{"pageNumber":"7057","pageRowStart":"176400","pageSize":"25","recordCount":185311,"records":[{"id":71244,"text":"tei172 - 1953 - Preliminary reconnaissance survey for thorium, uranium, and rare-earth oxides, Bear Lodge Mountains, Crook County, Wyoming","interactions":[],"lastModifiedDate":"2014-06-03T12:51:26","indexId":"tei172","displayToPublicDate":"1953-01-01T09:23:00","publicationYear":"1953","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":"172","title":"Preliminary reconnaissance survey for thorium, uranium, and rare-earth oxides, Bear Lodge Mountains, Crook County, Wyoming","docAbstract":"<p>An area about 6 miles north of Sundance, in the Bear Lodge Mountains, in Crook County, Wyo., was examined during August 1950 for thorium, uranium, and rare-earth oxides and samples were collected.</p>\n<br/>\n<p>Uranium is known to occur in fluorite veins and iron-manganese veins and in the igneous rocks of Tertiary age that compose the core of the Bear Lodge Mountains. The uranium content of the samples ranges from 0.001 to 0.015 percent in those from the fluorite veins, from 0.005 to 0.018 percent in those from the iron-manganese veins, and from 0.001 to 0.017 percent in those from the igneous rocks. The radioactivity of the samples is more than that expected from the uranium content. Thorium accounts for most of this discrepancy. The thorium oxide content of samples ranges from 0.07 to 0.25 percent in those from the iron-manganese veins and from 0.07 to 0.39 percent in those from the sedimentary rocks, and from0.04 to 0.30 in those from the igneous rocks.</p>\n<br/>\n<p>Rare-earth oxides occur in iron-manganese veins and in zones of altered igneous rocks. The veins contain from 0.16 to 12.99 percent rare-earth oxides, and the igneous rocks, except for two localities, contain from 0.01 to 0.42 percent rare-earth oxides. Inclusions of metamorphosed sedimentary rocks in the intrusive rocks contain from 0.07 to 2.01 percent rare-earth oxides.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei172","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Wilmarth, V., and Johnson, D.H., 1953, Preliminary reconnaissance survey for thorium, uranium, and rare-earth oxides, Bear Lodge Mountains, Crook County, Wyoming: U.S. Geological Survey Trace Elements Investigations 172, Report: 26 p.; 2 Plates: 30.99 x 29.34 inches and 15.10 x 20.60 inches, https://doi.org/10.3133/tei172.","productDescription":"Report: 26 p.; 2 Plates: 30.99 x 29.34 inches and 15.10 x 20.60 inches","numberOfPages":"26","costCenters":[],"links":[{"id":283504,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei172.jpg"},{"id":285601,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0172/figure-2.pdf"},{"id":285602,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0172/table-4.pdf"},{"id":285603,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0172/report.pdf"}],"country":"United States","state":"Wyoming","county":"Crook County","otherGeospatial":"Bear Lodge Mountains","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.0874,44.1791 ], [ -105.0874,45.0004 ], [ -104.0546,45.0004 ], [ -104.0546,44.1791 ], [ -105.0874,44.1791 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53559528e4b0120853e8c151","contributors":{"authors":[{"text":"Wilmarth, V.R.","contributorId":20803,"corporation":false,"usgs":true,"family":"Wilmarth","given":"V.R.","email":"","affiliations":[],"preferred":false,"id":283856,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, Douglas H. 0000-0002-7778-6641","orcid":"https://orcid.org/0000-0002-7778-6641","contributorId":70327,"corporation":false,"usgs":true,"family":"Johnson","given":"Douglas","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":283857,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70048603,"text":"tem644 - 1953 - Airborne radioactivity survey of parts of Atlantic Ocean beach, Virginia to Florida","interactions":[{"subject":{"id":70048603,"text":"tem644 - 1953 - Airborne radioactivity survey of parts of Atlantic Ocean beach, Virginia to Florida","indexId":"tem644","publicationYear":"1953","noYear":false,"title":"Airborne radioactivity survey of parts of Atlantic Ocean beach, Virginia to Florida"},"predicate":"SUPERSEDED_BY","object":{"id":51597,"text":"ofr53286 - 1953 - Radioactivity anomalies detected along parts of the Atlantic Ocean beach from Cape Henry, Virginia, to Cape Fear, North Carolina, and from Savannah Beach, Georgia, to Miami Beach, Florida","indexId":"ofr53286","publicationYear":"1953","noYear":false,"title":"Radioactivity anomalies detected along parts of the Atlantic Ocean beach from Cape Henry, Virginia, to Cape Fear, North Carolina, and from Savannah Beach, Georgia, to Miami Beach, Florida"},"id":1}],"supersededBy":{"id":51597,"text":"ofr53286 - 1953 - Radioactivity anomalies detected along parts of the Atlantic Ocean beach from Cape Henry, Virginia, to Cape Fear, North Carolina, and from Savannah Beach, Georgia, to Miami Beach, Florida","indexId":"ofr53286","publicationYear":"1953","noYear":false,"title":"Radioactivity anomalies detected along parts of the Atlantic Ocean beach from Cape Henry, Virginia, to Cape Fear, North Carolina, and from Savannah Beach, Georgia, to Miami Beach, Florida"},"lastModifiedDate":"2014-03-04T13:58:55","indexId":"tem644","displayToPublicDate":"1953-01-01T09:18:00","publicationYear":"1953","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":"644","title":"Airborne radioactivity survey of parts of Atlantic Ocean beach, Virginia to Florida","docAbstract":"The accompanying maps show the results of an airborne radioactivity survey along the Atlantic Ocean beach from Cape Henry, Virginia to Cape Fear, North Carolina and from Savannah Bach Georgia to Miami Beach, Florida. The survey was made March 23-24, 1953, as part of a cooperative program with the U.S. Atomic Energy Commission.  The survey was made with scintillation detection equipment mounted in a Douglas DC-3 aircraft and consisted of one flight line, at a 500-foot altitude, parallel to the beach.  The vertical projection of the flight line coincided approximately with the landward limit of the modern beach.  The width of the zone on the ground from which anomalous radiation is measured at the normal 500 foot flight altitude varies with the areal extent radioactivity of the source.  For strong sources of radioactivity the width of the zone would be as much as 1,400 feet.  The location of the flight lines is shown on the index map below.  No abnormal radioactivity was detected along the northern flight line between Cape Henry, Virginia and Cape Fear, North Carolina.  Along the southern flight line fourteen areas of abnormal radioactivity were detected between Savannah Beach, Georgia and Anastasia Island, Florida as shown on the map on the left. The abnormal radioactivity is apparently due to radioactive minerals associated with \"black sand\" deposits with occur locally along the beach in this region.  The present technique of airborne radioactivity measurement does not permit distinguishing between activity sue to thorium and that due to uranium.  An anomaly, therefore, may represent radioactivity due entirely to one or to a combination of these elements.  It is not possible to determine the extent or radioactive content of the materials responsible for the abnormal radioactivity.  The information given on the accompanying map indicates only those localities of greater-than-average radioactivity and, therefore suggest areas in which uranium and thorium deposits are more likely to occur.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem644","collaboration":"Prepared in cooperation with United States Atomic Energy Commission","usgsCitation":"Moxham, R., and Johnson, R., 1953, Airborne radioactivity survey of parts of Atlantic Ocean beach, Virginia to Florida: U.S. Geological Survey Trace Elements Memorandum 644, Report: 3 p.; 1 Plate: 14.53 x 21.38 inches, https://doi.org/10.3133/tem644.","productDescription":"Report: 3 p.; 1 Plate: 14.53 x 21.38 inches","numberOfPages":"3","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278408,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0644/report-thumb.jpg"},{"id":283297,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0644/report.pdf"},{"id":283296,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0644/plate-1.pdf"}],"country":"United States","state":"Florida;Georgia;North Carolina;South Carolina;Virginia","otherGeospatial":"Atlantic Ocean Beach","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -81.8,29.6 ], [ -81.8,32.2 ], [ -80.8,32.2 ], [ -80.8,29.6 ], [ -81.8,29.6 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"526b92e4e4b058918d0acaf7","contributors":{"authors":[{"text":"Moxham, R.M.","contributorId":42234,"corporation":false,"usgs":true,"family":"Moxham","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":485189,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, R.W.","contributorId":83194,"corporation":false,"usgs":true,"family":"Johnson","given":"R.W.","affiliations":[],"preferred":false,"id":485190,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70048714,"text":"tem676 - 1953 - Distribution of coarse- and fire-grained rocks in the Wasatch formation and their relationship to uranium deposits, Powder River Basin, Wyoming","interactions":[],"lastModifiedDate":"2014-03-04T14:07:26","indexId":"tem676","displayToPublicDate":"1953-01-01T09:17:00","publicationYear":"1953","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":"676","title":"Distribution of coarse- and fire-grained rocks in the Wasatch formation and their relationship to uranium deposits, Powder River Basin, Wyoming","docAbstract":"A brief study of the areal distribution of the various rock types of the Wasatch formation in the Powder River Basin, Wyoming, was made during the summer of 1952.  In the south and central parts if the basin, the Wasatch formation appears to contain coarser-grained rocks in contrast to the northern part, which contain relatively no coarser-grained rocks.  The finer-grained rocks are abundant in the northern and central parts of the basin but relatively scare in the southern part. The known uranium deposits in the Wasatch are in the central area where coarser-grained sandstones are complemented by abundant finer-grained rocks such as shales and siltstones.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem676","collaboration":"Prepared by the Geological Survey for the United States Atomic Energy Commission","usgsCitation":"Davidson, D., 1953, Distribution of coarse- and fire-grained rocks in the Wasatch formation and their relationship to uranium deposits, Powder River Basin, Wyoming: U.S. Geological Survey Trace Elements Memorandum 676, 12 p., https://doi.org/10.3133/tem676.","productDescription":"12 p.","numberOfPages":"12","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278593,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0676/report-thumb.jpg"},{"id":283305,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0676/report.pdf"}],"country":"United States","state":"Wyoming","otherGeospatial":"Powder River Basin;Wasatch Formation","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.0,42.0 ], [ -108.0,45.0 ], [ -104.0,45.0 ], [ -104.0,42.0 ], [ -108.0,42.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52737be5e4b097f32ac3dafd","contributors":{"authors":[{"text":"Davidson, David F.","contributorId":90594,"corporation":false,"usgs":true,"family":"Davidson","given":"David F.","affiliations":[],"preferred":false,"id":485474,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70048601,"text":"tem642 - 1953 - Photogeologic map, Tidwell-5 quadrangle, Emery county, Utah","interactions":[{"subject":{"id":70048601,"text":"tem642 - 1953 - Photogeologic map, Tidwell-5 quadrangle, Emery county, Utah","indexId":"tem642","publicationYear":"1953","noYear":false,"title":"Photogeologic map, Tidwell-5 quadrangle, Emery county, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":66733,"text":"i113 - 1955 - Photogeologic map of the Tidwell-5 quadrangle, Emery County, Utah","indexId":"i113","publicationYear":"1955","noYear":false,"title":"Photogeologic map of the Tidwell-5 quadrangle, Emery County, Utah"},"id":1}],"supersededBy":{"id":66733,"text":"i113 - 1955 - Photogeologic map of the Tidwell-5 quadrangle, Emery County, Utah","indexId":"i113","publicationYear":"1955","noYear":false,"title":"Photogeologic map of the Tidwell-5 quadrangle, Emery County, Utah"},"lastModifiedDate":"2014-03-04T13:58:17","indexId":"tem642","displayToPublicDate":"1953-01-01T09:10:00","publicationYear":"1953","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":"642","title":"Photogeologic map, Tidwell-5 quadrangle, Emery county, Utah","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem642","collaboration":"Prepared in cooperation with the Atomic Energy Commission","usgsCitation":"Orkild, P., 1953, Photogeologic map, Tidwell-5 quadrangle, Emery county, Utah: U.S. Geological Survey Trace Elements Memorandum 642, Report: 3 p.; 1 Plate: 23.60 x 31.82 inches, https://doi.org/10.3133/tem642.","productDescription":"Report: 3 p.; 1 Plate: 23.60 x 31.82 inches","numberOfPages":"3","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278404,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0642/report-thumb.jpg"},{"id":283295,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0642/report.pdf"},{"id":283294,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0642/plate-1.pdf"}],"scale":"24000","country":"United States","state":"Utah","county":"Emery County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.5,38.75 ], [ -110.5,38.875 ], [ -110.375,38.875 ], [ -110.375,38.75 ], [ -110.5,38.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"526b9308e4b058918d0acc24","contributors":{"authors":[{"text":"Orkild, P. P.","contributorId":46494,"corporation":false,"usgs":true,"family":"Orkild","given":"P. P.","affiliations":[],"preferred":false,"id":485187,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70276505,"text":"70276505 - 1953 - United States base map","interactions":[],"lastModifiedDate":"2026-06-16T15:39:04.872398","indexId":"70276505","displayToPublicDate":"1953-01-01T07:54:26","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"United States base map","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70276505","usgsCitation":"U.S. Geological Survey, 1953, United States base map, 1 Plate: 41.99 x 28.13 inches, https://doi.org/10.3133/70276505.","productDescription":"1 Plate: 41.99 x 28.13 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,{"id":1013778,"text":"1013778 - 1953 - A new adjuvant in the diagnosis of fish furunculosis caused by Bacterium salmonicida","interactions":[],"lastModifiedDate":"2012-02-02T00:04:30","indexId":"1013778","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3683,"text":"Veterinary Medicine","active":true,"publicationSubtype":{"id":10}},"title":"A new adjuvant in the diagnosis of fish furunculosis caused by Bacterium salmonicida","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Veterinary Medicine","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"35/FH","usgsCitation":"Griffin, P.J., Snieszko, S.F., and Friddle, S.B., 1953, A new adjuvant in the diagnosis of fish furunculosis caused by Bacterium salmonicida: Veterinary Medicine, v. 48, no. 7, p. 280-282.","productDescription":"p. 280-282","startPage":"280","endPage":"282","numberOfPages":"3","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":132198,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"48","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b20e4b07f02db6ac037","contributors":{"authors":[{"text":"Griffin, P. J.","contributorId":50111,"corporation":false,"usgs":true,"family":"Griffin","given":"P.","middleInitial":"J.","affiliations":[],"preferred":false,"id":319245,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Snieszko, S. F.","contributorId":13169,"corporation":false,"usgs":true,"family":"Snieszko","given":"S.","middleInitial":"F.","affiliations":[],"preferred":false,"id":319243,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Friddle, S. B.","contributorId":18299,"corporation":false,"usgs":true,"family":"Friddle","given":"S.","middleInitial":"B.","affiliations":[],"preferred":false,"id":319244,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1000271,"text":"1000271 - 1953 - Technique for the application of a streamer-type fish tag","interactions":[],"lastModifiedDate":"2016-02-15T13:20:20","indexId":"1000271","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Technique for the application of a streamer-type fish tag","docAbstract":"<p>Principal features of the technique are: attachment of the plastic tag by means of a nylon-thread loop prepared in advance of field work; use of a curved surgical needle with cutting edge and a split eye for application of the tag. The procedures for splitting the needle's eye and for applying the tag are described and illustrated by a series of photographs.</p>","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1952)82[42:TFTAOA]2.0.CO;2","usgsCitation":"Joeris, L.S., 1953, Technique for the application of a streamer-type fish tag: Transactions of the American Fisheries Society, v. 82, no. 1, p. 42-47, https://doi.org/10.1577/1548-8659(1952)82[42:TFTAOA]2.0.CO;2.","productDescription":"6 p.","startPage":"42","endPage":"47","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133295,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"82","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c333","contributors":{"authors":[{"text":"Joeris, Leonard S.","contributorId":104430,"corporation":false,"usgs":true,"family":"Joeris","given":"Leonard","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":308319,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1000296,"text":"1000296 - 1953 - Lake fisheries need lamprey control and research","interactions":[],"lastModifiedDate":"2012-02-02T00:04:05","indexId":"1000296","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3560,"text":"The Fisherman","active":true,"publicationSubtype":{"id":10}},"title":"Lake fisheries need lamprey control and research","docAbstract":"Since 1921, when the first sea lamprey was recorded from Lake Erie, concern about this parasite in the Great Lakes above Niagara Falls, where previously it had never occurred, grew successively.  At first, the concern was shared only in scientific circles, but as the parasite continued its persistent and rapid spread throughout the upper Great Lakes this concern was voiced by state conservation departments, the U.S. Fish and Wildlife Service, and interested fishermen.  Catches of lake trout especially, and other species secondarily, began to fall below anything representing normal fluctuations in abundance.  The fishing industry on Lake Huron and Lake Michigan became extremely concerned due to the fact that income was diminishing greatly.  Producers on Lake Superior were fearful that the same decline in production would soon characterize their fishery.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"The Fisherman","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Moffett, J.W., 1953, Lake fisheries need lamprey control and research: The Fisherman, v. 21, no. 4, p. 10-11.","productDescription":"p. 10-11,14","startPage":"10","endPage":"11","numberOfPages":"1","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128655,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b12b5","contributors":{"authors":[{"text":"Moffett, James W.","contributorId":94245,"corporation":false,"usgs":true,"family":"Moffett","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":308353,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1013777,"text":"1013777 - 1953 - A more comprehensive description of Bacterium salmonicida","interactions":[],"lastModifiedDate":"2026-04-20T16:04:37.996823","indexId":"1013777","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"A more comprehensive description of Bacterium salmonicida","docAbstract":"<p class=\"chapter-para\">The purpose of this study was to establish a set of descriptive data which could be used as a reference or a standard in the identification of Bacterium salmonicida, the cause of furunculosis in fish. Since a complete description of B. salmonicida was not available, bacteriologists were not in a position to identify this microorganism in a manner which would meet the rigorous requirements of present‐day bacteriology.</p><p class=\"chapter-para\">Ten strains of B. salmonicida were employed in these studies. A detailed description is presented which includes the morphological, cultural, and physiological characteristics of B. salmonicida. In addition, various factors such as oxygen, pH, temperature, and composition of media are discussed in terms of their influence on the formation of the melanin‐like pigment which is characteristically produced by this microorganism.</p>","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1952)82[129:AMCDOB]2.0.CO;2","usgsCitation":"Griffin, P.J., Snieszko, S.F., and Friddle, S.B., 1953, A more comprehensive description of Bacterium salmonicida: Transactions of the American Fisheries Society, v. 82, no. 1, p. 129-138, https://doi.org/10.1577/1548-8659(1952)82[129:AMCDOB]2.0.CO;2.","productDescription":"10 p.","startPage":"129","endPage":"138","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":132197,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"82","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ade50","contributors":{"authors":[{"text":"Griffin, P. J.","contributorId":50111,"corporation":false,"usgs":true,"family":"Griffin","given":"P.","middleInitial":"J.","affiliations":[],"preferred":false,"id":319242,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Snieszko, S. F.","contributorId":13169,"corporation":false,"usgs":true,"family":"Snieszko","given":"S.","middleInitial":"F.","affiliations":[],"preferred":false,"id":319240,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Friddle, S. B.","contributorId":18299,"corporation":false,"usgs":true,"family":"Friddle","given":"S.","middleInitial":"B.","affiliations":[],"preferred":false,"id":319241,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1000163,"text":"1000163 - 1953 - The movement of tagged lake trout in Lake Superior, 1950-52","interactions":[],"lastModifiedDate":"2026-04-20T15:59:50.564467","indexId":"1000163","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"The movement of tagged lake trout in Lake Superior, 1950-52","docAbstract":"<p>A total of 733 native lake trout was tagged at two widely separated localities in Lake Superior; subsequent recaptures numbered 155 fish (21.1 percent) during the year following marking. In October 1950, 116 large lake trout (average total length, 27.3 inches) were tagged near Keweenaw Point, Michigan. Fifteen (12.9 percent) were recovered during the first year at points as far west as the Gooseberry River, Minnesota (190 miles), north to the Slate Islands, Ontario (95 miles), and east to Grand Marais, Michigan (100 miles). Nine fish (7.8 percent) were recovered during the second year after marking. Returns from 617 tagged lake trout of smaller size (average length 18.2 inches) released in the Apostle Island region of Wisconsin during the period June 12 to August 6, 1951, numbered 140 (22.7 percent) during the first year. Of these fish, 90 percent were recaptured within a radius of 50 miles of the points of release. Seventy-six percent were caught in Wisconsin, 14 percent in Minnesota, and 9 percent in Michigan waters. The fish retaken in Michigan had moved 120 to 255 miles between the time of release and recapture, traveling as far west as Grand Marais. Lake trout recaptured at distances of more than 50 miles from the tagging locality were of larger average size than marked fish caught within this radius. </p><p>The four types of tags used in the marking of lake trout in the Apostle Island region, together with the number tagged and percentage recovered during the first year were as follows: 103 aluminum lower-jaw tags (used only on fish less than 17 inches in length when marked)-10.7 percent; 200 monel upper-jaw tags-14 percent; 162 streamer tags-19.8 percent; and 152 Peterson tags-45.4 percent. Obviously lake trout marked with the Peterson tag, with the discs and ends of the pin projecting from each side near the point of maximum girth, were more vulnerable to the fishery than were fish marked with other tags. The recoveries of marked fish show that Lake Superior lake trout-particularly fish of large size-may move many miles and freely cross political boundaries; and that the rate of harvest is moderately high for a fish with a life history as long as that of the lake trout.</p>","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1952)82[68:TMOTLT]2.0.CO;2","usgsCitation":"Eschmeyer, P.H., Daly, R., and Erkkila, L.F., 1953, The movement of tagged lake trout in Lake Superior, 1950-52: Transactions of the American Fisheries Society, v. 82, no. 1, p. 68-77, https://doi.org/10.1577/1548-8659(1952)82[68:TMOTLT]2.0.CO;2.","productDescription":"9 p.","startPage":"68","endPage":"77","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":131506,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Michigan, Minnesota, Wisconsin","otherGeospatial":"Lake Superior","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -91.19938850679905,\n              47.70219251975135\n            ],\n            [\n              -92.37337344484679,\n              46.40701495117111\n            ],\n            [\n              -83.83637874402585,\n              45.65664135395102\n            ],\n            [\n              -84.57836262100768,\n              47.082340243879926\n            ],\n            [\n              -88.18587494263889,\n              48.25603863790735\n            ],\n            [\n              -89.83058347192485,\n              48.02490350307414\n            ],\n            [\n              -91.19938850679905,\n              47.70219251975135\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"82","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4732","contributors":{"authors":[{"text":"Eschmeyer, Paul H.","contributorId":86719,"corporation":false,"usgs":true,"family":"Eschmeyer","given":"Paul","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":308169,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Daly, Russell","contributorId":97857,"corporation":false,"usgs":true,"family":"Daly","given":"Russell","email":"","affiliations":[],"preferred":false,"id":308171,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Erkkila, Leo F.","contributorId":92197,"corporation":false,"usgs":true,"family":"Erkkila","given":"Leo","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":308170,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011073,"text":"70011073 - 1953 - Field method for determination of traces of arsenic in soils: Confined spot procedure using a modified Gutzeit apparatus","interactions":[],"lastModifiedDate":"2012-03-12T17:18:31","indexId":"70011073","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","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":"Field method for determination of traces of arsenic in soils: Confined spot procedure using a modified Gutzeit apparatus","docAbstract":"[No abstract available]","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Analytical Chemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00032700","usgsCitation":"Almond, H., 1953, Field method for determination of traces of arsenic in soils: Confined spot procedure using a modified Gutzeit apparatus: Analytical Chemistry, v. 25, no. 11, p. 1766-1767.","startPage":"1766","endPage":"1767","numberOfPages":"2","costCenters":[],"links":[{"id":221088,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0fc6e4b0c8380cd539f8","contributors":{"authors":[{"text":"Almond, H.","contributorId":47911,"corporation":false,"usgs":true,"family":"Almond","given":"H.","email":"","affiliations":[],"preferred":false,"id":360222,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011091,"text":"70011091 - 1953 - Analysis of mixed-layer clay mineral structures","interactions":[],"lastModifiedDate":"2012-03-12T17:18:27","indexId":"70011091","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Analysis of mixed-layer clay mineral structures","docAbstract":"Among the enormously abundant natural occurrences of clay minerals, many examples are encountered in which no single specific crystallization scheme extends through a single ultimate grain. The characterization of such assemblages becomes an analysis of the distribution of matter within such grains, rather than the simple identification of mineral species. It having become established that the particular coordination complex typified by mica is a common component of many natural subcrystalline assemblages, the opportunity is afforded to analyze scattering from random associations of these complexes with other structural units. Successful analyses have been made of mixed hydration states of montmorillonite, of montmorillonite with mica, of vermiculite with mica, and of montmorillonite with chlorite, all of which are variants of the mica complex, and of halloysite with hydrated halloysite.","largerWorkTitle":"Analytical Chemistry","language":"English","issn":"00032700","usgsCitation":"Bradley, W., 1953, Analysis of mixed-layer clay mineral structures, <i>in</i> Analytical Chemistry, v. 25, no. 5, p. 727-730.","startPage":"727","endPage":"730","numberOfPages":"4","costCenters":[],"links":[{"id":221347,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059eb21e4b0c8380cd48c3c","contributors":{"authors":[{"text":"Bradley, W. F.","contributorId":84070,"corporation":false,"usgs":true,"family":"Bradley","given":"W. F.","affiliations":[],"preferred":false,"id":360262,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5221320,"text":"5221320 - 1953 - The effects of DDT upon the survival and growth of nestling songbirds","interactions":[],"lastModifiedDate":"2025-01-29T17:00:22.192614","indexId":"5221320","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","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":"The effects of DDT upon the survival and growth of nestling songbirds","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Wiley","doi":"10.2307/3796804","usgsCitation":"Mitchell, R.T., Blagbrough, H., and VanEtten, R., 1953, The effects of DDT upon the survival and growth of nestling songbirds: Journal of Wildlife Management, v. 17, no. 1, p. 45-54, https://doi.org/10.2307/3796804.","productDescription":"10 p.","startPage":"45","endPage":"54","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":194123,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryland","otherGeospatial":"Patuxent Research Refuge","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -76.82358536957531,\n              39.05213804748183\n            ],\n            [\n              -76.82358536957531,\n              39.0079813077387\n            ],\n            [\n              -76.7490854859807,\n              39.0079813077387\n            ],\n            [\n              -76.7490854859807,\n              39.05213804748183\n            ],\n            [\n              -76.82358536957531,\n              39.05213804748183\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"17","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db667050","contributors":{"authors":[{"text":"Mitchell, Robert T.","contributorId":49020,"corporation":false,"usgs":true,"family":"Mitchell","given":"Robert","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":333553,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blagbrough, H.P.","contributorId":27566,"corporation":false,"usgs":true,"family":"Blagbrough","given":"H.P.","email":"","affiliations":[],"preferred":false,"id":333554,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"VanEtten, R.C.","contributorId":51864,"corporation":false,"usgs":true,"family":"VanEtten","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":333555,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70184460,"text":"70184460 - 1953 - River meanders and vorticity theorem","interactions":[],"lastModifiedDate":"2017-03-09T12:33:42","indexId":"70184460","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3879,"text":"Eos, Earth and Space Science News","active":true,"publicationSubtype":{"id":10}},"title":"River meanders and vorticity theorem","docAbstract":"<p>T<span>he serpentine windings of rivers, which in certain reaches attain a remarkable symmetry and are then called meanders, must represent one aspect of the tendency for establishment of quasi-equilibrium in natural streams. With the increase in knowledge of the interaction of forces operating in rivers, this tendency toward equilibrium has assumed a greater significance.</span></p>","language":"English","publisher":"AGU Publications","doi":"10.1029/TR034i006p00955","usgsCitation":"Leopold, L.B., 1953, River meanders and vorticity theorem: Eos, Earth and Space Science News, v. 34, no. 6, p. 955-959, https://doi.org/10.1029/TR034i006p00955.","productDescription":"5 p.","startPage":"955","endPage":"959","costCenters":[],"links":[{"id":337183,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"34","issue":"6","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","scienceBaseUri":"58c277fbe4b014cc3a3e7718","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":681605,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70184457,"text":"70184457 - 1953 - Downstream change of velocity in rivers","interactions":[],"lastModifiedDate":"2017-03-09T12:02:51","indexId":"70184457","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":732,"text":"American Journal of Science","active":true,"publicationSubtype":{"id":10}},"title":"Downstream change of velocity in rivers","docAbstract":"<p>Because river slope generally decreases in a downstream direction, it is generally supposed that velocity of flow also decreases downstream. Analysis of some of the large number of velocity measurements made at stream-gaging stations demonstrates that mean velocity generally tends to increase downstream. Although there are many reaches in nearly all rivers where mean velocity decreases downstream, the general tendency for conservation or for downstream increase was found in all data studied.</p><p>Computations of bed velocity indicate that this parameter also tends to increase downstream.</p><p>Near the streambed, shear in the vertical profile of velocity (rate of decrease of velocity with depth) tends to decrease downstream. This down-valley decrease of shear implies decreasing competence downstream.</p>","language":"English","publisher":"American Journal of Science","doi":"10.2475/ajs.251.8.606","usgsCitation":"Leopold, L.B., 1953, Downstream change of velocity in rivers: American Journal of Science, v. 251, no. 8, p. 606-624, https://doi.org/10.2475/ajs.251.8.606.","productDescription":"19 p.","startPage":"606","endPage":"624","costCenters":[],"links":[{"id":480434,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2475/ajs.251.8.606","text":"Publisher Index Page"},{"id":337177,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"251","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58c277fbe4b014cc3a3e771c","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":681597,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70184458,"text":"70184458 - 1953 - Relation of suspended-sediment concentration to channel scour and fill","interactions":[],"lastModifiedDate":"2017-03-09T12:18:27","indexId":"70184458","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Relation of suspended-sediment concentration to channel scour and fill","docAbstract":"<p>It is known that during the passage of a flood the channel of an alluvial stream scours and fills with considerable rapidity. Though such changes may be random, it seems more likely that there is a definite pattern of channel change directly related both to discharge and to the sediment load provided to the river by the drainage basin.</p><p>In a study by the authors [1] an analysis was made of concurrent values of suspended sediment load and width, mean depth, mean velocity, and discharge at a number of gaging stations. From the data analyzed it appeared that fairly definite relations exist between these variables.</p>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Proceedings of the fifth Hydraulics Conference, June 9-11, 1952, arranged by the Iowa Institute of Hydraulic Research","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"Proceedings of the fifth Hydraulics Conference","conferenceDate":"June 9-11, 1952","conferenceLocation":"Iowa City, IA","language":"English","usgsCitation":"Leopold, L.B., and Maddock, T., 1953, Relation of suspended-sediment concentration to channel scour and fill, <i>in</i> Proceedings of the fifth Hydraulics Conference, June 9-11, 1952, arranged by the Iowa Institute of Hydraulic Research, Iowa City, IA, June 9-11, 1952, p. 159-178.","productDescription":"20 p.","startPage":"159","endPage":"178","costCenters":[],"links":[{"id":337178,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://ir.uiowa.edu/uisie/34/","text":"Conference Proceedings"},{"id":337179,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"publicComments":"University of Iowa Studies in Engineering, 34","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58c277fbe4b014cc3a3e771a","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":681598,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Maddock, Thomas Jr.","contributorId":14402,"corporation":false,"usgs":true,"family":"Maddock","given":"Thomas","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":681599,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1285,"text":"wsp1190 - 1953 - Ground-water conditions in artesian aquifers in Brown County, Wisconsin","interactions":[],"lastModifiedDate":"2023-04-11T19:43:34.619708","indexId":"wsp1190","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","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":"1190","title":"Ground-water conditions in artesian aquifers in Brown County, Wisconsin","docAbstract":"The principal water-bearing rocks underlying Brown County, Wis., are thick sandstone units of Cambrian and Ordovician age. Other aquifers include limestone and dolomite of Ordovician age, dolomite of Silurian age, and sands and gravel of Pleistocene and Recent age. Underlying the water-bearing formations are crystalline rocks of pre-Cambrian age which contain little or no water. \r\n\r\nGround water is the source of all public and most private and industrial supplies in. the county. Several of the large industries use large quantities of surface water also. Most of the water is pumped from wells that penetrate the Cambrian sandstones where the water occurs under artesian conditions. From 1886, when the first deep well was drilled, to 1949, the pumpage in the county increased to an average of about 5 million gallons a day (mgd) in 1939 and to about 10 mgd in 1949.\r\n\r\nThe piezometric level, which was about 100 feet above the land surface in 1886, was about 300 feet below the land surface in 1949. About 200 feet of this decline took place after 1938. The water-level-measurement program begun in 1946 shows that yearly fluctuations of water levels in observation wells range from less than 1 foot to about 90 feet, the fluctuations being larger at the center of the heavily pumped area. The highest water levels occur in the winter or spring and the lowest in the summer near the end of the season of maximum withdrawal. Coefficients of transmissibility and storage for the sandstones were obtained by making controlled pumping tests at Green Bay and De Pere. The coefficients were verified by comparing computed water-level declines and rates of withdrawal with actual ones. The computed values were within I0 percent of the actual values. \r\n\r\nProbable declines of water levels by 1960 were computed, using the same coefficients of transmissibility and storage, and assuming three different conditions of pumping. The additional decline in water level will be 15 to 150 feet in the center of the pumped area, depending upon the amount of increased pumping and its distribution relative to the present pumped area and to the recharge area. \r\n\r\nThe water from the sandstones is a hard calcium magnesium bicarbonate water. Further work is needed to determine whether there is danger of contamination by salt water which occurs down the dip in the same formations. It is concluded that the rate of withdrawal from the area can be increased to 15 mgd by 1960 without dangerously lowering water levels, provided that new wells are properly spaced. In order to avoid expressive lowering of water levels, it is recommended that new wells be located west of Green Bay toward the recharge area. \r\n\r\nA detailed study has not been made of shallow aquifers in the county. Further work should be done to evaluate the possibilities of auxiliary supplies from the limestone of the Platteville formation or from the Niagara dolomite. \r\n\r\nConservation should be practice.4 by all users of ground water to avoid waste resulting in lower water levels and higher pumping costs.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1190","usgsCitation":"Drescher, W.J., 1953, Ground-water conditions in artesian aquifers in Brown County, Wisconsin: U.S. Geological Survey Water Supply Paper 1190, Report: iv, 49 p.; 7 Plates: 20.00 x 9.00 inches or smaller, https://doi.org/10.3133/wsp1190.","productDescription":"Report: iv, 49 p.; 7 Plates: 20.00 x 9.00 inches or smaller","numberOfPages":"53","costCenters":[],"links":[{"id":415594,"rank":10,"type":{"id":36,"text":"NGMDB Index 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States","state":"Wisconsin","county":"Brown 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William James","contributorId":95448,"corporation":false,"usgs":true,"family":"Drescher","given":"William","email":"","middleInitial":"James","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":143500,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70189740,"text":"70189740 - 1953 - The use of soils and paleosols for interpreting geomorphic and climatic history of arid regions","interactions":[],"lastModifiedDate":"2017-07-22T13:01:12","indexId":"70189740","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"seriesTitle":{"id":5468,"text":"Research Council of Israel Special Publication","active":false,"publicationSubtype":{"id":19}},"seriesNumber":"2","title":"The use of soils and paleosols for interpreting geomorphic and climatic history of arid regions","docAbstract":"<p>The study of modern surface soils, and ancient weathering zones, which occur either buried or as surface relicts, has contributed materially to understanding the complex events of the glacial and post-glacial period both in glaciated areas and in regions not influenced by glaciation. Most work of this kind in the United States has been done by geologists.</p><p>Numerous Pleistocene geologists have noted weathered zones between sheets of glacial drift or loess in the middle western United States. These include Condra, et al<sup>5</sup>; Frye<sup>7</sup>; Frye and Leonard<sup>8</sup>; Kay and Pearce<sup>13</sup>; Leighton and MacClintock<sup>15</sup>; Leverett<sup>16</sup>,<sup>17</sup>,<sup>18</sup>; Lugn<sup>19</sup>; Peltier<sup>23</sup>; Schultz and Stout<sup>26</sup>; Schultz, et al<sup>27</sup>; and Simonson<sup>28</sup>. Kay and Pearce<sup>13</sup> interpreted the weathered zones between sheets of glacial drift as profiles of ancient soils which they referred to as gumbotil. Hseung, Marshall and Krusekopf<sup>10</sup> have recently questioned the pedogenic character of gumbotil, but have failed to offer a satisfactory alternative explanation. Thorp, and coworkers<sup>30</sup>, in a general review of buried soils, apparently consider gumbotil a product of ancient soil-forming processes.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Desert research: Proceedings (Research Council of Israel Special Publication No. 2)","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Desert Research","conferenceDate":"May 7-14, 1952","conferenceLocation":"Jerusalem, Israel","language":"English","publisher":"Research Council of Israel","publisherLocation":"Jerusalem, Israel","usgsCitation":"Miller, J., and Leopold, L.B., 1953, The use of soils and paleosols for interpreting geomorphic and climatic history of arid regions, <i>in</i> Desert research: Proceedings (Research Council of Israel Special Publication No. 2), Jerusalem, Israel, May 7-14, 1952, p. 453-462.","productDescription":"10 p.","startPage":"453","endPage":"462","costCenters":[],"links":[{"id":344223,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59746421e4b0ec1a48878495","contributors":{"authors":[{"text":"Miller, John","contributorId":190242,"corporation":false,"usgs":false,"family":"Miller","given":"John","email":"","affiliations":[],"preferred":false,"id":706049,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":706050,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70194900,"text":"70194900 - 1953 - Biologists in the field of wildlife conservation","interactions":[],"lastModifiedDate":"2018-01-26T17:29:35","indexId":"70194900","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5610,"text":"AIBS Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Biologists in the field of wildlife conservation","docAbstract":"<p>We often hear comments such as \"people are funny\" and \"one meets the strangest people!\" Such sage remarks are not infrequently directed towards biologists, particularly those engaged in one of the many phases of wildlife conservation work. Bulletins of the \"love life\" of the raccoon or frog, and biologists who, for one reason or another, count the \"whiskers\" on a fox squirrel are held up for ridicule or dismissed with a shake of the head or a shrug of the shoulder and termed \"batty.\"</p>","language":"English","publisher":"Oxford University Press","doi":"10.2307/1292023","usgsCitation":"Leedy, D.L., 1953, Biologists in the field of wildlife conservation: AIBS Bulletin, v. 3, no. 2, p. 21-23, https://doi.org/10.2307/1292023.","productDescription":"3 p.","startPage":"21","endPage":"23","costCenters":[],"links":[{"id":350731,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a6c4cb6e4b06e28e9cabb5a","contributors":{"authors":[{"text":"Leedy, Daniel L.","contributorId":37787,"corporation":false,"usgs":true,"family":"Leedy","given":"Daniel","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":726045,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1000150,"text":"1000150 - 1953 - Movement of tagged lake trout in Lake Superior, 1950-1952","interactions":[],"lastModifiedDate":"2012-02-02T00:04:34","indexId":"1000150","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3560,"text":"The Fisherman","active":true,"publicationSubtype":{"id":10}},"title":"Movement of tagged lake trout in Lake Superior, 1950-1952","docAbstract":"A total of 733 native lake trout was tagged at two widely separated localities in Lake Superior; subsequent recaptures numbered 155 fish (21.1 percent) during the year following marking.  In October 1950, 116 large lake trout (average total length, 27.3 inches) were tagged near Keweenaw Point, Michigan.  Fifteen (12.9 percent) were recovered during the first year at points as far west as the Gooseberry River, Minnesota (190 miles), north to the Slate Islands, Ontario (95 miles), and east to Grand Marais, Michigan (100 miles).  Nine fish (7.8 percent) were recovered during the second year after marking.  Returns from 617 tagged lake trout of smaller size released in the Apostle Island region of Wisconsin during the period June 12 to August 6, 1951, numbered 140 (22.7 percent) during the first year.  Of these fish, 90 percent were recaptured within a radius of 50 miles of the point of release.  Seventy-six percent were caught in Wisconsin, 14 percent in Minnesota, and 9 percent in Michigan waters.  The fish retaken in Michigan had moved 120 to 255 miles between the time of release and recapture, traveling as far east as Grand Marais.  Lake trout recaptured at distances of more than 50 miles from the tagging locality were of larger average size than marked fish caught within this radius.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"The Fisherman","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"Out-of-print","usgsCitation":"Eschmeyer, P.H., Daly, R., and Erkkila, L.F., 1953, Movement of tagged lake trout in Lake Superior, 1950-1952: The Fisherman, v. 21, no. 3.","productDescription":"p. 4, 11","startPage":"4, 11","numberOfPages":"-4","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":132929,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4816","contributors":{"authors":[{"text":"Eschmeyer, Paul H.","contributorId":86719,"corporation":false,"usgs":true,"family":"Eschmeyer","given":"Paul","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":308148,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Daly, Russell","contributorId":97857,"corporation":false,"usgs":true,"family":"Daly","given":"Russell","email":"","affiliations":[],"preferred":false,"id":308150,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Erkkila, Leo F.","contributorId":92197,"corporation":false,"usgs":true,"family":"Erkkila","given":"Leo","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":308149,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":39177,"text":"pp248G - 1953 - Mica deposits of the southeastern Piedmont, Part 11, Alabama district","interactions":[{"subject":{"id":40064,"text":"ofr5272 - 1952 - Crystal Clear mica mine, Randolph County, Alabama","indexId":"ofr5272","publicationYear":"1952","noYear":false,"title":"Crystal Clear mica mine, Randolph County, Alabama"},"predicate":"SUPERSEDED_BY","object":{"id":39177,"text":"pp248G - 1953 - Mica deposits of the southeastern Piedmont, Part 11, Alabama district","indexId":"pp248G","publicationYear":"1953","noYear":false,"chapter":"G","title":"Mica deposits of the southeastern Piedmont, Part 11, Alabama district"},"id":1},{"subject":{"id":55378,"text":"ofr4350 - 1943 - M and G mica mine, Clay County, Alabama","indexId":"ofr4350","publicationYear":"1943","noYear":false,"title":"M and G mica mine, Clay County, Alabama"},"predicate":"SUPERSEDED_BY","object":{"id":39177,"text":"pp248G - 1953 - Mica deposits of the southeastern Piedmont, Part 11, Alabama district","indexId":"pp248G","publicationYear":"1953","noYear":false,"chapter":"G","title":"Mica deposits of the southeastern Piedmont, Part 11, Alabama district"},"id":2},{"subject":{"id":55379,"text":"ofr4463 - 1944 - Alabama mica mines","indexId":"ofr4463","publicationYear":"1944","noYear":false,"title":"Alabama mica mines"},"predicate":"SUPERSEDED_BY","object":{"id":39177,"text":"pp248G - 1953 - Mica deposits of the southeastern Piedmont, Part 11, Alabama district","indexId":"pp248G","publicationYear":"1953","noYear":false,"chapter":"G","title":"Mica deposits of the southeastern Piedmont, Part 11, Alabama district"},"id":3},{"subject":{"id":55482,"text":"ofr4583 - 1945 - Friendship No. 1 mica mine, Randolph County, Alabama","indexId":"ofr4583","publicationYear":"1945","noYear":false,"title":"Friendship No. 1 mica mine, Randolph County, Alabama"},"predicate":"SUPERSEDED_BY","object":{"id":39177,"text":"pp248G - 1953 - Mica deposits of the southeastern Piedmont, Part 11, Alabama district","indexId":"pp248G","publicationYear":"1953","noYear":false,"chapter":"G","title":"Mica deposits of the southeastern Piedmont, Part 11, Alabama district"},"id":4}],"lastModifiedDate":"2024-09-24T20:13:25.636637","indexId":"pp248G","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"248","chapter":"G","title":"Mica deposits of the southeastern Piedmont, Part 11, Alabama district","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp248G","usgsCitation":"Heinrich, E.W., and Olson, J.C., 1953, Mica deposits of the southeastern Piedmont, Part 11, Alabama district: U.S. Geological Survey Professional Paper 248, Report: iv, 62 p.; 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