During the night of March 1 and 2, 1951, an inconspicuous group of hot springs and small mud volcanoes in northeastern California burst into spectacular eruption, unequalled by other known mud volcanoes. The eruption cloud of steam, gases, and mud particles rose several thousand feet in the air and distributed fine debris to the southeast for a distance of at least 4 miles. More than 20 acres of the hot-spring area was intensely disturbed and greatly modified by the eruption, estimated to involve at least 6 million cubic feet or 300,000 tons of mud. Several days after the eruption, the area was barely active. The eruption appears to be unique in the history of the springs.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1955)66[1109:VMEOLC]2.0.CO;2","usgsCitation":"White, D.E., 1955, Violent mud-volcano eruption of lake city hot springs, northeastern California: GSA Bulletin, v. 66, no. 9, p. 1109-1130, https://doi.org/10.1130/0016-7606(1955)66[1109:VMEOLC]2.0.CO;2.","productDescription":"22 p.","startPage":"1109","endPage":"1130","costCenters":[],"links":[{"id":385607,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","county":"Modoc County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-120.0003,41.9953],[-119.9998,41.9502],[-119.9996,41.9302],[-119.9998,41.9076],[-119.9998,41.9011],[-119.9996,41.8049],[-119.9986,41.7131],[-119.9984,41.6905],[-119.9984,41.6564],[-119.9986,41.3683],[-119.9986,41.2811],[-119.9994,41.2389],[-119.9994,41.1982],[-119.9995,41.1845],[-120.0498,41.1847],[-120.0986,41.1845],[-120.1169,41.1844],[-120.3794,41.1865],[-120.4069,41.1863],[-120.4551,41.1864],[-120.4576,41.1864],[-120.4704,41.1858],[-120.5155,41.1859],[-120.5339,41.1862],[-120.5528,41.1861],[-120.5723,41.1859],[-120.7225,41.1859],[-120.8965,41.1864],[-120.9557,41.1862],[-121.1638,41.185],[-121.1986,41.1846],[-121.2261,41.1847],[-121.2304,41.1851],[-121.3323,41.1841],[-121.3457,41.1844],[-121.3695,41.1845],[-121.4074,41.1844],[-121.4459,41.1847],[-121.4457,41.2246],[-121.4462,41.2401],[-121.4464,41.2723],[-121.4473,41.2827],[-121.4469,41.3562],[-121.446,41.4107],[-121.4481,41.4661],[-121.4495,41.5605],[-121.4495,41.6041],[-121.4492,41.6386],[-121.4494,41.6908],[-121.4485,41.7008],[-121.4493,41.7757],[-121.458,41.7756],[-121.4571,41.7879],[-121.4572,41.8124],[-121.4572,41.8355],[-121.4575,41.8483],[-121.4574,41.8637],[-121.4577,41.8982],[-121.4579,41.9282],[-121.4579,41.9504],[-121.4468,41.9506],[-121.4469,41.9981],[-121.34,41.9981],[-121.3322,41.9981],[-121.3295,41.9981],[-121.3125,41.998],[-121.3098,41.998],[-121.2921,41.9979],[-121.2418,41.9976],[-121.2246,41.9975],[-121.2149,41.9975],[-121.1074,41.9975],[-121.106,41.9975],[-121.0015,41.9933],[-120.9821,41.9934],[-120.9518,41.9936],[-120.8827,41.9939],[-120.5906,41.9944],[-120.5316,41.9944],[-120.489,41.9944],[-120.4301,41.9944],[-120.2951,41.9947],[-120.2788,41.9947],[-120.2719,41.9948],[-120.1908,41.9952],[-120.095,41.9952],[-120.0855,41.9952],[-120.0753,41.9952],[-120.0345,41.9955],[-120.0262,41.9955],[-120.0003,41.9953]]]},\"properties\":{\"name\":\"Modoc\",\"state\":\"CA\"}}]}","volume":"66","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"White, Donald E.","contributorId":76787,"corporation":false,"usgs":true,"family":"White","given":"Donald","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":815535,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010695,"text":"70010695 - 1955 - Radiocarbon dates of pre-Mankato events in eastern and central North America","interactions":[],"lastModifiedDate":"2026-03-02T22:21:32.384723","indexId":"70010695","displayToPublicDate":"1955-05-06T00:00:00","publicationYear":"1955","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Radiocarbon dates of pre-Mankato events in eastern and central North America","docAbstract":"Hepatozoon sciuri (Coles, 1914) is reported from gray squirrels (Sciurus carolinensis) in Washington, D.C. and Maryland. Blood smears stained with Giemsa's stain revealed a parasitemia in 16 to 71% of the squirrels examined. A technique for laking the red cells and concentrating the white cells in blood samples demonstrated this protozoon to be present in every squirrel so tested.
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\"}}]}","volume":"2","issue":"2","noUsgsAuthors":false,"publicationDate":"2007-04-29","publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4404","contributors":{"authors":[{"text":"Herman, C. M.","contributorId":101335,"corporation":false,"usgs":true,"family":"Herman","given":"C.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":332065,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Price, D.L.","contributorId":94399,"corporation":false,"usgs":true,"family":"Price","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":332064,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70220708,"text":"70220708 - 1955 - A gold-scheelite-cinnabar placer in Humboldt County, Nevada","interactions":[],"lastModifiedDate":"2021-05-25T13:40:04.875752","indexId":"70220708","displayToPublicDate":"1955-05-04T08:36:43","publicationYear":"1955","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":"A gold-scheelite-cinnabar placer in Humboldt County, Nevada","docAbstract":"Gold, scheelite, and cinnabar in amounts that might be profitably extracted are found in a placer deposit in the Dutch Flat mining district in north-central Nevada. These materials are the products of at least two and possibly three stages of metallogenic activity recorded in the district. The gold and perhaps most of the scheelite were derived from quartz veins that cut a small granodiorite stock and lower Paleozoic sedimentary rocks. Part of the scheelite may have been derived from contact-metamorphic deposits associated with the granodiorite stock. The cinnabar came from a shear zone that is later than the quartz veins. The proximity of the placer to the source of the minerals is the factor that made a significant concentration of these minerals possible. Incomplete sampling of the placer indicates an average value of $1.50 per cubic yard in combined gold, tungsten, and mercury based on the price of these metals in August 1954.
No abstract available.
","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.121.3147.608.b","issn":"00368075","usgsCitation":"Stieff, L.R., Stern, T.W., and Sherwood, A., 1955, Preliminary description of coffinite - A new uranium mineral: Science, v. 121, no. 3147, p. 608-609, https://doi.org/10.1126/science.121.3147.608.b.","productDescription":"2 p.","startPage":"608","endPage":"609","costCenters":[],"links":[{"id":219710,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","county":"Mesa County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -109.03979652261282,\n 39.4009020577397\n ],\n [\n -109.06817478344583,\n 38.57628945404758\n ],\n [\n -108.07921504280233,\n 38.56514000092463\n ],\n [\n -108.08726736436759,\n 38.78808362764579\n ],\n [\n -108.02363285929954,\n 38.9774973165676\n ],\n [\n -107.75313405058641,\n 39.14435356970067\n ],\n [\n -107.61347198626564,\n 39.40090163943319\n ],\n [\n -109.03979652261282,\n 39.4009020577397\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"121","issue":"3147","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a838ce4b0c8380cd7c003","contributors":{"authors":[{"text":"Stieff, L. R.","contributorId":25619,"corporation":false,"usgs":true,"family":"Stieff","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":359632,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stern, T. W.","contributorId":36122,"corporation":false,"usgs":true,"family":"Stern","given":"T.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":359634,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sherwood, A.M.","contributorId":25987,"corporation":false,"usgs":true,"family":"Sherwood","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":359633,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70209157,"text":"70209157 - 1955 - Outbreak of aspergillosis in mallards","interactions":[],"lastModifiedDate":"2020-03-19T14:14:01","indexId":"70209157","displayToPublicDate":"1955-04-15T14:09:55","publicationYear":"1955","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Outbreak of aspergillosis in mallards","docAbstract":"No abstract available.
","language":"English","publisher":"Wildlife Society","doi":"10.2307/3797408","usgsCitation":"Neff, J.A., 1955, Outbreak of aspergillosis in mallards: Journal of Wildlife Management, v. 19, no. 3, p. 415-416, https://doi.org/10.2307/3797408.","productDescription":"2 p.","startPage":"415","endPage":"416","costCenters":[],"links":[{"id":488886,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2307/3797408","text":"Publisher Index Page"},{"id":373381,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","city":"Boulder","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -105.23065567016602,\n 39.985406886592884\n ],\n [\n -105.17555236816406,\n 39.985406886592884\n ],\n [\n -105.17555236816406,\n 40.04956256234405\n ],\n [\n -105.23065567016602,\n 40.04956256234405\n ],\n [\n -105.23065567016602,\n 39.985406886592884\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"19","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Neff, Johnson A.","contributorId":51156,"corporation":false,"usgs":true,"family":"Neff","given":"Johnson","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":785159,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010778,"text":"70010778 - 1955 - That and which again","interactions":[],"lastModifiedDate":"2026-03-02T22:42:39.011695","indexId":"70010778","displayToPublicDate":"1955-04-15T00:00:00","publicationYear":"1955","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"That and which again","docAbstract":"No abstract available.
","language":"English","publisher":"American Association for the Advancement of Scienc","doi":"10.1126/science.121.3146.567.b","issn":"00368075","usgsCitation":"Calkins, F.C., 1955, That and which again: Science, v. 121, no. 3146, p. 567-568, https://doi.org/10.1126/science.121.3146.567.b.","productDescription":"2 p.","startPage":"567","endPage":"568","costCenters":[],"links":[{"id":218731,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"121","issue":"3146","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba60ae4b08c986b320e50","contributors":{"authors":[{"text":"Calkins, F. C.","contributorId":55402,"corporation":false,"usgs":true,"family":"Calkins","given":"F.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":359626,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010668,"text":"70010668 - 1955 - U.S. Geological Survey radiocarbon dates II","interactions":[],"lastModifiedDate":"2026-03-02T22:48:46.593584","indexId":"70010668","displayToPublicDate":"1955-04-08T00:00:00","publicationYear":"1955","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"U.S. Geological Survey radiocarbon dates II","docAbstract":"No abstract available.
","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.121.3145.481","issn":"00368075","usgsCitation":"Rubin, M., and Suess, H.E., 1955, U.S. Geological Survey radiocarbon dates II: Science, v. 121, no. 3145, p. 481-488, https://doi.org/10.1126/science.121.3145.481.","productDescription":"8 p.","startPage":"481","endPage":"488","costCenters":[],"links":[{"id":219394,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"121","issue":"3145","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbb0be4b08c986b328484","contributors":{"authors":[{"text":"Rubin, M.","contributorId":88079,"corporation":false,"usgs":true,"family":"Rubin","given":"M.","email":"","affiliations":[],"preferred":false,"id":359393,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Suess, H. E.","contributorId":69292,"corporation":false,"usgs":false,"family":"Suess","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":359392,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010986,"text":"70010986 - 1955 - Isolation of organic carbon from bones for C14 dating","interactions":[],"lastModifiedDate":"2026-03-03T15:23:23.983276","indexId":"70010986","displayToPublicDate":"1955-04-08T00:00:00","publicationYear":"1955","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Isolation of organic carbon from bones for C14 dating","docAbstract":"No abstract available.
","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.121.3145.508","issn":"00368075","usgsCitation":"May, I., 1955, Isolation of organic carbon from bones for C14 dating: Science, v. 121, no. 3145, p. 508-509, https://doi.org/10.1126/science.121.3145.508.","productDescription":"2 p.","startPage":"508","endPage":"509","costCenters":[],"links":[{"id":221345,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"South Dakota","otherGeospatial":"Craven Canyon","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -103.8154991531584,\n 43.40757997128466\n ],\n [\n -103.8154991531584,\n 43.36539801664995\n ],\n [\n -103.74293833184126,\n 43.36539801664995\n ],\n [\n -103.74293833184126,\n 43.40757997128466\n ],\n [\n -103.8154991531584,\n 43.40757997128466\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"121","issue":"3145","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3f54e4b0c8380cd6444f","contributors":{"authors":[{"text":"May, I.","contributorId":84896,"corporation":false,"usgs":true,"family":"May","given":"I.","email":"","affiliations":[],"preferred":false,"id":360029,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5220843,"text":"5220843 - 1955 - Neck-banding and other color-marking of waterfowl; Its merits and shortcomings","interactions":[],"lastModifiedDate":"2025-01-31T15:43:44.788398","indexId":"5220843","displayToPublicDate":"1955-04-04T00:00:00","publicationYear":"1955","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Neck-banding and other color-marking of waterfowl; Its merits and shortcomings","docAbstract":"No abstract available.
","language":"English","publisher":"Wiley","doi":"10.2307/3796876","usgsCitation":"Aldrich, J.W., and Steenis, J.H., 1955, Neck-banding and other color-marking of waterfowl; Its merits and shortcomings: Journal of Wildlife Management, v. 19, no. 2, p. 317-318, https://doi.org/10.2307/3796876.","productDescription":"2 p.","startPage":"317","endPage":"318","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":194043,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Missouri","city":"Sumner","otherGeospatial":"Swan Lake National Wildlife Refuge","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -93.26181584892859,\n 39.674456128679566\n ],\n [\n -93.26181584892859,\n 39.57443340227121\n ],\n [\n -93.12543604668674,\n 39.57443340227121\n ],\n [\n -93.12543604668674,\n 39.674456128679566\n ],\n [\n -93.26181584892859,\n 39.674456128679566\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"19","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697e3d","contributors":{"authors":[{"text":"Aldrich, John W.","contributorId":65900,"corporation":false,"usgs":true,"family":"Aldrich","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":332578,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Steenis, John H.","contributorId":57918,"corporation":false,"usgs":true,"family":"Steenis","given":"John","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":332577,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5220253,"text":"5220253 - 1955 - Bicolor as a rabbit food","interactions":[],"lastModifiedDate":"2025-01-31T15:35:13.79293","indexId":"5220253","displayToPublicDate":"1955-04-04T00:00:00","publicationYear":"1955","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Bicolor as a rabbit food","docAbstract":"No abstract available.
","language":"English","publisher":"Wiley","doi":"10.2307/3796880","usgsCitation":"Rosene, W., 1955, Bicolor as a rabbit food: Journal of Wildlife Management, v. 19, no. 2, p. 324-324, https://doi.org/10.2307/3796880.","productDescription":"1 p.","startPage":"324","endPage":"324","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":489757,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2307/3796880","text":"Publisher Index Page"},{"id":193805,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"South Carolina","city":"Pineville","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -80.09071466980241,\n 33.48524485584464\n ],\n [\n -80.09071466980241,\n 33.403971542415846\n ],\n [\n -79.97066207803113,\n 33.403971542415846\n ],\n [\n -79.97066207803113,\n 33.48524485584464\n ],\n [\n -80.09071466980241,\n 33.48524485584464\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"19","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ce4b07f02db62638b","contributors":{"authors":[{"text":"Rosene, W.","contributorId":67609,"corporation":false,"usgs":true,"family":"Rosene","given":"W.","email":"","affiliations":[],"preferred":false,"id":331551,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":37885,"text":"37885 - 1955 - Public use of National Wildlife Refuges, 1954","interactions":[],"lastModifiedDate":"2014-07-22T10:19:04","indexId":"37885","displayToPublicDate":"1955-04-01T10:18:17","publicationYear":"1955","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"366","title":"Public use of National Wildlife Refuges, 1954","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","usgsCitation":"U.S. Fish and Wildlife Service, 1955, Public use of National Wildlife Refuges, 1954: Wildlife Leaflet 366, 4 p.","productDescription":"4 p.","numberOfPages":"4","costCenters":[],"links":[{"id":290673,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd582e4b0824b2d177680","contributors":{"authors":[{"text":"U.S. Fish and Wildlife Service","contributorId":128143,"corporation":true,"usgs":false,"organization":"U.S. Fish and Wildlife Service","id":529757,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010987,"text":"70010987 - 1955 - Crystal structure of rutherfordine, UO2CO3","interactions":[],"lastModifiedDate":"2026-03-03T15:31:23.431191","indexId":"70010987","displayToPublicDate":"1955-04-01T00:00:00","publicationYear":"1955","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Crystal structure of rutherfordine, UO2CO3","docAbstract":"No abstract available.
","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.121.3144.472","issn":"00368075","usgsCitation":"Christ, C., Clark, J.R., and Evans, H.T., 1955, Crystal structure of rutherfordine, UO2CO3: Science, v. 121, no. 3144, p. 472-473, https://doi.org/10.1126/science.121.3144.472.","productDescription":"2 p.","startPage":"472","endPage":"473","costCenters":[],"links":[{"id":221346,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"121","issue":"3144","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fcfce4b0c8380cd4e56f","contributors":{"authors":[{"text":"Christ, C. L.","contributorId":53906,"corporation":false,"usgs":true,"family":"Christ","given":"C. L.","affiliations":[],"preferred":false,"id":360031,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clark, J. R.","contributorId":55764,"corporation":false,"usgs":true,"family":"Clark","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":360032,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Evans, H. T. Jr.","contributorId":41859,"corporation":false,"usgs":true,"family":"Evans","given":"H.","suffix":"Jr.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":360030,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70048360,"text":"tei357 - 1955 - Relation of uranium to hypogene mineral zoning in the Front Range mineral belt, Colorado","interactions":[],"lastModifiedDate":"2014-03-07T10:48:37","indexId":"tei357","displayToPublicDate":"1955-03-07T14:12:00","publicationYear":"1955","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":"357","title":"Relation of uranium to hypogene mineral zoning in the Front Range mineral belt, Colorado","docAbstract":"Many of the mining districts of the Colorado Front Range mineral belt contain mesothermal sulfide ores that exhibit a zonal distribution. Present data indicate that in most of the zoned districts pitchblende and/or secondary uranium minerals are most abundant in a transition zone between central areas containing predominantly pyritic gold ores and peripheral areas containing dominantly lead-zinc-silver deposits. Copper in the form of chalcopyrite is also probably more abundant in the transition zone than in adjacent zones. Many mineralized areas in the Front Range mineral belt are roughly co-extensive with and probably related to groups of Tertiary intrusives. The solutions that deposited sulfide and pitchblende in these areas probably were derived from many different types of source magma, but some bostonite magmas were probably particularly important sources of uranium-bearing solutions. At most localities where the relative ages of pitchblende and associated sulfides are known, the pitchblende is early in the paragenetic sequence, and not of intermediate age as suggested by its zonal position. This discrepancy may be the result of overlapping zones of deposition related to adjacent centers of mineralization, to changing environments of deposition within zones during the period of mineralization, or to unknown factors. Uranium is also present in districts in which the dominant mineralization is markedly different from the common pyritic gold-base metal sulfide mineralization. In the Jamestown district uranium appears to be associated'.mainly with fluorspar;, in other districts that exhibit little or no systematic hypogene zoning) it is ubiquitous. If uranium is present in zoned districts, a large proportion of she deposits probably should be in the transition zones. The application of this concept may be a valuable guide in prospecting for\nuranium.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei357","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Wallace, S.R., Leonard, B.F., and Campbell, R.H., 1955, Relation of uranium to hypogene mineral zoning in the Front Range mineral belt, Colorado: U.S. Geological Survey Trace Elements Investigations 357, Report: 43 p.; Plate 1: 42.17 inches x 55.88 inches; Plate 2: 20.87 inches x 20.14 inches, https://doi.org/10.3133/tei357.","productDescription":"Report: 43 p.; Plate 1: 42.17 inches x 55.88 inches; Plate 2: 20.87 inches x 20.14 inches","costCenters":[],"links":[{"id":278013,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/357/report-thumb.jpg"},{"id":279524,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/357/plate-1.pdf"},{"id":279525,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/357/plate-2.pdf"},{"id":279523,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/357/report.pdf"}],"country":"United States","state":"Arizona;Colorado","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.2,35.3 ], [ -114.2,40.1663 ], [ -105.5566,40.1663 ], [ -105.5566,35.3 ], [ -114.2,35.3 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"524162e8e4b0ec672f073afc","contributors":{"authors":[{"text":"Wallace, Stewart Raynor","contributorId":53396,"corporation":false,"usgs":true,"family":"Wallace","given":"Stewart","email":"","middleInitial":"Raynor","affiliations":[],"preferred":false,"id":484418,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leonard, B. F.","contributorId":32911,"corporation":false,"usgs":true,"family":"Leonard","given":"B.","middleInitial":"F.","affiliations":[],"preferred":false,"id":484416,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Campbell, R. H.","contributorId":52160,"corporation":false,"usgs":true,"family":"Campbell","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":484417,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":71339,"text":"tei289 - 1955 - Carnotite resources of San Miguel bench, Montrose County, Colorado","interactions":[],"lastModifiedDate":"2014-05-16T15:19:17","indexId":"tei289","displayToPublicDate":"1955-03-06T15:14:00","publicationYear":"1955","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":"289","title":"Carnotite resources of San Miguel bench, Montrose County, Colorado","docAbstract":"San Miguel bench includes about 4 square miles in the southern part of T. 48 N., R. 17 W., New Mexico principal meridian, Montrose County, Colorado.
\nProduction of carnotite ore from the area has been about 15,000 short tons having an estimated average grade of 0.31 percent U3O8 and 1.6 percent V2O5.\n
\n
Nearly all of the carnotite deposits occur in a single continuous sandstone bed near the top of the Salt Wash member of the Jurassic Morrison formation. These deposits consist chiefly of sandstone impregnated with uranium- and vanadium-bearing minerals. They are irregular tabular-shaped masses ranging in size from a few short tons to 30,000 short tons or more of minable carnotite ore.
\nDuring the period November 27, 1951, to April 17, 1953, the U.S. Geological Survey drilled 309 holes totaling 92,194 feet on the San Miguel bench.
\nReserves total about 43,000 short tons of material 1 foot or more thick and contain 0.10 percent or More U3O8 or 1.0 percent or more V2O5. Of these reserves 3,300 short tons occur in private land. These reserves are in ten deposits found by Geological Survey drilling. Potential reserves (reserves based on geologic evidence only) are predicted to total about 15,000 short tons, averaging 0.30 percent U3O8 and 1.6 percent V2O5.
\nNo additional drilling in the San Miguel bench is planned by the Geological Survey. Some drilling by private enterprise is recommended.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei289","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Alvord, D.C., 1955, Carnotite resources of San Miguel bench, Montrose County, Colorado: U.S. Geological Survey Trace Elements Investigations 289, Report: 42 p.; Plate 1: 23.93 x 25.81 inches; Plate 2: 29.89 x 21.02, https://doi.org/10.3133/tei289.","productDescription":"Report: 42 p.; Plate 1: 23.93 x 25.81 inches; Plate 2: 29.89 x 21.02","costCenters":[],"links":[{"id":284531,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0289/plate-1.pdf"},{"id":284532,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0289/report.pdf"},{"id":283437,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei289.PNG"}],"country":"United States","state":"Colorado","county":"Montrose County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.060256,38.152156 ], [ -109.060256,38.668569 ], [ -107.50002,38.668569 ], [ -107.50002,38.152156 ], [ -109.060256,38.152156 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53558ff8e4b0120853e8be69","contributors":{"authors":[{"text":"Alvord, Donald Clayton","contributorId":49356,"corporation":false,"usgs":true,"family":"Alvord","given":"Donald","email":"","middleInitial":"Clayton","affiliations":[],"preferred":false,"id":284013,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":37878,"text":"37878 - 1955 - The opossum","interactions":[],"lastModifiedDate":"2014-07-22T10:11:33","indexId":"37878","displayToPublicDate":"1955-03-01T10:11:03","publicationYear":"1955","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"359","title":"The opossum","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","usgsCitation":"U.S. Fish and Wildlife Service, 1955, The opossum: Wildlife Leaflet 359, 2 p.","productDescription":"2 p.","numberOfPages":"2","costCenters":[],"links":[{"id":290669,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd582e4b0824b2d177682","contributors":{"authors":[{"text":"U.S. Fish and Wildlife Service","contributorId":128143,"corporation":true,"usgs":false,"organization":"U.S. Fish and Wildlife Service","id":529755,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":51856,"text":"ofr55123 - 1955 - Reproposal for review report of survey scope, Snake River basin above Weiser, Idaho","interactions":[],"lastModifiedDate":"2015-10-22T13:06:12","indexId":"ofr55123","displayToPublicDate":"1955-02-18T00:00:00","publicationYear":"1955","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":"55-123","title":"Reproposal for review report of survey scope, Snake River basin above Weiser, Idaho","docAbstract":"This submission applies to the available waters accruing to Snake River between Milner Dam and Weiser, Idaho. For basin upstram see statement by Lynn Crandall, \"New storage on Snake River for irrigation use above Milner, Idaho\" as filed February 15 at Idaho Falls hearing.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr55123","usgsCitation":"Newell, T.R., 1955, Reproposal for review report of survey scope, Snake River basin above Weiser, Idaho: U.S. Geological Survey Open-File Report 55-123, 5 p., https://doi.org/10.3133/ofr55123.","productDescription":"5 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":178900,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr55123.jpg"},{"id":310492,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1955/0123/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -116.91650390625,\n 44.23732831822538\n ],\n [\n -116.8670654296875,\n 44.13097085672744\n ],\n [\n -116.94946289062499,\n 43.8899753738369\n ],\n [\n -116.91650390625,\n 43.71156424665851\n ],\n [\n -116.7132568359375,\n 43.5326204268101\n ],\n [\n -116.3177490234375,\n 43.27320591705845\n ],\n [\n -115.9112548828125,\n 43.03677585761058\n ],\n [\n -115.4608154296875,\n 43.01268088642034\n ],\n [\n -115.08178710937499,\n 42.98857645832184\n ],\n [\n -114.466552734375,\n 42.783307077249624\n ],\n [\n -114.1754150390625,\n 42.64608143458068\n ],\n [\n -113.917236328125,\n 42.60970621339408\n ],\n [\n -113.9666748046875,\n 42.48019996901214\n ],\n [\n -114.76867675781249,\n 42.61779143282346\n ],\n [\n -115.27954101562499,\n 42.89206418807337\n ],\n [\n -115.72998046875,\n 42.867912483915305\n ],\n [\n -116.20239257812499,\n 42.99259451971113\n ],\n [\n -116.93847656250001,\n 43.54058479482877\n ],\n [\n -117.10876464843749,\n 43.683763524273346\n ],\n [\n -116.99890136718749,\n 44.09153051045218\n ],\n [\n -116.993408203125,\n 44.19402066387343\n ],\n [\n -116.91650390625,\n 44.23732831822538\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a55e4b07f02db62c77b","contributors":{"authors":[{"text":"Newell, Thomas R.","contributorId":106876,"corporation":false,"usgs":true,"family":"Newell","given":"Thomas","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":244397,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":13652,"text":"ofr5491 - 1955 - The relation between composition and swelling in clays","interactions":[],"lastModifiedDate":"2015-10-22T11:56:51","indexId":"ofr5491","displayToPublicDate":"1955-02-08T00:00:00","publicationYear":"1955","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":"54-91","title":"The relation between composition and swelling in clays","docAbstract":"The phenomenon of swelling is associated with the hydration of clays; however, all clays do not swell when hydrated. those of the kaolin group, for example, exhibit little or no swelling on hydration. Sodiwm montmoillonite, on the other hand, characteristically swells in water to many times its dry volume. Calcium and magnesium montmorillonite and the hydrous micas, or so called illites, fall between these two extremes in swelling properties, but are, in general, much closer to kaolinite than to sodium montmorillonite in their increase in volume on hydration. These differences in the swelling characteristics of different clays may be related to their chemical composition, to the kind and degree of isomorphous replacements in their structure, and to the amount and nature of their associated exchangeable cations.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5491","usgsCitation":"Foster, M.D., 1955, The relation between composition and swelling in clays: U.S. Geological Survey Open-File Report 54-91, 34 p., https://doi.org/10.3133/ofr5491.","productDescription":"34 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":147301,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr5491.jpg"},{"id":310461,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1954/0091/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640f4c","contributors":{"authors":[{"text":"Foster, Margaret D.","contributorId":21141,"corporation":false,"usgs":true,"family":"Foster","given":"Margaret","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":168179,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":71957,"text":"tem563A - 1955 - Reconnaissance for radioactivity in the Gold Hill Mining Area, Boulder County, Colorado, Part 1","interactions":[],"lastModifiedDate":"2014-07-16T13:20:57","indexId":"tem563A","displayToPublicDate":"1955-02-01T13:19:03","publicationYear":"1955","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":"563","chapter":"A","title":"Reconnaissance for radioactivity in the Gold Hill Mining Area, Boulder County, Colorado, Part 1","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/tem563A","collaboration":"Prepared by the Geological Survey for the United States Atomic Energy Commission, Technical Information Service.","usgsCitation":"Campbell, R., 1955, Reconnaissance for radioactivity in the Gold Hill Mining Area, Boulder County, Colorado, Part 1: U.S. Geological Survey Trace Elements Memorandum 563, 28 p., https://doi.org/10.3133/tem563A.","productDescription":"28 p.","numberOfPages":"28","costCenters":[],"links":[{"id":290291,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Colorado","county":"Boulder County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.694377,39.912886 ], [ -105.694377,40.262785 ], [ -105.052637,40.262785 ], [ -105.052637,39.912886 ], [ -105.694377,39.912886 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c79f14e4b01948416424a5","contributors":{"authors":[{"text":"Campbell, Russell H.","contributorId":91074,"corporation":false,"usgs":true,"family":"Campbell","given":"Russell H.","affiliations":[],"preferred":false,"id":284916,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70048095,"text":"tei303 - 1955 - Geology of the Huron River pitchblende occurrence, Baraga County, Michigan","interactions":[],"lastModifiedDate":"2014-03-07T09:36:07","indexId":"tei303","displayToPublicDate":"1955-01-11T11:07:00","publicationYear":"1955","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":"303","title":"Geology of the Huron River pitchblende occurrence, Baraga County, Michigan","docAbstract":"Small quantities of uranium-bearing minerals were discovered by a geologist of the Jones and Laughlin Ore Company during the summer of 1949 along the East Branch of the Huron River, sec. 1, T. 51 N., R. 30 W., Baraga County, Mich. Subsequent diamond drilling of the prospect by the Jones and Laughlin Ore Company and the Ford Motor Company disclosed only minor amounts of radioactive materials at shallow depths in the immediate vicinity of the surface showings.\nPitchblende and secondary uranium minerals occur as very small, discontinuous stringers and pods in calcite and quartz cementing the breccia within a low-angle shear zone that dips about 10 degrees to the southwest. The shear zone has a thickness of 10 to 30 feet and cuts black, locally carbonaceous slates of the upper Huronian Precambrian Michigamme slate. Mineral deposition during two hypogene stages and one supergene stage was identified in polished sections. The first phase consisted of the introduction of quartz and minor hematite into the sheared slate. After fracturing of the quartz the second stage was initiated by deposition of calcite, pyrite, rutile, pitchblende, bornite, sphalerite, chalcopyrite, galena, and greenockite. The supergene stage consisted of the development of metatyuyamunite, chalcopyrite, chalcocite, covellite, cuprite, volborthite, malachite, and goethite.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/tei303","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Vickers, R., 1955, Geology of the Huron River pitchblende occurrence, Baraga County, Michigan: U.S. Geological Survey Trace Elements Investigations 303, Report: 21 p.; Plate: 26.39 inches x 30.24 inches, https://doi.org/10.3133/tei303.","productDescription":"Report: 21 p.; Plate: 26.39 inches x 30.24 inches","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":277449,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/303/report-thumb.jpg"},{"id":279895,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/303/plate-2.pdf"},{"id":279894,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/303/report.pdf"}],"country":"United States","state":"Michigan","county":"Baraga County","otherGeospatial":"Huron River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.681999,46.418903 ], [ -88.681999,46.967216 ], [ -87.99176,46.967216 ], [ -87.99176,46.418903 ], [ -88.681999,46.418903 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52303f63e4b04b8e63a20640","contributors":{"authors":[{"text":"Vickers, R.C.","contributorId":50583,"corporation":false,"usgs":true,"family":"Vickers","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":483735,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70048371,"text":"tei561 - 1955 - Uranium deposits at the Jomac mine, White Canyon area, San Juan County, Utah","interactions":[],"lastModifiedDate":"2013-11-22T09:24:08","indexId":"tei561","displayToPublicDate":"1955-01-07T10:03:00","publicationYear":"1955","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":"561","title":"Uranium deposits at the Jomac mine, White Canyon area, San Juan County, Utah","docAbstract":"The Jomac mine is in the White Canyon area. San Juan County, Utah, about 13 miles northeast of the town of White Canyon, Utah. The mine is owned by the Ellihill Mining Company, White Canyon, Utah. Mine workings consist pf two adits connected by a crosscut. Two hundred feet of exploratory drifting and 2,983.5 feet of exploratory core drilling were completed during 1953 by the owners with Defense Minerals Exploration Administration assistance. Sedimentary rocks exposed in the area of the Jomac mine are of Permian to Late Triassic age, having a combined thickness of more than 1,700 feet. An ancient channel, from 200 to 400 feet wide and about 4 feet deep, enters the mine area from the southwest, swinging abruptly northwest near the mine workings and continuing to the northern tip of the Jomac Hillo This channel was cut into the upper beds of the Moenkopi formation and filled in part by Chinle and in part by Shinarump sediments. This channel is marked by depressions that apparently were scoured into its floor; a tributary channel may have joined it from the southeast at a point near the mine workings. Chinle beds Intertongue with Shinarump beds along the southwestern part of the channel. After the main channel was partly filled by siltstone of the Chinle formation, the stream was apparently diverted into the tributary channel, and scours were cut into\nthe Chinle siltstone and filled by Shina'rump sandstone, conglomerate, and siltstone. Statistical study of wood orientation in the beds of the Shinarump conglomerate further indicates a channel trend of about N. 23° W. Basal siltstoned-pebble conglomerates appear to mark the edge of channels and scours. Jomac Hill is on the crest of a southwest-plunging fold that is on the west flank of a larger syncline. The area surrounding the hill is broken by intense faulting, but no faults were noted in the vicinity of the mine. The major fractures in the mine workings strike N. 70° to 80° E. and are steeply dipping. Secondary steeply dipping fractures strike N. 40° to 60 °E., and N. 10° E. to N. 10° W. The fractures are believed to be related to the anticlinal structure rather than the faults. Most of the uranium is contained in coa!5 associated with jarosite and gypsum in sandstone, conglomerate, or sandy siltstone near the base of the Shinarump conglomerate. Uranium occurs ill a fibrous green secondary mineral, metazeunerite, an unknown fibrous yellow mineral, and an unknown massive yellow mineral. Secondary copper minerals including malachite\nazurite, and chalcanthite occur locally with the uranium minerals. Principal ore guides at the Jomac mine are channels, and scours at the bottom of these channels coal-bearing sandstone or conglomerate at the base of the Shinarump conglomerate, coal, and jarosite.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei561","collaboration":"Prepared in cooperation with the U.S. Atomic Energy Commission","usgsCitation":"Trites, A., and Hadd, G., 1955, Uranium deposits at the Jomac mine, White Canyon area, San Juan County, Utah: U.S. Geological Survey Trace Elements Investigations 561, Report: 39 p.; Plate 3: 33.32 inches x 28.01 inches, https://doi.org/10.3133/tei561.","productDescription":"Report: 39 p.; Plate 3: 33.32 inches x 28.01 inches","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278029,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/561/report-thumb.jpg"},{"id":279534,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/561/plate-3.pdf"},{"id":279533,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/561/report.pdf"}],"country":"United States","state":"Utah","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.2500,37.8750 ], [ -110.2500,38.0000 ], [ -110.1250,38.0000 ], [ -110.1250,37.8750 ], [ -110.2500,37.8750 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5242b466e4b096ee6246420a","contributors":{"authors":[{"text":"Trites, A.F.","contributorId":25196,"corporation":false,"usgs":true,"family":"Trites","given":"A.F.","affiliations":[],"preferred":false,"id":484464,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hadd, G.A.","contributorId":105763,"corporation":false,"usgs":true,"family":"Hadd","given":"G.A.","affiliations":[],"preferred":false,"id":484465,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5220250,"text":"5220250 - 1955 - Recommendations for the culture of Lespedeza bicolor","interactions":[],"lastModifiedDate":"2025-01-31T16:26:47.408851","indexId":"5220250","displayToPublicDate":"1955-01-03T00:00:00","publicationYear":"1955","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Recommendations for the culture of Lespedeza bicolor","docAbstract":"No abstract available.
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The amount of radiation is influenced by the size of the uranium deposit, the size of the drainage area of the stream, the grain size of the sediments, and the lithology of the rocks over which the stream flows. The spacing of the stations where readings are taken is controlled by the size of the stream, and special readings are also taken directly downstream from important tributaries. An anomaly is empirically defined as a 10 percent rise over background. Radioactive material from large uranium deposits has been detected as much as 1 mile downstream. Radioactive material from smaller deposits is detachable over shorter distances. 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