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,{"id":34815,"text":"b1133B - 1962 - Geology and hydrology of the site of the Hallam Nuclear Power Facility, Nebraska","interactions":[],"lastModifiedDate":"2021-12-02T21:16:22.840163","indexId":"b1133B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1133","chapter":"B","title":"Geology and hydrology of the site of the Hallam Nuclear Power Facility, Nebraska","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Studies of sites for nuclear energy facilities","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1133B","usgsCitation":"Keech, C.F., 1962, Geology and hydrology of the site of the Hallam Nuclear Power Facility, Nebraska: U.S. Geological Survey Bulletin 1133, Report: iv, 51 p.; 4 Plates: 8.00 × 20.00 inches or smaller, https://doi.org/10.3133/b1133B.","productDescription":"Report: iv, 51 p.; 4 Plates: 8.00 × 20.00 inches or smaller","costCenters":[],"links":[{"id":109384,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20848.htm","linkFileType":{"id":5,"text":"html"},"description":"20848"},{"id":163061,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1133b/report-thumb.jpg"},{"id":62731,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1133b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62732,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1133b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62733,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1133b/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62734,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1133b/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62735,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1133b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nebraska","otherGeospatial":"Hallam Nuclear Power Facility","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -96.87400817871094,\n              40.51066695034288\n            ],\n            [\n              -96.71195983886719,\n              40.51066695034288\n            ],\n            [\n              -96.71195983886719,\n              40.70302525959208\n            ],\n            [\n              -96.87400817871094,\n              40.70302525959208\n            ],\n            [\n              -96.87400817871094,\n              40.51066695034288\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4694","contributors":{"authors":[{"text":"Keech, Charles Franklin","contributorId":44123,"corporation":false,"usgs":true,"family":"Keech","given":"Charles","email":"","middleInitial":"Franklin","affiliations":[],"preferred":false,"id":213629,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68185,"text":"ha26 - 1962 - Availability of ground water in Butler and Ohio Counties, Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:13:42","indexId":"ha26","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"26","title":"Availability of ground water in Butler and Ohio Counties, Kentucky","language":"ENGLISH","doi":"10.3133/ha26","usgsCitation":"Maxwell, B.W., and Devaul, R.W., 1962, Availability of ground water in Butler and Ohio Counties, Kentucky: U.S. Geological Survey Hydrologic Atlas 26, 3 col. maps ;56 x 68 cm.  (Two maps scale 1:125,000 and generalized columnar section. Sheet 1, 22 1/2 by 30 1/2 inches; sheet 2, 23 by 30 inches; and sheet 3, 20 by 21 inches.), https://doi.org/10.3133/ha26.","productDescription":"3 col. maps ;56 x 68 cm.  (Two maps scale 1:125,000 and generalized columnar section. Sheet 1, 22 1/2 by 30 1/2 inches; sheet 2, 23 by 30 inches; and sheet 3, 20 by 21 inches.)","costCenters":[],"links":[{"id":186469,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89495,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/026/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89496,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/026/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89497,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/026/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"25000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db6672c5","contributors":{"authors":[{"text":"Maxwell, Bruce William","contributorId":67489,"corporation":false,"usgs":true,"family":"Maxwell","given":"Bruce","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":277798,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Devaul, Robert Washburn","contributorId":84338,"corporation":false,"usgs":true,"family":"Devaul","given":"Robert","email":"","middleInitial":"Washburn","affiliations":[],"preferred":false,"id":277799,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":48196,"text":"ofr73254 - 1962 - Hydrologic investigations for northeastern Brazil","interactions":[],"lastModifiedDate":"2012-02-02T00:10:41","indexId":"ofr73254","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"73-254","title":"Hydrologic investigations for northeastern Brazil","language":"ENGLISH","doi":"10.3133/ofr73254","usgsCitation":"Schoff, S., 1962, Hydrologic investigations for northeastern Brazil: U.S. Geological Survey Open-File Report 73-254,  67 p. : maps ; 28 cm., https://doi.org/10.3133/ofr73254.","productDescription":" 67 p. : maps ; 28 cm.","costCenters":[],"links":[{"id":171349,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606960","contributors":{"authors":[{"text":"Schoff, Stuart L.","contributorId":104467,"corporation":false,"usgs":true,"family":"Schoff","given":"Stuart L.","affiliations":[],"preferred":false,"id":236953,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68470,"text":"ha29 - 1962 - Availability of ground water in McLean and Muhlenberg Counties, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:11:24","indexId":"ha29","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"29","title":"Availability of ground water in McLean and Muhlenberg Counties, Kentucky","language":"ENGLISH","doi":"10.3133/ha29","isbn":"0607760346","usgsCitation":"Devaul, R.W., and Maxwell, B.W., 1962, Availability of ground water in McLean and Muhlenberg Counties, Kentucky: U.S. Geological Survey Hydrologic Atlas 29, 3 col. maps ;56 x 68 cm.  (Two maps, scale 1:125,000, and generalized columnar section.  Sheet 1, 20 by 28 inches,; sheet 2, 20 by 27 inches; sheet 3, 20 1/2 by 25 inches), https://doi.org/10.3133/ha29.","productDescription":"3 col. maps ;56 x 68 cm.  (Two maps, scale 1:125,000, and generalized columnar section.  Sheet 1, 20 by 28 inches,; sheet 2, 20 by 27 inches; sheet 3, 20 1/2 by 25 inches)","costCenters":[],"links":[{"id":188712,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90010,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/029/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90011,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/029/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90012,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/029/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"25000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87.48472222222222,37.034166666666664 ], [ -87.48472222222222,37.668055555555554 ], [ -86.88444444444445,37.668055555555554 ], [ -86.88444444444445,37.034166666666664 ], [ -87.48472222222222,37.034166666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db660b0d","contributors":{"authors":[{"text":"Devaul, Robert Washburn","contributorId":84338,"corporation":false,"usgs":true,"family":"Devaul","given":"Robert","email":"","middleInitial":"Washburn","affiliations":[],"preferred":false,"id":278289,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Maxwell, Bruce William","contributorId":67489,"corporation":false,"usgs":true,"family":"Maxwell","given":"Bruce","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":278288,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68696,"text":"ha47 - 1962 - Floods at Fremont, Ohio","interactions":[],"lastModifiedDate":"2012-02-10T00:11:25","indexId":"ha47","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"47","title":"Floods at Fremont, Ohio","language":"ENGLISH","doi":"10.3133/ha47","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1962, Floods at Fremont, Ohio: U.S. Geological Survey Hydrologic Atlas 47, 1 map :col. ;on sheet 72 x 84 in folder 30 x 24.  (Contour interval 5 feet.  30 by 31 inches)), https://doi.org/10.3133/ha47.","productDescription":"1 map :col. ;on sheet 72 x 84 in folder 30 x 24.  (Contour interval 5 feet.  30 by 31 inches))","costCenters":[],"links":[{"id":188097,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90418,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/047/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -83.18333333333334,41.25 ], [ -83.18333333333334,41.3675 ], [ -83.05,41.3675 ], [ -83.05,41.25 ], [ -83.18333333333334,41.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7280","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":534516,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68070,"text":"ha36 - 1962 - Availability of ground water in Breathitt, Floyd, Harlan, Knott, Letcher, Martin, Magoffin, Perry, and Pike Counties, Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:13:36","indexId":"ha36","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"36","title":"Availability of ground water in Breathitt, Floyd, Harlan, Knott, Letcher, Martin, Magoffin, Perry, and Pike Counties, Kentucky","language":"ENGLISH","doi":"10.3133/ha36","usgsCitation":"Price, W.E., Kilburn, C., and Mull, D.S., 1962, Availability of ground water in Breathitt, Floyd, Harlan, Knott, Letcher, Martin, Magoffin, Perry, and Pike Counties, Kentucky: U.S. Geological Survey Hydrologic Atlas 36, 3 col. maps ;64 x 68 cm. (Sheet 1 and 2, 28 by 35; sheet 3 25 by 28), https://doi.org/10.3133/ha36.","productDescription":"3 col. maps ;64 x 68 cm. (Sheet 1 and 2, 28 by 35; sheet 3 25 by 28)","costCenters":[],"links":[{"id":187830,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":91787,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/036/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":91788,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/036/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":91789,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/036/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667302","contributors":{"authors":[{"text":"Price, William Evans Jr.","contributorId":31470,"corporation":false,"usgs":true,"family":"Price","given":"William","suffix":"Jr.","email":"","middleInitial":"Evans","affiliations":[],"preferred":false,"id":277600,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kilburn, Chabot","contributorId":83499,"corporation":false,"usgs":true,"family":"Kilburn","given":"Chabot","email":"","affiliations":[],"preferred":false,"id":277602,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mull, D. S.","contributorId":43331,"corporation":false,"usgs":true,"family":"Mull","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":277601,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":68469,"text":"ha27 - 1962 - Availability of ground water in Daviess and Hancock Counties, Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:13:36","indexId":"ha27","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"27","title":"Availability of ground water in Daviess and Hancock Counties, Kentucky","language":"ENGLISH","doi":"10.3133/ha27","usgsCitation":"Devaul, R.W., and Maxwell, B.W., 1962, Availability of ground water in Daviess and Hancock Counties, Kentucky: U.S. Geological Survey Hydrologic Atlas 27, 3 col. maps ;56 x 68 cm.  (Two maps, scale 1:125,000, and generalied columna section. Sheet 1, 21 by 27 inches;  sheet 2, 30 by 27 inches; and sheet 3, 20 by 24 inches), https://doi.org/10.3133/ha27.","productDescription":"3 col. maps ;56 x 68 cm.  (Two maps, scale 1:125,000, and generalied columna section. Sheet 1, 21 by 27 inches;  sheet 2, 30 by 27 inches; and sheet 3, 20 by 24 inches)","costCenters":[],"links":[{"id":188711,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90007,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/027/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90008,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/027/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90009,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/027/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"25000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db667201","contributors":{"authors":[{"text":"Devaul, Robert Washburn","contributorId":84338,"corporation":false,"usgs":true,"family":"Devaul","given":"Robert","email":"","middleInitial":"Washburn","affiliations":[],"preferred":false,"id":278287,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Maxwell, Bruce William","contributorId":67489,"corporation":false,"usgs":true,"family":"Maxwell","given":"Bruce","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":278286,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":52264,"text":"ofr6294 - 1962 - Water supply for a fish hatchery site, Clearwater Valley, Idaho","interactions":[],"lastModifiedDate":"2013-11-19T11:48:46","indexId":"ofr6294","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"62-94","title":"Water supply for a fish hatchery site, Clearwater Valley, Idaho","docAbstract":"A fish hatchery proposed for the lower Clearwater River basin would require a continuous water supply of 10 to 12 cubic feet per second. Limitations on maximum and minimum temperatures and on turbidity are such that a combination surface-and ground-water supply probably would be required.\n\nSix prospective sites were examined with respect to their water supply. The sites were at the mouths of Orofino, Jim Fork, Lolo, Lawyer, Clear, and Cottonwood Creeks.\n\nThe geology and ground-water hydrology were studied to determine the potential ground-water supply at each of the sites. Spot measurements were made on the six tributary streams and comparative studies were made with records on nearby streams to determine probable minimum flows.\n\nOf the six sites studied, only one, at the mouth of Clear Creek, had a favorable potential for both surface-and ground-water supply. As an alternative to the Clear Creek site, a location along the South Fork Clearwater River near Kooskia might be considered.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6294","collaboration":"Prepared in cooperation with the U.S. Bureau of Sport Fisheries and Wildlife","usgsCitation":"Mundorff, M., and Travis, W.I., 1962, Water supply for a fish hatchery site, Clearwater Valley, Idaho: U.S. Geological Survey Open-File Report 62-94, Report: iii. 35 p.; 4 plates: 14.12 x 10.22 inches and smaller, https://doi.org/10.3133/ofr6294.","productDescription":"Report: iii. 35 p.; 4 plates: 14.12 x 10.22 inches and smaller","numberOfPages":"51","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":173865,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1962/0094/report-thumb.jpg"},{"id":86774,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0094/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86775,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0094/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86776,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0094/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86777,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0094/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86778,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1962/0094/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","otherGeospatial":"Clearwater Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.032525,46.133835 ], [ -117.032525,46.527176 ], [ -115.875978,46.527176 ], [ -115.875978,46.133835 ], [ -117.032525,46.133835 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0112","contributors":{"authors":[{"text":"Mundorff, M.J.","contributorId":48158,"corporation":false,"usgs":true,"family":"Mundorff","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":245057,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Travis, W. I.","contributorId":47445,"corporation":false,"usgs":true,"family":"Travis","given":"W.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":245056,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":57722,"text":"ofr62161 - 1962 - Geologic and hydrologic aspects of test-well drilling","interactions":[],"lastModifiedDate":"2012-02-02T00:12:12","indexId":"ofr62161","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"62-161","title":"Geologic and hydrologic aspects of test-well drilling","language":"ENGLISH","doi":"10.3133/ofr62161","usgsCitation":"Johnson, P.W., White, N.D., and Page, H.G., 1962, Geologic and hydrologic aspects of test-well drilling: U.S. Geological Survey Open-File Report 62-161, vi, 112 p. : ill. ; 27 cm., https://doi.org/10.3133/ofr62161.","productDescription":"vi, 112 p. : ill. ; 27 cm.","costCenters":[],"links":[{"id":184242,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8242","contributors":{"authors":[{"text":"Johnson, Phillip W.","contributorId":27422,"corporation":false,"usgs":true,"family":"Johnson","given":"Phillip","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":257638,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"White, Natalie D.","contributorId":97064,"corporation":false,"usgs":true,"family":"White","given":"Natalie","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":257640,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Page, Harry G.","contributorId":62203,"corporation":false,"usgs":true,"family":"Page","given":"Harry","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":257639,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1973,"text":"wsp1619U - 1962 - Methods of measuring soil moisture in the field","interactions":[],"lastModifiedDate":"2012-02-02T00:05:24","indexId":"wsp1619U","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1619","chapter":"U","title":"Methods of measuring soil moisture in the field","docAbstract":"For centuries, the amount of moisture in the soil has been of interest in agriculture. The subject of soil moisture is also of great importance to the hydrologist, forester, and soils engineer. \r\n\r\nMuch equipment and many methods have been developed to measure soil moisture under field conditions. This report discusses and evaluates the various methods for measurement of soil moisture and describes the equipment needed for each method. The advantages and disadvantages of each method are discussed and an extensive list of references is provided for those desiring to study the subject in more detail. \r\n\r\nThe gravimetric method is concluded to be the most satisfactory method for most problems requiring onetime moisture-content data. The radioactive method is normally best for obtaining repeated measurements of soil moisture in place. It is concluded that all methods have some limitations and that the ideal method for measurement of soil moisture under field conditions has yet to be perfected.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1619U","usgsCitation":"Johnson, A., 1962, Methods of measuring soil moisture in the field: U.S. Geological Survey Water Supply Paper 1619, iii, 25 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1619U.","productDescription":"iii, 25 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":138299,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1619u/report-thumb.jpg"},{"id":27349,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1619u/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62bee4","contributors":{"authors":[{"text":"Johnson, A.I.","contributorId":82676,"corporation":false,"usgs":true,"family":"Johnson","given":"A.I.","email":"","affiliations":[],"preferred":false,"id":144460,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4149,"text":"cir457 - 1962 - Floods in Utah, magnitude and frequency","interactions":[],"lastModifiedDate":"2017-02-21T16:28:11","indexId":"cir457","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"457","title":"Floods in Utah, magnitude and frequency","docAbstract":"This report presents a procedure for estimating the magnitude and frequency of floods, within the range of the base data, for any site, gaged or ungaged. From the relation of annual floods to the mean annual flood, a composite frequency curve was derived for recurrence intervals of 1.1 to 50 years. For regions of similar hydrologic characteristics, curves were developed by multiple correlation to express the relation of mean annual flood to drainage area and mean altitude. The records of gaging stations having 5 or more years of record were used as base data when the natural conditions of streamflow are not affected by works of man. For major rivers where the flow is affected by diversion or regulation, separate analyses were made for each stream. The results may be applied to any area in Utah, except the Great Salt Lake Desert and a small area of the State in the Snake River basin.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/cir457","usgsCitation":"Berwick, V., 1962, Floods in Utah, magnitude and frequency: U.S. Geological Survey Circular 457, iii, 24 p., https://doi.org/10.3133/cir457.","productDescription":"iii, 24 p.","numberOfPages":"28","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":124558,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1962/0457/report-thumb.jpg"},{"id":31255,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1962/0457/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e0a37","contributors":{"authors":[{"text":"Berwick, Vernon K.","contributorId":100373,"corporation":false,"usgs":true,"family":"Berwick","given":"Vernon K.","affiliations":[],"preferred":false,"id":148294,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3506,"text":"cir468 - 1962 - Ground-water studies and analog models","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"cir468","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"468","title":"Ground-water studies and analog models","docAbstract":"Hydrologists make ground-water studies to aid managers and users of water resources in solving their problems in the development and management of ground water. Geologic and hydrologic information provides the basic knowledge for construction of electric analog models that portray the ground-water system in miniature. Analog models can be analyzed electrically, and the results of the analysis are presented in terms of the ground-water system so that the effects of alternative methods of water development can be assessed.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir468","usgsCitation":"Robinove, C.J., 1962, Ground-water studies and analog models: U.S. Geological Survey Circular 468, 12 p. :ill. ;27 cm., https://doi.org/10.3133/cir468.","productDescription":"12 p. :ill. ;27 cm.","costCenters":[],"links":[{"id":123185,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1962/0468/report-thumb.jpg"},{"id":30520,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1962/0468/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696865","contributors":{"authors":[{"text":"Robinove, Charles Joseph","contributorId":71153,"corporation":false,"usgs":true,"family":"Robinove","given":"Charles","email":"","middleInitial":"Joseph","affiliations":[],"preferred":false,"id":147055,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1986,"text":"wsp1475H - 1962 - Availability of Additional Water for Chiricahua National Monument, Cochise County, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1475H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1475","chapter":"H","title":"Availability of Additional Water for Chiricahua National Monument, Cochise County, Arizona","docAbstract":"The Chiricahua National Monument is in the eastern part of Cochise County, Ariz. The monument is about 35 miles southeast of Wilicox in the north end of the Chiricahua Mountains which border Sulphur Springs Valley on the west. The area is drained by two intermittent washes, one in Bonita and the other in Rhyolite Canyons.\r\n\r\nShake Spring is the present source of water for the monument. It ranges in rate of flow from 2 to 12 gpm (gallons per minute) and during dry periods It is not adequate to support the requirements of the monument.\r\n\r\nAmple water to meet the present and future needs of the Chiricahua National Monument is available from a combination of several sources - undeveloped springs or seeps, capture of runoff out of the canyons, and wells drilled in the alluvium.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Hydrology of the Public Domain","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1475H","collaboration":"Prepared in cooperation with the National Park Service","usgsCitation":"Johnson, P.W., 1962, Availability of Additional Water for Chiricahua National Monument, Cochise County, Arizona: U.S. Geological Survey Water Supply Paper 1475, 209-216 p. & 1 map in pocket., https://doi.org/10.3133/wsp1475H.","productDescription":"209-216 p. & 1 map in pocket.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":137684,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1475h/report-thumb.jpg"},{"id":27370,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1475h/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27371,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1475h/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":12449,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.nps.gov/history/history/online_books/geology/publications/wsp/1475-H/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a98e","contributors":{"authors":[{"text":"Johnson, Phillip W.","contributorId":27422,"corporation":false,"usgs":true,"family":"Johnson","given":"Phillip","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":144479,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3505,"text":"cir466 - 1962 - Notes on earth fissures in southern Arizona","interactions":[],"lastModifiedDate":"2018-01-02T20:18:52","indexId":"cir466","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"466","title":"Notes on earth fissures in southern Arizona","docAbstract":"This report describes earth fissures at six sites in southern Arizona. These notes are preliminary to a more extensive study and detailed analysis being prepared by hydrologists in the Water Resources Division. Earth fissures were first recorded in Arizona in 1927, and have been noticed with increasing frequency since 1949. Fissures at Black Canyon, Bowie, Chandler Heights, Luke Air Force Base, Picacho, and Sells are discussed and illustrated with photographs.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir466","usgsCitation":"Robinson, G., and Peterson, D., 1962, Notes on earth fissures in southern Arizona: U.S. Geological Survey Circular 466, iii, 7 p. :illus., fold. map (in pocket) profile. ;27cm., https://doi.org/10.3133/cir466.","productDescription":"iii, 7 p. :illus., fold. map (in pocket) profile. ;27cm.","costCenters":[],"links":[{"id":30519,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1962/0466/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117655,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1962/0466/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696a0f","contributors":{"authors":[{"text":"Robinson, G.M.","contributorId":68710,"corporation":false,"usgs":true,"family":"Robinson","given":"G.M.","email":"","affiliations":[],"preferred":false,"id":147054,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peterson, D.E.","contributorId":6834,"corporation":false,"usgs":true,"family":"Peterson","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":147053,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1333,"text":"wsp1536E - 1962 - Theory of aquifer tests","interactions":[],"lastModifiedDate":"2012-02-02T00:05:13","indexId":"wsp1536E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1536","chapter":"E","title":"Theory of aquifer tests","docAbstract":"The development of water supplies from wells was placed on a rational basis with Darcy's development of the law governing the movement of fluids through sands and with Dupuit's application of that law to the problem of radial flow toward a pumped well. As field experience increased, confidence in the applicability of quantitative methods was gained and interest in developing solutions for more complex hydrologic problems was stimulated. An important milestone was Theis' development in 1935 of a solution for the nonsteady flow of ground water, which enabled hydrologists for the first time to predict future changes in ground-water levels resulting from pumping or recharging of wells. In the quarter century since, quantitative ground-water hydrology has been enlarging so rapidly as to discourage the preparation of comprehensive textbooks. \r\n\r\nThis report surveys developments in fluid mechanics that apply to groundwater hydrology. It emphasizes concepts and principles, and the delineation of limits of applicability of mathematical models for analysis of flow systems in the field. It stresses the importance of the geologic variable and its role in governing the flow regimen. \r\n\r\nThe report discusses the origin, occurrence, and motion of underground water in relation to the development of terminology and analytic expressions for selected flow systems. It describes the underlying assumptions necessary for mathematical treatment of these flow systems, with particular reference to the way in which the assumptions limit the validity of the treatment.","language":"ENGLISH","publisher":"U.S. Government Print. Office,","doi":"10.3133/wsp1536E","usgsCitation":"Ferris, J., Knowles, D., Brown, R.H., and Stallman, R., 1962, Theory of aquifer tests: U.S. Geological Survey Water Supply Paper 1536, vii, 105 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1536E.","productDescription":"vii, 105 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":12,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wsp1536-E","linkFileType":{"id":5,"text":"html"}},{"id":137382,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd475","contributors":{"authors":[{"text":"Ferris, J.G.","contributorId":12453,"corporation":false,"usgs":true,"family":"Ferris","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":143577,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Knowles, D.B.","contributorId":83898,"corporation":false,"usgs":true,"family":"Knowles","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":143580,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, R. H.","contributorId":19931,"corporation":false,"usgs":false,"family":"Brown","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":143578,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stallman, R.H.","contributorId":55800,"corporation":false,"usgs":true,"family":"Stallman","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":143579,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":1190,"text":"wsp1475J - 1962 - Ground water in the Wupatki and Sunset Crater National Monuments, Coconino County, Arizona","interactions":[{"subject":{"id":51815,"text":"ofr5531 - 1955 - Ground water in the Wupatki and Sunset Crater National Monuments, Coconino County, Arizona","indexId":"ofr5531","publicationYear":"1955","noYear":false,"title":"Ground water in the Wupatki and Sunset Crater National Monuments, Coconino County, Arizona"},"predicate":"SUPERSEDED_BY","object":{"id":1190,"text":"wsp1475J - 1962 - Ground water in the Wupatki and Sunset Crater National Monuments, Coconino County, Arizona","indexId":"wsp1475J","publicationYear":"1962","noYear":false,"chapter":"J","title":"Ground water in the Wupatki and Sunset Crater National Monuments, Coconino County, Arizona"},"id":1}],"lastModifiedDate":"2024-01-10T21:22:09.485848","indexId":"wsp1475J","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1475","chapter":"J","title":"Ground water in the Wupatki and Sunset Crater National Monuments, Coconino County, Arizona","docAbstract":"The Wupatki and Sunset Crater National Monuments are 15 and 30 miles, respectively, northeast of Flagstaff on the San Francisco Plateau. They are in the eastern part of the San Francisco volcanic field and on the southwest flank of the Black Mesa basin. The Supai formation, Coconino sandstone, Kaibab limestone, Moenkopi formation, and Chinle formation are overlain in parts of the area by volcanic rocks and alluvium. The regional water table occurs chiefly in the Coconino sandstone at altitudes of about 5,000 feet at Sunset Crater, about 4,075 feet near Wupatki Ruin, and about 4,100 feet near Citadel Ruin. The general movement of the ground water is northeastward. Small supplies of perched water occur in the Moenkopi formation and in the alluvium, and perched water may be present locally in the volcanic rocks. The results of the field investigation indicated that adequate ground-water supplies were available from the Coconino sandstone to meet the needs of the National Monuments, and a well was drilled at the Wupatki Monument headquarters in 1958 to a total depth of 904 feet. It produced 50 gpm (gallons per minute) of water with 45 feet of drawdown from a static water level of 780 feet below land surface.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Hydrology of the Public Domain","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1475J","collaboration":"Prepared in cooperation with the National Park Service","usgsCitation":"Cosner, O.J., 1962, Ground water in the Wupatki and Sunset Crater National Monuments, Coconino County, Arizona: U.S. Geological Survey Water Supply Paper 1475, Report: iv, 15 p.; 2 Plates: 29.25 x 30.88 inches and 14.80 x 9.90 inches, https://doi.org/10.3133/wsp1475J.","productDescription":"Report: iv, 15 p.; 2 Plates: 29.25 x 30.88 inches and 14.80 x 9.90 inches","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":424287,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24413.htm","linkFileType":{"id":5,"text":"html"}},{"id":26053,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1475j/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137938,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1475j/report-thumb.jpg"},{"id":26055,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1475j/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26054,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1475j/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona","county":"Coconino County","otherGeospatial":"Wupatki and Sunset Crater National Monuments","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n      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,{"id":1327,"text":"wsp1475K - 1962 - Ground-Water Reconnaissance at Pinnacles National Monument, California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1475K","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1475","chapter":"K","title":"Ground-Water Reconnaissance at Pinnacles National Monument, California","docAbstract":"Ground-water supplies at Pinnacles National Monument have been obtained from springs that occur in fractures and along bedding planes of volcanic flows and deposits, and from springs discharged from perched water in a sedimentary fanglomerate formation. The spring-water yield is barely adequate to supply existing camp facilities, and therefore a supplemental water supply is necessary before existing campgrounds can be expanded.\r\n\r\nThis supplemental water can be supplied by good-quality ground water obtained from shallow wells drilled in the alluvium of Chalone Creek. The yield of properly constructed wells in this area should exceed 10 gallons per minute.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Hydrology of the Public Domain","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1475K","collaboration":"Prepared in cooperation with the National Park Service","usgsCitation":"Evenson, R.E., 1962, Ground-Water Reconnaissance at Pinnacles National Monument, California: U.S. Geological Survey Water Supply Paper 1475, iii, 375-382 p., https://doi.org/10.3133/wsp1475K.","productDescription":"iii, 375-382 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":137990,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1475k/report-thumb.jpg"},{"id":12513,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.nps.gov/history/history/online_books/geology/publications/wsp/1475-K/","linkFileType":{"id":5,"text":"html"}},{"id":26378,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1475k/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26379,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1475k/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d538","contributors":{"authors":[{"text":"Evenson, R. E.","contributorId":19933,"corporation":false,"usgs":true,"family":"Evenson","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":143569,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3441,"text":"cir472 - 1962 - Current studies of the hydrology of prairie potholes","interactions":[],"lastModifiedDate":"2018-03-16T14:18:10","indexId":"cir472","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"472","title":"Current studies of the hydrology of prairie potholes","docAbstract":"<p>The prairie potholes in the North-Central States and in Canada are of glacial origin. Because many of them contain ponds or marshes, they are important in the production of livestock and waterfowl. The objective of the present investigation is to determine the amount of water that accumulates in and is used in the potholes in their natural environment.</p><p>Two study areas were selected in North Dakota, and construction of gaging facilities was completed in 1960. Each study area contains four potholes. Three of the potholes for each area contain dense growths of aquatic vegetation, and one is clear of aquatic vegetation. The instruments to provide the basic data for computing water losses include: water-stage recorder, water-temperature recorder, rain gage, anemometer, and hygrothermograph. Observations will also be made of ground-water levels, rate of growth and type of vegetation, and quality of water.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir472","usgsCitation":"Shjeflo, J.B., 1962, Current studies of the hydrology of prairie potholes: U.S. Geological Survey Circular 472, iii, 11 p., https://doi.org/10.3133/cir472.","productDescription":"iii, 11 p.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":30456,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1962/0472/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124419,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1962/0472/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e5f8","contributors":{"authors":[{"text":"Shjeflo, Jelmer B.","contributorId":27428,"corporation":false,"usgs":true,"family":"Shjeflo","given":"Jelmer","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":146921,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4164,"text":"cir458 - 1962 - Floods in Nebraska on small drainage areas, magnitude and frequency","interactions":[],"lastModifiedDate":"2012-02-02T00:05:40","indexId":"cir458","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"458","title":"Floods in Nebraska on small drainage areas, magnitude and frequency","docAbstract":"Flood hazard information is needed for small streams as well as for large ones. This report explains methods of defining the magnitude and frequency of floods in Nebraska on uncontrolled and unregulated streams which have about 300 square miles or less of drainage area contributing to surface runoff. Composite frequency curves defined for two flood regions express a ratio of floods with recurrence intervals ranging from 1.1 to 25 years to the mean annual flood. Curves for 10 hydrologic areas were defined to show the relation of the mean annual flood to the contributing drainage area, A flood-frequency curve can be drawn from these two sets of curves for any site in the State within the range of drainage area and recurrence interval that is defined by the base data and not materially affected by the works of man. The two sets of curves are based on all available pertinent data from records of 5 or more years' duration. \r\n\r\nThis report includes a tabulation of maximum flood peaks at gaging stations used and at a number of miscellaneous sites which have less than 300 square miles of contributing drainage area.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir458","usgsCitation":"Beckman, E., and Hutchison, N.E., 1962, Floods in Nebraska on small drainage areas, magnitude and frequency: U.S. Geological Survey Circular 458, iii, 33 p. :ill., maps ;27 cm., https://doi.org/10.3133/cir458.","productDescription":"iii, 33 p. :ill., maps ;27 cm.","costCenters":[],"links":[{"id":124494,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1962/0458/report-thumb.jpg"},{"id":31274,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1962/0458/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6fee","contributors":{"authors":[{"text":"Beckman, Emil W.","contributorId":82293,"corporation":false,"usgs":true,"family":"Beckman","given":"Emil W.","affiliations":[],"preferred":false,"id":148326,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hutchison, Norman E.","contributorId":71161,"corporation":false,"usgs":true,"family":"Hutchison","given":"Norman","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":148325,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2594,"text":"wsp1546 - 1962 - Annotated bibliography on hydrology and sedimentation, United States and Canada, 1955-58","interactions":[],"lastModifiedDate":"2012-02-02T00:05:20","indexId":"wsp1546","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1546","title":"Annotated bibliography on hydrology and sedimentation, United States and Canada, 1955-58","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1546","usgsCitation":"Riggs, H.C., 1962, Annotated bibliography on hydrology and sedimentation, United States and Canada, 1955-58: U.S. Geological Survey Water Supply Paper 1546, iv, 236 p. ;24 cm., https://doi.org/10.3133/wsp1546.","productDescription":"iv, 236 p. ;24 cm.","costCenters":[],"links":[{"id":137592,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1546/report-thumb.jpg"},{"id":28872,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1546/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bdc6","contributors":{"authors":[{"text":"Riggs, H. C.","contributorId":17210,"corporation":false,"usgs":true,"family":"Riggs","given":"H.","email":"","middleInitial":"C.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":145458,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2207,"text":"wsp1475G - 1962 - Water-supply possibilities at Capitol Reef National Monument, Utah","interactions":[],"lastModifiedDate":"2017-09-07T10:01:00","indexId":"wsp1475G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1475","chapter":"G","title":"Water-supply possibilities at Capitol Reef National Monument, Utah","docAbstract":"A water supply of 50 gpm (gallons per minute) is estimated to be sufficient to supply the present and future water demand at the monument. The Coconino sandstone of Permian age seems to be capable of yielding this quantity to a well between 1,500 and 2,700 feet deep in the vicinity of Fruita. Recharge to this aquifer probably is principally from the Fremont River. Water derived from the Coconino sandstone should be of potable quality. A water supply of suitable chemical quality also could be obtained directly from the Fremont River.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Hydrology of the Public Domain (Water Supply Paper 1475)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1475G","collaboration":"Prepared in cooperation with the National Park Service","usgsCitation":"Marine, I.W., 1962, Water-supply possibilities at Capitol Reef National Monument, Utah: U.S. Geological Survey Water Supply Paper 1475, Report: iii, 8 p.; 2 Plates: 14.20 x 11.41 inches and 18.50 x 9.35 inches, https://doi.org/10.3133/wsp1475G.","productDescription":"Report: iii, 8 p.; 2 Plates: 14.20 x 11.41 inches and 18.50 x 9.35 inches","startPage":"201","endPage":"208","numberOfPages":"12","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true},{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":27880,"rank":399,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1475g/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Geologic map of the Headquarters Area, Capitol Reef National Monument, Utah"},{"id":27881,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1475g/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Geologic section A-A' showing estimated depth of a typical water-test well in the vicinity of Fruita, Utah"},{"id":27882,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1475g/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138445,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1475g/report-thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Capitol Reef National Monument","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f0e4b07f02db5ee0e0","contributors":{"authors":[{"text":"Marine, I. Wendell","contributorId":49339,"corporation":false,"usgs":true,"family":"Marine","given":"I.","email":"","middleInitial":"Wendell","affiliations":[],"preferred":false,"id":144826,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2535,"text":"wsp1607 - 1962 - Reconnaissance of ground-water resources in the Eastern Coal Field Region, Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:05:29","indexId":"wsp1607","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1607","title":"Reconnaissance of ground-water resources in the Eastern Coal Field Region, Kentucky","docAbstract":"In the Eastern Coal Field region of Kentucky, water is obtained from consolidated sedimentary rocks ranging in age from Devonian to Pennsylvanian and from unconsolidated sediments of Quaternary age. About 95 percent of the area is underlain by shale, sandstone, and coal of Pennsylvanian age. Principal factors governing the availability of water in the region are depth, topographic location, and the lithology of the aquifer penetrated. In general, the yield of the well increases as the depth increases. Wells drilled in topographic lows, such as valleys, are likely to yield more water than wells drilled on topographic highs, such as hills. Sand and gravel, present in thick beds in the alluvium along the Ohio River, form the most productive aquifer in the Eastern Coal Field. Of the consolidated rocks in the region sandstone strata are the best aquifers chiefly because joints, openings along bedding planes, and intergranular pore spaces are best developed in them. Shale also supplies water to many wells in the region, chiefly from joints and openings along bedding planes. Coal constitutes a very small part of the sedimentary section, but it yields water from fractures to many wells. Limestone yields water readily from solution cavities developed along joint and bedding-plane openings. \r\n\r\nThe availability of water in different parts of the region was determined chiefly by analyzing well data collected during the reconnaissance. The resulting water-availability maps, published as hydrologic investigations atlases (Price and others, 1961 a, b; Kilburn and others, 1961) were designed to be used in conjunction with this report. The maps were constructed by dividing the region into 5 physiographic areas, into 10 subareas based chiefly on lithologic facies, and, in the case of the Kanawha section, into 2 quality-of-water areas. The 5 physiographic areas are the Knobs, Mississippian Plateau, Cumberland Plateau section, Kanawha section, and Cumberland Mountain section. \r\n\r\nThe 10 subareas are as follows: \r\n\r\n1. The Chattanooga shale. This black shale yields only enough water for a minimum domestic supply-100 to 500 gpd (gallons per day). \r\n\r\n2. Mississippian-Devonian rocks exposed along Pine Mountain. These rocks consist of shale, limestone, and sandstone. The limestone yields water to springs, and faulted limestone and sandstone lying below drainage may yield several hundred gallons per minute to wells. \r\n\r\n3. Mississippian rocks exposed along the western margin of the region. These rocks consist of thick limestone underlain by shale. The limestone yields enough water for a modern domestic supply (more than 500 gpd) , and discharges as much as 100 gpm (gallons per minute) to springs. The shale yields only enough water for a minimum domestic supply. \r\n\r\n4. Subarea 1 of the Lee formation of Pennsylvanian age. The thin shaly rocks of this subarea generally yield only enough water for a minimum domestic supply. \r\n\r\n5. Subarea 2 of the Lee formation of Pennsylvanian age. This subarea is predominantly underlain by massive sandstones; it generally yields enough water for a modern domestic supply, and in some places, enough water for small public and industrial supplies. \r\n\r\n6. Subarea 1 of the Breathitt and Conemaugh formations of Pennsylvanian age. Rocks in this subarea contain more shale than sandstone. Wells in this subarea range from adequate for a minimum domestic supply to adequate for a modern domestic supply. \r\n\r\n7. Subarea 2 of the Breathitt formation of Pennsylvanian age and undifferentiated post-Lee Pennsylvanian rocks. Wells in this subarea yield enough water for a modern domestic supply, and in many places, enough water for small public and industrial supplies. \r\n\r\n8. Alluvium along the Ohio River. Mostly composed of glacial outwash sand and gravel, the alluvium is reported to yield as much as 360 gpm to wells. \r\n\r\n9. Alluvium along the Big Sandy River and lower reaches of its Tug and Levisa Forks. Where consisting mostly of sand, ","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1607","usgsCitation":"Price, W.E., Mull, D.S., and Kilburn, C., 1962, Reconnaissance of ground-water resources in the Eastern Coal Field Region, Kentucky: U.S. Geological Survey Water Supply Paper 1607, iv, 56 p. :ill., maps ;24 cm. + plates folded in pocket., https://doi.org/10.3133/wsp1607.","productDescription":"iv, 56 p. :ill., maps ;24 cm. + plates folded in pocket.","costCenters":[],"links":[{"id":138579,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1607/report-thumb.jpg"},{"id":28766,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1607/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28767,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1607/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28768,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1607/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28769,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1607/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28770,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1607/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28771,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1607/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28772,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1607/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28773,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1607/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28774,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1607/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28775,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1607/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28776,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1607/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a69e4b07f02db63c1ba","contributors":{"authors":[{"text":"Price, William E.","contributorId":84740,"corporation":false,"usgs":true,"family":"Price","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":145361,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mull, D. S.","contributorId":43331,"corporation":false,"usgs":true,"family":"Mull","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":145359,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kilburn, Chabot","contributorId":83499,"corporation":false,"usgs":true,"family":"Kilburn","given":"Chabot","email":"","affiliations":[],"preferred":false,"id":145360,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2481,"text":"wsp1539E - 1962 - Ground-water geology and hydrology of the Maynard area, Massachusetts","interactions":[{"subject":{"id":56085,"text":"ofr5788 - 1957 - Ground-water conditions, Maynard Ordnance Test Station and vicinity, Sudbury, Massachusetts","indexId":"ofr5788","publicationYear":"1957","noYear":false,"title":"Ground-water conditions, Maynard Ordnance Test Station and vicinity, Sudbury, Massachusetts"},"predicate":"SUPERSEDED_BY","object":{"id":2481,"text":"wsp1539E - 1962 - Ground-water geology and hydrology of the Maynard area, Massachusetts","indexId":"wsp1539E","publicationYear":"1962","noYear":false,"chapter":"E","title":"Ground-water geology and hydrology of the Maynard area, Massachusetts"},"id":1}],"lastModifiedDate":"2023-10-30T22:00:02.423038","indexId":"wsp1539E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1539","chapter":"E","title":"Ground-water geology and hydrology of the Maynard area, Massachusetts","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1539E","usgsCitation":"Perlmutter, N., 1962, Ground-water geology and hydrology of the Maynard area, Massachusetts: U.S. Geological Survey Water Supply Paper 1539, Report: iv, 69 p.; 4 Plates: 28.50 x 15.98 inches or smaller, https://doi.org/10.3133/wsp1539E.","productDescription":"Report: iv, 69 p.; 4 Plates: 28.50 x 15.98 inches or smaller","costCenters":[],"links":[{"id":109975,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24728.htm","linkFileType":{"id":5,"text":"html"},"description":"24728"},{"id":28574,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539e/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28573,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539e/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28572,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539e/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28571,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28575,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1539e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138765,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1539e/report-thumb.jpg"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Maynard area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -71.5,\n              42.5\n            ],\n            [\n              -71.5,\n              42.375\n            ],\n            [\n              -71.38630924839453,\n              42.375\n            ],\n            [\n              -71.38630924839453,\n              42.5\n            ],\n            [\n              -71.5,\n              42.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668e19","contributors":{"authors":[{"text":"Perlmutter, Nathaniel M.","contributorId":32139,"corporation":false,"usgs":true,"family":"Perlmutter","given":"Nathaniel M.","affiliations":[],"preferred":false,"id":145266,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32767,"text":"pp426 - 1962 - Data on uranium and radium in ground water in the United States, 1954 to 1957","interactions":[],"lastModifiedDate":"2023-01-04T22:35:54.445213","indexId":"pp426","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"426","title":"Data on uranium and radium in ground water in the United States, 1954 to 1957","docAbstract":"<p>This report is one of a series resulting from a study by the U.S. Geological Survey to determine the occurrence and distribution of naturally radioactive substances in water. From 1954-57 uranium and radium concentrations were determined in 561 samples, mainly of ground water, having wide geologic and geographic distribution. These concentrations, together with data on the hydrologic and geologic environment, the beta-gamma activity, and the chemical characteristics of each sample, are tabulated by States.</p><p>The conterminous United States was subdivided into 10 geotectonic regions to facilitate statistical interpretation of the occurrence of uranium and radium in fresh water in approximately homogeneous geologic provinces. For each geotectonic region, the range and median were determined for the concentrations of radium and uranium; for regions from which sufficient data were available, log-normal frequency distribution curves were calculated and superimposed on histograms of radium and uranium concentrations in the samples. An \"anomaly threshold\" is suggested for both radioelements for each region analyzed statistically. The western stable region had the greatest median and highest \"anomaly threshold\" for uranium. This region also had the highest \"anomaly threshold\" for radium, but the largest median for radium was found for samples collected in the Ozark-Ouachita system. The median concentration for uranium was lowest for the Atlantic and Gulf Coastal Plain and the Pacific orogenic belt. This latter region also had the lowest median-radium content.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/pp426","usgsCitation":"Scott, R.C., and Barker, F.B., 1962, Data on uranium and radium in ground water in the United States, 1954 to 1957: U.S. Geological Survey Professional Paper 426, Report: iii, 115 p.; 2 Plates: 29.00 x 19.00 inches, https://doi.org/10.3133/pp426.","productDescription":"Report: iii, 115 p.; 2 Plates: 29.00 x 19.00 inches","numberOfPages":"120","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":411397,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4420.htm","linkFileType":{"id":5,"text":"html"}},{"id":119273,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0426/report-thumb.jpg"},{"id":60704,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0426/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60703,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0426/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Geotectonic regions of the conterminous United States"},{"id":60702,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0426/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map of the conterminous United States showing sampling sites"}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"geometry\": {\n        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