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,{"id":652,"text":"wsp1238 - 1954 - Surface water supply of the United States, 1952, Part V, Hudson Bay and upper Mississippi River basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:08","indexId":"wsp1238","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1954","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1238","title":"Surface water supply of the United States, 1952, Part V, Hudson Bay and upper Mississippi River basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1238","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1954, Surface water supply of the United States, 1952, Part V, Hudson Bay and upper Mississippi River basins: U.S. Geological Survey Water Supply Paper 1238, xii, 518 p. ;23 cm., https://doi.org/10.3133/wsp1238.","productDescription":"xii, 518 p. ;23 cm.","costCenters":[],"links":[{"id":136042,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1238/report-thumb.jpg"},{"id":25215,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1238/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db69649b","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":527624,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":51704,"text":"ofr54178 - 1954 - Availability of primary or juvenile water for ordinary uses","interactions":[],"lastModifiedDate":"2014-06-18T08:31:50","indexId":"ofr54178","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1954","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"54-178","title":"Availability of primary or juvenile water for ordinary uses","docAbstract":"Progressive depletion of the water supplies of many of the desert valleys of the Southwest, both because of recurrent droughts and because of overdevelopment, has focused increasing attention on the possibilities of developing supplementary water supplies from sources that are immune to drought, or at least whose development will not interfere with an existing supply now being utilized. Among the possibilities that are the subject of research by scientific organizations and other agencies are conversion of sea water and other saline water, salvage of water now used by phreatophytes (water-loving plants) of low economic value, and induced precipitation (rain-making).","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr54178","usgsCitation":"McGuinness, C.L., and Poland, J.F., 1954, Availability of primary or juvenile water for ordinary uses: U.S. Geological Survey Open-File Report 54-178, 5 p., https://doi.org/10.3133/ofr54178.","productDescription":"5 p.","numberOfPages":"5","costCenters":[],"links":[{"id":288726,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":288725,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1954/0178/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d65b","contributors":{"authors":[{"text":"McGuinness, C. L.","contributorId":20313,"corporation":false,"usgs":true,"family":"McGuinness","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":244161,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Poland, J. F.","contributorId":64223,"corporation":false,"usgs":true,"family":"Poland","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":244162,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":329,"text":"wsp1243 - 1954 - Surface water supply of the United States, 1952, Part IX, Colorado River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:12","indexId":"wsp1243","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1954","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1243","title":"Surface water supply of the United States, 1952, Part IX, Colorado River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1243","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1954, Surface water supply of the United States, 1952, Part IX, Colorado River basin: U.S. Geological Survey Water Supply Paper 1243, x, 496 p. :ill., map ;24 cm., https://doi.org/10.3133/wsp1243.","productDescription":"x, 496 p. :ill., map ;24 cm.","costCenters":[],"links":[{"id":137371,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1243/report-thumb.jpg"},{"id":24891,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1243/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696493","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":527311,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16085,"text":"ofr54291 - 1954 - A resistivity survey to locate an aquifer in the glacial deposits near Marshfield, Wisconsin","interactions":[],"lastModifiedDate":"2021-02-22T17:27:25.058846","indexId":"ofr54291","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1954","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"54-291","title":"A resistivity survey to locate an aquifer in the glacial deposits near Marshfield, Wisconsin","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr54291","usgsCitation":"Spicer, H., and Edwards, G.J., 1954, A resistivity survey to locate an aquifer in the glacial deposits near Marshfield, Wisconsin: U.S. Geological Survey Open-File Report 54-291, Report: 74 p.; 3 Figures: 6.70 x 7.18 inches or smaller, https://doi.org/10.3133/ofr54291.","productDescription":"Report: 74 p.; 3 Figures: 6.70 x 7.18 inches or smaller","numberOfPages":"77","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":383427,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1954/0291/figure-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383426,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1954/0291/figure-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383425,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1954/0291/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":149049,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1954/0291/report-thumb.jpg"}],"country":"United States","state":"Wisconsin","city":"Marshfield","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -90.263671875,\n              44.61588908327616\n            ],\n            [\n              -90.076904296875,\n              44.61588908327616\n            ],\n            [\n              -90.076904296875,\n              44.67841867818858\n            ],\n            [\n              -90.263671875,\n              44.67841867818858\n            ],\n            [\n              -90.263671875,\n              44.61588908327616\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8355","contributors":{"authors":[{"text":"Spicer, H. Cecil","contributorId":16000,"corporation":false,"usgs":true,"family":"Spicer","given":"H. Cecil","affiliations":[],"preferred":false,"id":172210,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Edwards, George J.","contributorId":58285,"corporation":false,"usgs":true,"family":"Edwards","given":"George","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":172211,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61891,"text":"gq44 - 1954 - Geology of the Noonan quadrangle, North Dakota","interactions":[],"lastModifiedDate":"2012-02-10T00:10:50","indexId":"gq44","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1954","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"44","title":"Geology of the Noonan quadrangle, North Dakota","language":"ENGLISH","doi":"10.3133/gq44","usgsCitation":"Townsend, R.C., 1954, Geology of the Noonan quadrangle, North Dakota: U.S. Geological Survey Geologic Quadrangle 44, 1 map :col. ;44 x 30 cm. on sheet 76 x 128 cm., folded to 76 x 64 cm., https://doi.org/10.3133/gq44.","productDescription":"1 map :col. ;44 x 30 cm. on sheet 76 x 128 cm., folded to 76 x 64 cm.","costCenters":[],"links":[{"id":102458,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_907.htm","linkFileType":{"id":5,"text":"html"},"description":"907"},{"id":248180,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0044/report.pdf","size":"132","linkFileType":{"id":1,"text":"pdf"}},{"id":252923,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0044/report-thumb.jpg"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.25,48.75 ], [ -103.25,49 ], [ -103,49 ], [ -103,48.75 ], [ -103.25,48.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e8ff","contributors":{"authors":[{"text":"Townsend, Roland C.","contributorId":52668,"corporation":false,"usgs":true,"family":"Townsend","given":"Roland","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":266519,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61886,"text":"gq43 - 1954 - Geology of the Haas quadrangle, Washington","interactions":[],"lastModifiedDate":"2012-02-10T00:10:50","indexId":"gq43","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1954","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"43","title":"Geology of the Haas quadrangle, Washington","language":"ENGLISH","doi":"10.3133/gq43","usgsCitation":"Trimble, D.E., 1954, Geology of the Haas quadrangle, Washington: U.S. Geological Survey Geologic Quadrangle 43, 1 map :col. ;45 x 31 cm. on sheet 76 x 128 cm., folded to 76 x 64 cm., https://doi.org/10.3133/gq43.","productDescription":"1 map :col. ;45 x 31 cm. on sheet 76 x 128 cm., folded to 76 x 64 cm.","costCenters":[],"links":[{"id":102448,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_897.htm","linkFileType":{"id":5,"text":"html"},"description":"897"},{"id":248175,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0043/report.pdf","size":"119","linkFileType":{"id":1,"text":"pdf"}},{"id":252918,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0043/report-thumb.jpg"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.5,46.5 ], [ -118.5,46.75 ], [ -118.25,46.75 ], [ -118.25,46.5 ], [ -118.5,46.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acfe4b07f02db680023","contributors":{"authors":[{"text":"Trimble, Donald E.","contributorId":75910,"corporation":false,"usgs":true,"family":"Trimble","given":"Donald","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":266510,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15659,"text":"ofr54256 - 1954 - Geology of the Eureka pegmatite, Pennington County, South Dakota","interactions":[{"subject":{"id":15659,"text":"ofr54256 - 1954 - Geology of the Eureka pegmatite, Pennington County, South Dakota","indexId":"ofr54256","publicationYear":"1954","noYear":false,"title":"Geology of the Eureka pegmatite, Pennington County, South Dakota"},"predicate":"SUPERSEDED_BY","object":{"id":39087,"text":"pp297E - 1964 - Pegmatites and other Precambrian Rocks in the Southern Black Hills; Geology and mineral deposits of some pegmatites in the southern Black Hills, South Dakota","indexId":"pp297E","publicationYear":"1964","noYear":false,"chapter":"E","title":"Pegmatites and other Precambrian Rocks in the Southern Black Hills; Geology and mineral deposits of some pegmatites in the southern Black Hills, South Dakota"},"id":1}],"supersededBy":{"id":39087,"text":"pp297E - 1964 - Pegmatites and other Precambrian Rocks in the Southern Black Hills; Geology and mineral deposits of some pegmatites in the southern Black Hills, South Dakota","indexId":"pp297E","publicationYear":"1964","noYear":false,"title":"Pegmatites and other Precambrian Rocks in the Southern Black Hills; Geology and mineral deposits of some pegmatites in the southern Black Hills, South Dakota"},"lastModifiedDate":"2025-05-30T15:02:35.96913","indexId":"ofr54256","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1954","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"54-256","title":"Geology of the Eureka pegmatite, Pennington County, South Dakota","docAbstract":"<p>The Eureka Pegmatite, two miles southeast of Keystone, Pennington County, South Dakota, is a small but possibly valuable zoned body containing more than 85,000 tons of coarse-grained granite-pegmatite rock.</p><p>The mica in the pegmatite is probably not of any great importance, but the potash feldspar and beryl may comprise a considerable tonnage of valuable reserves. If the pegmatite can be exploited at a profit in spite of the graphite-damaged feldspar, it may yield substantial amounts of strategically important beryl by open-cut mining of the entire body.</p><p>This report contains complete, megascopic mineralogical and structural details of the pegmatite, which are supplemented with drill core logs and a geologic map and cross-sections.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr54256","usgsCitation":"Roadifer, R.E., 1954, Geology of the Eureka pegmatite, Pennington County, South Dakota: U.S. Geological Survey Open-File Report 54-256, Report: 29 p.; 1 Figure: 37.58 x 30.39 inches, https://doi.org/10.3133/ofr54256.","productDescription":"Report: 29 p.; 1 Figure: 37.58 x 30.39 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,{"id":14611,"text":"ofr54164 - 1954 - Copper and uranium mineralization in the Coyote mining district, Mora County, New Mexico","interactions":[{"subject":{"id":14611,"text":"ofr54164 - 1954 - Copper and uranium mineralization in the Coyote mining district, Mora County, New Mexico","indexId":"ofr54164","publicationYear":"1954","noYear":false,"title":"Copper and uranium mineralization in the Coyote mining district, Mora County, New Mexico"},"predicate":"SUPERSEDED_BY","object":{"id":36059,"text":"b1030L - 1958 - Copper and uranium deposits of the Coyote district, Mora County, New Mexico","indexId":"b1030L","publicationYear":"1958","noYear":false,"chapter":"L","title":"Copper and uranium deposits of the Coyote district, Mora County, New Mexico"},"id":1}],"supersededBy":{"id":36059,"text":"b1030L - 1958 - Copper and uranium deposits of the Coyote district, Mora County, New Mexico","indexId":"b1030L","publicationYear":"1958","noYear":false,"title":"Copper and uranium deposits of the Coyote district, Mora County, New Mexico"},"lastModifiedDate":"2026-01-06T15:19:15.441956","indexId":"ofr54164","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1954","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"54-164","title":"Copper and uranium mineralization in the Coyote mining district, Mora County, New Mexico","docAbstract":"<p>Sedimentary copper-uranium deposits lie along the eastern flank of the Sangre de Cristo Range in the Coyote mining district, Mora County, New ilexico. The oldest rocks in the district are pre-Cambrian granites, pegmatites and metasediments. These are unconformably overlain by marine limestones and shales of Pennsylvanian age and fluviatile sediments of Pennsylvanian-Permian age. Tertiary basalt flows are extensive to the east and cover Pennsylvanian and Permian rocks locally.</p><p>The copper-uranium mineralization occurred in a belt of thrusting and transverse faulting associated with the uplift of the Ancestral Rockies, but there is no visible evidence to relate the ore deposits to faults. The uranium deposition seems to have been controlled by channels containing carbonized plant remains in the coarser sandstone lenses of the Sangre de Cristo formation.</p><p>There are two major types of ore deposits in the Coyote district. One consists of copper-replaced pyrite nodules and plant remains in black carbonaceous shales, the other consists of uranium in cross bedded sandstones. Copper is most abundant in the lower 1500 feet of the Sangre de Cristo formation.</p><p>The most important copper mineral is chalcocite with minor amounts of chalcopyrite, bornite, covellite, pyrite, malachite, and azurite. The uranium minerals are metatyuyamunite and an undetermined black radioactive mineral associated with chalcopyrite.</p><p>The uranium occurs in stream channels approximately 2000 feet stratigraphically above the top of the Aagdalena group (as mapped).</p><p>The copper-uranium was probably derived from nearby pre-Cambrian highlands which contain abundant copper mines, granitic intrusions, and uranium bearing pegmatites. Heteoric waters containing copper sulfate and a soluble uranium compound transported the minerals to their present site and upon encountering carbonaceous material were precipitated out.</p><p><br data-mce-bogus=\"1\"></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr54164","usgsCitation":"Laub, D.C., 1954, Copper and uranium mineralization in the Coyote mining district, Mora County, New Mexico: U.S. Geological Survey Open-File Report 54-164, 24 p., https://doi.org/10.3133/ofr54164.","productDescription":"24 p.","costCenters":[],"links":[{"id":148114,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1954/0164/report-thumb.jpg"},{"id":498349,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1954/0164/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Mexico","county":"Mora 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,{"id":70048102,"text":"tei340 - 1954 - Localization of uranium minerals in channel sediments at the base of the Shinarump conglomerate, Monument Valley, Arizona","interactions":[],"lastModifiedDate":"2014-04-07T13:27:07","indexId":"tei340","displayToPublicDate":"1990-01-24T13:10:00","publicationYear":"1954","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":"340","title":"Localization of uranium minerals in channel sediments at the base of the Shinarump conglomerate, Monument Valley, Arizona","docAbstract":"During the summers of 1951 and 1952 the U.S. Geological Survey mapped the geology and uranium deposits in three 15-minute quadrangles on the Navajo\nIndian Reservation in Apache and Navajo Counties, northeastern Arizona. Exposed sedimentary rocks range in age from the Halgaito tongue of the Cutler\nformation (Permian) to the Salt Wash member of the Morrison formation (Jurassic), The dominant structural element of the area is the Monument upwarp, a arge asymmetrical anticline whose northern end is near the junction of the Green and Colorado Rivers in Utah, and whose southern end disappears near Kayenta, Ariz. Asymmetrical anticlines with steeply dipping east flanks and gently dipping west flanks are superimposed on the upwarp. These subsidiary structures trend north. The uranium ore bodies are localized in conglomeratic sandstone of the Upper Triassic Shinarump conglomerate that fills channels scoured in the underlying Lower and Middle (?) Triassic Moenkopi formation. These channels range from relatively narrow and shallow ones 15 feet wide and 10 feet deep to much broader and deeper ones 2,300 feet wide and 70 feet deep. Two types of channels can be distinguished-r-a short-type less than 2 miles Iong 5 and a long-type traceable for distances greater than 2 miles Plant matter in the form of trees, branches,'and twigs was deposited with Shinarump sediments in the channels. It is suggested that when the Shinarump conglomerate was invaded by mineralizing solutions the uranium ore was deposited primarily in localities formerly occupied by the plant material. Further, it is suggested that the short channels are more likely to have ore accumulations than long channels.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei340","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Witkind, I.J., 1954, Localization of uranium minerals in channel sediments at the base of the Shinarump conglomerate, Monument Valley, Arizona: U.S. Geological Survey Trace Elements Investigations 340, Report: 43 p.; 2 Plates: 29.10 x 17.55 inches and 22.02 x 19.71 inches, https://doi.org/10.3133/tei340.","productDescription":"Report: 43 p.; 2 Plates: 29.10 x 17.55 inches and 22.02 x 19.71 inches","numberOfPages":"43","costCenters":[],"links":[{"id":277456,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/340/report-thumb.jpg"},{"id":285789,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0340/figure-5.pdf"},{"id":285790,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0340/figure-8.pdf"},{"id":285791,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0340/report.pdf"}],"country":"United States","state":"Arizona","county":"Apache County","otherGeospatial":"Monument Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.489502,36.658505 ], [ -110.489502,37.262031 ], [ -109.677887,37.262031 ], [ -109.677887,36.658505 ], [ -110.489502,36.658505 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52303f64e4b04b8e63a20647","contributors":{"authors":[{"text":"Witkind, I. J.","contributorId":54221,"corporation":false,"usgs":true,"family":"Witkind","given":"I.","middleInitial":"J.","affiliations":[],"preferred":false,"id":483747,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70048214,"text":"tei353 - 1954 - Thorium and rare earth minerals in the Powderhorn district, Gunnison County, Colorado","interactions":[],"lastModifiedDate":"2014-06-19T06:31:20","indexId":"tei353","displayToPublicDate":"1990-01-09T10:20:00","publicationYear":"1954","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":"353","title":"Thorium and rare earth minerals in the Powderhorn district, Gunnison County, Colorado","docAbstract":"<p>Thorium has been found since 1949 in at least 33 deposits in an area 6 miles wide and 20 miles long in the Powderhorn district, Gunnison County, Colo. The district is composed largely of pre-Jurassic metamorphic and igneous rocks, which are chiefly if not entirely pre-Cambrian in age. The metamorphic and igneous rocks are overlain by sandstone of the Morrison formation of Jurassic age, and by volcanic rocks of the Alboroto group and Hinsdale formation of Miocene and Pliocene (?) age, respectively.</p>\n<br>\n<p>The thorium deposits occur in or near alkalic igneous rocks in which such elements as titanium, rare earths, barium, strontium, and niobium occur in greater-than-average amounts. The greatest mass of the alkalic igneous rocks the Iron Hill composite stoc,- occupies an area of 12 square miles in the southeastern part of the district. The age of the thorium deposits, like that of the alkalic igneous rocks, is not known other than pre-Jurassic.</p> \n<br>\n<p>The thorium veins and mineralized shear zones range from a few inches to 18 feet in thickness and from a few feet to 3,500 feet in length. The veins are composed of calcite,.dolomite, siderite, ankerite, quartz, barite, pyrite, sphalerite, galena, goethite,. apatite, alkali feldspar, and many other minerals. The thorium occurs at least partly in thorite or hydrothorite. Sparse xenotime has been tentatively identified in one deposit. Several minerals containing rare earths of the cerium group as major constituents are found in carbonate veins near Iron Hill. Bastnaesite has been identified by X-ray methods, and cerite and synchisite are probably present also.The fluorapatite in some veins and in parts of the carbonate rock mass that occupies 2 square miles in the central part of the Iron Hill complex contains rare earths of the cerium group, generally in amounts of a fraction of a percent of the rock.</p> \n<br>\n<p>The radioactivity of the deposits appears to be due almost entirely to thorium and its daughter products The ThO<sub>2</sub> content of selected highgrade samples from the Little Johnnie vein is as much as 4 percent. The ThO<sub>2</sub> content of the veins is generally less than 1 percent, however, and is only 0.05 to 0.1 percent in many of the veins studied.</p> \n<br>\n<p>The little Johnnie vein, which was mapped in detail, can be traced discontinuously for a distance of more than 3,500 feet. The thoriumbearing material occurs as irregular veinlets and thin films introduced into the fault zone. The mineralized shear zone ranges from less than 6 inches to 5 feet in thickness. Near its west end the vein is broken by many faults in a zone that marks the edge of a roughly circular fault block, 1<sub>1/2.</sub>miles in diameter, that has dropped 1,000 feet or more since the deposition of Miocene volcanic-rocks that now floor the Milkranch basin.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei353","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Olson, J.C., and Wallace, S., 1954, Thorium and rare earth minerals in the Powderhorn district, Gunnison County, Colorado: U.S. Geological Survey Trace Elements Investigations 353, Report: 58 p.; 2 Plates: 20.93 x 11.91 inches and 9.29 x 11.96 inches, https://doi.org/10.3133/tei353.","productDescription":"Report: 58 p.; 2 Plates: 20.93 x 11.91 inches and 9.29 x 11.96 inches","numberOfPages":"58","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":288854,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":288851,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0353/figure-2.pdf"},{"id":288852,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0353/figure-3.pdf"},{"id":288853,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0353/report.pdf"}],"country":"United States","state":"Colorado","county":"Gunnison County","otherGeospatial":"Powderhorn District","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.0603,36.9924 ], [ -109.0603,41.0024 ], [ -102.0416,41.0024 ], [ -102.0416,36.9924 ], [ -109.0603,36.9924 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"523979fde4b04b9308ae4fbc","contributors":{"authors":[{"text":"Olson, Jerry C.","contributorId":89202,"corporation":false,"usgs":true,"family":"Olson","given":"Jerry","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":484022,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wallace, Stewart R.","contributorId":53371,"corporation":false,"usgs":true,"family":"Wallace","given":"Stewart R.","affiliations":[],"preferred":false,"id":484021,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70173589,"text":"70173589 - 1954 - The quality and character of Pacific Northwest waters","interactions":[],"lastModifiedDate":"2016-06-21T14:05:03","indexId":"70173589","displayToPublicDate":"1959-12-31T00:00:00","publicationYear":"1954","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"The quality and character of Pacific Northwest waters","docAbstract":"<p>This paper is a general discussion of the quality and chemical character of surface and ground waters in the Pacific Northwest as shown by the available data. Previous quality of water studies reported in the literature are reviewed. The composition of natural waters is considered as to the source and significance of the different mineral constituents. Analytical data are presented showing mineral constituents and physical properties of selected surface and ground waters in the region.</p>","conferenceTitle":"Pacific Northwest Metals and Minerals Conference, American Mining and Metallurgical Engineers","conferenceDate":"April 30, 1954","conferenceLocation":"Portland, OR","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70173589","usgsCitation":"Swenson, H.A., 1954, The quality and character of Pacific Northwest waters: Open-File Report, 9 p., https://doi.org/10.3133/70173589.","productDescription":"9 p.","numberOfPages":"18","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":323087,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70173589.jpg"},{"id":324137,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70173589/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5757f064e4b04f417c24dd28","contributors":{"authors":[{"text":"Swenson, Herbert A.","contributorId":93461,"corporation":false,"usgs":true,"family":"Swenson","given":"Herbert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":637377,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71522,"text":"tei496 - 1954 - Germanium and uranium in coalified wood from Upper Devonian black shale","interactions":[],"lastModifiedDate":"2014-05-27T14:34:26","indexId":"tei496","displayToPublicDate":"1955-01-01T14:39:00","publicationYear":"1954","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":"496","title":"Germanium and uranium in coalified wood from Upper Devonian black shale","docAbstract":"<p>Microscopic study of black, vitreous, carbonaceous material occurring in the Chattanooga shale in Tennessee and in the Cleveland member of the Ohio shale in Ohio has revealed coalified woody plant tissue. Some samples have shown sufficient detail to be identified with the genus Callixylon. Similar material has been reported in the literature as \"bituminous\" or \"asphaltic\" stringers.</p>\n<br/>\n<p>Spectrographic analyses of the ash from the coalified wood have shown unusually high percentages of germanium, uranium, vanadium, and nickel. The inverse relationship between uranium and germanium in the ash and the ash content of various samples shows an association of these elements with the organic constituents of the coal.</p>\n<br/>\n<p>On the basis of geochemical considerations, it seems most probable that the wood or coalified wood was germanium-bearing at the time logs or woody fragments were floated into the basins of deposition of the Chattanooga shale and the Cleveland member of the Ohio shale. Once within the marine environment, the material probably absorbed uranium with the formation of organo-uranium compounds such as have been found to exist in coals.</p>\n<br/>\n<p>It is suggested that a more systematic search for germaniferous coals in the vicinity of the Chattanooga shale and the Cleveland member of the Ohio shale might be rewarding.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/tei496","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Breger, I., and Schopf, J., 1954, Germanium and uranium in coalified wood from Upper Devonian black shale: U.S. Geological Survey Trace Elements Investigations 496, 13 p., https://doi.org/10.3133/tei496.","productDescription":"13 p.","costCenters":[],"links":[{"id":284572,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0496/report.pdf"},{"id":284573,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/0496/report-thumb.jpg"}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5355946fe4b0120853e8bfdc","contributors":{"authors":[{"text":"Breger, Irving A.","contributorId":41901,"corporation":false,"usgs":true,"family":"Breger","given":"Irving A.","affiliations":[],"preferred":false,"id":284318,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schopf, James M.","contributorId":94297,"corporation":false,"usgs":true,"family":"Schopf","given":"James M.","affiliations":[],"preferred":false,"id":284319,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70111703,"text":"tei229 - 1954 - Radioactive deposits in California","interactions":[],"lastModifiedDate":"2014-06-19T06:25:32","indexId":"tei229","displayToPublicDate":"1955-01-01T12:50:00","publicationYear":"1954","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":"229","title":"Radioactive deposits in California","docAbstract":"<p>Reconnaissance examination by Government geologists of many areas, mine properties, and prospects in California during the period between 1948 and 1953 has confirmed the presence of radioactive materials in place at more than 40 localities. Abnormal radioactivity at these localities is due to concentrations of primary and secondary uranium minerals, to radon gas, radium (?), and to thorium minerals. Of the known occurrences only three were thought to contain uranium oxide (uranitite or pitchblende), 4 contained uranium-bearing columbate, tantalate, or titanate minerals, 12 contained secondary uranium minerals, such as autunite, carnotite, and torbernite, one contained radon gas, 7 contained thorium minerals, and, at the remaining 16 localities, the source of the anomalous radiation was not positively determined.</p>\n<br/>\n<p>The occurrences in which uranium oxide has been tentatively identified include the Rathgeb mine (Calaveras County), the Yerih group of claims (San Bernardino County), and the Rainbow claim (Madera County). Occurrences of secondary uranium minerals are largely confined to the arid desert regions of south-eastern California including deposits in San Bernardino, Kern, Inyo, and Imperial Counties. Uranium-bearing columbate, tantalate, or titanate minerals have been reported from pegmatite and granitic rock in southeastern and eastern California.</p>\n<br/>\n<p>Thorium minerals have been found in vein deposits in eastern San Bernardino County and from pegmatites and granitic rocks in various parts of southeastern California; placer concentrations of thorium minerals are known from nearly all areas in the State that are underlain, in part, by plutonic crystalline rocks.</p>\n<br/>\n<p>The primary uranium minerals occur principally as minute accessory crystals in pegmatite or granitic rock, or with base-metal sulfide minerals in veins. Thorium minerals also occur as accessory crystals in pegmatite or granitic rock, in placer deposits derived from such rock, and, at Mountain Pass, in veins containing rare earths. Secondary uranium minerals have been found as fracture coatings and as disseminations in various types of wall rock, although they are largely confined to areas of Tertiary volcanic rocks. Probably the uranium in the uraniferous deposits in California is related genetically to felsic crystalline rocks and felsic volcanic rocks; the present distribution of the secondary uranium minerals has been controlled, in part, by circulating ground waters and probably, in part, by magmatic waters related to the Tertiary volcanic activity. The thorium minerals are genetically related to the intrusion of pegmatite and plutonic crystalline rocks.</p>\n<br/>\n<p>None of the known deposits of radioactive minerals in California contain marketable reserves of uranium or thorium ore under economic conditions existing in 1952. With a favorable local market small lots of uranium ore may be available in the following places: the Rosamund prospect, the Rafferty and Chilson properties, the Lucky Star claim, and the Yerih group. The commercial production of thorium minerals will be possible, in the near future, only if these minerals can be recovered cheaply as a byproduct either from the mining of rare earths minerals at Mountain Pass or as a byproduct of placer mining for gold.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei229","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission.","usgsCitation":"Walker, G.W., and Lovering, T., 1954, Radioactive deposits in California: U.S. Geological Survey Trace Elements Investigations 229, Report: 69 p.; Plate: 15.74 x 19.77 inches, https://doi.org/10.3133/tei229.","productDescription":"Report: 69 p.; Plate: 15.74 x 19.77 inches","numberOfPages":"78","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":288850,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":288848,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0229/plate-1.pdf"},{"id":288849,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0229/report.pdf"}],"country":"United States","state":"California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.41,32.53 ], [ -124.41,42.01 ], [ -114.13,42.01 ], [ -114.13,32.53 ], [ -124.41,32.53 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ae77fde4b0abf75cf2c688","contributors":{"authors":[{"text":"Walker, George W.","contributorId":101308,"corporation":false,"usgs":true,"family":"Walker","given":"George","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":494447,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lovering, Tom G.","contributorId":31679,"corporation":false,"usgs":true,"family":"Lovering","given":"Tom G.","affiliations":[],"preferred":false,"id":494446,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70207417,"text":"70207417 - 1954 - Geology of the iron deposits of the Congonhas District, Minas Gerais, Brazil","interactions":[],"lastModifiedDate":"2019-12-19T08:57:08","indexId":"70207417","displayToPublicDate":"1954-12-31T08:53:29","publicationYear":"1954","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Geology of the iron deposits of the Congonhas District, Minas Gerais, Brazil","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","doi":"10.1126/science.119.3096.616","issn":"00368075","usgsCitation":"Guild, P.W., 1954, Geology of the iron deposits of the Congonhas District, Minas Gerais, Brazil: Science, v. 119, no. 3096, p. 616-616, https://doi.org/10.1126/science.119.3096.616.","productDescription":"1 p. ","startPage":"616","endPage":"616","costCenters":[],"links":[{"id":370458,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Brazil","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-57.62513,-30.21629],[-56.2909,-28.85276],[-55.16229,-27.88192],[-54.49073,-27.47476],[-53.64874,-26.92347],[-53.62835,-26.12487],[-54.13005,-25.54764],[-54.62529,-25.73926],[-54.42895,-25.16218],[-54.29348,-24.5708],[-54.29296,-24.02101],[-54.65283,-23.83958],[-55.0279,-24.00127],[-55.40075,-23.95694],[-55.51764,-23.572],[-55.61068,-22.65562],[-55.79796,-22.35693],[-56.47332,-22.0863],[-56.88151,-22.28215],[-57.93716,-22.09018],[-57.87067,-20.73269],[-58.16639,-20.1767],[-57.8538,-19.97],[-57.95,-19.4],[-57.67601,-18.96184],[-57.49837,-18.17419],[-57.73456,-17.55247],[-58.2808,-17.27171],[-58.38806,-16.87711],[-58.24122,-16.29957],[-60.15839,-16.25828],[-60.54297,-15.09391],[-60.25115,-15.07722],[-60.26433,-14.64598],[-60.4592,-14.35401],[-60.5033,-13.77595],[-61.08412,-13.47938],[-61.7132,-13.4892],[-62.12708,-13.19878],[-62.80306,-13.00065],[-63.1965,-12.62703],[-64.31635,-12.46198],[-65.40228,-11.56627],[-65.3219,-10.89587],[-65.44484,-10.51145],[-65.33844,-9.76199],[-66.64691,-9.93133],[-67.1738,-10.30681],[-68.04819,-10.71206],[-68.27125,-11.01452],[-68.78616,-11.03638],[-69.52968,-10.95173],[-70.09375,-11.12397],[-70.54869,-11.00915],[-70.48189,-9.49012],[-71.30241,-10.07944],[-72.18489,-10.0536],[-72.56303,-9.52019],[-73.22671,-9.46221],[-73.01538,-9.03283],[-73.57106,-8.42445],[-73.98724,-7.52383],[-73.7234,-7.341],[-73.72449,-6.9186],[-73.12003,-6.62993],[-73.21971,-6.08919],[-72.96451,-5.74125],[-72.89193,-5.27456],[-71.74841,-4.59398],[-70.92884,-4.40159],[-70.79477,-4.25126],[-69.89364,-4.29819],[-69.4441,-1.55629],[-69.42049,-1.12262],[-69.57707,-0.54999],[-70.02066,-0.18516],[-70.01557,0.54141],[-69.4524,0.70616],[-69.25243,0.60265],[-69.21864,0.98568],[-69.8046,1.08908],[-69.81697,1.71481],[-67.86857,1.69246],[-67.53781,2.03716],[-67.26,1.72],[-67.06505,1.13011],[-66.87633,1.25336],[-66.32577,0.72445],[-65.54827,0.78925],[-65.35471,1.09528],[-64.61101,1.32873],[-64.19931,1.49285],[-64.08309,1.91637],[-63.36879,2.2009],[-63.42287,2.41107],[-64.27,2.49701],[-64.40883,3.12679],[-64.36849,3.79721],[-64.81606,4.05645],[-64.62866,4.14848],[-63.88834,4.02053],[-63.0932,3.77057],[-62.80453,4.00697],[-62.08543,4.16212],[-60.96689,4.53647],[-60.60118,4.9181],[-60.73357,5.20028],[-60.21368,5.24449],[-59.98096,5.01406],[-60.111,4.57497],[-59.76741,4.4235],[-59.53804,3.9588],[-59.81541,3.6065],[-59.97452,2.75523],[-59.71855,2.24963],[-59.64604,1.78689],[-59.03086,1.3177],[-58.54001,1.26809],[-58.42948,1.46394],[-58.11345,1.5072],[-57.66097,1.68258],[-57.33582,1.94854],[-56.7827,1.86371],[-56.53939,1.89952],[-55.9957,1.81767],[-55.9056,2.022],[-56.07334,2.22079],[-55.97332,2.51036],[-55.56976,2.42151],[-55.09759,2.52375],[-54.52475,2.31185],[-54.08806,2.10556],[-53.77852,2.3767],[-53.55484,2.3349],[-53.41847,2.05339],[-52.93966,2.12486],[-52.55642,2.50471],[-52.24934,3.24109],[-51.6578,4.15623],[-51.31715,4.20349],[-51.06977,3.6504],[-50.50888,1.90156],[-49.97408,1.73648],[-49.9471,1.04619],[-50.69925,0.22298],[-50.38821,-0.07844],[-48.62057,-0.23549],[-48.5845,-1.23781],[-47.82496,-0.58162],[-46.56658,-0.94103],[-44.9057,-1.55174],[-44.41762,-2.13775],[-44.58159,-2.69131],[-43.41879,-2.38311],[-41.47266,-2.91202],[-39.97867,-2.87305],[-38.50038,-3.70065],[-37.22325,-4.82095],[-36.45294,-5.1094],[-35.5978,-5.1495],[-35.23539,-5.46494],[-34.89603,-6.73819],[-34.72999,-7.34322],[-35.12821,-8.9964],[-35.63697,-9.64928],[-37.04652,-11.04072],[-37.68361,-12.17119],[-38.42388,-13.03812],[-38.67389,-13.05765],[-38.95328,-13.79337],[-38.8823,-15.66705],[-39.16109,-17.20841],[-39.26734,-17.86775],[-39.58352,-18.2623],[-39.76082,-19.59911],[-40.77474,-20.90451],[-40.94476,-21.93732],[-41.75416,-22.37068],[-41.98828,-22.97007],[-43.0747,-22.96769],[-44.64781,-23.35196],[-45.35214,-23.79684],[-46.47209,-24.08897],[-47.64897,-24.8852],[-48.49546,-25.87702],[-48.641,-26.6237],[-48.47474,-27.17591],[-48.66152,-28.18613],[-48.88846,-28.67412],[-49.58733,-29.22447],[-50.69687,-30.98447],[-51.57623,-31.7777],[-52.25608,-32.24537],[-52.7121,-33.19658],[-53.37366,-33.76838],[-53.65054,-33.202],[-53.20959,-32.72767],[-53.78795,-32.04724],[-54.57245,-31.49451],[-55.60151,-30.85388],[-55.97324,-30.88308],[-56.97603,-30.10969],[-57.62513,-30.21629]]]},\"properties\":{\"name\":\"Brazil\"}}]}","volume":"119","issue":"3096","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Guild, P. W.","contributorId":39039,"corporation":false,"usgs":true,"family":"Guild","given":"P.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":777934,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70197719,"text":"70197719 - 1954 - Tungsten in southeastern California: Chapter 8","interactions":[],"lastModifiedDate":"2023-06-07T18:27:54.517069","indexId":"70197719","displayToPublicDate":"1954-12-31T00:00:00","publicationYear":"1954","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5710,"text":"California Division of Mines and Geology Bulletin","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"170","title":"Tungsten in southeastern California: Chapter 8","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geology of southern California","language":"English","publisher":"California Division of Mines","usgsCitation":"Bateman, P.C., and Irwin, W., 1954, Tungsten in southeastern California: Chapter 8: California Division of Mines and Geology Bulletin 170, 10 p.","productDescription":"10 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