{"pageNumber":"2572","pageRowStart":"64275","pageSize":"25","recordCount":68807,"records":[{"id":2355,"text":"wsp1619CC - 1963 - Ground water in the Raft River Basin, Idaho, with special reference to irrigation use, 1956-60","interactions":[],"lastModifiedDate":"2013-11-26T14:46:59","indexId":"wsp1619CC","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"1619","chapter":"CC","title":"Ground water in the Raft River Basin, Idaho, with special reference to irrigation use, 1956-60","docAbstract":"

In the Raft River basin in south-central Idaho, ground-water withdrawals \nfor irrigation have more than doubled since 1955, when data were compiled \nfor a comprehensive report on the area. The present report summerizes data \non the ground-water use and changes in the water regimen during the intervening \n5 years. Water levels have declined 10 to 20 feet in the areas of heaviest pumping \nand 3 to 5 feet throughout the remainder of the area. These water-level declines \nare related to increased ground-water pumpage and below-normal precipitation \nin the basin. The total pumpage during the 1960 irrigation season is estimated \nto be about 127,000 acre-feet, of which about half was consumed by crops or \nevaporated. The remainder returned to the aquifer.

\n
\n

Irrigation development is acting to reduce the amount of underflow out of the \nbasin. The water table can be lowered considerably more before underflow from \nthe basin would be reduced substantially.

","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1619CC","usgsCitation":"Mundorff, M.J., and Sisco, H., 1963, Ground water in the Raft River Basin, Idaho, with special reference to irrigation use, 1956-60: U.S. Geological Survey Water Supply Paper 1619, iii, 23 p., https://doi.org/10.3133/wsp1619CC.","productDescription":"iii, 23 p.","numberOfPages":"29","temporalStart":"1956-01-01","temporalEnd":"1960-12-31","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":137783,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1619cc/report-thumb.jpg"},{"id":28284,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619cc/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28285,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1619cc/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"125000","country":"United States","state":"Idaho","otherGeospatial":"Raft River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -113.6014,41.9942 ], [ -113.6014,42.6996 ], [ -113.1303,42.6996 ], [ -113.1303,41.9942 ], [ -113.6014,41.9942 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d9b8","contributors":{"authors":[{"text":"Mundorff, Maurice John","contributorId":41404,"corporation":false,"usgs":true,"family":"Mundorff","given":"Maurice","email":"","middleInitial":"John","affiliations":[],"preferred":false,"id":145070,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sisco, H.G.","contributorId":54185,"corporation":false,"usgs":true,"family":"Sisco","given":"H.G.","email":"","affiliations":[],"preferred":false,"id":145071,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":3045,"text":"wsp1619L - 1963 - Ground water in the alluvium of Kings River Valley, Humboldt County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:05:41","indexId":"wsp1619L","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"1619","chapter":"L","title":"Ground water in the alluvium of Kings River Valley, Humboldt County, Nevada","language":"ENGLISH","publisher":"U.S. Government Printing Office,","doi":"10.3133/wsp1619L","usgsCitation":"Zones, C., 1963, Ground water in the alluvium of Kings River Valley, Humboldt County, Nevada: U.S. Geological Survey Water Supply Paper 1619, iv, 38 p. :ill., maps ;23 cm., https://doi.org/10.3133/wsp1619L.","productDescription":"iv, 38 p. :ill., maps ;23 cm.","costCenters":[],"links":[{"id":139286,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1619l/report-thumb.jpg"},{"id":29897,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619l/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29898,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1619l/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d7a1","contributors":{"authors":[{"text":"Zones, C.P.","contributorId":70750,"corporation":false,"usgs":true,"family":"Zones","given":"C.P.","affiliations":[],"preferred":false,"id":146203,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2525,"text":"wsp1669T - 1963 - Reconnaissance of ground-water conditions in Maine","interactions":[],"lastModifiedDate":"2012-02-02T00:05:27","indexId":"wsp1669T","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"T","title":"Reconnaissance of ground-water conditions in Maine","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1962","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1669T","usgsCitation":"Prescott, G., 1963, Reconnaissance of ground-water conditions in Maine: U.S. Geological Survey Water Supply Paper 1669, iv, 52 p. :ill., maps ;23 cm., https://doi.org/10.3133/wsp1669T.","productDescription":"iv, 52 p. :ill., maps ;23 cm.","costCenters":[],"links":[{"id":138718,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1669t/report-thumb.jpg"},{"id":28745,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669t/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28746,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1669t/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ce4b07f02db63e812","contributors":{"authors":[{"text":"Prescott, Glenn C.","contributorId":38126,"corporation":false,"usgs":true,"family":"Prescott","given":"Glenn C.","affiliations":[],"preferred":false,"id":145346,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3199,"text":"wsp1544D - 1963 - Application of electrical and radioactive well logging to ground-water hydrology","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"wsp1544D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"1544","chapter":"D","title":"Application of electrical and radioactive well logging to ground-water hydrology","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1544D","usgsCitation":"Patten, E.P., and Bennett, G.D., 1963, Application of electrical and radioactive well logging to ground-water hydrology: U.S. Geological Survey Water Supply Paper 1544, v. :ill. ;23 cm. ;60 p., https://doi.org/10.3133/wsp1544D.","productDescription":"v. :ill. ;23 cm. ;60 p.","costCenters":[],"links":[{"id":138323,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1544d/report-thumb.jpg"},{"id":30186,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1544d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67aa3c","contributors":{"authors":[{"text":"Patten, Eugene P. Jr.","contributorId":59777,"corporation":false,"usgs":true,"family":"Patten","given":"Eugene","suffix":"Jr.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":146421,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bennett, Gordon D.","contributorId":18740,"corporation":false,"usgs":true,"family":"Bennett","given":"Gordon","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":146420,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70106991,"text":"70106991 - 1963 - Surface water records of Indiana, 1963","interactions":[],"lastModifiedDate":"2014-06-02T06:01:42","indexId":"70106991","displayToPublicDate":"1964-01-01T13:43:33","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Surface water records of Indiana, 1963","docAbstract":"

The surface-water records for the 1963 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of Indiana are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering States. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey, under the direction of Malcolm D. Hale, district engineer, Surface Water Branch.

\n
\n

This report marks the beginning of a new method of presenting, annually, basic data on surface-water records by States. Through September 30, 1960, the records of discharge and stage of streams and contents and stage of lakes or reservoirs were published in an annual series of U.S. Geological Survey water-supply papers entitled \"Surface Water Supply of the United States.\" Since 1951 there have been 20 volumes in the series; each volume covered an area whose boundaries coincided with those of certain natural drainage areas. The records in Indiana were contained in Parts 3A, 4 and 5 of that series.

\n
\n

Beginning with the 1961 water year, streamflow records and related data will be released by the Geological Survey in annual reports on a State-boundary basis. Distribution of these basic-data reports will be limited and primarily for local needs. The records later will be published in Geological Survey water-supply papers at 5-year intervals. These 5-year water-supply papers will show daily discharge and will be compiled on the same geographical areas previously used for the annual series; however, some of the 14 parts of coterminous United States will be further subdivided.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/70106991","collaboration":"Prepared in cooperation with Indiana Flood Control and Water Resources Commission; State Department of Conservation, Division of Water Resources; State Highway Commission; State Board of Health; Corps of Engineers, U.S. Army","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1963, Surface water records of Indiana, 1963, vii, 194 p., https://doi.org/10.3133/70106991.","productDescription":"vii, 194 p.","numberOfPages":"204","temporalStart":"1962-10-01","temporalEnd":"1963-09-30","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":287924,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":287923,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70106991/report.pdf"}],"country":"United States","state":"Indiana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.0979,37.7717 ], [ -88.0979,41.7607 ], [ -84.7847,41.7607 ], [ -84.7847,37.7717 ], [ -88.0979,37.7717 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"537b2808e4b0929ba496abc2","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535653,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010836,"text":"70010836 - 1963 - Tritium distribution in ground water around large underground fusion explosions","interactions":[],"lastModifiedDate":"2026-02-13T16:54:23.910977","indexId":"70010836","displayToPublicDate":"1963-11-29T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Tritium distribution in ground water around large underground fusion explosions","docAbstract":"Tritium will be released in significant amounts from large underground nuclear fusion explosions in the Plowshare Program. The tritium could become highly concentrated in nearby ground waters, and could be of equal or more importance as a possible contaminant than other long-lived fission-product and induced radionuclides. Behavior of tritiated water in particular hydrologic and geologic environments, as illustrated by hypothetical explosions in dolomite and tuff, must be carefully evaluated to predict under what conditions high groundwater concentrations of tritium might occur.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.142.3596.1163","issn":"00368075","usgsCitation":"Stead, F., 1963, Tritium distribution in ground water around large underground fusion explosions: Science, v. 142, no. 3596, p. 1163-1165, https://doi.org/10.1126/science.142.3596.1163.","productDescription":"3 p.","startPage":"1163","endPage":"1165","costCenters":[],"links":[{"id":218957,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"142","issue":"3596","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb86ce4b08c986b327852","contributors":{"authors":[{"text":"Stead, F.W.","contributorId":42653,"corporation":false,"usgs":true,"family":"Stead","given":"F.W.","email":"","affiliations":[],"preferred":false,"id":359759,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221091,"text":"70221091 - 1963 - Water-level trends in key observation well May-July 1963 (Abstracted from U. S. Geological Survey “Water Resources Review”)","interactions":[],"lastModifiedDate":"2021-06-01T19:30:58.880533","indexId":"70221091","displayToPublicDate":"1963-10-01T14:28:07","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Water-level trends in key observation well May-July 1963 (Abstracted from U. S. Geological Survey “Water Resources Review”)","docAbstract":"

No abstract available. 

","language":"English","publisher":"NGWA The Groundwater Association","doi":"10.1111/j.1745-6584.1963.tb01934.x","usgsCitation":"West, S.W., 1963, Water-level trends in key observation well May-July 1963 (Abstracted from U. S. Geological Survey “Water Resources Review”): Groundwater, v. 1, no. 4, p. 50-50, https://doi.org/10.1111/j.1745-6584.1963.tb01934.x.","productDescription":"1 p.","startPage":"50","endPage":"50","costCenters":[],"links":[{"id":386070,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"4","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"West, S. W.","contributorId":104029,"corporation":false,"usgs":true,"family":"West","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":816726,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221090,"text":"70221090 - 1963 - Television — A new tool for the ground‐water geologist","interactions":[],"lastModifiedDate":"2021-06-01T19:26:42.462439","indexId":"70221090","displayToPublicDate":"1963-10-01T14:22:28","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Television — A new tool for the ground‐water geologist","docAbstract":"

The television camera has become a tool of the ground‐water geologist, enabling him to examine visually the inside of a well deep below the land surface. Using the camera, the rocks can be viewed in place. Of great importance to the ground‐water studies in coastal Georgia, the camera enables the geologist to see the important water‐bearing zones in a limestone aquifer, and to recognize cracks and solution cavities, the changes in geologic formations, and the irregularities in the well bore that indicate the relative hardness of the rocks. The engineer, well driller, and water developer can examine a well when “trouble shooting” to see whether the casing is broken, whether screens are eroded, or whether the well contains obstructions.

","language":"English","publisher":"Wiley Blackwell","doi":"10.1111/j.1745-6584.1963.tb01926.x","usgsCitation":"Callahan, J., Wait, R.L., and McCollum, M., 1963, Television — A new tool for the ground‐water geologist: Groundwater, v. 1, no. 4, p. 4-6, https://doi.org/10.1111/j.1745-6584.1963.tb01926.x.","productDescription":"3 p.","startPage":"4","endPage":"6","costCenters":[],"links":[{"id":386069,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Georgia","otherGeospatial":"coastal Georgia","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -81.32080078125,\n 32.519026027827515\n ],\n [\n -81.859130859375,\n 30.873940237887624\n ],\n [\n -81.968994140625,\n 30.477082932837682\n ],\n [\n -81.221923828125,\n 30.391830328088137\n ],\n [\n -80.66162109375,\n 32.045332838858506\n ],\n [\n -81.32080078125,\n 32.519026027827515\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"1","issue":"4","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Callahan, J.T.","contributorId":100920,"corporation":false,"usgs":true,"family":"Callahan","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":816723,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wait, R. L.","contributorId":15988,"corporation":false,"usgs":true,"family":"Wait","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":816724,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McCollum, M.J.","contributorId":40576,"corporation":false,"usgs":true,"family":"McCollum","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":816725,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":37471,"text":"37471 - 1963 - Waterfowl status report, 1963","interactions":[],"lastModifiedDate":"2014-07-15T13:28:46","indexId":"37471","displayToPublicDate":"1963-10-01T13:27:21","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":83,"text":"Special Scientific Report - Wildlife","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"75","title":"Waterfowl status report, 1963","docAbstract":"No abstract available.","language":"English","publisher":"U.s. Fish and Wildlife Service","publisherLocation":"Washington, D.C.","usgsCitation":"Glover, F., and Smith, J.D., 1963, Waterfowl status report, 1963: Special Scientific Report - Wildlife 75, iv, 178 p.","productDescription":"iv, 178 p.","numberOfPages":"182","costCenters":[],"links":[{"id":290140,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c64debe4b0001bd51477d8","contributors":{"authors":[{"text":"Glover, F.A.","contributorId":71485,"corporation":false,"usgs":true,"family":"Glover","given":"F.A.","email":"","affiliations":[],"preferred":false,"id":218134,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, J. Donald","contributorId":12380,"corporation":false,"usgs":true,"family":"Smith","given":"J.","email":"","middleInitial":"Donald","affiliations":[],"preferred":false,"id":218133,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":25147,"text":"25147 - 1963 - Chemical analyses of surface waters in Colorado, October 1959 to September 1962","interactions":[],"lastModifiedDate":"2025-07-21T20:15:08.184674","indexId":"25147","displayToPublicDate":"1963-10-01T11:59:21","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Chemical analyses of surface waters in Colorado, October 1959 to September 1962","docAbstract":"

Data presented herein are records of water quality for the period October 1959 to September 1962 for the sampling sites shown below and on the enclosed map. The data are preliminary and subject to revision. Final records are published in the annual series of Geological Survey Water-Supply Papers entitled \"Quality of Surface Waters of the United States, \" which can be obtained from the Superintendent of Documents, U. S. Government Printing Office, Washington, D. C. 20242.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/25147","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1963, Chemical analyses of surface waters in Colorado, October 1959 to September 1962, 56 p., https://doi.org/10.3133/25147.","productDescription":"56 p.","temporalStart":"1959-10-01","temporalEnd":"1962-09-30","costCenters":[],"links":[{"id":492699,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/25147/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":290129,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/25147/report-thumb.jpg"}],"country":"United States","state":"Colorado","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.0603,36.9924 ], [ -109.0603,41.0034 ], [ -102.0409,41.0034 ], [ -102.0409,36.9924 ], [ -109.0603,36.9924 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c64d78e4b0001bd5147745","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":529183,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221074,"text":"70221074 - 1963 - Origin of some intermittent ponds on quartzite ridges in western North Carolina","interactions":[],"lastModifiedDate":"2021-06-01T17:36:55.332649","indexId":"70221074","displayToPublicDate":"1963-09-01T12:31:41","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Origin of some intermittent ponds on quartzite ridges in western North Carolina","docAbstract":"

Several intermittent ponds and closed depressions as much as 200 feet wide occur on the crests of ridges in gently dipping Cambrian(?) quartzites in the southeastern foothills of the Blue Ridge Mountains near Morganton, North Carolina. The unconsolidated fill and debris in the ponds consists of clayey sand and saprolite with accessory minerals that could have been derived entirely from the quartzite. The pond water contains appreciable quantities of dissolved silica and with the aid of organic substances could have formed the depressions by solution since the beginning of the Pleistocene.

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1963)74[1183:OOSIPO]2.0.CO;2","usgsCitation":"Reed, J.C., Bryant, B.H., and Hack, J., 1963, Origin of some intermittent ponds on quartzite ridges in western North Carolina: Geological Society of America Bulletin, v. 74, no. 9, p. 1183-1188, https://doi.org/10.1130/0016-7606(1963)74[1183:OOSIPO]2.0.CO;2.","productDescription":"6 p.","startPage":"1183","endPage":"1188","costCenters":[],"links":[{"id":386047,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North Carolina","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -75.87158203125,\n 36.56260003738545\n ],\n [\n -82.28759765625,\n 36.66841891894786\n ],\n [\n -82.5732421875,\n 35.99578538642032\n ],\n [\n -83.91357421875,\n 35.53222622770337\n ],\n [\n -84.1552734375,\n 35.24561909420681\n ],\n [\n -84.26513671875,\n 34.97600151317588\n ],\n [\n -82.7490234375,\n 35.08395557927643\n ],\n [\n -82.177734375,\n 35.24561909420681\n ],\n [\n -80.83740234375,\n 35.191766965947394\n ],\n [\n -80.74951171875,\n 34.77771580360469\n ],\n [\n -79.60693359375,\n 34.77771580360469\n ],\n [\n -78.46435546875,\n 33.76088200086917\n ],\n [\n -77.95898437499999,\n 33.8339199536547\n ],\n [\n -76.3330078125,\n 34.88593094075317\n ],\n [\n -75.6298828125,\n 35.8356283888737\n ],\n [\n -75.87158203125,\n 36.56260003738545\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"74","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Reed, John C. Jr.","contributorId":223980,"corporation":false,"usgs":false,"family":"Reed","given":"John","suffix":"Jr.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":816700,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bryant, Bruce H. bbryant@usgs.gov","contributorId":26713,"corporation":false,"usgs":true,"family":"Bryant","given":"Bruce","email":"bbryant@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":false,"id":816701,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hack, John T.","contributorId":45168,"corporation":false,"usgs":true,"family":"Hack","given":"John T.","affiliations":[],"preferred":false,"id":816702,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70221068,"text":"70221068 - 1963 - Distribution of fluorine in unaltered silicic volcanic rocks of the western conterminous United States","interactions":[],"lastModifiedDate":"2021-06-01T17:04:12.010628","indexId":"70221068","displayToPublicDate":"1963-09-01T11:59:53","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Distribution of fluorine in unaltered silicic volcanic rocks of the western conterminous United States","docAbstract":"

An investigation of more than 170 samples of glass-rich volcanic rocks of rhyolitic or rhyodacitic composition shows marked regional variations in the fluorine content. The uniformity of the class of rocks was controlled by index of refraction determinations on fused beads and by chemical analyses of about one-seventh of the total number. The fluorine content ranges from 20 to 4,900 ppm. The frequency distribution closely approaches a log-normal one; the median value is 520 ppm, the 90 percentile 1,820 ppm. The mean for 167 samples is 820 ppm. These correspond fairly well with earlier averages for similar types of rocks. The highest values are predominantly from a belt in central Colorado and west-central New Mexico, from the Big Bend region of Texas, and from southeastern Idaho and western Utah and northeastern Nevada. The distribution of the fluorine in these rocks correlates well with the distribution of significant fluorspar deposits and somewhat less well with areas where volcanic rocks are prevalent and ground waters carry large amounts of fluorine.

","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.58.6.941","usgsCitation":"Coats, R., Gross, W., and Rader, L.F., 1963, Distribution of fluorine in unaltered silicic volcanic rocks of the western conterminous United States: Economic Geology, v. 58, no. 6, p. 941-951, https://doi.org/10.2113/gsecongeo.58.6.941.","productDescription":"11 p.","startPage":"941","endPage":"951","costCenters":[],"links":[{"id":386041,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"58","issue":"6","noUsgsAuthors":false,"publicationDate":"1963-09-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Coats, R.R.","contributorId":78339,"corporation":false,"usgs":true,"family":"Coats","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":816688,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gross, W.D.","contributorId":259165,"corporation":false,"usgs":false,"family":"Gross","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":816689,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rader, L. F. Jr.","contributorId":100909,"corporation":false,"usgs":true,"family":"Rader","given":"L.","suffix":"Jr.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":816690,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70221114,"text":"70221114 - 1963 - The hydraulic geometry of a shallow estuary","interactions":[],"lastModifiedDate":"2021-06-02T14:02:29.569826","indexId":"70221114","displayToPublicDate":"1963-09-01T08:59:12","publicationYear":"1963","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":"The hydraulic geometry of a shallow estuary","docAbstract":"

An analogy with entropy production in steady-state systems leads to a statement that the geometry of natural waterways is governed by two opposing influences: a) equal work per unit of area of bed, and b) minimum work done in the system as a whole. The resulting calculations applied to shallow, estuaries are verified by field measurements. 

","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626666309493340","usgsCitation":"Langbein, W.B., 1963, The hydraulic geometry of a shallow estuary: International Association of Scientific Hydrology - Bulletin , v. 8, no. 3, p. 84-94, https://doi.org/10.1080/02626666309493340.","productDescription":"11 p.","startPage":"84","endPage":"94","costCenters":[],"links":[{"id":386123,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Langbein, W. B.","contributorId":102053,"corporation":false,"usgs":true,"family":"Langbein","given":"W.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":816792,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221111,"text":"70221111 - 1963 - Preliminary results of a study of calcium carbonate saturation of ground water in central Florida","interactions":[],"lastModifiedDate":"2021-06-02T12:59:17.848563","indexId":"70221111","displayToPublicDate":"1963-09-01T07:55:41","publicationYear":"1963","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":"Preliminary results of a study of calcium carbonate saturation of ground water in central Florida","docAbstract":"

The departure of ground water from equilibrium with calcite is being studied in central Florida. Measurements of pH, temperature, and concentration of bicarbonate made in the field are used with standard laboratory analyses of water samples to calculate an ion activity product (K) for calcium carbonate. The calculated Kiap is compared with the equilibrium constant (Keq) for calcite to determine the departure from equilibrium. The calcium concentration is lowest in the area of the highest piezometric surface. Some of the highest concentrations of bicarbonate are in the area of low calcium. In about half of the area of study, the water is undersaturated with respect to calcite. This indicates that solution of limestone can occur several hundred feet below the water table.

","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626666309493336","usgsCitation":"Back, W., 1963, Preliminary results of a study of calcium carbonate saturation of ground water in central Florida: International Association of Scientific Hydrology - Bulletin , v. 8, no. 3, p. 43-51, https://doi.org/10.1080/02626666309493336.","productDescription":"9 p.","startPage":"43","endPage":"51","costCenters":[],"links":[{"id":480368,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/02626666309493336","text":"Publisher Index Page"},{"id":386120,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"central Florida","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -83.265380859375,\n 27.21555620902969\n ],\n [\n -79.541015625,\n 27.21555620902969\n ],\n [\n -79.541015625,\n 29.516110386062277\n ],\n [\n -83.265380859375,\n 29.516110386062277\n ],\n [\n -83.265380859375,\n 27.21555620902969\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"8","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Back, William","contributorId":59007,"corporation":false,"usgs":true,"family":"Back","given":"William","email":"","affiliations":[],"preferred":false,"id":816789,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221093,"text":"70221093 - 1963 - Hydrologic bench marks to distinguish the effects of climate vs. man","interactions":[],"lastModifiedDate":"2021-06-01T19:42:25.484388","indexId":"70221093","displayToPublicDate":"1963-07-01T14:39:43","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Hydrologic bench marks to distinguish the effects of climate vs. man","docAbstract":"

There is a vital need for hydrologic data representing various environments that are free from the effects of man's activities. Without such data hydrologists will be stymied in distinguishing hydrologic changes caused by man from those caused by climate. To provide this background information, the U. S. Geological Survey is planning a nationwide hydrologic bench‐mark program in which runoff, transport of sediment, precipitation, changes in vegetation, fluctuations in ground water, and other hydrologic events will be studied in locales unaffected by the works of man. The knowledge gained in operating these bench marks will be invaluable in statistical appraisals of hydrologic data wherein a part of the record is affected by man's activities.

","language":"English","publisher":"Wiley Blackwell","doi":"10.1111/j.1745-6584.1963.tb01918.x","usgsCitation":"Wilson, H., 1963, Hydrologic bench marks to distinguish the effects of climate vs. man: Groundwater, v. 1, no. 3, p. 13-14, https://doi.org/10.1111/j.1745-6584.1963.tb01918.x.","productDescription":"2 p.","startPage":"13","endPage":"14","costCenters":[],"links":[{"id":386073,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"3","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Wilson, H.D. Jr.","contributorId":51370,"corporation":false,"usgs":true,"family":"Wilson","given":"H.D.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":816734,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221089,"text":"70221089 - 1963 - Saline ground water — A little used and unmapped resource","interactions":[],"lastModifiedDate":"2021-06-01T19:19:26.466115","indexId":"70221089","displayToPublicDate":"1963-07-01T14:16:32","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Saline ground water — A little used and unmapped resource","docAbstract":"

Vast quantities of saline ground water await new commercial uses and economical demineralization processes for recognition as a valuable resource. Saline ground water is more widely distributed than any other natural resource, occurring throughout the United States and in geologic formations ranging from the oldest to the youngest. The Coastal Plain has the greatest reserve of fresh water in the country, but at depths ranging from a few feet to about 3,500 feet most of the fresh‐water aquifers also contain large quantities of brackish water. Paleozoic formations in the east‐central United States have long been producers of saline water as commercial brines and in association with oil and gas. The volume of saline ground water perhaps exceeds the fresh ground‐water supply in the Great Plains Region. The greater part of the Western Mountain Region is generally deficient in fresh ground water; however, saline water is present in highly permeable deposits in numerous closed basins and along saline streams. In each of these major ground‐water regions small to very large amounts of saline water can be pumped from wells ranging from a few tens of feet to several thousand feet in depth. Knowledge of saline water distribution is general and inadequate, having been attained as a by‐product of investigations of fresh‐water supplies. This knowledge should be expanded as technological advances in demineralization processes enhance the importance of saline water for potential supply in numerous water‐deficient areas. 

","language":"English","publisher":"Wiley Blackwell","doi":"10.1111/j.1745-6584.1963.tb01921.x","usgsCitation":"Poole, J.L., 1963, Saline ground water — A little used and unmapped resource: Groundwater, v. 1, no. 3, p. 18-20, https://doi.org/10.1111/j.1745-6584.1963.tb01921.x.","productDescription":"3 p.","startPage":"18","endPage":"20","costCenters":[],"links":[{"id":386068,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"3","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Poole, J. L.","contributorId":40583,"corporation":false,"usgs":true,"family":"Poole","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":816722,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221084,"text":"70221084 - 1963 - Some aspects of chemical equilibrium in ground water","interactions":[],"lastModifiedDate":"2021-06-01T18:51:47.135535","indexId":"70221084","displayToPublicDate":"1963-07-01T13:48:46","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Some aspects of chemical equilibrium in ground water","docAbstract":"

The influence of individual factors such as geologic and hydrologic characteristics of environment, biologic activity in soil, and pollutants on ground‐water composition is discussed. Aspects of chemical equilibria in ground water, sorption reactions, carbonate equilibria, chemistry of iron, and factors altering equilibria are presented.

","language":"English","publisher":"Wiley Blackwell","doi":"10.1111/j.1745-6584.1963.tb01924.x","usgsCitation":"Hem, J., 1963, Some aspects of chemical equilibrium in ground water: Groundwater, v. 1, no. 3, p. 30-34, https://doi.org/10.1111/j.1745-6584.1963.tb01924.x.","productDescription":"5 p.","startPage":"30","endPage":"34","costCenters":[],"links":[{"id":386058,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"3","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Hem, J.D.","contributorId":54576,"corporation":false,"usgs":true,"family":"Hem","given":"J.D.","affiliations":[],"preferred":false,"id":816713,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1014449,"text":"1014449 - 1963 - Kidney disease of salmonid fishes and the analysis of hatchery waters","interactions":[],"lastModifiedDate":"2025-08-01T16:02:09.353044","indexId":"1014449","displayToPublicDate":"1963-07-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"Kidney disease of salmonid fishes and the analysis of hatchery waters","docAbstract":"

No abstract available. 

","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1963)25[121:KDOSFA]2.0.CO;2","usgsCitation":"Warren, J., 1963, Kidney disease of salmonid fishes and the analysis of hatchery waters: Progressive Fish-Culturist, v. 25, no. 3, p. 121-131, https://doi.org/10.1577/1548-8659(1963)25[121:KDOSFA]2.0.CO;2.","productDescription":"11 p.","startPage":"121","endPage":"131","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":130494,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b47d2","contributors":{"authors":[{"text":"Warren, J.W.","contributorId":20285,"corporation":false,"usgs":true,"family":"Warren","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":320383,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1003298,"text":"1003298 - 1963 - Endothal derivatives as aquatic herbicides in fishery habitats","interactions":[],"lastModifiedDate":"2026-03-18T22:31:43.780726","indexId":"1003298","displayToPublicDate":"1963-07-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3741,"text":"Weeds","active":true,"publicationSubtype":{"id":10}},"title":"Endothal derivatives as aquatic herbicides in fishery habitats","docAbstract":"

The disodium salt of 3,6-endoxohexahydrophthalic acid (disodium endothal) and the derivative identified by the manufacturer as the di-N,N′-dimethylococoamine salt of endothal (coded as TD-47) were particularly effective upon submersed species of aquatic vegetation as contact herbicides. Disodium endothal at concentrations of 0.5 to 10.0 ppmw was effective in controlling approximately 50 per cent of the 19 species of plants involved in 270 tests. TD-47 at concentrations of 0.02 to 10.0 ppmw trolled 77 per cent of the 11 plant species in 94 tests.

Algae (Chara, Cladophora, Pithophora, and Spirogyra) were more effectively controlled by TD-47 than by disodium endothal. Although TD-47 was at least 10 times more herbicidal than disodium endothal, it was about 100 times more toxic to fish. Disodium endothal was more than 50 per cent effective on submersed aquatic plants at rates in excess of 2.5 ppmw with a wide margin of safety in fish (4- to 10-fold). Disodium endothal had a median tolerance limit ranging from 95 to 150 ppmw in the aggregate of nine fish species tested extensively. Median tolerance limits for TD-47 ranged from about 0.06 to 0.3 ppmw for five species of fish. TD-47 applied at a concentration lethal to fish (0.3 to 1.0 ppmw) was effective as a dual management tool in controlling vegetation and achieving partial or complete renovation of stunted fish populations.

Young, growing vegetation was most susceptible to control, and best results were achieved at water temperatures exceeding 60 F. Higher rates were required to kill plants as they matured and stands became dense. Endothal liquid formulations were superior to granules in controlling algal mats, floating and emergent plants. Granules were more effective on submersed rooted plants.

TD-47 residues were of short duration. The rate of disappearance depended on time and concentration. Detectable residues disappeared within 8 days following application of 0.3 ppmw and within 2 weeks for 0.6 ppmw. However, 1.0 to 3.0 ppmw took up to 25 days to disappear. Some residues were found in fish-food organisms from treated enclosures 3 weeks after application. Fish flesh showed no absorption of endothal-armeens at sublethal concentrations. Intraperitoneal injection of endothal into fish produced a disturbance of the osmoregulation. The physiological effect of endothal was measured by chemical analysis of blood serum.

","language":"English","publisher":"Cambridge University Press","doi":"10.2307/4040590","usgsCitation":"Walker, C., 1963, Endothal derivatives as aquatic herbicides in fishery habitats: Weeds, v. 11, no. 3, p. 226-232, https://doi.org/10.2307/4040590.","productDescription":"7 p.","startPage":"226","endPage":"232","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":178348,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cae9","contributors":{"authors":[{"text":"Walker, C.R.","contributorId":69097,"corporation":false,"usgs":true,"family":"Walker","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":313088,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70175775,"text":"70175775 - 1963 - Graphs of ground-water levels in Minnesota, 1957-1961","interactions":[],"lastModifiedDate":"2018-04-02T11:30:33","indexId":"70175775","displayToPublicDate":"1963-05-14T10:30:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":105,"text":"Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"18","title":"Graphs of ground-water levels in Minnesota, 1957-1961","docAbstract":"

No abstract available.

","language":"English","publisher":"Minnesota Department of Conservation, Division of Waters","publisherLocation":"St. Paul, MN","usgsCitation":"Straka, G., and Miller, W.A., 1963, Graphs of ground-water levels in Minnesota, 1957-1961: Bulletin 18, 58 p.","productDescription":"58 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":326901,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b82dc0e4b03fd6b7da3731","contributors":{"authors":[{"text":"Straka, G.C.","contributorId":173863,"corporation":false,"usgs":false,"family":"Straka","given":"G.C.","email":"","affiliations":[],"preferred":false,"id":646333,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, W. A.","contributorId":100007,"corporation":false,"usgs":true,"family":"Miller","given":"W.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":646334,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70175725,"text":"70175725 - 1963 - Quality of waters, Minnesota--A compilation, 1955-62","interactions":[],"lastModifiedDate":"2018-03-19T10:04:08","indexId":"70175725","displayToPublicDate":"1963-05-06T15:45:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":105,"text":"Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"21","title":"Quality of waters, Minnesota--A compilation, 1955-62","docAbstract":"

No abstract available.

","language":"English","publisher":"Minnesota Department of Conservation, Division of Waters","usgsCitation":"Maderak, M., 1963, Quality of waters, Minnesota--A compilation, 1955-62: Bulletin 21, 104 p.","productDescription":"104 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":326836,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b6dc6ae4b03fd6b7d94c7a","contributors":{"authors":[{"text":"Maderak, M.L.","contributorId":41452,"corporation":false,"usgs":true,"family":"Maderak","given":"M.L.","affiliations":[],"preferred":false,"id":646206,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221072,"text":"70221072 - 1963 - Studies of fluid inclusions iii: Extraction and uantitative analysis of inclusions in the milligram range","interactions":[],"lastModifiedDate":"2021-06-01T17:24:34.237717","indexId":"70221072","displayToPublicDate":"1963-05-01T12:21:19","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Studies of fluid inclusions iii: Extraction and uantitative analysis of inclusions in the milligram range","docAbstract":"

A method has been developed for the extraction and chemical microanalysis of individual fluid inclusions, or groups of inclusions, in the milligram range. Usable quantitative analyses for Na, K, Ca, Mg, CI, B, and SO* have been obtained of mineral samples containing several milligrams of inclusion fluid, and with increased experimental errors, on fractional milligram samples. The steps involved are: 1) concentration of inclusions by sample selection and cutting; 2) electrolytic cleaning; 3) crushing in soft copper sample tube in vacuo; 4) conversion of emitted water to hydrogen and determination of its volume; 5) mass spectrometric determination of the D/H ratio if desired; 6) leaching of the crushed mineral to dissolve soluble salts remaining; 7) microanalysis of the filtrate by sensitive colorimetric and flame photometric methods. The method has been applied to determine the composition of fluid inclusions in mineral samples from several types of deposits, with special attention to a series of samples from Mississippi Valley-type ore deposits. 

","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.58.3.353","usgsCitation":"Roedder, E., Ingram, B., and Hall, W., 1963, Studies of fluid inclusions iii: Extraction and uantitative analysis of inclusions in the milligram range: Economic Geology, v. 58, no. 3, p. 353-374, https://doi.org/10.2113/gsecongeo.58.3.353.","productDescription":"22 p.","startPage":"353","endPage":"374","costCenters":[],"links":[{"id":386045,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"58","issue":"3","noUsgsAuthors":false,"publicationDate":"1963-05-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Roedder, E.","contributorId":100986,"corporation":false,"usgs":true,"family":"Roedder","given":"E.","affiliations":[],"preferred":false,"id":816696,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ingram, B.","contributorId":20891,"corporation":false,"usgs":true,"family":"Ingram","given":"B.","affiliations":[],"preferred":false,"id":816697,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hall, W. E.","contributorId":6431,"corporation":false,"usgs":true,"family":"Hall","given":"W. E.","affiliations":[],"preferred":false,"id":816698,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70221060,"text":"70221060 - 1963 - Determination of total sulfur in water by neutron activation analysis","interactions":[],"lastModifiedDate":"2021-06-02T12:45:34.27739","indexId":"70221060","displayToPublicDate":"1963-05-01T11:05:27","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Determination of total sulfur in water by neutron activation analysis","docAbstract":"

No abstract available. 

","language":"English","publisher":"American Chemical Society","doi":"10.1021/ac60199a033","usgsCitation":"Wayman, C.H., 1963, Determination of total sulfur in water by neutron activation analysis: Analytical Chemistry, v. 35, no. 6, p. 768-768, https://doi.org/10.1021/ac60199a033.","productDescription":"1 p.","startPage":"768","endPage":"768","costCenters":[],"links":[{"id":386031,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"35","issue":"6","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Wayman, C. H.","contributorId":87618,"corporation":false,"usgs":true,"family":"Wayman","given":"C.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":816671,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221073,"text":"70221073 - 1963 - Studies of fluid inclusions; [Part] 2, Freezing data and their interpretation","interactions":[],"lastModifiedDate":"2021-06-01T17:30:35.930425","indexId":"70221073","displayToPublicDate":"1963-04-01T12:28:03","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Studies of fluid inclusions; [Part] 2, Freezing data and their interpretation","docAbstract":"

Aqueous and non-aqueous inclusions in 84 samples of various minerals from a wide range of geologic environments were studied with the freezing stage in order to gain an insight into the range of concentrations and compositions of fluid inclusions. Inclusions in most Mississippi Valley-type ore minerals contain highly concentrated saline solutions, showing freezing temperatures between -23.4° and -10.5° C; minerals from ore deposits of more typically hydrothermal affiliations mainly show temperatures of -9.4° to nearly 0° C; and inclusions in quartz crystals from sedimentary, metamorphic, and igneous rock environments show a wide range of freezing temperatures. Inclusions in pegmatite minerals in particular vary over a wide range, from the most concentrated solutions found in any inclusion (> 40% salts) to fairly dilute solutions (< 5% salts). Most inclusions in quartz from Swiss Alpine-type veins, and from Brazilian quartz veins and pegmatites, show freezing temperatures in the range -8.5° to -2.5°, and considerable free C02. Other geologic environments sampled include Colombian emerald, pegmatitic topaz and fluorite, the Triassic traprock zeolite assemblage, and sedimentary halite beds. Not all the phenomena exhibited by inclusions at low temperature are completely understood at present but several crystalline hydrate phases, such as NaCl-2H,0 and CO,-5%H,0 (structural formula 8C02-46H20), are shown to be stable in inclusions of appropriate composition even at temperatures above 0° C, and probably exist in the inclusions in natural rocks in polar regions. More significantly, the formation and recognition of such phases aid in establishing the gross composition of individual inclusions far too small for chemical analysis. The data obtained are useful in a variety of ways, such as: discriminating among gas, liquid, and supercritical fluid, and among liquid water, liquid oil, and liquid C02 in inclusions; improving precision of the pressure corrections applied to inclusion filling temperature determinations; proving the general lack of leakage into or out of inclusions; estimating the minimum pressure at the time of deposition of certain samples; verifying the lack of extraneous solid crystallization nuclei in the inclusions and hence their formation from exceedingly quiet, clean solutions; determining the total equivalent NaCl concentrations and some information concerning the composition of the fluids from which ores have formed; and determining changes in the composition of the fluids bathing a single crystal during its growth, and at certain times throughout its history. 

","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.58.2.167","usgsCitation":"Roedder, E., 1963, Studies of fluid inclusions; [Part] 2, Freezing data and their interpretation: Economic Geology, v. 58, no. 2, p. 167-211, https://doi.org/10.2113/gsecongeo.58.2.167.","productDescription":"45 p.","startPage":"167","endPage":"211","costCenters":[],"links":[{"id":386046,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"58","issue":"2","noUsgsAuthors":false,"publicationDate":"1963-04-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Roedder, E.","contributorId":100986,"corporation":false,"usgs":true,"family":"Roedder","given":"E.","affiliations":[],"preferred":false,"id":816699,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010630,"text":"70010630 - 1963 - Geothermal brine well: Mile-deep drill hole may tap ore-bearing magmatic water and rocks undergoing metamorphism","interactions":[],"lastModifiedDate":"2026-02-24T16:29:47.121403","indexId":"70010630","displayToPublicDate":"1963-03-08T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Geothermal brine well: Mile-deep drill hole may tap ore-bearing magmatic water and rocks undergoing metamorphism","docAbstract":"A deep geothermal well in California has tapped a very saline brine extraordinarily high in heavy metals and other rare elements; copper and silver are precipitated during brine production. Preliminary evidence suggests that the brine may be pure magmatic water and an active ore-forming solution. Metamorphism of relatively young rocks may also be occurring within accessible depths.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.139.3558.919","issn":"00368075","usgsCitation":"White, D., Anderson, E., and Grubbs, D., 1963, Geothermal brine well: Mile-deep drill hole may tap ore-bearing magmatic water and rocks Undergoing Metamorphism: Science, v. 139, no. 3558, p. 919-922.","productDescription":"4 p.","startPage":"919","endPage":"922","costCenters":[],"links":[{"id":219250,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -124.35833009199186,\n 41.92267234102607\n ],\n [\n -124.82267524623933,\n 40.77876112732989\n ],\n [\n -123.32762724490286,\n 37.07156994461869\n ],\n [\n -120.07531410012949,\n 33.03699572297022\n ],\n [\n -117.36160626955325,\n 32.503385963168625\n ],\n [\n -114.59741427971602,\n 32.744584528523106\n ],\n [\n -114.49350453241671,\n 33.59775702209137\n ],\n [\n -114.11681520286865,\n 34.321044739732756\n ],\n [\n -114.31835152514394,\n 34.83342016839895\n ],\n [\n -119.97715136272916,\n 38.98563563041786\n ],\n [\n -119.96983102849805,\n 42.03687795072952\n ],\n [\n -124.35833009199186,\n 41.92267234102607\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"139","issue":"3558","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a28cbe4b0c8380cd5a3f9","contributors":{"authors":[{"text":"White, D. E.","contributorId":20729,"corporation":false,"usgs":false,"family":"White","given":"D. E.","affiliations":[{"id":6672,"text":"former: USGS Southwest Biological Science Center, Colorado Plateau Research Station, Flagstaff, AZ. Current address: TN-SCORE, Univ of Tennessee, Knoxville, TN, e-mail: jennen@gmail.com","active":true,"usgs":false}],"preferred":false,"id":359298,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, E.T.","contributorId":30750,"corporation":false,"usgs":true,"family":"Anderson","given":"E.T.","email":"","affiliations":[],"preferred":false,"id":359300,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Grubbs, D.K.","contributorId":22086,"corporation":false,"usgs":true,"family":"Grubbs","given":"D.K.","email":"","affiliations":[],"preferred":false,"id":359299,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ]}