{"pageNumber":"6614","pageRowStart":"165325","pageSize":"25","recordCount":184904,"records":[{"id":63090,"text":"gq500 - 1966 - Geologic map of the Ketchen quadrangle, Tennessee-Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:39","indexId":"gq500","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"500","title":"Geologic map of the Ketchen quadrangle, Tennessee-Kentucky","language":"ENGLISH","doi":"10.3133/gq500","usgsCitation":"Englund, K.J., 1966, Geologic map of the Ketchen quadrangle, Tennessee-Kentucky: U.S. Geological Survey Geologic Quadrangle 500, 1 map :col. ;83 x 103 cm., https://doi.org/10.3133/gq500.","productDescription":"1 map :col. ;83 x 103 cm.","costCenters":[],"links":[{"id":102522,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_971.htm","linkFileType":{"id":5,"text":"html"},"description":"971"},{"id":249216,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0500/report.pdf","size":"35","linkFileType":{"id":1,"text":"pdf"}},{"id":252381,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0500/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.36749999999999,36.5 ], [ -84.36749999999999,36.6175 ], [ -84.25,36.6175 ], [ -84.25,36.5 ], [ -84.36749999999999,36.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697538","contributors":{"authors":[{"text":"Englund, Kenneth John","contributorId":59023,"corporation":false,"usgs":true,"family":"Englund","given":"Kenneth","email":"","middleInitial":"John","affiliations":[],"preferred":false,"id":268313,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4416,"text":"cir525 - 1966 - Tectonic creep in the Hayward fault zone, California","interactions":[],"lastModifiedDate":"2017-08-27T17:57:33","indexId":"cir525","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"525","title":"Tectonic creep in the Hayward fault zone, California","docAbstract":"Tectonic creep is slight apparently continuous movement along a fault. Evidence of creep has been noted at several places within the Hayward fault zone--a zone trending northwestward near the western front of the hills bordering the east side of San Francisco Bay. \r\n\r\nD. H. Radbruch of the Geological Survey and B. J. Lennert, consulting engineer, confirmed a reported cracking of a culvert under the University of California stadium. \r\n\r\nF. B. Blanchard and C. L. Laverty of the East Bay Municipal Utility District of Oakland studied cracks in the Claremont water tunnel in Berkeley. \r\n\r\nM. G. Bonilla of the Geological Survey noted deformation of railroad tracks in the Niles district of Fremont. Six sets of tracks have been bent and shifted. \r\n\r\nL. S. Cluff of Woodward-Clyde-Sherard and Associates and K. V. Steinbrugge of the Pacific Fire Rating Bureau noted that the concrete walls of a warehouse in the Irvington district of Fremont have been bent and broken, and the columns forced out of line. \r\n\r\nAll the deformations noted have been right lateral and range from about 2 inches in the Claremont tunnel to about 8 inches on the railroad tracks. Tectonic creep almost certainly will continue to damage buildings, tunnels, and other structures that cross the narrow bands of active movement within the Hayward fault zone.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir525","usgsCitation":"Radbruch-Hall, D.H., and Bonilla, M.G., 1966, Tectonic creep in the Hayward fault zone, California: U.S. Geological Survey Circular 525, vi, 13 p. :illus., maps. ;27 cm., https://doi.org/10.3133/cir525.","productDescription":"vi, 13 p. :illus., maps. ;27 cm.","costCenters":[],"links":[{"id":31521,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1966/0525/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":126727,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1966/0525/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db68596e","contributors":{"authors":[{"text":"Radbruch-Hall, Dorothy H.","contributorId":102462,"corporation":false,"usgs":true,"family":"Radbruch-Hall","given":"Dorothy","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":149086,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bonilla, M. G.","contributorId":33698,"corporation":false,"usgs":true,"family":"Bonilla","given":"M.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":149085,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":62802,"text":"gq474 - 1966 - Surficial geologic map of the Greenfield quadrangle, Franklin County, Massachusetts","interactions":[],"lastModifiedDate":"2012-02-10T00:10:48","indexId":"gq474","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"474","title":"Surficial geologic map of the Greenfield quadrangle, Franklin County, Massachusetts","language":"ENGLISH","doi":"10.3133/gq474","usgsCitation":"Jahns, R.H., 1966, Surficial geologic map of the Greenfield quadrangle, Franklin County, Massachusetts: U.S. Geological Survey Geologic Quadrangle 474, 1 map :col. ;on sheet 73 x 87 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/gq474.","productDescription":"1 map :col. ;on sheet 73 x 87 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":102494,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_943.htm","linkFileType":{"id":5,"text":"html"},"description":"943"},{"id":248954,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0474/report.pdf","size":"410","linkFileType":{"id":1,"text":"pdf"}},{"id":251627,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0474/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -72.61749999999999,42.5 ], [ -72.61749999999999,42.6175 ], [ -72.5,42.6175 ], [ -72.5,42.5 ], [ -72.61749999999999,42.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db688f7d","contributors":{"authors":[{"text":"Jahns, Richard Henry","contributorId":45291,"corporation":false,"usgs":true,"family":"Jahns","given":"Richard","email":"","middleInitial":"Henry","affiliations":[],"preferred":false,"id":267876,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":62805,"text":"gq543 - 1966 - Geologic map of the Milo quadrangle, Kentucky-West Virginia, and the part of the Webb quadrangle in Kentucky","interactions":[],"lastModifiedDate":"2022-11-01T19:05:38.290453","indexId":"gq543","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"543","title":"Geologic map of the Milo quadrangle, Kentucky-West Virginia, and the part of the Webb quadrangle in Kentucky","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gq543","usgsCitation":"Jenkins, E.C., 1966, Geologic map of the Milo quadrangle, Kentucky-West Virginia, and the part of the Webb quadrangle in Kentucky: U.S. Geological Survey Geologic Quadrangle 543, Report: 1 p.; 1 Plate: 46.83 x 33.35 inches, https://doi.org/10.3133/gq543.","productDescription":"Report: 1 p.; 1 Plate: 46.83 x 33.35 inches","costCenters":[],"links":[{"id":103271,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1857.htm","linkFileType":{"id":5,"text":"html"},"description":"1857"},{"id":248956,"rank":301,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0543/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":251629,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0543/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Kentucky, West Virginia","otherGeospatial":"Milo quadrangle, Webb quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.625,\n              37.875\n            ],\n            [\n              -82.625,\n              38\n            ],\n            [\n              -82.4167,\n              38\n            ],\n            [\n              -82.4167,\n              37.875\n            ],\n            [\n              -82.625,\n              37.875\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6969a6","contributors":{"authors":[{"text":"Jenkins, Evan Cramer","contributorId":49460,"corporation":false,"usgs":true,"family":"Jenkins","given":"Evan","email":"","middleInitial":"Cramer","affiliations":[],"preferred":false,"id":267879,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":62933,"text":"gq470 - 1966 - Geologic map of the Valley View quadrangle, central Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:11:01","indexId":"gq470","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"470","title":"Geologic map of the Valley View quadrangle, central Kentucky","language":"ENGLISH","doi":"10.3133/gq470","usgsCitation":"Greene, R.C., 1966, Geologic map of the Valley View quadrangle, central Kentucky: U.S. Geological Survey Geologic Quadrangle 470, 1 map., https://doi.org/10.3133/gq470.","productDescription":"1 map.","costCenters":[],"links":[{"id":102490,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_939.htm","linkFileType":{"id":5,"text":"html"},"description":"939"},{"id":249073,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0470/report.pdf","size":"35","linkFileType":{"id":1,"text":"pdf"}},{"id":251910,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0470/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.5,37.75 ], [ -84.5,37.8675 ], [ -84.36749999999999,37.8675 ], [ -84.36749999999999,37.75 ], [ -84.5,37.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a226","contributors":{"authors":[{"text":"Greene, Robert C.","contributorId":36108,"corporation":false,"usgs":true,"family":"Greene","given":"Robert","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":268072,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42053,"text":"ofr6686 - 1966 - Aeromagnetic map of Hayden Peak and vicinity, Uinta Mountains, Utah","interactions":[],"lastModifiedDate":"2025-07-24T18:42:55.622271","indexId":"ofr6686","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":"66-86","title":"Aeromagnetic map of Hayden Peak and vicinity, Uinta Mountains, Utah","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6686","usgsCitation":"Meuschke, J.L., and Kirby, J., 1966, Aeromagnetic map of Hayden Peak and vicinity, Uinta Mountains, Utah: U.S. Geological Survey Open-File Report 66-86, 1 Plate: 47.95 x 28.09 inches, https://doi.org/10.3133/ofr6686.","productDescription":"1 Plate: 47.95 x 28.09 inches","costCenters":[],"links":[{"id":492845,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8141.htm","linkFileType":{"id":5,"text":"html"}},{"id":79801,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0086/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":136765,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"25000","country":"United States","state":"Utah","otherGeospatial":"Hayden Peak and vicinity, Uinta Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -111.625,\n              41\n            ],\n            [\n              -111.625,\n              40.333\n            ],\n            [\n              -110.262,\n              40.333\n            ],\n            [\n              -110.262,\n              41\n            ],\n            [\n              -111.625,\n              41\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db698272","contributors":{"authors":[{"text":"Meuschke, J. L.","contributorId":53349,"corporation":false,"usgs":true,"family":"Meuschke","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":225881,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kirby, J.R.","contributorId":6428,"corporation":false,"usgs":true,"family":"Kirby","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":225880,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"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":63758,"text":"gp581 - 1966 - Aeromagnetic map of the Mount Pleasant, Albemarle, Denton, and Salisbury quadrangles, west-central North Carolina","interactions":[],"lastModifiedDate":"2012-02-10T00:11:00","indexId":"gp581","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"581","title":"Aeromagnetic map of the Mount Pleasant, Albemarle, Denton, and Salisbury quadrangles, west-central North Carolina","language":"ENGLISH","doi":"10.3133/gp581","usgsCitation":"Henderson, J.R., and Gilbert, F.P., 1966, Aeromagnetic map of the Mount Pleasant, Albemarle, Denton, and Salisbury quadrangles, west-central North Carolina: U.S. Geological Survey Geophysical Investigations Map 581, 1 map., https://doi.org/10.3133/gp581.","productDescription":"1 map.","costCenters":[],"links":[{"id":104157,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3539.htm","linkFileType":{"id":5,"text":"html"},"description":"3539"},{"id":186890,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -80.5,35.25 ], [ -80.5,35.75 ], [ -80,35.75 ], [ -80,35.25 ], [ -80.5,35.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691d41","contributors":{"authors":[{"text":"Henderson, J. R.","contributorId":78705,"corporation":false,"usgs":true,"family":"Henderson","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":269527,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gilbert, F. P.","contributorId":53033,"corporation":false,"usgs":true,"family":"Gilbert","given":"F.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":269526,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":63755,"text":"gp562 - 1966 - Aeromagnetic map of northern New Jersey and adjacent parts of New York and Pennsylvania","interactions":[],"lastModifiedDate":"2025-05-06T16:06:53.651777","indexId":"gp562","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"562","title":"Aeromagnetic map of northern New Jersey and adjacent parts of New York and Pennsylvania","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp562","usgsCitation":"Henderson, J.R., Andreasen, G.E., and Petty, A.J., 1966, Aeromagnetic map of northern New Jersey and adjacent parts of New York and Pennsylvania: U.S. Geological Survey Geophysical Investigations Map 562, 1 Plate: 39.72 x 46.40 inches, https://doi.org/10.3133/gp562.","productDescription":"1 Plate: 39.72 x 46.40 inches","costCenters":[],"links":[{"id":253454,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0562/report-thumb.jpg"},{"id":249934,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0562/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":249933,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0562/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":485460,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3518.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"25000","country":"United States","state":"New Jersey, New York, Pennsylvania","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -75.25,\n              41.5\n            ],\n            [\n              -75.25,\n              40.25\n            ],\n            [\n              -73.8333,\n              40.25\n            ],\n            [\n              -73.8333,\n              41.5\n            ],\n            [\n              -75.25,\n              41.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697d0a","contributors":{"authors":[{"text":"Henderson, J. R.","contributorId":78705,"corporation":false,"usgs":true,"family":"Henderson","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":269520,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andreasen, G. E.","contributorId":105315,"corporation":false,"usgs":true,"family":"Andreasen","given":"G.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":269521,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Petty, A. J.","contributorId":35384,"corporation":false,"usgs":true,"family":"Petty","given":"A.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":269519,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":63756,"text":"gp561 - 1966 - Aeromagnetic map of parts of the Mother Lode gold and Sierra Foothills copper mining districts, California, and its geologic interpretation","interactions":[{"subject":{"id":51288,"text":"ofr53116 - 1953 - Preliminary total intensity aeromagnetic maps of the Mother Lode district, California","indexId":"ofr53116","publicationYear":"1953","noYear":false,"title":"Preliminary total intensity aeromagnetic maps of the Mother Lode district, California"},"predicate":"SUPERSEDED_BY","object":{"id":63756,"text":"gp561 - 1966 - Aeromagnetic map of parts of the Mother Lode gold and Sierra Foothills copper mining districts, California, and its geologic interpretation","indexId":"gp561","publicationYear":"1966","noYear":false,"title":"Aeromagnetic map of parts of the Mother Lode gold and Sierra Foothills copper mining districts, California, and its geologic interpretation"},"id":1}],"lastModifiedDate":"2012-02-10T00:11:00","indexId":"gp561","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"561","title":"Aeromagnetic map of parts of the Mother Lode gold and Sierra Foothills copper mining districts, California, and its geologic interpretation","language":"ENGLISH","doi":"10.3133/gp561","usgsCitation":"Henderson, J.R., Stromquist, A.A., and Jespersen, A., 1966, Aeromagnetic map of parts of the Mother Lode gold and Sierra Foothills copper mining districts, California, and its geologic interpretation: U.S. Geological Survey Geophysical Investigations Map 561, 1 map., https://doi.org/10.3133/gp561.","productDescription":"1 map.","costCenters":[],"links":[{"id":249935,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0561/report.pdf","size":"336","linkFileType":{"id":1,"text":"pdf"}},{"id":249936,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0561/plate-1.pdf","size":"11304","linkFileType":{"id":1,"text":"pdf"}},{"id":253455,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0561/report-thumb.jpg"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.86749999999999,37.8675 ], [ -120.86749999999999,38.166666666666664 ], [ -120,38.166666666666664 ], [ -120,37.8675 ], [ -120.86749999999999,37.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69763d","contributors":{"authors":[{"text":"Henderson, J. R. Jr.","contributorId":88802,"corporation":false,"usgs":true,"family":"Henderson","given":"J.","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":269524,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stromquist, A. A.","contributorId":6025,"corporation":false,"usgs":true,"family":"Stromquist","given":"A.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":269522,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jespersen, Anna","contributorId":71264,"corporation":false,"usgs":true,"family":"Jespersen","given":"Anna","email":"","affiliations":[],"preferred":false,"id":269523,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":58091,"text":"wdrWI6512 - 1966 - Water resources data for Wisconsin, 1965; Part 1. Surface water records and Part 2. Water quality records","interactions":[],"lastModifiedDate":"2012-02-02T00:12:32","indexId":"wdrWI6512","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"WI-65-1-2","title":"Water resources data for Wisconsin, 1965; Part 1. Surface water records and Part 2. Water quality records","language":"ENGLISH","doi":"10.3133/wdrWI6512","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1966, Water resources data for Wisconsin, 1965; Part 1. Surface water records and Part 2. Water quality records: U.S. Geological Survey Water Data Report WI-65-1-2, 223 p., https://doi.org/10.3133/wdrWI6512.","productDescription":"223 p.","numberOfPages":"223","costCenters":[],"links":[{"id":182567,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1965/wi-65-1-2/report-thumb.jpg"},{"id":88320,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1965/wi-65-1-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f16db","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":533204,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":62118,"text":"gq541 - 1966 - Geologic map of the Monument quadrangle, Grant County, Oregon","interactions":[],"lastModifiedDate":"2012-02-10T00:10:29","indexId":"gq541","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"541","title":"Geologic map of the Monument quadrangle, Grant County, Oregon","language":"ENGLISH","doi":"10.3133/gq541","usgsCitation":"Wilcox, R.E., and Fisher, R.V., 1966, Geologic map of the Monument quadrangle, Grant County, Oregon: U.S. Geological Survey Geologic Quadrangle 541, 1 map., https://doi.org/10.3133/gq541.","productDescription":"1 map.","costCenters":[],"links":[{"id":103270,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1856.htm","linkFileType":{"id":5,"text":"html"},"description":"1856"},{"id":248313,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0541/report.pdf","size":"33","linkFileType":{"id":1,"text":"pdf"}},{"id":253207,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0541/report-thumb.jpg"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -119.5,44.75 ], [ -119.5,45 ], [ -119.25,45 ], [ -119.25,44.75 ], [ -119.5,44.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6967f3","contributors":{"authors":[{"text":"Wilcox, Ray E.","contributorId":63074,"corporation":false,"usgs":true,"family":"Wilcox","given":"Ray","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":266938,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fisher, Richard V.","contributorId":106946,"corporation":false,"usgs":true,"family":"Fisher","given":"Richard","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":266939,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":57735,"text":"ofr66146 - 1966 - Surface- and ground-water conditions during 1959-61 in a part of the Flett Creek basin, Tacoma, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:12:13","indexId":"ofr66146","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":"66-146","title":"Surface- and ground-water conditions during 1959-61 in a part of the Flett Creek basin, Tacoma, Washington","language":"ENGLISH","doi":"10.3133/ofr66146","usgsCitation":"Veatch, F.M., Kimmel, G.E., and Johnston, E.A., 1966, Surface- and ground-water conditions during 1959-61 in a part of the Flett Creek basin, Tacoma, Washington: U.S. Geological Survey Open-File Report 66-146, 42 p. : ill., maps ; 27 cm., https://doi.org/10.3133/ofr66146.","productDescription":"42 p. : ill., maps ; 27 cm.","costCenters":[],"links":[{"id":184548,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af3e4b07f02db691a52","contributors":{"authors":[{"text":"Veatch, Fred M.","contributorId":46517,"corporation":false,"usgs":true,"family":"Veatch","given":"Fred","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":257666,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kimmel, Grant E.","contributorId":20741,"corporation":false,"usgs":true,"family":"Kimmel","given":"Grant","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":257665,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Johnston, Earle A.","contributorId":98807,"corporation":false,"usgs":true,"family":"Johnston","given":"Earle","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":257667,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":33530,"text":"b1203C - 1966 - Preparation of thermistor cables used in geothermal investigations","interactions":[],"lastModifiedDate":"2012-02-02T00:09:42","indexId":"b1203C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1203","chapter":"C","title":"Preparation of thermistor cables used in geothermal investigations","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/b1203C","usgsCitation":"Raspet, R., Swartz, J., Lillard, M., and Robertson, E., 1966, Preparation of thermistor cables used in geothermal investigations: U.S. Geological Survey Bulletin 1203, p. C1-C11, ill. ;24 cm., https://doi.org/10.3133/b1203C.","productDescription":"p. C1-C11, ill. ;24 cm.","costCenters":[],"links":[{"id":167210,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1203b-c/report-thumb.jpg"},{"id":91276,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1203b-c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db6691ac","contributors":{"authors":[{"text":"Raspet, Rudolph","contributorId":12095,"corporation":false,"usgs":true,"family":"Raspet","given":"Rudolph","email":"","affiliations":[],"preferred":false,"id":211464,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swartz, J.H.","contributorId":101721,"corporation":false,"usgs":true,"family":"Swartz","given":"J.H.","email":"","affiliations":[],"preferred":false,"id":211467,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lillard, M.E.","contributorId":20385,"corporation":false,"usgs":true,"family":"Lillard","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":211465,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Robertson, E.C.","contributorId":43365,"corporation":false,"usgs":true,"family":"Robertson","given":"E.C.","email":"","affiliations":[],"preferred":false,"id":211466,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":2018,"text":"wsp1586G - 1966 - Fresh-water discharge salinity relations in the tidal Delaware River","interactions":[],"lastModifiedDate":"2017-06-26T08:24:55","indexId":"wsp1586G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1586","chapter":"G","title":"Fresh-water discharge salinity relations in the tidal Delaware River","docAbstract":"Sustained flows of fresh water greater than 3,500, 4,400, and 5,300 cubic feet per second into the Delaware River estuary at Trenton, NJ assure low salinity at League Island, Eddystone, and Marcus Hook, respectively. When the discharge at Trenton is less than these critical values, salinity is very sensitive to change in discharge, so that a relatively small decrease in fresh-water discharge results in a relatively great increase in salinity. Comparison of the discharge-salinity relations observed for the 14-year period August 1949-December 1963 with relations proposed by other workers but based on other time periods indicate that such relations change with time and that salinity is affected not only by discharge but also by dredging; construction of breakwater, dikes, and tidal barriers; changing sea level; tidal elevation; tidal range; and wind intensity and direction.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp1586G","usgsCitation":"Keighton, W.B., 1966, Fresh-water discharge salinity relations in the tidal Delaware River: U.S. Geological Survey Water Supply Paper 1586, 16 p. ;28 cm., https://doi.org/10.3133/wsp1586G.","productDescription":"16 p. ;28 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":27485,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1586g/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137597,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1586g/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a49c4","contributors":{"authors":[{"text":"Keighton, Walter B.","contributorId":81877,"corporation":false,"usgs":true,"family":"Keighton","given":"Walter","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":144536,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32576,"text":"pp560D - 1966 - Geology of the Arabian Peninsula: Sedimentary geology of Saudi Arabia","interactions":[],"lastModifiedDate":"2022-02-15T19:58:22.404539","indexId":"pp560D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"560","chapter":"D","title":"Geology of the Arabian Peninsula: Sedimentary geology of Saudi Arabia","docAbstract":"<p>Systematic mapping of the sedimentary geology of Saudi Arabia by Arabian-American Oil Co. (Aramco) began in 1933. By 1959, exploration parties of one type or another had surveyed more than 1,300,000 square kilometers (500,000 square miles) of sedimentary outcrop.</p><p>The foundation for sedimentary deposition is the Arabian Shield a vast Precambrian complex of igneous and metamorphic rocks that occupies roughly one-third of the Arabian Peninsula in the west and crops out sporadically along the southern coast. Since the outset of the Paleozoic Era the shield has been amazingly stable, subject only to gentle, epeirogenic movement. On this rigid land mass was deposited an aggregate total of nearly 5,500 meters (18,000 feet) of sedimentary rocks ranging in age from presumed Cambrian to Pliocene(?).</p><p>Paleozoic, Mesozoic, and lower Tertiary strata are magnificently exposed in central Arabia where they crop out in a great curved belt bordering the shield. Here the landscape is dominated by a series of essentially parallel west-facing escarpments, each supported by a resistant limestone cap. Exposures are unusually good, and many rock units can be traced without significant interruption for 500 to nearly 1,000 km. Beds reflecting buried basement configuration dip gently and uniformly away from the escarpment region into the Persian Gulf and Rub' al Khali basins.</p><p>East of the escarpment belt is a broad expanse of relatively low-relief terrain in which Tertiary and younger deposits effectively mask older units. Clues to the character of pre-Tertiary rocks in this large area, which includes the Rub' al Khali desert and most of northeastern Arabia, are afforded only by widely scattered bore holes and oil wells.</p><p>In extreme northwestern Arabia, largely lower Paleozoic sedimentary rocks are exposed, although a basinal area bordering the Paleozoic rocks on the north is characterized by thick Upper Cretaceous to Tertiary strata. Tertiary to Recent volcanic rocks cover substantial parts of the area.</p><p>In general the older sedimentary rocks are exposed in north-central and northwestern Arabia near the Precambrian basement where as much as 2,000 m of lower Paleozoic rocks are present. Although unfossiliferous, the lower 600 m can be equated, at least in part, to rocks of certain Cambrian age in Jordan. Higher beds contain intervals confidently dated as Lower Ordovician, Silurian, and Lower Devonian. Lower Paleozoic rocks are chiefly coarse-grained sandstone of terrestrial origin, although marine shale occurs at several levels and the upper 300 m is mainly shale with thin beds of limestone.</p><p>Lower Paleozoic strata are succeeded in the central escarpment region by a thick sequence (about 1,000 m) of Upper Permian and Triassic sedimentary rocks. The initial deposit, the Khuff Formation, is mostly shallow-water limestone; overlying beds are nonmarine elastics except for thick carbonate units in the middle part of the section.</p><p>Above the Triassic System is some 200 to 500 m of Lower and Middle Jurassic rocks which, near the middle of the escarpment region, are interbedded marine shale and shelf limestone. These grade to sandstone, in part continental, in the northern and southern areas of outcrop. The Middle Jurassic is overlain by a great sequence-of nearly pure carbonate rocks, highly fossiliferous and accurately dated as Upper Jurassic and early Lower Cretaceous.</p><p>The Jurassic System is spectacularly displayed in central Arabia where it forms the backbone of the escarpment region the Tuwayq Mountains. Carbonate sedimentation was interrupted several times in the closing stages of the Jurassic b^ the onset of evaporite conditions which gave rise to cyclic deposits of anhydrite and calcarenite. The resulting sequence the Arab Formation is of prime importance for its porous carbonate members contain billions of barrels of proved oil reserves</p><p>The carbonate sequence is succeeded by a thick body of late Lower and Middle Cretaceous sandstone. (The Middle Cretaceous Series and Epoch, as defined by European geologist-, are used in this report.) Late Lower Cretaceous rocks are nonmarine and appear only in the middle and southern parts of the escarpment region. Middle Cretaceous rocks, nonmarine in the south, become progressively more marine in the north where they follow a transgressive path northwest across older beds as far as Jordan.</p><p>Upper Cretaceous and Eocene rocks, almost exclusively in limestone and dolomite facies, are extensively exposed alorc the eastern edge of the escarpment belt and continue northwest into Iraq. The sequence, with an average thickness of about 5^0 m, includes rocks of Upper Cretaceous, Paleocene, lower Eocene, and middle Eocene ages.</p><p>The stratigraphic sequence above the Eocene consists of 200 to 600 m of Miocene and Pliocene rocks, mostly of nonmarine origin. These deposits a heterogeneous assemblage of marly sandstone, sandy marl, and sandy limestone blanket the Rub' al Khali and northeastern Arabia.</p><p>Above the Miocene and Pliocene rocks are unconsolidated Quaternary deposits which comprise great sand deserts and widespread gravel sheets. Sand of the Rub' al Khali Desert alone covers about 600,000 sq km (230,000 sq mi) or most of southern Arabia.</p><p>Two major structural provinces are recognized within the Arabian Peninsula and adjacent areas. One is the comparatively stable interior region whose rigidity is controlled by the Precambrian basement. The other is the great mobile belt of Taurus, Zagros, and Oman Mountains, bordering the stable region on the north and east. Saudi Arabia falls entirely within the stable region.</p><p>The interior stable region contains the Arabian shield as well as the Arabian Shelf an extension of the basement thinly veneered with little-disturbed sedimentary rocks. Widespread structural events, presumably related to epeirogenic movement within the basement, have divided the Arabian Shelf into several distinct and significant structural elements the Interior Homocline, the Interior Platform, and several basinal areas.</p><p>Bordering the shield is a great belt of sedimentary rocks whose dip basinward is so slight and uniform as to be impreceptible to the eye. This Interior Homocline has an average width of about 400 km and a persistent dip varying from slightly more than 1°00' in older units to less than 0°30' in the youngest. One structural feature of the homocline the central Arabian arch has greatly influenced the present surface distribution of sedimentary rocks in the interior escarpment region. The arch, which affects all rocks from the basement up, marks the area of maximum curvature of the homocline in central Arabia. Although the arch has a varied history, it is apparently a residual high between the periodically sinking Persian Gulf and Rub' al Khali basins rather than a true independent positive feature. Support for this concept conies from the presence of a great arc of tensional structures the central Arabian graben and trough system near the crest of the arch and along the hinge line between the Persian Gulf basin and the stable western block.</p><p>Bordering the homocline is the Interior Platform, a remarkably flat area of varying width in which systematic dip off the crystalline core no longer prevails. Superimposed on the platform are several major north-south anticlinal trends which include the great oil fields of Arabia</p><p>Adjacent to the platform are several basinal areas that have from time to time received thick sedimentary deposits. Such basinal sags have developed on the shelf in the northeastern Rub' al Khali, northern Persian Gulf, Dibdibah and Sirhan-Turayf areas.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp560D","usgsCitation":"Powers, R., Ramirez, L.F., Redmond, C., and Elberg, E., 1966, Geology of the Arabian Peninsula: Sedimentary geology of Saudi Arabia: U.S. Geological Survey Professional Paper 560, p. D1-D147; 10 Plates: 44.20 x 21.43 inches or smaller, https://doi.org/10.3133/pp560D.","productDescription":"p. 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,{"id":67261,"text":"i485 - 1966 - Geologic map of the Pitatus region of the moon","interactions":[],"lastModifiedDate":"2016-12-28T12:56:46","indexId":"i485","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"485","subseriesTitle":"MOON","title":"Geologic map of the Pitatus region of the moon","language":"ENGLISH","doi":"10.3133/i485","usgsCitation":"Trask, N., and Titley, S.R., 1966, Geologic map of the Pitatus region of the moon: U.S. Geological Survey IMAP 485, 1 map., https://doi.org/10.3133/i485.","productDescription":"1 map.","costCenters":[],"links":[{"id":439094,"rank":401,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P14RZWG3","text":"USGS data release","linkHelpText":"Interactive Map: IMAP 485 - Geologic map of the Pitatus region of the moon"},{"id":439093,"rank":401,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9TUQEPP","text":"USGS data release","linkHelpText":" Geologic map of the Pitatus region of the moon"},{"id":115210,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0485/report.pdf","size":"46","linkFileType":{"id":1,"text":"pdf"}},{"id":115211,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0485/plate-1.pdf","size":"8742","linkFileType":{"id":1,"text":"pdf"}},{"id":188930,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0485/report-thumb.jpg"}],"scale":"1000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aefe4b07f02db69164c","contributors":{"authors":[{"text":"Trask, N.J.","contributorId":31729,"corporation":false,"usgs":true,"family":"Trask","given":"N.J.","email":"","affiliations":[],"preferred":false,"id":275868,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Titley, Spencer Rowe","contributorId":51151,"corporation":false,"usgs":true,"family":"Titley","given":"Spencer","email":"","middleInitial":"Rowe","affiliations":[],"preferred":false,"id":275869,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":52525,"text":"ofr667 - 1966 - A progress report on the test-well drilling program in the west part of Antelope Valley, California","interactions":[],"lastModifiedDate":"2018-01-04T11:37:27","indexId":"ofr667","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":"66-7","title":"A progress report on the test-well drilling program in the west part of Antelope Valley, California","docAbstract":"<p>This progress report presents the results of a test-well drilling program undertaken by the Antelope Valley-East Kern Water Agency and the U.S. Geological Survey in the western part of Antelope Valley, Calif. </p><p>Eight test wells were drilled by the rotary method, and electric and lithologic logs were made of each well. </p><p>A water-level-contour map was drawn, based on water-level measurements in the test wells and other wells. On the basis of data from these wells, the Neenach and Randsburg-Mojave faults were located. The concealed trace of another fault, north of the Randsburg-Mojave fault, was postulated from water-level data. </p><p>This progress report considers the feasibility of utilizing a part of the Antelope Valley ground-water basin as a natural water-storage reservoir. The West Antelope ground-water subunit could probably be used as a large-volume holdover storage reservoir. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr667","collaboration":"Prepared in cooperation with the Antelope Valley-East Kern Water Agency","usgsCitation":"Bloyd, R., 1966, A progress report on the test-well drilling program in the west part of Antelope Valley, California: U.S. Geological Survey Open-File Report 66-7, Report: 20 p.; 1 Plate: 44.12 x 34.54 inches, https://doi.org/10.3133/ofr667.","productDescription":"Report: 20 p.; 1 Plate: 44.12 x 34.54 inches","costCenters":[],"links":[{"id":177834,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1966/0007/report-thumb.jpg"},{"id":86946,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0007/plate-1.pdf","text":"Figure 2","linkFileType":{"id":1,"text":"pdf"}},{"id":350296,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1966/0007/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Antelope Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.8,\n              34.6\n            ],\n            [\n              -118.2,\n              34.6\n            ],\n            [\n              -118.2,\n              35\n            ],\n            [\n              -118.8,\n              35\n            ],\n            [\n              -118.8,\n              34.6\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8d02","contributors":{"authors":[{"text":"Bloyd, R. M. Jr.","contributorId":73243,"corporation":false,"usgs":true,"family":"Bloyd","given":"R. M.","suffix":"Jr.","affiliations":[],"preferred":false,"id":245496,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":63661,"text":"gp580 - 1966 - Simple Bouguer gravity map of Maine","interactions":[],"lastModifiedDate":"2025-05-06T16:55:42.229511","indexId":"gp580","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"580","title":"Simple Bouguer gravity map of Maine","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp580","usgsCitation":"Kane, M.F., and Bromery, R.W., 1966, Simple Bouguer gravity map of Maine: U.S. Geological Survey Geophysical Investigations Map 580, 1  Plate: 28.87 x 44.22 inches, https://doi.org/10.3133/gp580.","productDescription":"1  Plate: 28.87 x 44.22 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F.","contributorId":45708,"corporation":false,"usgs":true,"family":"Kane","given":"M.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":269329,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bromery, R. W.","contributorId":11676,"corporation":false,"usgs":true,"family":"Bromery","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":269328,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":19552,"text":"ofr6668 - 1966 - Glacier observations, Glacier National Park, Montana, 1965","interactions":[],"lastModifiedDate":"2012-02-02T00:07:37","indexId":"ofr6668","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":"66-68","title":"Glacier observations, Glacier National Park, Montana, 1965","language":"ENGLISH","publisher":"U.S. Geological Survey and U.S. National Park Service,","doi":"10.3133/ofr6668","usgsCitation":"Johnson, A., 1966, Glacier observations, Glacier National Park, Montana, 1965: U.S. Geological Survey Open-File Report 66-68, 1 v. (various pagings) :ill., maps ;28 cm., https://doi.org/10.3133/ofr6668.","productDescription":"1 v. (various pagings) :ill., maps ;28 cm.","costCenters":[],"links":[{"id":152370,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1966/0068/report-thumb.jpg"},{"id":49019,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0068/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49020,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0068/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49021,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0068/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49022,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1966/0068/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac0e4b07f02db676d66","contributors":{"authors":[{"text":"Johnson, Arthur","contributorId":76720,"corporation":false,"usgs":true,"family":"Johnson","given":"Arthur","affiliations":[],"preferred":false,"id":181107,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2033,"text":"wsp1819E - 1966 - Salinity of the ground water in western Pinal County, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:05:19","indexId":"wsp1819E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1819","chapter":"E","title":"Salinity of the ground water in western Pinal County, Arizona","docAbstract":"The chemical quality of the ground water in western Pinal County is nonuniform areally and stratigraphically. The main areas of highly mineralized water are near Casa Grande and near Coolidge. Striking differences have been noted in the quality of water from different depths in the same well. Water from one well, (D-6-7) 25cdd, showed an increase in chloride content from 248 ppm (parts per million) at 350 feet below the land surface to 6,580 ppm at 375 feet; the concentration of chloride increased to 10,400 ppm at 550 feet below the land surface. This change was accompanied by an increase in the total dissolved solids as indicated by conductivity measurements. The change in water quality can be correlated with sediment types. The upper and lower sand and gravel units seem to yield water of better quality than the intermediate silt and clay unit. In places the silt and clay unit contains zones of gypsum and common table salt. These zones yield water that contains large amounts of the dissolved minerals usually associated with water from playa deposits. \r\n\r\nHighly mineralized ground water in an area near Casa Grande has moved southward and westward as much as 4 miles. Similar water near Coolidge has moved a lesser distance. \r\n\r\nGood management practices and proper use of soil amendments have made possible the use of water that is high in salinity and alkali hazard for agricultural purposes in western Pinal County. \r\n\r\nThe fluoride content of the ground water in western Pinal County is usually low; however, water from wells that penetrate either the bedrock or unconsolidated sediments that contain certain volcanic rocks may have as much as 9 ppm of fluoride.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1819E","usgsCitation":"Kister, L.R., and Hardt, W.F., 1966, Salinity of the ground water in western Pinal County, Arizona: U.S. Geological Survey Water Supply Paper 1819, 21 p. :illus., maps (2 fold. in pocket), https://doi.org/10.3133/wsp1819E.","productDescription":"21 p. :illus., maps (2 fold. in pocket)","costCenters":[],"links":[{"id":137670,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1819e/report-thumb.jpg"},{"id":27512,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1819e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27513,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1819e/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27514,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1819e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdf9e","contributors":{"authors":[{"text":"Kister, Lester Ray","contributorId":107670,"corporation":false,"usgs":true,"family":"Kister","given":"Lester","email":"","middleInitial":"Ray","affiliations":[],"preferred":false,"id":144560,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hardt, W. F.","contributorId":12455,"corporation":false,"usgs":true,"family":"Hardt","given":"W.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":144559,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"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":42296,"text":"ofr66127 - 1966 - Bedrock geologic map of the Denton quadrangle, North Carolina","interactions":[{"subject":{"id":42296,"text":"ofr66127 - 1966 - Bedrock geologic map of the Denton quadrangle, North Carolina","indexId":"ofr66127","publicationYear":"1966","noYear":false,"title":"Bedrock geologic map of the Denton quadrangle, North Carolina"},"predicate":"SUPERSEDED_BY","object":{"id":61806,"text":"gq872 - 1971 - Geologic map of the Denton quadrangle, central North Carolina","indexId":"gq872","publicationYear":"1971","noYear":false,"title":"Geologic map of the Denton quadrangle, central North Carolina"},"id":1}],"supersededBy":{"id":61806,"text":"gq872 - 1971 - Geologic map of the Denton quadrangle, central North Carolina","indexId":"gq872","publicationYear":"1971","noYear":false,"title":"Geologic map of the Denton quadrangle, central North Carolina"},"lastModifiedDate":"2020-02-05T15:14:09","indexId":"ofr66127","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":"66-127","title":"Bedrock geologic map of the Denton quadrangle, North Carolina","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr66127","usgsCitation":"Stromquist, A.A., 1966, Bedrock geologic map of the Denton quadrangle, North Carolina: U.S. Geological Survey Open-File Report 66-127, 2 Plates: 22.44 x 29.70 inches and 17.07 x 21.26 inches, https://doi.org/10.3133/ofr66127.","productDescription":"2 Plates: 22.44 x 29.70 inches and 17.07 x 21.26 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