No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp413","usgsCitation":"Dempsey, W., and Fackler, W., 1963, Aeromagnetic map of the Cochise quadrangle, Cochise County, Arizona: U.S. Geological Survey Geophysical Investigations Map 413, 1 Plate: 21.60 x 22.10 inches, https://doi.org/10.3133/gp413.","productDescription":"1 Plate: 21.60 x 22.10 inches","costCenters":[],"links":[{"id":260654,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0413/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":187026,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":485002,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3354.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"62500","country":"United States","state":"Arizona","county":"Cochise County","otherGeospatial":"Cochise quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -110,\n 32.25\n ],\n [\n -110,\n 32\n ],\n [\n -109.75,\n 32\n ],\n [\n -109.75,\n 32.25\n ],\n [\n -110,\n 32.25\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696ee4","contributors":{"authors":[{"text":"Dempsey, W.J.","contributorId":13988,"corporation":false,"usgs":true,"family":"Dempsey","given":"W.J.","affiliations":[],"preferred":false,"id":270856,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fackler, W.D.","contributorId":66787,"corporation":false,"usgs":true,"family":"Fackler","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":270857,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":68534,"text":"ha33 - 1963 - Availability of ground water in Breckinridge, Grayson, Hardin, Larue, and Meade Counties, Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:13:40","indexId":"ha33","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"33","title":"Availability of ground water in Breckinridge, Grayson, Hardin, Larue, and Meade Counties, Kentucky","language":"ENGLISH","doi":"10.3133/ha33","usgsCitation":"Brown, R., and Lambert, T.W., 1963, Availability of ground water in Breckinridge, Grayson, Hardin, Larue, and Meade Counties, Kentucky: U.S. Geological Survey Hydrologic Atlas 33, 3 col. maps ;53 x 54 cm. (Two mpas, scale 1:250,000, and generalized columnar section. Sheet 1, 21 by 21 inches; sheet 2, 21 by 31 inches; sheet 3, 22 by 23 inches), https://doi.org/10.3133/ha33.","productDescription":"3 col. maps ;53 x 54 cm. (Two mpas, scale 1:250,000, and generalized columnar section. Sheet 1, 21 by 21 inches; sheet 2, 21 by 31 inches; sheet 3, 22 by 23 inches)","costCenters":[],"links":[{"id":186121,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90140,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/033/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90141,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/033/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90142,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/033/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6672f0","contributors":{"authors":[{"text":"Brown, Richmond F.","contributorId":40577,"corporation":false,"usgs":true,"family":"Brown","given":"Richmond F.","affiliations":[],"preferred":false,"id":278412,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lambert, T. William","contributorId":40574,"corporation":false,"usgs":true,"family":"Lambert","given":"T.","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":278411,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":6122,"text":"pp374E - 1963 - Reconnaissance geology between Lake Mead and Davis Dam, Arizona-Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:05:56","indexId":"pp374E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"374","chapter":"E","title":"Reconnaissance geology between Lake Mead and Davis Dam, Arizona-Nevada","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp374E","usgsCitation":"Longwell, C.R., 1963, Reconnaissance geology between Lake Mead and Davis Dam, Arizona-Nevada: U.S. Geological Survey Professional Paper 374, p. E1-E51, https://doi.org/10.3133/pp374E.","productDescription":"p. E1-E51","costCenters":[],"links":[{"id":126829,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0374e/report-thumb.jpg"},{"id":33189,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0374e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a70e4b07f02db641037","contributors":{"authors":[{"text":"Longwell, Chester R.","contributorId":55424,"corporation":false,"usgs":true,"family":"Longwell","given":"Chester","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":152154,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":64342,"text":"gp380 - 1963 - Aeromagnetic map of the Telos Lake quadrangle, Piscataquis County, Maine","interactions":[],"lastModifiedDate":"2012-02-10T00:10:54","indexId":"gp380","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"380","title":"Aeromagnetic map of the Telos Lake quadrangle, Piscataquis County, Maine","language":"ENGLISH","doi":"10.3133/gp380","usgsCitation":"Bromery, R.W., and McGowan, E., 1963, Aeromagnetic map of the Telos Lake quadrangle, Piscataquis County, Maine: U.S. Geological Survey Geophysical Investigations Map 380, 1 map., https://doi.org/10.3133/gp380.","productDescription":"1 map.","costCenters":[],"links":[{"id":250997,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0380/report.pdf","size":"30","linkFileType":{"id":1,"text":"pdf"}},{"id":250998,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0380/plate-1.pdf","size":"1566","linkFileType":{"id":1,"text":"pdf"}},{"id":251730,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0380/report-thumb.jpg"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -69.25,46 ], [ -69.25,46.25 ], [ -69,46.25 ], [ -69,46 ], [ -69.25,46 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db6910c4","contributors":{"authors":[{"text":"Bromery, R. W.","contributorId":11676,"corporation":false,"usgs":true,"family":"Bromery","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":270643,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McGowan, E.F.","contributorId":96769,"corporation":false,"usgs":true,"family":"McGowan","given":"E.F.","email":"","affiliations":[],"preferred":false,"id":270644,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":62756,"text":"gq252 - 1963 - Geology of the Madisonville East quadrangle, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:40","indexId":"gq252","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"252","title":"Geology of the Madisonville East quadrangle, Kentucky","language":"ENGLISH","doi":"10.3133/gq252","usgsCitation":"Kehn, T.M., 1963, Geology of the Madisonville East quadrangle, Kentucky: U.S. Geological Survey Geologic Quadrangle 252, 1 map :col. ;58 x 46 cm., on sheet 79 x 87 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/gq252.","productDescription":"1 map :col. ;58 x 46 cm., on sheet 79 x 87 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":102257,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_706.htm","linkFileType":{"id":5,"text":"html"},"description":"706"},{"id":248911,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0252/report.pdf","size":"33","linkFileType":{"id":1,"text":"pdf"}},{"id":254386,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0252/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87.5,37.25 ], [ -87.5,37.3675 ], [ -87.36749999999999,37.3675 ], [ -87.36749999999999,37.25 ], [ -87.5,37.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae02d","contributors":{"authors":[{"text":"Kehn, Thomas M.","contributorId":64219,"corporation":false,"usgs":true,"family":"Kehn","given":"Thomas","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":267816,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2390,"text":"wsp1757A - 1963 - Ground-water exploration in Al Marj area, Cyrenaica, United Kingdom of Libya","interactions":[],"lastModifiedDate":"2012-02-02T00:05:33","indexId":"wsp1757A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"1757","chapter":"A","title":"Ground-water exploration in Al Marj area, Cyrenaica, United Kingdom of Libya","docAbstract":"The present report, based largely on fieldwork during 1959-61, describes the results of reconnaissance hydrogeologic studies and exploratory drilling to evaluate the general water-bearing properties of the rocks and the availability of groundwater supplies for irrigation, stock, and village uses in Al Marj area. These studies and the drilling were conducted under the auspices of the U.S. Operations Mission of the International Cooperation Administration. \r\n\r\nAl Marj area, located in the Province of Cyrenaica on the southern coast of the Mediterranean Sea, contains a land area of about 6,770 square kilometers. Along the Mediterranean shore is a narrow coastal plain that rises evenly to the base of an escarpment that forms the seaward front of an undulating plateau known as. Al Jabal al Akhgiar. The climate is semiarid; seasonal rainfall occurs during the winter months. Owing to orographic effects, the rainfall is somewhat higher in the Jabal than in the coastal plain. The average annual rainfall ranges from about 250 millimeters in the coastal plain to 450 millimeters on the Jabal. All the streams (wadis) of the area are ephemeral and flow only in response to heavy rains of the winter season. From a drainage divide on the Jabal some streams flow north and northwest toward the sea and the others, south and southeast to the interior desert. Solution features, such as limestone sink holes, are common in the coastal plain and a large solution depression occurs near Al Marj. \r\n\r\nThe rocks of A1 Marj area consist predominantly of limestone and some sandstone and shale; they range from Cretaceous to Miocene age. On the coastal plain Miocene limestone is locally mantled by Quaternary alluvial, beach and lagoonal deposits. The Miocene and older beds have a regional southerly dip. These rocks are broken by northeast-trending normal faults in the coastal and inland escarpments. \r\n\r\nThe ground-water reservoir is contained chiefly in fractures, bedding planes, and solution openings in the limestone country rock. The upper limit of this reservoir is marked by a water table which generally lies within 40 meters of the land surface in the coastal plain but is 100 meters or more below the surface of most of the Jabal and the interior desert. The ground-water reservoir is replenished chiefly by infiltration from surface-water runoff in wadis and to less extent by direct infiltration of rainfall. Ground water moves north and northwest toward the Mediterranean Sea and south toward the interior desert from a ground-water divide near the crest of A1 Jabal al Akhgiar. Discharge of ground water takes place by submarine outflow, spring flow, evapotranspiration, and withdrawals from wells. \r\n\r\nWells, springs, and cisterns furnish almost all water supplies for municipal, village, stock and irrigation purposes. Bengasi, A1 Marj, and A1 Abyar are the only centers of population with municipal distribution systems. Drafts from individual dug wells used for irrigation in the coastal plain generally are no more than 10 to 15 cubic meters per day. In the Jabal and the interior desert drafts from individual stock and village wells are generally less than 10 cubic meters per day and from most wells only a few thousand liters per day. \r\n\r\nSome 21 test wells were put down during the present investigation to depths ranging from 30 to 309 meters. The yields obtained by test pump and bailer ranged from 45 to 0.6 cubic meters per hour. With few exceptions, well yields sufficient for stock and village requirements were obtained. Well yields sufficient for irrigation even on a moderate scale, however, are not everywhere available. In the Jabal and the interior desert the ground water is generally of good to fair chemical quality and suitable for most purposes. In the coastal plain, however, the ground water is in places moderately to highly mineralized, and consequently for irrigation use it must be applied to the land under optimum crop soil, and drainage conditions.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1757A","usgsCitation":"Newport, T., and Haddor, Y., 1963, Ground-water exploration in Al Marj area, Cyrenaica, United Kingdom of Libya: U.S. Geological Survey Water Supply Paper 1757, iii, 24 p. :ill., maps ;24 cm. + plates folded in pocket., https://doi.org/10.3133/wsp1757A.","productDescription":"iii, 24 p. :ill., maps ;24 cm. + plates folded in pocket.","costCenters":[],"links":[{"id":139184,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1757a/report-thumb.jpg"},{"id":28365,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1757a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28366,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1757a/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28367,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1757a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66ce76","contributors":{"authors":[{"text":"Newport, T.G.","contributorId":80258,"corporation":false,"usgs":true,"family":"Newport","given":"T.G.","email":"","affiliations":[],"preferred":false,"id":145123,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haddor, Yousef","contributorId":78722,"corporation":false,"usgs":true,"family":"Haddor","given":"Yousef","email":"","affiliations":[],"preferred":false,"id":145122,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":63012,"text":"gq200 - 1963 - Bedrock geology of the Southington quadrangle, Connecticut","interactions":[],"lastModifiedDate":"2012-02-10T00:10:46","indexId":"gq200","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"200","title":"Bedrock geology of the Southington quadrangle, Connecticut","language":"ENGLISH","doi":"10.3133/gq200","usgsCitation":"Fritts, C., 1963, Bedrock geology of the Southington quadrangle, Connecticut: U.S. Geological Survey Geologic Quadrangle 200, 1 map., https://doi.org/10.3133/gq200.","productDescription":"1 map.","costCenters":[],"links":[{"id":102203,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_652.htm","linkFileType":{"id":5,"text":"html"},"description":"652"},{"id":249146,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0200/report.pdf","size":"35","linkFileType":{"id":1,"text":"pdf"}},{"id":252147,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0200/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -73,41.5 ], [ -73,41.6175 ], [ -72.86749999999999,41.6175 ], [ -72.86749999999999,41.5 ], [ -73,41.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db633fcf","contributors":{"authors":[{"text":"Fritts, Crawford E.","contributorId":87619,"corporation":false,"usgs":true,"family":"Fritts","given":"Crawford E.","affiliations":[],"preferred":false,"id":268195,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":63156,"text":"gq223 - 1963 - Geology of the Hartford North quadrangle, Connecticut","interactions":[],"lastModifiedDate":"2012-02-10T00:10:43","indexId":"gq223","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"223","title":"Geology of the Hartford North quadrangle, Connecticut","language":"ENGLISH","doi":"10.3133/gq223","usgsCitation":"Cushman, R., 1963, Geology of the Hartford North quadrangle, Connecticut: U.S. Geological Survey Geologic Quadrangle 223, 1 map :col. ;57 x 43 cm., on sheet 70 x 77 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/gq223.","productDescription":"1 map :col. ;57 x 43 cm., on sheet 70 x 77 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":102227,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_676.htm","linkFileType":{"id":5,"text":"html"},"description":"676"},{"id":249277,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0223/report.pdf","size":"34","linkFileType":{"id":1,"text":"pdf"}},{"id":252441,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0223/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -72.75,41.75 ], [ -72.75,41.8675 ], [ -72.61749999999999,41.8675 ], [ -72.61749999999999,41.75 ], [ -72.75,41.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acfe4b07f02db67ffcb","contributors":{"authors":[{"text":"Cushman, R.V.","contributorId":28220,"corporation":false,"usgs":true,"family":"Cushman","given":"R.V.","email":"","affiliations":[],"preferred":false,"id":268417,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":63113,"text":"gq196 - 1963 - Geology of the Ashland quadrangle, Kentucky-Ohio, and the Catlettsburg quadrangle in Kentucky","interactions":[],"lastModifiedDate":"2022-12-27T20:24:26.87574","indexId":"gq196","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"196","title":"Geology of the Ashland quadrangle, Kentucky-Ohio, and the Catlettsburg quadrangle in Kentucky","docAbstract":"No abstract available.
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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha76","usgsCitation":"Prescott, G., 1963, Geologic map of the surficial deposits of part of southwestern Maine and their water-bearing characteristics: U.S. Geological Survey Hydrologic Atlas 76, 1 Plate: 40.00 × 54.00 inches, https://doi.org/10.3133/ha76.","productDescription":"1 Plate: 40.00 × 54.00 inches","costCenters":[],"links":[{"id":187921,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":251447,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/076/plate-1-preview.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89337,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/076/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":398601,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_16173.htm"}],"scale":"62500","country":"United States","state":"Maine","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -71,40 ], [ -71,43.75 ], [ -70.25,43.75 ], [ -70.25,40 ], [ -71,40 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688809","contributors":{"authors":[{"text":"Prescott, Glenn C.","contributorId":38126,"corporation":false,"usgs":true,"family":"Prescott","given":"Glenn C.","affiliations":[],"preferred":false,"id":277608,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":6425,"text":"pp363 - 1963 - Geology of the Capitol Reef area, Wayne and Garfield Counties, Utah","interactions":[],"lastModifiedDate":"2025-09-22T17:57:42.361737","indexId":"pp363","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"363","title":"Geology of the Capitol Reef area, Wayne and Garfield Counties, Utah","docAbstract":"The Capitol Reef area includes about 900 square miles in western Wayne and north-central Garfield Counties, Utah. It is along the border between the High Plateaus of Utah and the Canyon Lands sections of the Colorado' Plateaus province. Capitol Reef National Monument is in the eastern part of the mapped area.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp363","usgsCitation":"Smith, J.F., Huff, L.C., Hinrichs, E.N., and Luedke, R.G., 1963, Geology of the Capitol Reef area, Wayne and Garfield Counties, Utah: U.S. Geological Survey Professional Paper 363, Report: iv, 102 p.; 2 Plates: 38.88 x 44.60 inches and 18.44 x 18.72 inches, https://doi.org/10.3133/pp363.","productDescription":"Report: iv, 102 p.; 2 Plates: 38.88 x 44.60 inches and 18.44 x 18.72 inches","numberOfPages":"107","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":495847,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4361.htm","linkFileType":{"id":5,"text":"html"}},{"id":140281,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0363/report-thumb.jpg"},{"id":112832,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0363/plate-2.pdf","text":"Plate 2","size":"1.16 MB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Structure contour map and wall sections of the Oyler Mine, Capitol Reef area"},{"id":112830,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0363/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":112831,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0363/plate-1.pdf","text":"Plate 1","size":"14.6 MB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Geologic map and sections of the Capitol Reef area"}],"country":"United States","state":"Utah","county":"Garfield County, Wayne County","otherGeospatial":"Capitol Reef area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.625,\n 38.5\n ],\n [\n -111.25,\n 38.5\n ],\n [\n -111.25,\n 38.37317\n ],\n [\n -111.1296,\n 38.37317\n ],\n [\n -111.1296,\n 38.25\n ],\n [\n -111,\n 38.25\n ],\n [\n -111,\n 38\n ],\n [\n -111.5,\n 38\n ],\n [\n -111.5,\n 38.1167\n ],\n [\n -111.625,\n 38.1167\n ],\n [\n -111.625,\n 38.5\n ]\n ]\n ]\n }\n }\n ]\n}","publicComments":"Prepared on behalf of the U.S. Atomic Energy Commission.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db683207","contributors":{"authors":[{"text":"Smith, J. Fred Jr.","contributorId":106482,"corporation":false,"usgs":true,"family":"Smith","given":"J.","suffix":"Jr.","email":"","middleInitial":"Fred","affiliations":[],"preferred":false,"id":152702,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Huff, Lyman C.","contributorId":47440,"corporation":false,"usgs":true,"family":"Huff","given":"Lyman","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":152699,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hinrichs, E. Neal","contributorId":46488,"corporation":false,"usgs":true,"family":"Hinrichs","given":"E.","email":"","middleInitial":"Neal","affiliations":[],"preferred":false,"id":152701,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Luedke, Robert G.","contributorId":18339,"corporation":false,"usgs":true,"family":"Luedke","given":"Robert","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":152700,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":64146,"text":"gp443 - 1963 - Aeromagnetic map of the Timber Mountain quadrangle and part of the Silent Canyon quadrangle, Nye County, Nevada","interactions":[],"lastModifiedDate":"2025-04-24T20:01:34.618868","indexId":"gp443","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"443","title":"Aeromagnetic map of the Timber Mountain quadrangle and part of the Silent Canyon quadrangle, Nye County, Nevada","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp443","usgsCitation":"Boynton, G.R., Meuschke, J.L., and Vargo, J.L., 1963, Aeromagnetic map of the Timber Mountain quadrangle and part of the Silent Canyon quadrangle, Nye County, Nevada: U.S. Geological Survey Geophysical Investigations Map 443, 1 Plate: 20.42 x 28.45 inches, https://doi.org/10.3133/gp443.","productDescription":"1 Plate: 20.42 x 28.45 inches","costCenters":[],"links":[{"id":485033,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3387.htm","linkFileType":{"id":5,"text":"html"}},{"id":254114,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0443/report-thumb.jpg"},{"id":250630,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0443/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":250629,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0443/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"Nevada","county":"Nye County","otherGeospatial":"Timber Mountain quadrangle and part of the Silent Canyon quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -116.5,\n 37.333\n ],\n [\n -116.5,\n 37\n ],\n [\n -116.25,\n 37\n ],\n [\n -116.25,\n 37.333\n ],\n [\n -116.5,\n 37.333\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db6910a3","contributors":{"authors":[{"text":"Boynton, G. R.","contributorId":82276,"corporation":false,"usgs":true,"family":"Boynton","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":270048,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meuschke, J. L.","contributorId":53349,"corporation":false,"usgs":true,"family":"Meuschke","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":270047,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Vargo, J. L.","contributorId":108198,"corporation":false,"usgs":true,"family":"Vargo","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":270049,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":64148,"text":"gp440 - 1963 - Aeromagnetic map of the Topopah Spring quadrangle and part of the Bare Mountain quadrangle, Nye County, Nevada","interactions":[],"lastModifiedDate":"2025-04-24T19:47:47.470791","indexId":"gp440","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"440","title":"Aeromagnetic map of the Topopah Spring quadrangle and part of the Bare Mountain quadrangle, Nye County, Nevada","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp440","usgsCitation":"Boynton, G.R., and Vargo, J.L., 1963, Aeromagnetic map of the Topopah Spring quadrangle and part of the Bare Mountain quadrangle, Nye County, Nevada: U.S. Geological Survey Geophysical Investigations Map 440, 1 Plate: 26.48 x 21.88 inches, https://doi.org/10.3133/gp440.","productDescription":"1 Plate: 26.48 x 21.88 inches","costCenters":[],"links":[{"id":485031,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3384.htm","linkFileType":{"id":5,"text":"html"}},{"id":254116,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0440/report-thumb.jpg"},{"id":250634,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0440/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":250633,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0440/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"Nevada","county":"Nye County","otherGeospatial":"Topopah Spring quadrangle and part of the Bare Mountain quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -116.625,\n 37\n ],\n [\n -116.625,\n 36.75\n ],\n [\n -116.25,\n 36.75\n ],\n [\n -116.25,\n 37\n ],\n [\n -116.625,\n 37\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae7e4b07f02db68c3cb","contributors":{"authors":[{"text":"Boynton, G. 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L.","contributorId":108198,"corporation":false,"usgs":true,"family":"Vargo","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":270054,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":32728,"text":"pp444 - 1963 - Geology of Mount Rainier National Park, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:09:10","indexId":"pp444","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"444","title":"Geology of Mount Rainier National Park, Washington","docAbstract":"Mount Rainier National Park includes 378 square miles of \r\nrugged terrain on the west slope of the Cascade Mountains \r\nin central Washington. Its mast imposing topographic and geologic feature is glacier-clad Mount Rainier. This volcano, \r\ncomposed chiefly of flows of pyroxene andesite, was built upon \r\nalt earlier mountainous surface, carved from altered volcanic \r\nand sedimentary rocks invaded by plutonic and hypabyssal \r\nigneous rocks of great complexity. \r\nThe oldest rocks in the park area are those that make up \r\nthe Olmnapecosh Formation of late Eocene age. This formation \r\nis more than 10,000 feet thick, and consists almost entirely of \r\nvolcanic debris. It includes some lensoid accumulations of \r\nlava and coarse mudflows, heaped around volcanic centers., but \r\nthese are surrounded by vastly greater volumes of volcanic \r\nclastic rocks, in which beds of unstratified coarse tuff-breccia, \r\nabout 30 feet in average thickness, alternate with thin-bedded \r\nbreccias, sandstones, and siltstones composed entirely of volcanic debris. The coarser tuff-breccias were probably deposited \r\nfrom subaqueous volcanic mudflows generated when eruption \r\nclouds were discharged directly into water, or when subaerial \r\nash flows and mudflows entered bodies of water. The less \r\nmobile mudflows and viscous lavas built islands surrounded \r\nby this sea of thinner bedded water-laid clastics. In compostion the lava flows and coarse lava fragments of the \r\nOhanapecosh Formation are mostly andesite, but they include \r\nless abundant dacite, basalt, and rhyolite. \r\nThe Ohanapecosh Formation was folded, regionally altered \r\nto minerals characteristic of the zeolite facies of metamorphism, uplifted, and deeply eroded before the overlying Stevens \r\nRidge Formation of Oligocene or early Miocene age was deposited upon it. The Stevens Ridge rocks, which are about \r\n3,000 feet in maximum total thickness, consist mainly of massive \r\nash flows. These are now devitrified and altered, but they \r\noriginally consisted of rhyodacite pumice lapilli and glass \r\nshards, which compacted and welded into thick massive units \r\nduring emplacement and cooling. Subordinate water-laid clastic rocks occur t(ward the top of the formation, and thin-bedded \r\npyroclastic layers occur between some of the ash flows. \r\nExposures on Backbone Ridge and on Carbon River below \r\nthe mouth of Cataract Creek show that in places the thick \r\nbasal Stevens Ridge ash flows swept with great violence over \r\nan old erosion surface developed on rocks of the Ohanapecosh \r\nFormation. Masses of mud, tree trunks, and other surface \r\ndebris were swirled upward into the base of the lowermost ash \r\nfiery, and lobes and tongues of hot ash were forced downward \r\ninto. the saprolitic mud. \r\nThe Stevens Ridge Formation is concordantly overlain by the Fifes Peak Formation of probable early Miocene age, which consists of lava flows, subordinate mudflows, and minor quantities of tuffaceous clastic rocks. The lavas are predominantly olivine basalt and basaltic andesite, but they include a little rhyolite. They are slightly to moderately altered: the ferromagnesian phenocrysts are generally replaced by saponite, chiprite, or carbonate ; the glass is devitrified ; and the rocks are locally permeated by veinlets of zeolite. Swarms of diabase sills and dikes are probably intrusive equivalents of the Fifes Peak lavas. \r\n\r\nThe upper part of the Fifes Peak Formation has been mostly eroded from Mount Rainier National Park, but farther north, in the Cedar Lake quadrangle, it attains a thickness of more than 5,000 feet. \r\n\r\nThe Fifes Peak and earlier formations were gently folded, faulted, uplifted, and eroded before the. late Miocene Tatoosh pluton worked its way upward to shallow depths and eventually broke through to the surface. The rise of the pluton was accompanied by .the injection of a complicated melange of satellitic stocks, sills, and dikes. A favored horizon for intrusion of sills was along or near the unconfo","language":"ENGLISH","publisher":"U. S. Govt. Print. 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