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,{"id":625,"text":"wsp1141 - 1952 - Surface water supply of the United States, 1949, Part I, North Atlantic slope basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:08","indexId":"wsp1141","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","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":"1141","title":"Surface water supply of the United States, 1949, Part I, North Atlantic slope basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1141","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1952, Surface water supply of the United States, 1949, Part I, North Atlantic slope basins: U.S. Geological Survey Water Supply Paper 1141, xiv, 745 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1141.","productDescription":"xiv, 745 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":25188,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1141/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":136422,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1141/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db69672d","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":527597,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4185,"text":"cir162 - 1952 - Reconnaissance of the geology and ground-water resources of the Horse Creek-Bear Creek area, Laramie and Goshen Counties, Wyoming","interactions":[],"lastModifiedDate":"2021-10-20T18:38:06.058166","indexId":"cir162","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"162","title":"Reconnaissance of the geology and ground-water resources of the Horse Creek-Bear Creek area, Laramie and Goshen Counties, Wyoming","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir162","usgsCitation":"Babcock, H.M., Rapp, J.R., and Durum, W.H., 1952, Reconnaissance of the geology and ground-water resources of the Horse Creek-Bear Creek area, Laramie and Goshen Counties, Wyoming: U.S. Geological Survey Circular 162, Report: ii, 28 p.; 1 Plate: 33.50 × 16.00 inches, https://doi.org/10.3133/cir162.","productDescription":"Report: ii, 28 p.; 1 Plate: 33.50 × 16.00 inches","costCenters":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":31298,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/1952/0162/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":31299,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1952/0162/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118238,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1952/0162/report-thumb.jpg"},{"id":390689,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23593.htm"}],"country":"United States","state":"Wyoming","county":"Goshen County, Laramie County","otherGeospatial":"Horse Creek - Bear Creek Area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.16,\n              41.439\n            ],\n            [\n              -104.118,\n              41.439\n            ],\n            [\n              -104.118,\n              41.703\n            ],\n            [\n              -105.176,\n              41.703\n            ],\n            [\n              -105.176,\n              41.439\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a63e4b07f02db636eec","contributors":{"authors":[{"text":"Babcock, H. M.","contributorId":90698,"corporation":false,"usgs":true,"family":"Babcock","given":"H.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":148361,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rapp, John Richard","contributorId":75516,"corporation":false,"usgs":true,"family":"Rapp","given":"John","email":"","middleInitial":"Richard","affiliations":[],"preferred":false,"id":148359,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Durum, W. H.","contributorId":78311,"corporation":false,"usgs":true,"family":"Durum","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":148360,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":16441,"text":"ofr52164 - 1952 - Preliminary report on geology of part of the Chamberlain quadrangle, South Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:07:09","indexId":"ofr52164","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","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":"52-164","title":"Preliminary report on geology of part of the Chamberlain quadrangle, South Dakota","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr52164","usgsCitation":"Warren, C.R., and Crandell, D.R., 1952, Preliminary report on geology of part of the Chamberlain quadrangle, South Dakota: U.S. Geological Survey Open-File Report 52-164, 45 p. :folded map ;27 cm., https://doi.org/10.3133/ofr52164.","productDescription":"45 p. :folded map ;27 cm.","costCenters":[],"links":[{"id":148355,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1952/0164/report-thumb.jpg"},{"id":45418,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1952/0164/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45419,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1952/0164/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45420,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1952/0164/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cad9","contributors":{"authors":[{"text":"Warren, Charles Reynolds","contributorId":46964,"corporation":false,"usgs":true,"family":"Warren","given":"Charles","email":"","middleInitial":"Reynolds","affiliations":[],"preferred":false,"id":172850,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crandell, Dwight Raymond","contributorId":6440,"corporation":false,"usgs":true,"family":"Crandell","given":"Dwight","email":"","middleInitial":"Raymond","affiliations":[],"preferred":false,"id":172849,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":13662,"text":"ofr5249 - 1952 - Engineering report on the Elk basin, Embar-Tensleep Reservoir, Wyoming and Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:06:55","indexId":"ofr5249","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","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":"52-49","title":"Engineering report on the Elk basin, Embar-Tensleep Reservoir, Wyoming and Montana","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr5249","usgsCitation":"Fraher, J.A., 1952, Engineering report on the Elk basin, Embar-Tensleep Reservoir, Wyoming and Montana: U.S. Geological Survey Open-File Report 52-49, 54 p. ill., maps (some folded) ;28 cm., https://doi.org/10.3133/ofr5249.","productDescription":"54 p. ill., maps (some folded) ;28 cm.","costCenters":[],"links":[{"id":146934,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1952/0049/report-thumb.jpg"},{"id":42205,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1952/0049/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602723","contributors":{"authors":[{"text":"Fraher, John Albert","contributorId":59813,"corporation":false,"usgs":true,"family":"Fraher","given":"John","email":"","middleInitial":"Albert","affiliations":[],"preferred":false,"id":168192,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42595,"text":"ofr5273 - 1952 - Preliminary total intensity aeromagnetic map of part of the Somerville quadrangle, New Jersey","interactions":[],"lastModifiedDate":"2012-02-02T00:11:00","indexId":"ofr5273","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","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":"52-73","title":"Preliminary total intensity aeromagnetic map of part of the Somerville quadrangle, New Jersey","language":"ENGLISH","doi":"10.3133/ofr5273","usgsCitation":"Henderson, J., 1952, Preliminary total intensity aeromagnetic map of part of the Somerville quadrangle, New Jersey (Superceded by: GP-173 and GP-174): U.S. Geological Survey Open-File Report 52-73, 1 map., https://doi.org/10.3133/ofr5273.","productDescription":"1 map.","costCenters":[],"links":[{"id":168321,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Superceded by: GP-173 and GP-174","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db66931c","contributors":{"authors":[{"text":"Henderson, John R.","contributorId":93445,"corporation":false,"usgs":true,"family":"Henderson","given":"John R.","affiliations":[],"preferred":false,"id":226791,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16249,"text":"ofr52153 - 1952 - Geology of the Conant Creek-Muskrat Creek area, Fremont County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:07:09","indexId":"ofr52153","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","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":"52-153","title":"Geology of the Conant Creek-Muskrat Creek area, Fremont County, Wyoming","language":"ENGLISH","publisher":"[s.n.],","doi":"10.3133/ofr52153","usgsCitation":"Thompson, R.M., and White, V., 1952, Geology of the Conant Creek-Muskrat Creek area, Fremont County, Wyoming: U.S. Geological Survey Open-File Report 52-153, [1 v.] :ill., 3 folded maps ;29 cm., https://doi.org/10.3133/ofr52153.","productDescription":"[1 v.] :ill., 3 folded maps ;29 cm.","costCenters":[],"links":[{"id":148263,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":45168,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1952/0153/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45169,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1952/0153/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45170,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1952/0153/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db68307f","contributors":{"authors":[{"text":"Thompson, R. M.","contributorId":13961,"corporation":false,"usgs":true,"family":"Thompson","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":172497,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"White, V.L.","contributorId":25958,"corporation":false,"usgs":true,"family":"White","given":"V.L.","email":"","affiliations":[],"preferred":false,"id":172498,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":71251,"text":"tei184 - 1952 - Stratigraphic sections of the Phosphoria formation in Wyoming, 1947-48","interactions":[],"lastModifiedDate":"2014-07-14T13:56:58","indexId":"tei184","displayToPublicDate":"1986-10-17T15:13:19","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"184","title":"Stratigraphic sections of the Phosphoria formation in Wyoming, 1947-48","docAbstract":"<p>As part of a comprehensive investigation of the phosphate deposits of the western field begun in 1947, the U. S. Geological Survey has measured and sampled the Permian Phosphoria formation at many localities in Wyoming and adjacent states.  Because these data will not be fully synthesized for many years, segments of the data, accompanied by little or no interpretation, will be published as preliminary reports as they are assembled.  This report, which contains abstracts of some of the sections measured in western Wyoming (pl. 1), is one of this series.  The field and laboratory procedures adopted in these investigations are described rather fully in a companion report (McKelvey and others, 1952a).</p>\n<br/>\n<p>Many people have taken part in this investigation.  R. M. Campbell, R. A. Gulbrandsen, R. A. Harris, D. M. Larrabee, F. W. O'Malley, O. A. Payne, R. S. Sears, R. P. Sheldon, and R. A. Smart participated in the description of the strata and the collection of the samples referred to in this report.  D. B. Dimick, H. A. Larsen, and T. K. Rigby assisted in the preparation of exposures and the crushing and splitting of samples in the field.  The laboratory preparation of samples for chemical analysis was done in Denver, Colo., under the direction of W. P. Huleatt.</p>\n<br/>\n<p>Most of the P<sub>2</sub>O<sub>5</sub> and acid-insoluble analyses were made for the Survey by the U. S. Bureau of Mines at the Northwest Electrodevelopment Laboratory, Albany, Oreg., under the direction of S. M. Shelton and M. L. Wright.  Most of the Al<sub>2</sub>O<sub>3</sub>, Fe<sub>2</sub>O<sub>3</sub>, and loss-on-ignition analyses were made by the Trace Elements Section laboratory of the Survey in Washington, D. C., under the direction of J. C. Rabbitt by chemists I. Barlow, A. Caemmerer, J. Greene, F. S. Grimadli, N. Guttag, H. Levine, H. Mela, Jr., and R. G. Milkey, and most of the spectrographic reports were prepared in this laboratory by C. L. Waring.  The samples from one locality (Coal Canyon) were analyzed for P<sub>2</sub>O<sub>5</sub>, Al<sub>2</sub>O<sub>3</sub>, Fe<sub>2</sub>O<sub>3</sub>, V<sub>2</sub>O<sub>5</sub>, F, loss on ignition, and acid insoluble in the Chemical Laboratory of the Tennessee Valley Authority at Wilson Dam, Alabama, and spectrographically by D. M. Mortimer, of the Bureau of Mines at Albany.</p>\n<br/>\n<p>Compilation of the data has been largely by R. P. Sheldon and F. D. Frieske under the supervision of R. W. Swanson.  Organization of the tabular data has been largely by Anita Cozzetto.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei184","collaboration":"Also issued as Circular 210, 1953","usgsCitation":"McKelvey, V.E., Smith, L., Hoppin, R., and Armstrong, F., 1952, Stratigraphic sections of the Phosphoria formation in Wyoming, 1947-48: U.S. Geological Survey Trace Elements Investigations 184, 38 p., https://doi.org/10.3133/tei184.","productDescription":"38 p.","numberOfPages":"39","temporalStart":"1947-01-01","temporalEnd":"1948-12-31","costCenters":[],"links":[{"id":289954,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":289953,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0184/report.pdf"}],"country":"United States","state":"Wyoming","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.0569,40.9947 ], [ -111.0569,45.0059 ], [ -104.0522,45.0059 ], [ -104.0522,40.9947 ], [ -111.0569,40.9947 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53aa9dfce4b065055fab167f","contributors":{"authors":[{"text":"McKelvey, Vincent Ellis","contributorId":92650,"corporation":false,"usgs":true,"family":"McKelvey","given":"Vincent","email":"","middleInitial":"Ellis","affiliations":[],"preferred":false,"id":283880,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, L.E.","contributorId":102059,"corporation":false,"usgs":true,"family":"Smith","given":"L.E.","email":"","affiliations":[],"preferred":false,"id":283881,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hoppin, R.A.","contributorId":82682,"corporation":false,"usgs":true,"family":"Hoppin","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":283879,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Armstrong, F.C.","contributorId":32140,"corporation":false,"usgs":true,"family":"Armstrong","given":"F.C.","email":"","affiliations":[],"preferred":false,"id":283878,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":71253,"text":"tei186 - 1952 - Stratigraphic sections of the Phosphoria in Montana, 1947-48","interactions":[],"lastModifiedDate":"2014-07-14T14:04:32","indexId":"tei186","displayToPublicDate":"1980-06-25T16:04:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"186","title":"Stratigraphic sections of the Phosphoria in Montana, 1947-48","docAbstract":"<p>The U. S. Geological Survey has recently measured and sampled the Phosphoria formation at many localities in Montana and other western states.  These data will not be fully synthesized and analyzed for several years, but segments of the data, accompanied by little or no interpretation, will be published as preliminary reports as they are assembled.  This report, which contains abstracts of many of the sections measured in southwestern Montana (pl. 1), is one of this series.  The field and laboratory procedures adopted in these investigations are described rather fully in a companion report (McKelvey and others, 1952).</p>\n<br/>\n<p>Many people have taken part in this investigation.  The program of which this work is a part was organized by V. E. McKelvey.  J. G. Evans, J. E. Joyce, J. A. Kelleher, R. L. Konizeski, J. A. Mann, R. L. Parker, J. E Smedley, L. A. Thomas, and W. H. Wilson participated in the description of strata and collection of samples referred to in this report.  The laboratory preparation of samples for chemical analysis was done in Denver, Colo., under the direction of W. P. Huleatt.</p>\n<br/>\n<p>All the P<sub>2</sub>O<sub>5</sub>, F, V<sub>2</sub>O<sub>5</sub>, and acid-insoluble analyses were made for the Survey by the U. S. Bureau of Mines at the Northwest Electrodevelopment Laboratory, Albany, Oreg., under the direction of S. M. Shelton and M. L. Wright.  The Al<sub>2</sub>O<sub>3</sub>, Fe<sub>2</sub>O<sub>3</sub>, and loss-on-ignition analyses were about equally distributed between the Bureau of Mines and the Trace Elements Section laboratory of the Survey in Washington, D. C., under the direction of J. C. Rabbit by chemists I. Barlow, A. Caemmerer, J. Greene, N. Guttag, and E. H. Humphrey.  The spectrographic analyses were made by D. M. Mortimer, of the Bureau Mines in Albany, and the oil-shale analyses were made by the Bureau of Mines Petroleum and Oil-Shale Experiment Station at Laramie, Wyo.</p>\n<br/>\n<p>Compilation of the data has been largely by R. P. Sheldon and F. D. Frieske.  Organization of the tabular data has been largely by Anita Cozzetto.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei186","usgsCitation":"Swanson, R.W., Klepper, M.R., Lowell, W., Honkala, F., Cressman, E.R., Bostwick, D., Payne, O., and Ruppel, E.T., 1952, Stratigraphic sections of the Phosphoria in Montana, 1947-48: U.S. Geological Survey Trace Elements Investigations 186, 69 p., https://doi.org/10.3133/tei186.","productDescription":"69 p.","numberOfPages":"70","temporalStart":"1947-01-01","temporalEnd":"1948-12-31","costCenters":[],"links":[{"id":289958,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0186/report.pdf"},{"id":289960,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/0186/report-thumb.jpg"}],"country":"United States","state":"Montana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.05,44.3582 ], [ -116.05,49.0014 ], [ -104.0396,49.0014 ], [ -104.0396,44.3582 ], [ -116.05,44.3582 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53aa9dfce4b065055fab1681","contributors":{"authors":[{"text":"Swanson, Roger Warren","contributorId":13946,"corporation":false,"usgs":true,"family":"Swanson","given":"Roger","email":"","middleInitial":"Warren","affiliations":[],"preferred":false,"id":283891,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Klepper, M. R.","contributorId":64278,"corporation":false,"usgs":true,"family":"Klepper","given":"M.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":283894,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lowell, W.R.","contributorId":31381,"corporation":false,"usgs":true,"family":"Lowell","given":"W.R.","email":"","affiliations":[],"preferred":false,"id":283892,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Honkala, F.S.","contributorId":82270,"corporation":false,"usgs":true,"family":"Honkala","given":"F.S.","email":"","affiliations":[],"preferred":false,"id":283895,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Cressman, E. R.","contributorId":83494,"corporation":false,"usgs":true,"family":"Cressman","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":283896,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Bostwick, D.A.","contributorId":38541,"corporation":false,"usgs":true,"family":"Bostwick","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":283893,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Payne, O.A.","contributorId":108094,"corporation":false,"usgs":true,"family":"Payne","given":"O.A.","email":"","affiliations":[],"preferred":false,"id":283897,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Ruppel, E. T.","contributorId":6041,"corporation":false,"usgs":true,"family":"Ruppel","given":"E.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":283890,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":71252,"text":"tei185 - 1952 - Stratigraphic sections of the Phosphoria formation in Utah, 1947-48","interactions":[],"lastModifiedDate":"2014-07-14T13:59:55","indexId":"tei185","displayToPublicDate":"1980-06-25T15:42:28","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"185","title":"Stratigraphic sections of the Phosphoria formation in Utah, 1947-48","docAbstract":"<p>As part of a comprehensive investigation of the phosphate deposits of the western field begun in 1947, the U. S. Geological survey has measured an sampled the full thickness of the Permian Phosphoria formation and its partial correlative, the Park City formation, at many localities in Utah and other western states.  Although these data will not be fully analyzed for several years, segments of the data, accompanied by little or no interpretation, will be published as preliminary reports.  This report, which contains abstracts of many of the sections measured in northeastern Utah (pl. 1), is one of this series.  The field and laboratory procedures adopted in these investigations are described rather fully in a companion report (McKelvey and others, 1952).</p>\n<br/>\n<p>A large number of people have taken part in this investigation.  J. B. Collins, R. A. Gulbrandsen, R. A. Hoppin, J. A. Noel, F. W. O'Malley, O. A. Payne, J. F. Rominger, R. P. Sheldon, J. E. Smedley, and R. G. Waring participated in the description of strata and collection of samples referred to in this report.  D. B. Dimick, H. A. Larsen, and T. K. Rigby assisted in the preparation of trenches and the crushing and splitting of samples in the field.  The laboratory preparation of samples for chemical analysis was done in Denver, Colo., under the direction of W. P. Huleatt.</p>\n<br/>\n<p>Most of the chemical analyses reported herein were made for the Survey by the U. S. Bureau of Mines at the Northwest Electrodevelopment Laboratory, Albany, Oreg., under the direction of S. M. Shelton and M. L. Wright.  All the samples from one locality (Brazer Canyon) were analyzed in the Chemical Laboratory of the Tennessee Valley Authority at Wilson Dam, Ala.  Some of the Al<sub>2</sub>O<sub>3</sub>, Fe<sub>2</sub>O<sub>3</sub>, and loss-on-ignition analyses were made in the Trace Elements Section laboratory of the Survey in Washington, D. C., under the direction of J. C. Rabbitt by chemists I. Barlow, A Caemmerer, J. Greene, N. Guttag, and E. H. Humphrey.  The spectrographic analyses were made by D. M. Mortimer, of the Bureau of Mines in Albany.</p>\n<br/>\n<p>Compilation of the data has been largely by R. P. Sheldon and F. D. Frieske under the supervision of R. W. Swanson.  Organization of the tabular data has been largely by Anita Cozzetto.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei185","usgsCitation":"McKelvey, V.E., Smith, L., Kinney, D., Huddle, J.W., Hosford, G., Sears, R., Sprouse, D., and Steward, M., 1952, Stratigraphic sections of the Phosphoria formation in Utah, 1947-48: U.S. Geological Survey Trace Elements Investigations 185, 51 p., https://doi.org/10.3133/tei185.","productDescription":"51 p.","numberOfPages":"52","temporalStart":"1947-01-01","temporalEnd":"1948-12-31","costCenters":[],"links":[{"id":289956,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":289955,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0185/report.pdf"}],"country":"United States","state":"Utah","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.053,36.9979 ], [ -114.053,42.0016 ], [ -109.0411,42.0016 ], [ -109.0411,36.9979 ], [ -114.053,36.9979 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53aa9dfce4b065055fab167d","contributors":{"authors":[{"text":"McKelvey, Vincent Ellis","contributorId":92650,"corporation":false,"usgs":true,"family":"McKelvey","given":"Vincent","email":"","middleInitial":"Ellis","affiliations":[],"preferred":false,"id":283885,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, L.E.","contributorId":102059,"corporation":false,"usgs":true,"family":"Smith","given":"L.E.","email":"","affiliations":[],"preferred":false,"id":283889,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kinney, D.M.","contributorId":24014,"corporation":false,"usgs":true,"family":"Kinney","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":283882,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Huddle, J. W.","contributorId":29043,"corporation":false,"usgs":true,"family":"Huddle","given":"J.","middleInitial":"W.","affiliations":[],"preferred":false,"id":283883,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hosford, G.F.","contributorId":40199,"corporation":false,"usgs":true,"family":"Hosford","given":"G.F.","email":"","affiliations":[],"preferred":false,"id":283884,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Sears, R.S.","contributorId":93891,"corporation":false,"usgs":true,"family":"Sears","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":283886,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Sprouse, D.P.","contributorId":95456,"corporation":false,"usgs":true,"family":"Sprouse","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":283887,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Steward, M.D.","contributorId":97005,"corporation":false,"usgs":true,"family":"Steward","given":"M.D.","email":"","affiliations":[],"preferred":false,"id":283888,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70114219,"text":"tei156 - 1952 - Uranium deposits in Grant County, New Mexico","interactions":[],"lastModifiedDate":"2014-07-14T13:40:44","indexId":"tei156","displayToPublicDate":"1978-07-18T14:02:29","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"156","title":"Uranium deposits in Grant County, New Mexico","docAbstract":"<p>The known uranium deposits of Grant county, N. Mex., are principally in the White Signal and Black Hawk districts.  Both districts are within a northwesterly-trending belt of pre-Cambrian rocks, composed chiefly of granite with included gneisses, schists, and quartzites.  Younger dikes and stocks intrude the pre-Cambrian complex.  The White Signal district is on the southeast flanks of the Burro Mountains; the Black Hawk district is about 18 miles northwest of the town of White Signal.</p>\n<br/>\n<p>In the White Signal district the seconday uranium phosphates--autunite and torbernite--occur as fracture coatings and disseminations in oxidized parts of quartz-pyrite veins, and in the adjacent mafic dikes and granites; uraniferous limonite is common locally.  Most of the known uraniferous deposits are less that 50 feet in their greatest dimension.</p>\n<br/>\n<p>The most promising deposits in the district are on the Merry Widow and Blue Jay claims.  The richest sample taken from the Merry Widow mine contained more than 2 percent uranium and a sample from the Blue Jay property contained as much as 0.11 percent; samples from the other properties were of lower grade.</p>\n<br/>\n<p>In the Black Hawk district pitchblende is associated with nickel, silver, and cobalt minerals in fissure veins.  The most promising properties in the Black Hawk district are the Black Hawk, Alhambra, and Rose mines.  No uranium analyses from this district were available in 1951.</p>\n<br/>\n<p>There are no known minable reserves of uranium ore in either district, although there is some vein material at the Merry Widow mine of ore grade, if a market were available in the region.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei156","usgsCitation":"Granger, H., Bauer, H.L., Lovering, T., and Gillerman, E., 1952, Uranium deposits in Grant County, New Mexico: U.S. Geological Survey Trace Elements Investigations 156, Report: 65 p.; Figure 2; Figure 3; Figure 5, https://doi.org/10.3133/tei156.","productDescription":"Report: 65 p.; Figure 2; Figure 3; Figure 5","numberOfPages":"66","costCenters":[],"links":[{"id":289939,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":289933,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0156/figure-2.pdf"},{"id":289936,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0156/figure-5.pdf"},{"id":289935,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0156/figure-3.pdf"},{"id":289938,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0156/report.pdf"}],"country":"United States","state":"New Mexico","county":"Grant County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.0475,31.8637 ], [ -109.0475,33.2096 ], [ -107.6083,33.2096 ], [ -107.6083,31.8637 ], [ -109.0475,31.8637 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53aa9dfee4b065055fab1686","contributors":{"authors":[{"text":"Granger, Harry C.","contributorId":67992,"corporation":false,"usgs":true,"family":"Granger","given":"Harry C.","affiliations":[],"preferred":false,"id":495282,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bauer, Herman L. Jr.","contributorId":16484,"corporation":false,"usgs":true,"family":"Bauer","given":"Herman","suffix":"Jr.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":495279,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lovering, Tom G.","contributorId":31679,"corporation":false,"usgs":true,"family":"Lovering","given":"Tom G.","affiliations":[],"preferred":false,"id":495280,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gillerman, Elliot","contributorId":35741,"corporation":false,"usgs":true,"family":"Gillerman","given":"Elliot","email":"","affiliations":[],"preferred":false,"id":495281,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70048343,"text":"tem428 - 1952 - Pastora Peak SW, preliminary geologic map of part of the Carrizo mountains area, northeastern Arizona","interactions":[],"lastModifiedDate":"2014-03-04T13:34:22","indexId":"tem428","displayToPublicDate":"1962-01-01T15:02:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"428","title":"Pastora Peak SW, preliminary geologic map of part of the Carrizo mountains area, northeastern Arizona","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem428","usgsCitation":"Strobell, J., 1952, Pastora Peak SW, preliminary geologic map of part of the Carrizo mountains area, northeastern Arizona: U.S. Geological Survey Trace Elements Memorandum 428, Report: 2 p.; 1 Plate: 29.97 x 36.52 inches, https://doi.org/10.3133/tem428.","productDescription":"Report: 2 p.; 1 Plate: 29.97 x 36.52 inches","numberOfPages":"2","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":277985,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0428/report-thumb.jpg"},{"id":283225,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0428/report.pdf"},{"id":283226,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0428/plate-1.pdf"}],"scale":"20000","country":"United States","state":"Arizona","otherGeospatial":"Carrizo Mountains","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.25,36.75 ], [ -109.25,36.875 ], [ -109.125,36.875 ], [ -109.125,36.75 ], [ -109.25,36.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"523d6e65e4b097188d6c76de","contributors":{"authors":[{"text":"Strobell, J.D. Jr.","contributorId":22823,"corporation":false,"usgs":true,"family":"Strobell","given":"J.D.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":484353,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71237,"text":"tei139 - 1952 - Pegmatites of the Crystal Mountain district, Larimer County, Colorado","interactions":[],"lastModifiedDate":"2014-07-14T13:28:29","indexId":"tei139","displayToPublicDate":"1955-01-01T11:37:40","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"139","title":"Pegmatites of the Crystal Mountain district, Larimer County, Colorado","docAbstract":"<p>The Front Range of Colorado is composed chiefly of schists of the pre-Cambrian Idaho Springs formation which have been intruded by a variety of granitic batholiths. In the Crystal Mountain district the Mount Olympus granite, a satellite of the Longs Peak batholith, forms sills and essentially concordant multiple intrusions in quartz-mica schist that dips southward at moderate to steep angles. A great number of pegmatites accompanied and followed the intrusion of the sills, and formed concordant and discordant bodies in schist and granite.</p>\n<br/>\n<p>Over 1,300 pegmatites in the Hyatt area north of the Big Thompson River are mapped and individually described. There are 27 pegmatites in the area that are made up of a wall zone and a core, and one, the pegmatite at the Hyatt mine, is composed of five zones. The largest pegmatites in the area are discordant in schist and occupy zones that are interpreted to be tear faults and tension fractures produced by the successive intrusions of granite that formed multiple sills. The majority of pegmatites in the large multiple sills were emplaced along the foliation and fractures.</p>\n<br/>\n<p>The composition of 96 percent of the pegmatites is granitic, 3.5 percent are quartz-rich pegmatites, and a few are tourmaline-rich. The pegmatites were intruded over a period of time and probably were derived from a granitic magma at different stages during differentiation. Solutions escaping from many of the pegmatites tournalinized and silicified the wall rocks for a few inches to two feet, but chemical and spectrographic analyses fail to show the transport of any other constituents.</p>\n<br/>\n<p>Perthite, plagioclase, and quartz are the essential minerals of the pegmatites, and muscovite is a minor but widespread constituent. Tourmaline, garnet, beryl, and apatite are common accessory minerals, and lithiophillitite-triphylite, bismuthinite, uraninite, columbite-tantalite, and chrysoberyl are rare constituents. Beryl is found in 250 or 27 percent of the pegmatites and makes up 0.01 percent or more of 77 bodies. The beryl-bearing pegmatites are richest in two of the three large granite masses, and are somewhat less rich at a distance of more than a thousand feet from the margins of the intrusives, but contain the least beryl in the thousand-foot belt immediately surrounding the intrusives. The Hyatt pegmatite is by far the richest deposit of beryl in the area mapped.</p>\n<br/>\n<p>Most of the pegmatites mapped are \"unzoned\" or homogeneous pegmatites. All gradations are visible between bodies consisting of uniform texture and mineral distribution to zoned pegmatites. The interpretation is made that, for most pegmatites, the initial composition determines whether or not zones will form. Pegmatites containing many zones can form from a magma composed of the elements in perthite, plagioclase, quartz, and muscovite, depending on the proportions of the components crystallizing at any given time. The complexly zoned deposits depend for their formation on the presence of a number of the rarer elements, principally lithium. Replacement textures in zones result from the interaction of the rest-liquid with the earlier-formed solid crystals. No mappable pegmatite in the Crystal Mountain district formed from the replacement of pre-existing pegmatite by solutions escaping from the rest-liquid, or by solutions originating outside the pegmatite.</p>\n<br/>\n<p>Three beryl-bearing zoned pegmatites, the Hyatt, Big Boulder, and Buckhorn Mica deposits, were explored by core drilling. Each deposit is mapped and described in detail, and the mineral reserves evaluated. The exploration indicates a total of 2,000 tons of beryl, of which 480 tons is estimated to be recoverable by hand sorting. The mapping of the 3 3/4-square mile Hyatt area indicates beryl in sufficient abundance to infer beryl resources of an additional 1,150 tons.</p>\n<br/>\n<p>Small tonnages of scrap mica and perthite may be obtained from the Hyatt and Big Boulder prospects, and columbite-tantalite may occur in sufficient amounts at the Buckhorn Mica mine and Tantalum claim to produce several hundred pounds as a byproduct of beryl mining. Dumps at the various deposits contain 25 to 50 tons of beryl.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei139","usgsCitation":"Thurston, W.R., 1952, Pegmatites of the Crystal Mountain district, Larimer County, Colorado: U.S. Geological Survey Trace Elements Investigations 139, 167 p., https://doi.org/10.3133/tei139.","productDescription":"167 p.","numberOfPages":"168","costCenters":[],"links":[{"id":289925,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":289924,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0139/report.pdf"}],"country":"United States","state":"Colorado","county":"Larimer County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.1954,40.2578 ], [ -106.1954,40.9984 ], [ -104.9431,40.9984 ], [ -104.9431,40.2578 ], [ -106.1954,40.2578 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53aa9dfae4b065055fab1674","contributors":{"authors":[{"text":"Thurston, William R.","contributorId":9712,"corporation":false,"usgs":true,"family":"Thurston","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":283846,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70048319,"text":"tem415 - 1952 - Dinne Mesa NW, preliminary geologic map of part of the Carrizo Mountains area, northeastern Arizona","interactions":[],"lastModifiedDate":"2014-02-28T14:48:53","indexId":"tem415","displayToPublicDate":"1955-01-01T11:11:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"415","title":"Dinne Mesa NW, preliminary geologic map of part of the Carrizo Mountains area, northeastern Arizona","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem415","usgsCitation":"Strobell, J., 1952, Dinne Mesa NW, preliminary geologic map of part of the Carrizo Mountains area, northeastern Arizona: U.S. Geological Survey Trace Elements Memorandum 415, Report: 2 p.; 1 Plate: 31.06 x 37.86 inches, https://doi.org/10.3133/tem415.","productDescription":"Report: 2 p.; 1 Plate: 31.06 x 37.86 inches","numberOfPages":"2","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":277960,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0415/report-thumb.jpg"},{"id":283124,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0415/report.pdf"},{"id":283123,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0415/plate-1.pdf"}],"scale":"20000","country":"United States","state":"Arizona","otherGeospatial":"Carrizo Mountains","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.5,36.875 ], [ -109.5,37.0 ], [ -109.375,37.0 ], [ -109.375,36.875 ], [ -109.5,36.875 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"523d6e60e4b097188d6c76aa","contributors":{"authors":[{"text":"Strobell, J.D. Jr.","contributorId":22823,"corporation":false,"usgs":true,"family":"Strobell","given":"J.D.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":484312,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71250,"text":"tei183 - 1952 - Stratigraphic sections of the Phosphoria formation in Idaho, 1947-48, Part I","interactions":[],"lastModifiedDate":"2014-06-18T10:58:16","indexId":"tei183","displayToPublicDate":"1953-01-01T14:11:01","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"183","title":"Stratigraphic sections of the Phosphoria formation in Idaho, 1947-48, Part I","docAbstract":"<p>The Permian Phosphoria formation of the western states contains one of the world's largest reserves of phosphate. Although previous investigations (see especially Mansfield, 1927), including reconnaissance geologic mapping and sampling, established the location of most of the important deposits and their quality of scattered localities, they were not sufficiently detailed to permit a comparison of the merits of individual deposits or an appraisal of the reserves of phosphate rock that might be available under present economic conditions. Because the growing importance of the western phosphate deposits requires a better, more detailed understanding of their distribution and quality, the Geological Survey began in 1947 a comprehensive investigation, including (1) reconnaissance geologic mapping, mostly in Montana, of areas in which the Phosphoria formation could occur but where it had not previously been looked for or found; (2) geologic mapping, mostly in Montana, at a scale no smaller than 1:62,500, of several areas known to contain the Phosphoria formation but not previously mapped except in reconnaissance fashion; (3) geologic and topographic mapping, at a scale of 1:12,000, of some of the richest, thickest, and most accessible deposits; (4) measuring, describing, and sampling all beds of the phosphatic and shaly parts, and in some places the full thickness, of the Phosphoria formation and its stratigraphic equivalents at one or two localities per township over the entire field; (5) chemical and spectrographic analysis of the samples for phosphate, fluorine, minor metals, oil, and rock-forming constituents; and (6) petrologic and geochemical studies of the rocks and minerals of the formation.</p>\n<br/>\n<p>These studies are designed to define the regional and local geologic structures in which the phosphate bed lie, to provide a basis for the estimation of reserves of the inferred class over the entire region, and to determine the origin of the rocks and the elements contained in them. The data collected are not of the detail required to plan actual mining operations, but it is hoped they will guide industry in the selection of individual deposits worthy of further exploration.</p>\n<br/>\n<p>Most of the field work contemplated as a part of this investigation is now completed. Although the data will not be compiled or published in final form for some years to come, segments of the data, accompanied by little or no interpretation, will be published as preliminary maps or reports as they are assembled. The present report is the first of a series presenting in abbreviated form the description and analyses of the beds measured and sampled at various localities in southeastern Idaho (pl. 1). Companion reports presenting segments of the data from Montana, Wyoming, and Utah (Swanson and others, 1952, and McKelvey and others, 1952a and 1952b) are being released at the same time as this report, and others are in preparation.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei183","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"McKelvey, V.E., Davidson, D., O’Malley, F.W., Smith, L., Armstrong, F., and Sheldon, R., 1952, Stratigraphic sections of the Phosphoria formation in Idaho, 1947-48, Part I: U.S. Geological Survey Trace Elements Investigations 183, 53 p., https://doi.org/10.3133/tei183.","productDescription":"53 p.","numberOfPages":"54","costCenters":[],"links":[{"id":288792,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":288791,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0183/report.pdf"}],"country":"United States","state":"Idaho","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -113.3075,41.9922 ], [ -113.3075,44.9065 ], [ -111.0333,44.9065 ], [ -111.0333,41.9922 ], [ -113.3075,41.9922 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ae783be4b0abf75cf2ced2","contributors":{"authors":[{"text":"McKelvey, Vincent Ellis","contributorId":92650,"corporation":false,"usgs":true,"family":"McKelvey","given":"Vincent","email":"","middleInitial":"Ellis","affiliations":[],"preferred":false,"id":283875,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davidson, D.F.","contributorId":68293,"corporation":false,"usgs":true,"family":"Davidson","given":"D.F.","email":"","affiliations":[],"preferred":false,"id":283873,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"O’Malley, F. W.","contributorId":98707,"corporation":false,"usgs":true,"family":"O’Malley","given":"F.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":283876,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smith, L.E.","contributorId":102059,"corporation":false,"usgs":true,"family":"Smith","given":"L.E.","email":"","affiliations":[],"preferred":false,"id":283877,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Armstrong, F.C.","contributorId":32140,"corporation":false,"usgs":true,"family":"Armstrong","given":"F.C.","email":"","affiliations":[],"preferred":false,"id":283872,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Sheldon, R.P.","contributorId":71158,"corporation":false,"usgs":true,"family":"Sheldon","given":"R.P.","email":"","affiliations":[],"preferred":false,"id":283874,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70210467,"text":"70210467 - 1952 - Progress report on photogeologic studies in the Chandler River area","interactions":[],"lastModifiedDate":"2022-05-27T18:19:36.055643","indexId":"70210467","displayToPublicDate":"1952-12-31T16:23:05","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":5963,"text":"Geological Investigations, Naval Petroleum Reserve No. 4, Alaska","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"32","subseriesTitle":"Special Report","title":"Progress report on photogeologic studies in the Chandler River area","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70210467","usgsCitation":"Brosge, W., and Reiser, H.N., 1952, Progress report on photogeologic studies in the Chandler River area: Geological Investigations, Naval Petroleum Reserve No. 4, Alaska 32, Report: 3 p.; 1 Plate: 45.70 x 12.00 inches, https://doi.org/10.3133/70210467.","productDescription":"Report: 3 p.; 1 Plate: 45.70 x 12.00 inches","costCenters":[],"links":[{"id":396730,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70210467/report-thumb.jpg"},{"id":375337,"rank":1,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74632.htm","linkFileType":{"id":5,"text":"html"}},{"id":401307,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70210467/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":401306,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70210467/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Chandler River area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -152.3264,\n              68.9067\n            ],\n            [\n              -151,\n              68.9067\n            ],\n            [\n              -151,\n              69\n            ],\n            [\n              -152.3264,\n              69\n            ],\n            [\n              -152.3264,\n              68.9067\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Brosge, W. P.","contributorId":58248,"corporation":false,"usgs":true,"family":"Brosge","given":"W. P.","affiliations":[],"preferred":false,"id":837178,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reiser, Hillard N.","contributorId":189303,"corporation":false,"usgs":true,"family":"Reiser","given":"Hillard","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":837179,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70207237,"text":"70207237 - 1952 - Foraminifera in glacial till from Northeastern Montana","interactions":[],"lastModifiedDate":"2019-12-13T07:58:08","indexId":"70207237","displayToPublicDate":"1952-12-31T14:44:21","publicationYear":"1952","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Foraminifera in glacial till from Northeastern Montana","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1952)63[881:FIGTFN]2.0.CO;2","issn":"00167606","usgsCitation":"Kaye, C., 1952, Foraminifera in glacial till from Northeastern Montana: Geological Society of America Bulletin, v. 63, no. 8, 881, 1 p., https://doi.org/10.1130/0016-7606(1952)63[881:FIGTFN]2.0.CO;2.","productDescription":"881, 1 p.","costCenters":[],"links":[{"id":370239,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Montana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.5,\n              48.96579381461063\n            ],\n            [\n              -110.0390625,\n              46.89023157359399\n            ],\n            [\n              -104.04052734375,\n              45.767522962149876\n            ],\n            [\n              -104.08447265624999,\n              48.951366470947725\n            ],\n            [\n              -112.5,\n              48.96579381461063\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"63","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Kaye, Clifford A.","contributorId":17624,"corporation":false,"usgs":true,"family":"Kaye","given":"Clifford A.","affiliations":[],"preferred":false,"id":777430,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221562,"text":"70221562 - 1952 - Sedimentary volumes in Gulf Coastal Plain of the United States And Mexico: Part I: Volume of Mesozoic Sediments In Florida and Georgia","interactions":[],"lastModifiedDate":"2021-06-22T14:59:40.78571","indexId":"70221562","displayToPublicDate":"1952-12-01T09:54:32","publicationYear":"1952","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Sedimentary volumes in Gulf Coastal Plain of the United States And Mexico: Part I: Volume of Mesozoic Sediments In Florida and Georgia","docAbstract":"<p><span>Mesozoic sedimentary rocks are present throughout Florida and the Coastal Plain of Georgia, but chiefly in the subsurface in an area of approximately 93,500 square miles. The Mesozoic rocks in this area belong, for the most part, to the Gulf and Comanche series of the Cretaceous system. Rocks tentatively classified as part Jurassic and part Triassic underlie the Comanche series in parts of Florida and Georgia. In the northern part of the Georgia Coastal Plain, an irregular outcrop belt of sandstone and shale belonging to the early Upper Cretaceous Tuscaloosa formation borders on the south the crystalline rocks of the Piedmont. Southward from its outcrop in western Georgia, the Tuscaloosa formation dips under roughly parallel belts of the progressively younger Eutaw formation and formations equivalent to the Selma group of the Gulf series. In central and eastern Georgia, the Eutaw formation and formations equivalent to the Selma group are covered by overlaps of Tertiary formations. Conclusions in regard to the stratigraphy, structure, and thickness of the Mesozoic rocks are based largely on interpretations of the records of approximately 200 oil test wells. The total volume of the Mesozoic rocks in Florida and southern Georgia is estimated at 60,000 to 75,000 cubic miles.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1952)63[1159:SVIGCP]2.0.CO;2","usgsCitation":"Applin, P.L., 1952, Sedimentary volumes in Gulf Coastal Plain of the United States And Mexico: Part I: Volume of Mesozoic Sediments In Florida and Georgia: Geological Society of America Bulletin, v. 63, no. 12, p. 1159-1164, https://doi.org/10.1130/0016-7606(1952)63[1159:SVIGCP]2.0.CO;2.","productDescription":"6 p.","startPage":"1159","endPage":"1164","costCenters":[],"links":[{"id":386655,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Florida, Georgia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -85.62744140625,\n              34.994003757575776\n            ],\n            [\n              -85.078125,\n              31.728167146023935\n            ],\n            [\n              -85.01220703125,\n              31.034108344903512\n            ],\n            [\n              -87.60498046875,\n              31.015278981711266\n            ],\n            [\n              -87.4072265625,\n              30.751277776257812\n            ],\n            [\n              -87.4072265625,\n              30.315987718557867\n            ],\n            [\n              -85.10009765625,\n              29.611670115197377\n            ],\n            [\n              -82.9248046875,\n              27.839076094777816\n            ],\n            [\n              -81.34277343749999,\n              25.085598897064752\n            ],\n            [\n              -80.17822265625,\n              24.926294766395593\n            ],\n            [\n              -79.87060546875,\n              26.64745870265938\n            ],\n            [\n              -81.5185546875,\n              30.524413269923986\n            ],\n            [\n              -80.96923828125,\n              32.045332838858506\n            ],\n            [\n              -81.93603515625,\n              33.32134852669881\n            ],\n            [\n              -82.94677734375,\n              35.0120020431607\n            ],\n            [\n              -85.62744140625,\n              34.994003757575776\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"63","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Applin, Paul Livingston","contributorId":29404,"corporation":false,"usgs":true,"family":"Applin","given":"Paul","email":"","middleInitial":"Livingston","affiliations":[],"preferred":false,"id":818055,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221561,"text":"70221561 - 1952 - Deformation, metamorphism, and mineralization in gypsum-anhydrite cap rock","interactions":[],"lastModifiedDate":"2021-06-23T12:53:45.701859","indexId":"70221561","displayToPublicDate":"1952-12-01T09:39:04","publicationYear":"1952","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2711,"text":"Memoir of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Deformation, metamorphism, and mineralization in gypsum-anhydrite cap rock","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/MEM50-p1","usgsCitation":"Goldman, M., 1952, Deformation, metamorphism, and mineralization in gypsum-anhydrite cap rock: Memoir of the Geological Society of America, v. 50, no. 1, 163 p., https://doi.org/10.1130/MEM50-p1.","productDescription":"163 p.","costCenters":[],"links":[{"id":386654,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"50","issue":"1","noUsgsAuthors":false,"publicationDate":"1952-01-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Goldman, M.I.","contributorId":6028,"corporation":false,"usgs":true,"family":"Goldman","given":"M.I.","email":"","affiliations":[],"preferred":false,"id":818054,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221611,"text":"70221611 - 1952 - Magmatic differentiation in tertiary and quaternary volcanic rocks from Adak and Kanaga Islands, Aleutian Islands, Alaska","interactions":[],"lastModifiedDate":"2021-06-25T13:47:20.593876","indexId":"70221611","displayToPublicDate":"1952-12-01T08:40:41","publicationYear":"1952","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Magmatic differentiation in tertiary and quaternary volcanic rocks from Adak and Kanaga Islands, Aleutian Islands, Alaska","docAbstract":"<p><span>Samples of 17&nbsp;</span>volcanic<span>&nbsp;</span>rocks<span>&nbsp;of&nbsp;</span>Tertiary<span>&nbsp;and&nbsp;</span>Quaternary<span>&nbsp;age from&nbsp;</span>Adak<span>&nbsp;and&nbsp;</span>Kanaga<span>&nbsp;</span>islands<span>&nbsp;have been chemically analyzed and studied microscopically. Spectrograms have been made of 10 of them. The&nbsp;</span>rocks<span>&nbsp;from&nbsp;</span>Adak<span>&nbsp;represent one center of possibly older&nbsp;</span>Tertiary<span>&nbsp;age and two centers of younger&nbsp;</span>Tertiary<span>&nbsp;or&nbsp;</span>Quaternary<span>&nbsp;age. The&nbsp;</span>rocks<span>&nbsp;from&nbsp;</span>Kanaga<span>&nbsp;</span>Island<span>&nbsp;represent both a shield volcano of possibly&nbsp;</span>Tertiary<span>&nbsp;age, partly destroyed by the formation of a caldera, and a young cone of&nbsp;</span>Quaternary<span>&nbsp;age that has grown within the caldera. All the&nbsp;</span>rocks<span>&nbsp;are basalt or andesite. Modally, all are characterized by relatively large crystals of plagioclase more calcic than andesine, and by one or more of the following ferromagnesian minerals: olivine, hypersthene, augite, and hornblende. Apatite and iron ores are common, and late silica minerals and orthoclase occur interstitially&nbsp;</span>in<span>&nbsp;the groundmasses of some&nbsp;</span>rocks<span>. As analyses of no more than four samples are available for each center, the small differences between sets of analyses representing different centers are of doubtful significance. Consequently, the analyses representing all the centers have been plotted on each of the several diagrams used. The several types of variation diagrams show that the province is a calc-alkaline one. The alkali-lime index is&nbsp;</span>in<span>&nbsp;the neighborhood of 63. This very high value is comparable with that for Katmai and is only slightly less than the maximum for the Japanese&nbsp;</span>volcanic<span>&nbsp;</span>rock<span>&nbsp;series. The quantities of minor constituents present are not exceptional for the&nbsp;</span>rock<span>&nbsp;types analyzed; the&nbsp;</span>rocks<span>&nbsp;from&nbsp;</span>Adak<span>&nbsp;are apparently more strontium-rich than those from&nbsp;</span>Kanaga<span>. The chemical analyses of the more basic&nbsp;</span>rock<span>&nbsp;types, as compared with the average analysis of plateau basalt, suggest that the&nbsp;</span>Aleutian<span>&nbsp;parental magma could have been derived from a plateau basalt magma by the addition of plagioclase and the subtraction of pyroxene, iron ore, and some quartz. The distribution of the minor elements can be explained more easily by postulating that, at least on&nbsp;</span>Kanaga<span>&nbsp;</span>Island<span>, some sediments have been assimilated. The derivation of the analyzed&nbsp;</span>rocks<span>&nbsp;from the&nbsp;</span>Aleutian<span>&nbsp;parental magma is most easily explained by the hypothesis that the plagioclase remained&nbsp;</span>in<span>&nbsp;suspension while the ferromagnesian minerals were settling out.&nbsp;</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1952)63[485:MDITAQ]2.0.CO;2","usgsCitation":"Coats, R.R., 1952, Magmatic differentiation in tertiary and quaternary volcanic rocks from Adak and Kanaga Islands, Aleutian Islands, Alaska: Geological Society of America Bulletin, v. 63, no. 5, p. 485-514, https://doi.org/10.1130/0016-7606(1952)63[485:MDITAQ]2.0.CO;2.","productDescription":"30 p.","startPage":"485","endPage":"514","costCenters":[],"links":[{"id":386736,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Alaska","otherGeospatial":"Aleutian Islands","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -157.1484375,\n              58.95000823335702\n            ],\n            [\n              -169.3212890625,\n              54.49556752187406\n            ],\n            [\n              -182.1533203125,\n              52.482780222078226\n            ],\n            [\n              -187.470703125,\n              53.61857936489517\n            ],\n            [\n              -193.9306640625,\n              55.89995614406812\n            ],\n            [\n              -194.4580078125,\n              55.00282580979323\n            ],\n            [\n              -180.17578125,\n              50.28933925329178\n            ],\n            [\n              -162.59765625,\n              53.199451902831555\n            ],\n            [\n              -156.2255859375,\n              56.389583525613055\n            ],\n            [\n              -157.1484375,\n              58.95000823335702\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"63","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Coats, Robert R.","contributorId":37788,"corporation":false,"usgs":true,"family":"Coats","given":"Robert","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":818262,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221610,"text":"70221610 - 1952 - Late quaternary geology and frost phenomena along Alaska Highway, Northern British Columbia and Southeastern Yukon","interactions":[],"lastModifiedDate":"2021-06-25T13:34:53.224712","indexId":"70221610","displayToPublicDate":"1952-12-01T08:30:32","publicationYear":"1952","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Late quaternary geology and frost phenomena along Alaska Highway, Northern British Columbia and Southeastern Yukon","docAbstract":"<p><span>Reconnaissance field work&nbsp;</span>along<span>&nbsp;the&nbsp;</span>Alaska<span>&nbsp;</span>Highway<span>&nbsp;in&nbsp;</span>northern<span>&nbsp;</span>British<span>&nbsp;</span>Columbia<span>&nbsp;and&nbsp;</span>southeastern<span>&nbsp;</span>Yukon<span>&nbsp;furnishes preliminary data on the later&nbsp;</span>Quaternary<span>&nbsp;history of the region, and on the processes and results of intensive&nbsp;</span>frost<span>&nbsp;action. Extensive erosion surfaces were developed prior to glaciation, such as the Alberta Plateau of northeastern&nbsp;</span>British<span>&nbsp;</span>Columbia<span>&nbsp;and the&nbsp;</span>Yukon<span>&nbsp;Plateau in southern&nbsp;</span>Yukon<span>. In the region from Dawson Creek to Fort Nelson,&nbsp;</span>British<span>&nbsp;</span>Columbia<span>, the drift is dominantly a slightly weathered bouldery clay till of Wisconsin age, deposited by ice that came from the east. In the&nbsp;</span>northern<span>&nbsp;Rocky Mountains, the last eastward advance of the Wisconsin glaciers to the mountain front preceded the maximum westward advance of the ice sheets. In the foothills belt west of the&nbsp;</span>Highway<span>, the tills of these two advances are separated by lake deposits. Much of the drift is probably pre-Altamont in age and was subjected to vigorous&nbsp;</span>frost<span>&nbsp;action during the Altamont substage. The climate ameliorated perhaps with the advent of the post-glacial optimum and possibly coincident with the development of prairies. A recent change from prairie to forest perhaps indicates a slight cooling in recent time. In the&nbsp;</span>northern<span>&nbsp;Rocky Mountains, four substages of Wisconsin glaciation are recognized tentatively on the basis of morainal deposits and outwash terraces. The upper Liard basin is characterized by extensive pitted outwash plains, probably of&nbsp;</span>late<span>&nbsp;Wisconsin age. From Teslin Lake to Whitehorse, the&nbsp;</span>Highway<span>&nbsp;is bordered by extensive terraces of gravel and sand deposited in ice-marginal streams and lakes. Intensive&nbsp;</span>frost<span>&nbsp;action has modified pre-existing land forms and has produced a wide variety of features, such as talus, blockfields, stone rings, stone stripes, and terraces. Long smooth slopes, chiefly due to mass movements such as solifluction, are characteristic of the landscapes. These slopes and ancient soil structures extend down into forested areas and probably developed prior to the advent of forests, doubtless prior to the post-glacial optimum.&nbsp;</span>Phenomena<span>&nbsp;resulting from intensive&nbsp;</span>frost<span>&nbsp;action at the present time are restricted largely to areas above timber line.&nbsp;</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1952)63[883:LQGAFP]2.0.CO;2","usgsCitation":"Denny, C.S., 1952, Late quaternary geology and frost phenomena along Alaska Highway, Northern British Columbia and Southeastern Yukon: Geological Society of America Bulletin, v. 63, no. 9, p. 883-922, https://doi.org/10.1130/0016-7606(1952)63[883:LQGAFP]2.0.CO;2.","productDescription":"40 p.","startPage":"883","endPage":"922","costCenters":[],"links":[{"id":386735,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States, Canada","state":"Alaska, Yukon, British Columbia","otherGeospatial":"Alaska Highway","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -139.04296875,\n              61.95961583829658\n            ],\n            [\n              -144.404296875,\n              63.58767529470318\n            ],\n            [\n              -147.5244140625,\n              60.951776809566965\n            ],\n            [\n              -143.7451171875,\n              59.977005492196\n            ],\n            [\n              -135.2197265625,\n              56.559482483762245\n            ],\n            [\n              -131.9677734375,\n              54.67383096593114\n            ],\n            [\n              -129.1552734375,\n              57.040729838360875\n            ],\n            [\n              -128.5400390625,\n              58.401711667608\n            ],\n            [\n              -139.04296875,\n              61.95961583829658\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"63","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Denny, Charles Storrow","contributorId":86331,"corporation":false,"usgs":true,"family":"Denny","given":"Charles","email":"","middleInitial":"Storrow","affiliations":[],"preferred":false,"id":818261,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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