{"pageNumber":"6577","pageRowStart":"164400","pageSize":"25","recordCount":184904,"records":[{"id":40730,"text":"ofr6721 - 1967 - Water-resources of the Antelope Valley-East Kern Water Agency area, California","interactions":[],"lastModifiedDate":"2023-02-07T20:12:11.899667","indexId":"ofr6721","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"67-21","title":"Water-resources of the Antelope Valley-East Kern Water Agency area, California","docAbstract":"The Antelope Valley-East Kern Water Agency (AVEK) area, most of which is within the Mojave Desert region of southern California, lacks adequate water resources to sustain the existing rate of ground-water pumpage for irrigation, industrial, and domestic use. However, by 1972 the California Aqueduct, a part of the California Water Plan, will be completed and will begin to convey water from northern California into the area. \r\n\r\nThe chief economic pursuits in the area are irrigated agriculture and poultry production. At present, the major industries are related to national defense and mining. In the future, industry will increase and probably become the major economic activity. \r\n\r\nThe Mojave Desert region, part of which lies within the AVEK area, is characterized by fault-block mountains and fault-block basins. The Tehachapi and San Gabriel Mountains are the major bordering fault blocks. The adjacent lowland areas of Antelope and Fremont Valleys have been depressed by movements along major faults. There are two major ground-water basins in the AVEK area: Antelope Valley and Fremont Valley basins. Each large basin is divided by faults or bodies of consolidated rock into several groundwater subunits.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6721","usgsCitation":"Bloyd, R., 1967, Water-resources of the Antelope Valley-East Kern Water Agency area, California: U.S. Geological Survey Open-File Report 67-21, Report: v, 69 p.; 4 Plates: 38.03 x 37.66 inches or smaller, https://doi.org/10.3133/ofr6721.","productDescription":"Report: v, 69 p.; 4 Plates: 38.03 x 37.66 inches or smaller","costCenters":[],"links":[{"id":78007,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0021/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":78005,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0021/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":78006,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0021/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":78008,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1967/0021/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":110343,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52175.htm","linkFileType":{"id":5,"text":"html"},"description":"52175"},{"id":78004,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0021/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":171426,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1967/0021/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Antelope Valley-East Kern Water Agency area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -118.8603,\n              35.3603\n            ],\n            [\n              -118.8603,\n              34.3833\n            ],\n            [\n              -117.6333,\n              34.3833\n            ],\n            [\n              -117.6333,\n              35.3603\n            ],\n            [\n              -118.8603,\n              35.3603\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cbe4b07f02db543823","contributors":{"authors":[{"text":"Bloyd, R. M. Jr.","contributorId":73243,"corporation":false,"usgs":true,"family":"Bloyd","given":"R. M.","suffix":"Jr.","affiliations":[],"preferred":false,"id":223867,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":36306,"text":"b1063K - 1967 - Geology of the Hot Springs quadrangle, Fall River and Custer Counties, South Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:09:45","indexId":"b1063K","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"1063","chapter":"K","title":"Geology of the Hot Springs quadrangle, Fall River and Custer Counties, South Dakota","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1063K","usgsCitation":"Wolcott, D.E., 1967, Geology of the Hot Springs quadrangle, Fall River and Custer Counties, South Dakota: U.S. Geological Survey Bulletin 1063, p. 427-442, ill., map (1 fold. col.in pocket) ;24 cm., https://doi.org/10.3133/b1063K.","productDescription":"p. 427-442, ill., map (1 fold. col.in pocket) ;24 cm.","costCenters":[],"links":[{"id":109267,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20703.htm","linkFileType":{"id":5,"text":"html"},"description":"20703"},{"id":93843,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1063k/plate-28.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":93844,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1063k/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":166621,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1063k/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67ff4d","contributors":{"authors":[{"text":"Wolcott, Don E.","contributorId":48154,"corporation":false,"usgs":true,"family":"Wolcott","given":"Don","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":216108,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42095,"text":"ofr67233 - 1967 - Aeromagnetic map of the Coaldale quadrangle, Nevada","interactions":[],"lastModifiedDate":"2025-07-24T20:46:40.113606","indexId":"ofr67233","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"67-233","title":"Aeromagnetic map of the Coaldale quadrangle, Nevada","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr67233","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1967, Aeromagnetic map of the Coaldale quadrangle, Nevada: U.S. Geological Survey Open-File Report 67-233, 1 Plate: 30.48 x 41.71 inches, https://doi.org/10.3133/ofr67233.","productDescription":"1 Plate: 30.48 x 41.71 inches","costCenters":[],"links":[{"id":492859,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8188.htm","linkFileType":{"id":5,"text":"html"}},{"id":79838,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0233/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":176106,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Coaldale quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -118,\n              38.5\n            ],\n            [\n              -118,\n              38\n            ],\n            [\n              -117.5,\n              38\n            ],\n            [\n              -117.5,\n              38.5\n            ],\n            [\n              -118,\n              38.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696d9a","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530828,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42102,"text":"ofr67252 - 1967 - Aeromagnetic map of the Schurz, Gillis Canyon, Mount Grant, and Hawthorne quadrangles, Nevada","interactions":[],"lastModifiedDate":"2025-07-25T18:36:08.854115","indexId":"ofr67252","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"67-252","title":"Aeromagnetic map of the Schurz, Gillis Canyon, Mount Grant, and Hawthorne quadrangles, Nevada","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr67252","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1967, Aeromagnetic map of the Schurz, Gillis Canyon, Mount Grant, and Hawthorne quadrangles, Nevada: U.S. Geological Survey Open-File Report 67-252, 1 Plate: 29.56 x 41.31 inches, https://doi.org/10.3133/ofr67252.","productDescription":"1 Plate: 29.56 x 41.31 inches","costCenters":[],"links":[{"id":492930,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8207.htm","linkFileType":{"id":5,"text":"html"}},{"id":79846,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0252/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":176617,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Schurz, Gillis Canyon, Mount Grant, and Hawthorne quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -119,\n              39\n            ],\n            [\n              -119,\n              38.5\n            ],\n            [\n              -118.5,\n              38.5\n            ],\n            [\n              -118.5,\n              39\n            ],\n            [\n              -119,\n              39\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db69125e","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530835,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42055,"text":"ofr67234 - 1967 - Aeromagnetic map of the Como and Wabuska quadrangles, and parts of the Churchill Butte and Silver Springs quadrangles, Nevada","interactions":[],"lastModifiedDate":"2025-07-24T20:50:56.411119","indexId":"ofr67234","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"67-234","title":"Aeromagnetic map of the Como and Wabuska quadrangles, and parts of the Churchill Butte and Silver Springs quadrangles, Nevada","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr67234","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1967, Aeromagnetic map of the Como and Wabuska quadrangles, and parts of the Churchill Butte and Silver Springs quadrangles, Nevada: U.S. Geological Survey Open-File Report 67-234, 1 Plate: 30.08 × 42.44 inches, https://doi.org/10.3133/ofr67234.","productDescription":"1 Plate: 30.08 × 42.44 inches","costCenters":[],"links":[{"id":79803,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0234/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":394932,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8189.htm"},{"id":136767,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Como and Wabuska quadrangles, and parts of the Churchill Butte and Silver Springs quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.5,\n              39.284\n            ],\n            [\n              -119,\n              39.284\n            ],\n            [\n              -119,\n              39\n            ],\n            [\n              -119.5,\n              39\n            ],\n            [\n              -119.5,\n              39.284\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696d45","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530802,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41993,"text":"ofr67235 - 1967 - Aeromagnetic map of the Dixie Flats and Elko 2 quadrangles, Elko County, Nevada","interactions":[],"lastModifiedDate":"2025-07-24T20:57:31.652913","indexId":"ofr67235","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"67-235","title":"Aeromagnetic map of the Dixie Flats and Elko 2 quadrangles, Elko County, Nevada","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr67235","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1967, Aeromagnetic map of the Dixie Flats and Elko 2 quadrangles, Elko County, Nevada: U.S. Geological Survey Open-File Report 67-235, 1 Plate: 18.71 x 39.91 inches, https://doi.org/10.3133/ofr67235.","productDescription":"1 Plate: 18.71 x 39.91 inches","costCenters":[],"links":[{"id":492860,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8190.htm","linkFileType":{"id":5,"text":"html"}},{"id":135455,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79750,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0235/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nevada","county":"Elko County","otherGeospatial":"Dixie Flats and Elko 2 quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -115.75,\n              41\n            ],\n            [\n              -116,\n              41\n            ],\n            [\n              -116,\n              40.5\n            ],\n            [\n              -115.75,\n              40.5\n            ],\n            [\n              -115.75,\n              41\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696afd","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530759,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32595,"text":"32595 - 1967 - National Atlas, Indian tribes, cultures & languages","interactions":[],"lastModifiedDate":"2017-03-29T12:59:50","indexId":"32595","displayToPublicDate":"1991-01-01T09:59:44","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"National Atlas, Indian tribes, cultures & languages","docAbstract":"<p>Tribal distributions depicted on these maps (and on all other tribal maps covering a comparable area) are arbitrary at many points. Detailed knowledge of tribal areas was acquired at different times in different regions. For example, by the time knowledge was gained of the areas occupied by Plains tribes, many groups in the East had become extinct or had moved from their aboriginal locations. Some of these movements ultimately affected distributions on the Plains prior to reasonably detailed knowledge of Plains occupancy. Hence, it is not possible to approximate aboriginal areas of occupancy on a single map of continental scope. Furthermore, most groups did not occupy sharply defined areas, so that the delineation of territories is misleading.</p><p>Distributions were derived, with slight modifications, from Indian tribes of North America (Driver and others, 1953), and boundaries within California were simplified after Languages, territories, and names of California Indian tribes (Heizer, 1966). According to the authors of these publications, the boundaries shown are those of the mid-17th century in the Southeast and the eastern part of the Northeast, the late 17th and early 18th centuries farther west in the Northeast, the late 18th and early 19th centuries in the Plains, the late 18th century in California, and the middle-to-late 19th century elsewhere. Even so, many compromises had to be made.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/32595","usgsCitation":"Sturtevant, W.C., 1967, National Atlas, Indian tribes, cultures & languages, 2 Plates: 13.85 x 18.01 inches and 27.81 x 18.54 inches, https://doi.org/10.3133/32595.","productDescription":"2 Plates: 13.85 x 18.01 inches and 27.81 x 18.54 inches","costCenters":[],"links":[{"id":289518,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":338480,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/32595/plate-1_back.pdf","text":"Back","size":"2.63 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate - Back"},{"id":338479,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/32595/plate-1_front.pdf","text":"Front","size":"6.24 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate - Front"}],"scale":"7500000","projection":"Albers Equal Area","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53bd12e4e4b00cbf31f72341","contributors":{"authors":[{"text":"Sturtevant, William C.","contributorId":60963,"corporation":false,"usgs":true,"family":"Sturtevant","given":"William","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":208752,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70112266,"text":"70112266 - 1967 - Surveying the earth's resources from space","interactions":[],"lastModifiedDate":"2017-03-27T13:52:29","indexId":"70112266","displayToPublicDate":"1990-06-12T11:12:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3502,"text":"Surveying and Mapping","active":true,"publicationSubtype":{"id":10}},"title":"Surveying the earth's resources from space","docAbstract":"<p>Two developments, aerial photography and airborne geophysical surveying techniques, have already increased the rate at which new knowledge of the world's resources can be acquired. But even with far wider use of the tools and techniques already available, the problems that face us are greater than our current ability to solve them. Fortunately, some of the further acceleration required can be obtained through use of remote-sensing devices mounted in high-flying aircraft and earth-orbiting satellites.</p>","language":"English","publisher":"American Congress on Surveying and Mapping","publisherLocation":"Washington, D.C.","usgsCitation":"Pecora, W.T., 1967, Surveying the earth's resources from space: Surveying and Mapping, v. 27, no. 4, p. 639-643.","productDescription":"5 p.","startPage":"639","endPage":"643","numberOfPages":"5","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288462,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"539acc57e4b0e83db6d0901b","contributors":{"authors":[{"text":"Pecora, William T.","contributorId":45167,"corporation":false,"usgs":true,"family":"Pecora","given":"William","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":494599,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70112265,"text":"70112265 - 1967 - Changes in surface temperature at Taal Volcano, Philippines 1965-1966","interactions":[],"lastModifiedDate":"2019-11-18T14:40:57","indexId":"70112265","displayToPublicDate":"1990-06-12T11:03:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1093,"text":"Bulletin Volcanologique","active":true,"publicationSubtype":{"id":10}},"title":"Changes in surface temperature at Taal Volcano, Philippines 1965-1966","docAbstract":"<p>Taal Volcano erupted in September 1965 ending a dormant period of 54 years. A quiescent interval of 9 months followed, terminated by new eruptions in July 1966 at the same site. Aerial surveys with a scanning infrared radiometer were made at three periods during the quiescent interval and twice following the July 1966 eruption. The survey technique yields a quasiphotographic image of the radiant temperature of the volcanic terrain. Results indicate that the principal changes in surface temperature stemmed from changes in convective heat transfer by hydrothermal fluids. New hot springs developed along the structurally-controlled northwest and southeast flanks of the 1965 explosion crater. The northwest spring grew in size prior to the 1966 eruption, persisted through that eruption and has since maintained its discharge. The 1965 cinder cone meanwhile showed a persistent rim of hydrothermal activity with some shift in position of maximum discharge. The July 1966 eruptions took place on the rim about midway between two positions of maximum discharge.</p>","language":"English","publisher":"Springer Berlin Heidelberg","doi":"10.1007/BF02597014","issn":"0366483x","usgsCitation":"Moxham, R., 1967, Changes in surface temperature at Taal Volcano, Philippines 1965-1966: Bulletin Volcanologique, v. 31, no. 1, p. 215-234, https://doi.org/10.1007/BF02597014.","productDescription":"20 p.","startPage":"215","endPage":"234","numberOfPages":"20","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288461,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":288459,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02597014"}],"country":"Philippines","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 120.981317,13.992801 ], [ 120.981317,14.024946 ], [ 121.013203,14.024946 ], [ 121.013203,13.992801 ], [ 120.981317,13.992801 ] ] ] } } ] }","volume":"31","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"539acbe8e4b0e83db6d08ec4","contributors":{"authors":[{"text":"Moxham, R.M.","contributorId":42234,"corporation":false,"usgs":true,"family":"Moxham","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":494598,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70112264,"text":"70112264 - 1967 - Radar remote sensing in biology","interactions":[],"lastModifiedDate":"2017-03-27T13:48:48","indexId":"70112264","displayToPublicDate":"1990-06-12T11:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":997,"text":"BioScience","active":true,"publicationSubtype":{"id":10}},"title":"Radar remote sensing in biology","docAbstract":"<p>The present status of research on discrimination of natural and cultivated vegetation using radar imaging systems is sketched. The value of multiple polarization radar in improved discrimination of vegetation types over monoscopic radars is also documented. Possible future use of multi-frequency, multi-polarization radar systems for all weather agricultural survey is noted.</p>","language":"English","publisher":"Oxford University Press","doi":"10.2307/1293798","usgsCitation":"Moore, R.K., and Simonett, D.S., 1967, Radar remote sensing in biology: BioScience, v. 17, no. 6, p. 384-390, https://doi.org/10.2307/1293798.","productDescription":"7 p.","startPage":"384","endPage":"390","numberOfPages":"7","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288458,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":288457,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.2307/1293798"}],"volume":"17","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"539acc0ee4b0e83db6d08fbb","contributors":{"authors":[{"text":"Moore, Richard K.","contributorId":86268,"corporation":false,"usgs":true,"family":"Moore","given":"Richard","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":494597,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simonett, David S.","contributorId":54212,"corporation":false,"usgs":true,"family":"Simonett","given":"David","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":494596,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70112262,"text":"70112262 - 1967 - Geologic interpretation of the Gemini V photograph of the Salt Range-Potwar Plateau region west Pakistan","interactions":[],"lastModifiedDate":"2017-03-27T13:47:16","indexId":"70112262","displayToPublicDate":"1990-06-12T10:58:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3051,"text":"Photogrammetric Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Geologic interpretation of the Gemini V photograph of the Salt Range-Potwar Plateau region west Pakistan","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Society of Photogrammetry","publisherLocation":"Falls Church, VA","usgsCitation":"Hemphill, W.R., 1967, Geologic interpretation of the Gemini V photograph of the Salt Range-Potwar Plateau region west Pakistan: Photogrammetric Engineering, v. 33, no. 6, p. 667-667.","productDescription":"1 p.","startPage":"667","endPage":"667","numberOfPages":"1","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288456,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"539acbfee4b0e83db6d08f3c","contributors":{"authors":[{"text":"Hemphill, William R.","contributorId":21970,"corporation":false,"usgs":true,"family":"Hemphill","given":"William","email":"","middleInitial":"R.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":494590,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70112261,"text":"70112261 - 1967 - Explorers from space","interactions":[],"lastModifiedDate":"2017-03-27T13:46:42","indexId":"70112261","displayToPublicDate":"1990-06-12T10:36:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2307,"text":"Journal of Geological Education","active":true,"publicationSubtype":{"id":10}},"title":"Explorers from space","docAbstract":"<p>The statement that a new era in exploration is opening will almost surely bring to mind the venturing of man into space and the ever more imminent exploration of the moon. The reference here, however, is to exploration of earth itself and to the unique capabilities for study of the earth that space technology will provide. Demands for water, minerals, energy, food, and for working, living and recreational space are outrunning our ability to meet them by traditional methods. In order to satisfy these demands, it is necessary now, just as it has been in the past, to look to the activities, the instruments, and the technologies that in part create the pressures for aid in meeting them. Studies being made at the U.S. Geological Survey and elsewhere of the potential applications of remote sensors in space to earth resources research indicate that now, at last, it will be possible to approach solutions on a regional or global basis. This paper discusses the plans for an Earth Resources Observational Satellites Program which will be designed for that purpose.</p>","language":"English","publisher":"National Association of Geology Teachers","publisherLocation":"Appleton, WI","usgsCitation":"Fary, R.W., 1967, Explorers from space: Journal of Geological Education, v. 15, no. 3, p. 99-104.","productDescription":"6 p.","startPage":"99","endPage":"104","numberOfPages":"6","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288453,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"539acbf7e4b0e83db6d08f23","contributors":{"authors":[{"text":"Fary, Raymond W. Jr.","contributorId":22830,"corporation":false,"usgs":true,"family":"Fary","given":"Raymond","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":494589,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70048241,"text":"pp545 - 1967 - The Alaska earthquake, March 27, 1964: effects on transportation, communications, and utilities","interactions":[{"subject":{"id":32614,"text":"pp545D - 1970 - Effects of the earthquake of March 27, 1964, on the Alaska Railroad","indexId":"pp545D","publicationYear":"1970","noYear":false,"chapter":"D","title":"Effects of the earthquake of March 27, 1964, on the Alaska Railroad"},"predicate":"IS_PART_OF","object":{"id":70048241,"text":"pp545 - 1967 - The Alaska earthquake, March 27, 1964: effects on transportation, communications, and utilities","indexId":"pp545","publicationYear":"1967","noYear":false,"title":"The Alaska earthquake, March 27, 1964: effects on transportation, communications, and utilities"},"id":1},{"subject":{"id":32615,"text":"pp545A - 1967 - Effect of the earthquake of March 27, 1964, on the Eklutna Hydroelectric Project, Anchorage, Alaska, with a section on television examination of earthquake damage to underground communication and electrical systems in Anchorage","indexId":"pp545A","publicationYear":"1967","noYear":false,"chapter":"A","title":"Effect of the earthquake of March 27, 1964, on the Eklutna Hydroelectric Project, Anchorage, Alaska, with a section on television examination of earthquake damage to underground communication and electrical systems in Anchorage"},"predicate":"IS_PART_OF","object":{"id":70048241,"text":"pp545 - 1967 - The Alaska earthquake, March 27, 1964: effects on transportation, communications, and utilities","indexId":"pp545","publicationYear":"1967","noYear":false,"title":"The Alaska earthquake, March 27, 1964: effects on transportation, communications, and utilities"},"id":2},{"subject":{"id":38784,"text":"pp545B - 1967 - Effects of the earthquake of March 27, 1964, on air and water transport, communications, and utilities systems in south-central Alaska","indexId":"pp545B","publicationYear":"1967","noYear":false,"chapter":"B","title":"Effects of the earthquake of March 27, 1964, on air and water transport, communications, and utilities systems in south-central Alaska"},"predicate":"IS_PART_OF","object":{"id":70048241,"text":"pp545 - 1967 - The Alaska earthquake, March 27, 1964: effects on transportation, communications, and utilities","indexId":"pp545","publicationYear":"1967","noYear":false,"title":"The Alaska earthquake, March 27, 1964: effects on transportation, communications, and utilities"},"id":3},{"subject":{"id":38785,"text":"pp545C - 1968 - Effects of the earthquake of March 27, 1964, on the Alaska highway system","indexId":"pp545C","publicationYear":"1968","noYear":false,"chapter":"C","title":"Effects of the earthquake of March 27, 1964, on the Alaska highway system"},"predicate":"IS_PART_OF","object":{"id":70048241,"text":"pp545 - 1967 - The Alaska earthquake, March 27, 1964: effects on transportation, communications, and utilities","indexId":"pp545","publicationYear":"1967","noYear":false,"title":"The Alaska earthquake, March 27, 1964: effects on transportation, communications, and utilities"},"id":4}],"lastModifiedDate":"2014-09-24T15:06:22","indexId":"pp545","displayToPublicDate":"1980-01-23T10:12:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"545","title":"The Alaska earthquake, March 27, 1964: effects on transportation, communications, and utilities","docAbstract":"This is the forth in a series of six reports that the U.S. Geological Survey published on the results of a comprehensive geologic study that began, as a reconnaissance survey, within 24 hours after the March 27, 1964, Magnitude 9.2 Great Alaska Earthquake and extended, as detailed investigations, through several field seasons. The 1964 Great Alaska earthquake was the largest earthquake in the U.S. since 1700. Professional Paper 545, in 4 parts, describes the effects on transportation, communications, and utilities.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, DC","doi":"10.3133/pp545","usgsCitation":"Logan, M.H., Burton, L.R., Eckel, E.B., Kachadoorian, R., McCulloch, D.S., and Bonilla, M.G., 1967, The Alaska earthquake, March 27, 1964: effects on transportation, communications, and utilities: U.S. Geological Survey Professional Paper 545, https://doi.org/10.3133/pp545.","costCenters":[{"id":380,"text":"Menlo ParkCalif. Office-Earthquake Science Center","active":false,"usgs":true}],"links":[{"id":277799,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":277798,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/0545/"}],"country":"United States","state":"Alaska","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 172.45,51.21 ], [ 172.45,71.39 ], [ -129.99,71.39 ], [ -129.99,51.21 ], [ 172.45,51.21 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd76c7e4b0b2908510b1d3","contributors":{"authors":[{"text":"Logan, Malcolm H.","contributorId":42127,"corporation":false,"usgs":true,"family":"Logan","given":"Malcolm","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":484100,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burton, Lynn R.","contributorId":103962,"corporation":false,"usgs":true,"family":"Burton","given":"Lynn","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":484102,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Eckel, Edwin B.","contributorId":26680,"corporation":false,"usgs":true,"family":"Eckel","given":"Edwin","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":484099,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kachadoorian, Reuben","contributorId":24336,"corporation":false,"usgs":true,"family":"Kachadoorian","given":"Reuben","email":"","affiliations":[],"preferred":false,"id":484098,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"McCulloch, David S. dmccullo@usgs.gov","contributorId":3100,"corporation":false,"usgs":true,"family":"McCulloch","given":"David","email":"dmccullo@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":484097,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Bonilla, Manuel G.","contributorId":74384,"corporation":false,"usgs":true,"family":"Bonilla","given":"Manuel","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":484101,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70174084,"text":"70174084 - 1967 - Availability of ground water in Decatur County, Iowa","interactions":[],"lastModifiedDate":"2025-07-29T19:04:41.331482","indexId":"70174084","displayToPublicDate":"1970-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5106,"text":"Iowa Geological Survey Water Atlas","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"2","title":"Availability of ground water in Decatur County, Iowa","docAbstract":"<p>Decatur County and several other counties in south-central Iowa comprise an area that has been chronically short of good-quality water. &nbsp;Municipalities, industries and rural water users alike have been affected by the water shortage. &nbsp;Municipalities have experienced serious problems in obtaining potable supplies adequate to keep pace with their growth and development: industrial expansion has been hindered and continues to be hindered by the shortage of good-quality water; and rural supplies for domestic and livestock use are difficult to obtain at many places. &nbsp;The increased use of water for all purposes and periodic drought conditions have greatly magnified an already serious problem of water shortage.</p>","language":"English","publisher":"Iowa Geological Survey","usgsCitation":"Cagle, J., and Steinhilber, W.L., 1967, Availability of ground water in Decatur County, Iowa: Iowa Geological Survey Water Atlas 2, v, 28 p.","productDescription":"v, 28 p.","numberOfPages":"33","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":324448,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":324447,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70174084/IGS_Water_Atlas_Number_2.pdf","text":"Report","size":"6.43 MB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Iowa","county":"Decatur County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-93.558,40.8985],[-93.5573,40.811],[-93.5566,40.7234],[-93.5565,40.6372],[-93.5565,40.5789],[-93.6866,40.5783],[-93.7784,40.5769],[-93.9589,40.5743],[-94.0182,40.5735],[-94.0169,40.6376],[-94.0163,40.7228],[-94.0163,40.8099],[-94.0151,40.8961],[-93.9014,40.897],[-93.7884,40.8987],[-93.6741,40.8989],[-93.6109,40.8989],[-93.558,40.8985]]]},\"properties\":{\"name\":\"Decatur\",\"state\":\"IA\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57724e2de4b07657d1a81947","contributors":{"authors":[{"text":"Cagle, J.W.","contributorId":36229,"corporation":false,"usgs":true,"family":"Cagle","given":"J.W.","affiliations":[],"preferred":false,"id":640837,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Steinhilber, W. L.","contributorId":79456,"corporation":false,"usgs":true,"family":"Steinhilber","given":"W.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":640838,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70173977,"text":"70173977 - 1967 - Evaluation of potential sources of water in Crater Lake Natonal Park, Oregon","interactions":[],"lastModifiedDate":"2016-06-21T15:49:21","indexId":"70173977","displayToPublicDate":"1968-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Evaluation of potential sources of water in Crater Lake Natonal Park, Oregon","docAbstract":"<p>Crater Lake National Park, in volcanic terrain at the crest of the southern Cascade Range, is well watered by a 67-inch average annual precipitation, measured at park headquarters. Existing park facilities utilize springs that provide quantities of water adequate for present-day as well as foreseeable future needs.</p>\n<p>Ground water occurs under both perched and water-table conditions in the park. Perched ground-water bodies drain to the numerous springs that issue at various altitudes. Test drilling in the northern part failed to locate perched-water bodies capable of supplying quantities of water adequate for proposed facilities, and established that the regional water table is at an altitude below 4,960 feet.</p>\n<p>Many springs and streams at altitudes below 6,500 feet in the western, southern, and southeastern parts discharge quantities of water adequate for a variety of park facilities. Future park-facility development should take into account where water supplies are available. The western, southern, and southeastern parts of the park are more favorable than the northern part in this respect.</p>\n<p>In the northern part of the park, where there are no springs or streams, artificial catchment aprons and storage facilities could be constructed to provide water to points of use. A 100- by 100-foot catchment apron and suitably sized storage tank could provide as much as 1,850 gallons per day for 120 days.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Portland, OR","doi":"10.3133/70173977","usgsCitation":"Hampton, E.R., 1967, Evaluation of potential sources of water in Crater Lake Natonal Park, Oregon: Open-File Report, Report: i, 16 p.; Figure: 9.86 x 15.92 inches, https://doi.org/10.3133/70173977.","productDescription":"Report: i, 16 p.; Figure: 9.86 x 15.92 inches","numberOfPages":"20","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":324034,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70173977.jpg"},{"id":324141,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70173977/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":324162,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70173977/figure-1.pdf","text":"Figure 1","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon","otherGeospatial":"Crater Lake National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.29019165039062,\n              42.79741601927622\n            ],\n            [\n              -122.29019165039062,\n              43.08894918346591\n            ],\n            [\n              -121.98257446289062,\n              43.08894918346591\n            ],\n            [\n              -121.98257446289062,\n              42.79741601927622\n            ],\n            [\n              -122.29019165039062,\n              42.79741601927622\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"576913bae4b07657d19ff04e","contributors":{"authors":[{"text":"Hampton, E. R.","contributorId":57038,"corporation":false,"usgs":true,"family":"Hampton","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":639910,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70207462,"text":"70207462 - 1967 - ALVIN dives on the continental margin off the southeastern United States","interactions":[],"lastModifiedDate":"2022-12-23T16:13:14.205593","indexId":"70207462","displayToPublicDate":"1967-12-31T15:47:54","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"ALVIN dives on the continental margin off the southeastern United States","docAbstract":"<p><span>In late June and July, 1967, the Deep Submergence Research Vehicle (DSRV) ALVIN, aboard its mother snip, LULU, proceeded from the spring base of operations, Nassau, to its home port of Woods Hole. During this trip, from July 2 to July 14, a series of five dives were made by ALVIN on the Blake Plateau off Georgia and South Carolina, and on the continental slope north of Cape Hatteras.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70207462","usgsCitation":"Milliman, J.D., Manheim, F.T., Pratt, R.M., and Zarudzki, E.F., 1967, ALVIN dives on the continental margin off the southeastern United States, 70 p., https://doi.org/10.3133/70207462.","productDescription":"70 p.","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":370520,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Georgia, South Carolina","otherGeospatial":"Blake Plateau","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.54052734375,\n              30.741835717889792\n            ],\n            [\n              -79.07958984375,\n              30.278044377800153\n            ],\n            [\n              -76.8658447265625,\n              32.30106302536928\n            ],\n            [\n              -76.4373779296875,\n              33.280027811732154\n            ],\n            [\n              -78.5687255859375,\n              33.865854454071865\n            ],\n            [\n              -79.07958984375,\n              33.62376800118811\n            ],\n            [\n              -79.2169189453125,\n              33.18353672893615\n            ],\n            [\n              -79.85412597656249,\n              32.778037985363675\n            ],\n            [\n              -80.3594970703125,\n              32.47732919639942\n            ],\n            [\n              -80.57373046875,\n              32.26855544621476\n            ],\n            [\n              -81.112060546875,\n              31.793555207271424\n            ],\n            [\n              -81.5185546875,\n              30.713503990354965\n            ],\n            [\n              -81.54052734375,\n              30.741835717889792\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Milliman, John D.","contributorId":213518,"corporation":false,"usgs":false,"family":"Milliman","given":"John","email":"","middleInitial":"D.","affiliations":[{"id":38770,"text":"College of William and Mary, Virginia Institute of Marine Science","active":true,"usgs":false}],"preferred":false,"id":778139,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Manheim, Frank T. 0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":20770,"corporation":false,"usgs":true,"family":"Manheim","given":"Frank","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":778140,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pratt, R. M.","contributorId":41485,"corporation":false,"usgs":true,"family":"Pratt","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":778141,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Zarudzki, E. F. K.","contributorId":86759,"corporation":false,"usgs":true,"family":"Zarudzki","given":"E.","email":"","middleInitial":"F. K.","affiliations":[],"preferred":false,"id":778142,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70171294,"text":"70171294 - 1967 - Climate and streamflow of Puerto Rico","interactions":[],"lastModifiedDate":"2017-10-05T11:46:50","indexId":"70171294","displayToPublicDate":"1967-12-31T14:30:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1185,"text":"Caribbean Journal of Science","active":true,"publicationSubtype":{"id":10}},"title":"Climate and streamflow of Puerto Rico","docAbstract":"<p><span>The presently available data on&nbsp;streamflow, runoff rainfall, and temperature of Puerto&nbsp;Rico&nbsp;are evaluated, although the period of record is very short, with a view to contributing to the knowledge of hydrology of tropical islands. The average annual&nbsp;streamflow&nbsp;in&nbsp;Puerto&nbsp;Rico&nbsp;is&nbsp;45 percent&nbsp;of the annual rainfall, or 15 percent more than in the eastern piedmont of the U.S. where it is 30 percent.&nbsp;Climate&nbsp;is assumed to be responsible for this difference as well as for the differences of the flows of&nbsp;Puerto Rican streams which vary from 15 to 85 percent of the annual rainfall. Variations in the&nbsp;climate&nbsp;of&nbsp;Puerto&nbsp;Rico are shown by Thornthwaite's climatic index on a map of the island, and the variations of the streamflow&nbsp;to rainfall ratios of&nbsp;Puerto&nbsp;Rican streams are shown to be related to Thornthwaite's climatic index.</span></p>","language":"English","publisher":"University of Puerto Rico","usgsCitation":"Giusti, E., and Lopez, M.A., 1967, Climate and streamflow of Puerto Rico: Caribbean Journal of Science, v. 7, no. 3-4, p. 87-93.","productDescription":"7 p.","startPage":"87","endPage":"93","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":156,"text":"Caribbean Water Science Center","active":true,"usgs":true}],"links":[{"id":321744,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57481e2de4b07e28b664db8c","contributors":{"authors":[{"text":"Giusti, E.V.","contributorId":51342,"corporation":false,"usgs":true,"family":"Giusti","given":"E.V.","affiliations":[],"preferred":false,"id":630463,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lopez, M. A.","contributorId":12493,"corporation":false,"usgs":true,"family":"Lopez","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":630464,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70197629,"text":"70197629 - 1967 - Devonian rocks of the Yukon-Porcupine Rivers area and their tectonic relation to other Devonian sequences in Alaska","interactions":[],"lastModifiedDate":"2018-06-14T08:52:54","indexId":"70197629","displayToPublicDate":"1967-12-31T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Devonian rocks of the Yukon-Porcupine Rivers area and their tectonic relation to other Devonian sequences in Alaska","docAbstract":"<p class=\"indent\">Devonian rocks along the Yukon River near the Alaska-Yukon boundary comprise 250 feet of limestone and shale and 800 feet of chert and siliceous shale, all referred to the McCann Hill Chert of Early to Late Devonian age; about 3,000 feet of non-marine chert-pebble conglomerate, graywacke, and shale of the Nation River Formation (Late Devonian); and about 3,000 feet of an unnamed chert and siliceous shale formation, of Late Devonian to Early or Late Mississippian age. The McCann Hill Chert apparently rests disconformably on graptolitic shale of the Road River Formation that has a succession of graptolite zones ranging in age from Ordovician to possibly Early Devonian.</p><p class=\"indent\">The Devonian succession along the Porcupine River, 170 miles north of the Yukon River locality, consists of 600 feet of Salmon-trout Limestone, overlain by 200 feet of unnamed shale and about 500 feet of unnamed dolomite. The Salmontrout Limestone rests accordantly and probably conformably on graptolitic shale with<span>&nbsp;</span><i>Monograptus hercynicus</i><span>&nbsp;</span>of Late Silurian or Early Devonian age, and the dolomite is overlain unconformably by limestone and shale of Carboniferous age.</p><p class=\"indent\">Tentaculitid faunas from the top of the Salmontrout Limestone and from the basal limestone and shale member of the McCann Hill Chert are similar and indicate that the units are partly correlative. These faunas and others throughout the Salmontrout resemble those from the Lower Devonian of Bohemia, indicating that the Salmontrout Limestone and the limestone and shale member of the McCann Hill Chert are somewhat older than previously reported. The faunas, and those from the underlying graptolitic shales, also suggest that sedimentation in this area of Alaska was nearly continuous from Late Silurian into the Earliest Devonian, and that there is little record of Caledonian earth movements.</p><p class=\"indent\">The stratigraphy of the Porcupine River area is not as yet well enough established to determine if rocks equivalent in age to the Nation River Formation are present, were once present and have since been eroded, or were never deposited.</p><p class=\"indent\">Pillow basalt and andesitic breccia, although closely associated with Devonian limestone in the western part of the Yukon-Porcupine Rivers area, seem only structurally related and of different age.</p><p class=\"indent\">Devonian rocks in southern and southeastern Alaska consist of several thousand feet of graywacke, shale and volcanic rocks deposited in the northern Cordilleran geosyncline. A combination of strike-slip and thrust faults of Tertiary and Mesozoic age may have since displaced the Devonian geosynclinal rocks relatively northward into central Alaska.</p>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"International Symposium of the Devonian system: Papers","conferenceTitle":"International Symposium of the Devonian system","conferenceDate":"1967","conferenceLocation":"Calgary, CA","language":"English","publisher":"AAPG","usgsCitation":"Churkin, M., and Brabb, E.E., 1967, Devonian rocks of the Yukon-Porcupine Rivers area and their tectonic relation to other Devonian sequences in Alaska, <i>in</i> International Symposium of the Devonian system: Papers, v. 2, Calgary, CA, 1967, p. 227-258.","productDescription":"32 p.","startPage":"227","endPage":"258","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":355039,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","volume":"2","tableOfContents":"<p><br data-mce-bogus=\"1\"></p>","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Churkin, Michael Jr.","contributorId":62566,"corporation":false,"usgs":true,"family":"Churkin","given":"Michael","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":737980,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brabb, Earl E.","contributorId":48939,"corporation":false,"usgs":true,"family":"Brabb","given":"Earl","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":737981,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010516,"text":"70010516 - 1967 - Sierra Nevada batholith","interactions":[],"lastModifiedDate":"2026-02-06T17:00:22.593567","indexId":"70010516","displayToPublicDate":"1967-12-15T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Sierra Nevada batholith","docAbstract":"<p><span>The Sierra Nevada batholith is localized in the axial region of a complex faulted synclinorium that coincides with a downfold in the Mohorovicic discontinuity and in P-wave velocity boundaries within the crust. Observed P-wave velocities are compatible with downward increase in the proportion of diorite, quartz diorite, and calcic granodiorite relative to quartz monzonite and granite in the upper crust, with amphibolite or gabbro-basalt in the lower crust, and with periodotite in the upper mantle. The synclinorium was formed in Paleozoic and Mesozoic strata during early and middle Mesozoic time in a geosyncline marginal to the continent. Granitic magmas are believed to have formed in the lower half of the crust at depths of 25 to 45 kilometers or more, primarily as a result of high radiogenic heat production in the thickened prism of crustal rocks. Magma was generated at different times in different places as the locus of downfolding shifted. It rose into the upper crust because it was less dense than rock of the same composition or residual refractory rocks. Refractory rocks and crystals that were not melted and early crystallized mafic minerals that settled from the rising magma thickened the lower crust. Wall and roof rocks settled around, and perhaps through, the rising magma and provided space for its continued rise. Erosion followed each magmatic episode, and 10 to 12 kilometers of rock may have been eroded away since the Jurassic and 7 to 10 kilometers since the early Late Cretaceous.</span></p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.158.3807.1407","issn":"00368075","usgsCitation":"Bateman, P.C., and Eaton, J.P., 1967, Sierra Nevada batholith: Science, v. 158, no. 3807, p. 1407-1417, https://doi.org/10.1126/science.158.3807.1407.","productDescription":"11 p.","startPage":"1407","endPage":"1417","costCenters":[],"links":[{"id":219534,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Sierra Nevada","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.7841796875,\n              35.06597313798418\n            ],\n            [\n              -113.818359375,\n              34.52466147177172\n            ],\n            [\n              -118.34472656249997,\n              39.639537564366684\n            ],\n            [\n              -122.29980468749999,\n              43.03677585761058\n            ],\n            [\n              -123.35449218749997,\n              39.639537564366684\n            ],\n            [\n              -118.7841796875,\n              35.06597313798418\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"158","issue":"3807","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8f0ae4b08c986b318cc5","contributors":{"authors":[{"text":"Bateman, P. C.","contributorId":27851,"corporation":false,"usgs":true,"family":"Bateman","given":"P.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":359096,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eaton, J. P.","contributorId":105313,"corporation":false,"usgs":true,"family":"Eaton","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":359097,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011594,"text":"70011594 - 1967 - Freshwater peat on the continental shelf","interactions":[],"lastModifiedDate":"2026-02-06T17:18:25.460631","indexId":"70011594","displayToPublicDate":"1967-12-08T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Freshwater peat on the continental shelf","docAbstract":"Freshwater peats from the continental shelf off northeastern United States contain the same general pollen sequence as peats from ponds that are above sea level and that are of comparable radiocarbon ages. These peats indicate that during glacial times of low sea level terrestrial vegetation covered the region that is now the continental shelf in an unbroken extension from the adjacent land areas to the north and west.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.158.3806.1301","issn":"00368075","usgsCitation":"Emery, K., Wigley, R.L., Bartlett, A., Rubin, M., and Barghoorn, E., 1967, Freshwater peat on the continental shelf: Science, v. 158, no. 3806, p. 1301-1307, https://doi.org/10.1126/science.158.3806.1301.","productDescription":"7 p.","startPage":"1301","endPage":"1307","costCenters":[],"links":[{"id":221679,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"northeastern United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -67.67832559541925,\n              45.59295017118643\n            ],\n            [\n              -74.11886076058204,\n              43.28900296242085\n            ],\n            [\n              -75.98845493237955,\n              39.35817375874926\n            ],\n            [\n              -74.69853368493818,\n              38.767484141109136\n            ],\n            [\n              -71.23564085374394,\n              37.67242518679933\n            ],\n            [\n              -66.84637765114445,\n              44.53252563215288\n            ],\n            [\n              -67.67832559541925,\n              45.59295017118643\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"158","issue":"3806","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a13e6e4b0c8380cd5480b","contributors":{"authors":[{"text":"Emery, K.O.","contributorId":67865,"corporation":false,"usgs":true,"family":"Emery","given":"K.O.","email":"","affiliations":[],"preferred":false,"id":361496,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wigley, R. L.","contributorId":18440,"corporation":false,"usgs":true,"family":"Wigley","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":361495,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bartlett, A.S.","contributorId":80820,"corporation":false,"usgs":true,"family":"Bartlett","given":"A.S.","email":"","affiliations":[],"preferred":false,"id":361497,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rubin, M.","contributorId":88079,"corporation":false,"usgs":true,"family":"Rubin","given":"M.","email":"","affiliations":[],"preferred":false,"id":361498,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Barghoorn, E.S.","contributorId":105052,"corporation":false,"usgs":true,"family":"Barghoorn","given":"E.S.","email":"","affiliations":[],"preferred":false,"id":361499,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70011556,"text":"70011556 - 1967 - Silica in alkaline brines","interactions":[],"lastModifiedDate":"2026-02-06T17:25:28.745288","indexId":"70011556","displayToPublicDate":"1967-12-08T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Silica in alkaline brines","docAbstract":"<p><span id=\"_mce_caret\" data-mce-bogus=\"1\" data-mce-type=\"format-caret\"><span>Analysis of sodium carbonate-bicarbonate brines from closed basins in volcanic terranes of Oregon and Kenya reveals silica contents of up to 2700 parts per million at&nbsp;</span><i>p</i><span>H's higher than 10. These high concentrations of SiO</span><sub>2</sub><span>&nbsp;can be attributed to reaction of waters with silicates, and subsequent evaporative concentration accompanied by a rise in&nbsp;</span><i>p</i><span>H. Supersaturation with respect to amorphous silica may occur and persist for brines that are out of contact with silicate muds and undersaturated with respect to trona; correlation of SiO</span><sub>2</sub><span>&nbsp;with concentration of Na and total CO</span><sub>2</sub><span>&nbsp;support this interpretation. Addition of more-dilute waters to alkaline brines may lower the&nbsp;</span><i>p</i><span>H and cause inorganic precipitation of substantial amounts of silica.</span></span></p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.158.3806.1310","issn":"00368075","usgsCitation":"Jones, B., Rettig, S., and Eugster, H., 1967, Silica in alkaline brines: Science, v. 158, no. 3806, p. 1310-1314, https://doi.org/10.1126/science.158.3806.1310.","productDescription":"5 p.","startPage":"1310","endPage":"1314","costCenters":[],"links":[{"id":221119,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"158","issue":"3806","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8f32e4b08c986b318da9","contributors":{"authors":[{"text":"Jones, B.F.","contributorId":52156,"corporation":false,"usgs":true,"family":"Jones","given":"B.F.","email":"","affiliations":[],"preferred":false,"id":361398,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rettig, S.L.","contributorId":42592,"corporation":false,"usgs":true,"family":"Rettig","given":"S.L.","email":"","affiliations":[],"preferred":false,"id":361397,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Eugster, H.P.","contributorId":99992,"corporation":false,"usgs":true,"family":"Eugster","given":"H.P.","email":"","affiliations":[],"preferred":false,"id":361399,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70221321,"text":"70221321 - 1967 - Stratigraphy and paleoenvironment of the phosphatic miocene strata of North Carolina","interactions":[],"lastModifiedDate":"2021-06-09T19:09:08.163317","indexId":"70221321","displayToPublicDate":"1967-12-01T14:04:13","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Stratigraphy and paleoenvironment of the phosphatic miocene strata of North Carolina","docAbstract":"<p><span>Foraminifera and Mollusca collected from the&nbsp;</span>phosphatic<span>&nbsp;Pungo River Formation and the overlying Yorktown Formation in eastern&nbsp;</span>North<span>&nbsp;</span>Carolina<span>&nbsp;were analyzed and interpreted for stratigraphic and environmental significance in order to determine optimum depositional sites for primary phosphorite. The Mollusca and benthonic foraminifera of the Pungo River Formation correlate with those of the Calvert Formation of Maryland, and the planktonic foraminifera in both of these formations correlate with the Globigerinatella insueta zone of Trinidad, postulated as late Aquitanian age. The&nbsp;</span>paleoenvironment<span>&nbsp;of the phosphorite deposition, interpreted primarily from the benthonic foraminifera, was of cool-temperate waters, ranging in depth from 100 to 200 m in the&nbsp;</span>phosphatic<span>&nbsp;beds to less than 70 m in the upper calcareous beds where phosphate is scarce. Phosphorite deposition occurred in an oceanic embayment located south of the Fort Monroe high in southern Virginia and&nbsp;</span>north<span>&nbsp;of a positive feature whose axis lies in the vicinity of New Bern,&nbsp;</span>North<span>&nbsp;</span>Carolina<span>. Cool-temperate waters in this area during Pungo River time indicate that circulation patterns of ocean currents and the resultant faunal provinces were not the same as those at present and later in the&nbsp;</span>Miocene<span>. In the Pungo River and its time equivalents of the Atlantic Coastal Plain, the presence of thick diatomaceous clay units, volcanic ash beds, shards, attapulgite clays, and other minerals probably derived from volcanic rocks, suggests a volcanic source somewhere off the coast during the&nbsp;</span>Miocene<span>. The Yorktown unconformably overlies the Pungo River Formation. The unconformity is marked by channels into the Pungo River, filled with&nbsp;</span>phosphatic<span>&nbsp;pebbles, vertebrate bones, and lower York-town molluscs and microfauna. The coarse-grained&nbsp;</span>phosphatic<span>&nbsp;material is derived from the underlying fine-grained primary phosphorite in the Pungo River and is abundant only in the lower part of the Yorktown Formation. Deposition of the lower part of the Yorktown occurred in waters about 100 m deep. The waters gradually became more shallow as deposition of the formation continued until depths of less than 15 m, and probable brackish conditions, were reached as the uppermost part of the formation was deposited. Temperature of the waters, cool-temperate during lower Yorktown deposition, became warm-temperate to subtropical in later Yorktown time. The faunal patterns suggest that circulation patterns reached their present state during late Yorktown time.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1967)78[631:SAPOTP]2.0.CO;2","usgsCitation":"Gibson, T., 1967, Stratigraphy and paleoenvironment of the phosphatic miocene strata of North Carolina: Geological Society of America Bulletin, v. 78, no. 5, p. 631-650, https://doi.org/10.1130/0016-7606(1967)78[631:SAPOTP]2.0.CO;2.","productDescription":"20 p.","startPage":"631","endPage":"650","costCenters":[],"links":[{"id":386367,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"North Carolina","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -75.8056640625,\n              36.61552763134925\n            ],\n            [\n              -81.6943359375,\n              36.686041276581925\n            ],\n            [\n              -83.78173828125,\n              35.55010533588552\n            ],\n            [\n              -84.30908203125,\n              35.08395557927643\n            ],\n            [\n              -84.30908203125,\n              34.97600151317588\n            ],\n            [\n              -80.947265625,\n              35.137879119634185\n            ],\n            [\n              -80.70556640625,\n              34.813803317113155\n            ],\n            [\n              -79.6728515625,\n              34.77771580360469\n            ],\n            [\n              -78.5302734375,\n              33.88865750124075\n            ],\n            [\n              -78.0908203125,\n              33.925129700072\n            ],\n            [\n              -76.201171875,\n              34.831841149828655\n            ],\n            [\n              -75.52001953125,\n              35.764343479667176\n            ],\n            [\n              -75.8056640625,\n              36.61552763134925\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"78","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Gibson, T. G.","contributorId":103702,"corporation":false,"usgs":true,"family":"Gibson","given":"T. G.","affiliations":[],"preferred":false,"id":817299,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221317,"text":"70221317 - 1967 - Time and space relationships of the taconic allochthon and autochthon","interactions":[],"lastModifiedDate":"2021-06-09T18:42:14.902827","indexId":"70221317","displayToPublicDate":"1967-12-01T13:38:56","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3459,"text":"Special Paper of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Time and space relationships of the taconic allochthon and autochthon","docAbstract":"<p><span>The&nbsp;</span>Taconic<span>&nbsp;rock sequence extends from near Sudbury, Vermont, to near Poughkeepsie, New York, a length of about 150 miles; and from just west of the Green Mountain Range and Berkshire Highlands to the valleys of the Hudson River and Lake Champlain, a width of about 20 miles. The&nbsp;</span>Taconic<span>&nbsp;rocks are now in the axial region of the Middlebury synclinorium and its southward extension. The&nbsp;</span>Taconic<span>&nbsp;sequence consists of about 2000 feet of slate, with subsidiary graywacke, quartzite, and limestone; many of the rock units are turbidites. Fossils from the rocks include forms of Early, Middle, and Late Cambrian and Early and Middle Ordovician age. Evidence of stratigraphic tops derived from the fossils and from primary sedimentary features agrees with structural data and demonstrates that the&nbsp;</span>Taconic<span>&nbsp;rocks are geometrically the highest strata within the Middlebury synclinorium. The underlying rocks of the synclinorium (the synclinorium sequence) are right side up; they also range in age from Early Cambrian to Middle Ordovician but belong to a different sedimentary lithofacies (dominantly carbonate and orthoquartzite). The relation between the&nbsp;</span>Taconic<span>&nbsp;sequence and the synclinorium sequence, therefore, is a baffling problem. Lithostratigraphically, the&nbsp;</span>Taconic<span>&nbsp;sequence falls into three groups: (1) the pre- Normanskill \"low&nbsp;</span>Taconic<span>\" sequence, occurring in the area between the main&nbsp;</span>Taconic<span>&nbsp;Range and the Hudson River, as far south as Rhinebeck, New York; (2) the Normanskill Shale in the same area, as well as in the area south of Rhinebeck at least as far as Poughkeepsie, New York, and also west of the Hudson River; and (3) the \"high&nbsp;</span>Taconic<span>\" sequence, occupying the main&nbsp;</span>Taconic<span>&nbsp;Range from Dorset Mountain, Vermont, south to Indian Mountain in Sharon, Connecticut, as well as Mount Greylock in Massachusetts. Rocks of (1) and (2) are fossiliferous, but to date no fossil has been found in (3). Rocks of (1) and that part of (2) areally coextensive with (1) thus are of known age but uncertain three-dimensional geometric configuration, whereas rocks of (3) are of known configuration (in the centers of open synclinoria) but unknown age. Only that part of (2) beyond the areal confines of (1) is both of known age and known configuration; these rocks are in sedimentary contact above the older rocks of the synclinorium sequence and are autochthonous. At the north end of the&nbsp;</span>Taconic<span>&nbsp;sequence in western Vermont, rocks of group (1) are beyond reasonable doubt allochthonous. Because of the southward geometric continuity of the structural elements, all the&nbsp;</span>Taconic<span>&nbsp;rocks of group (1), and that part of group (2) areally coextensive with it, are interpreted as allochthonous. The structure of group (3), the high&nbsp;</span>Taconic<span>&nbsp;sequence, is inferred by topography and by detailed lithostratigraphic matching with rocks of the east Vermont sequence; on this basis, as well as on the basis of the broad lithic similarity with rocks of group (1), rocks of group (3) are concluded to be also allochthonous. A discontinuous polymict conglomerate underlies and surrounds the&nbsp;</span>allochthon<span>&nbsp;on all sides and is interpreted here as a record that dates the imminent arrival of the&nbsp;</span>allochthon<span>&nbsp;at each locality. The conglomerate contains unsorted blocks of rocks of both the&nbsp;</span>Taconic<span>&nbsp;sequence and the synclinorium sequence; the matrix is the autochthonous upper Normanskill Shale or its equivalent. Fossils from the matrix shale date the event as Trenton, probably Sherman Fall in age. The geologic history of the area is reconstructed as follows: The pre-Normanskill&nbsp;</span>Taconic<span>&nbsp;rocks were deposited in the area of the present Precambrian massifs of the Green Mountains-Berkshire Highlands belt between the clastic, eugeosynclinal east Vermont sequence to the east and the miogeosynclinal synclinorium sequence to the west; they constitute the transitional facies between these two belts. Conditions were relatively stable until early Middle Ordovician&nbsp;</span>time<span>, when the Green Mountain- Berkshire Highlands area began to rise and the area of the present Middlebury synclinorium began to subside. Subsidence took place largely by a series of high-angle longitudinal faults that, as a whole, step down to the west. Argillaceous sediments (the Normanskill Shale) began to inundate the former miogeosynclinal area; because the conditions of sedimentation had become similar, the sediments resembled, in facies, the synchronous&nbsp;</span>Taconic<span>&nbsp;rocks that were being deposited to the east. Continued rise of the Green Mountains-Berkshire Highlands area led in middle Trenton&nbsp;</span>time<span>&nbsp;to the decollement of the Cambrian and Ordovician sediments into the area of the present Middlebury synclinorium in a series of giant submarine slides. Sedimentation continued at the receiving site throughout the event; sedimentation may also have persisted on the moving slides. The record is found today in the turbidite-laden shale and graywacke in the upper part of the Normanskill Shale of both the&nbsp;</span>allochthon<span>&nbsp;and the&nbsp;</span>autochthon<span>. Restoration of the allochthonous rocks to the original site of deposition leads to correlations between rocks of the&nbsp;</span>Taconic<span>&nbsp;sequence and of the largely autochthonous east Vermont sequence. The lithic correlation can be carried to the level of individual formations and is confirmed by a few known ages in the east Vermont sequence. Several lines of reasoning lead to a plausible correlation of part of the Cavendish Formation of southeastern Vermont with the oldest part of the&nbsp;</span>Taconic<span>&nbsp;sequence. This correlation leads further to the conclusion that in this area the contacts between the Green Mountain massif and the Cavendish Formation and between the Cavendish and the overlying east Vermont sequence must both be thrust faults of large displacements. This conclusion is in fact inevitable because one of the&nbsp;</span>Taconic<span>&nbsp;thrust slices that extends without interruption between the latitudes corresponding to the gap in the Precambrian massifs has been shown by local structural evidence to be allochthonous; an outside original depositional site must be found for it. The present&nbsp;</span>Taconic<span>&nbsp;</span>allochthon<span>&nbsp;is coextensive with an area of marked negative Bouguer gravity anomaly; the Green Mountains-Berkshire massifs constitute a belt of positive anomaly. It is here proposed that these anomalies resulted from a deepseated transfer of material; subcrustal addition of material caused the rise of the Green Mountains-Berkshire Highlands area, and the concurrent subtraction of material caused subsidence in the Middlebury synclinorium area through a series of faults which were the near-surface expression of an episode of crustal collapse. If this interpretation is correct, then the regional gravity anomaly represents an uncompensated feature that has persisted since Middle Ordovician&nbsp;</span>time<span>.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/SPE97-p1","usgsCitation":"Zen, E., 1967, Time and space relationships of the taconic allochthon and autochthon: Special Paper of the Geological Society of America, v. 97, p. 1-82, https://doi.org/10.1130/SPE97-p1.","productDescription":"82 p.","startPage":"1","endPage":"82","costCenters":[],"links":[{"id":386363,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"97","noUsgsAuthors":false,"publicationDate":"1967-01-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Zen, E.","contributorId":101381,"corporation":false,"usgs":true,"family":"Zen","given":"E.","email":"","affiliations":[],"preferred":false,"id":817294,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221302,"text":"70221302 - 1967 - Orthorhombic sulphur formed by photosynthetic sulphur bacteria","interactions":[],"lastModifiedDate":"2021-06-10T12:00:19.386997","indexId":"70221302","displayToPublicDate":"1967-12-01T10:55:25","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"Orthorhombic sulphur formed by photosynthetic sulphur bacteria","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Nature","doi":"10.1038/215435a0","usgsCitation":"Truper, H., and Hathaway, J., 1967, Orthorhombic sulphur formed by photosynthetic sulphur bacteria: Nature, v. 215, no. 5099, p. 435-436, https://doi.org/10.1038/215435a0.","productDescription":"2 p.","startPage":"435","endPage":"436","costCenters":[],"links":[{"id":386349,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"215","issue":"5099","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Truper, H.G.","contributorId":260106,"corporation":false,"usgs":false,"family":"Truper","given":"H.G.","email":"","affiliations":[],"preferred":false,"id":817277,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hathaway, J.C.","contributorId":94280,"corporation":false,"usgs":true,"family":"Hathaway","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":817278,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70221361,"text":"70221361 - 1967 - Rocks of eocene age on fippennies ledge, Gulf of Maine","interactions":[],"lastModifiedDate":"2021-06-11T13:36:14.085543","indexId":"70221361","displayToPublicDate":"1967-12-01T08:32:23","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Rocks of eocene age on fippennies ledge, Gulf of Maine","docAbstract":"<p><span>In August 1965, a scallop dredge from R/V Albatross brought up many pieces of fossiliferous opaline chert or porcellanite of&nbsp;</span>Eocene<span>&nbsp;</span>age<span>&nbsp;from&nbsp;</span>Fippennies<span>&nbsp;</span>Ledge<span>, a bank 70 m deep in the central&nbsp;</span>Gulf<span>&nbsp;of&nbsp;</span>Maine<span>. Their presence in this area supports the idea that part of the&nbsp;</span>Gulf<span>&nbsp;is underlain by sedimentary&nbsp;</span>rocks<span>&nbsp;of Tertiary&nbsp;</span>age<span>. Occurrence in the porcellanite of two identifiable species of Bryozoa (ascophoran Cheilostomata), Kleidionella lobata Canu and Bassler and \"Ocheto-sella\" robusta Canu and Bassler, suggests (1) correlation with the Castle Hayne Limestone of Claiborne to Jackson&nbsp;</span>age<span>; (2) a temperate zone, distinctly American biogeographic provenance; and (3) accumulation in quiet water.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1967)78[681:ROEAOF]2.0.CO;2","usgsCitation":"Schlee, J., and Cheetham, A., 1967, Rocks of eocene age on fippennies ledge, Gulf of Maine: Geological Society of America Bulletin, v. 78, no. 5, p. 81-84, https://doi.org/10.1130/0016-7606(1967)78[681:ROEAOF]2.0.CO;2.","productDescription":"4 p.","startPage":"81","endPage":"84","costCenters":[],"links":[{"id":386424,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Maine","otherGeospatial":"Gulf of Maine","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -65.55541992187499,\n              43.42100882994726\n            ],\n            [\n              -66.181640625,\n              43.83452678223682\n            ],\n            [\n              -66.236572265625,\n              44.47299117260252\n            ],\n            [\n              -67.467041015625,\n              44.6061127451739\n            ],\n            [\n              -68.873291015625,\n              44.49650533109348\n            ],\n            [\n              -70.059814453125,\n              43.874138181474734\n            ],\n            [\n              -70.59814453125,\n              43.389081939117496\n            ],\n            [\n              -70.894775390625,\n              42.775243380699706\n            ],\n            [\n              -70.587158203125,\n              42.601619944327965\n            ],\n            [\n              -68.73046875,\n              42.22851735620852\n            ],\n            [\n              -65.55541992187499,\n              43.42100882994726\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"78","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Schlee, J.","contributorId":45821,"corporation":false,"usgs":true,"family":"Schlee","given":"J.","affiliations":[],"preferred":false,"id":817423,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cheetham, A.H.","contributorId":76189,"corporation":false,"usgs":true,"family":"Cheetham","given":"A.H.","email":"","affiliations":[],"preferred":false,"id":817424,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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