A study of the distribution of copper in transported alluvium on a pediment of the Rocky Range, Beaver County, Utah, undertaken to determine whether known copper deposits in bedrock concealed by alluvium could be detected by geochemical methods, was reported in Geological Survey Research 1960 ( Erickson, R.L., and Marrenzino, A.P., 1960, Geochemical prosecting for copper in the Rocky Range, Beaver County, Utah; U.S. Geol. Survey Prof. Paper 400-B, p. B98-E101). The attached map and table supplement that paper by giving the locations at which the samples were collected and the analytical determinations of copper in the samples.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6449","usgsCitation":"Erickson, R.L., and Marranzino, A.P., 1964, Copper determinations on samples of alluvium and caliche from the rocky Range, Beaver County, Utah: U.S. Geological Survey Open-File Report 64-49, Report: 5 p.; 1 Plate: 24.26 x 19.36 inches, https://doi.org/10.3133/ofr6449.","productDescription":"Report: 5 p.; 1 Plate: 24.26 x 19.36 inches","costCenters":[],"links":[{"id":490594,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0049/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":490593,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1964/0049/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145972,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1964/0049/report-thumb.jpg"}],"country":"United States","state":"Utah","county":"Beaver 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Ralph Leroy","contributorId":107263,"corporation":false,"usgs":true,"family":"Erickson","given":"Ralph","email":"","middleInitial":"Leroy","affiliations":[],"preferred":false,"id":167983,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Marranzino, Albert Pasquale","contributorId":64666,"corporation":false,"usgs":true,"family":"Marranzino","given":"Albert","email":"","middleInitial":"Pasquale","affiliations":[],"preferred":false,"id":167982,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":39109,"text":"pp305L - 1964 - Core tests, Simpson area, Alaska, with a section on temperature measurement studies","interactions":[],"lastModifiedDate":"2012-02-02T00:10:14","indexId":"pp305L","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"305","chapter":"L","title":"Core tests, Simpson area, Alaska, with a section on temperature measurement studies","language":"ENGLISH","doi":"10.3133/pp305L","usgsCitation":"Robinson, F.M., and Brewer, M., 1964, Core tests, Simpson area, Alaska, with a section on temperature measurement studies: U.S. Geological Survey Professional Paper 305, p. 645-730, https://doi.org/10.3133/pp305L.","productDescription":"p. 645-730","costCenters":[],"links":[{"id":120011,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0305l/report-thumb.jpg"},{"id":66559,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0305l/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66560,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0305l/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66561,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0305l/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66562,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0305l/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66563,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0305l/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66564,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0305l/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66565,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0305l/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66566,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0305l/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688e50","contributors":{"authors":[{"text":"Robinson, F. M.","contributorId":84830,"corporation":false,"usgs":true,"family":"Robinson","given":"F.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":220976,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brewer, M.C.","contributorId":54994,"corporation":false,"usgs":true,"family":"Brewer","given":"M.C.","email":"","affiliations":[],"preferred":false,"id":220975,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":47226,"text":"ofr6415 - 1964 - Gamma-ray logs from central Bluegrass Region, Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:10:58","indexId":"ofr6415","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"64-15","title":"Gamma-ray logs from central Bluegrass Region, Kentucky","language":"ENGLISH","doi":"10.3133/ofr6415","usgsCitation":"Black, D.F., and Cressman, E.R., 1964, Gamma-ray logs from central Bluegrass Region, Kentucky: U.S. Geological Survey Open-File Report 64-15, 1 diagram :photocopy ;on sheet 64 x 93 cm., https://doi.org/10.3133/ofr6415.","productDescription":"1 diagram :photocopy ;on sheet 64 x 93 cm.","costCenters":[],"links":[{"id":168722,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b13f3","contributors":{"authors":[{"text":"Black, Douglas F. B.","contributorId":106498,"corporation":false,"usgs":true,"family":"Black","given":"Douglas","email":"","middleInitial":"F. B.","affiliations":[],"preferred":false,"id":234859,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cressman, Earle Rupert","contributorId":43324,"corporation":false,"usgs":true,"family":"Cressman","given":"Earle","email":"","middleInitial":"Rupert","affiliations":[],"preferred":false,"id":234858,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":62486,"text":"gq355 - 1964 - Geology of the South Butte quadrangle New Mexico-Valencia County","interactions":[],"lastModifiedDate":"2021-11-10T19:56:51.078882","indexId":"gq355","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"355","title":"Geology of the South Butte quadrangle New Mexico-Valencia County","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gq355","usgsCitation":"Moench, R.H., 1964, Geology of the South Butte quadrangle New Mexico-Valencia County: U.S. Geological Survey Geologic Quadrangle 355, Report: 1 p.; Plate, https://doi.org/10.3133/gq355.","productDescription":"Report: 1 p.; Plate","costCenters":[],"links":[{"id":102367,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_816.htm","linkFileType":{"id":5,"text":"html"},"description":"816"},{"id":248649,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0355/report.pdf","size":"33","linkFileType":{"id":1,"text":"pdf"}},{"id":253876,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0355/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"New Mexico","county":"Valencia County","otherGeospatial":"South Butte quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -107.5,34.8675 ], [ -107.5,35 ], [ -107.36749999999999,35 ], [ -107.36749999999999,34.8675 ], [ -107.5,34.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e4b9","contributors":{"authors":[{"text":"Moench, Robert Hadley","contributorId":28238,"corporation":false,"usgs":true,"family":"Moench","given":"Robert","email":"","middleInitial":"Hadley","affiliations":[],"preferred":false,"id":267440,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3221,"text":"cir489 - 1964 - A magnetic anomaly of possible economic significance in southeastern Minnesota","interactions":[],"lastModifiedDate":"2018-01-02T19:49:02","indexId":"cir489","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"489","title":"A magnetic anomaly of possible economic significance in southeastern Minnesota","docAbstract":"An aeromagnetic survey in southeastern Minnesota by the U. S. Geological Survey in cooperation with the State of Minnesota has revealed a high-amplitude, linear, and narrow magnetic feature that suggests a possible source of Precambrian iron-formation of economic value. \r\n\r\nFor the past few years the U. S. Geological Survey has been conducting detailed geophysical studies of the midcontinent gravity anomaly--a broad, high-amplitude feature that extends from Lake Superior through the States of Minnesota, Iowa, Nebraska, and part of Kansas. As part of this study an aeromagnetic survey of the southern part of the State was made in cooperation with the State of Minnesota during the summer of 1963, in which a linear high-amplitude anomaly of the order of 4,000 gammas was discovered. Because of the high amplitude, the linearity, and the narrowness of the magnetic feature, it is believed the source may be Precambrian iron-formation of possible economic value. \r\n\r\nThe anomalous area is in Fillmore County, approximately between the towns of Lanesboro and Peterson in the extreme southeastern part of the State. (See figures 1 and 2.) At the site of the anomaly, Cambrian sedimentary rocks occur in the valley of the Root River, and Ordovician rocks (nearly flat lying) mantle the upland areas. \r\n\r\nThe uplands are largely covered by glacial deposits, which are relatively thin (Paul K. Sims, written communication, 1964). Depths to the Precambrian are estimated to range from 500 feet to 1,000 feet below the surface. \r\n\r\nThe aeromagnetic map shown in figure 2 was compiled from continuous magnetic profiles made along east-west flight lines 1,000 feet above ground, and spaced approximately 1 mile apart. Contour intervals of 20, 100, and 500 gammas were used depending on the intensity. The instrument for the survey was a flux-gate type magnetometer (AN/ASQ-3A) which measures total-field variations. The contour map displays variations in magnetic pattern which are typical of shallow Precambrian rocks. Anomalies of the order of 1,000 gammas are shown along the east and west edges of the map. The outstanding feature is the previously mentioned linear positive anomaly that trends northeast and reaches a peak of 3,960 gammas. The positive anomaly is contoured from data on four consecutive profiles, but only two show high amplitudes. The high-amplitude anomalies along traverses 1 and 2 are shown in figure 3. \r\n\r\nDepth calculations suggest that the source of the anomaly lies about 1,000 feet below the surface. Assuming a dikelike source and magnetization resulting entirely from induction in the earth's field, several calculations were made in an attempt to fit the magnetic profile taken along the line AA' (see figs. 2 and 4), considered to be a typical cross-section of the magnetic anomaly. Comparisons are shown between observed and computed profiles. The fixed parameters used were (a) distance from detector to source of 2,000 ft; width of dike of 5,000 ft; dip of dike of 75?, 90?, 105? , and 120? , as shown. The best fit occurs when the dike is vertical or dips 75? to the southwest. For these cases, the susceptibility, k, is computed to be 0.016 c.g.s, units, and is comparable to k = 0.02+ calculated by Bath (1962) for the relatively unmetamorphosed iron-formation of the Main Megabi district in Minnesota where the induced magnetization was most likely the dominant magnetization. If the dominant magnetization for the anomaly in Fillmore County were remanent rather than induced, the economic importance of the anomaly would be greatly reduced. \r\n\r\nThis anomaly seems sufficiently promising to warrant further geologic and geophysical investigation. Detailed ground magnetic and electrical studies would be useful to delineate the feature. In the final analysis, however, the presence of iron-formation can be determined only by the drill.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir489","usgsCitation":"Zietz, I., 1964, A magnetic anomaly of possible economic significance in southeastern Minnesota: U.S. Geological Survey Circular 489, 5 p. :maps ;27 cm., https://doi.org/10.3133/cir489.","productDescription":"5 p. :maps ;27 cm.","costCenters":[],"links":[{"id":138944,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1964/0489/report-thumb.jpg"},{"id":30214,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1964/0489/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae1de","contributors":{"authors":[{"text":"Zietz, Isidore","contributorId":76708,"corporation":false,"usgs":true,"family":"Zietz","given":"Isidore","affiliations":[],"preferred":false,"id":146462,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3226,"text":"cir483 - 1964 - Summary of developed and potential waterpower of the United States and other countries of the world, 1955-62","interactions":[],"lastModifiedDate":"2012-02-02T00:05:34","indexId":"cir483","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"483","title":"Summary of developed and potential waterpower of the United States and other countries of the world, 1955-62","docAbstract":"Estimates of potential waterpower and historical data on waterpower developments in various parts of the world are assembled in this report. Salient characteristics of the period studied, 1955-62, include increased use of the underground powerhouse, multiple -purpose developments, and use of storage (including pumped storage) to increase the value of waterpower for peaking purposes. High-voltage long-distance transmission has been improved, especially in the United States, Sweden, and the U.S.S.R., and generating facilities tend to be larger than ever before. Asia leads the continents in total potential waterpower; Europe is first in use of waterpower. In rate of increase of waterpower installations and in percent of hydroelectric to total installations Africa is first among the continents. The 1955-62 period saw a great increase in per capita consumption of electric energy. Norway leads all countries with annual consumption of about 9,000 kwhr per capita. Waterpower development was carried on in a majority of the countries of the world and in most of them at an accelerated rate.","language":"ENGLISH","publisher":"U.S. Govt. Print. 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