{"pageNumber":"1337","pageRowStart":"33400","pageSize":"25","recordCount":36989,"records":[{"id":12439,"text":"ofr653 - 1965 - A mineralogical and chemical study of the leached zone of the Bone Valley formation of Florida - a progress report","interactions":[],"lastModifiedDate":"2012-02-02T00:06:30","indexId":"ofr653","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-3","title":"A mineralogical and chemical study of the leached zone of the Bone Valley formation of Florida - a progress report","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr653","usgsCitation":"Altschuler, Z., and Boudreau, C., 1965, A mineralogical and chemical study of the leached zone of the Bone Valley formation of Florida - a progress report: U.S. Geological Survey Open-File Report 65-3, 89 p. ill. ;29 cm., https://doi.org/10.3133/ofr653.","productDescription":"89 p. ill. ;29 cm.","costCenters":[],"links":[{"id":143732,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adfb7","contributors":{"authors":[{"text":"Altschuler, Z. S.","contributorId":42962,"corporation":false,"usgs":true,"family":"Altschuler","given":"Z. S.","affiliations":[],"preferred":false,"id":166139,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boudreau, C.E.","contributorId":71178,"corporation":false,"usgs":true,"family":"Boudreau","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":166140,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":16318,"text":"ofr65165 - 1965 - Plant and miscellaneous microfossils from the Thermopolis and Mowry Shales","interactions":[],"lastModifiedDate":"2017-05-19T18:29:49","indexId":"ofr65165","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-165","title":"Plant and miscellaneous microfossils from the Thermopolis and Mowry Shales","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr65165","usgsCitation":"Tschudy, R.H., and Veach, S.D., 1965, Plant and miscellaneous microfossils from the Thermopolis and Mowry Shales: U.S. Geological Survey Open-File Report 65-165, 6 p. ill. ;29 cm., https://doi.org/10.3133/ofr65165.","productDescription":"6 p. ill. ;29 cm.","costCenters":[],"links":[{"id":149674,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1965/0165/report-thumb.jpg"},{"id":45247,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1965/0165/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db6850b2","contributors":{"authors":[{"text":"Tschudy, Robert H.","contributorId":67879,"corporation":false,"usgs":true,"family":"Tschudy","given":"Robert","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":172618,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Veach, Sharon Dee","contributorId":46106,"corporation":false,"usgs":true,"family":"Veach","given":"Sharon","email":"","middleInitial":"Dee","affiliations":[],"preferred":false,"id":172617,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":16680,"text":"ofr65179 - 1965 - Structure, Quaternary history, and general geology of the Corral Canyon area, Los Angeles County, California","interactions":[],"lastModifiedDate":"2018-05-01T14:46:38","indexId":"ofr65179","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-179","title":"Structure, Quaternary history, and general geology of the Corral Canyon area, Los Angeles County, California","docAbstract":"The Corral Canyon nuclear power plant site consists of about 305 acres near the mouth of Corral Canyon in the central Santa Monica Mountains; it is located on an east-trending segment of the Pacific Coast between Point Dume and Malibu Canyon, about 28 miles due west of Los Angeles. The Santa Monica Mountains are the southwesternmost mainland part of the Transverse Ranges province, the east-trending features of which transect the otherwise relatively uniform northwesterly trend of the geomorphic and geologic features of coastal California. The south margin of the Transverse Ranges is marked by the Santa Monica fault system, which extends eastward near the 34th parallel for at least 145 miles from near Santa Cruz Island to the San Andreas fault zone. In the central Santa Monica Mountains area the Santa Monica fault system includes the Malibu Coast fault and Malibu Coast zone of deformation on the north; from the south it includes an inferred fault--the Anacapa fault--considered to follow an east-trending topographic escarpmemt on the sea floor about 5 miles south of the Malibu Coast fault. The low-lying terrain south of the fault system, including the Los Angeles basin and the largely submerged Continental Borderland offshore, are dominated by northwest-trending structural features.\r\n\r\nThe Malibu Coat zone is a wide, east-trending band of asymmetrically folded, sheared, and faulted bedrock that extends for more than 20 miles along the north margin of the Santa Monica fault system west of Santa Monica. Near the north margin of the Malibu Coast zone the north-dipping, east-trending Malibu Coast fault juxtaposes unlike, in part contemporaneous sedimentary rock sections; it is inferred to be the near-surface expression of a major crustal boundary between completely unrelated basement rocks. Comparison of contemporaneous structural features and stratigraphic sections (Late Cretaceous to middle Miocene sedimentary, rocks and middle Miocene volcanic and intrusive igneous rocks on the north; middle and upper Miocene sedimentary and middle Miocene volcanic rocks on the south) across the fault demonstrates that neither strike slip of less than 25 miles nor high-angle dip slip can account for this juxtaposition. Instead, the Malibu Coast fault is inferred to have been the locus of large-magnitude, north-south oriented, horizontal shortening (north, or upper, block thrust over south block). This movement occurred at or near the northern boundary of the Continental Borderland, the eastern boundary of which is inferred to be the northwest-trending known-active Newport-Inglewood zone of en echelon right lateral strike-slip faults in the western Los Angeles basin.\r\n\r\nLocal structural features and their relation to regional features, such as those in the Malibu Coast zone, form the basis for the interpretation that the Malibu Coast fault has acted chiefly as a thrust fault. Within the Malibu Coast zone, on both sides of the Malibu Coast fault, structural features in rocks that range in age from Late Cretaceous to late Miocene are remarkably uniform in orientation. The predominant trend of bedding, axial surfaces of numerous asymmetric folds, locally pervasive shear surfaces, and faults is approximately east-west and their predominant dip is northward.. The axes of the folds plunge gently east or west. Evidence from faults and shears within the zone indicates that relative movement on most of these was north (upper) over south. Beyond the Malibu Coast zone to the north and south the rocks entirely lack the asymmetric folds, overturned beds, and the locally abundant shears that characterize the rocks within the zone; these rocks were therefore not subjected to the same deforming forces that existed near the Malibu Coast fault. Movement on the Malibu Coast fault and deformation in the Malibu Coast zone occurred chiefly during the interval between late Miocene and late Pleistocene time. The youngest-known faulting in the Malibu Coast zone is late Pl","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr65179","usgsCitation":"Yerkes, R.F., and Wentworth, C.M., 1965, Structure, Quaternary history, and general geology of the Corral Canyon area, Los Angeles County, California: U.S. Geological Survey Open-File Report 65-179, ix, 215, [13] p. :ill., maps ;27 cm., https://doi.org/10.3133/ofr65179.","productDescription":"ix, 215, [13] p. :ill., maps ;27 cm.","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":45750,"rank":414,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0179/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45751,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1965/0179/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45747,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0179/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45748,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0179/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45749,"rank":413,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0179/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45740,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0179/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":150529,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1965/0179/report-thumb.jpg"},{"id":45736,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0179/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45737,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0179/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45738,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0179/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45739,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0179/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45742,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0179/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45743,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0179/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45741,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0179/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45744,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0179/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45745,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0179/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45746,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0179/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b08e4b07f02db69b31a","contributors":{"authors":[{"text":"Yerkes, R. F.","contributorId":24754,"corporation":false,"usgs":true,"family":"Yerkes","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":173277,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wentworth, Carl M. 0000-0003-2569-569X cwent@usgs.gov","orcid":"https://orcid.org/0000-0003-2569-569X","contributorId":1178,"corporation":false,"usgs":true,"family":"Wentworth","given":"Carl","email":"cwent@usgs.gov","middleInitial":"M.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":173276,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":14050,"text":"ofr6569 - 1965 - Principal facts and Bouguer anomaly values, Crooks Gap gravity survey, Fremont County, Wyoming","interactions":[],"lastModifiedDate":"2025-06-17T16:13:07.166529","indexId":"ofr6569","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-69","title":"Principal facts and Bouguer anomaly values, Crooks Gap gravity survey, Fremont County, Wyoming","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6569","usgsCitation":"Healey, D., 1965, Principal facts and Bouguer anomaly values, Crooks Gap gravity survey, Fremont County, Wyoming: U.S. Geological Survey Open-File Report 65-69, 18 p., https://doi.org/10.3133/ofr6569.","productDescription":"18 p.","costCenters":[],"links":[{"id":490859,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1965/0069/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":147120,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1965/0069/report-thumb.jpg"}],"country":"United States","state":"Wyoming","county":"Fremont 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,{"id":14973,"text":"ofr65180 - 1965 - Hot brines and recent iron deposits in deeps of the Red Sea","interactions":[],"lastModifiedDate":"2018-06-22T11:00:45","indexId":"ofr65180","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-180","title":"Hot brines and recent iron deposits in deeps of the Red Sea","docAbstract":"<p><span>Sedimentary iron and heavy-metal deposits of undetermined size have been found in the middle of the Red Sea some 2000 meters below the surface of the sea. This discovery has been made from the Research Vessel&nbsp;</span><i>Atlantis II</i><span>, which is still at sea engaged in a series of oceanographic investigations which ultimately will end in November 1965, after the ship has circumnavigated the globe. The discovery is significant because the environment and the processes controlling deposition of heavy metals are observable and appear to be still active.</span></p><p>The environment of the deposits can be breiefly described as an isolated sub-marine pool of brine having a pH as low as 5.3, a temperature of 56° c. and a salt content of about 310 grams per liter (at 20° c). Shipboard oxygen determinations and the indicated presence of H<sub>2</sub>S, divalent iron and divalent manganese in the water suggest that the environment is anaerobic. This hot, dense brine is trapped in a local depression of the Red Sea median valley. (Atlantis II Deep). The iron deposits, consisting largely of hydrous iron oxides, are found in the same depression. Brines from the Discovery Deep (21° 17 1 N, 38° 02'E) (1), a few miles southwest of the Atlantis II Deep (21°21 1 N, 38 ° 04'E), have a pH of 6.2 and a temp­erature of 44.7° c, and are also associated with iron-bearing sedirnents. The Discovery and Atlantis II brine pools both extend about 150 meters above the bottom. A few miles south of the: Discovery Deep another depression of greater depth has been reported (2) containing essentially normal Red Sea water. Deeps several hundred miles to the north (Sta. 540) and south (Sta. 545) were investigated and contained no brine. One of these (Sta. 545) is known to contain normal sediments.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr65180","usgsCitation":"Miller, A., Densmore, C., Degens, E., Hathaway, J., Manheim, F., McFarlin, P., Pocklington, R., and Jokela, A., 1965, Hot brines and recent iron deposits in deeps of the Red Sea: U.S. Geological Survey Open-File Report 65-180, 19 p., https://doi.org/10.3133/ofr65180.","productDescription":"19 p.","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":148138,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":355188,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1965/0180/ofr1965180.pdf","text":"Report","size":"2.65 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 1965-180"}],"geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              32.3876953125,\n              29.53522956294847\n            ],\n            [\n              34.8486328125,\n              24.5271348225978\n            ],\n            [\n              37.4853515625,\n              19.31114335506464\n            ],\n            [\n              39.7265625,\n              15.326571801420842\n            ],\n            [\n              43.3740234375,\n              12.683214911818666\n            ],\n            [\n              43.59375,\n              12.811801316582619\n            ],\n            [\n              42.6708984375,\n              16.594081412718474\n            ],\n            [\n              40.693359375,\n              19.518375478601566\n            ],\n            [\n              38.7158203125,\n              21.3303150734318\n            ],\n            [\n              38.7158203125,\n              23.443088931121785\n            ],\n            [\n              37.3095703125,\n              24.647017162630366\n            ],\n            [\n              36.6943359375,\n              26.03704188651584\n            ],\n            [\n              35.4638671875,\n              28.110748760633534\n            ],\n            [\n              34.1015625,\n              27.994401411046148\n            ],\n            [\n              33.22265625,\n              28.729130483430154\n            ],\n            [\n              32.51953125,\n              29.80251790576445\n            ],\n            [\n              32.3876953125,\n              29.53522956294847\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p><a href=\"https://woodshole.er.usgs.gov/\" data-mce-href=\"https://woodshole.er.usgs.gov/\">Coastal and Marine Geology Program</a><br> U.S. Geological Survey<br> 384 Woods Hole Road<br> Woods Hole, MA 02543</p>","tableOfContents":"<ul><li>Introduction</li><li>Geologic Setting</li><li>Oceangraphic History</li><li>Shipboard Work</li><li>Hydrography and Water Chemistry</li><li>Mineralogy</li><li>Chemistry</li><li>Discussion</li><li>Summary and Conclusions</li><li>References and Notes</li></ul>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62bdad","contributors":{"authors":[{"text":"Miller, A.R.","contributorId":87560,"corporation":false,"usgs":true,"family":"Miller","given":"A.R.","email":"","affiliations":[],"preferred":false,"id":170350,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Densmore, C.D.","contributorId":94320,"corporation":false,"usgs":true,"family":"Densmore","given":"C.D.","email":"","affiliations":[],"preferred":false,"id":170352,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Degens, 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,{"id":22982,"text":"ofr6553 - 1965 - Ground-water resources at three towns on the Standing Rock Indian Reservation in South Dakota","interactions":[],"lastModifiedDate":"2016-04-05T10:20:25","indexId":"ofr6553","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-53","title":"Ground-water resources at three towns on the Standing Rock Indian Reservation in South Dakota","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6553","issn":"0094-9140","usgsCitation":"Ellis, M.J., and Adolphson, D.G., 1965, Ground-water resources at three towns on the Standing Rock Indian Reservation in South Dakota: U.S. Geological Survey Open-File Report 65-53, ii, 71 p., https://doi.org/10.3133/ofr6553.","productDescription":"ii, 71 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":155923,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"South Dakota","otherGeospatial":"Standing Rock Indian Reservation","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db667058","contributors":{"authors":[{"text":"Ellis, M. J.","contributorId":27840,"corporation":false,"usgs":true,"family":"Ellis","given":"M.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":189232,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Adolphson, D. G.","contributorId":106081,"corporation":false,"usgs":true,"family":"Adolphson","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":189233,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":19703,"text":"ofr6589 - 1965 - Plant microfossils of the Hazard No. 7 coal, Perry County, Kentucky","interactions":[{"subject":{"id":19703,"text":"ofr6589 - 1965 - Plant microfossils of the Hazard No. 7 coal, Perry County, Kentucky","indexId":"ofr6589","publicationYear":"1965","noYear":false,"title":"Plant microfossils of the Hazard No. 7 coal, Perry County, Kentucky"},"predicate":"SUPERSEDED_BY","object":{"id":6135,"text":"pp839 - 1973 - Palynological studies of the coals of the Princess Reserve District in northeastern Kentucky","indexId":"pp839","publicationYear":"1973","noYear":false,"title":"Palynological studies of the coals of the Princess Reserve District in northeastern Kentucky"},"id":1}],"supersededBy":{"id":6135,"text":"pp839 - 1973 - Palynological studies of the coals of the Princess Reserve District in northeastern Kentucky","indexId":"pp839","publicationYear":"1973","noYear":false,"title":"Palynological studies of the coals of the Princess Reserve District in northeastern Kentucky"},"lastModifiedDate":"2025-07-01T18:19:18.623313","indexId":"ofr6589","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-89","title":"Plant microfossils of the Hazard No. 7 coal, Perry County, Kentucky","docAbstract":"<p>The cooperative mapping program between the Kentucky Geological Survey and the U. S. Geological Survey has yielded a number of interesting and valuable by-products. As a part of the stratigraphic studies involving Carboniferous coal fields, R. M. Kosanke has been involved in a detailed analysis of spore floras from various coal horizons. This study is aimed toward a correlation within the eastern coal field and, eventually, toward more accurate correlations with the western Kentucky coal fields.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6589","usgsCitation":"Kosanke, R.M., 1965, Plant microfossils of the Hazard No. 7 coal, Perry County, Kentucky: U.S. Geological Survey Open-File Report 65-89, 10 p., https://doi.org/10.3133/ofr6589.","productDescription":"10 p.","costCenters":[],"links":[{"id":491639,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1965/0089/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":153867,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1965/0089/report-thumb.jpg"}],"country":"United States","state":"Kentucky","county":"Perry 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,{"id":19548,"text":"ofr6581 - 1965 - Glacier observations, Glacier National Park, Montana, 1964","interactions":[],"lastModifiedDate":"2025-07-01T18:52:49.496012","indexId":"ofr6581","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-81","title":"Glacier observations, Glacier National Park, Montana, 1964","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6581","usgsCitation":"Johnson, A., 1965, Glacier observations, Glacier National Park, Montana, 1964: U.S. Geological Survey Open-File Report 65-81, Report: 18 p.; 2 Figures: 31.48 x 20.99 inches and 17.05 x 18.32 inches, 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,{"id":13491,"text":"ofr6552 - 1965 - Computer simulation programs for investigation of geological sampling problems","interactions":[],"lastModifiedDate":"2012-02-02T00:06:37","indexId":"ofr6552","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-52","title":"Computer simulation programs for investigation of geological sampling problems","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr6552","usgsCitation":"Eicher, R.N., and Miesch, A., 1965, Computer simulation programs for investigation of geological sampling problems: U.S. Geological Survey Open-File Report 65-52, 60 p. ill. ;27 cm., https://doi.org/10.3133/ofr6552.","productDescription":"60 p. ill. ;27 cm.","costCenters":[],"links":[{"id":144729,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1965/0052/report-thumb.jpg"},{"id":41968,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0052/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41969,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0052/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41970,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0052/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41971,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1965/0052/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a64e0","contributors":{"authors":[{"text":"Eicher, Ralph Newton","contributorId":9648,"corporation":false,"usgs":true,"family":"Eicher","given":"Ralph","email":"","middleInitial":"Newton","affiliations":[],"preferred":false,"id":167884,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miesch, A.T.","contributorId":88726,"corporation":false,"usgs":true,"family":"Miesch","given":"A.T.","affiliations":[],"preferred":false,"id":167885,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":23647,"text":"ofr6594 - 1965 - Flows of homogeneous density in tidal reaches: Solution by the implicit method","interactions":[],"lastModifiedDate":"2012-02-02T00:08:01","indexId":"ofr6594","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-94","title":"Flows of homogeneous density in tidal reaches: Solution by the implicit method","language":"ENGLISH","publisher":"United States Dept. of the Interior, Geological Survey,","doi":"10.3133/ofr6594","issn":"0094-9140","usgsCitation":"Lai, C., 1965, Flows of homogeneous density in tidal reaches: Solution by the implicit method: U.S. Geological Survey Open-File Report 65-94, 43 p. :ill. ;28 cm., https://doi.org/10.3133/ofr6594.","productDescription":"43 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":154937,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de785","contributors":{"authors":[{"text":"Lai, Chintu","contributorId":16860,"corporation":false,"usgs":true,"family":"Lai","given":"Chintu","email":"","affiliations":[],"preferred":false,"id":190478,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14119,"text":"ofr6571 - 1965 - Field determination of nanogram quantities of mercury in soils and rocks","interactions":[],"lastModifiedDate":"2022-08-25T21:02:41.121849","indexId":"ofr6571","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-71","title":"Field determination of nanogram quantities of mercury in soils and rocks","docAbstract":"<p>A method for determining nanogram quantities of mercury in geological materials is based on the catalytic effect of mercury on the reaction of ferrocyanide with nitrosobenzene to produce a violet-covered compound whose intensity if proportional to the mercury present. The mercury is released by heating a sample of soil or crushed rock to about 650°C. As little as 30 nanograms of mercury (30 parts per billion with 1 gram sample) can be detected. The reliability of the method is adequate to permit its use in geochemical surveys that utilize mercury as a pathfinder element.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6571","usgsCitation":"Hinkle, M., Leong, K.W., and Ward, F.N., 1965, Field determination of nanogram quantities of mercury in soils and rocks: U.S. Geological Survey Open-File Report 65-71, 14 p., https://doi.org/10.3133/ofr6571.","productDescription":"14 p.","costCenters":[],"links":[{"id":405642,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1965/0071/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":146028,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1965/0071/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fce4b07f02db5f59d5","contributors":{"authors":[{"text":"Hinkle, Margaret","contributorId":36918,"corporation":false,"usgs":true,"family":"Hinkle","given":"Margaret","affiliations":[],"preferred":false,"id":168952,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leong, Kam Wo","contributorId":99987,"corporation":false,"usgs":true,"family":"Leong","given":"Kam","email":"","middleInitial":"Wo","affiliations":[],"preferred":false,"id":168953,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ward, F. N.","contributorId":96254,"corporation":false,"usgs":true,"family":"Ward","given":"F.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":168954,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":14574,"text":"ofr65181 - 1965 - A spectrophotometric method for the determination of gold useful in mineral exploration","interactions":[],"lastModifiedDate":"2022-04-06T17:45:12.49676","indexId":"ofr65181","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-181","title":"A spectrophotometric method for the determination of gold useful in mineral exploration","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr65181","usgsCitation":"Lakin, H.W., and Nakagawa, H.M., 1965, A spectrophotometric method for the determination of gold useful in mineral exploration: U.S. Geological Survey Open-File Report 65-181, 12 p., https://doi.org/10.3133/ofr65181.","productDescription":"12 p.","costCenters":[],"links":[{"id":398233,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1965/0181/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":146574,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1965/0181/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a6348","contributors":{"authors":[{"text":"Lakin, H. W.","contributorId":11594,"corporation":false,"usgs":true,"family":"Lakin","given":"H.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":169674,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nakagawa, H. M.","contributorId":106475,"corporation":false,"usgs":true,"family":"Nakagawa","given":"H.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":169675,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":14175,"text":"ofr6574 - 1965 - Preliminary materials map, Otis quadrangle, Massachusetts","interactions":[],"lastModifiedDate":"2022-03-24T21:23:51.366799","indexId":"ofr6574","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-74","title":"Preliminary materials map, Otis quadrangle, Massachusetts","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6574","usgsCitation":"Holmes, G.W., 1965, Preliminary materials map, Otis quadrangle, Massachusetts: U.S. Geological Survey Open-File Report 65-74, Report: 6 p.; 1 Plate: 27.19 × 27.08 inches, https://doi.org/10.3133/ofr6574.","productDescription":"Report: 6 p.; 1 Plate: 27.19 × 27.08 inches","costCenters":[],"links":[{"id":397580,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8109.htm"},{"id":42837,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1965/0074/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42836,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0074/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144673,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1965/0074/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Massachusetts","otherGeospatial":"Otis quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73,\n              42.125\n            ],\n            [\n              -73.125,\n              42.125\n            ],\n            [\n              -73.125,\n              42.25\n            ],\n            [\n              -73,\n              42.25\n            ],\n            [\n              -73,\n              42.125\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66ce59","contributors":{"authors":[{"text":"Holmes, George William","contributorId":79107,"corporation":false,"usgs":true,"family":"Holmes","given":"George","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":169031,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15687,"text":"ofr65139 - 1965 - Preliminary Report on the Engineering Geology of the Straight Creek Tunnel Pilot Bore, Clear Creek and Summit Counties, Colorado","interactions":[{"subject":{"id":15687,"text":"ofr65139 - 1965 - Preliminary Report on the Engineering Geology of the Straight Creek Tunnel Pilot Bore, Clear Creek and Summit Counties, Colorado","indexId":"ofr65139","publicationYear":"1965","noYear":false,"title":"Preliminary Report on the Engineering Geology of the Straight Creek Tunnel Pilot Bore, Clear Creek and Summit Counties, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":25017,"text":"pp815 - 1974 - Engineering geologic, geophysical, hydrologic, and rock-mechanics investigations of the Straight Creek Tunnel site and pilot bore, Colorado","indexId":"pp815","publicationYear":"1974","noYear":false,"title":"Engineering geologic, geophysical, hydrologic, and rock-mechanics investigations of the Straight Creek Tunnel site and pilot bore, Colorado"},"id":1}],"supersededBy":{"id":25017,"text":"pp815 - 1974 - Engineering geologic, geophysical, hydrologic, and rock-mechanics investigations of the Straight Creek Tunnel site and pilot bore, Colorado","indexId":"pp815","publicationYear":"1974","noYear":false,"title":"Engineering geologic, geophysical, hydrologic, and rock-mechanics investigations of the Straight Creek Tunnel site and pilot bore, Colorado"},"lastModifiedDate":"2012-02-02T00:06:58","indexId":"ofr65139","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-139","title":"Preliminary Report on the Engineering Geology of the Straight Creek Tunnel Pilot Bore, Clear Creek and Summit Counties, Colorado","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr65139","usgsCitation":"Robinson, C., and Lee, F.T., 1965, Preliminary Report on the Engineering Geology of the Straight Creek Tunnel Pilot Bore, Clear Creek and Summit Counties, Colorado: U.S. Geological Survey Open-File Report 65-139, 34 p. ill., maps ;27 cm., https://doi.org/10.3133/ofr65139.","productDescription":"34 p. ill., maps ;27 cm.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":147898,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":44676,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0139/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44677,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0139/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44678,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0139/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44679,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0139/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44680,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0139/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44681,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0139/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44682,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0139/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44683,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0139/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44684,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0139/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44685,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0139/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44686,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0139/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e462","contributors":{"authors":[{"text":"Robinson, Charles Sherwood 0000-0002-7623-2380","orcid":"https://orcid.org/0000-0002-7623-2380","contributorId":71163,"corporation":false,"usgs":true,"family":"Robinson","given":"Charles Sherwood","affiliations":[],"preferred":false,"id":171552,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lee, Fitzhugh T.","contributorId":82272,"corporation":false,"usgs":true,"family":"Lee","given":"Fitzhugh","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":171553,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":47150,"text":"ofr6566 - 1965 - Geologic map and sections for the Columbia Basin Irrigation Project area, Washington","interactions":[{"subject":{"id":47150,"text":"ofr6566 - 1965 - Geologic map and sections for the Columbia Basin Irrigation Project area, Washington","indexId":"ofr6566","publicationYear":"1965","noYear":false,"title":"Geologic map and sections for the Columbia Basin Irrigation Project area, Washington"},"predicate":"SUPERSEDED_BY","object":{"id":66013,"text":"i589 - 1971 - Geologic map and sections of parts of Grant, Adams, and Franklin Counties, Washington","indexId":"i589","publicationYear":"1971","noYear":false,"title":"Geologic map and sections of parts of Grant, Adams, and Franklin Counties, Washington"},"id":1}],"supersededBy":{"id":66013,"text":"i589 - 1971 - Geologic map and sections of parts of Grant, Adams, and Franklin Counties, Washington","indexId":"i589","publicationYear":"1971","noYear":false,"title":"Geologic map and sections of parts of Grant, Adams, and Franklin Counties, Washington"},"lastModifiedDate":"2012-02-02T00:10:56","indexId":"ofr6566","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-66","title":"Geologic map and sections for the Columbia Basin Irrigation Project area, Washington","language":"ENGLISH","doi":"10.3133/ofr6566","usgsCitation":"Grolier, M.J., and Bingham, J., 1965, Geologic map and sections for the Columbia Basin Irrigation Project area, Washington: U.S. Geological Survey Open-File Report 65-66, 1 map on two sheets., https://doi.org/10.3133/ofr6566.","productDescription":"1 map on two sheets.","costCenters":[],"links":[{"id":167894,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"62500","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a48e3","contributors":{"authors":[{"text":"Grolier, Maurice J.","contributorId":98292,"corporation":false,"usgs":true,"family":"Grolier","given":"Maurice","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":234713,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bingham, J.W.","contributorId":35295,"corporation":false,"usgs":true,"family":"Bingham","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":234712,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24283,"text":"ofr65131 - 1965 - Floods of December 1964 in the far western States","interactions":[],"lastModifiedDate":"2012-02-02T00:08:01","indexId":"ofr65131","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-131","title":"Floods of December 1964 in the far western States","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/ofr65131","issn":"0094-9140","usgsCitation":"Rantz, S., and Moore, A., 1965, Floods of December 1964 in the far western States: U.S. Geological Survey Open-File Report 65-131, vi, 112 p. :ill., maps ; c 27 cm., https://doi.org/10.3133/ofr65131.","productDescription":"vi, 112 p. :ill., maps ; c 27 cm.","costCenters":[],"links":[{"id":155017,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d9e4b07f02db5dfdfb","contributors":{"authors":[{"text":"Rantz, S. E.","contributorId":34106,"corporation":false,"usgs":true,"family":"Rantz","given":"S. E.","affiliations":[],"preferred":false,"id":191625,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, A.M.","contributorId":87909,"corporation":false,"usgs":true,"family":"Moore","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":191626,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":20475,"text":"ofr65124 - 1965 - Tectonic deformation, subaqueous slides, and destructive waves associated with the Alaskan March 27, 1964, earthquake: an interim geologic evaluation","interactions":[],"lastModifiedDate":"2023-09-05T20:16:11.95009","indexId":"ofr65124","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-124","title":"Tectonic deformation, subaqueous slides, and destructive waves associated with the Alaskan March 27, 1964, earthquake: an interim geologic evaluation","docAbstract":"<p>The great earthquake which struck Alaska on Good Friday, March 27, 1964, caused severe damage to the coast of south-central Alaska mainly through vertical tectonic displacements, subaqueous slides, and destructive waves of diverse origins.</p><p>Notable changes in land level occurred over an area in excess of 50,000 square miles in a broad northeast-trending belt more than 500 miles long and as much as 250 miles wide, which lies between the Aleutian Trench and the Aleutian Volcanic Arc. The northwest part of this belt, which includes most of the Kenai Peninsula and the Kodiak Island group, sank as much as 7 feet, bringing some roads, rail lines, docks, and settlements within reach of high tides and producing a fringe of salt-water-killed vegetation along the drowned coasts. The area to the southeast, including most of Prince William Sound and the adjacent continental shelf as far south as southern Kodiak Island, rose generally 4 to 8 feet, and locally at least 33 feet. Some beaches and surf-cut platforms were permanently raised above the reach of tides, resulting in mass extermination of intertidal faunas and floras and impaired usefulness of harbors, channels, and many shoreline installations.</p><p>Surface faulting was confined to Montague Island, and was dominantly vertical and subsidiary to regional uplift. Of the two known faults one has been traced more than 16 miles on land and about 15 miles in the submarine topography to the southwest of the island. Maximum measured vertical fault displacement on land was 16 feet on one fault and about 18 feet on the other.</p><p>Submarine uplift of the continental shelf generated a train of long-period large-amplitude seismic sea waves, the first of which struck the outer coasts of the Kenai Peninsula and Kodiak Island between 19 and 30 minutes after the initial shock. The highest waves inundated shorelines locally to elevations of 35 to 40 feet, causing 20 deaths and damage to property all along the coast of the Gulf of Alaska, especially in those areas that had been lowered relative to sea level by tectonic subsidence. The sea waves were recorded on tide gauges throughout the Pacific Ocean and resulted in casualties and local damage at points as distant as British Columbia, Oregon, and California.</p><p>The earthquake caused widespread subaqueous sliding and sedimentation in Prince William Sound, along the south coast of the Kenai Peninsula, and in Kenai Lake. These slides carried away the port facilities of Seward and Valdez and the small boat harbor at Homer. Local violent surges of water, many of which were generated by known subaqueous slides that occurred during the earthquake, left swash marks as much as 170 feet above water level and caused heavy damage and took 85 lives at Seward, Valdez, Whittier, Chenega, and several smaller communities in Prince William Sound.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr65124","usgsCitation":"Plafker, G., and Mayo, L., 1965, Tectonic deformation, subaqueous slides, and destructive waves associated with the Alaskan March 27, 1964, earthquake: an interim geologic evaluation: U.S. Geological Survey Open-File Report 65-124, 19 p., https://doi.org/10.3133/ofr65124.","productDescription":"19 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,{"id":41801,"text":"ofr65128 - 1965 - Approximate location of fault traces and historic surface ruptures within the Hayward fault zone between San Pablo and Warm Springs, California","interactions":[{"subject":{"id":41801,"text":"ofr65128 - 1965 - Approximate location of fault traces and historic surface ruptures within the Hayward fault zone between San Pablo and Warm Springs, California","indexId":"ofr65128","publicationYear":"1965","noYear":false,"title":"Approximate location of fault traces and historic surface ruptures within the Hayward fault zone between San Pablo and Warm Springs, California"},"predicate":"SUPERSEDED_BY","object":{"id":66878,"text":"i522 - 1967 - Approximate location of fault traces and historic surface ruptures within the Hayward fault zone between San Pablo and Warm Springs, California","indexId":"i522","publicationYear":"1967","noYear":false,"title":"Approximate location of fault traces and historic surface ruptures within the Hayward fault zone between San Pablo and Warm Springs, California"},"id":1}],"supersededBy":{"id":66878,"text":"i522 - 1967 - Approximate location of fault traces and historic surface ruptures within the Hayward fault zone between San Pablo and Warm Springs, California","indexId":"i522","publicationYear":"1967","noYear":false,"title":"Approximate location of fault traces and historic surface ruptures within the Hayward fault zone between San Pablo and Warm Springs, California"},"lastModifiedDate":"2020-02-05T15:27:04","indexId":"ofr65128","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-128","title":"Approximate location of fault traces and historic surface ruptures within the Hayward fault zone between San Pablo and Warm Springs, California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr65128","usgsCitation":"Radbruch-Hall, D.H., 1965, Approximate location of fault traces and historic surface ruptures within the Hayward fault zone between San Pablo and Warm Springs, California: U.S. Geological Survey Open-File Report 65-128, 1 Plate: 30.15 x 48.95 inches, https://doi.org/10.3133/ofr65128.","productDescription":"1 Plate: 30.15 x 48.95 inches","costCenters":[],"links":[{"id":372086,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0128/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":169037,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1965/0128/report-thumb.jpg"}],"scale":"62500","country":"United States","state":"California","city":"San Pablo, Warm Springs","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.70629882812499,\n              37.431250501793585\n            ],\n            [\n              -121.85760498046875,\n              37.431250501793585\n            ],\n            [\n              -121.85760498046875,\n              37.972349871995256\n            ],\n            [\n              -122.70629882812499,\n              37.972349871995256\n            ],\n            [\n              -122.70629882812499,\n              37.431250501793585\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a212","contributors":{"authors":[{"text":"Radbruch-Hall, Dorothy H.","contributorId":102462,"corporation":false,"usgs":true,"family":"Radbruch-Hall","given":"Dorothy","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":225549,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14179,"text":"ofr6576 - 1965 - Preliminary materials map, Windsor quadrangle","interactions":[],"lastModifiedDate":"2022-03-24T21:47:10.935936","indexId":"ofr6576","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-76","title":"Preliminary materials map, Windsor quadrangle","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6576","usgsCitation":"Holmes, G.W., 1965, Preliminary materials map, Windsor quadrangle: U.S. Geological Survey Open-File Report 65-76, Report: 4 p.; 1 Plate: 26.12 × 27.69 inches, https://doi.org/10.3133/ofr6576.","productDescription":"Report: 4 p.; 1 Plate: 26.12 × 27.69 inches","costCenters":[],"links":[{"id":144677,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1965/0076/report-thumb.jpg"},{"id":42844,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0076/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42845,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1965/0076/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":390500,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8111.htm"}],"scale":"24000","country":"United States","state":"Massachusetts","otherGeospatial":"Windsor quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73.125,\n              42.5\n            ],\n            [\n              -73,\n              42.5\n            ],\n            [\n              -73,\n              42.625\n            ],\n            [\n              -73.125,\n              42.625\n            ],\n            [\n              -73.125,\n              42.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cdf1","contributors":{"authors":[{"text":"Holmes, George William","contributorId":79107,"corporation":false,"usgs":true,"family":"Holmes","given":"George","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":169035,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15761,"text":"ofr65142 - 1965 - Geology and ore deposits of the central York Mountains, western Seward Peninsula, Alaska","interactions":[{"subject":{"id":15761,"text":"ofr65142 - 1965 - Geology and ore deposits of the central York Mountains, western Seward Peninsula, Alaska","indexId":"ofr65142","publicationYear":"1965","noYear":false,"title":"Geology and ore deposits of the central York Mountains, western Seward Peninsula, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":35708,"text":"b1287 - 1969 - Geology and ore deposits of the Central York Mountains, western Seward Peninsula, Alaska","indexId":"b1287","publicationYear":"1969","noYear":false,"title":"Geology and ore deposits of the Central York Mountains, western Seward Peninsula, Alaska"},"id":1}],"supersededBy":{"id":35708,"text":"b1287 - 1969 - Geology and ore deposits of the Central York Mountains, western Seward Peninsula, Alaska","indexId":"b1287","publicationYear":"1969","noYear":false,"title":"Geology and ore deposits of the Central York Mountains, western Seward Peninsula, Alaska"},"lastModifiedDate":"2024-05-20T19:22:29.519521","indexId":"ofr65142","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-142","title":"Geology and ore deposits of the central York Mountains, western Seward Peninsula, Alaska","docAbstract":"<p>In the central York Mountains, carbonate rocks of Lower and Middle Ordovician age and aggregating at least 8,000 feet thick are thrust northward over slate and argillaceous limestone of pre-Ordovician age which were intruded by gabbro in pre-Ordovician time. Normal faults of four distinct systems cut the thrust plates, and in Late Cretaceous time, stocks of biotite granite, abnormally rich in beryllium, tin, boron and certain other trace elements, pierced the thrust plates. In part following the intrusion of the granites, a strong set of normal faults developed striking N. 60°-85° E. through the central York Mountains and locally these faults cut the granites. Dikes of granite, rhyolite porphyry, and lamprophyre were injected into some of these faults, the lamprophyres being younger. Trace elements in the lamprophyres prove they are mafic rocks probably derived from the lama, and that they cannot be related genetically to granite. Shortly after the intrusion of lamprophyre dikes, ore deposits of tin, beryllium, and fluorite were formed from solutions probably derived from deeply-buried hot granite where the granite was ruptured by normal faults. Ore shoots were localized beneath thrust faults where the faults are intruded by dikes, and a major ore-bearing structure, the Rapid River fault, is mineralized for half its length for a distance of eight miles. The tin deposits contain cassiterite and stannite in topaz greisen with abundant sulfides of copper, lead, zinc, and iron, as well as wolframite. The beryllium deposits contain fluorite, chrysoberyl, diaspore, muscovite, and tourmaline, with trace to small amounts of euclase, bertrandite, helvite, phenikite(?), todorokite and hematite. Beryl occurs sparingly in late veins of quartz and fluorite. Chrysoberyl is the earliest and commonest beryllium mineral, followed by euclase and bertrandite, and then phenakite(?) and beryl. Helvite is restricted to banded skarns near granite, and which consist of magnetite and fluorite. Throughout the district, a strong zonation is displayed from tin deposits in greisen through transitional veins of sulfide minerals with fluorite and chrysoberyl to fluorite-beryllium deposits and thence to barren veins of silica and fluorite with trace amounts of beryllium. This zonal arrangement of deposits probably will be found elsewhere in the world where greisen tin deposits occur in carbonate rocks. The geochemical cycle of the trace elements Be, Sn, W, B, Li, Cu, Pb, Zn and Nb shows that these elements were enriched in the biotite granites and were strongly fractionated among the minerals of granites. Fran the granites, these rare elements moved outward into contact rocks and ore deposits. During the supergene cycle, clear geochemical anomalies were formed in stream sediments, soils and plants near ore deposits, and geochemical prospecting led to the discovery of the beryllium lodes. With the possible exception of zinc and niobium, the rare elements that are associated in the rocks and ores remain associated in the supergene processes. Fixation of zinc in clay soil and tundra plants may account for the relatively small amount of zinc in strew sediments.</p><p>Datable Pleistocene events in the York Mountains begin with the Yarmouth Interglaciation when the York Terrace, a wide marine platform, was cut. In Illinoian time, the York Terrace was uplifted almost 400 feet, and during the Sangamon Interglaciation a second marine platform (Lost River Terrace) was cut and is not deformed. During Wisconsin time the widespread York Glaciation was followed by the more restricted Mint River Glaciation. Because uplift of the York Terrace extended into the Bering Strait, it is probable that prior to the uplift in Illinoian time the Bering Strait was a seaway and a barrier to land migration rather than a land bridge.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr65142","usgsCitation":"Sainsbury, C., 1965, Geology and ore deposits of the central York Mountains, western Seward Peninsula, Alaska: U.S. Geological Survey Open-File Report 65-142, Report: 149 p.; 15 Plates: 20.55 x 27.89 inches or smaller; 8 Tables: 20.88 x 30.29 inches or smaller, https://doi.org/10.3133/ofr65142.","productDescription":"Report: 149 p.; 15 Plates: 20.55 x 27.89 inches or smaller; 8 Tables: 20.88 x 30.29 inches or 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States","state":"Alaska","otherGeospatial":"central York Mountains, western Seward Peninsula","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -167.56430004060184,\n              65.60933402498489\n            ],\n            [\n              -167.56430004060184,\n              65.36714034542257\n            ],\n            [\n              -166.82167890236178,\n              65.36714034542257\n            ],\n            [\n              -166.82167890236178,\n              65.60933402498489\n            ],\n            [\n              -167.56430004060184,\n              65.60933402498489\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  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,{"id":15753,"text":"ofr65141 - 1965 - Geology of the Romanzof Mountains, Brooks Range, northeastern Alaska","interactions":[{"subject":{"id":15753,"text":"ofr65141 - 1965 - Geology of the Romanzof Mountains, Brooks Range, northeastern Alaska","indexId":"ofr65141","publicationYear":"1965","noYear":false,"title":"Geology of the Romanzof Mountains, Brooks Range, northeastern Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":6313,"text":"pp897 - 1977 - Geology of the western Romanzof Mountains, Brooks Range, northeastern Alaska","indexId":"pp897","publicationYear":"1977","noYear":false,"title":"Geology of the western Romanzof Mountains, Brooks Range, northeastern Alaska"},"id":1},{"subject":{"id":15754,"text":"ofr59106 - 1959 - Preliminary report on sedimentary and metamorphic rocks in part of the Romanzof Mountains, Brooks Range, northeastern Alaska","indexId":"ofr59106","publicationYear":"1959","noYear":false,"title":"Preliminary report on sedimentary and metamorphic rocks in part of the Romanzof Mountains, Brooks Range, northeastern Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":15753,"text":"ofr65141 - 1965 - Geology of the Romanzof Mountains, Brooks Range, northeastern Alaska","indexId":"ofr65141","publicationYear":"1965","noYear":false,"title":"Geology of the Romanzof Mountains, Brooks Range, northeastern Alaska"},"id":2}],"supersededBy":{"id":6313,"text":"pp897 - 1977 - Geology of the western Romanzof Mountains, Brooks Range, northeastern Alaska","indexId":"pp897","publicationYear":"1977","noYear":false,"title":"Geology of the western Romanzof Mountains, Brooks Range, northeastern Alaska"},"lastModifiedDate":"2024-03-25T18:59:14.568941","indexId":"ofr65141","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-141","title":"Geology of the Romanzof Mountains, Brooks Range, northeastern Alaska","docAbstract":"<p>This remote 700 square mile area in the Brooks Range is topographically rugged and geologically diverse; it contains a granitic pluton, low-grade metamorphic rocks, sedimentary rocks, and mafic igneous rocks, as well as glacial features.</p><p>Rocks of sedimentary origin include from oldest to youngest:</p><p>1.Neruokpuk Formation Middle and Upper Devonian(?), more than 4000 feet thick, a variety of units which represent the greenschist facies, including quartzitic- and schistose-feldspathic graywacke; phyllite, argillite, and slate, as well as dark limestone, sandy limestone, and silicified carbonate rocks. The succession of units in parts of the area is uncertain. Correlations between these units and with others in the eastern Brooks Range are provisional.</p><p>2.Kekiktuk Conglomerate and Kayak(?) Shale (Upper Devonian(?) to Upper Mississippian), a single map unit, from absent(?) to 400+ feet thick, containing dark shale Kayak(?) in its uppermost part and quartzite, interbedded dark shale, and some pebble- to boulder-conglomerate in the locally absent lower part (Kekiktuk). The unit overlies the Neruokpuk with angular unconformity, which may reflect either a pre-Kayak(?) or pre-Kekiktuk hiatus or both.</p><p>3.Lisburne Group, almost entirely carbonate rocks, and relatively thin in this area, 600 to 800 feet thick. Alapah Limestone (Upper Mississippian), to 560 feet thick, includes gray sandy, crystalline, and cherty limestone; minor dark shale; and dark cherty carbonate rocks in the upper part. The lower contact is gradational with the Kayak(?). Wahoo(?) Limestone (Pennsylvanian(?) to Permian) conformably overlies the Alapah, is absent to 200+ feet thick, and is characterized by light-gray crinoidal limestones in its upper part.</p><p>4. Sadlerochit Formation, consisting of three intraconformable units: ferruginous sandstone member (Permian) of ironstained orthoquartzite and dark slate, 175 to 240 feet thick which unconformably overlies the Wahoo(?) and Alapah Limestones; shale member of dark shale, slate, and minor quartzite averaging 400 feet in thickness; and quartzite member (Lower(?) Triassic), 700 feet thick, mostly orthoquartzite with minor shale and conglomerate. The basal clastics were probably shed from the north.</p><p>5.Shublik Formation (Middle(?) and Upper Triassic), 600 to 700 feet thick, with the thin phosphatic sandstone member overlain by dark phosphatic limestones and limy shales of the limestone member.</p><p>6.Kingak Formation (Jurassic), more than 1000 feet thick. The siltstone member, resistant sandstone and siltstone 75 to 150 feet thick, is overlain by an undetermined thickness of black shale. The basal part contrasts sharply with the underlying Shublik, indicating possible disconformity.</p><p>7.Ignek(?) Formation (Cretaceous), represented in the foothills where lithic graywacke, shale, and coaly shale constitute the few exposures examined.</p><p>8.Glacial and glaciofluvial materials of five advances recognized on the basis of morphology and position, which are tentatively correlated with five glaciations 15 miles west of the area.</p><p>9. Recent alluvial and colluvial deposits including fans which appear to represent at least three stages of encroachment.<br></p><p>The Ramanzof granite, exposed in the Okpilak batholith and Jago stock, is mostly light-gray quartz monzonite to granite, and contains essential quartz, perthitic microcline, albite-oligoclase, and partly chloritized biotite. Limited modal and chemical data are presented. Three textural facies are: 1) porphyritic (marginal), with abundant large microcline megacrysts; 2) variable (middle to marginal), which exhibits textural and mineralogical banding; and 3) coarse (inner to marginal), which is gneissoid to equigranular. Facies relationships appear to be mostly gradational but may be locally intrusive. Some schistose metasedimentary(?) rock occurs in the granite. Aplite dikes, inclusions, tourmaline veins and replacements, and chlorite and quartz veins are locally common, as well as quartz monzonite and mafic igneous dikes. Contacts with Neruokpuk Formation rocks are mostly abrupt, concordant to cross-cutting, and locally adjoin tactite and hornfels of the albite-epidote-hornfels and hornblende-hornfels facies. Contacts with Kekiktuk Conglomerate are apparently gradational through a schistoze zone. Both primary and secondary structural elements are present in the Romanzof in granite. Textural and mineralogical banding and, in general, feldspar foliation are considered to be primary in origin; biotite foliation, gneissic and schistose foliation, and schistose zones are considered secondary. Lead-alpha age of zircons appears to be Late Devonian, K-Ar age of biotite is Cretaceous, possibly indicating updating by later reheating. Field age relationships are inconclusive but suggest pre-Kayak(?) (Upper Devonian) granite emplacement. The pluton is interpreted to be essentially the product of melt crystallization, synorogenically emplaced by forceful injection with minor stoping, and may include marginally granitized rock.<br></p><p>Mafic igneous rocks of altered basaltic composition (greenstones) include dikes in granitic and Neruokpuk Formation rocks, and volcanics(?). A late Paleozoic age is suggested for them.</p><p>Structural grain strikes east-northeast; south-dipping elements are common. Structures include the major positive nature of the area (first order), relatively broad folds (second order) which contain small tight folds (third order). Related south-dipping cleavage, schistosity, and biotite foliation in granite in the northern part of the area are cut by prominent sets of transverse joints and faults. Other features are longitudinal normal and reverse faults, at least one large-scale overthrust fault, and sheared zones in granite with possible attendant retrograde metamorphism.</p><p>Although Mesozoic and Tertiary deformational features are dominant in northern Alaska, the Romanzof area may have been part of a Late Devonian orogenic belt continuous with one in northern Canada. Three alternate trends of such a belt in northern Alaska are discussed, but evidence is inconclusive.</p><p>The mineral potential of the area is largely unknown. Minor amounts of metallic sulfides and oxides are present in granite and Neruokpuk Formation rocks. Analyses of stream silt samples suggest the possibility of tin and beryllium potential. The Shublik Formation contains rock phosphate.</p><p><br data-mce-bogus=\"1\"></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr65141","usgsCitation":"Sable, E.G., 1965, Geology of the Romanzof Mountains, Brooks Range, northeastern Alaska: U.S. Geological Survey Open-File Report 65-141, Report: x, 218 p.; 7 Plates: 35.95 x 37.74 inches or smaller, https://doi.org/10.3133/ofr65141.","productDescription":"Report: x, 218 p.; 7 Plates: 35.95 x 37.74 inches or smaller","costCenters":[],"links":[{"id":427049,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0141/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427048,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0141/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427047,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0141/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427046,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0141/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427045,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0141/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427044,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0141/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427043,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0141/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427042,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1965/0141/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148683,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1965/0141/report-thumb.jpg"}],"scale":"63360","country":"United States","state":"Alaska","otherGeospatial":"Brooks Range, Romanzof Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -144.61982095290645,\n              69.45543761208387\n            ],\n            [\n              -144.61982095290645,\n              68.6489771949642\n            ],\n            [\n              -142.45135071338586,\n              68.6489771949642\n            ],\n            [\n              -142.45135071338586,\n              69.45543761208387\n            ],\n            [\n              -144.61982095290645,\n              69.45543761208387\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e733","contributors":{"authors":[{"text":"Sable, Edward G.","contributorId":51273,"corporation":false,"usgs":true,"family":"Sable","given":"Edward","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":171648,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":40923,"text":"ofr65174 - 1965 - Preliminary geologic map of the Black Butte iron deposit, Madison County, Montana","interactions":[],"lastModifiedDate":"2025-09-25T19:54:22.461781","indexId":"ofr65174","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-174","title":"Preliminary geologic map of the Black Butte iron deposit, Madison County, Montana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr65174","usgsCitation":"Wier, K.L., 1965, Preliminary geologic map of the Black Butte iron deposit, Madison County, Montana: U.S. Geological Survey Open-File Report 65-174, 2 Plates: 30.30 x 48.95 inches and 6.24 x 23.32 inches, https://doi.org/10.3133/ofr65174.","productDescription":"2 Plates: 30.30 x 48.95 inches and 6.24 x 23.32 inches","costCenters":[],"links":[{"id":172202,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":78816,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0174/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":78817,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0174/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":496179,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8095.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"9600","country":"United States","state":"Montana","county":"Madison County","otherGeospatial":"Black Butte iron deposit","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -111.772,\n              44.933\n            ],\n            [\n              -111.772,\n              44.807\n            ],\n            [\n              -111.683,\n              44.807\n            ],\n            [\n              -111.683,\n              44.933\n            ],\n            [\n              -111.772,\n              44.933\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bccb","contributors":{"authors":[{"text":"Wier, K. L.","contributorId":106864,"corporation":false,"usgs":true,"family":"Wier","given":"K.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":224187,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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