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,{"id":15389,"text":"ofr6699 - 1966 - Principal facts for gravity stations in the San Francisco Mountains vicinity, Beaver and Millard Counties, Utah","interactions":[{"subject":{"id":15389,"text":"ofr6699 - 1966 - Principal facts for gravity stations in the San Francisco Mountains vicinity, Beaver and Millard Counties, Utah","indexId":"ofr6699","publicationYear":"1966","noYear":false,"title":"Principal facts for gravity stations in the San Francisco Mountains vicinity, Beaver and Millard Counties, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043043,"text":"70043043 - 1972 - Principal facts for gravity stations in the San Francisco district and adjoining areas, Utah","indexId":"70043043","publicationYear":"1972","noYear":false,"title":"Principal facts for gravity stations in the San Francisco district and adjoining areas, Utah"},"id":1}],"supersededBy":{"id":70043043,"text":"70043043 - 1972 - Principal facts for gravity stations in the San Francisco district and adjoining areas, Utah","indexId":"70043043","publicationYear":"1972","noYear":false,"title":"Principal facts for gravity stations in the San Francisco district and adjoining areas, Utah"},"lastModifiedDate":"2021-03-18T21:02:22.720531","indexId":"ofr6699","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"66-99","title":"Principal facts for gravity stations in the San Francisco Mountains vicinity, Beaver and Millard Counties, Utah","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr6699","usgsCitation":"Peterson, D.L., 1966, Principal facts for gravity stations in the San Francisco Mountains vicinity, Beaver and Millard Counties, Utah: U.S. Geological Survey Open-File Report 66-99, 18 p., https://doi.org/10.3133/ofr6699.","productDescription":"18 p.","costCenters":[],"links":[{"id":384464,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1966/0099/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":147811,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1966/0099/report-thumb.jpg"}],"country":"United States","state":"Utah","county":"Beaver County, Millard County","otherGeospatial":"San Francisco Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.44757080078124,\n              38.40410147066251\n            ],\n            [\n              -113.1317138671875,\n              38.40410147066251\n            ],\n            [\n              -113.1317138671875,\n              38.511639141458616\n            ],\n            [\n              -113.44757080078124,\n              38.511639141458616\n            ],\n            [\n              -113.44757080078124,\n              38.40410147066251\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667b09","contributors":{"authors":[{"text":"Peterson, Donald L.","contributorId":28597,"corporation":false,"usgs":true,"family":"Peterson","given":"Donald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":171055,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14054,"text":"ofr6660 - 1966 - Geophysical and geological investigations relating to earthquakes in the Denver area, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:51","indexId":"ofr6660","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"66-60","title":"Geophysical and geological investigations relating to earthquakes in the Denver area, Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr6660","usgsCitation":"Healy, J.H., and and others, 1966, Geophysical and geological investigations relating to earthquakes in the Denver area, Colorado: U.S. Geological Survey Open-File Report 66-60, 59 p. ill., maps ;30 cm., https://doi.org/10.3133/ofr6660.","productDescription":"59 p. ill., maps ;30 cm.","costCenters":[],"links":[{"id":258478,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1966/0060/report.pdf","size":"9621","linkFileType":{"id":1,"text":"pdf"}},{"id":258479,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1966/0060/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c29b","contributors":{"authors":[{"text":"Healy, J. H.","contributorId":48968,"corporation":false,"usgs":true,"family":"Healy","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":168856,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"and others","contributorId":127886,"corporation":true,"usgs":false,"organization":"and others","id":528972,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":14331,"text":"ofr6669 - 1966 - Engineering geology of Lexington and Fayette County, Kentucky","interactions":[],"lastModifiedDate":"2022-12-30T21:14:52.309556","indexId":"ofr6669","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"66-69","title":"Engineering geology of Lexington and Fayette County, Kentucky","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6669","usgsCitation":"Johnson, C.G., and Hopkins, H.T., 1966, Engineering geology of Lexington and Fayette County, Kentucky: U.S. Geological Survey Open-File Report 66-69, Report: 19 p.; 7 Plates: 26.40 x 45.86 inches or smaller, https://doi.org/10.3133/ofr6669.","productDescription":"Report: 19 p.; 7 Plates: 26.40 x 45.86 inches or smaller","costCenters":[],"links":[{"id":411252,"rank":10,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8138.htm","linkFileType":{"id":5,"text":"html"}},{"id":42999,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1966/0069/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42998,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0069/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42997,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0069/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42996,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0069/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42995,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0069/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42994,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0069/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42993,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0069/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42992,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0069/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148520,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1966/0069/report-thumb.jpg"}],"country":"United States","state":"Kentucky","county":"Fayette County, Lexington County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -84.7054032562891,\n              38.21627540794438\n            ],\n            [\n              -84.7054032562891,\n              37.81135562424184\n            ],\n            [\n              -84.27474877334932,\n              37.81135562424184\n            ],\n            [\n              -84.27474877334932,\n              38.21627540794438\n            ],\n            [\n              -84.7054032562891,\n              38.21627540794438\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db60276a","contributors":{"authors":[{"text":"Johnson, Charles George","contributorId":24365,"corporation":false,"usgs":true,"family":"Johnson","given":"Charles","email":"","middleInitial":"George","affiliations":[],"preferred":false,"id":169274,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hopkins, H. T.","contributorId":35749,"corporation":false,"usgs":true,"family":"Hopkins","given":"H.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":169275,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":13769,"text":"ofr66143 - 1966 - Test data sheets for \"Symposium on Shale\" field trip","interactions":[],"lastModifiedDate":"2019-11-10T19:09:51","indexId":"ofr66143","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"66-143","title":"Test data sheets for \"Symposium on Shale\" field trip","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr66143","usgsCitation":"Scott, G.R., Kirchen, H., and Lindvall, R.M., 1966, Test data sheets for \"Symposium on Shale\" field trip: U.S. Geological Survey Open-File Report 66-143, 21 p., https://doi.org/10.3133/ofr66143.","productDescription":"21 p.","costCenters":[],"links":[{"id":145347,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684cb1","contributors":{"authors":[{"text":"Scott, Glenn R.","contributorId":102046,"corporation":false,"usgs":true,"family":"Scott","given":"Glenn","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":168356,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kirchen, H.W.","contributorId":104904,"corporation":false,"usgs":true,"family":"Kirchen","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":168357,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lindvall, R. M.","contributorId":53797,"corporation":false,"usgs":true,"family":"Lindvall","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":168355,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":13341,"text":"ofr6624 - 1966 - Geology of the Cerro Summit quadrangle, Montrose County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:07:02","indexId":"ofr6624","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"66-24","title":"Geology of the Cerro Summit quadrangle, Montrose County, Colorado","docAbstract":"The Cerro Summit quadrangle covers 58 square miles of dissected plateau on the south flank of the Gunnison uplift in southwestern Colorado. It lies east of the Uncompahgre River valley and south of the Black Canyon of the Gunnison River. Rocks dip gently in most of the quadrangle, but they are locally upturned and faulted on the margin of the Gunnison uplift and are intensely deformed in the core of the uplift. The rocks exposed are of Precambrian, late Mesozoic, and Cenozoic age. \r\n\r\nPrecambrian rocks include metasedimentary schist and gneiss, granitic pegmatite, and olivine gabbro. The oldest Mesozoic rocks exposed are continental, fresh-water, and lagoonal deposits in the Late Jurassic Entrada Sandstone, Wanakah Formation, and Morrison Formation. Channel-fill deposits that unconformably overlie the Jurassic rocks are possibly the Burro Canyon Formation of Early Cretaceous age. Upper Cretaceous rocks include marine and nearshore deposits of the Dakota \r\n\r\nSandstone, Mancos Shale, and Pictured Cliffs Sandstone, and the fresh- and brackish-water sandstone, shale, and coal of the Fruitland Formation. Rocks of Late Cretaceous age that crop out in the adjacent Cimarron Ridge area may also have been deposited in this quadrangle but are now eroded; these rocks include the nonmarine Kirtland Shale and an unnamed volcanic conglomerate and tuff breccia. Nine faunal zones in the Mancos Shale help to establish the correct correlation of units in the Upper Cretaceous. The Pictured Cliffs Sandstone, Fruitland Formation, and Kirtland Shale of the Cerro Summit area have been mapped by some geologists as the Mesaverde Formation. Fossils indicate that the rocks are younger than the type Mesaverde. The unnamed volcanic rocks represent major volcanism in nearby areas. A Late Cretaceous (Maestrichtian) age for the volcanism is indicated by palynological evidence and an isotopic age of approximately 66 million years. Middle Tertiary rocks are conglomerate and tuff breccia. Upper Tertiary or lower Quaternary rocks include gravel along Pool Gulch and older landslide debris on Waterdog Peak. Pleistocene and Recent deposits consist of the older stream gravel of Shinn Park, valley-fill deposits of Bostwick-Shinn Park, and pediment, landslide, eolian, alluvial, and colluvial deposits. P1elstocene valley-fill deposits of Bostwick-Shinn Park were deposited during the Cedar Ridge, or Kansan, to Pinedale or late Wisconsin times. The valley-fill deposits are divided into five units that are separated by strong Interglacial or Interstadial soils and that contain three volcanic ash beds. Chemical and petrographic data suggest that the middle ash bed may correlate with the Pearlette Ash Member (late Kansan) of the Sappa Formation in Nebraska. Alluvium on two pediment surfaces seems to be of Sacagawea Ridge or Illinoian age. Landslide deposits, of Pleistocene and Recent age, cover about 85 percent of the quadrangle; most of the deposits were formerly mapped as till. The name Cerro Till was abandoned because till does not occur in the type area.\r\n\r\nThe dominant tectonic structures are the high-angle Cimarron fault of a few thousand feet displacement and the broad Montrose syncline. Evidence in the Cimarron Ridge area suggests that these structures formed in Late Cretaceous (Maestrichtian) time. Much of the strata near the surface of the quadrangle has been involved in landsliding that has continued from late Tertiary to the present.","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr6624","usgsCitation":"Dickinson, R.G., 1966, Geology of the Cerro Summit quadrangle, Montrose County, Colorado: U.S. Geological Survey Open-File Report 66-24, 117 p. ill., 2 maps (1 col.) ;30 cm., https://doi.org/10.3133/ofr6624.","productDescription":"117 p. ill., 2 maps (1 col.) ;30 cm.","costCenters":[],"links":[{"id":147751,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1966/0024/report-thumb.jpg"},{"id":41765,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0024/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41766,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1966/0024/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae884","contributors":{"authors":[{"text":"Dickinson, Robert G.","contributorId":79489,"corporation":false,"usgs":true,"family":"Dickinson","given":"Robert","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":167651,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":13883,"text":"ofr6653 - 1966 - Strike-slip faults in Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:06:38","indexId":"ofr6653","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"66-53","title":"Strike-slip faults in Alaska","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr6653","usgsCitation":"Grantz, A., 1966, Strike-slip faults in Alaska: U.S. Geological Survey Open-File Report 66-53, 82 p. ill., maps (some folded) ;28 cm., https://doi.org/10.3133/ofr6653.","productDescription":"82 p. ill., maps (some folded) ;28 cm.","costCenters":[],"links":[{"id":144733,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1966/0053/report-thumb.jpg"},{"id":42500,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1966/0053/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4c2b","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":168569,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":13399,"text":"ofr6629 - 1966 - Road log for southern Santa Rita Mountains, Santa Cruz and Pima Counties, Arizona","interactions":[],"lastModifiedDate":"2025-06-17T17:01:40.803879","indexId":"ofr6629","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"66-29","title":"Road log for southern Santa Rita Mountains, Santa Cruz and Pima Counties, Arizona","docAbstract":"<p>Geologic mapping of the Mount Wrightson quadrangle has been completed recently by the U.S. Geological Survey. As a result, I am able to present a summary (table 1) of the rocks exposed and to indicate their ages and relations with each other. The Mesozoic rocks are emphasized because the local geologic record of this era is more complete in the southern part of the Santa Rita Mountains than elsewhere in southern Arizona. For example, there is evidence to indicate that about 10,000 feet of volcanics (including pillow lava), eolian sandstone, and possibly even red beds was deposited during Triassic time and that these rocks were intruded by a monzonite stock before the end of that period. It is hoped that release of the data at this time, prior to the final publication by the U.S. Geological Survey, will stimulate in the geological community of southern Arizona a timely interest in some of the complex problems of the Mesozoic tectonic history. Solutions to these problems may suggest new approaches to minerals exploration in this region.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6629","usgsCitation":"Drewes, H., 1966, Road log for southern Santa Rita Mountains, Santa Cruz and Pima Counties, Arizona: U.S. Geological Survey Open-File Report 66-29, 6 p., https://doi.org/10.3133/ofr6629.","productDescription":"6 p.","costCenters":[],"links":[{"id":490872,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1966/0029/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145481,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1966/0029/report-thumb.jpg"}],"country":"United States","state":"Arizona","county":"Pima County, Santa Cruz County","otherGeospatial":"Santa Rita Mountains","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"id\":\"4\",\"properties\":{\"name\":\"Arizona\",\"nation\":\"USA  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,{"id":13999,"text":"ofr68120 - 1966 - Geologic interpretation of infrared imagery of the Pend Oreille area, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:06:51","indexId":"ofr68120","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"68-120","title":"Geologic interpretation of infrared imagery of the Pend Oreille area, Idaho","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr68120","usgsCitation":"Harrison, J.E., 1966, Geologic interpretation of infrared imagery of the Pend Oreille area, Idaho: U.S. Geological Survey Open-File Report 68-120, 10 p. ill., maps ;30 cm., https://doi.org/10.3133/ofr68120.","productDescription":"10 p. ill., maps ;30 cm.","costCenters":[],"links":[{"id":147369,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1968/0120/report-thumb.jpg"},{"id":42651,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1968/0120/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a549e","contributors":{"authors":[{"text":"Harrison, Jack Edward","contributorId":49778,"corporation":false,"usgs":true,"family":"Harrison","given":"Jack","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":168765,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":15024,"text":"ofr6687 - 1966 - Mines and prospects, Idaho Springs district, Clear Creek and Gilpin counties, Colorado -- Descriptions and maps","interactions":[],"lastModifiedDate":"2025-07-24T18:51:09.164983","indexId":"ofr6687","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"66-87","title":"Mines and prospects, Idaho Springs district, Clear Creek and Gilpin counties, Colorado -- Descriptions and maps","docAbstract":"<p>The Idaho Springs mining district forms an important segment of the Front Range mineral belt, a northeast-trending zone of coextensive intrusive rocks and hydrothermal ore deposits of early Tertiary age. This belt, which is about 50 miles long, extends from the region just west of Boulder southwestward across the Front Range. From 1859, when placer gold was discovered in Idaho Springs and lode gold in Central City, through 1959, ores valued at about <span>$</span>200 million were shipped from a 50-square-mile area that includes the Idaho Springs and adjacent districts to the north, west, and southwest. The adjacent Central City district, which produced ores valued at more than <span>\\$</span>100 million, is clearly the most important district in the mineral belt. The Idaho Springs district from 1860 to 1959 produced ores valued at about $65 million, and the districts to the west and southwest produced smaller amounts. Gold has accounted for about 60 percent of the value of the ore, but in some areas silver provides the chief values, and copper, lead, and zinc add value to the ores in most areas. Mining activity in the Idaho Springs and adjacent districts was at its 'heyday' in the late 1800's, it declined sharply after 1914, it was somewhat renewed during the 1930's, and it greatly declined during World War II. In the 1950's uranium prospecting stimulated some mining activity. No uranium was produced, however, and at the close of the decade only one mine--the Bald Eagle--was being worked for its precious- and base-metal ores. In this report, 135 mines and prospects are described. The mines and prospects described are those that were accessible at the time of this study, as well as a few inaccessible properties for which some information was available. Most of the data for the inaccessible or unimportant properties were obtained from Bastin and Hill (1917) and Spurr, Garrey, and Ball (1908). The following list shows, in alphabetical order, the names of about 325 openings of mines and prospects, their coordinate location on the district map (fig. 1), the page of this report on which their description starts, and the number of the illustration, if any, referring to them.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr6687","usgsCitation":"Moench, R.H., and Drake, A., 1966, Mines and prospects, Idaho Springs district, Clear Creek and Gilpin counties, Colorado -- Descriptions and maps: U.S. Geological Survey Open-File Report 66-87, Report: 213 p.; 81 Plates: 40.0 x 62.0 inches or smaller, https://doi.org/10.3133/ofr6687.","productDescription":"Report: 213 p.; 81 Plates: 40.0 x 62.0 inches or smaller","costCenters":[{"id":595,"text":"U.S. Geological 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,{"id":14757,"text":"ofr6678 - 1966 - Instrument installations for the study of coal mine bumps at Sunnyside, Utah","interactions":[],"lastModifiedDate":"2021-01-26T21:00:45.246188","indexId":"ofr6678","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"66-78","title":"Instrument installations for the study of coal mine bumps at Sunnyside, Utah","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr6678","usgsCitation":"Maberry, J.O., 1966, Instrument installations for the study of coal mine bumps at Sunnyside, Utah: U.S. Geological Survey Open-File Report 66-78, 12 p., https://doi.org/10.3133/ofr6678.","productDescription":"12 p.","costCenters":[],"links":[{"id":382646,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1966/0078/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":147706,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1966/0078/report-thumb.jpg"}],"country":"United States","state":"Utah","city":"Sunnyside","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.77617645263672,\n              39.58558227224178\n            ],\n            [\n              -110.69549560546874,\n              39.58558227224178\n            ],\n            [\n              -110.69549560546874,\n              39.62473049524288\n            ],\n            [\n              -110.77617645263672,\n              39.62473049524288\n            ],\n            [\n              -110.77617645263672,\n              39.58558227224178\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4e26","contributors":{"authors":[{"text":"Maberry, John O.","contributorId":87134,"corporation":false,"usgs":true,"family":"Maberry","given":"John","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":169953,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":13753,"text":"ofr66142 - 1966 - Lunar orbiter - image analysis studies report, May 1, 1965 to January 31, 1966","interactions":[],"lastModifiedDate":"2012-02-02T00:06:46","indexId":"ofr66142","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"66-142","title":"Lunar orbiter - image analysis studies report, May 1, 1965 to January 31, 1966","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr66142","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1966, Lunar orbiter - image analysis studies report, May 1, 1965 to January 31, 1966: U.S. Geological Survey Open-File Report 66-142, 148 p. ill., maps ;27 cm., https://doi.org/10.3133/ofr66142.","productDescription":"148 p. ill., maps ;27 cm.","costCenters":[],"links":[{"id":146585,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648a29","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":528950,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15383,"text":"ofr66100 - 1966 - Principal facts for gravity stations in Sulphur Springs Valley, Arizona","interactions":[{"subject":{"id":15383,"text":"ofr66100 - 1966 - Principal facts for gravity stations in Sulphur Springs Valley, Arizona","indexId":"ofr66100","publicationYear":"1966","noYear":false,"title":"Principal facts for gravity stations in Sulphur Springs Valley, Arizona"},"predicate":"SUPERSEDED_BY","object":{"id":70043099,"text":"70043099 - 1972 - Principal facts for gravity stations in Sulphur Springs Valley, Arizona","indexId":"70043099","publicationYear":"1972","noYear":false,"title":"Principal facts for gravity stations in Sulphur Springs Valley, Arizona"},"id":1}],"supersededBy":{"id":70043099,"text":"70043099 - 1972 - Principal facts for gravity stations in Sulphur Springs Valley, Arizona","indexId":"70043099","publicationYear":"1972","noYear":false,"title":"Principal facts for gravity stations in Sulphur Springs Valley, Arizona"},"lastModifiedDate":"2013-02-05T10:43:55","indexId":"ofr66100","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"66-100","title":"Principal facts for gravity stations in Sulphur Springs Valley, Arizona","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr66100","usgsCitation":"Peterson, D.L., 1966, Principal facts for gravity stations in Sulphur Springs Valley, Arizona: U.S. Geological Survey Open-File Report 66-100, 2 p. ;28 x 38 cm., https://doi.org/10.3133/ofr66100.","productDescription":"2 p. ;28 x 38 cm.","costCenters":[],"links":[{"id":147573,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db667f91","contributors":{"authors":[{"text":"Peterson, Donald L.","contributorId":28597,"corporation":false,"usgs":true,"family":"Peterson","given":"Donald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":171045,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14023,"text":"ofr6658 - 1966 - Seismic refraction surveys in the vicinity of Eagle City, Clark County, Ohio","interactions":[],"lastModifiedDate":"2016-11-07T10:16:41","indexId":"ofr6658","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"66-58","title":"Seismic refraction surveys in the vicinity of Eagle City, Clark County, Ohio","docAbstract":"<p>As part of a continuing program to define the thickness and extent of water-bearing sand and gravel deposits in southwestern Ohio, the U.S. Geological Survey, in cooperation with the Ohio Division of Water, in the summer of 1964 completed a seismic refraction survey in the vicinity of Eagle and Tremont Cities, Ohio (fig. 1). Similar surveys were completed in 1962 of the lower Great Miami River and Whitewater River Valleys (Watkins, 1963); in 1963 of the upper Great Miami River Valley (Watkins and Spieker, 1964) and of the Scioto River Valley (Watkins and Bailey, 1964). </p><p>The area of the survey includes known or inferred portions of an interglacial drainage system which is deeply entrenched into bedrock. Ohio was covered by glaciers at least twice during the Pleistocene Epoch. As the last glacier retreated from Clark County, floods of meltwater deposited up to 300 ft of sand and gravel, now forming the lowlands of the Mad River Valley. </p><p>The sand and gravel is highly permeable and saturated with large quantities of water of good quality. The underlying bedrock consists of limestone and dolomite, and limestone interbedded with shale. The limestone and dolomite sequence is the principal source of water along the edges of the buried valley where the sand and gravel thins. The city of Springfield has recently developed wells in the glacial deposits, and many industries in the area rely on wells in these deposits as their principal source of water. The purpose of the present survey is to define the thickness and extent of the important water-bearing sand and gravel deposits. Such information will make possible a more accurate evaluation of the area's water resources than has previously been possible.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6658","usgsCitation":"Hassemer, J.H., Watkins, J.S., and Bailey, N.G., 1966, Seismic refraction surveys in the vicinity of Eagle City, Clark County, Ohio: U.S. Geological Survey Open-File Report 66-58, 7 p., https://doi.org/10.3133/ofr6658.","productDescription":"7 p.","numberOfPages":"11","costCenters":[],"links":[{"id":147209,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":330800,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1966/0058/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Ohio","county":"Clark County","city":"Eagle City","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.86053085327148,\n              39.95185892663005\n            ],\n            [\n              -83.86053085327148,\n              40.016834928010034\n            ],\n            [\n              -83.79632949829102,\n              40.016834928010034\n            ],\n            [\n              -83.79632949829102,\n              39.95185892663005\n            ],\n            [\n              -83.86053085327148,\n              39.95185892663005\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb6b7","contributors":{"authors":[{"text":"Hassemer, Jerry H.","contributorId":8103,"corporation":false,"usgs":true,"family":"Hassemer","given":"Jerry","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":168807,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Watkins, Joel S.","contributorId":10788,"corporation":false,"usgs":true,"family":"Watkins","given":"Joel","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":168808,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bailey, Norman G.","contributorId":59439,"corporation":false,"usgs":true,"family":"Bailey","given":"Norman","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":168809,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":14016,"text":"ofr6657 - 1966 - Geology of the Cupsuptic quadrangle, Maine","interactions":[],"lastModifiedDate":"2012-02-02T00:06:53","indexId":"ofr6657","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"66-57","title":"Geology of the Cupsuptic quadrangle, Maine","docAbstract":"The Cupsuptic quadrangle, in west-central Maine, lies in a relatively narrow belt of pre-Silurian rocks extending from the Connecticut River valley across northern New Hampshire to north-central Maine. The Albee Formation, composed of green, purple, and black phyllite with interbedded-quartzite, is exposed in the core of a regional anticlinorium overlain to the southeast by greenstone of the Oquossoc Formation which in turn is overlain by black slate of the Kamankeag Formation. In the northern part of the quadrangle the Albee Formation is overlain by black slate, feldspathic graywacke, and minor greenstone of the Dixville Formation. The Kamankeag Formation is dated as 1-ate Middle Ordovician by graptolites (zone 12) found near the base of the unit. The Dixville Formation is correlated with the Kamankeag Formation and Oquossoc Formation and is considered to be Middle Ordovician. The Albee Formation is considered to be Middle to Lower Ordovician from correlations with similar rocks in northeastern and southwestern Vermont. The Oquossoc and Kamankeag Formations are correlated with the Amonoosuc and Partridge Formations of northern New Hampshire. \r\n\r\nThe pre-Silurian rocks are unconformably overlain by unnamed rocks of Silurian age in the southeast, west-central, and northwest ninths of the quadrangle. The basal Silurian units are boulder to cobble polymict conglomerate and quartz-pebble conglomerate of late Lower Silurian (Upper Llandovery) age. The overlying rocks are either well-bedded slate and quartzite, silty limestone, or arenaceous limestone. Thearenaceous limestone contains Upper Silurian (Lower Ludlow) brachiopods. \r\n\r\nThe stratified rocks have been intruded by three stocks of biotite-muscovite quartz monzonite, a large body of metadiorite and associated serpentinite, smaller bodies of gabbro, granodiorite, and intrusive felsite, as well as numerous diabase and quartz monzonite dikes. The metadiorite and serpentinite, and possibly the gabbro and granodiorite are Late Ordovician in age. The quartz monzonite is considered to be Late Devonian. \r\n\r\nFive tectonic events are inferred from the structural features in the area. The earliest was a period of folding producing tightly-appressed, northeast-trending folds in the rocks of pre-Silurian age. In the second stage the folded pre-Silurian rocks were uplifted, eroded, and truncated to produce a major unconformity between the Middle Ordovician and Lower Silurian rocks. These events constitute the Taconic orogeny. The third tectonic event was a period of folding, probably of Middle Devonian age, that warped the unconformity and overlying rocks into open, gently-plunging, east-trending folds. This period of folding undoubtedly changed the attitude of the early folds in the pre-Silurian units but it did not produce any recognizable, cross-cutting planar features in the older rocks. The fourth tectonic event was a period of igneous intrusion that locally deformed the northeast-trending folds in the pre-Silurian rocks into a macroscopic drag fold plunging at 80 degrees in a direction S.10?w. A north-trending, subvertical slip cleavage was produced locally during this period of Late Devonian (?) deformation. A period of faulting, possibly of Triassic age, dislocated some of the earlier features. \r\n\r\nThe rocks are in the chlorite zone of regional metamorphism, but have been contact metamorphosed to sillimanite-bearing hornfels adjacent to the quartz monzonite stocks. The chemical changes in chlorite, biotite, garnet, cordierite, and muscovite in the chlorite, biotite, andalusite, and sillimanite zones have been-studied by optical and x-ray methods and by partial chemical analyses. The progressive changes in mineral assemblages have been graphically portrayed on quaternary diagrams and ternary projections.","language":"ENGLISH","publisher":"[s.n.],","doi":"10.3133/ofr6657","usgsCitation":"Harwood, D.S., 1966, Geology of the Cupsuptic quadrangle, Maine: U.S. Geological Survey Open-File Report 66-57, 259 p. ill. (1 col.), maps (2 col.) ;29 cm., https://doi.org/10.3133/ofr6657.","productDescription":"259 p. ill. (1 col.), maps (2 col.) ;29 cm.","costCenters":[],"links":[{"id":147164,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1966/0057/report-thumb.jpg"},{"id":42665,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0057/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42666,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0057/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42667,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0057/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42668,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0057/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42669,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0057/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42670,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0057/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42671,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0057/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42672,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0057/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42673,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0057/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42674,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0057/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42675,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0057/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42676,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1966/0057/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acfe4b07f02db68072f","contributors":{"authors":[{"text":"Harwood, David S.","contributorId":48153,"corporation":false,"usgs":true,"family":"Harwood","given":"David","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":168795,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15635,"text":"ofr66110 - 1966 - Structure contours on top of the Vedder sand, southeastern San Joaquin Valley, California","interactions":[],"lastModifiedDate":"2012-02-02T00:07:02","indexId":"ofr66110","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"66-110","title":"Structure contours on top of the Vedder sand, southeastern San Joaquin Valley, California","docAbstract":"The redder sand (Miocene) is one of the principal oil sands of the southeastern San Joaquin Valley. Oil accumulation in this sand is controlled by structural traps, with stratigraphic traps playing a very minor role. Near the east border of the map area the traps are principally formed by normal strike faults. In the western and southern parts of the map area anticlinal folding is the dominant structural feature controlling the accumulation of oil. Cumulative production from the Vedder sand to January 1, 1965, is approximately 400 million barrels of oil.","language":"ENGLISH","publisher":"[s.n.],","doi":"10.3133/ofr66110","usgsCitation":"Richardson, E.E., 1966, Structure contours on top of the Vedder sand, southeastern San Joaquin Valley, California: U.S. Geological Survey Open-File Report 66-110, 15 p. ill. (2 folded, 1 col.), maps ;29 cm., https://doi.org/10.3133/ofr66110.","productDescription":"15 p. ill. (2 folded, 1 col.), maps ;29 cm.","costCenters":[],"links":[{"id":106368,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8122.htm","linkFileType":{"id":5,"text":"html"},"description":"8122"},{"id":147673,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1966/0110/report-thumb.jpg"},{"id":44597,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0110/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44598,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0110/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44599,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0110/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44600,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1966/0110/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ae4b07f02db69d14d","contributors":{"authors":[{"text":"Richardson, Everett E.","contributorId":14423,"corporation":false,"usgs":true,"family":"Richardson","given":"Everett","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":171472,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71813,"text":"tei866 - 1966 - Geologic map of the Deadhorse Flat quadrangle, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:14:05","indexId":"tei866","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"866","title":"Geologic map of the Deadhorse Flat quadrangle, Nye County, Nevada","language":"ENGLISH","doi":"10.3133/tei866","usgsCitation":"Noble, D.C., Krushensky, R.D., McKay, E.J., and Ege, J.R., 1966, Geologic map of the Deadhorse Flat quadrangle, Nye County, Nevada (See also USGS quad 614): U.S. Geological Survey Trace Elements Investigations 866, 1 map sheet, https://doi.org/10.3133/tei866.","productDescription":"1 map sheet","costCenters":[],"links":[{"id":193006,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/866/report-thumb.jpg"},{"id":91019,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/866/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":91020,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/866/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","edition":"See also USGS quad 614","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6496c1","contributors":{"authors":[{"text":"Noble, Donald C.","contributorId":64676,"corporation":false,"usgs":true,"family":"Noble","given":"Donald","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":284790,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krushensky, Richard D.","contributorId":106994,"corporation":false,"usgs":true,"family":"Krushensky","given":"Richard","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":284792,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McKay, E. J.","contributorId":57040,"corporation":false,"usgs":true,"family":"McKay","given":"E.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":284789,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ege, John R.","contributorId":69534,"corporation":false,"usgs":true,"family":"Ege","given":"John","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":284791,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
]}