{"pageNumber":"2632","pageRowStart":"65775","pageSize":"25","recordCount":68827,"records":[{"id":70216231,"text":"70216231 - 1956 - Silica in hot-spring waters","interactions":[],"lastModifiedDate":"2020-11-10T18:19:37.894704","indexId":"70216231","displayToPublicDate":"1956-11-10T12:10:07","publicationYear":"1956","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":"Silica in hot-spring waters","docAbstract":"<p>The silica in hot-spring waters and in a few cold waters was studied by moans of the colorimetrie ammonium-molybdate method of analysis.<span>&nbsp;</span><span class=\"small-caps\">Murata</span><span>&nbsp;</span>found in 1947 that only a part of the total silica in aged samples of high-silica waters was determinable by the colorimetric method.<span>&nbsp;</span><span class=\"small-caps\">Weitz</span>,<span>&nbsp;</span><span class=\"small-caps\">franck</span><span>&nbsp;</span>And<span>&nbsp;</span><span class=\"small-caps\">schuchard</span><span>&nbsp;</span>later showed that ammonium molybdate reacts readily with the monomeric form of silica (probably H<sub>4</sub>SiO<sub>4</sub>) but very slowly with polymeric silica. If the colorimetric measurement is completed in two or three minutes, only the monomer is determined.</p><p>Nearly all silica of hot springs is in the monomeric form. Solubility equilibrium exists between dissolved (monomeric) and amorphous silica. For the hot springs that were studied, the solubility is about 315 p.p.m. at 90°C and 110 p.p.m. at 25°C, which is very similar to<span>&nbsp;</span><span class=\"small-caps\">Krauskopf's</span><span>&nbsp;</span>experimental data.</p><p>Monomeric silica polymerizes so slowly to colloidal silica that many waters are supersaturated with respect to amorphous silica. The rate of polymerization is influenced by pH, temperature, degree of supersaturation, presence of previously formed colloidal and gelatinous silica and contact with opal and other substances. Supersaturated acid waters and alkaline waters with less than 100% supersaturation tend to remain supersaturated almost indefinitely, with little or no change. Precipitation of colloidal silica is favoured by high temperature and contact with opal.</p><p>Many connate and other ground waters, including some thermal springs, are much below saturation with respect to amorphous silica, probably because low-solubility quartz and chalcedony have been precipitating.</p><p>Quartz is favoured by relatively high temperature, slow rale of precipitation, and low degree of supersaturation, and is believed to form by deposition of monomeric molecules. Chalcedony is probably deposited when the degree of supersaturation is moderately high and the rate of deposition is relatively fast. The ranges of temperature over which quartz and chalcedony deposit no doubt overlap, but, if other factors are equal, quartz is favoured by high temperature.</p><p>Opal is favoured by relatively low temperature and rapid rate of precipitation. Although opal has probably been deposited at temperatures as high as 140°C, it is unstable and is slowly converted to chalcedony or quartz. Water that is saturated with respect to opal is highly supersaturated with respect to quartz. Opal is probably formed from monomeric or more probably, the smaller polymeric molecules of silica, retaining some of their water content. Evidence is lacking for the direct conversion of gelatinous silica to opal. Some differences in solubility probably exist between amorphous opal and opal that shows X-ray patterns like that of cristobalite.</p><p>The suggestion is made that clay minerals form by combination of monomeric silica and a comparable form of monomeric alumina, which must have very low solubility in waters within the pH range of 5 to 9. Because of the abundance and relatively high solubility of silica, the proposed reaction, dissolved alumina + dissolved silica ⇌ clay, is ordinarily displaced strongly to the right in hydrothermal alteration and in ordinary soil formation. With removal of free silica, aided by tropical rainfall and temperatures, the reaction may be displaced to the left by dissolution and removal of silica from the system. Alumina, because of its very low solubility, remains as bauxite.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(56)90010-2","usgsCitation":"White, D.E., Brannock, W.W., and Murata, K.J., 1956, Silica in hot-spring waters: Geochimica et Cosmochimica Acta, v. 10, no. 1-2, p. 27-29, https://doi.org/10.1016/0016-7037(56)90010-2.","productDescription":"33 p.","startPage":"27","endPage":"29","costCenters":[],"links":[{"id":380362,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"White, Donald E.","contributorId":76787,"corporation":false,"usgs":true,"family":"White","given":"Donald","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":804516,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brannock, W. W.","contributorId":74504,"corporation":false,"usgs":true,"family":"Brannock","given":"W.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":804517,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Murata, K. J.","contributorId":18759,"corporation":false,"usgs":true,"family":"Murata","given":"K.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":804518,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70216189,"text":"70216189 - 1956 - Water for nuclear engineering","interactions":[],"lastModifiedDate":"2020-11-09T20:51:59.543932","indexId":"70216189","displayToPublicDate":"1956-11-09T14:49:19","publicationYear":"1956","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1986,"text":"Industrial and Engineering Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Water for nuclear engineering","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"ACS Publications","doi":"10.1021/ie50560a022","usgsCitation":"Love, S.K., and White, W.F., 1956, Water for nuclear engineering: Industrial and Engineering Chemistry, v. 48, no. 8, p. 1248-1251, https://doi.org/10.1021/ie50560a022.","productDescription":"4 p.","startPage":"1248","endPage":"1251","costCenters":[],"links":[{"id":380313,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"48","issue":"8","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":804433,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"White, W. F.","contributorId":80259,"corporation":false,"usgs":true,"family":"White","given":"W.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":804434,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1000474,"text":"1000474 - 1956 - The solubility of 3-bromo-4-nitrophenol in water and acetone","interactions":[],"lastModifiedDate":"2023-12-19T14:19:58.196315","indexId":"1000474","displayToPublicDate":"1956-10-01T00:00:00","publicationYear":"1956","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1465,"text":"Ecology","active":true,"publicationSubtype":{"id":10}},"title":"The solubility of 3-bromo-4-nitrophenol in water and acetone","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Ecological Society of America","doi":"10.2307/1933075","usgsCitation":"Willeford, B., 1956, The solubility of 3-bromo-4-nitrophenol in water and acetone: Ecology, v. 37, no. 4, p. 840-840, https://doi.org/10.2307/1933075.","productDescription":"1 p.","startPage":"840","endPage":"840","numberOfPages":"1","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":130316,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"37","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db6360c7","contributors":{"authors":[{"text":"Willeford, B.R. Jr.","contributorId":79426,"corporation":false,"usgs":true,"family":"Willeford","given":"B.R.","suffix":"Jr.","affiliations":[],"preferred":false,"id":308598,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010476,"text":"70010476 - 1956 - Method of preparing radioactive cations for tracing ground water","interactions":[],"lastModifiedDate":"2026-03-02T15:59:52.013567","indexId":"70010476","displayToPublicDate":"1956-08-31T00:00:00","publicationYear":"1956","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Method of preparing radioactive cations for tracing ground water","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.124.3218.402.a","issn":"00368075","usgsCitation":"Lacey, W., and De Laguna, W., 1956, Method of preparing radioactive cations for tracing ground water: Science, v. 124, no. 3218, p. 402-402, https://doi.org/10.1126/science.124.3218.402.a.","productDescription":"1 p.","startPage":"402","endPage":"402","costCenters":[],"links":[{"id":219145,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"124","issue":"3218","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5560e4b0c8380cd6d1cb","contributors":{"authors":[{"text":"Lacey, W.J.","contributorId":74875,"corporation":false,"usgs":true,"family":"Lacey","given":"W.J.","email":"","affiliations":[],"preferred":false,"id":359008,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"De Laguna, W.","contributorId":53941,"corporation":false,"usgs":true,"family":"De Laguna","given":"W.","affiliations":[],"preferred":false,"id":359007,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70170998,"text":"70170998 - 1956 - Relationships between the chemistry of Minnesota surface waters and wildlife management","interactions":[],"lastModifiedDate":"2018-03-19T10:27:29","indexId":"70170998","displayToPublicDate":"1956-08-01T10:30:00","publicationYear":"1956","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Relationships between the chemistry of Minnesota surface waters and wildlife management","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Wildlife Society","publisherLocation":"Washington, D.C.","doi":"10.2307/3796967","usgsCitation":"Moyle, J., 1956, Relationships between the chemistry of Minnesota surface waters and wildlife management: Journal of Wildlife Management, v. 20, no. 3, p. 303-320, 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 \"}}]}","volume":"20","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"574d6640e4b07e28b6684d5f","contributors":{"authors":[{"text":"Moyle, J.B.","contributorId":54323,"corporation":false,"usgs":true,"family":"Moyle","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":629417,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70048375,"text":"tei624 - 1956 - Uranium content of ground and surface waters in western Kansas, eastern Colorado, and the Oklahoma Panhande","interactions":[],"lastModifiedDate":"2013-11-22T09:25:50","indexId":"tei624","displayToPublicDate":"1956-01-10T11:43:00","publicationYear":"1956","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"624","title":"Uranium content of ground and surface waters in western Kansas, eastern Colorado, and the Oklahoma Panhande","docAbstract":"During 1954, 1955, and 1956, 324 water samples were collected in western Kansas, eastern Colorado, the Oklahoma Panhandle, and northeastern New Mexico, to determine the uranium content of water from the various rock units and geologic terranes in the region, and to locate areas in which, large amounts of uranium in the water might reflect the presence of nearby uranium accumulations. Three geologic terranes are present in the report area: the Tertiary-Quaternary tuff ace o us terrane, the Upper Cretaceous shale terrane, and the upper Permian through Lower Cretaceous sandstone terrane. The average uranium content of 179 water samples from the tuffaceous terrane, which is composed primarily of tuffaceous, fluviatile rocks ranging in age from Pliocene to Pleistocene, is 6.7 parts per billion. A total of 48 samples from the Upper Cretaceous shale terrane, which is composed almost entirely\nof shale and limestone of marine origin, contain an average of 20.4 parts per billion uranium , Sandstone, silt stone, and clay stone of terrestrial and near-shore marine origin are the predominant constituents of the upper Permian through Lower Cretaceous sandstone terrane, and the 83 water samples collected from, or related to, rock units of this terrane contain an average of 10.2 parts per billion uranium. The average uranium content figure derived for the tipper Cretaceous shale terrane may not be representative of the uranium content of waters from this terrane throughout the report area because more than half of the samples assigned to the terrane were collected in an area in which most water samples contain relatively large amounts of uranium. Compared to the shale terrane, the tuffaceous terrane and the sandstone terrane are both represented by a greater number of samples collected over a much larger area and the average uranium content figures derived for them are believed to be representative of the uranium content of waters from, or related to, rock units of the two terranes in the report area. The average uranium content figures derived for different rock units, or groups of rock units, subdivided by the source type from which the samples were collected (well, spring, stream, municipal water system, reservoir, or lake), and in some cases by geographic parts of the report area, are believed to be of more potential use in any future hydrogeochemical exploration in the area than are the average uranium content figures derived for the three geologic terranes. The average uranium content of ground-water samples from 12 individual rock units or groups of rock units ranges from less than 1. 0 to 38 parts per billion. Several rock units were sampled over large enough areas to indicate that waters from the same rock unit in different parts of the report area may range widely in average uranium content. Water samples from some of the rock units in the area, particularly those of Triassic and Permian age, contain large amounts of uranium,\nand in some parts of the report area, such as the Cimarron River area of westernmost Oklahoma and northeastern New Mexico, and the Rule Creek area in Bent and Las Animas Counties, Colo. , most, or all, of the water samples collected contain relatively large amounts of uranium. Further exploration to determine the source of the uranium in the water from these rock units and areas may be worthwhile.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei624","collaboration":"Prepared in cooperation with the U.S. Atomic Energy Commission","usgsCitation":"Landis, E., 1956, Uranium content of ground and surface waters in western Kansas, eastern Colorado, and the Oklahoma Panhande: U.S. Geological Survey Trace Elements Investigations 624, Report: 73 p.; Plate 1: 33.36 inches x 23.81 inches, https://doi.org/10.3133/tei624.","productDescription":"Report: 73 p.; Plate 1: 33.36 inches x 23.81 inches","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278037,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/624/report-thumb.jpg"},{"id":279537,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/624/plate-1.pdf"},{"id":279536,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/624/report.pdf"}],"country":"United States","state":"Colorado;Kansas;New Mexico;Oklahoma","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104.62,36.13 ], [ -104.62,40.11 ], [ -99.47,40.11 ], [ -99.47,36.13 ], [ -104.62,36.13 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5242b466e4b096ee62464206","contributors":{"authors":[{"text":"Landis, E.R.","contributorId":40605,"corporation":false,"usgs":true,"family":"Landis","given":"E.R.","email":"","affiliations":[],"preferred":false,"id":484476,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5220815,"text":"5220815 - 1956 - Validity of mail survey data on bagged waterfowl","interactions":[],"lastModifiedDate":"2025-01-31T17:00:50.840908","indexId":"5220815","displayToPublicDate":"1956-01-02T00:00:00","publicationYear":"1956","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Validity of mail survey data on bagged waterfowl","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Wiley","doi":"10.2307/3797241","usgsCitation":"Atwood, E.L., 1956, Validity of mail survey data on bagged waterfowl: Journal of Wildlife Management, v. 20, no. 1, p. 1-16, https://doi.org/10.2307/3797241.","productDescription":"16 p.","startPage":"1","endPage":"16","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":194015,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California, 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L.","contributorId":43870,"corporation":false,"usgs":false,"family":"Atwood","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":332546,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70048448,"text":"tem568 - 1956 - Alteration of sandstone as a guide to uranium deposits and their origin, northern Black Hills, South Dakota","interactions":[],"lastModifiedDate":"2014-03-04T13:44:58","indexId":"tem568","displayToPublicDate":"1956-01-01T14:56:00","publicationYear":"1956","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":"568","title":"Alteration of sandstone as a guide to uranium deposits and their origin, northern Black Hills, South Dakota","docAbstract":"Several uranium deposits are present in the Fall River sandstone of Early Cretaceous age on the northeast flank of the Black Hills, Butte County, South Dakota.  The deposits are within a fine-grained, well-sorted, persistent basal sandstone unit that ranges in thickness from 2 to 18 feet and dips about 4&deg; NE. Detailed mapping of about 2 square miles surrounding the deposits have shown that all the uranium occurrences and most of the areas of high radioactivity are where the color changes in the basal sandstone from reddish on the up-dip side of the the occurrences to yellowish-gray or buff down-dip. Radioactivity measurements show that uranium is distributed almost continuously along the sinuous red-buff contact for more than 5 miles. Laboratory work indicates that the red color is caused by the hematite resulting from the alteration of ferrous iron minerals and hydrous ferric oxides. The close association of the red-buff contact and the uranium deposits suggest that the two were formed by the same solutions. The uranium was probably deposited originally from ground water which moved down-dip and gradually changed from an oxidizing solution near the surface to a mildly reducing solution at depth. Concentrations of uranium have resulted from the localization of reducing conditions cause perhaps by structures superimposed on the regional dip, local thinning or decrease in permeability of the sandstone, or concentrations of pyritiferous carbonaceous material. The red alteration is probably the result of pre-Oligocene weathering that has extended downward in the more permeable beds about 200 feet below the ancient erosion surface. Oxidation of the primary uranium during the present weathering cycle has resulted in the formation of carnotite and possibly other secondary uranium minerals.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem568","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Vickers, R., 1956, Alteration of sandstone as a guide to uranium deposits and their origin, northern Black Hills, South Dakota: U.S. Geological Survey Trace Elements Memorandum 568, Report: 24 p.; 1 Plate: 23.97 x 19.67 inches, https://doi.org/10.3133/tem568.","productDescription":"Report: 24 p.; 1 Plate: 23.97 x 19.67 inches","numberOfPages":"27","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278154,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0568/report-thumb.jpg"},{"id":283256,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0568/report.pdf"},{"id":283255,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0568/plate-3.pdf"}],"country":"United States","state":"South Dakota","county":"Butte County","otherGeospatial":"Black Hills","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104.0577,45.2143 ], [ -104.0577,44.5709 ], [ -102.9576,44.5709 ], [ -102.9576,45.2143 ], [ -104.0577,45.2143 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52455762e4b0b3d37307e16b","contributors":{"authors":[{"text":"Vickers, R.C.","contributorId":50583,"corporation":false,"usgs":true,"family":"Vickers","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":484679,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71639,"text":"tei619 - 1956 - The physical behavior and geologic control of radon in mountain streams","interactions":[],"lastModifiedDate":"2014-07-15T07:20:31","indexId":"tei619","displayToPublicDate":"1956-01-01T10:39:00","publicationYear":"1956","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"619","title":"The physical behavior and geologic control of radon in mountain streams","docAbstract":"<p>Radon measurement were made in several small, turbulent mountain streams in the Wasatch Mountains near Salt Lake City and Ogden, Utah, to determine the relationship between the distribution of radon and its geologic environment.</p>\n<br>\n<p>In this area, the distribution of radon in streams can be sued to locate points where relatively large amounts of radon-bearing ground water enter the stream, although other evidence of spring activity may be lacking. These points of influence ground water are marked by abrupt increases (as much as two orders of magnitude within a distance of 50 feet) in the radon content of the stream waters.</p>\n<br>\n<p>The excess radon in the stream water is then rapidly lost to the atmosphere through stream turbulence. The rate of radon dissipation is an exponential function, of different slopes, with respect to distance of streamflow, and depend upon the rate and volume of streamflow, and the gradient and nature of the stream channel.</p>\n<br>\n<p>The higher radon concentration can be generally related to specific stratigraphic horizons in several different drainage area. Thus, lithologic units which act as the primary aquifers can be identifies. In one area, thrust faults were found to control he influx of ground water into the stream.</p>\n<br>\n<p>Estimates, based on radon concentration in stream and related spring waters, can also be made of the major increments of addition of ground water to streamflow where conventional methods such as stream gaging are not practical.</p>\n<br>\n<p>The radon in the waters studied was found to be almost completely unsupported by radium in solution.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei619","collaboration":"This report concerns work done on behalf of the Division of Research of the U.S. Atomic Energy Commission","usgsCitation":"Rogers, A., 1956, The physical behavior and geologic control of radon in mountain streams: U.S. Geological Survey Trace Elements Investigations 619, 44 p., https://doi.org/10.3133/tei619.","productDescription":"44 p.","numberOfPages":"45","costCenters":[],"links":[{"id":290055,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":290054,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0619/report.pdf"}],"country":"United States","state":"Utah","city":"Ogden;Salt Lake City","otherGeospatial":"Wasatch Mountains","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.151,40.5021 ], [ -112.151,41.3868 ], [ -111.2973,41.3868 ], [ -111.2973,40.5021 ], [ -112.151,40.5021 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53a94c87e4b0f1f8e2fa8681","contributors":{"authors":[{"text":"Rogers, Allen S.","contributorId":66553,"corporation":false,"usgs":true,"family":"Rogers","given":"Allen S.","affiliations":[],"preferred":false,"id":284525,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2618,"text":"wsp1360B - 1956 - Ground water in northeastern Louisville, Kentucky with reference to induced infiltration","interactions":[],"lastModifiedDate":"2024-11-27T15:31:54.450981","indexId":"wsp1360B","displayToPublicDate":"1956-01-01T07:00:00","publicationYear":"1956","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":"1360","chapter":"B","title":"Ground water in northeastern Louisville, Kentucky with reference to induced infiltration","docAbstract":"<p>In cooperation with the city of Louisville, Ky., the U. S. Geological Survey made a detailed investigation during the period February 1945 to March 1947 of the ground-water resources of a 3-square-mile area along the Ohio River north-east of Louisville. Test drilling shows that the principal aquifer consists of about 80 feet of glacial-outwash sands and gravels lying in an old river channel which was cut into rocks of Ordovician, Silurian, and Devonian age.</p><p>The total ground-water storage in the area is estimated as 7 billion gallons. The ground-water levels are affected by changes in river elevation, by rainfall, and by the effects of pumping in the downtown part of Louisville 3 miles to the southwest. In the northeastern part of the area the flow of ground water, as defined by contour maps, is toward the river, and in the southwestern part of the area it is from the river toward the downtown area of overpumping.</p><p>Ground water in the area has an average temperature of 56° F. The water, which is moderately hard, is suitable for domestic and industrial uses.</p><p>Analysis of a pumping test made during the investigation proves that infiltration supplies can be developed. Studies to determine the degree of connection between the river and aquifer were made on the basis of chemical analyses, sections showing temperature distribution in the aquifer during the pumping test, shapes of water-level profiles in the test area, and shapes of time-drawdown curves for a number of observation wells. Quantitative studies to evaluate the hydrologic constants of the aquifer were made by both graphical and mathematical methods. The transmissibility was determined as 121,000 gpd/ft in the test area; the distance to the line source, 400 feet; and the coefficient of storage, 0.0003. A comparison of river-level fluctuations and water-level fluctuations in observation wells shows that conditions along the 6.4-mile reach of river are not greatly different from those at the site of the pumping test.</p><p>It is estimated that under adverse temperature and river-stage conditions infiltration supplies could be developed to the extent of 280 million gpd in the entire 6.4-mile reach investigated; at average river-water temperature (59° F) about 400 million gpd could be developed. Diagrams were drawn showing the estimated yield of wells of different radii, at various distances from the river, and at various spacings. In making the computations allowance was made for screen losses, dewatering of the aquifer, partial penetration of wells, location wells, eccentricity of large wells, and interference among wells.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1360B","collaboration":"Prepared in cooperation with the city of Louisville","usgsCitation":"Rorabaugh, M.I., 1956, Ground water in northeastern Louisville, Kentucky with reference to induced infiltration: U.S. Geological Survey Water Supply Paper 1360, Report: v, 69 p.; 17 Plates: 8 x 23.81 inches or smaller, https://doi.org/10.3133/wsp1360B.","productDescription":"Report: v, 69 p.; 17 Plates: 8 x 23.81 inches or smaller","startPage":"101","endPage":"169","numberOfPages":"73","costCenters":[],"links":[{"id":416093,"rank":20,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24337.htm","linkFileType":{"id":5,"text":"html"}},{"id":28927,"rank":19,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360b/plate-17.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28926,"rank":18,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360b/plate-16.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28925,"rank":17,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360b/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28924,"rank":16,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360b/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28923,"rank":15,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360b/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138850,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1360b/report-thumb.jpg"},{"id":28917,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360b/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28916,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360b/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28914,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360b/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28911,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360b/plate-18.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28920,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360b/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":279835,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1360b/report.pdf"},{"id":28912,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360b/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28913,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360b/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28915,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360b/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28918,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360b/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28919,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360b/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28921,"rank":13,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360b/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28922,"rank":14,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360b/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Kentucky","city":"Louisville","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -85.948441,37.9971 ], [ -85.948441,38.38051 ], [ -85.4051,38.38051 ], [ -85.4051,37.9971 ], [ -85.948441,37.9971 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66db38","contributors":{"authors":[{"text":"Rorabaugh, M. I.","contributorId":28221,"corporation":false,"usgs":true,"family":"Rorabaugh","given":"M.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":145505,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70185477,"text":"70185477 - 1956 - Floods in relation to the river channel","interactions":[],"lastModifiedDate":"2017-03-22T13:39:11","indexId":"70185477","displayToPublicDate":"1956-01-01T00:00:00","publicationYear":"1956","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5272,"text":"Proceedings of the International Association of Hydrological Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Floods in relation to the river channel","docAbstract":"<p>Among the rivers studied by us two broad types may be distinguished. Channels in the semi-arid areas scour at high discharges so that the bed lowers nearly as much as the water surface rises. Detailed data on the middle reaches of the Rio Grande in New Mexico during the spring floods of 1948 and 1952 indicate that the bed aggrades to nearly its pre-flood level as the flood recedes. Channel banks may move rapidly by undercutting during periods of scour and levees are liable to failure not from overtopping but by undercutting.</p><p>In Connecticut, a sub-humid area, the repetitive processes of scour and fill in the semi-arid region were not demonstrated by the great floods of 1955. In a few reaches fresh sand was deposited over gravel beds subsequently to be removed by lower flows. Boulders four to six feet in diameter were moved in places over undisturbed beds of one-inch gravel. Channel widening occurred primarily in rivers in narrow valleys which confined the flow within the channel. Scour and deposition on flood plains adjacent to the rivers was irregular. Most deposits could be traced to local sources. In general, flood waters modified but did not vastly alter the prevailing configuration of the channel and structure of the flood plain.</p>","conferenceTitle":"Symposium Darcy: Floods","conferenceDate":"September 20-26, 1956","conferenceLocation":"Dijon, France","language":"English","publisher":"International Association of Hydrological Sciences","usgsCitation":"Leopold, L.B., and Wolman, M.G., 1956, Floods in relation to the river channel: Proceedings of the International Association of Hydrological Sciences, p. 85-98.","productDescription":"14 p.","startPage":"85","endPage":"98","costCenters":[],"links":[{"id":338073,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":338071,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://iahs.info/Publications-News/","text":"Publisher's Website","linkHelpText":"Back issues of this publication are available using the search function"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d38d66e4b0236b68f98f9c","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":685683,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wolman, M. Gordon","contributorId":85163,"corporation":false,"usgs":true,"family":"Wolman","given":"M.","email":"","middleInitial":"Gordon","affiliations":[],"preferred":false,"id":685684,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70185489,"text":"70185489 - 1956 - Land use and sediment yield","interactions":[],"lastModifiedDate":"2017-03-22T14:22:18","indexId":"70185489","displayToPublicDate":"1956-01-01T00:00:00","publicationYear":"1956","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Land use and sediment yield","docAbstract":"<p>When the vegetal cover is removed from a land surface, the rate of removal of the soil material, at least initially, increases rapidly. So well known is this principle that it hardly needs restatement.</p><p>If attention is focused on any individual drainage basin in its natural state, large or small, and inquiry is made as to the rate of denudation, a quantitative answer is not easily obtained. The possible error in any computation of rate of sediment production from any given drainage basin is considerable. Significant variations are found in sediment yields from closely adjacent watersheds which appear to be generally similar. To make a quantitative evaluation of the change in the rate of denudation when the natural vegetation is disturbed is, therefore, even more difficult. Considering the fact that \"soil conservation\" has been promoted to the status of a science, our lack of ability to answer what is apparently so simple a question may seem surprising. Let us look at some of the reasons.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Man’s role in changing the face of the Earth","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Man's role in changing the face of the Earth: Second annual Wenner-Gren Symposium","conferenceDate":"June 16-22, 1955","conferenceLocation":"Princeton, NJ","language":"English","publisher":"University of Chicago Press","publisherLocation":"Chicago, IL","usgsCitation":"Leopold, L.B., 1956, Land use and sediment yield, <i>in</i> Man’s role in changing the face of the Earth, Princeton, NJ, June 16-22, 1955, p. 639-647.","productDescription":"9 p.","startPage":"639","endPage":"647","costCenters":[],"links":[{"id":338086,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d38d66e4b0236b68f98f98","contributors":{"editors":[{"text":"Thomas, William L. Jr.","contributorId":189691,"corporation":false,"usgs":false,"family":"Thomas","given":"William","suffix":"Jr.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":685718,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":685717,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70185482,"text":"70185482 - 1956 - Data and understanding","interactions":[],"lastModifiedDate":"2017-03-22T14:03:02","indexId":"70185482","displayToPublicDate":"1956-01-01T00:00:00","publicationYear":"1956","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Data and understanding","docAbstract":"<p>In the year 1534 when Cabeza de Vaca escaped from the aborigines of southern Texas by whom he had been enslaved for six years, he made his way on foot from the vicinity of Galveston to the west coast of Mexico. Although his <i>Relación</i> was not printed until 1542, the verbal report of Cabeza de Vaca gave impetus to the growing interest in exploration of New Spain. Estevanico, the black, one of de Vaca's companions, served as guide to Fray Marcos de Niza on the first Spanish reconnaissance to reach the village of Zuni in New Mexico.</p><p>The earliest Spanish exploring parties hoped to find riches, but expected to acquire, at the least, facts. These \"gentlemen of high quality,\" as Castaneda called them, wanted to see for themselves whether the cities of Cibola had streets of silver. Hearsay was not enough. Rumor was to be replaced by first-hand knowledge.</p><p>Without discounting the hope for personal gain, these men presumably were fired with some further intellectual and spiritual motivation, among which must have been the desire for facts about these parts where we are assembled. Inscription Rock, only a few miles west of Albuquerque, bears illuminating tidbits of history. Don Diego de Vargas, says the carved inscription of 1692, came here \"A su costa\"—at his own expense.</p><p>We are attempting to survey and correlate some of the facts which people have gained about the nature of semi-arid lands. We are better off than the early Spanish explorers, for in the intervening period data and information have been accumulated in scope and in detail beyond the imagination of our predecessors. We have available excellent maps, knowledge of the soils and of the rocks, both at the surface and below the ground, measurements of precipitation, descriptions of the vegetation, data on the flow of streams, experience in the use, if not the husbandry, of the land.</p><p>It is true that for the purposes of our complex civilization, the need for additional data has far outstripped the programs of fact-finding. But it appears that an indefinite expansion of the collection of routine measurements would still leave something lacking. I draw the distinction between measurement data and understanding; between the collection of facts and knowledge of processes and interrelationships. Although we have a wealth of data, our understanding of the semi-arid environment is poor.</p><p>Understanding the physical and biologic processes operating in an environment is important for living in and with the land. As an example, let us look briefly at the interrelation of the water and sediment in ephemeral streams, and the problem of valley trenching or arroyo cutting.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"The future of arid lands: Papers and recommendations from the International Arid Lands Meetings","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"International Arid Lands Meetings","conferenceDate":"April 26 - May 4, 1955","conferenceLocation":"Albuquerque, NM","language":"English","publisher":"American Association for the Advancement of Science","publisherLocation":"Washington, D.C.","doi":"10.1002/aic.690030425","usgsCitation":"Leopold, L.B., 1956, Data and understanding, <i>in</i> The future of arid lands: Papers and recommendations from the International Arid Lands Meetings, v. 43, Albuquerque, NM, April 26 - May 4, 1955, p. 114-120, https://doi.org/10.1002/aic.690030425.","productDescription":"7 p.","startPage":"114","endPage":"120","costCenters":[],"links":[{"id":338080,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"43","noUsgsAuthors":false,"publicationDate":"2004-06-17","publicationStatus":"PW","scienceBaseUri":"58d38d66e4b0236b68f98f9a","contributors":{"editors":[{"text":"White, Gilbert F.","contributorId":189688,"corporation":false,"usgs":false,"family":"White","given":"Gilbert","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":685700,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":685699,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1000372,"text":"1000372 - 1956 - Life history of lake herring of Green Bay, Lake Michigan","interactions":[],"lastModifiedDate":"2012-03-02T17:16:05","indexId":"1000372","displayToPublicDate":"1956-01-01T00:00:00","publicationYear":"1956","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1663,"text":"Fishery Bulletin","printIssn":"0090-0656","active":true,"publicationSubtype":{"id":10}},"title":"Life history of lake herring of Green Bay, Lake Michigan","docAbstract":"Although the lake herring has been an important contributor to the commercial fish production of Green Bay, little has been known about it.  This study is based on field observations and data from about 6,500 lake herring collected over the period 1948 to 1952. Relatively nonselective commercial pound nets were a primary source of material for the study of age and growth. Commercial and experimental gill nets were used to obtain data on gear selectivity and vertical distribution.  Scales were employed to investigate age and growth. Age group IV normally dominated commercial catches during the first half of the calendar year and age group III the last half. At these ages the fish averaged about 10.5 inches in length. The season's growth started in May, was most rapid in July, and terminated near the end of October. The sexes grew at the same rate. Selectivity of fishing gear was found to influence the estimation of growth. Geographical and annual differences in growth are shown. Factors that might contribute to discrepancies in calculated growth are evaluated. Possible real and apparent causes of growth compensation are given. The relation between length and weight is shown to vary with sex, season, year, and method of capture.  Females were relatively more plentiful in commercial catches in February than in May through December. The percentage of females decreased with increase in age in pound-net catches but increased with age in gill-net samples. Within a year class the percentage of females decreased with increase in age.  Most Green Bay lake herring mature during their second or third year of life. They are pelagic spawners with most intensive spawning over shallow areas. Spawning takes place between mid-November and mid-December, and eggs hatch in April and May. Lake herring ovaries contained from 3,500 to 11,200 eggs (averaged 6,375). Progress of spawning by age, sex, and length is given.  Lake herring were distributed at all depths in Green Bay in early May, were concentrated within 30 feet of the surface in late May, moved to deeper water in June, and were restricted to depths greater than 30 feet in July when temperatures in shallower water became unfavorably high (greater than 18A?C.). In October, lake herring were again at all depths but were most abundant near the surface.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Fishery Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"Out-of-print","usgsCitation":"Smith, S.H., 1956, Life history of lake herring of Green Bay, Lake Michigan: Fishery Bulletin, v. 109, p. 87-138.","productDescription":"p. 87-138","startPage":"87","endPage":"138","numberOfPages":"51","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":132962,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"109","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a539f","contributors":{"authors":[{"text":"Smith, Stanford H.","contributorId":86711,"corporation":false,"usgs":true,"family":"Smith","given":"Stanford","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":308476,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22946,"text":"ofr5641 - 1956 - Memorandum summarizing preliminary estimates of ground-water outflow from Bunker Hill Basin at Colton Narrows, San Bernardino County, California","interactions":[],"lastModifiedDate":"2024-12-11T21:39:33.039315","indexId":"ofr5641","displayToPublicDate":"1956-01-01T00:00:00","publicationYear":"1956","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":"56-41","title":"Memorandum summarizing preliminary estimates of ground-water outflow from Bunker Hill Basin at Colton Narrows, San Bernardino County, California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5641","usgsCitation":"Dutcher, L., 1956, Memorandum summarizing preliminary estimates of ground-water outflow from Bunker Hill Basin at Colton Narrows, San Bernardino County, California: U.S. Geological Survey Open-File Report 56-41, 14 p., https://doi.org/10.3133/ofr5641.","productDescription":"14 p.","costCenters":[],"links":[{"id":154301,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"California","county":"San Bernardino County","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ce4b07f02db61410d","contributors":{"authors":[{"text":"Dutcher, L.C.","contributorId":42191,"corporation":false,"usgs":true,"family":"Dutcher","given":"L.C.","email":"","affiliations":[],"preferred":false,"id":189174,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2515,"text":"wsp1109 - 1956 - Ground-water geology of the coastal zone, Long Beach-Santa Ana area, California","interactions":[],"lastModifiedDate":"2023-03-13T19:42:34.164567","indexId":"wsp1109","displayToPublicDate":"1956-01-01T00:00:00","publicationYear":"1956","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":"1109","title":"Ground-water geology of the coastal zone, Long Beach-Santa Ana area, California","docAbstract":"<p>This paper is the first chapter of a comprehensive report on the ground-water features in the southern part of the coastal plain in Los Angeles and Orange Counties, Calif., with special reference to the effectiveness of the so-called coastal barrier--the Newport-Inglewood structural zone--in restraining landwar,-1 movement of saline water. The coastal plain in Los Angeles and Orange Counties, which covers some 775 square miles, sustains a large urban and rural population, diverse industries, and intensive agricultural developments. The aggregate ground-water withdrawal in 1945 was about 400,000 acre-feet a year, an average of about 360 million gallons a day. The dominant land-form elements are a central lowland plain with tongues extending to the coast, bordering highlands and foothills, and a succession of low hills and mesas aligned northwestward along the coastal edge of the central low- land plain. These low hills and mesas are the land-surface expression of geologic structure in the Newport-Inglewood zone. The highland areas that border the inland edge of the coastal plain are of moderate altitude and relief; most of the ridge crests range from 1,400 to 2,500 feet in altitude, but Santiago Peak in the Santa Ana Mountains attains a height of 5,680 feet above sea level. From these highlands the land surface descends across foothills and aggraded alluvial aprons to the central lowland, Downey Plain, here defined as the surface formed by alluvial aggradation during the post-Pleistocene time of rising base level. The Newport-Inglewood belt of hills and plains (mesas) has a maximum relief of some 500 feet but is widely underlain at a depth of about 30 feet by a surface of marine plantation. As initially formed in late Pleistocene time that surface was largely a featureless plain. Thus the present land-surface forms within the Newport-Inglewood belt measure the earth deformation that has occurred there since late Pleistocene time and so are pertinent with respect to structural features that influence the watertightness of the so-called coastal barrier. The hills and mesas of the Newport-Inglewood belt are cut by six gaps through which tongues of the central lowland extend to the coast. The gaps are trenched in the deformed late Pleistocene surface and are floored with alluvium that is highly permeable in its lower part. The Long Beach-Santa Ana area, with which this report is concerned, encompasses the central and eastern segments of the coastal plain, and includes five of the gaps in succession from northwest to south- east: Dominguez, Alamitos, Sunset, Bolsa, and Santa Ana Gaps. In the Long Beach-Santa Ana area a thick sequence of Quaternary and Tertiary sedimentary rocks has been deposited on a basement of metamorphic and crystalline rocks of pre-Tertiary age. In the broad syncline underlying tl e central part of Downey Plain these sediments probably exceed 20,000 feet in thickness. This report pertains chiefly to the geology and water-bearing character of the rocks that underlie the coastal zone of the Long Beach-Santa Ana area. This area extends some 27 miles from Dominguez Hill on the northwest to Newport Beach on the southeast, has an average width of about 6 miles, includes some 180 square miles, and borders the Pacific Ocean. Of the Quaternary deposits the youngest are of Recent age and comprise silt, sand, gravel, and clay, chiefly of fluvial origin; they are the latest contributions to the alluvial cones of the Los Angeles, San Gabriel, and Santa Ana Rivers; their thickness is as much as 175 feet. The upper division of the Recent deposits, largely fine sand and silt of low permeability, commonly furnishes water only to a few wells of small yield; the lower division is coarse sand and gravel deposited chiefly in two tongues extending respectively, from Whittier Narrows through Dominguez Gap and from Santa Ana Canyon through Santa Ana Gap.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1109","usgsCitation":"Poland, J.F., and Piper, A.M., 1956, Ground-water geology of the coastal zone, Long Beach-Santa Ana area, California: U.S. Geological Survey Water Supply Paper 1109, Report: v, 162 p.; 8 Plates: 61.10 x 16.00 inches or smaller, https://doi.org/10.3133/wsp1109.","productDescription":"Report: v, 162 p.; 8 Plates: 61.10 x 16.00 inches or smaller","costCenters":[],"links":[{"id":414038,"rank":11,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25580.htm","linkFileType":{"id":5,"text":"html"}},{"id":28705,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1109/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28704,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1109/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28703,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1109/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28702,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1109/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28701,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1109/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28700,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1109/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28699,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1109/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28698,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1109/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28697,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1109/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138793,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1109/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Long Beach-Santa Ana area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -118.29,\n              33.875\n            ],\n            [\n              -118.29,\n              33.583\n            ],\n            [\n              -117.848,\n              33.583\n            ],\n            [\n              -117.848,\n              33.875\n            ],\n            [\n              -118.29,\n              33.875\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668d91","contributors":{"authors":[{"text":"Poland, J. F.","contributorId":64223,"corporation":false,"usgs":true,"family":"Poland","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":145325,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Piper, A. M.","contributorId":102865,"corporation":false,"usgs":true,"family":"Piper","given":"A.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":145326,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":95190,"text":"95190 - 1956 - Report on the problem of diseases in warm-water fish ponds, minnow hatcheries in particular (Mimeograph)","interactions":[],"lastModifiedDate":"2012-02-02T00:03:58","indexId":"95190","displayToPublicDate":"1956-01-01T00:00:00","publicationYear":"1956","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Report on the problem of diseases in warm-water fish ponds, minnow hatcheries in particular (Mimeograph)","docAbstract":"No abstract available at this time","language":"English","collaboration":"53/FH","usgsCitation":"Snieszko, S.F., 1956, Report on the problem of diseases in warm-water fish ponds, minnow hatcheries in particular (Mimeograph), 5 p.","productDescription":"5 p.","startPage":"5","numberOfPages":"5","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":128412,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ce4b07f02db613c1d","contributors":{"authors":[{"text":"Snieszko, S. F.","contributorId":13169,"corporation":false,"usgs":true,"family":"Snieszko","given":"S.","middleInitial":"F.","affiliations":[],"preferred":false,"id":298649,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70175983,"text":"70175983 - 1955 - Report of the Arkansas-White-Red Basins Inter-Agency Committee","interactions":[],"lastModifiedDate":"2016-08-23T10:53:51","indexId":"70175983","displayToPublicDate":"2016-08-23T00:00:00","publicationYear":"1955","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Report of the Arkansas-White-Red Basins Inter-Agency Committee","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70175983","usgsCitation":"U.S. Geological Survey, 1955, Report of the Arkansas-White-Red Basins Inter-Agency Committee, v. 2, no. 17, 122 p. , https://doi.org/10.3133/70175983.","productDescription":"122 p. ","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":327625,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"volume":"2","issue":"17","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bd659ae4b03fd6b7de7270","contributors":{"authors":[{"text":"U.S. Geological Survey","contributorId":152492,"corporation":true,"usgs":false,"organization":"U.S. Geological Survey","id":646754,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70175985,"text":"70175985 - 1955 - Ground-water resources of Osage County [Kansas]","interactions":[],"lastModifiedDate":"2016-08-23T11:07:56","indexId":"70175985","displayToPublicDate":"2016-01-11T00:00:00","publicationYear":"1955","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 resources of Osage County [Kansas]","language":"English","publisher":"University of Kansas","publisherLocation":"Lawrence, KS","usgsCitation":"O’Connor, H., 1955, Ground-water resources of Osage County [Kansas]: Kansas Geological Survey Bulletin, v. 13, no. 3, p. 28-49.","productDescription":"21 p. ","startPage":"28","endPage":"49","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":327629,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":327628,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.kgs.ku.edu/General/geologyBulls.html","linkHelpText":"http://www.kgs.ku.edu/General/geologyBulls.html"}],"volume":"13","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bd73dde4b03fd6b7df2d12","contributors":{"authors":[{"text":"O’Connor, H.G.","contributorId":173877,"corporation":false,"usgs":false,"family":"O’Connor","given":"H.G.","email":"","affiliations":[],"preferred":false,"id":646756,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70160577,"text":"70160577 - 1955 - A mycosis-like granuloma of fish","interactions":[],"lastModifiedDate":"2021-04-02T15:06:25.722348","indexId":"70160577","displayToPublicDate":"2015-12-23T00:00:00","publicationYear":"1955","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2353,"text":"Journal of Infectious Diseases","active":true,"publicationSubtype":{"id":10}},"title":"A mycosis-like granuloma of fish","docAbstract":"<p>Mycoses of systemic distribution are rarely observed in fresh-water fish in this country. In a recent review of atypical cell growths in fishes, Nigrelli cited the only known instance of a mycetoma in a North American fresh-water fish which occurred in the head of fingerling landlocked salmon from an Idaho hatchery. The fungus associated with this granuloma was characterized by a branching septate mycelium. Rucker reported a streptomycete which was pathogenic to blueblack salmon. This organism produced internal nodules containing masses of hyphae but no inflammatory response. A pathogenic fungus has been observed frequently in marine fish, however, and in both marine and fresh-water fish in Europe. This organism was tentatively classified as a Phycomycete in or near the order Chytridiales and was assigned to the genus and species <i>Ichthyophonus hoferi</i>, later reclassified as <i>Ichthyosporidium hoferi</i>. The graduloma described in this report occurs in fresh-water trout and is apparently caused by a budding, yeast-like form with no hyphae which evokes a tremendous inflammatory reaction. Morphologically, the organism does not resemble the previously described Ichthyosporidium. The lesions were first seen accidentally in sections prepared from a diplobacillus infection of brook trout termed &ldquo;kidney disease.&rdquo; Subsequently, the granuloma was observed in three widely separated infections involving the diplobacillus in each instance.<br />The histological material was received in a fixed condition; thus, no cultural data was available and the nomenclature and classification of the mycotic organism were not attempted. The present distribution of the disease, however, with its potential threat to domestic fish populations, seemed to warrant a description and discussion of the disease. Efforts are in progress to culture the organism.</p>","language":"English","publisher":"University of Chicago Press","publisherLocation":"Chicago","doi":"10.1093/infdis/97.3.262","usgsCitation":"Wood, E.M., Yasutake, W.T., and Lehman, W.L., 1955, A mycosis-like granuloma of fish: Journal of Infectious Diseases, v. 97, no. 3, p. 262-267, https://doi.org/10.1093/infdis/97.3.262.","productDescription":"6 p.","startPage":"262","endPage":"267","numberOfPages":"6","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":312788,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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,{"id":70175986,"text":"70175986 - 1955 - Geology and ground-water resources of Jewell County, Kansas","interactions":[],"lastModifiedDate":"2016-08-23T11:11:48","indexId":"70175986","displayToPublicDate":"2015-11-24T00:00:00","publicationYear":"1955","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 Jewell County, Kansas","language":"English","publisher":"University of Kansas","publisherLocation":"Lawrence, KS","usgsCitation":"Fishel, V., and Leonard, A., 1955, Geology and ground-water resources of Jewell County, Kansas: Kansas Geological Survey Bulletin, v. 115, 152 p.","productDescription":"152 p.","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":327633,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":327632,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.kgs.ku.edu/General/geologyBulls.html"}],"volume":"115","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bd73dae4b03fd6b7df2cd5","contributors":{"authors":[{"text":"Fishel, V.C.","contributorId":6126,"corporation":false,"usgs":true,"family":"Fishel","given":"V.C.","email":"","affiliations":[],"preferred":false,"id":646757,"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":646758,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70175984,"text":"70175984 - 1955 - Geology and ground-water resources of Graham County, Kansas","interactions":[],"lastModifiedDate":"2016-08-23T11:09:17","indexId":"70175984","displayToPublicDate":"2015-11-16T00:00:00","publicationYear":"1955","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 Graham County, Kansas","language":"English","publisher":"University of Kansas","publisherLocation":"Lawrence, KS","usgsCitation":"Prescott, G., 1955, Geology and ground-water resources of Graham County, Kansas: Kansas Geological Survey Bulletin, v. 110, 98 p.","productDescription":"98 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":327627,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":327631,"type":{"id":15,"text":"Index Page"},"url":"https://www.kgs.ku.edu/General/geologyBulls.html"}],"volume":"110","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bd73dae4b03fd6b7df2ccf","contributors":{"authors":[{"text":"Prescott, G.C. Jr.","contributorId":103352,"corporation":false,"usgs":true,"family":"Prescott","given":"G.C.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":646755,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70157478,"text":"70157478 - 1955 - Some effects of preciptiation on ground water in Wisconsin","interactions":[],"lastModifiedDate":"2018-01-08T19:52:04","indexId":"70157478","displayToPublicDate":"2015-04-06T08:00:00","publicationYear":"1955","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5596,"text":"Wisconsin Geological & Natural History Survey Information Circular","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"1","title":"Some effects of preciptiation on ground water in Wisconsin","docAbstract":"<p>The importance of our water supplies has become increasingly apparent to most of us in recent years. The importance of water was forcefully dramatized by the water shortage in New York City in 1950. In nearly every State in the Union, one or more communities now has or has had a water problem whose effect on the citizens has been no less to them as was the one in New York City to New Yorkers. The increasing numbers of these problems have led to widespread speculation as to the adequacy of the Nation' s water supplies.</p>","publisher":"Wisconsin Geological Survey","publisherLocation":"Madison, WI","collaboration":"Prepared in cooperation with the U.S. Geological Survey","usgsCitation":"Drescher, W.J., 1955, Some effects of preciptiation on ground water in Wisconsin: Wisconsin Geological & Natural History Survey Information Circular 1, 17 p.","productDescription":"17 p.","numberOfPages":"19","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":308500,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":350402,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://wgnhs.uwex.edu/pubs/ic01/"}],"country":"United 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,{"id":70046943,"text":"70046943 - 1955 - Interim report on the ground-water resources of Manatee County, Florida","interactions":[{"subject":{"id":51201,"text":"ofr534 - 1953 - A brief report on the progress of the Manatee County, Florida, ground-water investigation","indexId":"ofr534","publicationYear":"1953","noYear":false,"title":"A brief report on the progress of the Manatee County, Florida, ground-water investigation"},"predicate":"SUPERSEDED_BY","object":{"id":70046943,"text":"70046943 - 1955 - Interim report on the ground-water resources of Manatee County, Florida","indexId":"70046943","publicationYear":"1955","noYear":false,"title":"Interim report on the ground-water resources of Manatee County, Florida"},"id":1}],"lastModifiedDate":"2013-07-09T16:05:07","indexId":"70046943","displayToPublicDate":"2013-01-01T15:55:22","publicationYear":"1955","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":259,"text":"Information Circular","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"6","title":"Interim report on the ground-water resources of Manatee County, Florida","docAbstract":"Manatee County comprises an area of about 800 square miles adjacent to the Gulf of Mexico in the southwestern part of the Florida peninsula. The county is underlain at depths ranging from about 200 to 350 feet by a series of limestone formations of Tertiary age having a total thickness of several thousand feet. The upper part of the limestone section consists of the Ocala group of Eocene age, the Suwannee limestone of Oligocene age, and the Tampa formation of early Miocene age. These limestone formations are overlain by the Hawthorn formation of middle Miocene age which consists of interbedded clay, limestone, and sand. The Hawthorn is overlain by undifferentiated deposits of sand, limestone, and shell of Pliocene(?) and Pleistocene age that range in thickness from a few feet to about 75 feet.","language":"English","publisher":"Florida Geological Survey","publisherLocation":"Tallahassee, FL","collaboration":"Prepared by the Geological Survey, United States Department of the Interior in cooperation with the Florida Geological Survey the Board of County Commissioners of Manatee County and the Manatee River Soil Conservation District","usgsCitation":"Peek, H.M., and Anders, R.B., 1955, Interim report on the ground-water resources of Manatee County, Florida: Information Circular 6, 38 p.","productDescription":"38 p.","numberOfPages":"38","costCenters":[],"links":[{"id":274811,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70046943.png"},{"id":274810,"type":{"id":15,"text":"Index Page"},"url":"https://ufdc.ufl.edu/UF00001066/00001"}],"country":"United States","state":"Florida","county":"Manatee County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.823,27.2078 ], [ -82.823,27.6467 ], [ -82.0543,27.6467 ], [ -82.0543,27.2078 ], [ -82.823,27.2078 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51dd30ebe4b0f72b44719c8e","contributors":{"authors":[{"text":"Peek, Harry M.","contributorId":7599,"corporation":false,"usgs":true,"family":"Peek","given":"Harry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":480655,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anders, Robert B.","contributorId":44125,"corporation":false,"usgs":true,"family":"Anders","given":"Robert","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":480656,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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