{"pageNumber":"5042","pageRowStart":"126025","pageSize":"25","recordCount":165579,"records":[{"id":61833,"text":"gq1537 - 1980 - Geologic map of the Birdseye Pass quadrangle, showing chromolithofacies and coal beds in the Wind River Formation, Fremont and Hot Springs Counties, Wyoming","interactions":[{"subject":{"id":42515,"text":"ofr76346 - 1976 - Preliminary map of the Birdseye Pass Quadrangle, Fremont and Hot Springs counties, Wyoming","indexId":"ofr76346","publicationYear":"1976","noYear":false,"title":"Preliminary map of the Birdseye Pass Quadrangle, Fremont and Hot Springs counties, Wyoming"},"predicate":"SUPERSEDED_BY","object":{"id":61833,"text":"gq1537 - 1980 - Geologic map of the Birdseye Pass quadrangle, showing chromolithofacies and coal beds in the Wind River Formation, Fremont and Hot Springs Counties, Wyoming","indexId":"gq1537","publicationYear":"1980","noYear":false,"title":"Geologic map of the Birdseye Pass quadrangle, showing chromolithofacies and coal beds in the Wind River Formation, Fremont and Hot Springs Counties, Wyoming"},"id":1}],"lastModifiedDate":"2012-02-10T00:10:31","indexId":"gq1537","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1537","title":"Geologic map of the Birdseye Pass quadrangle, showing chromolithofacies and coal beds in the Wind River Formation, Fremont and Hot Springs Counties, Wyoming","language":"ENGLISH","doi":"10.3133/gq1537","usgsCitation":"Thaden, R.E., 1980, Geologic map of the Birdseye Pass quadrangle, showing chromolithofacies and coal beds in the Wind River Formation, Fremont and Hot Springs Counties, Wyoming: U.S. Geological Survey Geologic Quadrangle 1537, 1 map :col. ;58 x 43 cm. on sheet 82 x 102 cm., https://doi.org/10.3133/gq1537.","productDescription":"1 map :col. ;58 x 43 cm. on sheet 82 x 102 cm.","costCenters":[],"links":[{"id":102634,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1083.htm","linkFileType":{"id":5,"text":"html"},"description":"1083"},{"id":248124,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1537/report.pdf","size":"78","linkFileType":{"id":1,"text":"pdf"}},{"id":252867,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1537/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.11749999999999,43.3675 ], [ -108.11749999999999,43.5 ], [ -108,43.5 ], [ -108,43.3675 ], [ -108.11749999999999,43.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0de4b07f02db69f26d","contributors":{"authors":[{"text":"Thaden, Robert E.","contributorId":75502,"corporation":false,"usgs":true,"family":"Thaden","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":266426,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":35569,"text":"b1513 - 1980 - Sapphirine in Precambrian rocks associated with stratabound sulfide deposits, Custer County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:09:34","indexId":"b1513","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1513","title":"Sapphirine in Precambrian rocks associated with stratabound sulfide deposits, Custer County, Colorado","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1513","usgsCitation":"Raymond, W.H., Leiggi, P.A., and Sheridan, D.M., 1980, Sapphirine in Precambrian rocks associated with stratabound sulfide deposits, Custer County, Colorado: U.S. Geological Survey Bulletin 1513, 22 p. maps ; 23 cm., https://doi.org/10.3133/b1513.","productDescription":"22 p. maps ; 23 cm.","costCenters":[],"links":[{"id":166905,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1513/report-thumb.jpg"},{"id":63472,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1513/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c006","contributors":{"authors":[{"text":"Raymond, William H.","contributorId":48555,"corporation":false,"usgs":true,"family":"Raymond","given":"William","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":214868,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leiggi, Peter A.","contributorId":6513,"corporation":false,"usgs":true,"family":"Leiggi","given":"Peter","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":214866,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sheridan, Douglas M.","contributorId":13966,"corporation":false,"usgs":true,"family":"Sheridan","given":"Douglas","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":214867,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":35351,"text":"b1447 - 1980 - Geology and mineral resources of the North Absaroka Wilderness and vicinity, Park County, Wyoming, with sections on mineralization of the Sunlight mining region and geology and mineralization of the Cooke City mining district, and a section on aeromagnetic interpretation","interactions":[],"lastModifiedDate":"2022-06-06T21:03:19.525953","indexId":"b1447","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1447","title":"Geology and mineral resources of the North Absaroka Wilderness and vicinity, Park County, Wyoming, with sections on mineralization of the Sunlight mining region and geology and mineralization of the Cooke City mining district, and a section on aeromagnetic interpretation","docAbstract":"SUMMARY\r\n\r\nThe North Absaroka Wilderness is approximately 560 square miles (1,450 km 2 ) of rugged scenic mountainous terrain that adjoins the eastern boundary of Yellowstone National Park in northwestern Wyoming. The area was studied during 1970, 1971, and 1972 by personnel of the U. S. Geological Survey and the U. S. Bureau of Mines to evaluate its mineral-resource potential as required by the Wilderness Act of 1964. This evaluation is based on a search of the literature courthouse and production records, geologic field mapping, field inspection of claims and prospects, analyses of bedrock and stream-sediment samples, and an aeromagnetic survey.\r\n\r\nThe North Absaroka Wilderness is underlain almost entirely by andesitic and basaltic volcanic rocks of Eocene age. These volcanics rest on deformed sedimentary rocks of Paleozoic and, locally, of Mesozoic age that are exposed at places along the northern and eastern edges of the wilderness. Dikes and other igneous intrusive bodies cut both the volcanic and sedimentary rocks. A nearly flat detachment fault, the Heart Mountain fault, and a related steep break-away fault have displaced middle and upper Paleozoic rocks and some of the older part of the volcanic sequence to the southeast. A much greater thickness of volcanic rocks was found to be involved in Heart Mountain faulting than had previously been recognized; however, most of the volcanic rocks and many of the intrusives were emplaced after Heart Mountain faulting. Local folding and high-angle faulting in mid-Eocene time have deformed all but the youngest part of the volcanic sequence in the southeastern part of the wilderness. This deformation is interpreted as the last pulse of Laramide orogeny.\r\n\r\nThe results of this study indicate that the mineral-resource potential of the wilderness is minimal. Bentonite, petroleum, low-quality coal, and localized deposits of uranium and chromite have been produced in the surrounding region from rocks that underlie the volcanic rocks; but such deposits, if present in the wilderness, would be too deeply buried, too small, or too sporadically distributed to be profitably located and exploited. Copper and gold mines and prospects are present on the fringes of the wilderness, but otherwise the area seems to be devoid of economically valuable concentrations of metallic minerals. No surface evidence of geothermal-energy potential was found.\r\n\r\nKnown mineral deposits in the vicinity of the North Absaroka Wilderness are associated with intrusive rocks. From the Cooke City mining district, just north of the wilderness, replacement deposits in Upper Cambrian carbonate rocks may extend a short distance into the north edge of the wilderness, In the Sunlight mining region, an enclave nearly surrounded by the wilderness, mineralization occurs in veins and is disseminated in volcanic and plutonic rocks. Richer concentrations of metallic minerals may occur in carbonate rocks adjacent to intrusive bodies at depth beneath the volcanic rocks in the Sunlight region. A few small intrusive bodies occur in the wilderness, but no significant associated mineralization was detected. Aeromagnetic data indicate that other intrusives not exposed by erosion may occur in the wilderness; however, no significant metamorphism or alteration is evident at the surface to indicate their presence.\r\n\r\nAlthough most of the rocks of the wilderness are of igneous origin, they are all so old (Eocene) that it is unlikely that they retain any original heat. The Pleistocene rhyolitic ash-flow tuffs in the southwestern part of the wilderness were erupted from sources in Yellowstone National Park just to the west; however, in the wilderness these tuffs are too thin to contain any residual heat.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1447","usgsCitation":"Nelson, W.H., Prostka, H.J., Williams, F.E., Elliott, J., and Peterson, D.L., 1980, Geology and mineral resources of the North Absaroka Wilderness and vicinity, Park County, Wyoming, with sections on mineralization of the Sunlight mining region and geology and mineralization of the Cooke City mining district, and a section on aeromagnetic interpretation: U.S. Geological Survey Bulletin 1447, Report: vii, 101 p.; 2 Plates: 32.50 × 23.50 inches and 28.00 × 24.00 inches, https://doi.org/10.3133/b1447.","productDescription":"Report: vii, 101 p.; 2 Plates: 32.50 × 23.50 inches and 28.00 × 24.00 inches","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":109036,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_19319.htm","linkFileType":{"id":5,"text":"html"},"description":"19319"},{"id":165505,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1447/report-thumb.jpg"},{"id":63212,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1447/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63211,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1447/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63210,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1447/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"125000","country":"United States","state":"Wyoming","county":"Park County","otherGeospatial":"North Absaroka Wilderness and vicinity","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.2,\n              44.45\n            ],\n            [\n              -109.267,\n              44.45\n            ],\n            [\n              -109.267,\n              45\n            ],\n            [\n              -110.2,\n              45\n            ],\n            [\n              -110.2,\n              44.45\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db68648a","contributors":{"authors":[{"text":"Nelson, Willis H.","contributorId":84777,"corporation":false,"usgs":true,"family":"Nelson","given":"Willis","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":214497,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Prostka, Harold J.","contributorId":52185,"corporation":false,"usgs":true,"family":"Prostka","given":"Harold","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":214495,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Williams, Frank E.","contributorId":72383,"corporation":false,"usgs":true,"family":"Williams","given":"Frank","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":214496,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Elliott, James E.","contributorId":15595,"corporation":false,"usgs":true,"family":"Elliott","given":"James E.","affiliations":[],"preferred":false,"id":214493,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Peterson, Donald L.","contributorId":28597,"corporation":false,"usgs":true,"family":"Peterson","given":"Donald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":214494,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":34711,"text":"b1482C - 1980 - The Togiak Basalt, a new formation in southwestern Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:09:37","indexId":"b1482C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1482","chapter":"C","title":"The Togiak Basalt, a new formation in southwestern Alaska","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1482C","usgsCitation":"Hoare, J.M., and Coonrad, W., 1980, The Togiak Basalt, a new formation in southwestern Alaska: U.S. Geological Survey Bulletin 1482, p. C1-C11 ill., maps ; 23 cm., https://doi.org/10.3133/b1482C.","productDescription":"p. C1-C11 ill., maps ; 23 cm.","costCenters":[],"links":[{"id":167816,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1482c/report-thumb.jpg"},{"id":62576,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1482c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db6737c2","contributors":{"authors":[{"text":"Hoare, Joseph McCormick","contributorId":6055,"corporation":false,"usgs":true,"family":"Hoare","given":"Joseph","email":"","middleInitial":"McCormick","affiliations":[],"preferred":false,"id":213449,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coonrad, W.J.","contributorId":77993,"corporation":false,"usgs":true,"family":"Coonrad","given":"W.J.","email":"","affiliations":[],"preferred":false,"id":213450,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":35733,"text":"b1460 - 1980 - The Marquette Range Supergroup in the Gogebic iron district, Michigan and Wisconsin","interactions":[],"lastModifiedDate":"2022-06-15T18:23:47.122584","indexId":"b1460","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1460","title":"The Marquette Range Supergroup in the Gogebic iron district, Michigan and Wisconsin","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1460","usgsCitation":"Schmidt, R.G., 1980, The Marquette Range Supergroup in the Gogebic iron district, Michigan and Wisconsin: U.S. Geological Survey Bulletin 1460, vi, 96 p, https://doi.org/10.3133/b1460.","productDescription":"vi, 96 p","costCenters":[],"links":[{"id":402219,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21558.htm"},{"id":63649,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1460/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":167549,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1460/report-thumb.jpg"}],"country":"United States","state":"Michigan, Wisconsin","otherGeospatial":"Gogebic iron district","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -90.867,\n              46.231\n            ],\n            [\n              -89.537,\n              46.231\n            ],\n            [\n              -89.537,\n              46.5\n            ],\n            [\n              -90.867,\n              46.5\n            ],\n            [\n              -90.867,\n              46.231\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b965","contributors":{"authors":[{"text":"Schmidt, Robert Gordon","contributorId":39355,"corporation":false,"usgs":true,"family":"Schmidt","given":"Robert","email":"","middleInitial":"Gordon","affiliations":[],"preferred":false,"id":215131,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":35007,"text":"b1474 - 1980 - Jasperoids of the Pando Area, Eagle County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:09:46","indexId":"b1474","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1474","title":"Jasperoids of the Pando Area, Eagle County, Colorado","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1474","usgsCitation":"Lovering, T., and Heyl, A.V., 1980, Jasperoids of the Pando Area, Eagle County, Colorado: U.S. Geological Survey Bulletin 1474, iv, 36 p. ill., maps ; 23 cm., https://doi.org/10.3133/b1474.","productDescription":"iv, 36 p. ill., maps ; 23 cm.","costCenters":[],"links":[{"id":96737,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1474/report.pdf","size":"3241","linkFileType":{"id":1,"text":"pdf"}},{"id":165491,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1474/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa6e4b07f02db6666f5","contributors":{"authors":[{"text":"Lovering, T.G.","contributorId":55014,"corporation":false,"usgs":true,"family":"Lovering","given":"T.G.","affiliations":[],"preferred":false,"id":213969,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Heyl, Allen Van","contributorId":91078,"corporation":false,"usgs":true,"family":"Heyl","given":"Allen","email":"","middleInitial":"Van","affiliations":[],"preferred":false,"id":213970,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":34195,"text":"b1368B - 1980 - Stratigraphy, structure, and economic geology of the Iliamna Quadrangle, Alaska","interactions":[{"subject":{"id":43374,"text":"ofr6872 - 1968 - Geology of the Iliamna quadrangle, Alaska","indexId":"ofr6872","publicationYear":"1968","noYear":false,"title":"Geology of the Iliamna quadrangle, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":34195,"text":"b1368B - 1980 - Stratigraphy, structure, and economic geology of the Iliamna Quadrangle, Alaska","indexId":"b1368B","publicationYear":"1980","noYear":false,"chapter":"B","title":"Stratigraphy, structure, and economic geology of the Iliamna Quadrangle, Alaska"},"id":1}],"lastModifiedDate":"2017-06-10T11:55:00","indexId":"b1368B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1368","chapter":"B","title":"Stratigraphy, structure, and economic geology of the Iliamna Quadrangle, Alaska","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/b1368B","usgsCitation":"Detterman, R.L., and Reed, B.L., 1980, Stratigraphy, structure, and economic geology of the Iliamna Quadrangle, Alaska: U.S. Geological Survey Bulletin 1368, v, 86 p. : ill., maps (1 fold. col. in pocket) ; 23 cm., https://doi.org/10.3133/b1368B.","productDescription":"v, 86 p. : ill., maps (1 fold. col. in pocket) ; 23 cm.","costCenters":[],"links":[{"id":62099,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1368b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":109710,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21470.htm","linkFileType":{"id":5,"text":"html"},"description":"21470"},{"id":164203,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1368b/report-thumb.jpg"},{"id":62098,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1368b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a5384","contributors":{"authors":[{"text":"Detterman, Robert L.","contributorId":71526,"corporation":false,"usgs":true,"family":"Detterman","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":212594,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reed, Bruce L.","contributorId":19928,"corporation":false,"usgs":true,"family":"Reed","given":"Bruce","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":212593,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":34269,"text":"b1477A - 1980 - Relation of the carbon/oxygen ratio in coal to igneous intrusions in the Somerset coal field, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:09:42","indexId":"b1477A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1477","chapter":"A","title":"Relation of the carbon/oxygen ratio in coal to igneous intrusions in the Somerset coal field, Colorado","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1477A","usgsCitation":"Dyni, J.R., and Gaskill, D.L., 1980, Relation of the carbon/oxygen ratio in coal to igneous intrusions in the Somerset coal field, Colorado: U.S. Geological Survey Bulletin 1477, iv, p. A1-A20, ill., maps (1 fold. in pocket) ; 23 cm., https://doi.org/10.3133/b1477A.","productDescription":"iv, p. A1-A20, ill., maps (1 fold. in pocket) ; 23 cm.","costCenters":[],"links":[{"id":166960,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1477a/report-thumb.jpg"},{"id":62173,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1477a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62174,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1477a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db634aa3","contributors":{"authors":[{"text":"Dyni, John R. jdyni@usgs.gov","contributorId":756,"corporation":false,"usgs":true,"family":"Dyni","given":"John","email":"jdyni@usgs.gov","middleInitial":"R.","affiliations":[],"preferred":true,"id":212713,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gaskill, David L.","contributorId":53369,"corporation":false,"usgs":true,"family":"Gaskill","given":"David","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":212714,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":35454,"text":"b1463 - 1980 - Mineral resources of the Indian Peaks Study Area, Boulder and Grand counties, Colorado, with a section on interpretation of aeromagnetic data","interactions":[{"subject":{"id":15357,"text":"ofr75500 - 1975 - Mineral resources of the Indian Peaks study area, Boulder and Grand Counties, Colorado","indexId":"ofr75500","publicationYear":"1975","noYear":false,"title":"Mineral resources of the Indian Peaks study area, Boulder and Grand Counties, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":35454,"text":"b1463 - 1980 - Mineral resources of the Indian Peaks Study Area, Boulder and Grand counties, Colorado, with a section on interpretation of aeromagnetic data","indexId":"b1463","publicationYear":"1980","noYear":false,"title":"Mineral resources of the Indian Peaks Study Area, Boulder and Grand counties, Colorado, with a section on interpretation of aeromagnetic data"},"id":1}],"lastModifiedDate":"2012-02-02T00:09:45","indexId":"b1463","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1463","title":"Mineral resources of the Indian Peaks Study Area, Boulder and Grand counties, Colorado, with a section on interpretation of aeromagnetic data","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1463","usgsCitation":"Pearson, R.C., and Johnson, G., 1980, Mineral resources of the Indian Peaks Study Area, Boulder and Grand counties, Colorado, with a section on interpretation of aeromagnetic data: U.S. Geological Survey Bulletin 1463, vii, 109 p.  ill., maps (2 fold. col. in pocket) ; 24 cm., https://doi.org/10.3133/b1463.","productDescription":"vii, 109 p.  ill., maps (2 fold. col. in pocket) ; 24 cm.","costCenters":[],"links":[{"id":96925,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1463/report.pdf","size":"8313","linkFileType":{"id":1,"text":"pdf"}},{"id":96926,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1463/plate-1.pdf","size":"8521","linkFileType":{"id":1,"text":"pdf"}},{"id":96927,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1463/plate-2.pdf","size":"7144","linkFileType":{"id":1,"text":"pdf"}},{"id":167233,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1463/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a289","contributors":{"authors":[{"text":"Pearson, Robert Carl","contributorId":50876,"corporation":false,"usgs":true,"family":"Pearson","given":"Robert","email":"","middleInitial":"Carl","affiliations":[],"preferred":false,"id":214670,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, Gordon","contributorId":73872,"corporation":false,"usgs":true,"family":"Johnson","given":"Gordon","affiliations":[],"preferred":false,"id":214671,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":35225,"text":"b1503 - 1980 - Potential hazards from future eruptions in the vicinity of Mount Shasta Volcano, Northern California","interactions":[{"subject":{"id":10325,"text":"ofr78827 - 1978 - Potential hazards from future eruptions in the vicinity of Mount Shasta Volcano, northern California","indexId":"ofr78827","publicationYear":"1978","noYear":false,"title":"Potential hazards from future eruptions in the vicinity of Mount Shasta Volcano, northern California"},"predicate":"SUPERSEDED_BY","object":{"id":35225,"text":"b1503 - 1980 - Potential hazards from future eruptions in the vicinity of Mount Shasta Volcano, Northern California","indexId":"b1503","publicationYear":"1980","noYear":false,"title":"Potential hazards from future eruptions in the vicinity of Mount Shasta Volcano, Northern California"},"id":1}],"lastModifiedDate":"2017-02-09T13:00:04","indexId":"b1503","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1503","title":"Potential hazards from future eruptions in the vicinity of Mount Shasta Volcano, Northern California","docAbstract":"Mount Shasta has erupted, on the average, at least once per 800 years during the last 10,000 years, and about once per 600 years during the last 4,500 years. The last known eruption occurred about 200 radiocarbon years ago. Eruptions during the last 10,000 years produced lava flows and domes on and around the flanks of Mount Shasta, and pyroclastic flows from summit and flank vents extended as far as 20 kilometers from the summit. Most of these eruptions also produced large mudflows, many of which reached more than several tens of kilometers from Mount Shasta. Future eruptions like those of the past could endanger the communities of Weed, Mount Shasta, McCloud, and Dunsmuir, located at or near the base of Mount Shasta. Such eruptions will most likely produce deposits of lithic ash, lava flows, domes, and pyroclastic flows. Lava flows and pyroclastic flows may affect low-and flat-lying ground almost anywhere within about 20 kilometers of the summit of Mount Shasta, and mudflows may cover valley floors and other low areas as much as several tens of kilometers from the volcano. On the basis of its past behavior, Mount Shasta is not likely to erupt large volumes of pumiceous ash in the future; areas subject to the greatest risk from air-fall tephra are located mainly east and within about 50 kilometers of the summit of the volcano. 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,{"id":36069,"text":"b1493 - 1980 - The geologic story of the Great Plains","interactions":[],"lastModifiedDate":"2018-04-02T15:23:51","indexId":"b1493","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1493","title":"The geologic story of the Great Plains","docAbstract":"<p>The Great Plains! The words alone create a sense of space and a feeling of destiny a challenge. But what exactly is this special part of Western America that contains so much of our history? How did it come to be? Why is it different?</p>\n<p>Geographically, the Great Plains is an immense sweep of country; it reaches from Mexico far north into Canada and spreads out east of the Rocky Mountains like a huge welcome mat. So often maligned as a drab, featureless area, the Great Plains is in fact a land of marked contrasts and limitless variety: canyons carved into solid rock of an arid land by the waters of the Pecos and the Rio Grande; the seemingly endless grainfields of Kansas; the desolation of the Badlands; the beauty of the Black Hills.</p>\n<p>Before it was broken by the plow, most of the Great Plains from the Texas panhandle northward was treeless grassland. Trees grew only along the floodplains of streams and on the few mountain masses of the northern Great Plains. These lush prairies once were the grazing ground for immense herds of bison, and the land provided a bountiful life for those Indians who followed the herds. South of the grasslands, in Texas, shrubs mixed with the grasses: creosote bush along the valley of the Pecos River; mesquite, oak, and juniper to the east.</p>\n<p>The general lack of trees suggests that this is a land of little moisture, as indeed it is. Nearly all of the Great Plains receives less than 24 inches of rainfall a year, and most of it receives less than 16 inches. This dryness and the strength of sunshine in this area, which lies mostly between 2,000 and 6,000 feet above sea level, create the semiarid environment that typifies the Great Plains. But it was not always so. When the last continental glacier stood near its maximum extent, some 12,000-14,000 years ago, spruce forest reached southward as far as Kansas, and the Great Plains farther south was covered by deciduous forest. The trees retreated northward as the ice front receded, and the Great Plains has been a treeless grassland for the last 8,000-10,000 years.</p>\n<p>For more than half a century after Lewis and Clark crossed the country in 1805-6, the Great Plains was the testing ground of frontier America here America grew to maturity (fig. 1). In 1805-7, explorer Zebulon Pike crossed the southcentral Great Plains, following the Arkansas River from near Great Bend, Kans., to the Rocky Mountains. In later years, Santa Fe traders, lured by the wealth of New Mexican trade, followed Pike's path as far as Bents Fort, Colo., where they turned southwestward away from the river route. Those pioneers who later crossed the plains on the Oregon Trail reached the Platte River near the place that would become Kearney, Nebr., by a nearly direct route from Independence, Mo., and followed the Platte across the central part of the Great Plains.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/b1493","usgsCitation":"Trimble, D.E., 1980, The geologic story of the Great Plains (Reprinted 1990): U.S. Geological Survey Bulletin 1493, 55 p., https://doi.org/10.3133/b1493.","productDescription":"55 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":12461,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.nps.gov/parkhistory/online_books/geology/publications/bul/1493/index.htm","linkFileType":{"id":5,"text":"html"}},{"id":166454,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1493/report-thumb.jpg"},{"id":93752,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1493/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"Reprinted 1990","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c5e2","contributors":{"authors":[{"text":"Trimble, Donald E.","contributorId":75910,"corporation":false,"usgs":true,"family":"Trimble","given":"Donald","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":215714,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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