No abstract available.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Transactions of the 16th North American Wildlife Conference","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"16th North American Wildlife Conference","conferenceDate":"1950","language":"English","publisher":"Wildlife Management Institute","usgsCitation":"Petrides, G.A., and Byrant, C.R., 1950, An analysis of the 1949-50 fowl cholera epizootic in Texas panhandle waterfowl, in Transactions of the 16th North American Wildlife Conference, 1950, p. 193-216.","productDescription":"24 p.","startPage":"193","endPage":"216","costCenters":[],"links":[{"id":402208,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -103.084716796875,\n 34.51560953848204\n ],\n [\n -99.986572265625,\n 34.51560953848204\n ],\n [\n -99.986572265625,\n 36.527294814546245\n ],\n [\n -103.084716796875,\n 36.527294814546245\n ],\n [\n -103.084716796875,\n 34.51560953848204\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Petrides, George A.","contributorId":27577,"corporation":false,"usgs":true,"family":"Petrides","given":"George","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":844710,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Byrant, Charles R.","contributorId":292471,"corporation":false,"usgs":false,"family":"Byrant","given":"Charles","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":844711,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70048281,"text":"tem33 - 1950 - Preliminary examination of uranium deposits near Marysvale, Piute County, Utah","interactions":[],"lastModifiedDate":"2014-02-28T14:40:53","indexId":"tem33","displayToPublicDate":"1950-01-01T12:38:00","publicationYear":"1950","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"33","title":"Preliminary examination of uranium deposits near Marysvale, Piute County, Utah","docAbstract":"Autunite and other uranium minerals were discovered in 1948 by Pratt Seegmiller about 3 1/4 miles north of Marysvale, Piute County, Utah. Mining operations were begun in the summer of 1949 by the Vanadium Corporation of America on the Prospector and the Freedom claims, and by the Bullion Monarch Mining Company a the Bullion Monarch claims. These claims were examined briefly in December 1949 and January 1950 by the writers. The uranium deposits of the Marysvale district are in north-easterly striking fault zones in quartz monzonite that intrudes rocks of the \"older\" Tertiary volcanic sequence. Flows and tuffs of the \"younger\" Tertiary volcanic sequence uncomfortably overlie the earlier rocks. Autunite, tobernite, uranophane, schroeckingerite, and at least one unidentified secondary uranium mineral occur in the upper parts of the deposits. Pitchblende has been mined from the underground workings of the Prospector No. 1 mine. The uranium minerals are associated with dense quartz veins and intensely argillized wall rock. In the upper parts of the deposits pyrite is completely oxidized. The secondary uranium minerals probably were formed by the alteration of primary pitchblende by circulating meteoric waters.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem33","usgsCitation":"Granger, H., and Bauer, H., 1950, Preliminary examination of uranium deposits near Marysvale, Piute County, Utah: U.S. Geological Survey Trace Elements Memorandum 33, Report: 28 p.; 3 Plates: 25.47 x 29.95 inches or smaller, https://doi.org/10.3133/tem33.","productDescription":"Report: 28 p.; 3 Plates: 25.47 x 29.95 inches or smaller","numberOfPages":"39","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":277867,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0033/report-thumb.jpg"},{"id":283099,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0033/report.pdf"},{"id":283101,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0033/plate-3.pdf"},{"id":283100,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0033/plate-2.pdf"},{"id":283102,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0033/plate-6.pdf"}],"country":"United States","state":"Utah","county":"Piute County","city":"Marysvale","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.310933,38.415766 ], [ -112.310933,38.460575 ], [ -112.203991,38.460575 ], [ -112.203991,38.415766 ], [ -112.310933,38.415766 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"523c1cf4e4b024b60d40734a","contributors":{"authors":[{"text":"Granger, Harry C.","contributorId":67992,"corporation":false,"usgs":true,"family":"Granger","given":"Harry C.","affiliations":[],"preferred":false,"id":484236,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bauer, Herman L.","contributorId":13224,"corporation":false,"usgs":true,"family":"Bauer","given":"Herman L.","affiliations":[],"preferred":false,"id":484235,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":72090,"text":"tem171 - 1950 - Distribution of leached radioactive material in the Legin Group Area, San Miguel County, Colorado","interactions":[],"lastModifiedDate":"2014-06-03T11:40:19","indexId":"tem171","displayToPublicDate":"1950-01-01T10:50:00","publicationYear":"1950","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"171","title":"Distribution of leached radioactive material in the Legin Group Area, San Miguel County, Colorado","docAbstract":"Radioactivity anomalies, which are small in magnitude, and probably are not caused by extensions of known uranium-vanadium ore bodies, were detected during the gamma-ray logging of diamond-drill holes in the Legin group of claims, southwest San Miguel County, Colo. The positions of these anomalies are at the top surfaces of mudstone strata within, and at the base of, the ore-bearing sandstone of the Salt Wash member of the Morrison formation.
\nThe distribution of these anomalies suggests that ground water has leached radioactive material from the ore bodies and has carried it down dip and laterally along the top surfaces of underlying impermeable mudstone strata for distance as great as 300 feet.
\nThe anomalies are probably caused by radon and its daughter elements. Preliminary tests indicate that radon in quantities up to 10-7 curies per liter may be present in ground water flowing along sandstone-mudstone contacts under carnotite ore bodies. In comparison, the radium content of the same water is less than 10-10 curies per liter.
\nFurther substantiation of the relationship between ore bodies, the movement of water, and the radon-caused anomalies may greatly increase the scope of gamma-ray logs of drill holes as an aid to prospecting.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem171","usgsCitation":"Rogers, A., 1950, Distribution of leached radioactive material in the Legin Group Area, San Miguel County, Colorado: U.S. Geological Survey Trace Elements Memorandum 171, 8 p., https://doi.org/10.3133/tem171.","productDescription":"8 p.","numberOfPages":"22","costCenters":[],"links":[{"id":284600,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0171/report.pdf"},{"id":283470,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tem171.jpg"}],"country":"United States","state":"Colorado","county":"San Miguel County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.04515,37.772072 ], [ -109.04515,38.153099 ], [ -107.73111,38.153099 ], [ -107.73111,37.772072 ], [ -109.04515,37.772072 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"535593ffe4b0120853e8bf3b","contributors":{"authors":[{"text":"Rogers, Allen S.","contributorId":66553,"corporation":false,"usgs":true,"family":"Rogers","given":"Allen S.","affiliations":[],"preferred":false,"id":285095,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010862,"text":"70010862 - 1950 - The origin of high sodium bicarbonate waters in the Atlantic and Gulf Coastal Plains","interactions":[],"lastModifiedDate":"2020-11-23T17:46:06.498467","indexId":"70010862","displayToPublicDate":"1950-01-01T00:00:00","publicationYear":"1950","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"The origin of high sodium bicarbonate waters in the Atlantic and Gulf Coastal Plains","docAbstract":"Some sodium bicarbonate waters at depth in the Atlantic and Gulf Coastal Plains have the same bicarbonate content as the shallower calcium bicarbonate waters in the same formation and appear to be the result of replacement of calcium by sodium through the action of base-exchange minerals. Others, however, contain several hundred parts per million more of bicarbonate than any of the calcium bicarbonate waters and much more bicarbonate than can be attributed to solution of calcium carbonate through the action of carbon dioxide derived from the air and soil.
As the waters in the Potomac group (Cretaceous) are all low in sulphate and as the environmental conditions under which the sediments of the Potomac group were deposited do not indicate that large amounts of sulphate are available for solution, it does not seem probable that carbon dioxide generated by chemical or biochemical breakdown of sulphate is responsible for the high sodium bicarbonate waters in this area.
Sulphate as a source of oxygen is not necessary for the generation of carbon dioxide by carbonaceous material. Oxygen is an important constituent of carbonaceous material and carbon dioxide is a characteristic decomposition product of such material—as, for example, peat and lignite.
Experimental work showed that distilled water, calcium bicarbonate water, and sodium bicarbonate water, after contact with lignite, calcium carbonate, and permutite (a base-exchange material), had all increased greatly in sodium bicarbonate content and had become similar in chemical character and in mineral content to high sodium bicarbonate waters found in the Coastal Plain. The tests indicated that carbonaceous material can act as a source of carbon dioxide, which, when dissolved in water, enables it to take into solution more calcium carbonate. If base-exchange materials are also present to replace calcium with sodium, a still greater amount of bicarbonate can be held in solution. The presence of carbonaceous material, together with calcium carbonate and base-exchange minerals in a formation is, therefore, sufficient to account for the occurrence in it of high sodium bicarbonate waters.
","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(50)90007-X","usgsCitation":"Foster, M., 1950, The origin of high sodium bicarbonate waters in the Atlantic and Gulf Coastal Plains: Geochimica et Cosmochimica Acta, v. 1, no. 1, p. 33-48, https://doi.org/10.1016/0016-7037(50)90007-X.","productDescription":"16 p.","startPage":"33","endPage":"48","numberOfPages":"16","costCenters":[],"links":[{"id":218874,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bae6be4b08c986b3240ae","contributors":{"authors":[{"text":"Foster, Margaret D.","contributorId":97958,"corporation":false,"usgs":true,"family":"Foster","given":"Margaret D.","affiliations":[],"preferred":false,"id":359806,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010864,"text":"70010864 - 1950 - Water analysis","interactions":[],"lastModifiedDate":"2012-03-12T17:18:16","indexId":"70010864","displayToPublicDate":"1950-01-01T00:00:00","publicationYear":"1950","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":"Water analysis","docAbstract":"[No abstract available]","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Analytical Chemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00032700","usgsCitation":"Love, S.K., 1950, Water analysis: Analytical Chemistry, v. 22, no. 2, p. 264-268.","startPage":"264","endPage":"268","numberOfPages":"5","costCenters":[],"links":[{"id":218876,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"22","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc797e4b08c986b32c515","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":359809,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70175872,"text":"70175872 - 1949 - Geology and ground-water resources of a part of south-central Kansas, with specific references to the Wichita municipal water supply","interactions":[],"lastModifiedDate":"2016-08-19T13:08:54","indexId":"70175872","displayToPublicDate":"2014-10-14T12:25:00","publicationYear":"1949","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2579,"text":"Kansas Geological Survey Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Geology and ground-water resources of a part of south-central Kansas, with specific references to the Wichita municipal water supply","language":"English","publisher":"University of Kansas","publisherLocation":"Lawrence, KS","usgsCitation":"Williams, C.C., and Lohman, S.W., 1949, Geology and ground-water resources of a part of south-central Kansas, with specific references to the Wichita municipal water supply: Kansas Geological Survey Bulletin, v. 79, 455 p. .","productDescription":"455 p. ","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":327060,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":327059,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.kgs.ku.edu/General/geologyBulls.html"}],"volume":"79","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b82dbfe4b03fd6b7da3714","contributors":{"authors":[{"text":"Williams, Charles C.","contributorId":107367,"corporation":false,"usgs":true,"family":"Williams","given":"Charles","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":646474,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lohman, S. W.","contributorId":45318,"corporation":false,"usgs":true,"family":"Lohman","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":646475,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":16383,"text":"ofr144 - 1949 - Contribution to the problem of the capacity of water for spontaneous crystallization = K voprosu o sposobnosti vody k samoproizvol'noi kristallizatsii /","interactions":[],"lastModifiedDate":"2014-08-01T14:18:27","indexId":"ofr144","displayToPublicDate":"2013-08-01T14:17:00","publicationYear":"1949","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":"144","title":"Contribution to the problem of the capacity of water for spontaneous crystallization = K voprosu o sposobnosti vody k samoproizvol'noi kristallizatsii /","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/ofr144","usgsCitation":"Vinokurov, G., and Poire, I., 1949, Contribution to the problem of the capacity of water for spontaneous crystallization = K voprosu o sposobnosti vody k samoproizvol'noi kristallizatsii /: U.S. Geological Survey Open-File Report 144, 3 p., https://doi.org/10.3133/ofr144.","productDescription":"3 p.","costCenters":[],"links":[{"id":291529,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53dca9c0e4b0761578637716","contributors":{"authors":[{"text":"Vinokurov, G.A.","contributorId":27800,"corporation":false,"usgs":true,"family":"Vinokurov","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":172754,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Poire, Inna V.","contributorId":50916,"corporation":false,"usgs":true,"family":"Poire","given":"Inna V.","affiliations":[],"preferred":false,"id":172755,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70047667,"text":"70047667 - 1949 - Geology of the Roswell artesian basin, New Mexico, and its relation to the Hondo Reservoir and Effect on artesian aquifer storage of flood water in Hondo Reservoir","interactions":[{"subject":{"id":70047667,"text":"70047667 - 1949 - Geology of the Roswell artesian basin, New Mexico, and its relation to the Hondo Reservoir and Effect on artesian aquifer storage of flood water in Hondo Reservoir","indexId":"70047667","publicationYear":"1949","noYear":false,"title":"Geology of the Roswell artesian basin, New Mexico, and its relation to the Hondo Reservoir and Effect on artesian aquifer storage of flood water in Hondo Reservoir"},"predicate":"SUPERSEDED_BY","object":{"id":50957,"text":"ofr5197 - 1951 - Geology of the Roswell artesian basin, New Mexico, and its relation to the Hondo Reservoir","indexId":"ofr5197","publicationYear":"1951","noYear":false,"title":"Geology of the Roswell artesian basin, New Mexico, and its relation to the Hondo Reservoir"},"id":1}],"supersededBy":{"id":50957,"text":"ofr5197 - 1951 - Geology of the Roswell artesian basin, New Mexico, and its relation to the Hondo Reservoir","indexId":"ofr5197","publicationYear":"1951","noYear":false,"title":"Geology of the Roswell artesian basin, New Mexico, and its relation to the Hondo Reservoir"},"lastModifiedDate":"2013-08-16T15:30:03","indexId":"70047667","displayToPublicDate":"2013-01-01T15:20:00","publicationYear":"1949","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":138,"text":"Technical Report","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"9","title":"Geology of the Roswell artesian basin, New Mexico, and its relation to the Hondo Reservoir and Effect on artesian aquifer storage of flood water in Hondo Reservoir","docAbstract":"In the Roswell Basin in southeastern New Mexico artesian water is produced from cavernous zones in the carbonate rocks of the San Andres formation and the lower part of the Chalk Bluff formation, both of Permian age. The Hondo Reservoir, 9 miles west-southwest of Roswell, was completed by the U. S. Bureau of Reclamation in 1907, to store waters of the Rio Hondo for irrigation. The project was not successful, as the impounded water escaped rapidly through holes in the gypsum and limestone of the San Andres formation constituting its floor. Of 27,000 acre~feet that entered the reservoir between 1908 and 1913, only 1,100 acre-feet was drawn Ollt for use, the remainder escaping through the floor of the reservoir. Since 1939, plans have been drawn up by the State Engineer and by Federal agencies to utilize the reservoir to protect Roswell from floods. It has also been suggested that water from the Pecos River might be diverted into underground storage through the reservoir. Sinkholes in the Roswell Basin are largely clustered in areas where gypsum occurs in the bedrock. Collapse of strata is due to solution of underlying rock commonly containing gypsum. Domes occur in gypsiferous strata near Salt Creek. The Bottomless Lakes, sinkhole lakes in the escarpment on the east side of the Pecos, are believed to have developed in north-south hinge-line fractures opened when the westernmost beds in the escarpment collapsed. Collapse was due to solution and removal of gypsiferous rock by artesian water which now fills the lakes.","language":"English","publisher":"New Mexico State Engineer","publisherLocation":"Santa Fe, NM","collaboration":"Prepared in Cooperation with the Geological Survey and Bureau of Reclamation United States Department of the Interior","usgsCitation":"Bean, R.T., and Theis, C.V., 1949, Geology of the Roswell artesian basin, New Mexico, and its relation to the Hondo Reservoir and Effect on artesian aquifer storage of flood water in Hondo Reservoir: Technical Report 9, ii, 36 p.","productDescription":"ii, 36 p.","numberOfPages":"45","costCenters":[],"links":[{"id":276716,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047667.JPG"},{"id":276715,"type":{"id":11,"text":"Document"},"url":"https://www.ose.state.nm.us/PDF/Publications/Library/TechnicalReports/TechReport-009.pdf"}],"country":"United States","state":"New Mexico","otherGeospatial":"Artesian Basin;Hondo Reservoir","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.0,31.33 ], [ -109.0,37.0 ], [ -103.0,37.0 ], [ -103.0,31.33 ], [ -109.0,31.33 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"520f49e2e4b0fc50304bc4c4","contributors":{"authors":[{"text":"Bean, Robert T.","contributorId":105630,"corporation":false,"usgs":true,"family":"Bean","given":"Robert","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":482674,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Theis, Charles V.","contributorId":48080,"corporation":false,"usgs":true,"family":"Theis","given":"Charles","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":482673,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70040285,"text":"70040285 - 1949 - Buried preglacial ground-water channels in the Albany-Schenectady area in New York","interactions":[],"lastModifiedDate":"2021-02-05T17:28:49.958581","indexId":"70040285","displayToPublicDate":"2012-01-01T09:52:51","publicationYear":"1949","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":242,"text":"Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"GW-20A","title":"Buried preglacial ground-water channels in the Albany-Schenectady area in New York","docAbstract":"No abstract available.
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","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":327072,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":327071,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.kgs.ku.edu/General/geologyBulls.html"}],"volume":"84","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b82dc3e4b03fd6b7da375b","contributors":{"authors":[{"text":"Latta, B.F.","contributorId":173166,"corporation":false,"usgs":false,"family":"Latta","given":"B.F.","email":"","affiliations":[],"preferred":false,"id":646491,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70175881,"text":"70175881 - 1949 - Geology and ground-water resources of Pawnee and Edwards Counties, Kansas","interactions":[],"lastModifiedDate":"2016-08-19T13:30:36","indexId":"70175881","displayToPublicDate":"2011-06-08T13:30:00","publicationYear":"1949","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2579,"text":"Kansas Geological Survey Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Geology and ground-water resources of Pawnee and Edwards Counties, Kansas","language":"English","publisher":"University of Kansas","publisherLocation":"Lawrence, KS","usgsCitation":"McLaughlin, T.G., 1949, Geology and ground-water resources of Pawnee and Edwards Counties, Kansas: Kansas Geological Survey Bulletin, v. 80, 189 p. .","productDescription":"189 p. ","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":327070,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":327069,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.kgs.ku.edu/General/geologyBulls.html"}],"volume":"80","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b82dbde4b03fd6b7da36fb","contributors":{"authors":[{"text":"McLaughlin, Thad G.","contributorId":95548,"corporation":false,"usgs":true,"family":"McLaughlin","given":"Thad","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":646490,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70175883,"text":"70175883 - 1949 - Geology and ground-water resources of Norton County and north-western Phillips County, Kansas","interactions":[],"lastModifiedDate":"2016-08-19T13:36:50","indexId":"70175883","displayToPublicDate":"2011-02-15T00:00:00","publicationYear":"1949","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2579,"text":"Kansas Geological Survey Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Geology and ground-water resources of Norton County and north-western Phillips County, Kansas","language":"English","publisher":"University of Kansas","publisherLocation":"Lawrence, KS","usgsCitation":"Frye, J., and Leonard, A., 1949, Geology and ground-water resources of Norton County and north-western Phillips County, Kansas: Kansas Geological Survey Bulletin, v. 81, 144.","productDescription":"144","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":327073,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.kgs.ku.edu/General/geologyBulls.html"},{"id":327074,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"81","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b82dbde4b03fd6b7da36f7","contributors":{"authors":[{"text":"Frye, J.C.","contributorId":35067,"corporation":false,"usgs":true,"family":"Frye","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":646492,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leonard, A.R.","contributorId":101669,"corporation":false,"usgs":true,"family":"Leonard","given":"A.R.","email":"","affiliations":[],"preferred":false,"id":646493,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70175885,"text":"70175885 - 1949 - Ground water in southwestern Kansas","interactions":[],"lastModifiedDate":"2016-08-19T13:44:31","indexId":"70175885","displayToPublicDate":"2010-02-09T00:00:00","publicationYear":"1949","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2579,"text":"Kansas Geological Survey Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Ground water in southwestern Kansas","language":"English","publisher":"University of Kansas","publisherLocation":"Lawrence, KS","usgsCitation":"Frye, J., and Fishel, V., 1949, Ground water in southwestern Kansas: Kansas Geological Survey Bulletin, 24 p. .","productDescription":"24 p. 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1949 - Migration of the green-winged teal","interactions":[],"lastModifiedDate":"2012-02-02T00:15:13","indexId":"5210054","displayToPublicDate":"2009-06-09T09:23:16","publicationYear":"1949","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Migration of the green-winged teal","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Migration of some North American waterfowl: A progress report on an analysis of banding records","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","usgsCitation":"Low, S., 1949, Migration of the green-winged teal, chap. of Migration of some North American waterfowl: A progress report on an analysis of banding records, p. 17-18.","productDescription":"48","startPage":"17","endPage":"18","numberOfPages":"48","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196444,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b1658","contributors":{"authors":[{"text":"Low, S.H.","contributorId":105001,"corporation":false,"usgs":true,"family":"Low","given":"S.H.","email":"","affiliations":[],"preferred":false,"id":327688,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5210053,"text":"5210053 - 1949 - The migration of the pintail","interactions":[],"lastModifiedDate":"2012-02-02T00:15:13","indexId":"5210053","displayToPublicDate":"2009-06-09T09:23:16","publicationYear":"1949","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"The migration of the pintail","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Migration of some North American waterfowl: A progress report on an analysis of banding records","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","usgsCitation":"Low, S., 1949, The migration of the pintail, chap. of Migration of some North American waterfowl: A progress report on an analysis of banding records, p. 13-16.","productDescription":"48","startPage":"13","endPage":"16","numberOfPages":"48","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196443,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4955","contributors":{"authors":[{"text":"Low, S.H.","contributorId":105001,"corporation":false,"usgs":true,"family":"Low","given":"S.H.","email":"","affiliations":[],"preferred":false,"id":327687,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5210023,"text":"5210023 - 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Groundwater is pumped only from wells drilled in Precambrian rock in the northern two-thirds of the county. The generally low permeability of this rock limits the availability of groundwater in this area. Saturated deposits of sand and gravel yield more than 500 gal/min to wells in the southern part of the county. Background groundwater quality and indicators of groundwater-quality problems, such as elevated concentrations of nitrate, chloride, hardness, and iron, are compared by aquifer for the entire county. An elevated concentration of iron is the major water quality problem in the county. Results of water quality analysis from observation wells drilled next to abandoned landfills throughout the county indicate that groundwater in the immediate vicinity of these landfills has been affected by leachate. The report includes maps of the thickness and saturated thickness of unconsolidated deposits, a water-table map, and tables of aquifer-production and well-production data from about 1,500 drillers ' well-construction reports. (USGS)","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir60","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1949, Index of surface-water records, part 12, Pacific slope basins in Washington and upper Columbia River basin, to September 30, 1948: U.S. Geological Survey Circular 60, 17 p. ;27 cm., https://doi.org/10.3133/cir60.","productDescription":"17 p. ;27 cm.","costCenters":[],"links":[{"id":123816,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1949/0060/report-thumb.jpg"},{"id":30976,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1949/0060/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64977b","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":528134,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3899,"text":"cir45 - 1949 - Index of surface-water records, part 9, Colorado River basin, to September 30, 1948","interactions":[{"subject":{"id":43469,"text":"ofr62148 - 1962 - Geology and fuel resources of the southwestern part of the Raton coal field, Colfax County, New Mexico","indexId":"ofr62148","publicationYear":"1962","noYear":false,"title":"Geology and fuel resources of the southwestern part of the Raton coal field, Colfax County, New Mexico"},"predicate":"SUPERSEDED_BY","object":{"id":3899,"text":"cir45 - 1949 - Index of surface-water records, part 9, Colorado River basin, to September 30, 1948","indexId":"cir45","publicationYear":"1949","noYear":false,"title":"Index of surface-water records, part 9, Colorado River basin, to September 30, 1948"},"id":1}],"lastModifiedDate":"2013-05-22T15:31:01","indexId":"cir45","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1949","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"45","title":"Index of surface-water records, part 9, Colorado River basin, to September 30, 1948","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir45","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1949, Index of surface-water records, part 9, Colorado River basin, to September 30, 1948: U.S. Geological Survey Circular 45, 20 p. ;27 cm., https://doi.org/10.3133/cir45.","productDescription":"20 p. ;27 cm.","costCenters":[],"links":[{"id":139674,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/0045/report-thumb.jpg"},{"id":272577,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/0045/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f2925","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":528147,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":4762,"text":"wsp1073 - 1949 - Water levels and artesian pressure in observation wells in the United States, 1946, Part 3, North-Central States","interactions":[],"lastModifiedDate":"2012-02-02T00:05:52","indexId":"wsp1073","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1949","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":"1073","title":"Water levels and artesian pressure in observation wells in the United States, 1946, Part 3, North-Central States","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1073","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1949, Water levels and artesian pressure in observation wells in the United States, 1946, Part 3, North-Central States: U.S. Geological Survey Water Supply Paper 1073, vi, 366 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1073.","productDescription":"vi, 366 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":139795,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1073/report-thumb.jpg"},{"id":31744,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1073/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa031","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":528375,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":4337,"text":"cir46 - 1949 - Interpreting ground conditions from geologic maps","interactions":[],"lastModifiedDate":"2017-03-09T13:01:49","indexId":"cir46","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1949","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"46","title":"Interpreting ground conditions from geologic maps","docAbstract":"Intelligent planning for heavy construction, water supply, or other land utilization requires advance knowledge of ground conditions in the area. It is essential to know:
These elements usually are considered in planning land developments that involve much investment; detailed surveys generally are made of the topography, geology, soils, and hydrology at the site selected for development. Such detailed surveys are essential, but equally essential and often overlooked is the need for general surveys prior to site selection.
Only if the general surveys have been made is it possible to know that a particular site is most suitable for the purpose and that no situations in the tributary areas that might affect the project have been overlooked. Moreover, the general regional relations must be known in order to properly interpret the geology, soils, and hydrology at a particular locality. In brief, both the general and the specific are needed in order to avoid costly mistakes either during or after development.
The accompanying maps illustrate how a general geologic map can be used for interpreting grc .d conditions during a planning stage prior to site selection. The topographic and geologic maps, which provide the basic data, have been simplified from some existing ones. The interpretive sheets are intended to provide some examples of the kinds of information that trained persons can read from such basic maps.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/cir46","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1949, Interpreting ground conditions from geologic maps: U.S. Geological Survey Circular 46, 14 p., https://doi.org/10.3133/cir46.","productDescription":"14 p.","costCenters":[],"links":[{"id":117674,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1949/0046/report-thumb.jpg"},{"id":31447,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1949/0046/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d9e4b07f02db5dfeb5","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":528193,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3906,"text":"cir44 - 1949 - Large rivers of the United States","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"cir44","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1949","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"44","title":"Large rivers of the United States","language":"ENGLISH","publisher":"[U.S. Geological Survey],","doi":"10.3133/cir44","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1949, Large rivers of the United States: U.S. Geological Survey Circular 44, 5 p. :illus., map. ;27cm., https://doi.org/10.3133/cir44.","productDescription":"5 p. :illus., map. ;27cm.","costCenters":[],"links":[{"id":117118,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1949/0044/report-thumb.jpg"},{"id":30993,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1949/0044/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a90aa","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":528154,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}