{"pageNumber":"7030","pageRowStart":"175725","pageSize":"25","recordCount":184617,"records":[{"id":70265922,"text":"70265922 - 1953 - Reconnaissance of the Missouri River pumping units between Garrison Dam and Bismarck, North Dakota","interactions":[],"lastModifiedDate":"2025-04-21T17:58:53.451703","indexId":"70265922","displayToPublicDate":"1953-01-01T13:48:46","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Reconnaissance of the Missouri River pumping units between Garrison Dam and Bismarck, North Dakota","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70265922","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1953, Reconnaissance of the Missouri River pumping units between Garrison Dam and Bismarck, North Dakota, https://doi.org/10.3133/70265922.","costCenters":[],"links":[{"id":484787,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":933998,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70048289,"text":"tem342 - 1953 - Results of core drilling for uranium-bearing lignites in the Bar H area, Slim Buttes, Harding County, South Dakota","interactions":[],"lastModifiedDate":"2014-02-28T14:34:40","indexId":"tem342","displayToPublicDate":"1953-01-01T13:47:00","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"342","title":"Results of core drilling for uranium-bearing lignites in the Bar H area, Slim Buttes, Harding County, South Dakota","docAbstract":"Core drilling in the Car H area, Slim Buttes, Harding County, South Dakota, under a contract with the B. H. Mott Drilling Co., Huntington, West Virginia, was resumed June 12, 1952 after a 6-month recess during the winter and was completed July 18, 1952.  The drilling was undertaken to obtain information on the distribution and extent of the uranium-bearing lignite beds along the southeast edge of the Bar H area.  Eight holes totalling 885 feet were drilled and 52 feet of lignite core submitted for study and analysis. The report includes detailed lithographic descriptions of the lignite cores, Bureau of Mines coal analyses, and the results of 100 chemical analyses for uranium. The drilling showed that the thicker, more persistent lignite beds exposed in the northern part of the Bar H area were removed by erosion prior to the deposition of the overlaying White River formation in the south-eastern part of the area.  The beds penetrated by drilling were not of sufficient thickness or uranium content to add to the previously known reserves.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem342","collaboration":"The report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Zeller, H., 1953, Results of core drilling for uranium-bearing lignites in the Bar H area, Slim Buttes, Harding County, South Dakota: U.S. Geological Survey Trace Elements Memorandum 342, Report: 46 p.; 2 Plates: 19.47 x 21.46 inches and 39.77 x 24.14 inches, https://doi.org/10.3133/tem342.","productDescription":"Report: 46 p.; 2 Plates: 19.47 x 21.46 inches and 39.77 x 24.14 inches","numberOfPages":"50","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":277912,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0342/report-thumb.jpg"},{"id":283089,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0342/plate-4.pdf"},{"id":283087,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0342/report.pdf"},{"id":283088,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0342/plate-2.pdf"}],"country":"United States","state":"South Dakota","county":"Harding County","otherGeospatial":"Slim Buttes;Bar H","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104.0454,45.2124 ], [ -104.0454,45.9453 ], [ -102.9425,45.9453 ], [ -102.9425,45.2124 ], [ -104.0454,45.2124 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"523c1cf9e4b024b60d40738f","contributors":{"authors":[{"text":"Zeller, Howard D.","contributorId":65526,"corporation":false,"usgs":true,"family":"Zeller","given":"Howard D.","affiliations":[],"preferred":false,"id":484250,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70048582,"text":"tem606 - 1953 - Airborne radioactivity survey of the Miller Hill area, Carbon county, Wyoming","interactions":[{"subject":{"id":70048582,"text":"tem606 - 1953 - Airborne radioactivity survey of the Miller Hill area, Carbon county, Wyoming","indexId":"tem606","publicationYear":"1953","noYear":false,"title":"Airborne radioactivity survey of the Miller Hill area, Carbon county, Wyoming"},"predicate":"SUPERSEDED_BY","object":{"id":51593,"text":"ofr53281 - 1953 - Photomosaic map of radioactivity anomalies in the Miller Hill region of Carbon County, Wyoming","indexId":"ofr53281","publicationYear":"1953","noYear":false,"title":"Photomosaic map of radioactivity anomalies in the Miller Hill region of Carbon County, Wyoming"},"id":1}],"supersededBy":{"id":51593,"text":"ofr53281 - 1953 - Photomosaic map of radioactivity anomalies in the Miller Hill region of Carbon County, Wyoming","indexId":"ofr53281","publicationYear":"1953","noYear":false,"title":"Photomosaic map of radioactivity anomalies in the Miller Hill region of Carbon County, Wyoming"},"lastModifiedDate":"2014-03-04T13:51:14","indexId":"tem606","displayToPublicDate":"1953-01-01T13:43:00","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"606","title":"Airborne radioactivity survey of the Miller Hill area, Carbon county, Wyoming","docAbstract":"The accompanying map shows the results of an airborne radioactivity survey covering 65 square miles northwest of Miller Hill, Carbon county, Wyoming. The survey was made by the U.S. Geological Survey as part of a cooperative program with the U.S. Atomic Energy Commission. At 500 feet above the ground, the width of the zone from which anomalous radioactivity is measured varies with the intensity of radiation of the source and, for strong sources, the width would be as much as 1,400 feet. Quarter-mile spacing of the flight paths of the aircraft should be adequate to detect anomalies from strong sources of radioactivity. However, small areas of considerable radioactivity midway between flight paths may not be noted. The approximate location of each radioactivity anomaly is shown on the accompanying map. The plotted position of an anomaly may be in error by as much as a quarter of a mile owing to errors in the available base maps up to several square miles in which it is impossible to find and plot recognizable landmarks. The radioactivity anomalies shown on the accompanying map cannot be interpreted in terms of either the radioactive content or the extent of the source materials. The present technique of airborne radioactivity measurement does not permit distinguishing between activity due to thorium and that due to uranium.  An anomaly, therefore, may represent radioactivity due entirely to uranium, or to thorium, or to a combination of uranium and thorium. The radioactivity that is recorded by airborne measurements at 500 feet above the ground can be caused by: 1. A moderately large area in which the rocks and soils are slightly more radioactive than the rocks and soils of the surrounding area. 2. A smaller area in which the rocks and soils are considerably more radioactive than rocks and soils in the surrounding area. 3. A very small area in which to rocks and soils are much more radioactive than the rocks and soils of the surrounding area. Any particular anomaly, therefore, may represent either slightly greater-than-average radioactivity over an area of a few thousand square feet, or high radioactivity over an area of a few hundred square feet. The radioactivity anomalies shown on the accompanying map indicate localities of more-than-average radioactivity, and therefore, suggest areas in which uranium or thorium deposits are more likely to occur.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem606","collaboration":"Prepared in cooperation with the United Stated Atomic Energy Commission","usgsCitation":"Meuschke, J.L., and Moxham, R., 1953, Airborne radioactivity survey of the Miller Hill area, Carbon county, Wyoming: U.S. Geological Survey Trace Elements Memorandum 606, Report: 2 p.; 1 Plate: 16.34 x 21.68 inches, https://doi.org/10.3133/tem606.","productDescription":"Report: 2 p.; 1 Plate: 16.34 x 21.68 inches","numberOfPages":"2","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278384,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0606/report-thumb.jpg"},{"id":283276,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0606/plate-1.pdf"},{"id":283275,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0606/report.pdf"}],"country":"United States","state":"Wyoming","city":"Carbon County","otherGeospatial":"Miller Hill Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -107.35,41.333333 ], [ -107.35,41.5 ], [ -107.25,41.5 ], [ -107.25,41.333333 ], [ -107.35,41.333333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"526a416ee4b0c0d229f9f65a","contributors":{"authors":[{"text":"Meuschke, J. L.","contributorId":53349,"corporation":false,"usgs":true,"family":"Meuschke","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":485131,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moxham, R.M.","contributorId":42234,"corporation":false,"usgs":true,"family":"Moxham","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":485130,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70210472,"text":"70210472 - 1953 - Progress report on the Kiligwa anticlinorium","interactions":[],"lastModifiedDate":"2025-01-22T15:22:56.797626","indexId":"70210472","displayToPublicDate":"1953-01-01T13:35:35","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":5963,"text":"Geological Investigations, Naval Petroleum Reserve No. 4, Alaska","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"40","subseriesTitle":"Special Report","title":"Progress report on the Kiligwa anticlinorium","docAbstract":"<p>This report was prepared to assist in the planning of seismic profiles to be run across the anticlinorium in the vicinity pf the Kiligwa River. The stratigraphy and structure of the mapped area south of the anticlinorium are reviewed.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70210472","usgsCitation":"Tailleur, I.L., and Kent, B.H., 1953, Progress report on the Kiligwa anticlinorium: Geological Investigations, Naval Petroleum Reserve No. 4, Alaska 40, Report: 17 p.; 1 Plate: 68.65 x 26.80 inches, https://doi.org/10.3133/70210472.","productDescription":"Report: 17 p.; 1 Plate: 68.65 x 26.80 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Irvin L.","contributorId":105304,"corporation":false,"usgs":true,"family":"Tailleur","given":"Irvin","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":924670,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kent, Bion H.","contributorId":63389,"corporation":false,"usgs":true,"family":"Kent","given":"Bion","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":924671,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70048733,"text":"tem699 - 1953 - Geology of the Horse Range Mesa quadrangle, Colorado","interactions":[],"lastModifiedDate":"2014-03-04T14:23:50","indexId":"tem699","displayToPublicDate":"1953-01-01T13:34:00","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"699","title":"Geology of the Horse Range Mesa quadrangle, Colorado","docAbstract":"The Horse Range Mesa quadrangle is one of eighteen 7 1/2-minute quadrangles covering the principal carnotite-producing area of southwestern Colorado.  The geology of the quadrangles was mapped by the U.S. Geological Survey for the Atomic Energy Commission as part of a comprehensive study of carnotite deposits.  The rocks exposed in the eighteen quadrangles consist of crystalline rocks of pre-Cambrian age and sedimentary rocks that range in age from late Paleozoic to Quaternary.  Over much of the area the sedimentary rocks are flat lying, but in places the rocks are disrupted by high-angle faults, and northwest-trending folds. Conspicuous among the folds are large anticlines having cores of intrusive salt and gypsum. Most of the carnotite deposits are confined to the Salt Wash sandstone member of the Jurassic Morrison formation. Within this sandstone, most of the deposits are spottily distributed through an arcuate zone known as the \"Uravan Mineral Belt\". Individual deposits range in size from irregular masses containing only a few tons of ore to large, tabular masses containing many thousands of tons.  The ore consists largely of sandstone selectively impregnated and in part replaced by uranium and vanadium minerals. Most of the deposits appear to be related to certain sedimentary strictures in sandstones of favorable composition.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem699","collaboration":"This report concerns work done partly on behalf of the Division of Raw Materials of the U.S Atomic Energy Commission","usgsCitation":"Cater, F.W., Bush, A., Bell, H., and Withington, C.F., 1953, Geology of the Horse Range Mesa quadrangle, Colorado: U.S. Geological Survey Trace Elements Memorandum 699, Report: 28 p.; 1 Plate: 33.88 x 27.89 inches, https://doi.org/10.3133/tem699.","productDescription":"Report: 28 p.; 1 Plate: 33.88 x 27.89 inches","numberOfPages":"31","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278608,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0699/report-thumb.jpg"},{"id":283327,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0699/plate-1.pdf"},{"id":283328,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0699/report.pdf"}],"country":"United States","state":"Colorado","otherGeospatial":"Horse Range Mesa Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.0,38.0 ], [ -109.0,38.125 ], [ -108.875,38.125 ], [ -108.875,38.0 ], [ -109.0,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52737bece4b097f32ac3db33","contributors":{"authors":[{"text":"Cater, Fred W. Jr.","contributorId":36988,"corporation":false,"usgs":true,"family":"Cater","given":"Fred","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":485505,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bush, A.L.","contributorId":70404,"corporation":false,"usgs":true,"family":"Bush","given":"A.L.","email":"","affiliations":[],"preferred":false,"id":485507,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bell, Henry III","contributorId":37710,"corporation":false,"usgs":true,"family":"Bell","given":"Henry","suffix":"III","email":"","affiliations":[],"preferred":false,"id":485506,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Withington, C. F.","contributorId":98394,"corporation":false,"usgs":true,"family":"Withington","given":"C.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":485508,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70100566,"text":"tem444A - 1953 - Results of reconnaissance for uranium in nonmarine carbonaceous rocks in parts of California, Idaho, Nevada, Oregon, Utah, and Washington during 1951 and 1952","interactions":[],"lastModifiedDate":"2014-04-09T13:37:56","indexId":"tem444A","displayToPublicDate":"1953-01-01T13:33:00","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"444","chapter":"A","title":"Results of reconnaissance for uranium in nonmarine carbonaceous rocks in parts of California, Idaho, Nevada, Oregon, Utah, and Washington during 1951 and 1952","docAbstract":"Nonmarine carbonaceous rocks, including shales, coal, and peat, were tested at about 3 localities in California, Idaho, Nevada, Oregon, Utah, and Washington. Rocks ranging in age from Carboniferous to Quaternary were examine, although the principal attention was given middle and late Tertiary lignites of the northern part of the Great Basin. Most carbonaceous rocks examined contained essentially no uranium, but lignitic shales in the Goose Creek district, Idaho, a thin carbonaceous shale near Hagerman, Idaho, and a small peat deposit in Davis County, Utah contained more than 0.003 percent uranium.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem444A","collaboration":"Prepared by the Geological Survey for the United Stated Atomic Energy Commission","usgsCitation":"Duncan, D., 1953, Results of reconnaissance for uranium in nonmarine carbonaceous rocks in parts of California, Idaho, Nevada, Oregon, Utah, and Washington during 1951 and 1952: U.S. Geological Survey Trace Elements Memorandum 444, 26 p., https://doi.org/10.3133/tem444A.","productDescription":"26 p.","numberOfPages":"26","temporalStart":"1951-01-01","temporalEnd":"1952-12-31","costCenters":[],"links":[{"id":286016,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0444-A/report-thumb.jpg"}],"country":"United States","state":"California;Idaho;Nevada;Oregon;Utah;Washington","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.79,37.0 ], [ -124.79,49.0 ], [ -109.03,49.0 ], [ -109.03,37.0 ], [ -124.79,37.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5355955ce4b0120853e8c1b2","contributors":{"authors":[{"text":"Duncan, Donald C.","contributorId":56152,"corporation":false,"usgs":true,"family":"Duncan","given":"Donald C.","affiliations":[],"preferred":false,"id":492325,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70228616,"text":"70228616 - 1953 - High Plains, or Llano Estacado, Texas-New Mexico","interactions":[],"lastModifiedDate":"2022-02-14T18:29:00.632682","indexId":"70228616","displayToPublicDate":"1953-01-01T13:28:43","publicationYear":"1953","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"High Plains, or Llano Estacado, Texas-New Mexico","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"The physical and economic foundation of natural resources; Volume 4: Subsurface facilities of water management and patterns of supply, type area studies","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Interior and Insular Affairs Committee, House of Representatives, United States Congress","usgsCitation":"Gaum, C.H., 1953, High Plains, or Llano Estacado, Texas-New Mexico, chap. <i>of</i> The physical and economic foundation of natural resources; Volume 4: Subsurface facilities of water management and patterns of supply, type area studies, p. 94-104.","productDescription":"11 p.","startPage":"94","endPage":"104","costCenters":[],"links":[{"id":395905,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Mexico, Texas","otherGeospatial":"Llano Estacado","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Gaum, Carl H.","contributorId":278598,"corporation":false,"usgs":true,"family":"Gaum","given":"Carl","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":834834,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70268053,"text":"70268053 - 1953 - The volcano letter: A weekly news leaflet of the Hawaiian Volcano Research Association - 1953","interactions":[{"subject":{"id":70268053,"text":"70268053 - 1953 - The volcano letter: A weekly news leaflet of the Hawaiian Volcano Research Association - 1953","indexId":"70268053","publicationYear":"1953","noYear":false,"title":"The volcano letter: A weekly news leaflet of the Hawaiian Volcano Research Association - 1953"},"predicate":"IS_PART_OF","object":{"id":70246900,"text":"70246900 - 1925 - The volcano letter: A weekly news leaflet of the Hawaiian Volcano Research Association","indexId":"70246900","publicationYear":"1925","noYear":false,"title":"The volcano letter: A weekly news leaflet of the Hawaiian Volcano Research Association"},"id":1}],"isPartOf":{"id":70246900,"text":"70246900 - 1925 - The volcano letter: A weekly news leaflet of the Hawaiian Volcano Research Association","indexId":"70246900","publicationYear":"1925","noYear":false,"title":"The volcano letter: A weekly news leaflet of the Hawaiian Volcano Research Association"},"lastModifiedDate":"2025-06-20T13:43:04.549142","indexId":"70268053","displayToPublicDate":"1953-01-01T13:23:14","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"title":"The volcano letter: A weekly news leaflet of the Hawaiian Volcano Research Association - 1953","docAbstract":"<p>The Volcano Letter was an informal publication issued at irregular intervals by the Hawaiian Volcano Observatory (HVO) during the years 1925 to 1955. Individual issues contain information on volcanic activity, volcano research, and volcano monitoring in Hawaii. Information on volcanic activity at other locations is also occasionally included.</p><p>The Volcano Letter was published by HVO through multiple changes in administration, including the Hawaiian Volcano Research Association (1925 to 1932), the U.S. Geological Survey (1932 to 1935), the Department of the Interior (1935 to 1938), and the University of Hawai‘i (1938 to 1955). Issues 1-262 were published weekly from January 1, 1925, to January 2, 1930, and consisted of a single page of text. Issues 263-384, also published weekly, from January 9, 1930, to May 5, 1932, were generally longer—four pages— and provided more detail on volcanic activity, including photographs, maps, and plots. Weekly issues 385-387, published May 12-26, 1932, were a single page of text due to budget reductions brought on by the Great Depression. Budget restrictions reduced the publishing frequency to monthly for issues 388-428, covering the period of June 1932 to October 1935; these issues were generally shorter, 1-2 pages, and sometimes featured figures. From November 1935 to July 1938, issues 429-461 remained monthly but increased in length (generally eight pages) and featured figures frequently. Issues 462-530, published over the period of August 1938 to December 1955, varied in length from 2-15 pages, but were published quarterly, rather than monthly.</p><p>Six of the Volcano Letters are misnumbered:<br>Jan. 21, 1926 number is 55 though it should 56<br>July 29, 1926 number is 82 though it should be 83<br>Feb. 16, 1928 number is 161 though it should be 164<br>May 31, 1928 number is 197 though it should be 179<br>Nov. 29, 1928 number is 204 though it should be 205</p>","language":"English","publisher":"Hawaiian Volcano Research Association","usgsCitation":"Hawaiian Volcano Research Association, 1953, The volcano letter: A weekly news leaflet of the Hawaiian Volcano Research Association - 1953, 33 p.","productDescription":"33 p.","costCenters":[{"id":336,"text":"Hawaiian Volcano 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,{"id":70048580,"text":"tem605 - 1953 - Airborne radioactivity survey of the Devils Tower area, Crook county, Wyoming","interactions":[{"subject":{"id":70048580,"text":"tem605 - 1953 - Airborne radioactivity survey of the Devils Tower area, Crook county, Wyoming","indexId":"tem605","publicationYear":"1953","noYear":false,"title":"Airborne radioactivity survey of the Devils Tower area, Crook county, Wyoming"},"predicate":"SUPERSEDED_BY","object":{"id":51591,"text":"ofr53279 - 1953 - Airborne radioactivity survey in the Devils Tower region, Wyoming","indexId":"ofr53279","publicationYear":"1953","noYear":false,"title":"Airborne radioactivity survey in the Devils Tower region, Wyoming"},"id":1}],"supersededBy":{"id":51591,"text":"ofr53279 - 1953 - Airborne radioactivity survey in the Devils Tower region, Wyoming","indexId":"ofr53279","publicationYear":"1953","noYear":false,"title":"Airborne radioactivity survey in the Devils Tower region, Wyoming"},"lastModifiedDate":"2014-03-04T13:50:32","indexId":"tem605","displayToPublicDate":"1953-01-01T13:16:00","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"605","title":"Airborne radioactivity survey of the Devils Tower area, Crook county, Wyoming","docAbstract":"The accompanying map shows the results of an airborne radioactivity survey covering 45 square miles northwest of Devils Tower, Crook County, Wyoming. The survey was made by the U.S. Geological Survey on September 4, 1952, as part of a cooperative program with the U.S. Atomic Energy Commission.  The survey was made with scintillation-detection equipment mounted in a Douglas DC-3 aircraft.  Parallel traverse lines, spaced at quarter-mile intervals, were flown approximately 500 feet above the ground. Aerial photographs were used for pilot guidance, and the flight path of the aircraft was recorded by a gyro-stabilized, continuous-strip-film camera.  The distance of the aircraft from the ground was measured with a continuously recording radio altimeter.  At 500 feet above the ground, the width of the zone from which anomalous radioactivity is measured varies with the intensity of radiation of the source and, for strong sources, the width would be as much as 1,400 feet.  Quarter-mile spacing of the flight paths of the aircraft should be adequate to detect anomalies from strong sources of radioactivity. However, small areas of considerable radioactivity midway between flight paths may not be noted.  The approximate location of each radioactivity anomaly is shown on the accompanying map.  The plotted position of an anomaly may be in error by as much as a quarter of a mile owing to errors in the available base maps up to several square miles in which it is impossible to find and plot recognizable landmarks.  The radioactivity that is recorded by airborne measurements at 500 feet above the ground can be caused by: 1. A moderately large area in which the rocks and soils are slightly more radioactive than the rocks and soils of the surrounding area. 2. A smaller area in which the rocks and soils are considerably more radioactive than rocks and soils in the surrounding area. 3. A very small area in which to rocks and soils are much more radioactive than the rocks and soils of the surrounding area.  Any particular anomaly, therefore, may represent either slightly greater-than-average radioactivity over an area of a few thousand square feet, or high radioactivity over an area of a few hundred square feet.  The radioactivity anomalies shown on the accompanying map indicate localities of more-than-average radioactivity, and therefore, suggest areas in which uranium or thorium deposits are more likely to occur.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem605","collaboration":"Prepared in cooperation with the United States Atomic Energy Commission","usgsCitation":"Henderson, J.R., and Moxham, R., 1953, Airborne radioactivity survey of the Devils Tower area, Crook county, Wyoming: U.S. Geological Survey Trace Elements Memorandum 605, Report: 2 p.; 1 Plate: 21.89 x 16.65 inches, https://doi.org/10.3133/tem605.","productDescription":"Report: 2 p.; 1 Plate: 21.89 x 16.65 inches","numberOfPages":"2","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278383,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0605/report-thumb.jpg"},{"id":283273,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0605/plate-1.pdf"},{"id":283274,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0605/report.pdf"}],"country":"United States","state":"Wyoming","county":"Crook County","otherGeospatial":"Devils Tower Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104.833333,44.65 ], [ -104.833333,44.75 ], [ -104.65,44.75 ], [ -104.65,44.65 ], [ -104.833333,44.65 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"526a416de4b0c0d229f9f654","contributors":{"authors":[{"text":"Henderson, J. 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,{"id":70048732,"text":"tem698 - 1953 - Geology of the Hamm Canyon quadrangle, Colorado","interactions":[{"subject":{"id":70048732,"text":"tem698 - 1953 - Geology of the Hamm Canyon quadrangle, Colorado","indexId":"tem698","publicationYear":"1953","noYear":false,"title":"Geology of the Hamm Canyon quadrangle, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":59104,"text":"mf21 - 1955 - Hamm Canyon quadrangle, Colorado","indexId":"mf21","publicationYear":"1955","noYear":false,"title":"Hamm Canyon quadrangle, Colorado"},"id":1}],"supersededBy":{"id":59104,"text":"mf21 - 1955 - Hamm Canyon quadrangle, Colorado","indexId":"mf21","publicationYear":"1955","noYear":false,"title":"Hamm Canyon quadrangle, Colorado"},"lastModifiedDate":"2019-05-09T08:14:51","indexId":"tem698","displayToPublicDate":"1953-01-01T13:13:00","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"698","title":"Geology of the Hamm Canyon quadrangle, Colorado","docAbstract":"The Hamm Canyon quadrangle is on eof eighteen 7 1/2-minute quadrangles covering the principal carnotite-producing area of southwestern Colorado.  The geology of these quadrangles was mapped by the U.S. Geological Survey for the Atomic Energy Commission as part of a comprehensive study of carnotite deposits.  The rocks exposed in the eighteen quadrangles consist of crystalline rocks of pre-Cambrian age and sedimentary rocks that range in age from late Paleozoic to Quaternary.  Over much of the area the sedimentary rocks are flat lying, but in places the rocks are disrupted by high-angle faults, and northwest-trending folds.  Conspicuous among the folds are large anticlines having cores of intrusive salt and gypsum.  Most of the carnotite deposits are confined to the Salt Wash sandstone member of the Jurassic Morrison formation.  Within this sandstone, most of the deposits are spottily distributed through an arcuate zone known as the \"Uravan Mineral Belt\".  Individual deposits range in size from irregular masses containing only a few tons of ore to large, tabular masses containing many thousands of tons.  The ore consists largely of sandstone selectively impregnated and in part replaced by uranium and vanadium minerals.  Most of the deposits appear to be related to certain sedimentary structures in sandstones of favorable composition.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem698","collaboration":"This report concerns work done partly on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Cater, F.W., 1953, Geology of the Hamm Canyon quadrangle, Colorado: U.S. Geological Survey Trace Elements Memorandum 698, Report: 27 p.; 1 Plate: 34.00 x 27.96 inches, https://doi.org/10.3133/tem698.","productDescription":"Report: 27 p.; 1 Plate: 34.00 x 27.96 inches","numberOfPages":"30","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":283325,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0698/plate-1.pdf"},{"id":283326,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0698/report.pdf"},{"id":278607,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0698/report-thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Hamm Canyon Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.875,38.0 ], [ -108.875,38.125 ], [ -108.75,38.125 ], [ -108.75,38.0 ], [ -108.875,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52737bebe4b097f32ac3db30","contributors":{"authors":[{"text":"Cater, Fred W. Jr.","contributorId":36988,"corporation":false,"usgs":true,"family":"Cater","given":"Fred","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":485504,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71336,"text":"tei286 - 1953 - Carnotite resources of the Spud Patch area, San Miguel County, Colorado","interactions":[],"lastModifiedDate":"2018-03-26T16:05:39","indexId":"tei286","displayToPublicDate":"1953-01-01T13:06:00","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"286","title":"Carnotite resources of the Spud Patch area, San Miguel County, Colorado","docAbstract":"<p>The Spud Patch area comprises about 8 square in T. 43 M., R. 18 and 19 W., San Miguel County, Colo., and is about 4 miles northeast of Egnar, Colo. Claims of the United States Vanadium Co. and the Vanadium Corp. of America cover about half the area. Claims of other owners, public land, and patented agricultural land, comprise the remainder of the area. The area is about 38 miles from the Government mill at Montecello, Utah, and 55 miles from the Vanadium Corp. of America mill at Naturita, Colo.</p><p>Between 1940 and 1951, the Spud Patch area yielded about 24,000 short tons of carnotite ore that probably averaged 0.21 percent U<sub>3</sub>O<sub>8</sub> and 2.2 percent V<sub>2</sub>O<sub>5</sub>.</p><p>The deposits are in a broad sandstone lens near the top of the Salt Wash member of the Jurassic Morrison formation. Although the deposits mined have been mainly impregnations of sandstone by carnotite and gray vanadium-bearing clay minerals, some of the richer deposits found by Geological Survey drilling have a finely disseminated black uranium mineral but no carnotite. The deposits commonly are thin irregular tabular layers, which locally thicken to form elongate masses called \"rolls\". These rolls have a dominant northeasterly trend. Geologic features found to be most useful as guides to ore are listed.</p><p>From November 1949 to May 1952, the U.S. Geological Survey drilled 415 diamond-drill holes totaling 67,215 feet in the Spud Patch area. The purpose of this drilling was to find deposits that would make new mines and to appraise the reserves in the unexplored area.</p><p>As a result of Geological Survey drilling, indicated and inferred reserves computed at the cutoff of 1 foot or more thick and 0.10 percent U<sub>3</sub>O<sub>8</sub> or 1.0 percent V<sub>2</sub>O<sub>5</sub> total 20,500 short tons, averaging 0.28 percent U<sub>3</sub>O<sub>8</sub> and 2.1 percent V<sub>2</sub>O<sub>5</sub>. These reserves and those computed at a lower grade cutoff of 0.05 percent U<sub>3</sub>O<sub>8</sub> or 0.50 percent V<sub>2</sub>O<sub>5</sub> and the pounds of contained metal are summarized in table 1.</p><p>Potential reserves, whose existence is based on geologic evidence alone, are predicted to total about 42,000 short tons, averaging 0.25 percent U<sub>3</sub>O<sub>8</sub> and 2.0 percent V<sub>2</sub>O<sub>5</sub>.</p><p>No additional exploratory-type drilling by the Geological Survey is planned in the Spud Patch area. Recommendations are offered for additional development-type drilling, preferably by claim owners or lessees in specific areas in the vicinity of deposits discovered by Geological Survey drilling.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei286","usgsCitation":"Bell, H., 1953, Carnotite resources of the Spud Patch area, San Miguel County, Colorado: U.S. Geological Survey Trace Elements Investigations 286, Report: 46 p.; 2 Plates: 30.17 x 24.02 and 30.54 x 24.35 inches, https://doi.org/10.3133/tei286.","productDescription":"Report: 46 p.; 2 Plates: 30.17 x 24.02 and 30.54 x 24.35 inches","numberOfPages":"47","costCenters":[],"links":[{"id":284522,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0286/report.pdf"},{"id":284524,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0286/figure-3.pdf"},{"id":284523,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0286/figure-2.pdf"},{"id":283487,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei286.PNG"}],"country":"United States","state":"Colorado","county":"San Miguel County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.04515,37.772072 ], [ -109.04515,38.153099 ], [ -107.73111,38.153099 ], [ -107.73111,37.772072 ], [ -109.04515,37.772072 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53558ff8e4b0120853e8be6f","contributors":{"authors":[{"text":"Bell, Henry III","contributorId":37710,"corporation":false,"usgs":true,"family":"Bell","given":"Henry","suffix":"III","email":"","affiliations":[],"preferred":false,"id":284009,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70048730,"text":"tem697 - 1953 - Geology of the Gypsum Gap quadrangle, Colorado","interactions":[],"lastModifiedDate":"2014-03-04T14:22:27","indexId":"tem697","displayToPublicDate":"1953-01-01T12:58:00","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"697","title":"Geology of the Gypsum Gap quadrangle, Colorado","docAbstract":"The Gypsum Gap quadrangle is one eighteen 7 1/2-minute quadrangles covering the principal carnotite-producing area of southwestern Colorado.  The geology of these quadrangles was mapped by the U.S. Geological Survey for the Atomic Energy Commission as part of a comparative study of carnotite deposits.  The rocks exposed in the eighteen quadrangles consist of crystalline rocks of pre-Cambrian age and sedimentary rocks that range in age from late Paleozoic to Quaternary.  Over much of the area the sedimentary rocks are flat lying, but in places the rocks are disrupted by high-angle faults, and northwest-trending folds.  Conspicuous among the folds are large anticlines having cores of intrusive salt and gypsum.  Most of the carnotite deposits are confined to the Salt Wash sandstone member of the Jurassic Morrison formation.  Within this sandstone, most of the deposits are spottily distributed through a arcuate zone known as the \"Uravan Mineral Belt\".  Individual deposits range in size from irregular masses containing only a few tons of ore to large, tabular masses containing many thousands of tons. The core consists largely of sandstone selectively impregnated and in part replaced by uranium and vanadium minerals. Most of the deposits appear to be related to certain sedimentary structures in sandstones of favorable composition.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem697","collaboration":"This report concerns works done partly on behalf of the Division of Raw Materials of the U.S Atomic Energy Commission","usgsCitation":"Cater, F.W., 1953, Geology of the Gypsum Gap quadrangle, Colorado: U.S. Geological Survey Trace Elements Memorandum 697, Report: 36 p.; 1 Plate: 34.69 x 28.56 inches, https://doi.org/10.3133/tem697.","productDescription":"Report: 36 p.; 1 Plate: 34.69 x 28.56 inches","numberOfPages":"39","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278606,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0697/report-thumb.jpg"},{"id":283323,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0697/plate-1.pdf"},{"id":283324,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0697/report.pdf"}],"country":"United States","state":"Colorado","otherGeospatial":"Gypsum Gap Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.75,38.0 ], [ -108.75,38.125 ], [ -108.625,38.125 ], [ -108.625,38.0 ], [ -108.75,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52737bebe4b097f32ac3db2d","contributors":{"authors":[{"text":"Cater, Fred W. Jr.","contributorId":36988,"corporation":false,"usgs":true,"family":"Cater","given":"Fred","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":485498,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70048728,"text":"tem696 - 1953 - Geology of the Gateway quadrangle, Mesa county Colorado","interactions":[{"subject":{"id":70048728,"text":"tem696 - 1953 - Geology of the Gateway quadrangle, Mesa county Colorado","indexId":"tem696","publicationYear":"1953","noYear":false,"title":"Geology of the Gateway quadrangle, Mesa county Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":69553,"text":"gq55 - 1955 - Geology of the Gateway quadrangle, Colorado","indexId":"gq55","publicationYear":"1955","noYear":false,"title":"Geology of the Gateway quadrangle, Colorado"},"id":1}],"supersededBy":{"id":69553,"text":"gq55 - 1955 - Geology of the Gateway quadrangle, Colorado","indexId":"gq55","publicationYear":"1955","noYear":false,"title":"Geology of the Gateway quadrangle, Colorado"},"lastModifiedDate":"2014-03-04T14:21:46","indexId":"tem696","displayToPublicDate":"1953-01-01T12:43:00","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"696","title":"Geology of the Gateway quadrangle, Mesa county Colorado","docAbstract":"The Gateway quadrangle is one of eighteen 7 1/2-minute quadrangles covering the principal carnotite-producing area of southwestern Colorado. The geology of these quadrangles was mapped by the U.S. Geological Survey for the Atomic Energy Commission as part of a comprehensive study of carnotite deposits. The rocks exposed in the eighteen quadrangles consist of crystalline rocks of pre-Cambrian age and sedimentary rocks that range in age from late Paleozoic to Quaternary. Over much of the area the sedimentary rocks are flat lying, but in places the rocks are disrupted by hih-angle faults, and northwest-trending folds. Conspicuous among the folds are large anticlines having cores of intrusive salt and gypsum. Most of the carnotite deposits are confined to the Salt Wash sandstone member of Jurassic Morrison formation. Within this sandstone, most of the deposits are spottily distributed through an arcuate zone known as \"Uruvan Mineral Belt\". Individual deposits range in size from irregular masses containing only a few tons of ore to large, tabular masses containing many thousands of tons. The ore consists largely of sandstone selectively impregnated and in part replaced by uranium and vanadium minerals. Most of the deposits appear to be related to certain sedimentary structures in sandstones of favorable composition.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem696","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Cater, F.W., 1953, Geology of the Gateway quadrangle, Mesa county Colorado: U.S. Geological Survey Trace Elements Memorandum 696, Report: 26 p.; 1 Plate: 34.42 x 28.38 inches, https://doi.org/10.3133/tem696.","productDescription":"Report: 26 p.; 1 Plate: 34.42 x 28.38 inches","numberOfPages":"29","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278605,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0696/report-thumb.jpg"},{"id":283321,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0696/report.pdf"},{"id":283322,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0696/plate-1.pdf"}],"country":"United States","state":"Colorado","county":"Mesa County","otherGeospatial":"Gateway Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.0,37.625 ], [ -109.0,38.75 ], [ -108.875,38.75 ], [ -108.875,37.625 ], [ -109.0,37.625 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52737bebe4b097f32ac3db2a","contributors":{"authors":[{"text":"Cater, Fred W. Jr.","contributorId":36988,"corporation":false,"usgs":true,"family":"Cater","given":"Fred","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":485497,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71943,"text":"tem509 - 1953 - Progress report on original-state core studies","interactions":[],"lastModifiedDate":"2014-07-16T12:00:51","indexId":"tem509","displayToPublicDate":"1953-01-01T11:59:00","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"509","title":"Progress report on original-state core studies","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Oak Ridge, TN","doi":"10.3133/tem509","usgsCitation":"Manger, G.E., and Gates, G.L., 1953, Progress report on original-state core studies: U.S. Geological Survey Trace Elements Memorandum 509, 21 p., https://doi.org/10.3133/tem509.","productDescription":"21 p.","numberOfPages":"21","costCenters":[],"links":[{"id":290280,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c79f12e4b019484164249b","contributors":{"authors":[{"text":"Manger, George Edward","contributorId":80693,"corporation":false,"usgs":true,"family":"Manger","given":"George","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":284914,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gates, George Laurence","contributorId":101566,"corporation":false,"usgs":true,"family":"Gates","given":"George","email":"","middleInitial":"Laurence","affiliations":[],"preferred":false,"id":284915,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":71894,"text":"tei364 - 1953 - Stratigraphic sections of the Phosphoria Formation in Idaho, 1949: part I","interactions":[],"lastModifiedDate":"2014-06-03T11:34:50","indexId":"tei364","displayToPublicDate":"1953-01-01T11:53:00","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"364","title":"Stratigraphic sections of the Phosphoria Formation in Idaho, 1949: part I","docAbstract":"<p> The U.S. Geological Survey has recently measured and sampled the Phosphoria formation at many localities in Idaho and other western states. These data will not be fully synthesized for many years, but segments of the data, accompanied by little or no interpretation, are published as preliminary reports as they are assembled. This report, which contains abstracts of the sections measured in southeastern Idaho (fig. 1), is one of this series and is the fourth report of data gathered in Idaho; it includes about half of the data gathered in Idaho in 1949. The field and laboratory procedures adopted in these investigations are described rather fully in a previous report (McKelvey and others, 1953a).</p>\n<br/>\n<p>Many people have taken part in this investigation, which was organized and supervised by V. E. McKelvey. F. J. Anderson, D. F. Davidson, R. S. Jones, R. A. Smart, R. G. Waring, and J. D. Weiser participated in the description of strata and the collection of samples referred to in this report. T. K. Rigby assisted in the preparation of trenches and the collection, crushing, and splitting of samples in the field. The laboratory preparation of samples for chemical analysis was done in Denver, Colo., under the direction of W. P. Huleatt.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei364","collaboration":"This report concerns work done partly on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Sheldon, R., Warner, M., Thompson, M., and Peirce, H., 1953, Stratigraphic sections of the Phosphoria Formation in Idaho, 1949: part I: U.S. Geological Survey Trace Elements Investigations 364, 10 p., https://doi.org/10.3133/tei364.","productDescription":"10 p.","numberOfPages":"37","temporalStart":"1949-01-01","temporalEnd":"1949-12-31","costCenters":[],"links":[{"id":283480,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei364.jpg"},{"id":284580,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0364/report.pdf"}],"country":"United States","state":"Idaho","otherGeospatial":"Phosphoria Formation","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -113.0,42.0 ], [ -113.0,44.0 ], [ -111.0,44.0 ], [ -111.0,42.0 ], [ -113.0,42.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53559567e4b0120853e8c20d","contributors":{"authors":[{"text":"Sheldon, R.P.","contributorId":71158,"corporation":false,"usgs":true,"family":"Sheldon","given":"R.P.","email":"","affiliations":[],"preferred":false,"id":284867,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Warner, M.A.","contributorId":104476,"corporation":false,"usgs":true,"family":"Warner","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":284869,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thompson, M.E.","contributorId":98794,"corporation":false,"usgs":true,"family":"Thompson","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":284868,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Peirce, H.W.","contributorId":19935,"corporation":false,"usgs":true,"family":"Peirce","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":284866,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70095726,"text":"tei198 - 1953 - Reconnaissance for uranium-bearing carbonaceous rocks in New Mexico, 1952","interactions":[],"lastModifiedDate":"2014-04-03T14:48:16","indexId":"tei198","displayToPublicDate":"1953-01-01T11:53:00","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"198","title":"Reconnaissance for uranium-bearing carbonaceous rocks in New Mexico, 1952","docAbstract":"Reconnaissance for uranium in coal and black shale in New Mexico during 1952 was largely an extension of work initiated during the 1951 field season. No uranium deposits of economic interest were found, although minor amounts of uranium were noted at several localities.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei198","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Bachman, G., Baltz, E., and O’Sullivan, R., 1953, Reconnaissance for uranium-bearing carbonaceous rocks in New Mexico, 1952: U.S. Geological Survey Trace Elements Investigations 198, 20 p., https://doi.org/10.3133/tei198.","productDescription":"20 p.","numberOfPages":"21","temporalStart":"1952-01-01","temporalEnd":"1952-12-31","costCenters":[],"links":[{"id":285618,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0198/report.pdf"},{"id":283650,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei198.jpg"}],"country":"United States","state":"New Mexico","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.0502,31.3322 ], [ -109.0502,37.0003 ], [ -103.002,37.0003 ], [ -103.002,31.3322 ], [ -109.0502,31.3322 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53559532e4b0120853e8c19b","contributors":{"authors":[{"text":"Bachman, G.O.","contributorId":55858,"corporation":false,"usgs":true,"family":"Bachman","given":"G.O.","email":"","affiliations":[],"preferred":false,"id":491408,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baltz, E.H.","contributorId":67146,"corporation":false,"usgs":true,"family":"Baltz","given":"E.H.","affiliations":[],"preferred":false,"id":491409,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"O’Sullivan, R.B.","contributorId":30133,"corporation":false,"usgs":true,"family":"O’Sullivan","given":"R.B.","email":"","affiliations":[],"preferred":false,"id":491407,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":71382,"text":"tei336 - 1953 - Reconnaissance during 1952 for uranium-bearing carbonaceous rocks in parts of Colorado, Utah, Idaho, and Wyoming","interactions":[],"lastModifiedDate":"2014-06-06T14:52:37","indexId":"tei336","displayToPublicDate":"1953-01-01T11:50:00","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"336","title":"Reconnaissance during 1952 for uranium-bearing carbonaceous rocks in parts of Colorado, Utah, Idaho, and Wyoming","docAbstract":"<p>A reconnaissance for uranium-bearing carbonaceous rocks was made during the 1952 field season in 23 areas in Colorado, Utah, Idaho, and Wyoming. Uranium in small amounts occurs in several of the areas examined, but no deposits were found that might have commercial possibilities. As much as 0.03 percent uranium is in the ash of coal in the Caribou Mountain area in southwestern Idaho; 0.012 percent in the ash of coal in the Burnt Fork area of southwestern Wyoming; and 0.009 percent in the ash of coal from near Driggs in eastern Idaho. Seven additional areas were examined in which beds of coal or carbonaceous shale contained more than 0.002 but less than 0.007 percent uranium in the ash. Unweathered samples of bituminous sandstone from the Vernal area, Utah, contain minor quantities of uranium.</p>ilities.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei336","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Vine, J.D., and Flege, R.F., 1953, Reconnaissance during 1952 for uranium-bearing carbonaceous rocks in parts of Colorado, Utah, Idaho, and Wyoming: U.S. Geological Survey Trace Elements Investigations 336, 19 p., https://doi.org/10.3133/tei336.","productDescription":"19 p.","numberOfPages":"20","temporalStart":"1952-01-01","temporalEnd":"1952-12-31","costCenters":[],"links":[{"id":284063,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei336.jpg"},{"id":285647,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0336/report.pdf"}],"country":"United States","state":"Colorado;Idaho;Utah;Wyoming","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.3936,38.0175 ], [ -114.3936,44.4193 ], [ -106.1956,44.4193 ], [ -106.1956,38.0175 ], [ -114.3936,38.0175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53559530e4b0120853e8c185","contributors":{"authors":[{"text":"Vine, James D.","contributorId":105287,"corporation":false,"usgs":true,"family":"Vine","given":"James","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":284085,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Flege, Robert F. Jr.","contributorId":25463,"corporation":false,"usgs":true,"family":"Flege","given":"Robert","suffix":"Jr.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":284084,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":71891,"text":"tei361 - 1953 - Stratigraphic sections of the Phosphoria Formation in Montana, 1949-50: part I","interactions":[],"lastModifiedDate":"2014-06-03T11:33:09","indexId":"tei361","displayToPublicDate":"1953-01-01T11:43:00","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"361","title":"Stratigraphic sections of the Phosphoria Formation in Montana, 1949-50: part I","docAbstract":"<p> The U.S. Geological Survey has recently measured and sampled the Phosphoria formation at many localities in Montana and other western states. These data will not be fully synthesized for many years, but segments of the data, accompanied by little or no interpretation, are published as preliminary reports as they are assembled. This report, which contains abstracts of the sections measured in southwestern Montana (fig. 1) is one of this series and is the third Montana report; it includes about half of the data gathered in Montana during 1949 and 1950. The field and laboratory procedures adopted in these investigations are described rather fully in a previous report (McKelvey and others, 1953).</p>\n<br/>\n<p>Many people have taken part in this investigation. The program which this work is a part was organized by V. E. McKelvey and the field program was supervised by R. W. Swanson, T. M. Cheney, J. L. Elliott, F. D. Frieske, R. F. Gosman, R. S. Jones, B. K. Replogle, and R. G. Waring participated in the description of strata and the collection of samples referred to in this report. Crushing and splitting of the samples in the field was done by T. K. Rigby. The laboratory preparation of samples for chemical analysis was done in Denver, Colo., under the direction of W. P. Huleatt.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei361","collaboration":"This report concerns work done partly on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Cressman, E.R., Wilson, W., Tandy, C., and Garmoe, W., 1953, Stratigraphic sections of the Phosphoria Formation in Montana, 1949-50: part I: U.S. Geological Survey Trace Elements Investigations 361, 9 p., https://doi.org/10.3133/tei361.","productDescription":"9 p.","numberOfPages":"29","temporalStart":"1949-01-01","temporalEnd":"1950-12-31","costCenters":[],"links":[{"id":283478,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei361.jpg"},{"id":284577,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0361/report.pdf"}],"country":"United States","state":"Montana","otherGeospatial":"Phosphoria Formation","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -113.0,44.0 ], [ -113.0,47.0 ], [ -111.0,47.0 ], [ -111.0,44.0 ], [ -113.0,44.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53559568e4b0120853e8c211","contributors":{"authors":[{"text":"Cressman, E. R.","contributorId":83494,"corporation":false,"usgs":true,"family":"Cressman","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":284856,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilson, W.H.","contributorId":32293,"corporation":false,"usgs":true,"family":"Wilson","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":284854,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tandy, C.W.","contributorId":86628,"corporation":false,"usgs":true,"family":"Tandy","given":"C.W.","email":"","affiliations":[],"preferred":false,"id":284857,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Garmoe, W.J.","contributorId":60072,"corporation":false,"usgs":true,"family":"Garmoe","given":"W.J.","email":"","affiliations":[],"preferred":false,"id":284855,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":71896,"text":"tei365 - 1953 - Stratigraphic sections of the Phosphoria Formation in Idaho, 1949: part II","interactions":[],"lastModifiedDate":"2014-06-03T11:35:22","indexId":"tei365","displayToPublicDate":"1953-01-01T11:36:00","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"365","title":"Stratigraphic sections of the Phosphoria Formation in Idaho, 1949: part II","docAbstract":"<p>The U.S. Geological Survey has recently measured and sampled the Phosphoria formation at many localities in Idaho and other western states. These data will not be fully synthesized and analyzed for several years, but segments of the data, accompanied by little or no interpretation, are published as preliminary reports as they are assembled. This is the fifth report of data containing abstracts of sections measured in southeastern Idaho; it includes about half of the data gathered in Idaho in 1949. The field and laboratory procedures adopted in these investigations are described rather fully in a previous report (McKelvey and others, 1953a).</p>\n<br/>\n<p>Many people have taken part in this investigation, which was organized and supervised by V. E. McKelvey. F. J. Anderson, A. L. Bush, R. S. Jones, K. B. Krauskopf, K. Lutz, M. E. Thompson, R. G. Waring, and M. A. Warner participated in the description of strata and the collection of samples referred to in this report. T. K. Rigby assisted in the preparation of trenches and the collection, crushing, and splitting of samples in the field. The laboratory preparation of samples for chemical analysis was done in Denver, Colo., under the direction of W. P. Huleatt.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei365","collaboration":"This report concerns work done partly on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Davidson, D., Smart, R., Peirce, H., and Weiser, J., 1953, Stratigraphic sections of the Phosphoria Formation in Idaho, 1949: part II: U.S. Geological Survey Trace Elements Investigations 365, 10 p., https://doi.org/10.3133/tei365.","productDescription":"10 p.","numberOfPages":"35","temporalStart":"1949-01-01","temporalEnd":"1949-12-31","costCenters":[],"links":[{"id":283476,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei365.jpg"},{"id":284581,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0365/report.pdf"}],"country":"United States","state":"Idaho","otherGeospatial":"Phosphoria Formation","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -113.0,42.0 ], [ -113.0,44.0 ], [ -111.0,44.0 ], [ -111.0,42.0 ], [ -113.0,42.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53559567e4b0120853e8c20f","contributors":{"authors":[{"text":"Davidson, D.F.","contributorId":68293,"corporation":false,"usgs":true,"family":"Davidson","given":"D.F.","email":"","affiliations":[],"preferred":false,"id":284874,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smart, R.A.","contributorId":6039,"corporation":false,"usgs":true,"family":"Smart","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":284871,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Peirce, H.W.","contributorId":19935,"corporation":false,"usgs":true,"family":"Peirce","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":284873,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Weiser, J.D.","contributorId":12458,"corporation":false,"usgs":true,"family":"Weiser","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":284872,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70095722,"text":"tei197 - 1953 - Reconnaissance for radioactive deposits in the Fairbanks and Livengood Quadrangles, east-central Alaska, 1949","interactions":[],"lastModifiedDate":"2014-06-05T13:59:24","indexId":"tei197","displayToPublicDate":"1953-01-01T11:35:00","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"197","title":"Reconnaissance for radioactive deposits in the Fairbanks and Livengood Quadrangles, east-central Alaska, 1949","docAbstract":"<p>Several mines and prospects in the Fairbanks and Livengood quadrangles, east-central Alaska, were examined for the possible presence of radioactive materials in the summer of 1949. Also tested were pre-Cambrian and Paleozoic metamorphic and sedimentary rocks crossed by the Elliott Highway, which extends from Fox, near Fairbanks, northward about 70 miles to the town of Livengood. None of the lodes tested exhibited radioactivity in excess of 0.003 percent equivalent uranium, although nuggets consisting chiefly of native bismuth and containing as much as 0.1 percent equivalent uranium had been found previously in a placer on Fish Creek several miles below the reported bismuth-bearing lode on Melba Creek. The greatest radioactivity found in the rocks along the Elliott Highway was in an iron-stained schist of pre-Cambrian age and in carbonaceous shale of Middle Devonian or Carboniferous age. Respective samples of these rocks contain 0.003 and 0.004 percent equivalent uranium. A possible local bedrock source for a euxenite-polycrase mineral found in a placer concentrate containing about 0.04 percent equivalent uranium was sought in the watershed of Goodluck Creek, near Livengood. The bedrock source of this mineral could not be located; it is believed that the source could be outside of the Goodluck watershed, as drainage changes in the area during Quaternary time might well have introduced gravels from nearby areas.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei197","collaboration":"This report concerns work done on behalf of the Division of Raw materials of the U.S. Atomic Energy Commission","usgsCitation":"Wedow, H., Stevens, J., and Tolbert, G., 1953, Reconnaissance for radioactive deposits in the Fairbanks and Livengood Quadrangles, east-central Alaska, 1949: U.S. Geological Survey Trace Elements Investigations 197, Report: 13 p.; 1 Plate: 15.14 x 19.35 inches, https://doi.org/10.3133/tei197.","productDescription":"Report: 13 p.; 1 Plate: 15.14 x 19.35 inches","numberOfPages":"14","temporalStart":"1949-01-01","temporalEnd":"1949-12-31","costCenters":[],"links":[{"id":283648,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei197.jpg"},{"id":285616,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0197/figure-1.pdf"},{"id":285617,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0197/report.pdf"}],"country":"United States","state":"Alaska","otherGeospatial":"Fairbanks Quadrangle;Livengood Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -149.5,64.5 ], [ -149.5,66.0 ], [ -147.0,66.0 ], [ -147.0,64.5 ], [ -149.5,64.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53559531e4b0120853e8c18c","contributors":{"authors":[{"text":"Wedow, H. Jr.","contributorId":6369,"corporation":false,"usgs":true,"family":"Wedow","given":"H.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":491388,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stevens, J.M.","contributorId":49851,"corporation":false,"usgs":true,"family":"Stevens","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":491390,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tolbert, G.E.","contributorId":33759,"corporation":false,"usgs":true,"family":"Tolbert","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":491389,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":71373,"text":"tei325 - 1953 - Numerical list of U.S. Geological Survey Trace Elements Reports to April 30, 1953","interactions":[],"lastModifiedDate":"2014-06-06T11:00:26","indexId":"tei325","displayToPublicDate":"1953-01-01T11:29:00","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"325","title":"Numerical list of U.S. Geological Survey Trace Elements Reports to April 30, 1953","docAbstract":"<p>This report contains 1) a list in numerical order of U.S. Geological Survey Trace Elements Investigations and Memorandum Reports, and 2) an author index for these reports. It supercedes TEI-30, issued in November 1952.</p>\n<br/>\n<p>This report contains lists not only of reports that have been transmitted to the U.S Atomic Energy Commission, that is, those reports followed by a date, but also those reports for which tentative titles were available prior to the date of completion of this list, April 30, 1953. The reports that are in preparation and subject to change in title are indicated by an asterisk.</p>\n<br/>\n<p>The classifications that are shown for some of the reports issued prior to 1947 are uncertain: classifications shown are based on the best information available at the time that this report was prepared.</p>\n<br/>\n<p>The Geological Survey does not have additional copies for permanent distribution of most of the reports listed, but copies of many of the completed reports can be loaned to organizations or individuals who are cooperating with the Atomic Energy Commission.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei325","collaboration":"This report concerns work done chiefly on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Blatcher, V.K., and Wallace, J.H., 1953, Numerical list of U.S. Geological Survey Trace Elements Reports to April 30, 1953: U.S. Geological Survey Trace Elements Investigations 325, 116 p., https://doi.org/10.3133/tei325.","productDescription":"116 p.","numberOfPages":"118","costCenters":[],"links":[{"id":284062,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei325.jpg"},{"id":285645,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0325/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"535594e3e4b0120853e8c0b1","contributors":{"authors":[{"text":"Blatcher, Virginia K.","contributorId":55332,"corporation":false,"usgs":true,"family":"Blatcher","given":"Virginia","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":284067,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wallace, Jane H.","contributorId":95119,"corporation":false,"usgs":true,"family":"Wallace","given":"Jane","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":284068,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":71413,"text":"tei375 - 1953 - Stratigraphic sections of the Phosphoria formation in Montana, 1951","interactions":[],"lastModifiedDate":"2014-06-03T11:36:04","indexId":"tei375","displayToPublicDate":"1953-01-01T11:25:00","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"375","title":"Stratigraphic sections of the Phosphoria formation in Montana, 1951","docAbstract":"<p>The U.S. Geological Survey has recently measured and sampled the Phosphoria formation at many localities in Montana and other western states. These data will not be fully synthesized and analyzed for several years, but segments of the data, accompanied by little or no interpretation, are published as preliminary reports as they are assembled. This report, which contains abstracts of the sections measured in southwestern Montana (fig. 1), during 1951, is the fifth Montana report of this series. The field and laboratory procedures adopted in these investigations are described in a previous report (McKelvey and others, 1953).</p>\n<br/>\n<p>Many people have taken part in this investigation. Crushing and splitting of the samples in the field were done by T. K. Rigby. The laboratory preparation of samples for chemical analysis was done in Denver, Colo., under the direction of W. P. Huleatt.</p>\n<br/>\n<p>The P<sub>2</sub>0<sub>5</sub> and acid insoluble analyses were made for the Survey by the U.S. Bureau of Mines at the Northwest Electrodevelopment Laboratory, Albany, Oreg., under the direction of S. M. Sheldon and M. L. Wright.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei375","collaboration":"This report concerns work done partly on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Peterson, J.A., 1953, Stratigraphic sections of the Phosphoria formation in Montana, 1951: U.S. Geological Survey Trace Elements Investigations 375, 10 p., https://doi.org/10.3133/tei375.","productDescription":"10 p.","numberOfPages":"34","temporalStart":"1951-01-01","temporalEnd":"1951-12-31","costCenters":[],"links":[{"id":283475,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei375.jpg"},{"id":284562,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0375/report.pdf"}],"country":"United States","state":"Montana","otherGeospatial":"Phosphoria Formation","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -113.5,44.0 ], [ -113.5,47.0 ], [ -110.5,47.0 ], [ -110.5,44.0 ], [ -113.5,44.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53559568e4b0120853e8c217","contributors":{"authors":[{"text":"Peterson, James A.","contributorId":106872,"corporation":false,"usgs":true,"family":"Peterson","given":"James","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":284130,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70048726,"text":"tem694 - 1953 - Geology of the Davis Mesa quadrangle, Colorado","interactions":[],"lastModifiedDate":"2014-03-04T14:20:25","indexId":"tem694","displayToPublicDate":"1953-01-01T11:25:00","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"694","title":"Geology of the Davis Mesa quadrangle, Colorado","docAbstract":"The Davis Mesa quadrangle is one of eighteen 7 1/2-minute quadrangles covering the principal carnotite-producing area of southwestern Colorado.  The geology of these quadrangles was mapped by the U.S. Geological Survey for the Atomic Energy Commission as part of a comprehensive study of carnotite deposits. The rocks exposed in the eighteen quadrangles consist of crystalline rocks of pre-Cambrian age and sedimentary rocks that range in age from late Paleozoic to Quaternary. Over much of the area the sedimentary rocks are flat lying, but in places the rocks are disrupted by hih-angle faults, and northwest-trending folds.  Conspicuous among the folds are large anticlines having cores of intrusive salt and gypsum.  Most of the carnotite deposits are confined to the Salt Wash sandstone member of Jurassic Morrison formation.  Within this sandstone, most of the deposits are spottily distributed through an arcuate zone known as \"Uruvan Mineral Belt\".  Individual deposits range in size from irregular masses containing only a few tons of ore to large, tabular masses containing many thousands of tons.  The ore consists largely of sandstone selectively impregnated and in part replaced by uranium and vanadium minerals.  Most of the deposits appear to be related to certain sedimentary structures in sandstones of favorable composition.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem694","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Cater, F.W., and Bryner, L., 1953, Geology of the Davis Mesa quadrangle, Colorado: U.S. Geological Survey Trace Elements Memorandum 694, Report: 29 p.; 1 Plate: 34.57 x 28.53 inches, https://doi.org/10.3133/tem694.","productDescription":"Report: 29 p.; 1 Plate: 34.57 x 28.53 inches","numberOfPages":"32","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278603,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0694/report-thumb.jpg"},{"id":283317,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0694/plate-1.pdf"},{"id":283318,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0694/report.pdf"}],"country":"United States","state":"Colorado","otherGeospatial":"Davis Mesa Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.875,38.25 ], [ -108.875,38.375 ], [ -108.75,38.375 ], [ -108.75,38.25 ], [ -108.875,38.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52737beae4b097f32ac3db24","contributors":{"authors":[{"text":"Cater, Fred W. Jr.","contributorId":36988,"corporation":false,"usgs":true,"family":"Cater","given":"Fred","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":485492,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bryner, Leonid","contributorId":50041,"corporation":false,"usgs":true,"family":"Bryner","given":"Leonid","email":"","affiliations":[],"preferred":false,"id":485493,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":71366,"text":"tei318 - 1953 - A quantitative radiochemical method for the determination of the major sources of natural radioactivity in ores and minerals","interactions":[],"lastModifiedDate":"2014-06-06T10:25:24","indexId":"tei318","displayToPublicDate":"1953-01-01T11:16:00","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"318","title":"A quantitative radiochemical method for the determination of the major sources of natural radioactivity in ores and minerals","docAbstract":"<p>The determination of Th<sup>232</sup>, Rn<sup>222</sup>, and Pb<sup>210</sup> by isolation and subsequent activity analysis of some of their short-lived daughter products is described. The sulfides of bismuth and polonium are precipitated out of solutions of thorium or uranium ores, and the alpha particle activity of PO<sup>214</sup>. PO<sup>212</sup> and PO<sup>210</sup> is determined by scintillation counting techniques. PO<sup>214</sup> activity is used to determine Rn<sup>222</sup>, PO<sup>212</sup> activity for Th<sup>232</sup>, and PO<sup>210</sup> for Pb<sup>210</sup>.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei318","collaboration":"Prepared by the Geological Survey for the United States Atomic Energy Commission","usgsCitation":"Rosholt, J.N., 1953, A quantitative radiochemical method for the determination of the major sources of natural radioactivity in ores and minerals: U.S. Geological Survey Trace Elements Investigations 318, 35 p., https://doi.org/10.3133/tei318.","productDescription":"35 p.","numberOfPages":"35","costCenters":[],"links":[{"id":284061,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei318.jpg"},{"id":285638,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0318/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53558fc0e4b0120853e8be10","contributors":{"authors":[{"text":"Rosholt, John Nicholas Jr.","contributorId":26370,"corporation":false,"usgs":true,"family":"Rosholt","given":"John","suffix":"Jr.","email":"","middleInitial":"Nicholas","affiliations":[],"preferred":false,"id":284058,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70048725,"text":"tem693 - 1953 - Geology of the Calamity Mesa quadrangle, Mesa county, Colorado","interactions":[],"lastModifiedDate":"2014-03-04T14:19:49","indexId":"tem693","displayToPublicDate":"1953-01-01T11:08:00","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"693","title":"Geology of the Calamity Mesa quadrangle, Mesa county, Colorado","docAbstract":"The Calamity Mesa quadrangle is one of eighteen 7 1/2-minute quadrangles covering the principal carnotite-producing area of southwestern Colorado.  The geology of these quadrangles was mapped by the U.S. Geological Survey for the Atomic Energy Commission as part of a comprehensive study of carnotite deposits.  The rocks exposed in the eighteen quadrangles consist of crystalline rocks of pre-Cambrian age and sedimentary rocks the range in age from late Paleozoic to Quaternary.  Over much of the area the sedimentary rocks are flat lying, but in places the rocks are disrupted by high-angle faults, and northwest-trending folds.  Conspicuous among the folds are large anticlines having cores of intrusive salt and gypsum.  Most of the carnotite deposits are confined to the Salt Wash sandstone member of the Jurassic Morrison formation.  Within this sandstone, most of the deposits are spottily distributed through an arcuate zone known as the \"Uravan Mineral Belt\".  Individual deposits range in size from irregular masses containing only a few tons of ore to large tabular masses containing many thousands of tons.  The ore consists largely of sandstone selectively impregnated and in part replaced by uranium and vanadium minerals.  Most of the deposits appear to be related to certain sedimentary structures in sandstones of favorable composition.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem693","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Cater, F.W., and Stager, H., 1953, Geology of the Calamity Mesa quadrangle, Mesa county, Colorado: U.S. Geological Survey Trace Elements Memorandum 693, Report: 36 p.; 1 Plate: 30.68 x 28.56 inches, https://doi.org/10.3133/tem693.","productDescription":"Report: 36 p.; 1 Plate: 30.68 x 28.56 inches","numberOfPages":"39","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278602,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0693/report-thumb.jpg"},{"id":283315,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0693/plate-1.pdf"},{"id":283316,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0693/report.pdf"}],"country":"United States","state":"Colorado","county":"Mesa County","otherGeospatial":"Calamity Mesa Quardangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.875,38.5 ], [ -108.875,38.625 ], [ -108.75,38.625 ], [ -108.75,38.5 ], [ -108.875,38.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52737beae4b097f32ac3db21","contributors":{"authors":[{"text":"Cater, Fred W. Jr.","contributorId":36988,"corporation":false,"usgs":true,"family":"Cater","given":"Fred","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":485491,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stager, Harold K.","contributorId":17625,"corporation":false,"usgs":true,"family":"Stager","given":"Harold K.","affiliations":[],"preferred":false,"id":485490,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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