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Off.,","doi":"10.3133/pp343","usgsCitation":"Steven, T.A., and Ratte, J.C., 1960, Geology and ore deposits of the Summitville district, San Juan Mountains, Colorado: U.S. Geological Survey Professional Paper 343, 70 p., https://doi.org/10.3133/pp343.","productDescription":"70 p.","costCenters":[],"links":[{"id":140477,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0343/report-thumb.jpg"},{"id":112854,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0343/report.pdf","size":"14181","linkFileType":{"id":1,"text":"pdf"}},{"id":112855,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0343/plate-1.pdf","size":"2935","linkFileType":{"id":1,"text":"pdf"}},{"id":112856,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0343/plate-2.pdf","size":"5604","linkFileType":{"id":1,"text":"pdf"}},{"id":112857,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0343/plate-3.pdf","size":"8409","linkFileType":{"id":1,"text":"pdf"}},{"id":112858,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0343/plate-4.pdf","size":"899","linkFileType":{"id":1,"text":"pdf"}},{"id":112859,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0343/plate-5.pdf","size":"745","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db6843e5","contributors":{"authors":[{"text":"Steven, Thomas August","contributorId":73174,"corporation":false,"usgs":true,"family":"Steven","given":"Thomas","email":"","middleInitial":"August","affiliations":[],"preferred":false,"id":152754,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ratte, James Clifford","contributorId":9268,"corporation":false,"usgs":true,"family":"Ratte","given":"James","email":"","middleInitial":"Clifford","affiliations":[],"preferred":false,"id":152753,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":52132,"text":"ofr60125 - 1960 - Records of wells and water-level fluctuations in the Aberdeen-Springfield area, Bingham and Power Counties, Idaho, in 1959","interactions":[],"lastModifiedDate":"2012-02-02T00:11:28","indexId":"ofr60125","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"60-125","title":"Records of wells and water-level fluctuations in the Aberdeen-Springfield area, Bingham and Power Counties, Idaho, in 1959","language":"ENGLISH","doi":"10.3133/ofr60125","usgsCitation":"Sisco, H.G., 1960, Records of wells and water-level fluctuations in the Aberdeen-Springfield area, Bingham and Power Counties, Idaho, in 1959: U.S. Geological Survey Open-File Report 60-125, 37 p., 1 plate, https://doi.org/10.3133/ofr60125.","productDescription":"37 p., 1 plate","costCenters":[],"links":[{"id":178976,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1960/0125/report-thumb.jpg"},{"id":86666,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1960/0125/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db6355c0","contributors":{"authors":[{"text":"Sisco, Harold G.","contributorId":6115,"corporation":false,"usgs":true,"family":"Sisco","given":"Harold","email":"","middleInitial":"G.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":244852,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":62367,"text":"gq130 - 1960 - Geology of the Wildwood quadrangle, Tennessee","interactions":[],"lastModifiedDate":"2021-11-10T21:08:31.416572","indexId":"gq130","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"130","title":"Geology of the Wildwood quadrangle, Tennessee","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gq130","usgsCitation":"Neuman, R.B., 1960, Geology of the Wildwood quadrangle, Tennessee: U.S. Geological Survey Geologic Quadrangle 130, Report: 1 p.; Plate, https://doi.org/10.3133/gq130.","productDescription":"Report: 1 p.; Plate","costCenters":[],"links":[{"id":248543,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0130/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":253687,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0130/report-thumb.jpg"},{"id":102128,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_577.htm","linkFileType":{"id":5,"text":"html"},"description":"577"}],"scale":"24000","country":"United States","state":"Tennessee","otherGeospatial":"Wildwood quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -83.875,35.75 ], [ -83.875,35.875 ], [ -83.75,35.875 ], [ -83.75,35.75 ], [ -83.875,35.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e3aaf","contributors":{"authors":[{"text":"Neuman, Robert B.","contributorId":104046,"corporation":false,"usgs":true,"family":"Neuman","given":"Robert","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":267290,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":52131,"text":"ofr60123 - 1960 - Marine geology and bathymetry of nearshore shelf of Chukchi Sea, Ogotoruk Creek area, northwest Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:11:28","indexId":"ofr60123","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"60-123","title":"Marine geology and bathymetry of nearshore shelf of Chukchi Sea, Ogotoruk Creek area, northwest Alaska","docAbstract":"During July and August 1958 the U.S. Geological Survey conducted a study in behalf of the Atomic Energy Commission of the oceanography, bathymetry, and marine geology of the nearshore shelf of the Chukchi Sea off the Ogotoruk Creek area, northwest Alaska. Ogotoruk Creek enters the Chukchi Sea about 32 miles southeast of the large cuapate spit of Point Hope at long 165 degrees 44\u001946\u001D W. and lat 68 degrees 05\u001951\u001D N. The Ogotoruk Creek area extends approximately 10 miles west and 7 miles east of the creek mouth. Knowledge of the marine geology and oceanography is confined primarily to the nearshore shelf, which includes about 70 square miles of the shelf and is defined as the sea floor lying shoreward of the 50-foot submarine contour. The 50-foot contour generally lies from 2 to 4 miles from shore. Submarine topography was studied to a distance of 15 miles from shore over an area of approximately 340 square miles.\r\n\r\nA northwest coastal current flows past the Ogotoruk Creek area and during July and August averaged 0.5 mile per hour. Persistent northerly winds cause general upwelling near shore and at times of pronounced upwelling the coastal current was reversed or appreciably reduced in speed. Longshore currents shoreward of the breaker zone averaged 0.3 mile per hour and moved to the east for the greater part of the time of the study.\r\n\r\nThe overall seaward slope of the inner 15 miles of the Chukchi shelf from a depth of 40 to 135 feet is approximately 0 degrees 04\u0019, or about 6 feet per mile. Slopes near shore to depths of 15-20 feet are steep and average 2 degrees 30\u0019. Beyond these depths they increase gradually out to a depth of 40-45 feet. Seaward of this point the shelf is flattest and slopes are as low as 0 degree 01\u0019. This terrace or flat part of the nearshore shelf is about 2 miles wide and descends to a depth of 50-55 feet beyond which the gradient increases to about 0 degree 06\u001D. At depths greater than 85 feet the submarine declivity gradually decreases to 0 degree 03\u0019 at a distance of 15 miles from shore.\r\n\r\nA flat-bottomed trough, Ogotoruk Seavalley, heads about a quarter of a mile from shore off the mouth of Ogotoruk Creek. The shallow seavalley averages only 6 feet in relief and extends 15 miles from shore to a depth of 135 feet. A number of smaller channels also indent the gentle sloping inner Chukchi shelf east of the seavalley and nearshore west of it.\r\n\r\nMany outcrops of Paleozoic and Mesozoic formations on the nearshore shelf indicate that it is a wave-planed platform. Wave planation is thought to have taken place primarily in Sangamon and rpre-Sangamon time (approximately 100,000 to 1,000,000 years ago). Ogotoruk Seavalley is believed to be a drowned subaerial valley which was excavated by Ogotoruk Creek during periods of glacially depressed sea level.\r\n\r\nUnconsolidated sediments overlying the nearshore shelf are chiefly slightly rounded residual gravel which have been derived from submerged outcrops. Detrital sand and silt, contributed from the nearby coastal area during Recent time, overlie the shelf near shore and at depth as much as 50 feet seaward of segments of the coast underlain by fine-grained clastic rocks of Mesozoic age. Owing to a small volume of detrital clasts contributed by the coastal area detrital sedimentation is not prominent over the nearshore shelf.\r\n\r\nBeaches fronting the Ogotoruk Creek area are 30-260 feet wide, range from less than 10 to about 25 feet thick, and are composed of sandy gravel having a median diameter of about 10 mm. Rounded clasts of greywacke, siltstone, limestone, and chert are the principal constituents of the gravel. Longshore currents accompanying moderate storms transport gravel and sand parallel to shore at rates of 5 cubic yards per hour. Sediment transported by longshore currents accumulates as spits at stream mouths and as areas of new beach below rocky headlands.","language":"ENGLISH","doi":"10.3133/ofr60123","usgsCitation":"Scholl, D., and Sainsbury, C., 1960, Marine geology and bathymetry of nearshore shelf of Chukchi Sea, Ogotoruk Creek area, northwest Alaska: U.S. Geological Survey Open-File Report 60-123, 58 p., https://doi.org/10.3133/ofr60123.","productDescription":"58 p.","costCenters":[],"links":[{"id":178881,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1960/0123/report-thumb.jpg"},{"id":86665,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1960/0123/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606c21","contributors":{"authors":[{"text":"Scholl, D.W.","contributorId":106461,"corporation":false,"usgs":true,"family":"Scholl","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":244851,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sainsbury, C.L.","contributorId":99968,"corporation":false,"usgs":true,"family":"Sainsbury","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":244850,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":13876,"text":"ofr6059 - 1960 - An aeromagnetic reconnaissance of the Cook Inlet area, Alaska","interactions":[{"subject":{"id":13876,"text":"ofr6059 - 1960 - An aeromagnetic reconnaissance of the Cook Inlet area, Alaska","indexId":"ofr6059","publicationYear":"1960","noYear":false,"title":"An aeromagnetic reconnaissance of the Cook Inlet area, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":39075,"text":"pp316G - 1963 - An aeromagnetic reconnaissance of the Cook Inlet area, Alaska","indexId":"pp316G","publicationYear":"1963","noYear":false,"chapter":"G","title":"An aeromagnetic reconnaissance of the Cook Inlet area, Alaska"},"id":1}],"supersededBy":{"id":39075,"text":"pp316G - 1963 - An aeromagnetic reconnaissance of the Cook Inlet area, Alaska","indexId":"pp316G","publicationYear":"1963","noYear":false,"title":"An aeromagnetic reconnaissance of the Cook Inlet area, Alaska"},"lastModifiedDate":"2023-10-06T20:39:35.658058","indexId":"ofr6059","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"60-59","title":"An aeromagnetic reconnaissance of the Cook Inlet area, Alaska","docAbstract":"Forty-two east-west aeromagnetic lines were flown across the Cook Inlet-Susitna Lowland between Chelatna Lake and Seldovia at a flight altitude of approximately 2,500 feet. The lines traverse all or part of five Mesozoic tectonic elements that dominate the structure of the Cook Inlet area. Each of these tectonic elements, the Alaska Range geosyncline, the Talkeetna geanticline, the Matanuska geosyncline, the Seldovia geanticline, and the Chugach Mountains geosyncline, has a characteristic magnetic pattern.
The aeromagnetic data, compiled as total intensity aeromagnetic profiles, show several significant features which are consistent with the structural grain of the area. A two-dimensional anomaly was observed near the east edge of the area on all but the southernmost profiles, where it becomes obscure. Geologic evidence suggests that this feature, the Knik Arm anomaly, is produced by plutonic rocks that have been intruded along the Seldovia geanticline. Southeast of this anomaly the profiles are almost flat. This flatness indicates that magnetic rocks are deeply buried in this area, which is underlain by slate and graywacke deposited in the Chugach Mountains geosyncline.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6059","usgsCitation":"Grantz, A., Zietz, I., and Andreasen, G., 1960, An aeromagnetic reconnaissance of the Cook Inlet area, Alaska: U.S. Geological Survey Open-File Report 60-59, Report: 58 p.; 9 Plates: 27.85 x 35.82 inches or smaller, https://doi.org/10.3133/ofr6059.","productDescription":"Report: 58 p.; 9 Plates: 27.85 x 35.82 inches or smaller","costCenters":[],"links":[{"id":421784,"rank":11,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1960/0059/figure-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":421783,"rank":10,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1960/0059/figure-3explanation.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":421782,"rank":9,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1960/0059/figure-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":421781,"rank":8,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1960/0059/figure-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":421780,"rank":7,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1960/0059/figure-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":421779,"rank":6,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1960/0059/figure-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":421778,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1960/0059/figure-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":421777,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1960/0059/figure-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":421776,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1960/0059/figure-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":421775,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1960/0059/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144657,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1960/0059/report-thumb.jpg"}],"scale":"500000","country":"United States","state":"Alaska","otherGeospatial":"Cook Inlet area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -154.86692834754194,\n 58.461367338468136\n ],\n [\n -148.58541629436866,\n 58.461367338468136\n ],\n [\n -148.58541629436866,\n 61.78410578839723\n ],\n [\n -154.86692834754194,\n 61.78410578839723\n ],\n [\n -154.86692834754194,\n 58.461367338468136\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685c25","contributors":{"authors":[{"text":"Grantz, Arthur agrantz@usgs.gov","contributorId":2585,"corporation":false,"usgs":true,"family":"Grantz","given":"Arthur","email":"agrantz@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":168548,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zietz, Isidore","contributorId":76708,"corporation":false,"usgs":true,"family":"Zietz","given":"Isidore","affiliations":[],"preferred":false,"id":168549,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Andreasen, Gordon E.","contributorId":94272,"corporation":false,"usgs":true,"family":"Andreasen","given":"Gordon E.","affiliations":[],"preferred":false,"id":168550,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":12524,"text":"ofr6011 - 1960 - Gravity survey in part of the Snake River Plain, Idaho — A preliminary report","interactions":[],"lastModifiedDate":"2022-01-24T22:02:33.223909","indexId":"ofr6011","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"60-11","title":"Gravity survey in part of the Snake River Plain, Idaho — A preliminary report","docAbstract":"During the early summer of 1959, a total of 1,187 gravity stations were occupied on the western part of the Snake River plain in Idaho. An area of 2,000 square miles extending from Glenns Ferry, Idaho, to Caldwell, Idaho, was covered with a station density of one station per two square miles. An additional 1,200 square miles of surrounding area, mainly from Caldwell, Idaho, to the Oregon-Idaho state line, was covered with a density of one station per seven square miles. The mean reproducibility of the observed gravities of these stations was 0.05 milligal, with a maximum discrepancy of 0.2 milligal. Gravity data were reduced to simple Bouguer values using a combined free-air and Bouguer correction of 0.06 milligal per foot.\r\n\r\nThe only anomalies found with closure in excess of 10 milligals are two elongated highs, orientated northwest-southeast, with the northwestern high offset to the northeast by 10 miles. The smaller of these highs extends from Meridian, Idaho, to Nyssa, Oregon, and the larger extends from Swan Falls, Idaho, to Glenns Ferry, Idaho. The maximum value recorded is a simple Bouguer value of -66.5 milligals with respect to the International Ellipsoid. Gradients on the sides of these highs are largest on the northeast sides, reaching six milligals per mile in places. Graticule interpretations of a profile across the southeastern high using a density contrast of 0.3 gm per cubic centimeter indicate an accumulation of lava reaching a thickness of at least 28,000 feet.\r\n\r\nThe Snake River investigation was made for the purpose of searching out, defining, and interpreting gravity anomalies present on the western part of the Snake River lava plain in Idaho. In particular, it was desired to further define gradients associated with the gravity high shown by the regional work of Bonini and Lavin (1957). It was not planned to cover any specific area, but rather to let the observed anomalies determine the course of the field work.\r\n\r\nThe study was undertaken as part of a project on Volcanism and Crustal Deformation, supervised by L. C. Pakiser of the U.S. Geological Survey. 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