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F.","contributorId":40211,"corporation":false,"usgs":true,"family":"Buddington","given":"A.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":166769,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leonard, B. 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During World War II, the areas were studied by the U. S. Geological Survey in cooperation with the U. S. Bureau of Mines. The Bureau of Mines hand-augered 162 holes and made chemical analyses of the samples for available alumina, and available ferric oxide, and measured the ignition loss.
The deposit contains two types of clay: granite residual clay derived from the weathering of Cretaceous granite gneiss in place; and transported clays of the Latah formation derived from the weathered. debris of the granodiorite and older rocks.
The Stockton deposits average more than 20 percent available alumina and less than 10 percent available ferric oxide. The deposits, therefore, could serve as a small source of low-grade high alumina clay.
Clays containing more than 15 percent available alumina and less than 5 percent available ferric oxide would be suitable for many ceramic products and some may meet the requirements for high-heat or super-heat duties. Therefore, the Stockton and Stanley Hill clay deposits contain ceramic-grade clays.
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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4235","contributors":{"authors":[{"text":"Scheid, Vernon Edward","contributorId":96706,"corporation":false,"usgs":true,"family":"Scheid","given":"Vernon","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":171796,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":15455,"text":"ofr54241 - 1954 - Reconnaissance geology of the Malaspina district, Alaska","interactions":[{"subject":{"id":15455,"text":"ofr54241 - 1954 - Reconnaissance geology of the Malaspina district, Alaska","indexId":"ofr54241","publicationYear":"1954","noYear":false,"title":"Reconnaissance geology of the Malaspina district, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":68916,"text":"om189 - 1957 - Reconnaissance geology of the Malaspina district, Alaska","indexId":"om189","publicationYear":"1957","noYear":false,"title":"Reconnaissance geology of the Malaspina district, Alaska"},"id":1}],"supersededBy":{"id":68916,"text":"om189 - 1957 - Reconnaissance geology of the Malaspina district, Alaska","indexId":"om189","publicationYear":"1957","noYear":false,"title":"Reconnaissance geology of the Malaspina district, Alaska"},"lastModifiedDate":"2023-09-29T20:09:02.201305","indexId":"ofr54241","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1954","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":"54-241","title":"Reconnaissance geology of the Malaspina district, Alaska","docAbstract":"This report presents in preliminary form the results of a reconnaissance geologic investigation of the Malaspina district, undertaken by the United States Geological Survey as part of a project to investigate the petroleum possibilities of the Gulf of Alaska Tertiary province. (See index map.)
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr54241","usgsCitation":"Plafker, G., and Miller, D.J., 1954, Reconnaissance geology of the Malaspina district, Alaska: U.S. Geological Survey Open-File Report 54-241, Report: 15 p.; 1 Plate: 39.60 x 28.59 inches, https://doi.org/10.3133/ofr54241.","productDescription":"Report: 15 p.; 1 Plate: 39.60 x 28.59 inches","costCenters":[],"links":[{"id":421423,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1954/0241/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":421422,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1954/0241/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":149034,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1954/0241/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Malaspina district","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -141.3675,59.5 ], [ -141.3675,60.333333333333336 ], [ -139.5,60.333333333333336 ], [ -139.5,59.5 ], [ -141.3675,59.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640a44","contributors":{"authors":[{"text":"Plafker, George","contributorId":3920,"corporation":false,"usgs":false,"family":"Plafker","given":"George","email":"","affiliations":[],"preferred":false,"id":171162,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, Don John","contributorId":77120,"corporation":false,"usgs":true,"family":"Miller","given":"Don","email":"","middleInitial":"John","affiliations":[],"preferred":false,"id":171163,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":15491,"text":"ofr54248 - 1954 - High alumina metamorphic rocks of the Kings Mountain district, North Carolina and South Carolina","interactions":[],"lastModifiedDate":"2012-02-02T00:07:08","indexId":"ofr54248","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1954","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":"54-248","title":"High alumina metamorphic rocks of the Kings Mountain district, North Carolina and South Carolina","docAbstract":"The following evidence suggests that high alumina quartzite in this district is of metasedimentary origin: high alumina quartzite occurs as well defined thin beds that can be traced up to three and one half miles along strike; many outcrops of high alumina quartzite exhibit compositional layering (i.e., kyanigte quartzite is interlayered with staurolite quartzite, and with non-kyanitic magnetiferous quartzite); high alumina quartzite beds occur in a conformable sequence of high alumina metasedimentary and metavolcanic schists. It is suggested that the high alumina quartzite beds are metamorphosed beds of sandy or silty clay; these beds probably represent one stage in the deposition of fine grained clayey clastic sediments. \r\n\r\nNo evidence was found to support the view of Smith and Newcombe (1951) that the kyanite at Henry Knob developed by hudrothermal introduction of alumina. The present study indicates that kyanite in the kyanite quartzite here, as throughout the district, is of metasedimentary origin.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr54248","usgsCitation":"Potter, D.B., 1954, High alumina metamorphic rocks of the Kings Mountain district, North Carolina and South Carolina: U.S. Geological Survey Open-File Report 54-248, 201 p. :maps ;30 cm., https://doi.org/10.3133/ofr54248.","productDescription":"201 p. :maps ;30 cm.","costCenters":[],"links":[{"id":148470,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1954/0248/report-thumb.jpg"},{"id":44461,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1954/0248/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44462,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1954/0248/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44463,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1954/0248/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44464,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1954/0248/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44465,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1954/0248/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44466,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1954/0248/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44467,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1954/0248/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635ad7","contributors":{"authors":[{"text":"Potter, Donald Brandreth","contributorId":92272,"corporation":false,"usgs":true,"family":"Potter","given":"Donald","email":"","middleInitial":"Brandreth","affiliations":[],"preferred":false,"id":171211,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":55743,"text":"ofr5444 - 1954 - Estimates of permeability of water-bearing deposits in Bayward portions of Napa, Sonoma, and PEtaluma Valleys, California","interactions":[{"subject":{"id":55743,"text":"ofr5444 - 1954 - Estimates of permeability of water-bearing deposits in Bayward portions of Napa, Sonoma, and PEtaluma Valleys, California","indexId":"ofr5444","publicationYear":"1954","noYear":false,"title":"Estimates of permeability of water-bearing deposits in Bayward portions of Napa, Sonoma, and PEtaluma Valleys, California"},"predicate":"SUPERSEDED_BY","object":{"id":1110,"text":"wsp1427 - 1958 - Geology and ground water in the Santa Rosa and Petaluma Valley areas, Sonoma County, California","indexId":"wsp1427","publicationYear":"1958","noYear":false,"title":"Geology and ground water in the Santa Rosa and Petaluma Valley areas, Sonoma County, California"},"id":1}],"supersededBy":{"id":1110,"text":"wsp1427 - 1958 - Geology and ground water in the Santa Rosa and Petaluma Valley areas, Sonoma County, California","indexId":"wsp1427","publicationYear":"1958","noYear":false,"title":"Geology and ground water in the Santa Rosa and Petaluma Valley areas, Sonoma County, California"},"lastModifiedDate":"2012-02-02T00:11:49","indexId":"ofr5444","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1954","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":"54-44","title":"Estimates of permeability of water-bearing deposits in Bayward portions of Napa, Sonoma, and PEtaluma Valleys, California","language":"ENGLISH","doi":"10.3133/ofr5444","usgsCitation":"Cardwell, G., 1954, Estimates of permeability of water-bearing deposits in Bayward portions of Napa, Sonoma, and PEtaluma Valleys, California: U.S. Geological Survey Open-File Report 54-44, 5 p., https://doi.org/10.3133/ofr5444.","productDescription":"5 p.","costCenters":[],"links":[{"id":174088,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fca8e","contributors":{"authors":[{"text":"Cardwell, G.T.","contributorId":48160,"corporation":false,"usgs":true,"family":"Cardwell","given":"G.T.","email":"","affiliations":[],"preferred":false,"id":254178,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":14336,"text":"ofr54134 - 1954 - Preliminary report on the water-power possibilities of the Seldovia River, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:07:08","indexId":"ofr54134","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1954","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":"54-134","title":"Preliminary report on the water-power possibilities of the Seldovia River, Alaska","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr54134","usgsCitation":"Johnson, F., 1954, Preliminary report on the water-power possibilities of the Seldovia River, Alaska: U.S. Geological Survey Open-File Report 54-134, 17 p. ill., map ;29 cm., https://doi.org/10.3133/ofr54134.","productDescription":"17 p. ill., map ;29 cm.","costCenters":[],"links":[{"id":148252,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":111208,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.dggs.dnr.state.ak.us/pubs/id/10504","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aade4b07f02db66b5a3","contributors":{"authors":[{"text":"Johnson, Fred A.","contributorId":93863,"corporation":false,"usgs":true,"family":"Johnson","given":"Fred A.","affiliations":[],"preferred":false,"id":169282,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":15448,"text":"ofr54240 - 1954 - Geologic investigations of proposed power sites at Cooper, Grant, Ptarmigan and Crescent Lakes, Alaska","interactions":[{"subject":{"id":15448,"text":"ofr54240 - 1954 - Geologic investigations of proposed power sites at Cooper, Grant, Ptarmigan and Crescent Lakes, Alaska","indexId":"ofr54240","publicationYear":"1954","noYear":false,"title":"Geologic investigations of proposed power sites at Cooper, Grant, Ptarmigan and Crescent Lakes, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":35491,"text":"b1031A - 1955 - Geologic investigations of proposed power sites at Cooper, Grant, Ptarmigan and Crescent Lakes, Alaska","indexId":"b1031A","publicationYear":"1955","noYear":false,"chapter":"A","title":"Geologic investigations of proposed power sites at Cooper, Grant, Ptarmigan and Crescent Lakes, Alaska"},"id":1}],"supersededBy":{"id":35491,"text":"b1031A - 1955 - Geologic investigations of proposed power sites at Cooper, Grant, Ptarmigan and Crescent Lakes, Alaska","indexId":"b1031A","publicationYear":"1955","noYear":false,"title":"Geologic investigations of proposed power sites at Cooper, Grant, Ptarmigan and Crescent Lakes, Alaska"},"lastModifiedDate":"2023-10-04T21:29:09.390977","indexId":"ofr54240","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1954","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":"54-240","title":"Geologic investigations of proposed power sites at Cooper, Grant, Ptarmigan and Crescent Lakes, Alaska","docAbstract":"The Geological Survey, as part of its program of the classification of public lands with respect to mineral and water resources, is currently making a systematic study and evaluation of the potential water power sites in Alaska. This report describes the geologic conditions and their relation to possible plans for the development of water power at Cooper, Grant, Ptarmigan, and Crescent Lakes on the Kenai Peninsula near Seward, Alaska.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr54240","usgsCitation":"Plafker, G., 1954, Geologic investigations of proposed power sites at Cooper, Grant, Ptarmigan and Crescent Lakes, Alaska: U.S. Geological Survey Open-File Report 54-240, Report: 38 p.; 4 Plates: 23.38 x 29.30 inches or smaller, https://doi.org/10.3133/ofr54240.","productDescription":"Report: 38 p.; 4 Plates: 23.38 x 29.30 inches or smaller","costCenters":[],"links":[{"id":421640,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1954/0240/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":421639,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1954/0240/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":421638,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1954/0240/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":421637,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1954/0240/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":421636,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1954/0240/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148756,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1954/0240/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Cooper Lake, Crescent Lake, Grant Lake, Ptarmigan Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -153.95478843900045,\n 60.936198542908755\n ],\n [\n -153.95478843900045,\n 59.123393322902785\n ],\n [\n -147.7587939475696,\n 59.123393322902785\n ],\n [\n -147.7587939475696,\n 60.936198542908755\n ],\n [\n -153.95478843900045,\n 60.936198542908755\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4f1e","contributors":{"authors":[{"text":"Plafker, George","contributorId":3920,"corporation":false,"usgs":false,"family":"Plafker","given":"George","email":"","affiliations":[],"preferred":false,"id":171150,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":15937,"text":"ofr54283 - 1954 - Field method for the determination of titanium in rocks","interactions":[],"lastModifiedDate":"2020-02-03T11:51:57","indexId":"ofr54283","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1954","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":"54-283","title":"Field method for the determination of titanium in rocks","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr54283","usgsCitation":"Shapiro, L., and Brannock, W.W., 1954, Field method for the determination of titanium in rocks: U.S. Geological Survey Open-File Report 54-283, 7 p. , https://doi.org/10.3133/ofr54283.","productDescription":"7 p. ","costCenters":[],"links":[{"id":371923,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1954/0283/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148693,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1954/0283/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fce4b07f02db5f58e2","contributors":{"authors":[{"text":"Shapiro, Leonard","contributorId":61406,"corporation":false,"usgs":true,"family":"Shapiro","given":"Leonard","email":"","affiliations":[],"preferred":false,"id":171977,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brannock, Walter Wallace","contributorId":20727,"corporation":false,"usgs":true,"family":"Brannock","given":"Walter","email":"","middleInitial":"Wallace","affiliations":[],"preferred":false,"id":171976,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":15820,"text":"ofr54272 - 1954 - Olsen high-alumina and high-iron clay deposits, Latah County, Idaho","interactions":[{"subject":{"id":15820,"text":"ofr54272 - 1954 - Olsen high-alumina and high-iron clay deposits, Latah County, Idaho","indexId":"ofr54272","publicationYear":"1954","noYear":false,"title":"Olsen high-alumina and high-iron clay deposits, Latah County, Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":34753,"text":"b1091 - 1960 - Investigations of some clay deposits in Washington and Idaho","indexId":"b1091","publicationYear":"1960","noYear":false,"title":"Investigations of some clay deposits in Washington and Idaho"},"id":1}],"supersededBy":{"id":34753,"text":"b1091 - 1960 - Investigations of some clay deposits in Washington and Idaho","indexId":"b1091","publicationYear":"1960","noYear":false,"title":"Investigations of some clay deposits in Washington and Idaho"},"lastModifiedDate":"2012-02-02T00:07:10","indexId":"ofr54272","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1954","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":"54-272","title":"Olsen high-alumina and high-iron clay deposits, Latah County, Idaho","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr54272","usgsCitation":"Scheid, V.E., Hosterman, J.W., and Sohn, I.G., 1954, Olsen high-alumina and high-iron clay deposits, Latah County, Idaho: U.S. Geological Survey Open-File Report 54-272, 25 p. :maps ;30 cm., https://doi.org/10.3133/ofr54272.","productDescription":"25 p. :maps ;30 cm.","costCenters":[],"links":[{"id":149515,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af3e4b07f02db691be7","contributors":{"authors":[{"text":"Scheid, Vernon Edward","contributorId":96706,"corporation":false,"usgs":true,"family":"Scheid","given":"Vernon","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":171791,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hosterman, John W.","contributorId":48962,"corporation":false,"usgs":true,"family":"Hosterman","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":171789,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sohn, I. G.","contributorId":70751,"corporation":false,"usgs":true,"family":"Sohn","given":"I.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":171790,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":15697,"text":"ofr54259 - 1954 - The physical behavior and geologic control of radon in mountain streams","interactions":[],"lastModifiedDate":"2012-02-02T00:06:59","indexId":"ofr54259","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1954","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":"54-259","title":"The physical behavior and geologic control of radon in mountain streams","docAbstract":"Radon distribution ratio determinations in an all-water system were made. They checked very closely with those done by Kofler in 1913. \r\n\r\nThe distribution of radon in stream waters and related springs was investigated in the Wasatch Mountains adjacent to Salt Lake City, Utah, and in a part of the Weber River near Ogden, Utah. \r\n\r\nThe radon distribution in the stream waters studied forms a definite pattern which is dependent upon the local influx Of relatively large amounts of radon-bearing ground water into the stream, and, in turn, the ability of the stream to lose its radon to the atmosphere through turbulence. The ability of the stream to lose its radon is governed largely by the gradient and rate of flow of the stream and the nature of the stream channel, and tends to reach an equilibrium value of less than one micro-micro Curie per liter. This loss of radon generally occurs as an exponential function with respect to distance of stream flow. The slope of the function varies with different streams. \r\n\r\nThe stream waters investigated contain from one limit of the sensitivity of theinstrument to about 450 micro-micro Curies of radon per liter. The radon content of spring waters is generally higher than that of stream waters. The large radon contents mark the areas of ground water influx into the stream, although, in most cases, no spring activity in these areas was observed. The high-radon anomalies can usually be related to definite stratigraphic horizons or structural features. \r\n\r\nThe amount of ground water being added to the stream can be estimated in some cases by radon measurements of stream waters and related springs. \r\n\r\nAlmost complete disequilibrium occurs between radon and its parent radium in stream and spring waters in this area.","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr54259","usgsCitation":"Rogers, A.S., 1954, The physical behavior and geologic control of radon in mountain streams: U.S. Geological Survey Open-File Report 54-259, 58 p. ill., maps ;29 cm., https://doi.org/10.3133/ofr54259.","productDescription":"58 p. ill., maps ;29 cm.","costCenters":[],"links":[{"id":148164,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1954/0259/report-thumb.jpg"},{"id":44692,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1954/0259/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44693,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1954/0259/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44694,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1954/0259/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44695,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1954/0259/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44696,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1954/0259/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a74e4b07f02db644936","contributors":{"authors":[{"text":"Rogers, Allen Stuart","contributorId":36949,"corporation":false,"usgs":true,"family":"Rogers","given":"Allen","email":"","middleInitial":"Stuart","affiliations":[],"preferred":false,"id":171565,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}