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,{"id":34981,"text":"b1201D - 1965 - Chemical comparison of glassy and crystalline volcanic rocks","interactions":[],"lastModifiedDate":"2012-02-02T00:09:49","indexId":"b1201D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1201","chapter":"D","title":"Chemical comparison of glassy and crystalline volcanic rocks","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/b1201D","usgsCitation":"Lipman, P.W., 1965, Chemical comparison of glassy and crystalline volcanic rocks: U.S. Geological Survey Bulletin 1201, p. D1-D24, ill. ;24 cm., https://doi.org/10.3133/b1201D.","productDescription":"p. D1-D24, ill. ;24 cm.","costCenters":[],"links":[{"id":165065,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1201d/report-thumb.jpg"},{"id":62932,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1201d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e0e4b07f02db5e437f","contributors":{"authors":[{"text":"Lipman, Peter W. 0000-0001-9175-6118 plipman@usgs.gov","orcid":"https://orcid.org/0000-0001-9175-6118","contributorId":3486,"corporation":false,"usgs":true,"family":"Lipman","given":"Peter","email":"plipman@usgs.gov","middleInitial":"W.","affiliations":[{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":213929,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":34506,"text":"b1175 - 1965 - Geology of the Cortez quadrangle, Nevada, with a section on gravity and aeromagnetic surveys","interactions":[],"lastModifiedDate":"2022-09-14T18:49:34.264534","indexId":"b1175","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1175","title":"Geology of the Cortez quadrangle, Nevada, with a section on gravity and aeromagnetic surveys","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1175","usgsCitation":"Gilluly, J., and Masursky, H., 1965, Geology of the Cortez quadrangle, Nevada, with a section on gravity and aeromagnetic surveys: U.S. Geological Survey Bulletin 1175, Report: v, 117 p.; 3 Plates: 31.61 × 33.25 inches or smaller, https://doi.org/10.3133/b1175.","productDescription":"Report: v, 117 p.; 3 Plates: 31.61 × 33.25 inches or smaller","costCenters":[],"links":[{"id":92798,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1175/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":92797,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1175/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":92800,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1175/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":92799,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1175/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":109462,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20941.htm","linkFileType":{"id":5,"text":"html"},"description":"20941"},{"id":164135,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1175/report-thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Cortez quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.75,\n              40\n            ],\n            [\n              -116.5,\n              40\n            ],\n            [\n              -116.5,\n              40.25\n            ],\n            [\n              -116.75,\n              40.25\n            ],\n            [\n              -116.75,\n              40\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db68306d","contributors":{"authors":[{"text":"Gilluly, James","contributorId":51743,"corporation":false,"usgs":true,"family":"Gilluly","given":"James","email":"","affiliations":[],"preferred":false,"id":213079,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Masursky, Harold","contributorId":94304,"corporation":false,"usgs":true,"family":"Masursky","given":"Harold","email":"","affiliations":[],"preferred":false,"id":213080,"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":64193,"text":"gp523 - 1965 - Aeromagnetic map of northeastern Illinois and its geologic interpretation","interactions":[],"lastModifiedDate":"2023-03-21T19:33:12.617145","indexId":"gp523","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"523","title":"Aeromagnetic map of northeastern Illinois and its geologic interpretation","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp523","usgsCitation":"Beck, M.E., 1965, Aeromagnetic map of northeastern Illinois and its geologic interpretation: U.S. Geological Survey Geophysical Investigations Map 523, Report: 6 p.; 1 Plate: 27.21 x 38.59 inches, https://doi.org/10.3133/gp523.","productDescription":"Report: 6 p.; 1 Plate: 27.21 x 38.59 inches","costCenters":[],"links":[{"id":414487,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3476.htm","linkFileType":{"id":5,"text":"html"}},{"id":254160,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0523/report-thumb.jpg"},{"id":250727,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0523/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":250726,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0523/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Illinois","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.25,\n              40.7\n            ],\n            [\n              -89.25,\n              42.5\n            ],\n            [\n              -87.5,\n              42.5\n            ],\n            [\n              -87.5,\n              40.7\n            ],\n            [\n              -89.25,\n              40.7\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697e15","contributors":{"authors":[{"text":"Beck, M. E. Jr.","contributorId":58354,"corporation":false,"usgs":true,"family":"Beck","given":"M.","suffix":"Jr.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":270170,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":63026,"text":"gq426 - 1965 - Bedrock geologic map of the Ansonia quadrangle, Fairfield and New Haven Counties, Connecticut","interactions":[],"lastModifiedDate":"2012-02-10T00:10:46","indexId":"gq426","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"426","title":"Bedrock geologic map of the Ansonia quadrangle, Fairfield and New Haven Counties, Connecticut","language":"ENGLISH","doi":"10.3133/gq426","usgsCitation":"Fritts, C., 1965, Bedrock geologic map of the Ansonia quadrangle, Fairfield and New Haven Counties, Connecticut: U.S. Geological Survey Geologic Quadrangle 426, 1 map., https://doi.org/10.3133/gq426.","productDescription":"1 map.","costCenters":[],"links":[{"id":102446,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_895.htm","linkFileType":{"id":5,"text":"html"},"description":"895"},{"id":180095,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -73.11749999999999,41.25 ], [ -73.11749999999999,41.3675 ], [ -73,41.3675 ], [ -73,41.25 ], [ -73.11749999999999,41.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6be4b07f02db63d99d","contributors":{"authors":[{"text":"Fritts, Crawford E.","contributorId":87619,"corporation":false,"usgs":true,"family":"Fritts","given":"Crawford E.","affiliations":[],"preferred":false,"id":268215,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":47103,"text":"ofr6565 - 1965 - Geologic map and cross sections of the Nelchina area, south-central Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:10:47","indexId":"ofr6565","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":"65-65","title":"Geologic map and cross sections of the Nelchina area, south-central Alaska","language":"ENGLISH","doi":"10.3133/ofr6565","usgsCitation":"Grantz, A., 1965, Geologic map and cross sections of the Nelchina area, south-central Alaska: U.S. Geological Survey Open-File Report 65-65, 1 map on four sheets, https://doi.org/10.3133/ofr6565.","productDescription":"1 map on four sheets","costCenters":[],"links":[{"id":106360,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8106.htm","linkFileType":{"id":5,"text":"html"},"description":"8106"},{"id":172051,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":99862,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0065/plate-4.pdf","size":"5471","linkFileType":{"id":1,"text":"pdf"}},{"id":99861,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0065/plate-3.pdf","size":"4443","linkFileType":{"id":1,"text":"pdf"}},{"id":99859,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0065/plate-1.pdf","size":"10208","linkFileType":{"id":1,"text":"pdf"}},{"id":99860,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0065/plate-2.pdf","size":"10296","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a49fe","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":234632,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23205,"text":"ofr6564 - 1965 - Streamflow characteristics of the Brazos River basin, Texas","interactions":[],"lastModifiedDate":"2012-02-02T00:07:58","indexId":"ofr6564","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":"65-64","title":"Streamflow characteristics of the Brazos River basin, Texas","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/ofr6564","issn":"0094-9140","usgsCitation":"Goines, W., 1965, Streamflow characteristics of the Brazos River basin, Texas: U.S. Geological Survey Open-File Report 65-64, iii, 50 p. :ill., charts ;28 cm., https://doi.org/10.3133/ofr6564.","productDescription":"iii, 50 p. :ill., charts ;28 cm.","costCenters":[],"links":[{"id":155172,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4e29","contributors":{"authors":[{"text":"Goines, W.H.","contributorId":95088,"corporation":false,"usgs":true,"family":"Goines","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":189632,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52493,"text":"ofr65130 - 1965 - Floods of December 1964 in Redwood areas of north coastal California","interactions":[],"lastModifiedDate":"2025-07-01T15:16:07.355746","indexId":"ofr65130","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":"65-130","title":"Floods of December 1964 in Redwood areas of north coastal California","docAbstract":"<p>The flood of December 1964 in the redwood areas of north coastal California was the most damaging in the history of the area. The flood resulted from a series of storms in late December, but primarily from the warm torrential rainfall of December 21-23. This rainfall reflected the combined effect of moist unstable airmasses, strong west-southwest winds, and mountain ranges oriented nearly at right angles to the flow of air. The magnitude of the rainfall over much of the mountainous area was equal to or greater than that estimated to have an average return period of 100 years. Precipitation totals in excess of 10 inches in 24 hours and 15 inches in 48 hours were commonplace in the mountains and interior valleys. The peak discharge of streams draining these drenched areas was extremely high and also had a return period estimated to be greater than 100 years. By contrast, some of the areas immediately adjacent to the Pacific Ocean had maximum 24-hour rainfalls of only 2 inches and the small streams draining these low-altitude basins experienced rises that were little greater than those that occur during the usual winter storms.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr65130","usgsCitation":"Rantz, S., 1965, Floods of December 1964 in Redwood areas of north coastal California: U.S. Geological Survey Open-File Report 65-130, 39 p., https://doi.org/10.3133/ofr65130.","productDescription":"39 p.","costCenters":[],"links":[{"id":491599,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1965/0130/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":179423,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1965/0130/report-thumb.jpg"}],"country":"United 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d9e4b07f02db5dfdf3","contributors":{"authors":[{"text":"Rantz, S. E.","contributorId":34106,"corporation":false,"usgs":true,"family":"Rantz","given":"S. E.","affiliations":[],"preferred":false,"id":245435,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1231,"text":"wsp1809D - 1965 - An evaluation of aquifer and well characteristics of municipal well fields in Los Alamos and Guaje Canyons, near Los Alamos, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1809D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1809","chapter":"D","title":"An evaluation of aquifer and well characteristics of municipal well fields in Los Alamos and Guaje Canyons, near Los Alamos, New Mexico","docAbstract":"The Jenkins-Whitesburg area includes approximately 250 square miles In Letcher and Pike Counties in the southeastern part of the Eastern Coal Field. In this area ground water is the principal source of water for nearly all rural families, most public supplies, several coal mines and coal processing plants, and one bottling plant. \r\n\r\nThe major aquifers in the Jenkins-Whitesburg area are the Breathitt and Lee Formations of Pennsylvanian age. Other aquifers range in age from Devonian to Quaternary but are not important in this area because they occur at great depth or yield little or no water. The Breathitt Formation occurs throughout the area except along the crest and slopes of Pine Mountain and where it is covered by unconsolidated material of Quaternary age. The Breathitt Formation consists of shale, sandstone, and lesser amounts of coal and associated underclay. The yield of wells penetrating the Breathitt Formation ranges from less than 1 to 330 gallons per minute. Well yield is controlled by the type and depth of well, character of the aquifer, and topography of the well site. Generally, deep wells drilled in valleys of perennial streams offer the best potential for high yields. Although enough water for a minimum domestic supply (more than 100 gallons per day) may be obtained from shale, all high-yielding wells probably obtain water from vertical joints and from bedding planes which are best developed in sandstone. About 13 percent of the wells inventoried in the Breathitt Formation failed to supply enough water for a minimum domestic supply. Most of these are shallow dug wells or drilled wells on hillsides or hilltops. Abandoned coal dunes are utilized as large infiltration galleries and furnish part of the water for several public supplies. \r\n\r\nThe chemical quality of water from the Breathitt Formation varies considerably from place to place, but the water generally is acceptable for most domestic and industrial uses. Most water is a calcium magnesium bicarbonate or sodium bicarbonate type, and nearly all sampled water contained enough iron to stain cooking and laundry utensils. The water ranged from soft to very hard, and only one well in the Breathitt Formation produced salty water. The absence of salty water may be due to abundant fractures which are associated with the Pine Mountain fault and which have allowed fresh water to enter the formation. The Lee Formation underlies the Cumberland Mountain section and is exposed along the crest and southeast slope of Pine Mountain. The Lee Formation consists of massive sandstone and conglomerate with thin beds of shale and a few thin coal seams.\r\n\r\nAlthough the Lee Formation is tapped by only a few wells in this area, it is potentially an important aquifer. Wells penetrating the Lee Formation in the Cumberland Mountain section would probably yield water under artesian pressure.\r\n\r\nUnlike most water from the Lee Formation in other part.3 of eastern Kentucky, all water from the Lee Formation in the Jenkins-Whitesburg area is fresh. All water from the Lee Formation contained more than 0.3 parts per million of iron and ranged from soft to moderately hard.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1809D","usgsCitation":"Cushman, R., 1965, An evaluation of aquifer and well characteristics of municipal well fields in Los Alamos and Guaje Canyons, near Los Alamos, New Mexico: U.S. Geological Survey Water Supply Paper 1809, v, 50 p. :ill., maps ;24 cm. + plates folded in pocket., https://doi.org/10.3133/wsp1809D.","productDescription":"v, 50 p. :ill., maps ;24 cm. + plates folded in pocket.","costCenters":[],"links":[{"id":138069,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1809d/report-thumb.jpg"},{"id":26149,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26150,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809d/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26151,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809d/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26152,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809d/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26153,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1809d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db684a57","contributors":{"authors":[{"text":"Cushman, Robert L.","contributorId":22751,"corporation":false,"usgs":true,"family":"Cushman","given":"Robert L.","affiliations":[],"preferred":false,"id":143410,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1234,"text":"wsp1499J - 1965 - Water resources of the Waterbury-Bristol area, Connecticut","interactions":[],"lastModifiedDate":"2022-12-19T21:28:50.027076","indexId":"wsp1499J","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1499","chapter":"J","title":"Water resources of the Waterbury-Bristol area, Connecticut","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1499J","usgsCitation":"Cushman, R.V., Pauszek, F.H., Randall, A., and Thomas, M.P., 1965, Water resources of the Waterbury-Bristol area, Connecticut: U.S. Geological Survey Water Supply Paper 1499, Report: v, 86 p.; 1 Plate: 24.00 × 39.44 inches, https://doi.org/10.3133/wsp1499J.","productDescription":"Report: v, 86 p.; 1 Plate: 24.00 × 39.44 inches","costCenters":[],"links":[{"id":410737,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24446.htm","linkFileType":{"id":5,"text":"html"}},{"id":26162,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1499j/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26161,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1499j/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138072,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1499j/report-thumb.jpg"}],"country":"United States","state":"Connecticut","city":"Bristol, Waterbury","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -72.881,\n              41.722\n            ],\n            [\n              -73.095,\n              41.722\n            ],\n            [\n              -73.095,\n              41.514\n            ],\n            [\n              -72.881,\n              41.514\n            ],\n            [\n              -72.881,\n              41.722\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f02d9","contributors":{"authors":[{"text":"Cushman, Robert Vittum","contributorId":96661,"corporation":false,"usgs":true,"family":"Cushman","given":"Robert","email":"","middleInitial":"Vittum","affiliations":[],"preferred":false,"id":143418,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pauszek, F. H.","contributorId":61399,"corporation":false,"usgs":true,"family":"Pauszek","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":143415,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Randall, A. D.","contributorId":81077,"corporation":false,"usgs":true,"family":"Randall","given":"A. D.","affiliations":[],"preferred":false,"id":143417,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Thomas, M. P.","contributorId":62574,"corporation":false,"usgs":true,"family":"Thomas","given":"M.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":143416,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":34085,"text":"b1221A - 1965 - Rockfalls and Avalanches from Little Tahoma Peak on Mount Rainier, Washington","interactions":[],"lastModifiedDate":"2012-02-10T00:10:09","indexId":"b1221A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1221","chapter":"A","title":"Rockfalls and Avalanches from Little Tahoma Peak on Mount Rainier, Washington","docAbstract":"In December 1963 rockfalls from Little Tahoma Peak on the east side of Mount Rainier volcano fell onto Emmons Glacier and formed avalanches of rock debris that traveled about 4 miles down the glacier and the White River valley. In this distance, the rock debris descended as much as 6,200 feet in altitude. Minor lithologic differences and crosscutting relations indicate that the rockfalls caused at least seven separate avalanches, having an estimated total volume of 14 million cubic yards. The initial rockfall may have been caused by a small steam explosion near the base of Little Tahoma Peak.\r\n\r\nDuring movement, some of the avalanches were deflected from one side of the valley to the other. Calculations based on the height to which the avalanches rose on the valley walls suggest that their velocity reached at least 80 or 90 miles per hour. The unusually long distance some of the avalanches were transported is attributed to a cushion of trapped and compressed air at their base, which buoyed them up amid reduced friction.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/b1221A","usgsCitation":"Crandell, D.R., and Fahnestock, R.K., 1965, Rockfalls and Avalanches from Little Tahoma Peak on Mount Rainier, Washington: U.S. Geological Survey Bulletin 1221, p. A1-A30, https://doi.org/10.3133/b1221A.","productDescription":"p. A1-A30","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":96251,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1221a/report.pdf","size":"5958","linkFileType":{"id":1,"text":"pdf"}},{"id":163980,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1221a/report-thumb.jpg"},{"id":12498,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.nps.gov/history/history/online_books/geology/publications/bul/1221-A/index.htm","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -121.83333333333333,46.75 ], [ -121.83333333333333,46.916666666666664 ], [ -121.58333333333333,46.916666666666664 ], [ -121.58333333333333,46.75 ], [ -121.83333333333333,46.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fe45d","contributors":{"authors":[{"text":"Crandell, Dwight Raymond","contributorId":6440,"corporation":false,"usgs":true,"family":"Crandell","given":"Dwight","email":"","middleInitial":"Raymond","affiliations":[],"preferred":false,"id":212434,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fahnestock, Robert K.","contributorId":100381,"corporation":false,"usgs":true,"family":"Fahnestock","given":"Robert","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":212435,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1226,"text":"wsp1592B - 1965 - Cross-channel transfer of linear momentum in smooth rectangular channels","interactions":[],"lastModifiedDate":"2012-02-02T00:05:17","indexId":"wsp1592B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1592","chapter":"B","title":"Cross-channel transfer of linear momentum in smooth rectangular channels","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1592B","usgsCitation":"Cruff, R., 1965, Cross-channel transfer of linear momentum in smooth rectangular channels: U.S. Geological Survey Water Supply Paper 1592, v, 26 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1592B.","productDescription":"v, 26 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":137912,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1592b/report-thumb.jpg"},{"id":26144,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1592b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db6360b6","contributors":{"authors":[{"text":"Cruff, R.W.","contributorId":77510,"corporation":false,"usgs":true,"family":"Cruff","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":143401,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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":3158,"text":"wsp1819B - 1965 - Predicted hydrologic effects of pumping from the Lichterman Well Field in the Memphis Area, Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:05:27","indexId":"wsp1819B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1819","chapter":"B","title":"Predicted hydrologic effects of pumping from the Lichterman Well Field in the Memphis Area, Tennessee","docAbstract":"The Lichterman well field is scheduled to go into operation early in 1965 to supplement the municipal water-supply system for the city of Memphis, Tenn. Although the initial rate of withdrawal from the well field will be about 8 mgd (million gallons per day), the ultimate design capacity of the field is 20 mgd. A study of sand samples, drillers' logs, and geophysical logs collected during preliminary test drilling at the site for the Lichterman well field was used as a basis for defining three zones of sand favorable for the construction of high-capacity (1,000 gallons per minute or more) water wells. The three zones occur in the '500-foot' sand and are here designated (in descending order) as zone A, zone B, and zone C. The depth to the top of these zones below land surface has the following ranges: zone A, 125 to 225 feet; zone B, 200 to 350 feet; and zone C, 700 to 775 feet. Zones A and B range from 0 to 100 feet in thickness, and zone C ranges from 10 to 100 feet in thickness. Within the well field proper these zones are expected to react to the stress of pumping as separate hydrologic units, but outside the well field the three zones are expected to react as a single hydrologic unit. \r\n\r\nThe '500-foot' sand in the Germantown-Collierville area is recharged chiefly by precipitation on the outcrop area of the sand to the east, but the evidence indicates that additional recharge is entering the aquifer from the Wolf River. In spite of this additional recharge, water levels in the '500-foot' sand are declining at an average rate of about two-thirds of a foot per year, owing to municipal and industrial pumpage in the Memphis area. However, this decline is not expected to alter the excellent quality of the water in the '500-foot' sand at the site of the Lichterman well field. \r\n\r\nPumping in the Lichterman well field will create a cone of depression in the free-water (piezometric) surface of the '500-foot' sand. The decline in water levels will be directly proportional to the rate of pumping and inversely proportional to the distance from the well field. The resultant changes in hydraulic gradients will alter the direction of ground-water movement in the vicinity of the well field and increase the rate of movement toward the well field from areas of recharge. The lowering of water levels might also accelerate locally the changeover from artesian conditions to semiartesian or water-table conditions in the '500-foot' sand. \r\n\r\nWithin the well field proper, water levels are expected to fluctuate as individual wells are turned on and off to accommodate the demand for water. The presence of clay beds in the aquifer will tend to limit the specific capacity of individual production wells, but could serve to limit interference between wells if adjacent wells are screened in different sections of the aquifer. Interference between wells might also be lessened by pumping those wells having the highest specific capacities for the longest periods of time.","language":"ENGLISH","doi":"10.3133/wsp1819B","usgsCitation":"Nyman, D.J., 1965, Predicted hydrologic effects of pumping from the Lichterman Well Field in the Memphis Area, Tennessee: U.S. Geological Survey Water Supply Paper 1819, 26 p. , https://doi.org/10.3133/wsp1819B.","productDescription":"26 p. ","costCenters":[],"links":[{"id":138860,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1819b/report-thumb.jpg"},{"id":30106,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1819b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":30107,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1819b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e99e","contributors":{"authors":[{"text":"Nyman, Dale J.","contributorId":28584,"corporation":false,"usgs":true,"family":"Nyman","given":"Dale","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":146347,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4020,"text":"cir523 - 1965 - Organic-rich shale of the United States and world land areas","interactions":[],"lastModifiedDate":"2017-10-15T16:13:06","indexId":"cir523","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"523","title":"Organic-rich shale of the United States and world land areas","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir523","usgsCitation":"Duncan, D.C., and Swanson, V.E., 1965, Organic-rich shale of the United States and world land areas: U.S. Geological Survey Circular 523, iv, 30 p. :maps., https://doi.org/10.3133/cir523.","productDescription":"iv, 30 p. :maps.","costCenters":[],"links":[{"id":117332,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1965/0523/report-thumb.jpg"},{"id":31112,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1965/0523/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68ac1b","contributors":{"authors":[{"text":"Duncan, Donald Cave","contributorId":27427,"corporation":false,"usgs":true,"family":"Duncan","given":"Donald","email":"","middleInitial":"Cave","affiliations":[],"preferred":false,"id":147995,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swanson, Vernon Emanuel","contributorId":59014,"corporation":false,"usgs":true,"family":"Swanson","given":"Vernon","email":"","middleInitial":"Emanuel","affiliations":[],"preferred":false,"id":147996,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":34576,"text":"b1188 - 1965 - Geology of northwestern North Park, Colorado","interactions":[],"lastModifiedDate":"2021-08-18T11:56:41.108466","indexId":"b1188","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1188","title":"Geology of northwestern North Park, Colorado","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U. S. Government Printing Office","doi":"10.3133/b1188","usgsCitation":"Hail, W., 1965, Geology of northwestern North Park, Colorado: U.S. Geological Survey Bulletin 1188, Report: v, 133 p.; 5 Plates: 46.43 x 26.32 inches or smaller, https://doi.org/10.3133/b1188.","productDescription":"Report: v, 133 p.; 5 Plates: 46.43 x 26.32 inches or smaller","costCenters":[],"links":[{"id":92816,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1188/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":92817,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1188/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":92819,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1188/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":163113,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1188/report-thumb.jpg"},{"id":92814,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1188/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":92815,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1188/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":92818,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1188/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":109484,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20965.htm","linkFileType":{"id":5,"text":"html"},"description":"20965"}],"country":"United States","state":"Colorado","otherGeospatial":"North Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.3750,\n              40.6250\n            ],\n            [\n              -106.6250,\n              40.6250\n            ],\n            [\n              -106.6250,\n              41.00\n            ],\n            [\n              -106.3750,\n              41.00\n            ],\n            [\n              -106.3750,\n              40.6250\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683824","contributors":{"authors":[{"text":"Hail, W. J. Jr.","contributorId":35332,"corporation":false,"usgs":true,"family":"Hail","given":"W. J.","suffix":"Jr.","affiliations":[],"preferred":false,"id":213202,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52475,"text":"ofr6586 - 1965 - Probable effect of Canal 111 of salt-water encroachment, southern Dade County, Florida","interactions":[],"lastModifiedDate":"2025-04-18T00:27:53.374971","indexId":"ofr6586","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":"65-86","displayTitle":"Probable Effect of Canal 111 on Salt-Water Encroachment, Southern Dade County, Florida","title":"Probable effect of Canal 111 of salt-water encroachment, southern Dade County, Florida","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr6586","usgsCitation":"Probable effect of Canal 111 of salt-water encroachment, southern Dade County, Florida; 1965; OFR; 65-86; Klein, Howard","productDescription":"26 p.","numberOfPages":"26","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":4539,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1965/0086/ofr6586.pdf","text":"Report","size":"988 KB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 65-86"},{"id":179631,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1965/0086/coverthb.jpg"}],"contact":"<p><a href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","publishedDate":"1965-07-07","noUsgsAuthors":false,"publicationDate":"1965-07-07","publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db660b13","contributors":{"authors":[{"text":"Klein, Howard","contributorId":62189,"corporation":false,"usgs":true,"family":"Klein","given":"Howard","email":"","affiliations":[],"preferred":false,"id":245400,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52499,"text":"ofr65146 - 1965 - An appraisal of the ground-water resources of the lower Susquehanna River basin (An interim report)","interactions":[],"lastModifiedDate":"2018-11-08T09:34:54","indexId":"ofr65146","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":"65-146","title":"An appraisal of the ground-water resources of the lower Susquehanna River basin (An interim report)","docAbstract":"<p>This report describes the availability, quantity, quality, variability, and cost of development of the ground-water resources in the lower Susquehanna River basin. The report has been prepared for and under specifications established by the Corps of Engineers, U. S. Army, and the Public Health Service, Department of Health, Education, and Welfare.</p><p>A comprehensive study of the water and related land resources of the Susquehanna River basin was authorized by the Congress of the United States in October 1961, and the task of preparing a report and of coordinating the work being done by others in support of the study was assigned to the Corps of Engineers. The comprehensive study is being conducted by several Federal departments and independent agencies in cooperation with the States of New York, Pennsylvania, and Maryland. The Public Health Service under its authority in the Federal Water Pollution Control Act (P. L. 660) initiated a comprehensive water quality control program for the Chesapeake drainage basin, which includes the Susquehanna River basin.</p><p>This report is intended to serve the specific needs for ground-water information of both the Corps of Engineers and the Public Health Service, as well as those of the other participating Federal and State agencies.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr65146","usgsCitation":"Seaber, P.R., and Hollyday, E.F., 1965, An appraisal of the ground-water resources of the lower Susquehanna River basin (An interim report): U.S. Geological Survey Open-File Report 65-146, v, 75 p., https://doi.org/10.3133/ofr65146.","productDescription":"v, 75 p.","numberOfPages":"86","costCenters":[],"links":[{"id":359297,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1965/0146/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":179514,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1965/0146/report-thumb.jpg"}],"country":"United States","state":"Pennsylvania","otherGeospatial":"Lower Susquehanna River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -78,\n              39.5\n            ],\n            [\n              -76,\n              39.5\n            ],\n            [\n              -76,\n              41\n            ],\n            [\n              -78,\n              41\n            ],\n            [\n              -78,\n              39.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685610","contributors":{"authors":[{"text":"Seaber, Paul R.","contributorId":67492,"corporation":false,"usgs":true,"family":"Seaber","given":"Paul","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":245445,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hollyday, Este F.","contributorId":27089,"corporation":false,"usgs":true,"family":"Hollyday","given":"Este","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":245446,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":52508,"text":"ofr65157 - 1965 - Ground-water data of selected test holes and wells along the Arkansas River in Sequoyah County, Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:11:41","indexId":"ofr65157","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":"65-157","title":"Ground-water data of selected test holes and wells along the Arkansas River in Sequoyah County, Oklahoma","docAbstract":"The data in this report were collected during the period 1958-64 by the U.S. Geological Survey in cooperation with the U.S. Army, Corps of Engineers, as part of a comprehensive study of the ground-water resources of the alluvium along the Arkansas and Verdigris Rivers between Moffett and Catoosa, Oklahoma (fig. 1). The purpose of this report is to make the hydrologic data obtained during the study of ground water in the alluvium along the Arkansas River in Sequoyah County readily available to the public. The data in this report should be useful in predicting geologic and hydrologic conditions when drilling new wells. Table 1 gives information on the sizes, depths, yields, and other characteristics of wells in the area. The table also provides a key to the additional information for each well site given in tables 2 through 6. Table 2 gives logs for the materials penetrated at test holes and wells in the report area; table 3 gives depths to water measured in wells; table 4 includes chemical analyses of water from wells; table 5 gives laboratory determinations of particle-size distribution of earth samples collected from test holes and wells; and table 6 gives coefficients of permeability and other hydrologic properties of earth samples from the selected test holes. Similar data for LeFlore-Haskell Counties, Muskogee County, and Wagoner-Rogers Counties are available in other open-file reports.\r\nAn interpretive report, 'Hydrology of the alluvium of the Arkansas River, Muskogee, Oklahoma, to Fort Smith, Arkansas,' by Harry H. Tanaka and Jerrald R. Hollowell will be published as U.S. Geological Survey Water-Supply Paper 1809-T.","language":"ENGLISH","doi":"10.3133/ofr65157","usgsCitation":"Tanaka, H., Hart, D., and Knott, R., 1965, Ground-water data of selected test holes and wells along the Arkansas River in Sequoyah County, Oklahoma: U.S. Geological Survey Open-File Report 65-157, 238 p., https://doi.org/10.3133/ofr65157.","productDescription":"238 p.","costCenters":[],"links":[{"id":176974,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db69958c","contributors":{"authors":[{"text":"Tanaka, H.H.","contributorId":30610,"corporation":false,"usgs":true,"family":"Tanaka","given":"H.H.","email":"","affiliations":[],"preferred":false,"id":245465,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hart, D.L. Jr.","contributorId":49403,"corporation":false,"usgs":true,"family":"Hart","given":"D.L.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":245466,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Knott, R.K.","contributorId":102484,"corporation":false,"usgs":true,"family":"Knott","given":"R.K.","email":"","affiliations":[],"preferred":false,"id":245467,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":41891,"text":"ofr659 - 1965 - Aeromagnetic map of northwestern Dickinson County, Michigan","interactions":[],"lastModifiedDate":"2012-02-02T00:05:01","indexId":"ofr659","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":"65-9","title":"Aeromagnetic map of northwestern Dickinson County, Michigan","language":"ENGLISH","doi":"10.3133/ofr659","usgsCitation":"Balsley, J.R., and Long, C.L., 1965, Aeromagnetic map of northwestern Dickinson County, Michigan: U.S. Geological Survey Open-File Report 65-9, 1 map, https://doi.org/10.3133/ofr659.","productDescription":"1 map","costCenters":[],"links":[{"id":135482,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":98636,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0009/plate-1.pdf","size":"25574","linkFileType":{"id":1,"text":"pdf"}}],"scale":"31680","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697ce2","contributors":{"authors":[{"text":"Balsley, James R.","contributorId":10010,"corporation":false,"usgs":true,"family":"Balsley","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":225684,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Long, Carl L.","contributorId":32128,"corporation":false,"usgs":true,"family":"Long","given":"Carl","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":225685,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":52501,"text":"ofr65149 - 1965 - Freshwater inflow data for Corps of Engineers model study of Houston, Texas, ship channel","interactions":[],"lastModifiedDate":"2012-02-02T00:11:41","indexId":"ofr65149","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":"65-149","title":"Freshwater inflow data for Corps of Engineers model study of Houston, Texas, ship channel","language":"ENGLISH","doi":"10.3133/ofr65149","usgsCitation":"Smith, R.E., and Kaminski, E., 1965, Freshwater inflow data for Corps of Engineers model study of Houston, Texas, ship channel: U.S. Geological Survey Open-File Report 65-149, 19 p., https://doi.org/10.3133/ofr65149.","productDescription":"19 p.","costCenters":[],"links":[{"id":177654,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a862a","contributors":{"authors":[{"text":"Smith, R. E.","contributorId":76366,"corporation":false,"usgs":true,"family":"Smith","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":245450,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kaminski, E.G.","contributorId":16092,"corporation":false,"usgs":true,"family":"Kaminski","given":"E.G.","email":"","affiliations":[],"preferred":false,"id":245449,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":52507,"text":"ofr65156 - 1965 - Ground-water data of selected test holes and wells along the Verdigris River in Wagoner and Rogers Counties, Oklahoma","interactions":[],"lastModifiedDate":"2017-08-07T14:45:55","indexId":"ofr65156","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":"65-156","title":"Ground-water data of selected test holes and wells along the Verdigris River in Wagoner and Rogers Counties, Oklahoma","docAbstract":"<p>The data in this report were collected during the period 1958-64 by the U.S. Geological Survey in cooperation with the U.S. Army, Corps of Engineers, as part of a comprehensive study of the ground-water resources of the alluvium along the Arkansas and Verdigris Rivers between Moffett and Catoosa, Oklahoma (fig. 1). The purpose of this report is to make the hydrologic data obtained during the study of ground water in the alluvium along the Verdigris River in Wagoner and Rogers Counties readily available to the public. The data in this report should be useful in predicting geologic and hydrologic conditions when drilling new wells. Table 1 gives information on the sizes, depths, yields, and other characteristics of wells in the area. The table also provides a key to the additional information for each well site given in tables 2 through 6. Table 2 gives logs for the materials penetrated at test holes and wells in the report area; table 3 gives depths to water measured in wells; table 4 includes chemical analyses of water from wells; table 5 gives laboratory determinations of particle-size distribution of earth samples collected from test holes and wells; and table 6 gives coefficients of permeability and other hydrologic properties of earth samples from the selected test holes. Similar data for Sequoyah County, LeFlore-Haskell Counties, and Muskogee County are available in other open-file reports. </p><p>An interpretive report, 'Hydrology of the alluvium of the Arkansas River, Muskogee, Oklahoma, to Fort Smith, Arkansas,' by Harry H. Tanaka and Jerrald R. 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Jr.","contributorId":49403,"corporation":false,"usgs":true,"family":"Hart","given":"D.L.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":245463,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Knott, R.K.","contributorId":102484,"corporation":false,"usgs":true,"family":"Knott","given":"R.K.","email":"","affiliations":[],"preferred":false,"id":245464,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":3816,"text":"cir522 - 1965 - Resources of oil, gas, and natural-gas liquids in the United States and the world","interactions":[],"lastModifiedDate":"2017-10-15T16:13:53","indexId":"cir522","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"522","title":"Resources of oil, gas, and natural-gas liquids in the United States and the world","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir522","usgsCitation":"Hendricks, T.A., 1965, Resources of oil, gas, and natural-gas liquids in the United States and the world: U.S. Geological Survey Circular 522, iii, 20 p. :illus. ;27 cm., https://doi.org/10.3133/cir522.","productDescription":"iii, 20 p. :illus. ;27 cm.","costCenters":[],"links":[{"id":30886,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1965/0522/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117993,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1965/0522/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629b8e","contributors":{"authors":[{"text":"Hendricks, Thomas Andrews","contributorId":21147,"corporation":false,"usgs":true,"family":"Hendricks","given":"Thomas","email":"","middleInitial":"Andrews","affiliations":[],"preferred":false,"id":147658,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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