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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp101","usgsCitation":"Meuschke, J.L., and Henderson, J.R., 1953, Total intensity aeromagnetic and geologic map of southern Aitkin County and northern Mille Lacs County, Minnesota: U.S. Geological Survey Geophysical Investigations Map 101, 2 Plates: 46.58 × 37.00 inches and 38.79 × 31.17 inches, https://doi.org/10.3133/gp101.","productDescription":"2 Plates: 46.58 × 37.00 inches and 38.79 × 31.17 inches","costCenters":[],"links":[{"id":186985,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":388905,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3010.htm"},{"id":260509,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0101/plate-2.pdf"},{"id":260508,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0101/plate-1.pdf"}],"scale":"63360","country":"United States","state":"Minnesota","county":"Aitkin County, Mille Lacs County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -93.0583,\n 46.1661\n ],\n [\n -93.8,\n 46.1661\n ],\n [\n -93.8,\n 46.6\n ],\n [\n -93.0583,\n 46.6\n ],\n [\n -93.0583,\n 46.1661\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629a34","contributors":{"authors":[{"text":"Meuschke, J. 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The district is in east-central Idaho, about 20 miles west-southwest of Salmon. The area is one of deeply weathered nearly flat-topped upland surfaces cut by steep-walled valleys which are tributary to the canyon of Panther Creek. Most of the area has a relatively heavy vegetative cover, and outcrops are scarce except on the sides of the steeper valleys* Because of the importance of the surficial deposits and soils and the physiographic history of the region on the interpretation of the geochemical data, a separate chapter on this subject by Gerald H. Richmond follows the following brief description of the geology of the district.
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The lower 7 miles of the valley is cultivated, but upstream from this stretch the valley is narrow and is used mainly for summer grazing and recreation. Above the mouth of Thompson Creek, numerous dam sites are available, but the narrow valley and steep gradient do not favor storage for regulation of streamflow. The potential power from the natural flow of the stream in an average year is estimated to be 4,750 kilowatts for 95 percent of the time; 5,102 kw for 90 percent of the time; 10,570 kw for 50 percent of the time; and 36,940 kw at mean flow. Using the regulated flow resulting from the utilization of reservoirs at Marble and Redstone, the potential power is estimated to be 26,510 kw for 90 percent of the time and 27,810 kw for 50 percent of the time.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir292","usgsCitation":"Lawrence, F.F., 1953, Water-power resources of Crystal River, Colorado: U.S. Geological Survey Circular 292, 17 p. :ill., col. map ;27 cm., https://doi.org/10.3133/cir292.","productDescription":"17 p. :ill., col. map ;27 cm.","costCenters":[],"links":[{"id":30796,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1953/0292/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118288,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1953/0292/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e734a","contributors":{"authors":[{"text":"Lawrence, Fred Forrest","contributorId":93034,"corporation":false,"usgs":true,"family":"Lawrence","given":"Fred","email":"","middleInitial":"Forrest","affiliations":[],"preferred":false,"id":147505,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":14184,"text":"ofr53123 - 1953 - Preliminary report of the Centennial Range, Montana-Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:06:41","indexId":"ofr53123","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-123","title":"Preliminary report of the Centennial Range, Montana-Idaho","docAbstract":"Phosphate rock is present in the Phosphoria formation of Permian age in the Centennial Range of southwestern Montana and adjoining parts of Idaho. A Study was made to map the Phosphoria formation, study its stratigraphy, and to ascertain the reserves and mining problems. In the Centennial Range the Phosphoria formation is divisible into five members, designated A to E, from the bottom to the top of the formation. The B and D members contain phosphate rock. The B member contains six feet or more of high grade phosphate rock, mostly in one layer, and is the chief potential ore bed. The phosphate rock is of detrital origin and contains some quartz. Lithologic variations in the B member as well as areas where the B member is missing due to pre-member erosion, need more study.\r\n\r\nThe formation dips gently southward and is overlain by varying amounts of overburden, Underground mining would seem to be the best method of potential exploitation of the deposit, but core drilling and further trenching are needed. \r\n\r\nHigh grade phosphate rock reserves in. The Centennial Range may total scores of millions of tons.","language":"ENGLISH","publisher":"[U.S. Geological Survey], Mineral Deposits Branch,","doi":"10.3133/ofr53123","usgsCitation":"Honkala, F.S., 1953, Preliminary report of the Centennial Range, Montana-Idaho: U.S. Geological Survey Open-File Report 53-123, 19 p., https://doi.org/10.3133/ofr53123.","productDescription":"19 p.","costCenters":[],"links":[{"id":145659,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1953/0123/report-thumb.jpg"},{"id":42849,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1953/0123/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42850,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1953/0123/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42851,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1953/0123/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42852,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1953/0123/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42853,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1953/0123/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42854,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1953/0123/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42855,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1953/0123/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cbd9","contributors":{"authors":[{"text":"Honkala, Frederick Sauli","contributorId":65091,"corporation":false,"usgs":true,"family":"Honkala","given":"Frederick","email":"","middleInitial":"Sauli","affiliations":[],"preferred":false,"id":169043,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":51224,"text":"ofr5341 - 1953 - Photogeologic map, Emery 9 quadrangle, Emery County, Utah","interactions":[{"subject":{"id":70048456,"text":"tem588 - 1953 - Photogeologic map, Emery-9 quadrangle, Emery county, Utah","indexId":"tem588","publicationYear":"1953","noYear":false,"title":"Photogeologic map, Emery-9 quadrangle, Emery county, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":51224,"text":"ofr5341 - 1953 - Photogeologic map, Emery 9 quadrangle, Emery County, Utah","indexId":"ofr5341","publicationYear":"1953","noYear":false,"title":"Photogeologic map, Emery 9 quadrangle, Emery County, Utah"},"id":1}],"lastModifiedDate":"2013-09-26T15:42:28","indexId":"ofr5341","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-41","title":"Photogeologic map, Emery 9 quadrangle, Emery County, Utah","language":"ENGLISH","doi":"10.3133/ofr5341","usgsCitation":"Condon, W.H., 1953, Photogeologic map, Emery 9 quadrangle, Emery County, Utah: U.S. Geological Survey Open-File Report 53-41, 1 map, https://doi.org/10.3133/ofr5341.","productDescription":"1 map","costCenters":[],"links":[{"id":176817,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":86491,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1953/0041/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db686065","contributors":{"authors":[{"text":"Condon, W. H.","contributorId":28611,"corporation":false,"usgs":true,"family":"Condon","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":243185,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}