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,{"id":50937,"text":"ofr5116 - 1951 - Reconnaissance of Henry Mountains area, Wayne and Garfield Counties, Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:11:35","indexId":"ofr5116","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"51-16","title":"Reconnaissance of Henry Mountains area, Wayne and Garfield Counties, Utah","language":"ENGLISH","doi":"10.3133/ofr5116","usgsCitation":"Reinhardt, E., 1951, Reconnaissance of Henry Mountains area, Wayne and Garfield Counties, Utah: U.S. Geological Survey Open-File Report 51-16, 7 p., https://doi.org/10.3133/ofr5116.","productDescription":"7 p.","costCenters":[],"links":[{"id":177882,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1951/0016/report-thumb.jpg"},{"id":86407,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1951/0016/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86408,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1951/0016/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ce4b07f02db63e854","contributors":{"authors":[{"text":"Reinhardt, E.V.","contributorId":26008,"corporation":false,"usgs":true,"family":"Reinhardt","given":"E.V.","email":"","affiliations":[],"preferred":false,"id":242646,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":50938,"text":"ofr5179 - 1951 - Preliminary report on some uranium deposits along the west side of the San Rafael Swell (Utah)","interactions":[],"lastModifiedDate":"2021-01-27T17:17:03.933494","indexId":"ofr5179","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"51-79","title":"Preliminary report on some uranium deposits along the west side of the San Rafael Swell (Utah)","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr5179","usgsCitation":"Reynard, M., 1951, Preliminary report on some uranium deposits along the west side of the San Rafael Swell (Utah): U.S. Geological Survey Open-File Report 51-79, Report: iv, 31 p.; 1 Plate: 7.37 x 10.31 inches, https://doi.org/10.3133/ofr5179.","productDescription":"Report: iv, 31 p.; 1 Plate: 7.37 x 10.31 inches","costCenters":[],"links":[{"id":382674,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1951/0079/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":382673,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1951/0079/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":177883,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1951/0079/report-thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"San Rafael Swell","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.65704345703124,\n              38.739088441876866\n            ],\n            [\n              -110.43731689453125,\n              38.739088441876866\n            ],\n            [\n              -110.43731689453125,\n              38.858958910448536\n            ],\n            [\n              -110.65704345703124,\n              38.858958910448536\n            ],\n            [\n              -110.65704345703124,\n              38.739088441876866\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66ca2b","contributors":{"authors":[{"text":"Reynard, M.L.","contributorId":70471,"corporation":false,"usgs":true,"family":"Reynard","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":242647,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":50939,"text":"ofr5133 - 1951 - Reconnaissance of Basin-Boulder-Clancy area, Jefferson County, Montana","interactions":[],"lastModifiedDate":"2019-11-21T16:11:47","indexId":"ofr5133","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"51-33","title":"Reconnaissance of Basin-Boulder-Clancy area, Jefferson County, Montana","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr5133","usgsCitation":"Reyner, M.L., 1951, Reconnaissance of Basin-Boulder-Clancy area, Jefferson County, Montana: U.S. Geological Survey Open-File Report 51-33, iii, 13 p. , https://doi.org/10.3133/ofr5133.","productDescription":"iii, 13 p. ","costCenters":[],"links":[{"id":369433,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1951/0033/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":177884,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1951/0033/report-thumb.jpg"}],"country":"United States","state":"Montana","county":"Jefferson County","otherGeospatial":"Basin-Boulder-Clancy area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.313232421875,\n              46.244451065485094\n            ],\n            [\n              -111.90948486328125,\n              46.244451065485094\n            ],\n            [\n              -111.90948486328125,\n              46.50217348354072\n            ],\n            [\n              -112.313232421875,\n              46.50217348354072\n            ],\n            [\n              -112.313232421875,\n              46.244451065485094\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ce4b07f02db63e84b","contributors":{"authors":[{"text":"Reyner, Millard L.","contributorId":18446,"corporation":false,"usgs":true,"family":"Reyner","given":"Millard","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":242648,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":50940,"text":"ofr5138 - 1951 - Geologic map of the baritic carbonate body near Mountain Pass, San Bernardino County, California","interactions":[],"lastModifiedDate":"2024-12-20T20:10:45.108918","indexId":"ofr5138","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"51-38","title":"Geologic map of the baritic carbonate body near Mountain Pass, San Bernardino County, California","docAbstract":"<p>A geologic map of an important deposit of rare earth metals studied recently by Geological Survey geologists near Mountain Pass, California has been completed Secretary of the Interior Oscar L. Chapman announced today. The discovery of this deposit was announced on January 16, and because of the great interest that has been shown in the deposit, the map is being made available for public inspection immediately, Secretary Chapman explained.</p><p>The deposit covered by this map is in San Bernardino County, California near where prospectors made the original discovery on the Birthday claims in 1949. Subsequent studies by the Geological Survey have shown that an area roughly 6 miles long and 2 miles wide, extending southeast from the original discovery, contains a number of other rare carth-bearing deposits, including the large ore body covered by this map.</p><p>This ore body is made up largely of a carbonate mineral and barite, but contains significant quantities of the rare earth mineral, bastnasite as well. It is exposed over an area 2,400 feet long and 400 feet wide.</p>","language":"English","doi":"10.3133/ofr5138","usgsCitation":"Sharp, W.N., and Olson, J.C., 1951, Geologic map of the baritic carbonate body near Mountain Pass, San Bernardino County, California: U.S. Geological Survey Open-File Report 51-38, Report: 6 p.; 1 Plate: 25.01 x 27.99 inches, https://doi.org/10.3133/ofr5138.","productDescription":"Report: 6 p.; 1 Plate: 25.01 x 27.99 inches","costCenters":[],"links":[{"id":86409,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1951/0038/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":177954,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1951/0038/report-thumb.jpg"},{"id":465414,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1951/0038/report.pdf"}],"country":"United States","state":"California","county":"San Bernardino County","otherGeospatial":"Mountain Pass","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -120.89975427742033,\n              35.42429043114734\n            ],\n            [\n              -120.89975427742033,\n              32.545930620983015\n            ],\n            [\n              -114.00850381183034,\n              32.545930620983015\n            ],\n            [\n              -114.00850381183034,\n              35.42429043114734\n            ],\n            [\n              -120.89975427742033,\n              35.42429043114734\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688d45","contributors":{"authors":[{"text":"Sharp, William N.","contributorId":18751,"corporation":false,"usgs":true,"family":"Sharp","given":"William","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":242649,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Olson, Jerry Chipman","contributorId":57869,"corporation":false,"usgs":true,"family":"Olson","given":"Jerry","email":"","middleInitial":"Chipman","affiliations":[],"preferred":false,"id":242650,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":50941,"text":"ofr5181 - 1951 - A catalogue of study material of radio-active minerals","interactions":[],"lastModifiedDate":"2019-11-22T14:41:33","indexId":"ofr5181","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"51-81","title":"A catalogue of study material of radio-active minerals","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr5181","usgsCitation":"Stern, T.W., 1951, A catalogue of study material of radio-active minerals: U.S. Geological Survey Open-File Report 51-81, 80 p., https://doi.org/10.3133/ofr5181.","productDescription":"80 p.","costCenters":[],"links":[{"id":177955,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1951/0081/report-thumb.jpg"},{"id":369487,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1951/0081/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd497fe4b0b290850ef3c9","contributors":{"authors":[{"text":"Stern, T. W.","contributorId":36122,"corporation":false,"usgs":true,"family":"Stern","given":"T.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":242651,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":50942,"text":"ofr5141 - 1951 - Uranium resources in the Silver Reef (Harrisburg) district, Washington County, Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:11:35","indexId":"ofr5141","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"51-41","title":"Uranium resources in the Silver Reef (Harrisburg) district, Washington County, Utah","docAbstract":"The Silver Reef district is near Leeds, about 16 miles north of St. George, Utah. The major structural feature of the district is the Virgin anticline, a fold extending southwestward toward St. George. The anticline has been breached by erosion, and sandstone hogbacks or 'reefs' are carved from the Shinarump conglomerate mud sandstone members of the Chinle formation, both of Triassic age. Thirteen occurrences of uranium-vanadium minerals, all within the Tecumseh sandstone, which is the upper part of the Silver Reef sandstone member of the Chinle formation, have been examined over an area about 1.75 miles wide and 3 miles long.\r\n\r\nTwo shipments of uranium-vanadium ore have been produced from the Chloride Chief and Silver Point claims. Samples from the deposits contain as much as 0.94 percent U3O8. The ore contains several times as much vanadium oxide as uranium, some copper, and traces of silver. It occurs in thinly bedded cross-bedded shales and sandstones within the fluviatile Tecumseh sandstone member of the Chinle formation. The ore beds are lenticular and are localized 2 near the base, center, and top of this sandstone member. The uranium-vanadium ore contains several yellow and green minerals not yet identified; the occurrences are similar to, but not associated with, the cerargyrite ore that made the district famous from 1879 to 1909.","language":"ENGLISH","doi":"10.3133/ofr5141","usgsCitation":"Stugard, F., 1951, Uranium resources in the Silver Reef (Harrisburg) district, Washington County, Utah: U.S. Geological Survey Open-File Report 51-41, 33 p., https://doi.org/10.3133/ofr5141.","productDescription":"33 p.","costCenters":[],"links":[{"id":177956,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1951/0041/report-thumb.jpg"},{"id":86410,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1951/0041/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86411,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1951/0041/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86412,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1951/0041/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86413,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1951/0041/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6967e5","contributors":{"authors":[{"text":"Stugard, Frederick Jr.","contributorId":88373,"corporation":false,"usgs":true,"family":"Stugard","given":"Frederick","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":242652,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":50943,"text":"ofr5132 - 1951 - Free Enterprise uranium prospect, Jefferson County, Montana","interactions":[{"subject":{"id":50943,"text":"ofr5132 - 1951 - Free Enterprise uranium prospect, Jefferson County, Montana","indexId":"ofr5132","publicationYear":"1951","noYear":false,"title":"Free Enterprise uranium prospect, Jefferson County, Montana"},"predicate":"SUPERSEDED_BY","object":{"id":35627,"text":"b988G - 1953 - Geology of the area adjacent to the Free Enterprise mine, Jefferson County, Montana","indexId":"b988G","publicationYear":"1953","noYear":false,"chapter":"G","title":"Geology of the area adjacent to the Free Enterprise mine, Jefferson County, Montana"},"id":1}],"supersededBy":{"id":35627,"text":"b988G - 1953 - Geology of the area adjacent to the Free Enterprise mine, Jefferson County, Montana","indexId":"b988G","publicationYear":"1953","noYear":false,"title":"Geology of the area adjacent to the Free Enterprise mine, Jefferson County, Montana"},"lastModifiedDate":"2012-02-02T00:11:35","indexId":"ofr5132","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"51-32","title":"Free Enterprise uranium prospect, Jefferson County, Montana","language":"ENGLISH","doi":"10.3133/ofr5132","usgsCitation":"Thurlow, E., and Reynard, M., 1951, Free Enterprise uranium prospect, Jefferson County, Montana (Superceded by: B-988-G): U.S. Geological Survey Open-File Report 51-32, 12 p., https://doi.org/10.3133/ofr5132.","productDescription":"12 p.","costCenters":[],"links":[{"id":177957,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Superceded by: B-988-G","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a86a2","contributors":{"authors":[{"text":"Thurlow, E.E.","contributorId":51374,"corporation":false,"usgs":true,"family":"Thurlow","given":"E.E.","email":"","affiliations":[],"preferred":false,"id":242653,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reynard, M.L.","contributorId":70471,"corporation":false,"usgs":true,"family":"Reynard","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":242654,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":50944,"text":"ofr5145 - 1951 - Exploration of the Big Boulder prospect, Larimer County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:11:35","indexId":"ofr5145","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"51-45","title":"Exploration of the Big Boulder prospect, Larimer County, Colorado","language":"ENGLISH","doi":"10.3133/ofr5145","usgsCitation":"Thurston, W.R., 1951, Exploration of the Big Boulder prospect, Larimer County, Colorado: U.S. Geological Survey Open-File Report 51-45, 2 p., https://doi.org/10.3133/ofr5145.","productDescription":"2 p.","costCenters":[],"links":[{"id":177958,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1951/0045/report-thumb.jpg"},{"id":86414,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1951/0045/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86415,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1951/0045/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86416,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1951/0045/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86417,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1951/0045/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86418,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1951/0045/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8c5b","contributors":{"authors":[{"text":"Thurston, W. R.","contributorId":9277,"corporation":false,"usgs":true,"family":"Thurston","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":242655,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":50945,"text":"ofr5183 - 1951 - Exploration of the Hyatt pegmatite, Larimer County, Colorado","interactions":[{"subject":{"id":50945,"text":"ofr5183 - 1951 - Exploration of the Hyatt pegmatite, Larimer County, Colorado","indexId":"ofr5183","publicationYear":"1951","noYear":false,"title":"Exploration of the Hyatt pegmatite, Larimer County, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":36035,"text":"b1011 - 1955 - Pegmatites of the Crystal Mountain district, Larimer County, Colorado","indexId":"b1011","publicationYear":"1955","noYear":false,"title":"Pegmatites of the Crystal Mountain district, Larimer County, Colorado"},"id":1}],"supersededBy":{"id":36035,"text":"b1011 - 1955 - Pegmatites of the Crystal Mountain district, Larimer County, Colorado","indexId":"b1011","publicationYear":"1955","noYear":false,"title":"Pegmatites of the Crystal Mountain district, Larimer County, Colorado"},"lastModifiedDate":"2012-02-02T00:11:35","indexId":"ofr5183","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"51-83","title":"Exploration of the Hyatt pegmatite, Larimer County, Colorado","language":"ENGLISH","doi":"10.3133/ofr5183","usgsCitation":"Thurston, W.R., 1951, Exploration of the Hyatt pegmatite, Larimer County, Colorado (Superceded by: B-1011): U.S. Geological Survey Open-File Report 51-83, 3 p., https://doi.org/10.3133/ofr5183.","productDescription":"3 p.","costCenters":[],"links":[{"id":177959,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Superceded by: B-1011","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696fed","contributors":{"authors":[{"text":"Thurston, William R.","contributorId":9712,"corporation":false,"usgs":true,"family":"Thurston","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":242656,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":50946,"text":"ofr5185 - 1951 - Red and gray clay underlying ore-bearing sandstone of the Morrison formation in western Colorado","interactions":[],"lastModifiedDate":"2019-11-22T14:36:39","indexId":"ofr5185","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"51-85","title":"Red and gray clay underlying ore-bearing sandstone of the Morrison formation in western Colorado","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr5185","usgsCitation":"Weeks, A.D., 1951, Red and gray clay underlying ore-bearing sandstone of the Morrison formation in western Colorado: U.S. Geological Survey Open-File Report 51-85, 16 p. , https://doi.org/10.3133/ofr5185.","productDescription":"16 p. ","costCenters":[],"links":[{"id":369486,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1951/0085/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":177960,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1951/0085/report-thumb.jpg"}],"country":"United States","state":"Colorado","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -108.984375,\n              36.94989178681327\n            ],\n            [\n              -105.5126953125,\n              36.94989178681327\n            ],\n            [\n              -105.5126953125,\n              41.0130657870063\n            ],\n            [\n              -108.984375,\n              41.0130657870063\n            ],\n            [\n              -108.984375,\n              36.94989178681327\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687e2f","contributors":{"authors":[{"text":"Weeks, Alice Dowse","contributorId":26762,"corporation":false,"usgs":true,"family":"Weeks","given":"Alice","email":"","middleInitial":"Dowse","affiliations":[],"preferred":false,"id":242657,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":50949,"text":"ofr5190 - 1951 - Preliminary report on ground-water conditions in the Cloquet area, Carlton County, Minnesota","interactions":[{"subject":{"id":50949,"text":"ofr5190 - 1951 - Preliminary report on ground-water conditions in the Cloquet area, Carlton County, Minnesota","indexId":"ofr5190","publicationYear":"1951","noYear":false,"title":"Preliminary report on ground-water conditions in the Cloquet area, Carlton County, Minnesota"},"predicate":"SUPERSEDED_BY","object":{"id":70047843,"text":"70047843 - 1952 - Geology and ground-water resources of the Cloquet area, Carlton County, Minnesota","indexId":"70047843","publicationYear":"1952","noYear":false,"title":"Geology and ground-water resources of the Cloquet area, Carlton County, Minnesota"},"id":1}],"supersededBy":{"id":70047843,"text":"70047843 - 1952 - Geology and ground-water resources of the Cloquet area, Carlton County, Minnesota","indexId":"70047843","publicationYear":"1952","noYear":false,"title":"Geology and ground-water resources of the Cloquet area, Carlton County, Minnesota"},"lastModifiedDate":"2018-02-14T11:26:45","indexId":"ofr5190","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"51-90","title":"Preliminary report on ground-water conditions in the Cloquet area, Carlton County, Minnesota","docAbstract":"<p>A study of the geology and ground-water conditions in the.area including Cloquet, Minn., was begun by the United States Geological Survey in 1948 in financial cooperation with the Minnesota State Department of Conservation, at the request of the city of Cloquet for assistance in locating large additional ground-water supplies for industrial and municipal use. The location of the area is show on figure 1. Although the present municipal wells provide a fairly adequate supply for current municipal needs, which averaged about three-quarters of a million gallons a day in 1946, there is great need for large supplies of good water, on the order of 10 million gallons a day, for use by the paper mills and other industries there. At present the industries are using water from the St. Louis River, but the water is unsatisfactory and expensive to use because it contains a large amount of objectionable organic material.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr5190","collaboration":"Prepared in cooperation with the Minnesota State Department of Conservation","usgsCitation":"Akin, P., 1951, Preliminary report on ground-water conditions in the Cloquet area, Carlton County, Minnesota: U.S. Geological Survey Open-File Report 51-90, 12 p., https://doi.org/10.3133/ofr5190.","productDescription":"12 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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,{"id":50950,"text":"ofr5142 - 1951 - Progress report of the geology and ground-water resources of the Devils Lake area, North Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:11:35","indexId":"ofr5142","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"51-42","title":"Progress report of the geology and ground-water resources of the Devils Lake area, North Dakota","language":"ENGLISH","doi":"10.3133/ofr5142","usgsCitation":"Akin, P., 1951, Progress report of the geology and ground-water resources of the Devils Lake area, North Dakota: U.S. Geological Survey Open-File Report 51-42, 8 p., https://doi.org/10.3133/ofr5142.","productDescription":"8 p.","costCenters":[],"links":[{"id":178027,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1951/0042/report-thumb.jpg"},{"id":86419,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1951/0042/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65df23","contributors":{"authors":[{"text":"Akin, P.D.","contributorId":104471,"corporation":false,"usgs":true,"family":"Akin","given":"P.D.","email":"","affiliations":[],"preferred":false,"id":242661,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":50951,"text":"ofr5191 - 1951 - Ground water in the Mohall area, Bottineau and Renville Counties, North Dakota","interactions":[],"lastModifiedDate":"2021-03-18T21:28:50.810463","indexId":"ofr5191","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"51-91","title":"Ground water in the Mohall area, Bottineau and Renville Counties, North Dakota","docAbstract":"<p><span>The Mohall area includes about 120 square miles in Bottineau </span><span>and Renville Counties in northwestern North Dakota. Mohall, whose </span><span>1950 population was 1,073, is the only town in the area. </span></p><p><span>The area is part of the Drift Prairie section of the Central Lowland physiographic province. It is characterized by the gently undulating ground moraine plain which slopes regionally to the northeast. It is drained by several southeast-trending intermittent streams which run almost at right angles to the regional slope. </span></p><p><span>The geologic formations in the Mohall area may be conveniently grouped into three units: the alluvium or alluvial deposits, which are found in the valleys of the intermittent streams, the till and associated glaciofluvial deposits, and the bedrock formations. </span></p><p><span>Ground water of reasonably good quality is obtained in the area only from the alluvial deposits. Because of the limited areal extent of these deposits, only a small number of farms obtain water supplies from them. However, the municipal water supply of the town of Mohall is obtained from these deposits in Spring Coulee northeast of the town, and much water for rural domestic use is hauled from the Becker well southwest of the town, in Little Deep Creek.</span></p><p><span>The principal source of recharge to the alluvial deposits is seepage during the spring runoff period. Natural discharge occurs by underflow down the stream valleys, by evaporation from open water and marshy areas and transpiration by plants.</span></p><p><span>The coefficient of transmissibility of </span><span>the alluvium, n the basis </span><span>of short pumping tests on Mohan wells 3 </span><span>and 4, is </span><span>indicated to be </span><span>about 6,000 </span><span>gallons a day per foot </span><span>at well 3 and about 20,000 gallons </span><span>a day per foot at well 4. The specific yield was computed as 0.25 </span><span>from the pumping </span><span>test on well </span><span>3. </span><span>No gravel of importance was en</span><span>countered in the two cross sections that were drilled across Spring </span><span>Coulee near the municipal wells, and the greatest thickness of satu</span><span>rated alluvial deposits found was only about 10 feet.</span></p><p><span>A Saturated thickness of 20 feet of sand and gravel was penetrated in test drilling along Cut Bank Creek. This is the greatest thickness of saturated alluvial deposits penetrated anywhere in the area. Ground water in storage in these alluvial deposits has been estimated to be about 150 million gallons per mile. These deposits are favorably situated to receive recharge, as Cut Bank Creek drains a rather large area and contains long stretches of open water perennially, Therefore, it is believed that the alluvial deposits of Cut Bank Creek offer the best promise for the development of moderately large perennial ground-water supplies for the present and probable future needs of the town of Mohall. </span></p><p><span>Test drilling in West Cut Bank Creek and in Little Deep Creek did not reveal alluvial deposits of such character and saturated thickness as to be considered favorable for the development of moderate to large water supplies, though some of the material encountered should yield adequate quantities for farm supplies.</span></p><p><span>The till with its associated glaciofluvial deposits is the surface formation in the&nbsp;area except where covered by the alluvial deposits&nbsp;in the stream valleys. In the Mohall areas, this formation is not an important aquifer and fewer than half a dozen wells are known to obtain water from it. The glaciofluvial deposits penetrated&nbsp;by the test holes are not considered adequate&nbsp;sources for permanent municipal or industrial supplies because they are likely to have small-areal extent and the overlying, relatively impermeable till makes seasonal recharge to them practically impossible.</span></p><p><span>Test drilling in the Souris River Valley about 12 miles west of Mohall penetrated as mutt as 58 feet of fluvial sediments, but practi-cally all the material is clay and silt. No important aquifers were found there. </span></p><p><span>At least 50 percent of all the farm water supplies in the area are obtained from wells in the bedrock formations, which probably consist of the Fox Hills sandstone, the Cannonball formation, and the Ludlow and Tongue Rtter members of the Fort Union formation. </span></p><p><span>Underlying these formations is approximately 2,600 feet of Cretaceous shale, which'is not water bearing. Water from the \"Dakota\" sandstone (including the possible equivalent of the Fuson shale and Lakota sandstone) may be obtained at depths of about 3,200 to 3,300 feet. The \"Dakota sandstone\" probably would yield water in sufficient quantity for municipal and many industrial purposes in this areas but the water is likely to be too highly mineralized for most domestic uses.</span></p><p><span>Jurassic formations underlie the&nbsp;Cretaceous formations in the area. They do not constitute aquifers of importance, and, any water found in them is likely to be too highly mineralized for most purposes. </span></p><p><span>In the Mohall area,&nbsp;by far the most suitable water for general purposes is obtained from the shallow alluvial deposits in the stream valleys. Of the seven samples of this water water analyzed, the highest concentration of dissolved solids was 1,242 parts per million and the lowest, 317 parts. The iron content was&nbsp;higher than desirable in two samples but satisfactory in all the&nbsp;others. Total hardness ranged from 196 to 570, which is higher than desirable. Nitrate was present in all samples analyzed and was excessively high in two samples. </span></p><p><span>Water samples for analysis were not obtained from the till and associated glaciofluvial deposits but the water from these aquifers is likely to be more highly mineralized than the water from the alluvial. deposits. </span></p><p><span>The water from the upper part of the bedrock is highly mineralized, but its mineral content varies considerably. The chloride concentration of the samples analyzed ranges from 608 to 3,740 parts per million and the bicarbonate concentration ranges from 160 to 860 parts per million. The specific conductance ranges from 3,190 to 11,120 micromhos and may represent total mineralization on the order of 1,500 to more than 6,000 parts per million in the water with high chloride and bicarbonate content. </span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr5191","usgsCitation":"Akin, P., 1951, Ground water in the Mohall area, Bottineau and Renville Counties, North Dakota: U.S. Geological Survey Open-File Report 51-91, Report: 90 p.; 2 Plates: 8.00 x 7.80 inches and 10.30 x 5.66 inches, https://doi.org/10.3133/ofr5191.","productDescription":"Report: 90 p.; 2 Plates: 8.00 x 7.80 inches and 10.30 x 5.66 inches","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science 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