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At these localities the thorium occurs as a major constituent or in minor amounts as an impurity in one or more of the following 12 minerals: allanite, columbite, ellsworthite, eschynite, gummite, monazite, orangite, parisite, thorianite, thorite, xenotime, and zircon. In addition other minerals, such as biotite and sphene, are radioactive and may contain thorium. Several unidentified columbate minerals with uranium or thorium and uranium as major constituents have been recognized at some localities. The distribution, by type of deposit, of the 57 thorium occurrences is as follows: lode - 3, lode and placer - 1, granitic rock - 3, granitic rock and related placer - 14, and placer - 26. Of the four lode occurrences only the radioactive veins at Salmon Bay in southeastern Alaska and the contact metamorphic deposit in the Nixon Fork area of central Alaska warrant further consideration, although insufficient data are available to determine whether these two deposits have commercial possibilities. The remaining occurrences of thorium-bearing minerals in Alaska are limited to placer deposits and disseminations of accessory minerals in granitic rocks. In most of these occurrences the thorium-bearing minerals occur in only trace amounts and consequently warrent little further consideration. More data are needed to determine the possibilities of byproduct recovery of thorium-bearing minerals from several of the gold and tin placers.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem339","collaboration":"This reports concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Bates, R., and Wedow, H., 1952, Preliminary summary review of thorium-bearing mineral occurrences in Alaska: U.S. Geological Survey Trace Elements Memorandum 339, Report: 28 p.; 1 Plate: 19.61 x 15.26 inches, https://doi.org/10.3133/tem339.","productDescription":"Report: 28 p.; 1 Plate: 19.61 x 15.26 inches","numberOfPages":"30","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":277878,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0339/report-thumb.jpg"},{"id":283103,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0339/report.pdf"},{"id":283104,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0339/plate-1.pdf"}],"country":"United States","state":"Alaska","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 172.45,51.21 ], [ 172.45,71.39 ], [ -129.99,71.39 ], [ -129.99,51.21 ], [ 172.45,51.21 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"523c1cf8e4b024b60d407375","contributors":{"authors":[{"text":"Bates, Robert G.","contributorId":102867,"corporation":false,"usgs":true,"family":"Bates","given":"Robert G.","affiliations":[],"preferred":false,"id":484242,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wedow, Helmuth Jr.","contributorId":14374,"corporation":false,"usgs":true,"family":"Wedow","given":"Helmuth","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":484241,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70048329,"text":"tem420 - 1952 - Red Rock Valley NE, preliminary geologic map of part of the Carrizo Mountains area, northeastern Arizona and northwestern New Mexico","interactions":[],"lastModifiedDate":"2014-02-28T14:52:01","indexId":"tem420","displayToPublicDate":"1952-01-01T13:05:00","publicationYear":"1952","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":"420","title":"Red Rock Valley NE, preliminary geologic map of part of the Carrizo Mountains area, northeastern Arizona and northwestern New Mexico","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem420","usgsCitation":"Strobell, J., 1952, Red Rock Valley NE, preliminary geologic map of part of the Carrizo Mountains area, northeastern Arizona and northwestern New Mexico: U.S. Geological Survey Trace Elements Memorandum 420, Report: 2 p.; 1 Plate: 31.34 x 39.58 inches, https://doi.org/10.3133/tem420.","productDescription":"Report: 2 p.; 1 Plate: 31.34 x 39.58 inches","numberOfPages":"2","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":277971,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0420/report-thumb.jpg"},{"id":283133,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0420/report.pdf"},{"id":283134,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0420/plate-1.pdf"}],"scale":"20000","country":"United States","state":"Arizona","otherGeospatial":"Carrizo Mountains","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.125,36.625 ], [ -109.125,36.75 ], [ -109.0,36.75 ], [ -109.0,36.625 ], [ -109.125,36.625 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"523d6e67e4b097188d6c7700","contributors":{"authors":[{"text":"Strobell, J.D. 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Unless the concentration of radioactive minerals in the beach deposits is considerably higher than the present qualitative data indicate, the placers at Yakataga beach do not constitute a feasible source of supply of radioactive materials.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem326","collaboration":"The report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Moxham, R.M., 1952, Radioactive minerals in the Yakataga beach placers, southern Alaska: U.S. Geological Survey Trace Elements Memorandum 326, Report: 10 p.; 1 Plate: 16.37 x 14.87 inches, https://doi.org/10.3133/tem326.","productDescription":"Report: 10 p.; 1 Plate: 16.37 x 14.87 inches","numberOfPages":"13","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":277561,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0326/report-thumb.jpg"},{"id":283097,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0326/plate-1.pdf"},{"id":283098,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0326/report.pdf"}],"country":"United States","state":"Alaska","otherGeospatial":"Yakataga Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -142.7101,59.856 ], [ -142.7101,60.278 ], [ -140.8975,60.278 ], [ -140.8975,59.856 ], [ -142.7101,59.856 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"523433f0e4b0b9e9b3336db7","contributors":{"authors":[{"text":"Moxham, Robert M.","contributorId":56210,"corporation":false,"usgs":true,"family":"Moxham","given":"Robert","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":483917,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70048324,"text":"tem419 - 1952 - Red Rock Valley NW, preliminary geologic map of part of the Carrizo Mountains area, northeastern Arizona","interactions":[],"lastModifiedDate":"2014-02-28T14:51:20","indexId":"tem419","displayToPublicDate":"1952-01-01T11:49:00","publicationYear":"1952","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":"419","title":"Red Rock Valley NW, preliminary geologic map of part of the Carrizo Mountains area, northeastern Arizona","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem419","usgsCitation":"Strobell, J., 1952, Red Rock Valley NW, preliminary geologic map of part of the Carrizo Mountains area, northeastern Arizona: U.S. Geological Survey Trace Elements Memorandum 419, Report: 2 p.; 1 Plate: 30.84 x 39.14 inches, https://doi.org/10.3133/tem419.","productDescription":"Report: 2 p.; 1 Plate: 30.84 x 39.14 inches","numberOfPages":"2","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":277969,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0419/report-thumb.jpg"},{"id":283131,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0419/plate-1.pdf"},{"id":283132,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0419/report.pdf"}],"scale":"20000","country":"United States","state":"Arizona","otherGeospatial":"Carrizo Mountains","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.25,36.625 ], [ -109.25,36.75 ], [ -109.125,36.75 ], [ -109.125,36.625 ], [ -109.25,36.625 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"523d6e68e4b097188d6c7704","contributors":{"authors":[{"text":"Strobell, J.D. 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Jr.","contributorId":22823,"corporation":false,"usgs":true,"family":"Strobell","given":"J.D.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":484317,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70048322,"text":"tem417 - 1952 - Los Gigantes NW, preliminary geologic map of part of the Carrizo mountains area, northeastern Arizona","interactions":[],"lastModifiedDate":"2014-02-28T14:50:14","indexId":"tem417","displayToPublicDate":"1952-01-01T11:38:00","publicationYear":"1952","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":"417","title":"Los Gigantes NW, preliminary geologic map of part of the Carrizo mountains area, northeastern Arizona","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem417","usgsCitation":"Strobell, J., 1952, Los Gigantes NW, preliminary geologic map of part of the Carrizo mountains area, northeastern Arizona: U.S. Geological Survey Trace Elements Memorandum 417, Report: 2 p.; 1 Plate: 30.67 x 38.96 inches, https://doi.org/10.3133/tem417.","productDescription":"Report: 2 p.; 1 Plate: 30.67 x 38.96 inches","numberOfPages":"2","costCenters":[],"links":[{"id":277967,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0417/report-thumb.jpg"},{"id":283127,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0417/report.pdf"},{"id":283128,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0417/plate-1.pdf"}],"scale":"20000","country":"United States","state":"Arizona","otherGeospatial":"Carrizo Mountains","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.5,36.625 ], [ -109.5,36.75 ], [ -109.375,36.75 ], [ -109.375,36.625 ], [ -109.5,36.625 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"523d6e62e4b097188d6c76c3","contributors":{"authors":[{"text":"Strobell, J.D. Jr.","contributorId":22823,"corporation":false,"usgs":true,"family":"Strobell","given":"J.D.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":484316,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70113711,"text":"tei124 - 1952 - The uranium deposit at the Yellow Canary claims, Daggett County, Utah","interactions":[],"lastModifiedDate":"2014-07-14T11:04:44","indexId":"tei124","displayToPublicDate":"1952-01-01T11:33:00","publicationYear":"1952","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":"124","title":"The uranium deposit at the Yellow Canary claims, Daggett County, Utah","docAbstract":"

The Yellow Canary claims uranium deposit is on the west side of Red Creek Canyon in the northern part of the Uinta Mountains, Daggett County, Utah. The claims have been developed by two adits, three open cuts, and several hundred deep of bulldozer trenches. No uranium ore has been produced from this deposit.

\n
\n

The uranium deposit at the Yellow Canary claims is in the Red Creek quartzite of pre-Cambrian age. The formation is composed of intercalated beds of quartzite, hornblendite, garnet schist, staurolite schist, and quartz-mica schist and is intruded by diorite dikes. A thick unit of highly fractured white quatrzite at the top of the formation contains tyutamunite as coatings on fracture surfaces. The tyutamunite is associated with carnotite, volborthite, iron oxides, azurite, malachite, brochantite, and hyalite. The secondary uranium and vanadium minerals are believed to be alteration products of primary minerals.

\n
\n

The uranium content of 15 samples from this property ranged from 0.000 to 0.57 percent.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei124","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Wilmarth, V., Vickers, R., McKeown, F.A., and Beroni, E., 1952, The uranium deposit at the Yellow Canary claims, Daggett County, Utah: U.S. Geological Survey Trace Elements Investigations 124, Report: 21 p.; 2 Plates: 16.94 x 21.97 inches and 12.62 x 9.70 inches, https://doi.org/10.3133/tei124.","productDescription":"Report: 21 p.; 2 Plates: 16.94 x 21.97 inches and 12.62 x 9.70 inches","numberOfPages":"22","costCenters":[],"links":[{"id":289889,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":289887,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0124/figure-3.pdf"},{"id":289888,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0124/report.pdf"},{"id":289886,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0124/figure-2.pdf"}],"country":"United States","state":"Utah","county":"Daggatt County","otherGeospatial":"Yellow Canary Claims","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.5,40.75 ], [ -109.5,41.5 ], [ -108.75,41.5 ], [ -108.75,40.75 ], [ -109.5,40.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ae7870e4b0abf75cf2d519","contributors":{"authors":[{"text":"Wilmarth, V.R.","contributorId":20803,"corporation":false,"usgs":true,"family":"Wilmarth","given":"V.R.","email":"","affiliations":[],"preferred":false,"id":495139,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vickers, R.C.","contributorId":50583,"corporation":false,"usgs":true,"family":"Vickers","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":495140,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McKeown, F. A.","contributorId":106100,"corporation":false,"usgs":true,"family":"McKeown","given":"F.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":495141,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Beroni, E.P.","contributorId":13222,"corporation":false,"usgs":true,"family":"Beroni","given":"E.P.","affiliations":[],"preferred":false,"id":495138,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70048321,"text":"tem416 - 1952 - Dinne Mesa SW, preliminary geologic map of part of the Carrizo Moutains area, northeastern Arizona","interactions":[],"lastModifiedDate":"2014-02-28T14:49:38","indexId":"tem416","displayToPublicDate":"1952-01-01T11:24:00","publicationYear":"1952","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":"416","title":"Dinne Mesa SW, preliminary geologic map of part of the Carrizo Moutains area, northeastern Arizona","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem416","usgsCitation":"Strobell, J., 1952, Dinne Mesa SW, preliminary geologic map of part of the Carrizo Moutains area, northeastern Arizona: U.S. Geological Survey Trace Elements Memorandum 416, Report: 2 p.; 1 Plate: 31.83 x 39.61 inches, https://doi.org/10.3133/tem416.","productDescription":"Report: 2 p.; 1 Plate: 31.83 x 39.61 inches","numberOfPages":"2","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":277961,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0416/report-thumb.jpg"},{"id":283125,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0416/report.pdf"},{"id":283126,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0416/plate-1.pdf"}],"scale":"20000","country":"United States","state":"Arizona","otherGeospatial":"Carrizo Mountains","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.5,36.75 ], [ -109.5,36.875 ], [ -109.375,36.875 ], [ -109.375,36.75 ], [ -109.5,36.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"523d6e60e4b097188d6c76b2","contributors":{"authors":[{"text":"Strobell, J.D. Jr.","contributorId":22823,"corporation":false,"usgs":true,"family":"Strobell","given":"J.D.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":484315,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":71260,"text":"tei195 - 1952 - Radioactivity at the Copper Creek copper lode prospect, Eagle district, east-central Alaska","interactions":[],"lastModifiedDate":"2014-04-03T14:47:18","indexId":"tei195","displayToPublicDate":"1952-01-01T11:24:00","publicationYear":"1952","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":"195","title":"Radioactivity at the Copper Creek copper lode prospect, Eagle district, east-central Alaska","docAbstract":"Investigation of radioactivity anomalies at the Copper Creek copper lode prospect, Eagle district, east-central Alaska, during 1949 disclosed that the radioactivity is associated with copper mineralization in highly metamorphosed sedimentary rocks. These rocks are a roof pendant in the Mesozoic \"Charley River\" batholith. The radioactivity is probably all due to uranium associated with bornite and malachite.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei195","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Wedow, H., and Tolbert, G.E., 1952, Radioactivity at the Copper Creek copper lode prospect, Eagle district, east-central Alaska: U.S. Geological Survey Trace Elements Investigations 195, 10 p., https://doi.org/10.3133/tei195.","productDescription":"10 p.","numberOfPages":"11","costCenters":[],"links":[{"id":283644,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei195.jpg"},{"id":285615,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0195/report.pdf"}],"country":"United States","state":"Alaska","otherGeospatial":"Eagle District","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -144.0,64.0 ], [ -144.0,66.0 ], [ -141.0,66.0 ], [ -141.0,64.0 ], [ -144.0,64.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5355952fe4b0120853e8c178","contributors":{"authors":[{"text":"Wedow, Helmuth","contributorId":67495,"corporation":false,"usgs":true,"family":"Wedow","given":"Helmuth","affiliations":[],"preferred":false,"id":283913,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tolbert, Gene Edward","contributorId":74443,"corporation":false,"usgs":true,"family":"Tolbert","given":"Gene","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":283914,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70048169,"text":"tem325 - 1952 - Preliminary report on the White Canyon area, San Juan county, Utah","interactions":[{"subject":{"id":70048169,"text":"tem325 - 1952 - Preliminary report on the White Canyon area, San Juan county, Utah","indexId":"tem325","publicationYear":"1952","noYear":false,"title":"Preliminary report on the White Canyon area, San Juan county, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":4157,"text":"cir217 - 1952 - Preliminary Report on the White Canyon Area, San Juan County, Utah","indexId":"cir217","publicationYear":"1952","noYear":false,"title":"Preliminary Report on the White Canyon Area, San Juan County, Utah"},"id":1}],"supersededBy":{"id":4157,"text":"cir217 - 1952 - Preliminary Report on the White Canyon Area, San Juan County, Utah","indexId":"cir217","publicationYear":"1952","noYear":false,"title":"Preliminary Report on the White Canyon Area, San Juan County, Utah"},"lastModifiedDate":"2014-02-28T14:39:07","indexId":"tem325","displayToPublicDate":"1952-01-01T11:21:00","publicationYear":"1952","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":"325","title":"Preliminary report on the White Canyon area, San Juan county, Utah","docAbstract":"The White Canyon area, in the central part of San Juan County, Utah, consists of approximately two 15-minute quadrangles. Approximately 75 square miles have been mapped by the Geological Survey on a scale of 1 inch equals 1 mile, using a combined aerial photography-plane table method. Structure contours were drawn on top of the Organ Rock member of the Cutler formation. Parts of the Gonway and North Point claims, 1/4 mile east of the Happy Jack mine, were mapped in detail. The principal objectives of the investigations were: (1) to establish ore guides; (2) to select areas favorable for exploration; and (3) to map the general geology and to determine the regional relationships of the uranium deposits. The White Canyon area is comprised of sedimentary rocks of Carboniferous to Jurassic age, more than 2,000 feet thick, having a regional dip of 1° to 2° SW. The nearest igneous rocks are in the Henry Mountains about 7 miles west of the northern part of the area; The Shinarump conglomerate of the late Triassic age, the principal ore horizon in the White Canyon area, consists of lenticular beds of sandstone, conglomeratic sandstone, conglomerate, clay, and siltstone. The Shinarump conglomerate, absent in places, is as much as 75 feet thick. The sandstones locally contain molds of logs and fragments of altered volcanic ash. Some of the logs have been replaced by copper and uranium minerals and iron oxides. The clay and siltstone underlie and are interbedded with the sandstone, and are most common in channels that cut into the underlying Moenkopi formation. The Shinarump conglomerate contains reworked Moenkopi siltstone fragments, clay balls, carbonized wood, and pebbles of quarts, quartzite, and chert. Jointing is prominent in the Western part of the mapped area. The three most prominent joint trends are due east, N. 65°-75° W., and N. 65°-75° E. All joints have vertical dips. The red beds are bleached along some joints, especially those that trend N. 65°-75° W. All uranium ore produced has been from the lower part of the Shinarump conglomerate, where it commonly occurs with copper as disseminations and fracture coatings in sandstone. Uranium and copper minerals also occur in low-grade disseminated deposits in the lower Chinle and in the Moenkopi formation and in veins cutting these formations. Although some uranium deposits occur in Chinarump channels and scours, copper and uranium minerals along fractures suggest that channel control may be secondary. Logs and clay balls apparently have exerted some chemical influences for deposition. The uranium occurs as the oxide in some deposits, and as secondary hydrous sulfates, phosphates, oxides, and silicates in these and several other deposits. Charcoal, iron and manganese oxides, and veinlets of hydrocarbon are abnormally radioactive in most of the deposits. Base-metal sulfides are commonly found inside the oxidized zone. Secondary copper minerals include the hydrous sulfates and carbonate. Gangue minerals include quarts, clay minerals, and manganese oxides, dickite (?), calcite, gypsum, pyrite, and chalcedony (?). Principal wall-rock alteration appears to have been silicification, clay alteration, and bleaching. Most of the shipped ore has contained more than 0.3 percent uranium. The ore also contains copper, commonly in grades lower than 1.0 percent. Criteria believed to be most useful for prospecting for concealed uranium deposits are (1) visible uranium minerals; (2) sulfide minerals; (3) secondary copper minerals; (4) dickite (?); (5) hydrocarbons; and (6) bleaching and alteration of the Moenkopi formation.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem325","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Benson, W.E., Trites, A.F., Beroni, E.P., and Feeger, J.A., 1952, Preliminary report on the White Canyon area, San Juan county, Utah: U.S. Geological Survey Trace Elements Memorandum 325, Report: 27 p.; 2 Plates: 20.77 x 16.37 inches and 26.04 x 30.11 inches, https://doi.org/10.3133/tem325.","productDescription":"Report: 27 p.; 2 Plates: 20.77 x 16.37 inches and 26.04 x 30.11 inches","numberOfPages":"27","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":277558,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0325/report-thumb.jpg"},{"id":283096,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0325/report.pdf"},{"id":283094,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0325/plate-2.pdf"},{"id":283095,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0325/plate-3.pdf"}],"country":"United States","state":"Utah","county":"San Juan County","otherGeospatial":"White Canyon","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.5,37.25 ], [ -110.5,38.0 ], [ -109.75,38.0 ], [ -109.75,37.25 ], [ -110.5,37.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"523433efe4b0b9e9b3336dad","contributors":{"authors":[{"text":"Benson, William E.","contributorId":58931,"corporation":false,"usgs":true,"family":"Benson","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":483909,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trites, Albert F. Jr.","contributorId":40652,"corporation":false,"usgs":true,"family":"Trites","given":"Albert","suffix":"Jr.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":483908,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Beroni, Ernest P.","contributorId":9347,"corporation":false,"usgs":true,"family":"Beroni","given":"Ernest","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":483907,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Feeger, John A.","contributorId":102778,"corporation":false,"usgs":true,"family":"Feeger","given":"John","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":483910,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":71933,"text":"tem301 - 1952 - Tectonic map of the Colorado Plateau","interactions":[],"lastModifiedDate":"2014-07-16T11:11:49","indexId":"tem301","displayToPublicDate":"1952-01-01T11:09:44","publicationYear":"1952","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":"301","title":"Tectonic map of the Colorado Plateau","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/tem301","usgsCitation":"Luedke, R.G., and Shoemaker, E.M., 1952, Tectonic map of the Colorado Plateau: U.S. Geological Survey Trace Elements Memorandum 301, 1 map, https://doi.org/10.3133/tem301.","productDescription":"1 map","costCenters":[],"links":[{"id":290269,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Arizona;Utah","otherGeospatial":"Colorado Plateau","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.064986,36.964627 ], [ -110.064986,37.035916 ], [ -109.936926,37.035916 ], [ -109.936926,36.964627 ], [ -110.064986,36.964627 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c79f18e4b01948416424b8","contributors":{"authors":[{"text":"Luedke, Robert G.","contributorId":18339,"corporation":false,"usgs":true,"family":"Luedke","given":"Robert","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":284903,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shoemaker, Eugene Merle","contributorId":20342,"corporation":false,"usgs":true,"family":"Shoemaker","given":"Eugene","email":"","middleInitial":"Merle","affiliations":[],"preferred":false,"id":284904,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70210468,"text":"70210468 - 1952 - Stratigraphy and paleontology of the Noatak and associated formations, Brooks Range, Alaska","interactions":[],"lastModifiedDate":"2021-08-31T15:09:42.366714","indexId":"70210468","displayToPublicDate":"1952-01-01T11:08:23","publicationYear":"1952","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":"33","subseriesTitle":"Special Report","title":"Stratigraphy and paleontology of the Noatak and associated formations, Brooks Range, Alaska","docAbstract":"

A think complex sequence of olastic rocks, formerly named the Noatak formation, underlies the Lisburns formation (Mississippian) in the Brooks Range, northern Alaska. Five formations have been recognized as a result of of recent investigations by the author and other geologists of the Navy Oil Unit, U.S. Geological Survey. In the western Brooks Range, the three formations present below the Lisburns formation are: Utukok formation (Upper Touranisian to Lower Visean), Montak formation (restricted) (Upper Devonian to Lower Tournaisian (?)) and Hunt Fork (?) formation (Upper Devonian). In the central Brooks Range the Kayak formation (Lower to Upper Tournaisian), Kanayut formation (Upper Devonian to Lower Tournaisian (?)), and Hunt Fork formation (Upper Devonian) lie below the Lisburns formation.

Lithologic and faunal characteristics of these sedimentary units reveal the regional pattern of sedimentation and suggest specific paleoecologic environments. The chart conglomerates in the Kanayut and Noatuk formations are thought to have formed in a belt characterized by fluctuating marine and nonmarine conditions, the chart source being a mid-Devonian ragolith.

Analysis of formulas suggest certain correlations with the European, Siberian, and western Cordilleran sections.

Described faunas of the Utukok and Kayak formations include 40 braciopod species and varieties, 9 echinodera species, 2 bryzoan species, 8 molluscan species, and 1 tribute species, of which 13 are new.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70210468","usgsCitation":"Dutro, J.T., 1952, Stratigraphy and paleontology of the Noatak and associated formations, Brooks Range, Alaska: Geological Investigations, Naval Petroleum Reserve No. 4, Alaska 33, Report: iii, 144 p.; 3 Plates; 1 Table, https://doi.org/10.3133/70210468.","productDescription":"Report: iii, 144 p.; 3 Plates; 1 Table","numberOfPages":"172","costCenters":[],"links":[{"id":375338,"rank":1,"type":{"id":15,"text":"Index 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Thomas Jr.","contributorId":102878,"corporation":false,"usgs":true,"family":"Dutro","given":"J.","suffix":"Jr.","email":"","middleInitial":"Thomas","affiliations":[],"preferred":false,"id":822257,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":71245,"text":"tei176 - 1952 - The Robinson and Weatherly uraniferous pyrobitumen deposits near Placerville, San Miguel County, Colorado","interactions":[],"lastModifiedDate":"2014-04-03T14:45:54","indexId":"tei176","displayToPublicDate":"1952-01-01T10:56:00","publicationYear":"1952","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":"176","title":"The Robinson and Weatherly uraniferous pyrobitumen deposits near Placerville, San Miguel County, Colorado","docAbstract":"Uranium deposits that contain uraniferous pyrobitumen of possible hydrothermal origin occur at the Weatherly and Robinson properties near Placerville, San Miguel County, Colo. These deposits were mined for copper, silver, and gold more than 50 years ago and were developed for uranium in 1950.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei176","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Wilmarth, V., and Vickers, R., 1952, The Robinson and Weatherly uraniferous pyrobitumen deposits near Placerville, San Miguel County, Colorado: U.S. Geological Survey Trace Elements Investigations 176, 47 p., https://doi.org/10.3133/tei176.","productDescription":"47 p.","numberOfPages":"48","costCenters":[],"links":[{"id":283639,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei176.jpg"},{"id":285612,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0176/report.pdf"}],"country":"United States","state":"Colorado","county":"San Miguel County","city":"Placerville","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":"5355959de4b0120853e8c26a","contributors":{"authors":[{"text":"Wilmarth, V.R.","contributorId":20803,"corporation":false,"usgs":true,"family":"Wilmarth","given":"V.R.","email":"","affiliations":[],"preferred":false,"id":283858,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vickers, R.C.","contributorId":50583,"corporation":false,"usgs":true,"family":"Vickers","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":283859,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70048431,"text":"tem500A - 1952 - Photogeologic map, Orange Cliffs-13 quadrangle, Garfield county, Utah","interactions":[{"subject":{"id":70048431,"text":"tem500A - 1952 - Photogeologic map, Orange Cliffs-13 quadrangle, Garfield county, Utah","indexId":"tem500A","publicationYear":"1952","noYear":false,"chapter":"A","title":"Photogeologic map, Orange Cliffs-13 quadrangle, Garfield county, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":66898,"text":"i178 - 1956 - Photogeologic map of the Orange Cliffs-13 quadrangle, Garfield County, Utah","indexId":"i178","publicationYear":"1956","noYear":false,"title":"Photogeologic map of the Orange Cliffs-13 quadrangle, Garfield County, Utah"},"id":1}],"supersededBy":{"id":66898,"text":"i178 - 1956 - Photogeologic map of the Orange Cliffs-13 quadrangle, Garfield County, Utah","indexId":"i178","publicationYear":"1956","noYear":false,"title":"Photogeologic map of the Orange Cliffs-13 quadrangle, Garfield County, Utah"},"lastModifiedDate":"2014-03-04T13:39:52","indexId":"tem500A","displayToPublicDate":"1952-01-01T10:47:00","publicationYear":"1952","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":"500","chapter":"A","title":"Photogeologic map, Orange Cliffs-13 quadrangle, Garfield county, Utah","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem500A","collaboration":"Prepared in cooperation with the U.S. Atomic Energy Commission","usgsCitation":"Ray, R., 1952, Photogeologic map, Orange Cliffs-13 quadrangle, Garfield county, Utah: U.S. Geological Survey Trace Elements Memorandum 500, Report: 3 p.; 1 Plate: 23.31 x 29.90 inches, https://doi.org/10.3133/tem500A.","productDescription":"Report: 3 p.; 1 Plate: 23.31 x 29.90 inches","numberOfPages":"3","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278122,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0500-A/report-thumb.jpg"},{"id":283244,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0500-A/report.pdf"},{"id":283243,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0500-A/plate-1.pdf"}],"scale":"24000","country":"United States","state":"Utah","county":"Garfield County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.5,38.0 ], [ -110.5,38.125 ], [ -110.375,38.125 ], [ -110.375,38.0 ], [ -110.5,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52455768e4b0b3d37307e1ab","contributors":{"authors":[{"text":"Ray, R.G.","contributorId":60664,"corporation":false,"usgs":true,"family":"Ray","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":484629,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70098029,"text":"tei308 - 1952 - Reconnaissance for uraniferous rocks in northwestern Colorado, southwestern Wyoming, and northeastern Utah","interactions":[],"lastModifiedDate":"2014-06-06T08:35:49","indexId":"tei308","displayToPublicDate":"1952-01-01T10:29:00","publicationYear":"1952","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":"308","title":"Reconnaissance for uraniferous rocks in northwestern Colorado, southwestern Wyoming, and northeastern Utah","docAbstract":"

Previous discoveries and studies of radioactive lignites of Tertiary age in North Dakota, South Dakota, Montana, and Wyoming led the Geological Survey in 1950 to do reconnaissance in the Green River and Uinta Basin of Wyoming and Utah, where similar lignites were believed to be present. Because of the common association of uranium with copper deposits and the presence of such deposits in the Uinta Basin, several areas containing copper-uranium minerals were also examined.

\n
\n

No deposits commercially exploitable under present conditions were found. Samples of coal from the Bear River formation at Sage, Wyo., assayed 0.004 to 0.013 percent uranium in the ash; in the old Uteland copper mine in Uinta County, Utah, 0.007 to 0.017 percent uranium; in a freshwater limestone, Duchesne County, Utah, as much as 0.019 percent uranium; and in the Mesaverde formation at the Snow and Bonniebell claims near Jensen, Uintah County, Utah, 0.003 to 0.090 percent uranium. Maps were made and samples were taken at the Skull Creek carnotite deposits in Moffat County, Colo. (0.006 to 0.16 percent uranium); at the Fair-U claims in Routt County, Colo. (0.002 to 0.040 percent uranium); and at the Lucky Strike claims near Kremmling in Grand County, Colo. (0.006 to 0.018 percent uranium).

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei308","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Beroni, E., and McKeown, F.A., 1952, Reconnaissance for uraniferous rocks in northwestern Colorado, southwestern Wyoming, and northeastern Utah: U.S. Geological Survey Trace Elements Investigations 308, Report: 41 p.; 1 Plate: 16.75 x 15.21 inches, https://doi.org/10.3133/tei308.","productDescription":"Report: 41 p.; 1 Plate: 16.75 x 15.21 inches","numberOfPages":"42","costCenters":[],"links":[{"id":284054,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei308.jpg"},{"id":285633,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0308/report.pdf"},{"id":285632,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0308/figure-1.pdf"}],"country":"United States","state":"Colorado;Utah;Wyoming","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.5,38.5 ], [ -111.5,42.5 ], [ -106.0,42.5 ], [ -106.0,38.5 ], [ -111.5,38.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53559532e4b0120853e8c193","contributors":{"authors":[{"text":"Beroni, E.P.","contributorId":13222,"corporation":false,"usgs":true,"family":"Beroni","given":"E.P.","affiliations":[],"preferred":false,"id":491545,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McKeown, F. A.","contributorId":106100,"corporation":false,"usgs":true,"family":"McKeown","given":"F.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":491546,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":71319,"text":"tei265 - 1952 - The geology of the Florida land-pebble phosphate deposits","interactions":[],"lastModifiedDate":"2014-06-06T08:28:50","indexId":"tei265","displayToPublicDate":"1952-01-01T10:17:00","publicationYear":"1952","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":"265","title":"The geology of the Florida land-pebble phosphate deposits","docAbstract":"

The land-pebble phosphate district is on the Gulf Coastal Plain of Florida. The phosphate deposits are in the Bone Valley formation, dated Pliocene by most writers. These strata overlie the Miocene Hawthorn formation and are overlain by consolidated sands 3 to 20 feet thick.

\n
\n

The minable phosphate deposits, called “matrix” in the district, range from a featheredge to about 50 feet in thickness and consist of phosphatic pellets and nodules, quartz sand, and montmorillonitic clay in about equal proportions. Locally the matrix displays cross-bedding and horizontal laminations, but elsewhere it is structureless. The phosphorite particles, composed largely of carbonate-fluorapatite, range in diameter from less than 0.1 mm to about 60 cm and in P2O5 content from 30 to 36 percent. Coarse-pebble deposits, containing 30 to 34 percent P2O5 are found mainly on basement highs; and fine-pebble deposits, containing 32 to 36 percent P2O5 are, are found in basement lows. Deposits in the northern part of the field contain more phosphate particles and their P2O5 content is higher than those in the southern part.

\n
\n

The upper part of the phosphatic strata is leached to an advanced degree and consists of quartz sand and clay-sized particules of pseudowavellite and wavellite. The leached zone ranges in thickness from a featheredge to 60 feet.

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\n

The origin of the land-pebble deposits is incompletely known. Possible modes of origin are a residuum of Miocene age, or a reworked residuum of Pliocene or Quaternary age.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei265","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Cathcart, J., Blade, L., Davidson, D., and Ketner, K.B., 1952, The geology of the Florida land-pebble phosphate deposits: U.S. Geological Survey Trace Elements Investigations 265, 21 p., https://doi.org/10.3133/tei265.","productDescription":"21 p.","numberOfPages":"22","costCenters":[],"links":[{"id":284053,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei265.jpg"},{"id":285631,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0265/report.pdf"}],"country":"United States","state":"Florida","otherGeospatial":"Gulf Coastal Plain","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.5,27.0 ], [ -82.5,28.25 ], [ -81.5,28.25 ], [ -81.5,27.0 ], [ -82.5,27.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5355959fe4b0120853e8c281","contributors":{"authors":[{"text":"Cathcart, J.B.","contributorId":83533,"corporation":false,"usgs":true,"family":"Cathcart","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":283986,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blade, L.V.","contributorId":65093,"corporation":false,"usgs":true,"family":"Blade","given":"L.V.","email":"","affiliations":[],"preferred":false,"id":283984,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Davidson, D.F.","contributorId":68293,"corporation":false,"usgs":true,"family":"Davidson","given":"D.F.","email":"","affiliations":[],"preferred":false,"id":283985,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ketner, K. B.","contributorId":23121,"corporation":false,"usgs":true,"family":"Ketner","given":"K.","email":"","middleInitial":"B.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":283983,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70048427,"text":"tem446 - 1952 - Results of reconnaissance for uraniferous coal, lignite, and carbonaceous shale in western Montana","interactions":[{"subject":{"id":70048427,"text":"tem446 - 1952 - Results of reconnaissance for uraniferous coal, lignite, and carbonaceous shale in western Montana","indexId":"tem446","publicationYear":"1952","noYear":false,"title":"Results of reconnaissance for uraniferous coal, lignite, and carbonaceous shale in western Montana"},"predicate":"SUPERSEDED_BY","object":{"id":3839,"text":"cir251 - 1953 - Results of reconnaissance for uraniferous coal, lignite, and carbonaceous shale in western Montana","indexId":"cir251","publicationYear":"1953","noYear":false,"title":"Results of reconnaissance for uraniferous coal, lignite, and carbonaceous shale in western Montana"},"id":1}],"supersededBy":{"id":3839,"text":"cir251 - 1953 - Results of reconnaissance for uraniferous coal, lignite, and carbonaceous shale in western Montana","indexId":"cir251","publicationYear":"1953","noYear":false,"title":"Results of reconnaissance for uraniferous coal, lignite, and carbonaceous shale in western Montana"},"lastModifiedDate":"2014-03-04T13:37:44","indexId":"tem446","displayToPublicDate":"1952-01-01T10:05:00","publicationYear":"1952","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":"446","title":"Results of reconnaissance for uraniferous coal, lignite, and carbonaceous shale in western Montana","docAbstract":"A reconnaissance search for uraniferous lignite and carbonaceous shale was made in western Montana and adjacent parts of Idaho during the summer of 1951. Particular emphasis in the examination was placed on coal and carbonaceous shale associated with volcanic rocks, as volcanic rocks in many area appear to have released uranium to circulating ground water from which it was concentrated in carbonaceous material. Twenty-two area in Montana and one area of Idaho were examine. The coal in five of these area is of Cretaceous age. The coal and carbonaceous shale in the remaining 18 area occur in Tertiary \"lake-bed\" deposits of Oligocene and younger age. Both the Cretaceous and Tertiary coal and carbonaceous shale are associated with contemporaneous or younger volcanic rocks and pyroclastic sequences. A sample of carbonaceous shale from the Prickly Pear Valley northeast of Helena, Montana, contained 0.013 percent uranium. A sample of carbonaceous shale from the Flint Creek Valley southwest of Drummond, Montana, contained 0.006 percent uranium. All other samples of both Cretaceous and Tertiary coal and carbonaceous shale were essentially non-radioactive. No further work is planned on the Cretaceous and Tertiary coal and carbonaceous shale in western Montana. A few localities in Idaho will be visited in the course of other work.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem446","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Hail, W.J., and Gill, J.R., 1952, Results of reconnaissance for uraniferous coal, lignite, and carbonaceous shale in western Montana: U.S. Geological Survey Trace Elements Memorandum 446, Report: 22 p.; 1 Plate: 23.48 x 13.76 inches, https://doi.org/10.3133/tem446.","productDescription":"Report: 22 p.; 1 Plate: 23.48 x 13.76 inches","numberOfPages":"24","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278113,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0446/report-thumb.jpg"},{"id":283237,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0446/report.pdf"},{"id":283238,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0446/plate-1.pdf"}],"country":"United States","state":"Idaho;Montana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.05,44.3582 ], [ -116.05,47.4128 ], [ -109.6316,47.4128 ], [ -109.6316,44.3582 ], [ -116.05,44.3582 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5245576ae4b0b3d37307e1bc","contributors":{"authors":[{"text":"Hail, William J. Jr.","contributorId":99952,"corporation":false,"usgs":true,"family":"Hail","given":"William","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":484623,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gill, James R.","contributorId":44904,"corporation":false,"usgs":true,"family":"Gill","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":484622,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":25194,"text":"25194 - 1952 - Relative clauses","interactions":[],"lastModifiedDate":"2014-07-15T10:02:56","indexId":"25194","displayToPublicDate":"1952-01-01T10:01:38","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Relative clauses","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","doi":"10.3133/25194","issn":"0364-7064","usgsCitation":"Calkins, F.C., 1952, Relative clauses, 15 p., https://doi.org/10.3133/25194.","productDescription":"15 p.","numberOfPages":"15","costCenters":[],"links":[{"id":290100,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c64db0e4b0001bd51477a3","contributors":{"authors":[{"text":"Calkins, Frank Cathcart","contributorId":31734,"corporation":false,"usgs":true,"family":"Calkins","given":"Frank","email":"","middleInitial":"Cathcart","affiliations":[],"preferred":false,"id":193321,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70232383,"text":"70232383 - 1952 - Wildlife research: Or disaster!","interactions":[],"lastModifiedDate":"2022-07-19T16:30:16.911678","indexId":"70232383","displayToPublicDate":"1952-01-01T10:01:32","publicationYear":"1952","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":688,"text":"Alabama Conservation","active":true,"publicationSubtype":{"id":10}},"title":"Wildlife research: Or disaster!","docAbstract":"

No abstract available.

","language":"English","publisher":"Alabama Department of Conservation","usgsCitation":"Haugen, A.O., 1952, Wildlife research: Or disaster!: Alabama Conservation, v. 24, no. 3, p. 6-7.","productDescription":"2 p.","startPage":"6","endPage":"7","costCenters":[{"id":104,"text":"Alabama Cooperative Fish & Wildlife Unit","active":false,"usgs":true}],"links":[{"id":404037,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Haugen, Arnold O.","contributorId":292651,"corporation":false,"usgs":false,"family":"Haugen","given":"Arnold","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":846926,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":71301,"text":"tei242 - 1952 - Compilation of data on the uranium and equivalent uranium content of samples analyzed by U.S. Geological Survey during a program of sampling mine, mill, and smelter products","interactions":[],"lastModifiedDate":"2014-06-06T07:50:28","indexId":"tei242","displayToPublicDate":"1952-01-01T09:53:00","publicationYear":"1952","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":"242","title":"Compilation of data on the uranium and equivalent uranium content of samples analyzed by U.S. Geological Survey during a program of sampling mine, mill, and smelter products","docAbstract":"

In 1942 the Geological Survey began to collect, in response to a request made by the War Production Board, samples of mine, mill, and smelter products. About 1,400 such samples were collected and analyzed spectrographically for about 20 elements that were of strategic importance, in order to determine whether any of the products analyzed might be possible sources of some of the needed elements. When attention was directed to radioactive elements in 1943, most of the samples were scanned for radioactivity. Part of the work was done on behalf of the Division of Raw Materials of the Atomic Energy Commission.

\n
\n

The sources, mine mill, smelter, or prospect, from which these samples were collected, the kind of material sampled, i.e. ores, concentrates, middlings, tailings, flue dusts, and so forth, and the radioactivity of the samples are listed in this report. Samples of the materials collected in the course of the Geological Survey’s investigations for uranium are excluded, but about 500 such samples were analyzed spectrographically for some or all of the same 20 elements sought in the samples that are the subject of this report. Most of the samples were tested only for their radioactivity, but a few were analyzed chemically for uranium. The radioactivity of many of the samples tested in the early screening was determined only qualitatively. Several samples were tested at one time, and if the count obtained did not exceed a predetermined minimum above background, the samples were not tested individually. If the count was more than this minimum, the samples were tested individually to identify the radioactive sample or samples and to obtain a quantitative value for the radioactivity. In general, the rough screening served as a basis for separating samples in which the radioactivity amount to less than 0.003 percent equivalent uranium from those in which it exceeded that amount. Some aspects of various phases of the investigation of radioactivity in these samples have been reported in various other reports, as follows.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei242","collaboration":"This report concerns work done partly on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Hall, M.L., and Butler, A.P., 1952, Compilation of data on the uranium and equivalent uranium content of samples analyzed by U.S. Geological Survey during a program of sampling mine, mill, and smelter products: U.S. Geological Survey Trace Elements Investigations 242, 46 p., https://doi.org/10.3133/tei242.","productDescription":"46 p.","numberOfPages":"47","costCenters":[],"links":[{"id":284051,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei242.jpg"},{"id":285625,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0242/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53558ffce4b0120853e8be90","contributors":{"authors":[{"text":"Hall, Marlene Louise","contributorId":40516,"corporation":false,"usgs":true,"family":"Hall","given":"Marlene","email":"","middleInitial":"Louise","affiliations":[],"preferred":false,"id":283961,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Butler, Arthur Pierce Jr.","contributorId":88826,"corporation":false,"usgs":true,"family":"Butler","given":"Arthur","suffix":"Jr.","email":"","middleInitial":"Pierce","affiliations":[],"preferred":false,"id":283962,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70048313,"text":"tem397 - 1952 - Photogeological map, Stinking Spring Creek-13 Quadrangle, Emery County, Utah","interactions":[],"lastModifiedDate":"2014-02-28T14:46:17","indexId":"tem397","displayToPublicDate":"1952-01-01T09:42:00","publicationYear":"1952","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":"397","title":"Photogeological map, Stinking Spring Creek-13 Quadrangle, Emery County, Utah","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem397","collaboration":"Prepared in cooperation with the Atomic Energy Commission","usgsCitation":"Bates, C., 1952, Photogeological map, Stinking Spring Creek-13 Quadrangle, Emery County, Utah: U.S. Geological Survey Trace Elements Memorandum 397, Report: 3 p.; 1 Plate: 23.33 x 25.45 inches, https://doi.org/10.3133/tem397.","productDescription":"Report: 3 p.; 1 Plate: 23.33 x 25.45 inches","numberOfPages":"3","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":277955,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0397/report-thumb.jpg"},{"id":283118,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0397/plate-1.pdf"},{"id":283117,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0397/report.pdf"}],"country":"United States","state":"Utah","county":"Emery County","otherGeospatial":"Stinking Spring Creek","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.0,38.5 ], [ -111.0,38.625 ], [ -110.875,38.625 ], [ -110.875,38.5 ], [ -111.0,38.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"523d6e66e4b097188d6c76ed","contributors":{"authors":[{"text":"Bates, C.E.","contributorId":48237,"corporation":false,"usgs":true,"family":"Bates","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":484299,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221604,"text":"70221604 - 1952 - Geology of the Iron King Mine, Yavapai county, Arizona","interactions":[],"lastModifiedDate":"2021-06-25T12:17:52.193622","indexId":"70221604","displayToPublicDate":"1952-01-01T07:09:55","publicationYear":"1952","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Geology of the Iron King Mine, Yavapai county, Arizona","docAbstract":"

The Iron King mine is about 2,000 feet west-northwest of the intersection of the 112 15 west meridian and the 34 30 north parallel in the Humboldt region in central Yavapai County, Arizona. The mine is approximately in the geographical center of the Humboldt region. Precambrian rocks form the bedrock. Late Cenozoic unconsolidated river wash and valley fill with some interbedded basalt locally mantle the Precambrian rocks, especially in the north-central part of the region. The Precambrian rocks consist of two metamorphosed volcanic formations and intrusive rocks that range in composition from quartz porphyry to gabbro. The volcanic formations originally were flows, volcanic breccias, and tuffaceous sedimentary rocks. Dynamothermal metamorphism of these rocks formed textures, structures, and mineral assemblages characteristic of low-grade ;riietamorphic rocks, but sufficient relict textures and structures remain to permit delineation of formations on the bases of their original nature. All the Precambrian rocks are foliated, except those in the interior parts of the larger intrusive masses. This foliation has two major trends, (1) north to N 20° W, and (2) N 20° E. The northeast-trending foliation is younger and locally is superimposed on the north- to northwest-trending foliation. The Precambrian rocks strike north to northwest and dip steeply, chiefly westward. Duplication of stratigraphic units and determination of tops suggest two major northeast-trending folds, which probably plunge southward. The northeast-trending foliation appears to bear an axial-plane relationship to these folds. Some masses of igneous rock probably were intruded during development of foliation. The Iron King deposit supports the only active mine in the Humboldt region. It consists of 12 steeply plunging echelon veins arranged along the footwall of a sheared and altered zone in the metamorphosed andesitic tuffaceous sedimentary rocks. Narrow zones of more intense shear probably localized the veins. Solutions first introduced quartz, pyrite, ankerite, and sericite, forming a sporadically mineralized zone (in the hanging wall of the deposit) and probably veins in the Iron King fracture system. Intra-mineralization shear strongly brecciated these early minerals and formed the structures that localized and distributed the ore minerals in the veins. After this deformation, sphalerite, galena, chalcopyrite, tennantite, arsenopyrite, pyrite, quartz, and ankerite were deposited; the last three minerals may have formed through solution and the redeposition of earlier minerals. Formation of sericite either accompanied or followed the deposition of ore-forming minerals. Silver is related closely in distribution to copper and probably is in the tennantite. Gold occurs chiefly in the pyrite. Banding, mimetic after foliation and planes developed by shearing, is pronounced in much of the vein material. Mineral zoning, generally similar in each vein, is a characteristic of the deposit. High-angle reverse faults of about 100 feet in maximum vertical separation offset the veins. These faults are nearly parallel to the veins in strike and dip.

","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.47.1.24","usgsCitation":"Creasey, S., 1952, Geology of the Iron King Mine, Yavapai county, Arizona: Economic Geology, v. 47, no. 1, p. 24-56, https://doi.org/10.2113/gsecongeo.47.1.24.","productDescription":"33 p.","startPage":"24","endPage":"56","costCenters":[],"links":[{"id":386727,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona","county":"Yavapai County","otherGeospatial":"Iron King Mine","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -112.25418090820312,\n 34.49693681996495\n ],\n [\n -112.21572875976561,\n 34.49693681996495\n ],\n [\n -112.21572875976561,\n 34.526358599757465\n ],\n [\n -112.25418090820312,\n 34.526358599757465\n ],\n [\n -112.25418090820312,\n 34.49693681996495\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"47","issue":"1","noUsgsAuthors":false,"publicationDate":"1952-01-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Creasey, S.C.","contributorId":36109,"corporation":false,"usgs":true,"family":"Creasey","given":"S.C.","email":"","affiliations":[],"preferred":false,"id":818257,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}