{"pageNumber":"1845","pageRowStart":"46100","pageSize":"25","recordCount":46603,"records":[{"id":5221092,"text":"5221092 - 1956 - Some uses of mark sensing in collecting game management data in the field","interactions":[],"lastModifiedDate":"2012-02-02T00:14:33","indexId":"5221092","displayToPublicDate":"2010-06-16T12:18:24","publicationYear":"1956","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3140,"text":"Proceedings of the Annual Conference of the Southeastern Association of Game and Fish Commissioners","active":true,"publicationSubtype":{"id":10}},"title":"Some uses of mark sensing in collecting game management data in the field","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Proceedings of the Annual Conference of the Southeastern Association of Game and Fish Commissioners","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Overton, S., and Sincock, J., 1956, Some uses of mark sensing in collecting game management data in the field: Proceedings of the Annual Conference of the Southeastern Association of Game and Fish Commissioners, v. 10, p. 131-134.","productDescription":"131-134","startPage":"131","endPage":"134","numberOfPages":"4","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":194029,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e77f3","contributors":{"authors":[{"text":"Overton, S.","contributorId":96786,"corporation":false,"usgs":true,"family":"Overton","given":"S.","email":"","affiliations":[],"preferred":false,"id":333018,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sincock, J.L.","contributorId":89994,"corporation":false,"usgs":true,"family":"Sincock","given":"J.L.","affiliations":[],"preferred":false,"id":333017,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70197596,"text":"70197596 - 1956 - Ground-water data collected in the Missouri River basin units in Kansas during 1955","interactions":[],"lastModifiedDate":"2022-05-25T18:55:08.636698","indexId":"70197596","displayToPublicDate":"1999-12-27T00:00:00","publicationYear":"1956","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Ground-water data collected in the Missouri River basin units in Kansas during 1955","docAbstract":"<p>Ground-water studies in the Missouri River Basin were begun by the United States Geological Survey during the fall of 1945 as a part of the program for development of the resources of the basin by the U.S. Bureau of Reclamation and other Federal Agencies. The studies of the ground-water resources in the part of Kansas that lies within the Basin have been coordinated with the cooperative program of ground-water studies already being carried on in Kansas by the U.S. Geological Survey, the Kansas State Geological Survey, the Division of Sanitation of the Kansas State Board of Health, and the Division of Water Resources of the Kansas State Board of Agriculture.</p><p>Areas in which ground-water data have been and are being collected are the following: Almena Unit in Norton and Phillips Counties; the Bostwick Unit in Jewell, Republic, and Cloud Counties; the Cedar Bluff Unit in Ellis, Rush, and Trego Counties; the Glen Elder Unit in Mitchell County; Kanopolis unit in Ellsworth, McPherson, and Saline Counties; Kirwin unit in Phillips, Smith, and Osborne Counties; St. Francis unit in Cheyenne County ; the Webster Unit in Osborne County; and the Wilson Unit in Lincoln County. Data relating to the Ladder Creek project in Greeley, Gove, Lane, Logan, Scott, Wallace, and Wichita Counties will be published later in a separate report.</p><p>This report is the ninth of a series of annual reports on ground-water in the nine above-named units in Kansas and contains the data collected during 1955. The first report of the series contained the data collected prior to and through 1947. An index to the data contained in this and previous reports is given in table 1.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70197596","collaboration":"Compiled in cooperation with the State Geological Survey of Kansas, the Division of Sanitation of the Kansas State Board of Health, and the Division of Water Resources of the Kansas State Board of Agriculture.","usgsCitation":"Mason, B., 1956, Ground-water data collected in the Missouri River basin units in Kansas during 1955: Open-File Report, 32 p., https://doi.org/10.3133/70197596.","productDescription":"32 p.","costCenters":[],"links":[{"id":401066,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70197596/report.pdf"},{"id":354994,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70197596/report-thumb.jpg"}],"country":"United States","state":"Kansas","otherGeospatial":"Missouri River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -102.030029296875,\n              38.44498466889473\n            ],\n            [\n              -97.415771484375,\n              38.44498466889473\n            ],\n            [\n              -97.415771484375,\n              40.002371935876475\n            ],\n            [\n              -102.030029296875,\n              40.002371935876475\n            ],\n            [\n              -102.030029296875,\n              38.44498466889473\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Mason, B.J.","contributorId":53029,"corporation":false,"usgs":true,"family":"Mason","given":"B.J.","email":"","affiliations":[],"preferred":false,"id":737868,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71612,"text":"tei589 - 1956 - A fluorimetric study of the thorium-morin system","interactions":[],"lastModifiedDate":"2014-07-15T06:46:23","indexId":"tei589","displayToPublicDate":"1994-01-01T07:00:00","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":"589","title":"A fluorimetric study of the thorium-morin system","docAbstract":"<p>Thorium reacts with morin to yield a yellow complex that fluoresces when irradiated with ultraviolet light.  The effect on the fluorescence of such variable as concentration of acid, alcohol, thorium, morin, and complex; time, temperature, and wavelength of exciting light are studied to determine experimental conditions yielding maximum fluorescence.  The effects of Zr<sup>4+</sup>, Al<sup>3+</sup>, Fe<sup>3+</sup>, Ca<sup>2+</sup>, and La<sup>3+</sup> are discussed.</p>\n<br/>\n<p>The fundamental relationships between light absorption and fluorescence are expressed in a general equation which applied to a three-component system when the fluorescence is measured in a transmission-type fluorimeter.  This general equation is used to obtain an expression for the fluorescence of the thorium-morin system.</p>\n<br/>\n<p>Equations, derived from experimental data, related both the fraction of thorium reacted to form complex and the fraction of unquenched fluorescence to the concentration of uncombined morin.  These functions, when combined with the general equation, give an expression which relates the total net fluorescence to the amount of uncombined morin in the solution.  This last equation can be used to determine the one region for the concentration of uncombined morin that gives maximum sensitivity for the system.  Calculated standard curves are in excellent agreement with experimental curves.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei589","usgsCitation":"Milkey, R.G., and Fletcher, M., 1956, A fluorimetric study of the thorium-morin system: U.S. Geological Survey Trace Elements Investigations 589, 56 p., https://doi.org/10.3133/tei589.","productDescription":"56 p.","numberOfPages":"57","costCenters":[],"links":[{"id":290037,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":290036,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0589/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aeb36","contributors":{"authors":[{"text":"Milkey, Robert G.","contributorId":84006,"corporation":false,"usgs":true,"family":"Milkey","given":"Robert","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":284477,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fletcher, Mary H.","contributorId":52954,"corporation":false,"usgs":true,"family":"Fletcher","given":"Mary H.","affiliations":[],"preferred":false,"id":284476,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":71608,"text":"tei584 - 1956 - Some observations on rutherfordine","interactions":[],"lastModifiedDate":"2014-07-15T06:37:23","indexId":"tei584","displayToPublicDate":"1994-01-01T07:00:00","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":"584","title":"Some observations on rutherfordine","docAbstract":"<p>The optical properties of rutherfordine, UO<sub>2</sub>CO<sub>3</sub>, previously determined on microscopic crystals, have been redetermined on considerably larger crystals; and the relations among the indices of refraction, the morphology, and the crystal structure have been examined.  Rutherfordine is orthorhombic, biaxial positive, with α = 1.715, β = 1.730, γ = 1.795, 2V = 53° (calc.); X = b, Y = c (elongation, Z = a.  The crystal structure of UO<sub>2</sub>CO <sub>3</sub> consists of layers of carbonate groups parallel to (010) with linear (O-U-O)<sup+2</sup> ions normal to the layers.  The indices β and γ correspond to vibration directions parallel to layers; the unexpectedly large difference in value between β and γ is ascribed to the optical anisotropy of the uranium-oxygen bonding in the layer.  Indexed X-ray powder data are given.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei584","usgsCitation":"Clark, J., and Christ, C., 1956, Some observations on rutherfordine: U.S. Geological Survey Trace Elements Investigations 584, 13 p., https://doi.org/10.3133/tei584.","productDescription":"13 p.","numberOfPages":"14","costCenters":[],"links":[{"id":290031,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":290030,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0584/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e8e4b07f02db5e8ed1","contributors":{"authors":[{"text":"Clark, Joan R.","contributorId":71648,"corporation":false,"usgs":true,"family":"Clark","given":"Joan R.","affiliations":[],"preferred":false,"id":284471,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Christ, C. L.","contributorId":53906,"corporation":false,"usgs":true,"family":"Christ","given":"C. L.","affiliations":[],"preferred":false,"id":284470,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":51929,"text":"ofr56104 - 1956 - Summary of ground-water data-collection stations in Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:11:34","indexId":"ofr56104","displayToPublicDate":"1994-01-01T00:00:00","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":"56-104","title":"Summary of ground-water data-collection stations in Florida","language":"ENGLISH","doi":"10.3133/ofr56104","usgsCitation":"Rorabaugh, M.I., 1956, Summary of ground-water data-collection stations in Florida: U.S. Geological Survey Open-File Report 56-104, NA, https://doi.org/10.3133/ofr56104.","productDescription":"NA","costCenters":[],"links":[{"id":177092,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db6991e3","contributors":{"authors":[{"text":"Rorabaugh, M. I.","contributorId":28221,"corporation":false,"usgs":true,"family":"Rorabaugh","given":"M.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":244493,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16376,"text":"ofr56126 - 1956 - Preliminary report on the geology of San Nicolas Island, California","interactions":[{"subject":{"id":16376,"text":"ofr56126 - 1956 - Preliminary report on the geology of San Nicolas Island, California","indexId":"ofr56126","publicationYear":"1956","noYear":false,"title":"Preliminary report on the geology of San Nicolas Island, California"},"predicate":"SUPERSEDED_BY","object":{"id":6480,"text":"pp369 - 1963 - Geology of San Nicolas Island, California","indexId":"pp369","publicationYear":"1963","noYear":false,"title":"Geology of San Nicolas Island, California"},"id":1}],"supersededBy":{"id":6480,"text":"pp369 - 1963 - Geology of San Nicolas Island, California","indexId":"pp369","publicationYear":"1963","noYear":false,"title":"Geology of San Nicolas Island, California"},"lastModifiedDate":"2024-07-19T22:48:41.844195","indexId":"ofr56126","displayToPublicDate":"1994-01-01T00:00:00","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":"56-126","title":"Preliminary report on the geology of San Nicolas Island, California","docAbstract":"<p>The U. S. Geological Survey, at the request of the Director of Naval Petroleum Reserves, undertook a geologic investigation of San Nicolas Island, Ventura County California, in the spring of 1955. This preliminary report summarizes present knowledge concerning the general stratigraphy and structure of the island. Additional surface and underwater geologic studies are needed to further differentiate lithologic units within the complexly faulted Eocene sequence and to obtain additional data concerning the northwestward extension of the general anticlinal structure of the island.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr56126","collaboration":"Prepared in cooperation with the Office of Naval Petroleum Reserves, Department of the Navy","usgsCitation":"Vedder, J.G., Schoelhamer, J., and Israelsky, M., 1956, Preliminary report on the geology of San Nicolas Island, California: U.S. Geological Survey Open-File Report 56-126, 15 p., https://doi.org/10.3133/ofr56126.","productDescription":"15 p.","costCenters":[],"links":[{"id":431279,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1956/0126/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":147823,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1956/0126/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Nicolas Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -119.58573792836644,\n              33.30759417992911\n            ],\n            [\n              -119.58573792836644,\n              33.20165400149669\n            ],\n            [\n              -119.42994005214368,\n              33.20165400149669\n            ],\n            [\n              -119.42994005214368,\n              33.30759417992911\n            ],\n            [\n              -119.58573792836644,\n              33.30759417992911\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66c930","contributors":{"authors":[{"text":"Vedder, J. G.","contributorId":97873,"corporation":false,"usgs":true,"family":"Vedder","given":"J.","middleInitial":"G.","affiliations":[],"preferred":false,"id":172745,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schoelhamer, J.E.","contributorId":32932,"corporation":false,"usgs":true,"family":"Schoelhamer","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":172744,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Israelsky, M.C.","contributorId":21623,"corporation":false,"usgs":true,"family":"Israelsky","given":"M.C.","email":"","affiliations":[],"preferred":false,"id":906675,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":51894,"text":"ofr5616 - 1956 - Analysis of basic data concerning ground water in the Yuma area, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:11:29","indexId":"ofr5616","displayToPublicDate":"1994-01-01T00:00:00","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":"56-16","title":"Analysis of basic data concerning ground water in the Yuma area, Arizona","language":"ENGLISH","doi":"10.3133/ofr5616","usgsCitation":"Brown, R.H., Harshbarger, J.W., and Thomas, H.E., 1956, Analysis of basic data concerning ground water in the Yuma area, Arizona: U.S. Geological Survey Open-File Report 56-16, 117 p., 2 plates, https://doi.org/10.3133/ofr5616.","productDescription":"117 p., 2 plates","costCenters":[],"links":[{"id":179555,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad0e4b07f02db680a4f","contributors":{"authors":[{"text":"Brown, R. H.","contributorId":19931,"corporation":false,"usgs":false,"family":"Brown","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":244442,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harshbarger, J. W.","contributorId":22309,"corporation":false,"usgs":true,"family":"Harshbarger","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":244443,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thomas, H. E.","contributorId":12829,"corporation":false,"usgs":true,"family":"Thomas","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":244441,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":51884,"text":"ofr561 - 1956 - Sediment data for streams in northwestern California","interactions":[],"lastModifiedDate":"2012-02-02T00:11:29","indexId":"ofr561","displayToPublicDate":"1994-01-01T00:00:00","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":"56-1","title":"Sediment data for streams in northwestern California","language":"ENGLISH","doi":"10.3133/ofr561","usgsCitation":"Ames, F., 1956, Sediment data for streams in northwestern California: U.S. Geological Survey Open-File Report 56-1, 5 p., https://doi.org/10.3133/ofr561.","productDescription":"5 p.","costCenters":[],"links":[{"id":178786,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fc093","contributors":{"authors":[{"text":"Ames, F.C.","contributorId":64232,"corporation":false,"usgs":true,"family":"Ames","given":"F.C.","email":"","affiliations":[],"preferred":false,"id":244429,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":51917,"text":"ofr5675 - 1956 - Surface-water resources of Polecat Creek basin, Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:11:34","indexId":"ofr5675","displayToPublicDate":"1994-01-01T00:00:00","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":"56-75","title":"Surface-water resources of Polecat Creek basin, Oklahoma","docAbstract":"A compilation of basic data on surface waters in Polecat Creek basin is presented on a monthly basis for Heyburn Reservoir and for Polecat Creek at Heyburn, Okla. Chemical analyses are shown for five sites in the basin.\r\nCorrelation of runoff records with those for nearby basins indicates that the average annual runoff of the basin above gaging station at Heyburn is 325 acre-feet per square mile.\r\n\r\nEstimated duration curves of daily flow indicate that under natural conditions there would be no flow in Polecat Creek at Heyburn (drainage area, 129 square miles) about 16 percent of the time on an average, and that the flow would be less than 3 cubic feet per second half of the time. As there is no significant base flow in the basin, comparable low flows during dry-weather periods may be expected in other parts of the basin.\r\n\r\nDuring drought periods Heyburn Reservoir does not sustain a dependable low-water flow in Polecat Creek. Except for possible re-use of the small sewage effluent from city of Sapulpa, dependable supplies for additional water needs on the main stem will require development of supplemental storage.\r\n\r\nThere has been no regular program for collection of chemical quality data in the basin, but miscellaneous analyses indicate a water of suitable quality for municipal and agricultural uses in Heyburn Reservoir and Polecat Creek near Heyburn. One recent chemical analysis indicates the possibility of a salt pollution problem in the Creek near Sapulpa.\r\n\r\n(available as photostat copy only)","language":"ENGLISH","doi":"10.3133/ofr5675","usgsCitation":"Laine, L., 1956, Surface-water resources of Polecat Creek basin, Oklahoma: U.S. Geological Survey Open-File Report 56-75, 20 p., https://doi.org/10.3133/ofr5675.","productDescription":"20 p.","costCenters":[],"links":[{"id":177522,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db623d0e","contributors":{"authors":[{"text":"Laine, L.L.","contributorId":100464,"corporation":false,"usgs":true,"family":"Laine","given":"L.L.","email":"","affiliations":[],"preferred":false,"id":244473,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71911,"text":"tem1012 - 1956 - Pyrite-uranium polycrystal","interactions":[],"lastModifiedDate":"2012-02-02T00:13:58","indexId":"tem1012","displayToPublicDate":"1994-01-01T00:00:00","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":"1012","title":"Pyrite-uranium polycrystal","docAbstract":"A texture was observed in a sample of ore in 'Which pyrite and uraninite occurred as thin alternate layers paralleling crystal faces of a pyrite nucleus. This texture could be formed either by replacement or by syntaxis. Although syntactic growth forming polyerystals of two chemically dissimilar minerals has not been previously described, this explanation fits the observed data better than the explanation offered by replacement. It is proposed, therefore, that this occurrence is an example of a polycrystal of uraninite and pyrite and that the mechanism of formation is syntaxis. \r\n\r\n\r\n","language":"ENGLISH","doi":"10.3133/tem1012","usgsCitation":"King, A., 1956, Pyrite-uranium polycrystal: U.S. Geological Survey Trace Elements Memorandum 1012, 16 p.: ill. ; 27 cm.; 6 figs., https://doi.org/10.3133/tem1012.","productDescription":"16 p.: ill. ; 27 cm.; 6 figs.","numberOfPages":"16","costCenters":[],"links":[{"id":193246,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/1012/report-thumb.jpg"},{"id":91043,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/1012/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db655683","contributors":{"authors":[{"text":"King, A.G.","contributorId":39883,"corporation":false,"usgs":true,"family":"King","given":"A.G.","email":"","affiliations":[],"preferred":false,"id":284884,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":21437,"text":"ofr56134 - 1956 - Geology of southeastern Ventura Basin, Los Angeles County, California","interactions":[{"subject":{"id":21437,"text":"ofr56134 - 1956 - Geology of southeastern Ventura Basin, Los Angeles County, California","indexId":"ofr56134","publicationYear":"1956","noYear":false,"title":"Geology of southeastern Ventura Basin, Los Angeles County, California"},"predicate":"SUPERSEDED_BY","object":{"id":45778,"text":"pp334H - 1962 - Geology of southeastern Ventura basin, Los Angeles County, California","indexId":"pp334H","publicationYear":"1962","noYear":false,"chapter":"H","title":"Geology of southeastern Ventura basin, Los Angeles County, California"},"id":1}],"supersededBy":{"id":45778,"text":"pp334H - 1962 - Geology of southeastern Ventura basin, Los Angeles County, California","indexId":"pp334H","publicationYear":"1962","noYear":false,"title":"Geology of southeastern Ventura basin, Los Angeles County, California"},"lastModifiedDate":"2022-01-21T21:04:09.633051","indexId":"ofr56134","displayToPublicDate":"1994-01-01T00:00:00","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":"56-134","title":"Geology of southeastern Ventura Basin, Los Angeles County, California","docAbstract":"<p>The Ventura Basin (see index map, fig. 1) has long been one of the important oil-producing districts of California. The eastern part of the Basin includes some of the oldest oil fields in the state and also several of those most recently discovered. Since 1937 several new fields have been discovered in the area and doubtless more oil remains to be found.</p><p>The first work of the U. S. Geological Survey in this region was reported by G. H. Eldridge and Ralph Arnold in Bulletin 309 (1907). The Survey's Bulletin 753 by W. S. W. Kew (1924) described part of the region studied by Eldridge and Arnold as well as much of the remainder of the Ventura Basin. Since the publication of Kew's report, and especially since 1937 when the Newhall-Potrero oil field was discovered, interest in the eastern part of the Ventura Basin has steadily increased.</p><p>The present report covers a small part of Kew's area on the larger scale of 1:12,000 (see index map, fig. 1). Attention is focused on the outcrop geology, particularly the stratigraphy. Subsurface data were collected where available, but they are incomplete.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr56134","usgsCitation":"Winterer, E.L., 1956, Geology of southeastern Ventura Basin, Los Angeles County, California: U.S. Geological Survey Open-File Report 56-134, Report: v, 141 p.; 12 Plates: 41.54 x 59.04 inches or smaller; 2 Figures; 6 Tables, https://doi.org/10.3133/ofr56134.","productDescription":"Report: v, 141 p.; 12 Plates: 41.54 x 59.04 inches or smaller; 2 Figures; 6 Tables","costCenters":[],"links":[{"id":394721,"rank":23,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1956/0134/table-6.pdf","text":"Table 6","linkFileType":{"id":1,"text":"pdf"}},{"id":394720,"rank":22,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1956/0134/table-5.pdf","text":"Table 5","linkFileType":{"id":1,"text":"pdf"}},{"id":394718,"rank":21,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1956/0134/table-4.pdf","text":"Table 4","linkFileType":{"id":1,"text":"pdf"}},{"id":394717,"rank":20,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1956/0134/table-3.pdf","text":"Table 3","linkFileType":{"id":1,"text":"pdf"}},{"id":394714,"rank":19,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1956/0134/table-2.pdf","text":"Table 2","linkFileType":{"id":1,"text":"pdf"}},{"id":394713,"rank":18,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1956/0134/table-1.pdf","text":"Table 1","linkFileType":{"id":1,"text":"pdf"}},{"id":394712,"rank":17,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1956/0134/figure-2.pdf","text":"Figure 2","linkFileType":{"id":1,"text":"pdf"}},{"id":394711,"rank":16,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1956/0134/figure-1.pdf","text":"Figure 1","linkFileType":{"id":1,"text":"pdf"}},{"id":394710,"rank":15,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1956/0134/plate-12.pdf","text":"Plate 12","linkFileType":{"id":1,"text":"pdf"}},{"id":394709,"rank":14,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1956/0134/plate-11.pdf","text":"Plate 11","linkFileType":{"id":1,"text":"pdf"}},{"id":394708,"rank":13,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1956/0134/plate-10.pdf","text":"Plate 10","linkFileType":{"id":1,"text":"pdf"}},{"id":394707,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1956/0134/plate-9.pdf","text":"Plate 9","linkFileType":{"id":1,"text":"pdf"}},{"id":394706,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1956/0134/plate-8.pdf","text":"Plate 8","linkFileType":{"id":1,"text":"pdf"}},{"id":394705,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1956/0134/plate-7.pdf","text":"Plate 7","linkFileType":{"id":1,"text":"pdf"}},{"id":394703,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1956/0134/plate-5.pdf","text":"Plate 5","linkFileType":{"id":1,"text":"pdf"}},{"id":394701,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1956/0134/plate-3.pdf","text":"Plate 3","linkFileType":{"id":1,"text":"pdf"}},{"id":394696,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1956/0134/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":154660,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1956/0134/report-thumb.jpg"},{"id":394699,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1956/0134/plate-1-2.pdf","text":"Plate 1 Sheet 2","linkFileType":{"id":1,"text":"pdf"}},{"id":394702,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1956/0134/plate-4.pdf","text":"Plate 4","linkFileType":{"id":1,"text":"pdf"}},{"id":394704,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1956/0134/plate-6.pdf","text":"Plate 6","linkFileType":{"id":1,"text":"pdf"}},{"id":394700,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1956/0134/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"}},{"id":394698,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1956/0134/plate-1-1.pdf","text":"Plate 1 Sheet 1","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"Los Angeles County","otherGeospatial":"Ventura Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.73199462890626,\n              34.286722590335955\n            ],\n      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,{"id":51916,"text":"ofr5670 - 1956 - Water levels in observation wells in Nebraska during 1955","interactions":[],"lastModifiedDate":"2018-11-08T15:42:49","indexId":"ofr5670","displayToPublicDate":"1994-01-01T00:00:00","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":"56-70","title":"Water levels in observation wells in Nebraska during 1955","docAbstract":"<p>The objective of the dbservation-well program in Nebraska is to provide an evaluation of the status of the ground-water supplies. Many uses for water-.level data are known but not all potential uses can be forseen. Among the important uses are the following:</p><ol><li>To indicate the status of ground water in storage or in transit and the availability of supplies.<br></li><li>To show the trend of ground-water supplies and the outlook for the future.<br></li><li>To estimate or forcast the base flow of streams.<br></li><li>To indicate areas in which the water level is approaching too close to the land surface (water-logging) or is receding toward economic limits of lift or tow rd impairment by water of poor quality.<br></li><li>To provide long-term vidence for evaluating the effectiveness of land-management and water...0 nservation programs in relation to water conservation actually of ected, and for use in basin or \"watershed\" studies.<br></li><li>To provide longterm ontinuous records to serve as a framework to which short-term records collected during intensive investigation may be related.<br></li></ol><p>The water level in an observation well functions as a gage to indicate the position of the water table o The water table is defined as the upper surface of the zone of saturation except where that surface is formed by overlying impermeable materials. The water table is also the boundary between the zone of saturation and the zone of aeration. It is not a level surface but is a sloping surface that has many irregularities, and it often conforms in a general way to the land surface. The irregularities are caused by several factors. In places where the recharge to the ground-water reservoir is exceptionally large, the water-table may rise to form a mound from which the water slowly spreads. Depressions or troughs in the water table indicate places where the ground water is discharging, as along streams that are below the normal level of the water table, or indicate places where water is being withdrawn by wells or vegetation.</p><p>The several factors that influence the water table vary in fact and amount from time to time because of changes in weather and the water requirements of vegetation and man; thus, the water table is nearly always rising or falling.</p><p>The fluctuations of the water table are shown by the changes in water levels in wells. Thus, the rate and amount of the fluctuation of the water table can be ascertained by observing the water levels in wells, and the magnitude of the several factors effecting the position of the water table can be interpreted by analyzing the water—level data.</p><p>Water-level measurements are given, in this report, in feet below the land surface at the well site. Water levels that are above land surface are preceded by a plus (+) sign, whereas those below land surface have no sign but are understood to be minus (-). The words \"land-surface datum\" are abbreviated \"lsd\" in tables of this report.</p><p>The altitude above mean sea level (msl) of the land surface at many of the well sites has been determined and is included in the tables of this report.</p><p>Lower case letters which appear in the table of water level measurements indicate the following: 6', nearby well pumped recently; f, dry; g, measured by outside agency; and j, frozen.</p><p>Twenty-.six observation wells in Nebraska are equipped with recording gages. Each recording gage produces a continuous graph of water-level fluctuations in the well. Only the lowest water level on the last day of record in each month, as recorded by the gage, is given in this report; the complete record is on file in the office of the U. S. Geological Survey in Lincoln, Nebr.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5670","usgsCitation":"Keech, C., 1956, Water levels in observation wells in Nebraska during 1955: U.S. Geological Survey Open-File Report 56-70, xiv, 106 p., https://doi.org/10.3133/ofr5670.","productDescription":"xiv, 106 p.","numberOfPages":"121","costCenters":[],"links":[{"id":359340,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1956/0070/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":177432,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1956/0070/report-thumb.jpg"}],"country":"United 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9c90","contributors":{"authors":[{"text":"Keech, C.F.","contributorId":67941,"corporation":false,"usgs":true,"family":"Keech","given":"C.F.","email":"","affiliations":[],"preferred":false,"id":244472,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":12908,"text":"ofr5623 - 1956 - Drilling data in the Montfort, Rewey, Mifflin, Belmont, and Calamine quadrangles, Wisconsin","interactions":[],"lastModifiedDate":"2019-06-28T11:10:01","indexId":"ofr5623","displayToPublicDate":"1994-01-01T00:00:00","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":"56-23","title":"Drilling data in the Montfort, Rewey, Mifflin, Belmont, and Calamine quadrangles, Wisconsin","docAbstract":"<p>Sixty-six churn drill holes aggregating 10,351 feet were drilled in the fall of 1955 in the zinc-lead district of southwestern Wisconsin (fig. 1). This drilling was part of a cooperative program of geologic mapping by the U. S. Geological Survey and the Wisconsin Geologic and Natural History Survey.</p><p>The holes penetrate the Maquoketa, Galena, Decorah, and Platteville formations of Late and Middle Ordovician age in areas of sparse outcrop and subsurface information. They provide basic data for stratigraphic study and for the projection of geologic structures in these areas. Exact location of the holes is shown in figs. 2, 3, 4, 5, and 6.</p><p>Generalized descriptive logs of the 66 holes were prepared mainly from driller's logs, and from a field study of the drill cuttings by J. E. Carlson. Where delineation of the formations drilled was difficult in the field, the cuttings were examined by binocular microscope. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5623","collaboration":"Prepared in cooperation with the Wisconsin Geological and Natural History Survey","usgsCitation":"Carlson, J.E., 1956, Drilling data in the Montfort, Rewey, Mifflin, Belmont, and Calamine quadrangles, Wisconsin: U.S. Geological Survey Open-File Report 56-23, Report: iv, 70 p.; 5 Plates: 21.90 x 27.24 inches or smaller, https://doi.org/10.3133/ofr5623.","productDescription":"Report: iv, 70 p.; 5 Plates: 21.90 x 27.24 inches or smaller","costCenters":[],"links":[{"id":146190,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1956/0023/report-thumb.jpg"},{"id":365138,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1956/0023/figure-2.pdf","text":"Figure 2","linkFileType":{"id":1,"text":"pdf"}},{"id":365137,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1956/0023/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":365139,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1956/0023/figure-3.pdf","text":"Figure 3","linkFileType":{"id":1,"text":"pdf"}},{"id":365140,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1956/0023/figure-4.pdf","text":"Figure 4","linkFileType":{"id":1,"text":"pdf"}},{"id":365141,"rank":6,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1956/0023/figure-5.pdf","text":"Figure 5","linkFileType":{"id":1,"text":"pdf"}},{"id":365142,"rank":7,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1956/0023/figure-6.pdf","text":"Figure 6","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","datum":"Mean Sea Level","country":"United States","state":"Wisconsin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -90.5,\n              42.625\n            ],\n            [\n              -90.125,\n              42.625\n            ],\n            [\n              -90.125,\n              43\n            ],\n            [\n              -90.5,\n              43\n            ],\n            [\n              -90.5,\n              42.625\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd55d5e4b0b290850f68e0","contributors":{"authors":[{"text":"Carlson, John Edward","contributorId":49803,"corporation":false,"usgs":true,"family":"Carlson","given":"John","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":166936,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2815,"text":"wsp1360A - 1956 - Reservoirs in the United States","interactions":[{"subject":{"id":3831,"text":"cir23 - 1948 - Reservoirs in the United States","indexId":"cir23","publicationYear":"1948","noYear":false,"title":"Reservoirs in the United States"},"predicate":"SUPERSEDED_BY","object":{"id":2815,"text":"wsp1360A - 1956 - Reservoirs in the United States","indexId":"wsp1360A","publicationYear":"1956","noYear":false,"chapter":"A","title":"Reservoirs in the United States"},"id":1}],"lastModifiedDate":"2024-11-27T14:54:57.46166","indexId":"wsp1360A","displayToPublicDate":"1994-01-01T00:00:00","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":"1360","chapter":"A","title":"Reservoirs in the United States","docAbstract":"<p>Reservoir storage facilities in the United States play an important part in the national economy. Storage facilities have enabled the country to utilize to a much fuller extent one of the most valuable natural resources: water. During recent years the construction of reservoirs has continued at a high rate. This report shows the status of these facilities on January 1, 1954, and describes briefly some of the reasons for growth of reservoir facilities in the United States. </p><p>Descriptive data are given for reservoirs having a capacity of 5, 000 acre-feet or more and for natural lakes having a usable capacity of 5,000 acre-feet or more. Included are reservoirs and lakes completed as of January 1, 1954, and reservoirs under construction on that date. The total number of such reservoirs and lakes is 1, 300. </p><p>A descriptive list of reservoirs in the United States was first published by the United States Geological Survey in March 1948. That report, Geological Survey Circular 23, entitled Reservoirs in the United States, included reservoirs completed as of January 1, 1947. Since January 1, 1947, reservoirs representing a total usable capacity of 115,000,000 acre-feet, or an increase of 71 percent, have been constructed or are under construction. Data about these new reservoirs are presented herein, and the data shown for reservoirs constructed before 1947 have been corrected on the basis of the latest available survey to determine reservoir capacity. </p><p>The total usable capacity of reservoirs and lakes included in this compilation amounts to 278, 120, 000 acre-feet, and the corresponding surface area totals 11, 046, 000 acres. </p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1955 (Water Supply Paper 1360)","largerWorkSubtype":{"id":1,"text":"Federal Government Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1360A","usgsCitation":"Thomas, N., and Harbeck, G.E., 1956, Reservoirs in the United States: U.S. Geological Survey Water Supply Paper 1360, Report: v, 99 p.; 9 Plates (in 10 Sheets): 50.19 x 33.95 inches or smaller, https://doi.org/10.3133/wsp1360A.","productDescription":"Report: v, 99 p.; 9 Plates (in 10 Sheets): 50.19 x 33.95 inches or smaller","numberOfPages":"106","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":29364,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1360a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138823,"rank":2,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1360a/report-thumb.jpg"},{"id":276482,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360a/plate-01.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map of United States showing drainage areas and index numbers"}],"country":"United States","publicComments":"Subtitle: <i>Revising and superseding Geological Survey Circular 23, Reservoirs in the United States, by G. Earl Harbeck, Jr.: March 1948</i>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a55e4b07f02db62c697","contributors":{"authors":[{"text":"Thomas, N.O.","contributorId":99962,"corporation":false,"usgs":true,"family":"Thomas","given":"N.O.","email":"","affiliations":[],"preferred":false,"id":145844,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harbeck, G. Earl Jr.","contributorId":18736,"corporation":false,"usgs":true,"family":"Harbeck","given":"G.","suffix":"Jr.","email":"","middleInitial":"Earl","affiliations":[],"preferred":false,"id":145843,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":71135,"text":"tem1000 - 1956 - An inferred relationship between some uranium deposits and calcium carbonate cement in southern Black Hills, South Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:13:47","indexId":"tem1000","displayToPublicDate":"1994-01-01T00:00:00","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":"1000","title":"An inferred relationship between some uranium deposits and calcium carbonate cement in southern Black Hills, South Dakota","docAbstract":"Evidence resulting from geologic mapping in the southern Black Hills indicates that the areas marginal to some of the larger carbonate-cemented sandstones constitute favorable geochemical environments for the localization of uranium deposits. To determine whether these favorable environments are predictable a limited experimental core-drilling program was carried out. An extensive deposit was discovered in an area marginal to a sandstone well-cemented with calcium carbonate. The deposit has not yet been developed, but from the available data it appears that there is a significant quantity of mineralized rock present containing as much as 3.0 percent eU3O8. \r\n\r\n\r\n","language":"ENGLISH","doi":"10.3133/tem1000","usgsCitation":"Gott, G.B., 1956, An inferred relationship between some uranium deposits and calcium carbonate cement in southern Black Hills, South Dakota: U.S. Geological Survey Trace Elements Memorandum 1000, 15 p.; 3 figs. (one in envelope); 1 table, https://doi.org/10.3133/tem1000.","productDescription":"15 p.; 3 figs. (one in envelope); 1 table","numberOfPages":"15","costCenters":[],"links":[{"id":186648,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/1000/report-thumb.jpg"},{"id":90536,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/1000/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db6845b8","contributors":{"authors":[{"text":"Gott, Garland B.","contributorId":8837,"corporation":false,"usgs":true,"family":"Gott","given":"Garland","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":283700,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24329,"text":"ofr56100 - 1956 - Data on water wells in Lucerne, Johnson, Fry, and Means Valleys, San Bernardino County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:18","indexId":"ofr56100","displayToPublicDate":"1994-01-01T00:00:00","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":"56-100","title":"Data on water wells in Lucerne, Johnson, Fry, and Means Valleys, San Bernardino County, California","language":"ENGLISH","publisher":"United States Department of the Interior, Geological Survey, Ground Water Branch,","doi":"10.3133/ofr56100","issn":"0094-9140","usgsCitation":"Riley, F.S., 1956, Data on water wells in Lucerne, Johnson, Fry, and Means Valleys, San Bernardino County, California: U.S. Geological Survey Open-File Report 56-100, 150 p. :map ;27 cm., https://doi.org/10.3133/ofr56100.","productDescription":"150 p. :map ;27 cm.","costCenters":[],"links":[{"id":157418,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1956/0100/report-thumb.jpg"},{"id":53434,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1956/0100/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53435,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1956/0100/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b59f","contributors":{"authors":[{"text":"Riley, Francis S.","contributorId":93028,"corporation":false,"usgs":true,"family":"Riley","given":"Francis","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":191700,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71656,"text":"tei638 - 1956 - Host rocks and their alterations as related to uranium-bearing veins in the United States","interactions":[],"lastModifiedDate":"2014-07-15T08:02:17","indexId":"tei638","displayToPublicDate":"1994-01-01T00:00:00","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":"638","title":"Host rocks and their alterations as related to uranium-bearing veins in the United States","docAbstract":"<p>This paper, dealing with the different kinds of host rocks and their alterations associated with uranium-bearing veins in the United States, is a chapter of a comprehensive report entitled , \"Geology of uranium-bearing vein deposits in the United States,\" in preparation by George W. Walker, Frank W. Osterwald, and others. The comprehensive report will include detailed information on tectonic and structural setting, kinds of host rocks, wall-rock alteration, mineralogy, physical characteristics, processes of deposition, and concepts of origin of uraniferous veins; but, because it will not be completed until sometime in the future, some chapters of the report are being transmitted as they are finished. Part of an introductory chapter to the comprehensive report entitled, \"Classification and distribution of uranium-bearing veins in the United States\" (Walker and Osterwald, 1956) has already been transmitted; several of the terms used herein are defined in the introductory chapter.</p>\n<br>\n<p>Data included in this chapter demonstrate that uranium-bearing veins are: 1) in rocks of nearly all textural, chemical, and mineralogic types;  2) most abundant in holocrystalline, commonly equigranular, igeneous and metamorphic rocks characterized by a moderate to high silica content and and by similar physical properties. Although some of the physiochemical properties of the host rocks are discussed in terms of favorability or nonfavoribility for uranium deposition, the principal purpose of this chapter is to establish the petroloic environment in which uranium-bearing veins have been found. Because favorability or nonfavorability of host rocks is related complexly to the chemistry of ore solutions and to methods or uranium transport and deposition, several hypothetical processes of transport and deposition have been referred to briefly; these and other hypotheses will be outlines and discussed in greater detail in a subsequent chapter.</p>\n<br>\n<p>The compilation of data leading to this report and its preparation by a member of the Uranium Research and Resource Section, U.S. Geological Survey, was done on behalf of the Division of Raw Materials, U.S. Atomic Energy Commission. The report is based on both published and unpublished information collected principally by personnel of the U.S. Geological Survey, the U.S. Atomic Energy Commission or its predecessor organization, the Manhattan Engineer District, and to a lesser extent by staff members of other Federal or State agencies and by geologists in private industry. Information concerning foreign uranium-bearing vein deposits has been extracted almost exclusively from published reports; references to these and other data are included at appropriate places.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei638","collaboration":"The report concerns works done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Walker, G.W., 1956, Host rocks and their alterations as related to uranium-bearing veins in the United States: U.S. Geological Survey Trace Elements Investigations 638, 59 p., https://doi.org/10.3133/tei638.","productDescription":"59 p.","numberOfPages":"61","costCenters":[],"links":[{"id":290077,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":290076,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0638/report.pdf"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.8,24.5 ], [ -124.8,49.383333 ], [ -66.95,49.383333 ], [ -66.95,24.5 ], [ -124.8,24.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6880de","contributors":{"authors":[{"text":"Walker, George W.","contributorId":101308,"corporation":false,"usgs":true,"family":"Walker","given":"George","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":284552,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71599,"text":"tei575 - 1956 - X-ray powder data for uranium and thorium minerals","interactions":[],"lastModifiedDate":"2014-06-19T06:52:31","indexId":"tei575","displayToPublicDate":"1994-01-01T00:00:00","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":"575","title":"X-ray powder data for uranium and thorium minerals","docAbstract":"<p>The U.S. Geological Survey has in preparation a comprehensive volume on the mineralogy of uranium and thorium. This work has been done as part of a continuing systematic survey of data on uranium and thorium minerals on behalf of the Division of Raw Materials, U.S. Atomic Energy Commission.</p>\n<br/>\n<p>Pending publication of this volume and in response to a widespread demand among workers in uranium and thorium mineralogy, the X-ray powder diffraction data for the known minerals that contain uranium or thorium as an essential constituent are presented here. The coverage is complete except for a few minerals for which there are no reliable data owing to lack of authentic specimens.</p>\n<br/>\n<p>With the exception of that for ianthinite, the new data either originated in the Geological Survey or in the Mineralogical Laboratory of Harvard University. Data from the literature or other sources were cross-checked against the files of standard patterns of these laboratories; the sources are indicated in the references. Data not accompanied by a reference were obtained from films in the Harvard Standard File and cross-checked as to the identity of the film with the Geological Survey's file.</p>\n<br/>\n<p>Minor differences can be expected in the d-spacings reported for the same specimens by different investigators because of the manner of preparation of the mount, the conditions of X-ray irradiation, and the method of photography and measurement of the film or chart. The Harvard and Geological Survey data all were obtained from films taken in 114-mm diameter cameras, using either ethyl cellulose and toluene or collodion spindle mounts and Straumanis-type film mounting. Unless otherwise indicated all patterns were taken with copper radiation (Kα 1.5418 A.) and nickel filter and data are given in Angstrom units. The d-spacings are not corrected for film shrinkage. The correction ordinarily is small and in general is less than either the variation in spacing arising from differences in experimental technique of different investigators, including the varying absorption of samples of different thickness and concentration, or the variation attending slight changes in the chemical composition of the mineral.</p>\n<br/>\n<p>Some uranium minerals give poor diffraction patterns. The best results are generally obtained by using relatively small diameter spindles and long exposures, with a take-off angle from teh X-ray tube of about 4°. It is sometimes advantageous to shield the film from fluorescence in the visible region excited by X-ray irradiation. Copper radiation is preferable. The patterns of a few uranium minerals are greatly impaired by heavy grinding of the sample. Light crushing of the coarse sample after mixing with about one-third its volume of coarsely powdered low-absorption glass is helpful.</p>\n<br/>\n<p>Many uranium minerals, such as the members of the torbernite group, readily lose zeolithic water or transform to lower hydrates at or near ordinary conditions of temperature and humidity and care should be taken to control this in the manner of preservation and preparation of the sample.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei575","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission.","usgsCitation":"Frondel, C., Riska, D., and Frondel, J.W., 1956, X-ray powder data for uranium and thorium minerals: U.S. Geological Survey Trace Elements Investigations 575, 96 p., https://doi.org/10.3133/tei575.","productDescription":"96 p.","numberOfPages":"101","costCenters":[],"links":[{"id":288867,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":288866,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0575/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de662","contributors":{"authors":[{"text":"Frondel, Clifford","contributorId":47002,"corporation":false,"usgs":true,"family":"Frondel","given":"Clifford","email":"","affiliations":[],"preferred":false,"id":284451,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Riska, Daphne","contributorId":106179,"corporation":false,"usgs":true,"family":"Riska","given":"Daphne","affiliations":[],"preferred":false,"id":284453,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Frondel, Judith Weiss","contributorId":55810,"corporation":false,"usgs":true,"family":"Frondel","given":"Judith","email":"","middleInitial":"Weiss","affiliations":[],"preferred":false,"id":284452,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":15664,"text":"ofr56101 - 1956 - Magnetite deposits near Klukwan and Haines, southeastern Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:06:47","indexId":"ofr56101","displayToPublicDate":"1994-01-01T00:00:00","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":"56-101","title":"Magnetite deposits near Klukwan and Haines, southeastern Alaska","docAbstract":"Low-grade iron ore is found in magnetite-bearing pyroxenite bodies near Klukwan and Haines in Southeastern Alaska. An alluvial fan at Haines also contains magnetite-bearing rock of possible economic significance. \r\n\r\nThe Haines-Klukwan area is underlain by rocks of Mesozoic Including epidote diorite, quartz diorite, and alaskite of the Coast Range batholith, metabasalt (recrystallized lava flows and pyroclastic rocks), and, in the southern part, interbedded slate and limestone. Layering and foliation, where perceptible, generally strike northwest and dip steeply northeast. The iron deposits are found at or near the contact between the metabasalt and epidote diorite; they appear to represent highly-altered lava flows that were metamorphosed during the emplacement of the batholith. Several billion tens of rock containing about 13 percent magnetic iron are included in the pyroxenite body at Klukwan. Sampling and dip-needle data suggest the presence there of two or three tabular aches in which the rock has an average magnetic iron content of 20 percent or more. Pyroxenite bodies outcropping in three areas near Haines apparently are lower in grade than the Klukwan deposit; lack of exposures prevented thorough sampling but reconnaissance traverses with a dip needle failed to reveal important zones of high-grade iron ore.\r\n\r\nAn alluvial fan adjoining the pyroxenite body at Klukwan contains several hundred million tons of broken rock having a magneticiron content of about 10 percent.","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr56101","usgsCitation":"Robertson, E.C., 1956, Magnetite deposits near Klukwan and Haines, southeastern Alaska: U.S. Geological Survey Open-File Report 56-101, 37 p. ill., maps (some folded) ;27 cm., https://doi.org/10.3133/ofr56101.","productDescription":"37 p. ill., maps (some folded) ;27 cm.","costCenters":[],"links":[{"id":146540,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1956/0101/report-thumb.jpg"},{"id":44627,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1956/0101/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44628,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1956/0101/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44629,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1956/0101/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44630,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1956/0101/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44631,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1956/0101/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44632,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1956/0101/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44633,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1956/0101/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a74e4b07f02db644465","contributors":{"authors":[{"text":"Robertson, Eugene C.","contributorId":71139,"corporation":false,"usgs":true,"family":"Robertson","given":"Eugene","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":171519,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23627,"text":"ofr5673 - 1956 - Data on water wells in Cuddeback, Superior, and Harper Valleys, San Bernardino County, California","interactions":[{"subject":{"id":23627,"text":"ofr5673 - 1956 - Data on water wells in Cuddeback, Superior, and Harper Valleys, San Bernardino County, California","indexId":"ofr5673","publicationYear":"1956","noYear":false,"title":"Data on water wells in Cuddeback, Superior, and Harper Valleys, San Bernardino County, California"},"predicate":"SUPERSEDED_BY","object":{"id":70046751,"text":"70046751 - 1971 - Water wells in the Harper, Superior, and Cuddeback Valley areas, San Bernardino County, California","indexId":"70046751","publicationYear":"1971","noYear":false,"title":"Water wells in the Harper, Superior, and Cuddeback Valley areas, San Bernardino County, California"},"id":1}],"supersededBy":{"id":70046751,"text":"70046751 - 1971 - Water wells in the Harper, Superior, and Cuddeback Valley areas, San Bernardino County, California","indexId":"70046751","publicationYear":"1971","noYear":false,"title":"Water wells in the Harper, Superior, and Cuddeback Valley areas, San Bernardino County, California"},"lastModifiedDate":"2013-07-01T14:18:34","indexId":"ofr5673","displayToPublicDate":"1994-01-01T00:00:00","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":"56-73","title":"Data on water wells in Cuddeback, Superior, and Harper Valleys, San Bernardino County, California","language":"ENGLISH","publisher":"United States Department of the Interior Geological Survey, Ground Water Branch,","doi":"10.3133/ofr5673","issn":"0094-9140","usgsCitation":"Kunkel, F., 1956, Data on water wells in Cuddeback, Superior, and Harper Valleys, San Bernardino County, California: U.S. Geological Survey Open-File Report 56-73, 73 p. :map ;27 cm., https://doi.org/10.3133/ofr5673.","productDescription":"73 p. :map ;27 cm.","costCenters":[],"links":[{"id":154930,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b592","contributors":{"authors":[{"text":"Kunkel, Fred","contributorId":47766,"corporation":false,"usgs":true,"family":"Kunkel","given":"Fred","email":"","affiliations":[],"preferred":false,"id":190445,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71654,"text":"tei636 - 1956 - Abundance and distribution of uranium and thorium in zircon, sphene, apatite, epidote, and monazite in granitic rocks","interactions":[],"lastModifiedDate":"2015-10-20T13:05:04","indexId":"tei636","displayToPublicDate":"1994-01-01T00:00:00","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":"636","title":"Abundance and distribution of uranium and thorium in zircon, sphene, apatite, epidote, and monazite in granitic rocks","docAbstract":"<p>Analyses were made of uranium and thorium in ziircon, sphene, apatite, epidote, and monazite separated as accessory minerals from samples of granitic rock from widely scattered localities to indicate the abundance and distribution of these two elements among the five mineral phases. &nbsp;For any pair of mineral phases the distribution ratio remains within the same order of magnitude over the different rocks tested, although the variability of the data is such that only wide departures from constancy could be ascertained. &nbsp;Such gross differences have not been found.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/tei636","usgsCitation":"Hurley, P.M., and Fairbairn, H.W., 1956, Abundance and distribution of uranium and thorium in zircon, sphene, apatite, epidote, and monazite in granitic rocks: U.S. Geological Survey Trace Elements Investigations 636, 20 p., https://doi.org/10.3133/tei636.","productDescription":"20 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":310156,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei636.PNG"},{"id":90903,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/636/report.pdf","text":"Report","size":"5.77 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a382c","contributors":{"authors":[{"text":"Hurley, Patrick M.","contributorId":12121,"corporation":false,"usgs":true,"family":"Hurley","given":"Patrick","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":284548,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fairbairn, Harold W.","contributorId":22627,"corporation":false,"usgs":true,"family":"Fairbairn","given":"Harold","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":284549,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":71650,"text":"tei632 - 1956 - Occurrence of selenium in sulfides from some sedimentary rocks of the western United States","interactions":[],"lastModifiedDate":"2014-07-15T07:47:15","indexId":"tei632","displayToPublicDate":"1994-01-01T00:00:00","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":"632","title":"Occurrence of selenium in sulfides from some sedimentary rocks of the western United States","docAbstract":"<p>Investigations of the minor- and trace-element content of sulfides associated with uranium ore deposits from sandstone-type deposits have shown that selenium commonly substitutes for sulfur. The Morrison formation and Entrada sandstone of Jurassic age and the Wind River formation of Eocene age seem to be seleniferous stratigraphic zones; sulfides deposited within these formations generally contain abnormal amounts of selenium. The selenium content of the pyrite, marcasite, and chalcocite is much greater than that reported in previously published data.</p>\n<br>\n<p>Under the prevailing temperatures and pressures of formation of the Colorado Plateau uranium deposits the maximum amount of Se substituting for S in the pyrite structure was found to be 3 percent by weight. Ferroselite, the iron selenide (FeSe<sub>2</sub>), was found in two deposits on the Colorado Plateau and it was also established that galena (PbS) forms an isomorphous series with clausthalite (PbSe) in nature.</p>\n<br>\n<p>During oxidation of the selenium-bearing sulfides and selenides in the Colorado Plateau and Wyoming, the selenium forms pinkish crusts of either monoclinic or hexagonal native selenium intergrown with soluble sulfates, suggesting that under \"normal\" oxidizing conditions native selenium is more stable than selenites or selenates.</p>\n<br>\n<p>The above-normal selenium content of these sulfides from sedimentary rocks of Mesozoic and Tertiary age is significant. The high selenium in these sulfides is related to periods of volcanic and intrusive activity penecontemporaneous with the formation of the containing sediments.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei632","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Coleman, R.G., and Delevaux, M., 1956, Occurrence of selenium in sulfides from some sedimentary rocks of the western United States: U.S. Geological Survey Trace Elements Investigations 632, 54 p., https://doi.org/10.3133/tei632.","productDescription":"54 p.","numberOfPages":"55","costCenters":[],"links":[{"id":290069,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":290068,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0632/report.pdf"}],"country":"United States","state":"Arizona;Colorado;New Mexico;Utah;Wyoming","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.05,34.61 ], [ -114.05,45.0 ], [ -103.97,45.0 ], [ -103.97,34.61 ], [ -114.05,34.61 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db69216a","contributors":{"authors":[{"text":"Coleman, Robert G.","contributorId":88022,"corporation":false,"usgs":true,"family":"Coleman","given":"Robert","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":284541,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Delevaux, Maryse","contributorId":104577,"corporation":false,"usgs":true,"family":"Delevaux","given":"Maryse","affiliations":[],"preferred":false,"id":284542,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":34407,"text":"b1036G - 1956 - X-ray powder data for uranium and thorium minerals","interactions":[],"lastModifiedDate":"2012-02-02T00:09:26","indexId":"b1036G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1956","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1036","chapter":"G","title":"X-ray powder data for uranium and thorium minerals","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1036G","usgsCitation":"Frondel, C., Riska, D., and Frondel, J.W., 1956, X-ray powder data for uranium and thorium minerals: U.S. Geological Survey Bulletin 1036, p. 91-153  ;24 cm., https://doi.org/10.3133/b1036G.","productDescription":"p. 91-153  ;24 cm.","costCenters":[],"links":[{"id":163783,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1036g/report-thumb.jpg"},{"id":62334,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1036g/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de62a","contributors":{"authors":[{"text":"Frondel, Clifford","contributorId":47002,"corporation":false,"usgs":true,"family":"Frondel","given":"Clifford","email":"","affiliations":[],"preferred":false,"id":212917,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Riska, Daphne","contributorId":106179,"corporation":false,"usgs":true,"family":"Riska","given":"Daphne","affiliations":[],"preferred":false,"id":212919,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Frondel, Judith Weiss","contributorId":55810,"corporation":false,"usgs":true,"family":"Frondel","given":"Judith","email":"","middleInitial":"Weiss","affiliations":[],"preferred":false,"id":212918,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":16607,"text":"ofr57124 - 1956 - Geology and ore deposits of the Monument Valley area, Apache and Navajo Counties, Arizona","interactions":[{"subject":{"id":16607,"text":"ofr57124 - 1956 - Geology and ore deposits of the Monument Valley area, Apache and Navajo Counties, Arizona","indexId":"ofr57124","publicationYear":"1956","noYear":false,"title":"Geology and ore deposits of the Monument Valley area, Apache and Navajo Counties, Arizona"},"predicate":"SUPERSEDED_BY","object":{"id":36300,"text":"b1103 - 1963 - Geology and uranium-vanadium deposits of the Monument Valley area, Apache and Navajo Counties, Arizona","indexId":"b1103","publicationYear":"1963","noYear":false,"title":"Geology and uranium-vanadium deposits of the Monument Valley area, Apache and Navajo Counties, Arizona"},"id":1}],"supersededBy":{"id":36300,"text":"b1103 - 1963 - Geology and uranium-vanadium deposits of the Monument Valley area, Apache and Navajo Counties, Arizona","indexId":"b1103","publicationYear":"1963","noYear":false,"title":"Geology and uranium-vanadium deposits of the Monument Valley area, Apache and Navajo Counties, Arizona"},"lastModifiedDate":"2025-08-08T16:28:38.737151","indexId":"ofr57124","displayToPublicDate":"1994-01-01T00:00:00","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":"57-124","title":"Geology and ore deposits of the Monument Valley area, Apache and Navajo Counties, Arizona","docAbstract":"<p>In 1951 the U.S. Geological Survey undertook a program of uranium investigations in Apache and Navajo Counties, northeastern Arizona. The work had three major objectives. The first was to accumulate data basic to an understanding of the regional geology. The second was to appraise the Triassic strata as host rocks for uranium deposits, and to select areas favorable for exploration for concealed deposits. The third objective was to study the controls that influence uranium deposition and from this study, to establish guides useful in prospecting for uranium deposits.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr57124","usgsCitation":"Witkind, I.J., 1956, Geology and ore deposits of the Monument Valley area, Apache and Navajo Counties, Arizona: U.S. Geological Survey Open-File Report 57-124, Report: 222 p.; 4 Tables: 23.51 x 23.27 inches or smaller; 6 Figures: 26.28 x 86.28 inches or smaller, https://doi.org/10.3133/ofr57124.","productDescription":"Report: 222 p.; 4 Tables: 23.51 x 23.27 inches or smaller; 6 Figures: 26.28 x 86.28 inches or smaller","costCenters":[],"links":[{"id":493855,"rank":5,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1957/0124/table-6.pdf","text":"Table 6","linkFileType":{"id":1,"text":"pdf"}},{"id":493854,"rank":4,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1957/0124/table-5.pdf","text":"Table 5","linkFileType":{"id":1,"text":"pdf"}},{"id":493860,"rank":10,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1957/0124/figure-3-1.pdf","text":"Figure 3-1","linkFileType":{"id":1,"text":"pdf"}},{"id":493859,"rank":9,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1957/0124/figure-3-2.pdf","text":"Figure 3-2","linkFileType":{"id":1,"text":"pdf"}},{"id":493853,"rank":3,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1957/0124/table-1.pdf","text":"Table 1","linkFileType":{"id":1,"text":"pdf"}},{"id":493862,"rank":12,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1957/0124/figure-10.pdf","text":"Figure 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,{"id":39141,"text":"pp282A - 1956 - Ephemeral streams - Hydraulic factors and their relation to the drainage net","interactions":[],"lastModifiedDate":"2017-03-23T15:51:55","indexId":"pp282A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1956","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":"282","chapter":"A","title":"Ephemeral streams - Hydraulic factors and their relation to the drainage net","docAbstract":"<p>The hydraulic factors of width, depth, velocity, and suspended sediment load of ephemeral streams near Santa Fe, N. Mex., were measured during flood flow. Later, channel slope was measured. These flood-flow data, in conjunction with an analysis of drainage-basin configuration by the methods proposed by Horton, are used to determine the generalized interrelation of stream order and hydraulic variables. The method developed for determining this interrelation allows an integration of the geographic and physiographic characteristics of a drainage basin with the channel characteristics; specifically, the interrelation of the length, number, and drainage area of streams of various sizes with their respective discharge, width, depth, velocity, slope, channel roughness, and suspended-sediment load.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Physiographic and hydraulic studies of rivers (Professional Paper 282)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington D.C.","doi":"10.3133/pp282A","usgsCitation":"Leopold, L.B., and Miller, J.P., 1956, Ephemeral streams - Hydraulic factors and their relation to the drainage net: U.S. Geological Survey Professional Paper 282, iv, 37 p., https://doi.org/10.3133/pp282A.","productDescription":"iv, 37 p.","numberOfPages":"42","costCenters":[],"links":[{"id":338217,"rank":5,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/pp282D","linkHelpText":"Professional Paper 212-D: Flow resistance in sinuous or irregular channels"},{"id":338216,"rank":4,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/pp282C","linkHelpText":"Professional Paper 212-C: River flood plains: Some observations on their formation"},{"id":119372,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0282a/report-thumb.jpg"},{"id":66640,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0282a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":338215,"rank":3,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/pp282B","linkHelpText":"Professional Paper 212-B: River channel patterns: Braided, meandering, and straight"}],"country":"United States","state":"New Mexico","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -107,\n              36\n            ],\n            [\n              -105.5,\n              36\n            ],\n            [\n              -105.5,\n              35\n            ],\n            [\n              -107,\n              35\n            ],\n            [\n              -107,\n              36\n             \n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db602146","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":221029,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, John P.","contributorId":33696,"corporation":false,"usgs":true,"family":"Miller","given":"John","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":221030,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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