":{"authors":[{"text":"Meisler, Harold","contributorId":34103,"corporation":false,"usgs":true,"family":"Meisler","given":"Harold","email":"","affiliations":[],"preferred":false,"id":245200,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52321,"text":"ofr6330 - 1963 - Regional hydrology of a part of southern Nevada - a reconnaissance","interactions":[],"lastModifiedDate":"2012-02-02T00:11:33","indexId":"ofr6330","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"63-30","title":"Regional hydrology of a part of southern Nevada - a reconnaissance","language":"ENGLISH","doi":"10.3133/ofr6330","usgsCitation":"Eakin, T., Schoff, S., and Cohen, P., 1963, Regional hydrology of a part of southern Nevada - a reconnaissance: U.S. Geological Survey Open-File Report 63-30, 40 p., https://doi.org/10.3133/ofr6330.","productDescription":"40 p.","costCenters":[],"links":[{"id":177516,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c4d6","contributors":{"authors":[{"text":"Eakin, T.E.","contributorId":101727,"corporation":false,"usgs":true,"family":"Eakin","given":"T.E.","email":"","affiliations":[],"preferred":false,"id":245159,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schoff, S.L.","contributorId":107365,"corporation":false,"usgs":true,"family":"Schoff","given":"S.L.","email":"","affiliations":[],"preferred":false,"id":245160,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cohen, Philip","contributorId":61576,"corporation":false,"usgs":true,"family":"Cohen","given":"Philip","affiliations":[],"preferred":false,"id":245158,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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