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,{"id":68265,"text":"ha38 - 1962 - Availability of ground water in Bell, Clay, Jackson, Knox, Laurel, Leslie, McCreary, Owsley, Rockcastle, and Whitley Counties, Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:13:26","indexId":"ha38","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":"38","title":"Availability of ground water in Bell, Clay, Jackson, Knox, Laurel, Leslie, McCreary, Owsley, Rockcastle, and Whitley Counties, Kentucky","language":"ENGLISH","doi":"10.3133/ha38","usgsCitation":"Kilburn, C., Price, W.E., and Mull, D.S., 1962, Availability of ground water in Bell, Clay, Jackson, Knox, Laurel, Leslie, McCreary, Owsley, Rockcastle, and Whitley Counties, Kentucky: U.S. Geological Survey Hydrologic Atlas 38, 3 col. maps ;57 x 66 cm.  (Two maps, scale 1:125,000, and generalized columnar section.  Sheet 1, 22.5 by 27 inches; sheet 2, 24 by 45 inches; sheet 3, 20 by 28 inches), https://doi.org/10.3133/ha38.","productDescription":"3 col. maps ;57 x 66 cm.  (Two maps, scale 1:125,000, and generalized columnar section.  Sheet 1, 22.5 by 27 inches; sheet 2, 24 by 45 inches; sheet 3, 20 by 28 inches)","costCenters":[],"links":[{"id":188471,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89664,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/038/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89665,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/038/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89666,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/038/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"25000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db66747b","contributors":{"authors":[{"text":"Kilburn, Chabot","contributorId":83499,"corporation":false,"usgs":true,"family":"Kilburn","given":"Chabot","email":"","affiliations":[],"preferred":false,"id":277933,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Price, William Evans Jr.","contributorId":31470,"corporation":false,"usgs":true,"family":"Price","given":"William","suffix":"Jr.","email":"","middleInitial":"Evans","affiliations":[],"preferred":false,"id":277931,"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":277932,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":68233,"text":"ha58 - 1962 - Emergency water supplies in the Wichita area, Kansas","interactions":[],"lastModifiedDate":"2012-10-30T16:17:44","indexId":"ha58","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":"58","title":"Emergency water supplies in the Wichita area, Kansas","language":"ENGLISH","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ha58","usgsCitation":"Lane, C.W., Reavis, E., and Stramel, G.J., 1962, Emergency water supplies in the Wichita area, Kansas: U.S. Geological Survey Hydrologic Atlas 58, 36 p.; 2 col. maps on one sheet: 32 x 42 inches, https://doi.org/10.3133/ha58.","productDescription":"36 p.; 2 col. maps on one sheet: 32 x 42 inches","costCenters":[],"links":[{"id":262850,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ha/058/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":190296,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ha/058/report-thumb.jpg"},{"id":89610,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/058/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -98,37 ], [ -98,38.25 ], [ -96.5,38.25 ], [ -96.5,37 ], [ -98,37 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66dd7b","contributors":{"authors":[{"text":"Lane, Charles W.","contributorId":103526,"corporation":false,"usgs":true,"family":"Lane","given":"Charles","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":277887,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reavis, E.L.","contributorId":70246,"corporation":false,"usgs":true,"family":"Reavis","given":"E.L.","email":"","affiliations":[],"preferred":false,"id":277885,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stramel, Gilbert J.","contributorId":95327,"corporation":false,"usgs":true,"family":"Stramel","given":"Gilbert","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":277886,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":68665,"text":"ha55 - 1962 - Summary of occurrence of ground water on the Papago Indian Reservation, Arizona","interactions":[],"lastModifiedDate":"2022-09-01T18:49:29.084083","indexId":"ha55","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":"55","title":"Summary of occurrence of ground water on the Papago Indian Reservation, Arizona","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha55","usgsCitation":"Heindl, L., Cosner, O.J., Page, H.G., Armstrong, C.A., and Kister, L., 1962, Summary of occurrence of ground water on the Papago Indian Reservation, Arizona: U.S. Geological Survey Hydrologic Atlas 55, 1 Plate: 39.50 × 30.00 inches, https://doi.org/10.3133/ha55.","productDescription":"1 Plate: 39.50 × 30.00 inches","costCenters":[],"links":[{"id":186049,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":406085,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15940.htm","linkFileType":{"id":5,"text":"html"}},{"id":90371,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/055/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Arizona","otherGeospatial":"Papago Indian Reservation","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.708,\n              31.508\n            ],\n            [\n              -111.25,\n              31.508\n            ],\n            [\n              -111.25,\n              32.767\n            ],\n            [\n              -112.708,\n              32.767\n            ],\n            [\n              -112.708,\n              31.508\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db6990fa","contributors":{"authors":[{"text":"Heindl, L.A.","contributorId":52150,"corporation":false,"usgs":true,"family":"Heindl","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":278671,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cosner, O. J.","contributorId":19587,"corporation":false,"usgs":true,"family":"Cosner","given":"O.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":278670,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Page, H. G.","contributorId":82775,"corporation":false,"usgs":true,"family":"Page","given":"H.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":278674,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Armstrong, C. A.","contributorId":66231,"corporation":false,"usgs":true,"family":"Armstrong","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":278673,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kister, L. R.","contributorId":54187,"corporation":false,"usgs":true,"family":"Kister","given":"L. R.","affiliations":[],"preferred":false,"id":278672,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":68187,"text":"ha28 - 1962 - Availability of ground water in Union and Henderson Counties, Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:13:42","indexId":"ha28","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":"28","title":"Availability of ground water in Union and Henderson Counties, Kentucky","language":"ENGLISH","doi":"10.3133/ha28","usgsCitation":"Maxwell, B.W., and Devaul, R.W., 1962, Availability of ground water in Union and Henderson Counties, Kentucky: U.S. Geological Survey Hydrologic Atlas 28, 3 col. maps ;56 x 70 cm.  (Tow maps, scale 1:125,000, and generalized columnar sction.  Sheets 1 and 2, 22 by 27 inches; sheet 3, 20 by 27 inches), https://doi.org/10.3133/ha28.","productDescription":"3 col. maps ;56 x 70 cm.  (Tow maps, scale 1:125,000, and generalized columnar sction.  Sheets 1 and 2, 22 by 27 inches; sheet 3, 20 by 27 inches)","costCenters":[],"links":[{"id":185562,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89501,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/028/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89502,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/028/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89503,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/028/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"25000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db660878","contributors":{"authors":[{"text":"Maxwell, Bruce William","contributorId":67489,"corporation":false,"usgs":true,"family":"Maxwell","given":"Bruce","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":277802,"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":277803,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":52288,"text":"ofr62138 - 1962 - Preliminary evaluation of the seismicity, geology, and hydrology of the northern Sand Springs Range, Churchill County, Nevada, as a possible site for Project Shoal","interactions":[],"lastModifiedDate":"2012-02-02T00:11:21","indexId":"ofr62138","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":"62-138","title":"Preliminary evaluation of the seismicity, geology, and hydrology of the northern Sand Springs Range, Churchill County, Nevada, as a possible site for Project Shoal","language":"ENGLISH","doi":"10.3133/ofr62138","usgsCitation":"Twenhofel, W., Moore, J., and Black, R., 1962, Preliminary evaluation of the seismicity, geology, and hydrology of the northern Sand Springs Range, Churchill County, Nevada, as a possible site for Project Shoal: U.S. Geological Survey Open-File Report 62-138, 20 p., https://doi.org/10.3133/ofr62138.","productDescription":"20 p.","costCenters":[],"links":[{"id":178921,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c3b5","contributors":{"authors":[{"text":"Twenhofel, W.S.","contributorId":30613,"corporation":false,"usgs":true,"family":"Twenhofel","given":"W.S.","email":"","affiliations":[],"preferred":false,"id":245090,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, J.E.","contributorId":34927,"corporation":false,"usgs":true,"family":"Moore","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":245091,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Black, R.A.","contributorId":44230,"corporation":false,"usgs":true,"family":"Black","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":245092,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":68204,"text":"ha13 - 1962 - Reconnaissance of ground-water resources of the Jackson Purchase region, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:11:28","indexId":"ha13","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":"13","title":"Reconnaissance of ground-water resources of the Jackson Purchase region, Kentucky","language":"ENGLISH","doi":"10.3133/ha13","usgsCitation":"MacCary, L., and Lambert, T.W., 1962, Reconnaissance of ground-water resources of the Jackson Purchase region, Kentucky: U.S. Geological Survey Hydrologic Atlas 13, 1 atlas (9 p.) :ill., maps (some col.) ;70 cm.; including geologic and water availability maps at a scale of 1:250,000, https://doi.org/10.3133/ha13.","productDescription":"1 atlas (9 p.) :ill., maps (some col.) ;70 cm.; including geologic and water availability maps at a scale of 1:250,000","costCenters":[],"links":[{"id":261125,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ha/013/report.pdf"},{"id":261126,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ha/013/report-thumb.jpg"}],"scale":"500000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -89.5,36 ], [ -89.5,37.25 ], [ -88,37.25 ], [ -88,36 ], [ -89.5,36 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a68e4b07f02db63b075","contributors":{"authors":[{"text":"MacCary, L.M.","contributorId":13200,"corporation":false,"usgs":true,"family":"MacCary","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":277835,"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":277836,"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":67936,"text":"ha59 - 1962 - Floods at Mount Clemens, Michigan","interactions":[],"lastModifiedDate":"2017-02-06T16:09:17","indexId":"ha59","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":"59","title":"Floods at Mount Clemens, Michigan","docAbstract":"<p>The approximate areas inundated during the flood of April 5-6, 1947, by Clinton River, North Branch and Middle Branch of Clinton River, and Harrington Drain, in Clinton Township, Macomb County, Mich., are shown on a topographic map base to record the flood hazard in graphical form. The flood of April 1947 is the highest known since 1934 and probably since 1902. Greater floods are possible, but no attempt was made to define their probable overflow limits.</p><p>The Clinton River Cut-Off Canal, a flood-relief channel which diverts flow directly into Lake St. Clair from a point about 1500 feet downstream from Gratiot Avenue (about 9 miles upstream from the mouth) has been in operation since October 1951. The approximate limits of overflow that would results from a flood equivalent in discharge to that of April 1947, and occurring with the Cut-Off Canal in operation, are also shown. Although the Cut-Off Canal may reduce the frequency and depth of flooding it will not necessarily eliminate future flooding in the area. Improvements and additions to the drainage systems in the basin, expanding urbanization, new highways, and other cultural changes may influence the inundation pattern of future floods.</p><p>The preparation of this flood inundation map was financed through a cooperative agreement between Clinton Township, Macomb County, Mich., and the U.S. Geological Survey.</p><p>Backwater curves used to define the profile for a hypothetical flood on the Clinton River downstream from Moravian Drive, equivalent in discharge to the 1947 flood, but occurring with the present Cut-Off Canal in operation; flood stage established at the gaging station on Clinton River at Mount Clemens; and supplementary floodmark elevations were furnished by the Corps of Engineers.</p><p>Bench-mark elevations and field survey data, used in the analysis of floods on Harrington Drain, were furnished by the Macomb County Drain Commission.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/ha59","collaboration":"Prepared in cooperation with Clinton Township, Macomb County, Michigan","usgsCitation":"Wiitala, S., and Ash, A.D., 1962, Floods at Mount Clemens, Michigan: U.S. Geological Survey Hydrologic Atlas 59, Plate: 35.5 x 31.0 inches, https://doi.org/10.3133/ha59.","productDescription":"Plate: 35.5 x 31.0 inches","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":188156,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89137,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/059/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"8000","country":"United States","state":"Michigan","city":"Mount Clemens","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.973611,\n              42.626389\n            ],\n            [\n              -82.858333,\n              42.626389\n            ],\n            [\n              -82.858333,\n              42.622222\n            ],\n            [\n              -82.861667,\n              42.622222\n            ],\n            [\n              -82.865278,\n              42.541111\n            ],\n            [\n              -82.973611,\n              42.541111\n            ],\n            [\n              -82.973611,\n              42.626389\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e71ab","contributors":{"authors":[{"text":"Wiitala, S.W.","contributorId":41806,"corporation":false,"usgs":true,"family":"Wiitala","given":"S.W.","email":"","affiliations":[],"preferred":false,"id":277352,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ash, Arlington D.","contributorId":65546,"corporation":false,"usgs":true,"family":"Ash","given":"Arlington","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":277353,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68213,"text":"ha77 - 1962 - Floods at Bayamon and Catano, Puerto Rico","interactions":[],"lastModifiedDate":"2012-02-10T00:11:28","indexId":"ha77","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":"77","title":"Floods at Bayamon and Catano, Puerto Rico","language":"ENGLISH","doi":"10.3133/ha77","usgsCitation":"Lopez, M., 1962, Floods at Bayamon and Catano, Puerto Rico: U.S. Geological Survey Hydrologic Atlas 77, 1 col. map ;on sheet 80 x 104 cm. in folder 30 x 24 cm., https://doi.org/10.3133/ha77.","productDescription":"1 col. map ;on sheet 80 x 104 cm. in folder 30 x 24 cm.","costCenters":[],"links":[{"id":185627,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89563,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/077/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"20000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -66.18361111111112,18.3675 ], [ -66.18361111111112,18.483333333333334 ], [ -66.10027777777778,18.483333333333334 ], [ -66.10027777777778,18.3675 ], [ -66.18361111111112,18.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e72ea","contributors":{"authors":[{"text":"Lopez, Miguel A.","contributorId":32202,"corporation":false,"usgs":true,"family":"Lopez","given":"Miguel A.","affiliations":[],"preferred":false,"id":277851,"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":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":3197,"text":"wsp1544B - 1962 - An application of thermometry to the study of ground water","interactions":[],"lastModifiedDate":"2018-04-02T10:17:13","indexId":"wsp1544B","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":"1544","chapter":"B","title":"An application of thermometry to the study of ground water","docAbstract":"<p>Except for studies of temperature data related to ground-water developments that induce infiltration from streams, little attention has been given to the possibility of using temperature fluctuations as a tool for studying the elements of the hydrologic cycle involving ground water.</p>\n<p>The temperature of the water discharged from large installations that induce river infiltration through alluvial deposits depends primarily on the following factors: (a) the porosity of the aquifer, (b) the specific heat of the rocks or mineral grains making it up, (c) the temperature of the ground water in storage, (d) the temperature of the river water, and (e) the amount of mixing that occurs as a result of pumping. In six installations of this type, where the annual rivertemperature fluctuations ranged from 44&deg; to 52&deg;F, the average range in groundwater temperature was 22 &deg;F. The cycles of ground-water temperature lagged behind the river-temperature cycles by 1 to 5<sup>1</sup>/<sub>2</sub> months. Under the conditions that existed, the lag of the minima of the cycles was much greater than that of the maxima, largely because of variations in pumpage and of the effect of viscosity differences on the rate of flow.</p>\n<p>An experimental study was made at Worthington in southwestern Minnesota to determine whether temperature fluctuations could be used to study rates and directions of ground-water movement or to evaluate recharge conditions. Three shallow glacial-outwash aquifers were studied by measuring temperatures at approximately monthly intervals in three municipal-supply wells whose average yields were about 60 to 150 gpm (gallons per minute). Temperatures were read with an accuracy of 0.01&deg; to 0.02&deg;C, and the data were analyzed graphically and correlated in detail with lake levels, lake temperatures, precipitation, and groundwater levels.</p>\n<p>Thermographs for 2 wells, 1 completed in a semiconfined aquifer about 200 feet from Okabena Lake and the other in a water-table aquifer about 850 feet from the lake, indicate that pumping induces water to move from the lake into the aquifers. A larger percentage of cold lake water was mixed with ground water from January to March 1958 than from January to March 1959. On the assumption that the cold or warm lake water was a distinct mass, the average time required for water to move from the lake to the well 200 feet away, under the prevailing hydraulic gradient, was 2 to 4 months; and to the well 850 feet away, 5 to 7 months.</p>\n<p>The thermograph for a well 1,800 feet from the lake, completed in an artesian aquifer that is confined by relatively impervious glacial till, indicates that the till acts as an insulating medium. However, despite the apparently low permeability of the till, the thermograph suggests that the lowering of artesian pressure, which results from pumping, induces warmer water to move downward through the till.</p>\n<p>The infiltration of relatively warm spring and summer rainfall can be detected on the thermographs of all the wells.</p>\n<p>The precise measurement of fluctuations in ground-water temperature, based on monthly readings in shallow glacial-outwash aquifers (up to about 70 feet deep), is useful in the study of ground-water movement and recharge. In addition to the study of natural phenomena in the hydrologic cycle, thermometry may be used as a tool in making detailed studies of (1) the effects of inducing the infiltration of surface water, (2) artificial recharge, (3) the effects of injecting petroleum products or radioactive or other wastes into the ground, and (4) ground-water movement in mines.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1544B","collaboration":"Prepared in cooperation with the Division of Waters, Minnesota Department of Conservation","usgsCitation":"Schneider, R., 1962, An application of thermometry to the study of ground water: U.S. Geological Survey Water Supply Paper 1544, Document: iii, 16 p.; 2 Plates: 16 x 12 inches and 16 x 17 inches, https://doi.org/10.3133/wsp1544B.","productDescription":"Document: iii, 16 p.; 2 Plates: 16 x 12 inches and 16 x 17 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":30184,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1544b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":30182,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1544b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":30183,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1544b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138321,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1544b/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db68571e","contributors":{"authors":[{"text":"Schneider, Robert","contributorId":102460,"corporation":false,"usgs":true,"family":"Schneider","given":"Robert","email":"","affiliations":[],"preferred":false,"id":146417,"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":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":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":32719,"text":"pp450D - 1962 - Short papers in geology, hydrology, and topography; articles 120-179","interactions":[],"lastModifiedDate":"2025-01-21T22:12:20.378505","indexId":"pp450D","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":"450","chapter":"D","title":"Short papers in geology, hydrology, and topography; articles 120-179","docAbstract":"<p>This collection of 60 short papers on subjects in the fields of geology, hydrology, topography, and related sciences is the third of a series to be released during the year as chapters of Professional Paper 450. The papers in this chapter report on the scientific and economic results of current work by members of the Geologic, Water Resources, and Topographic Divisions of the United States Geologicai Survey. Some of the papers announce new discoveries or present observations on problems of limited scope; other papers draw conclusions from more extensive or continuing investigations that in large part will be discussed in greater detail in reports to be published in the future.</p><p>Chapter A of this series, to be published later in the year, will present a synopsis of results from a wide range of work done during the present fiscal year. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/pp450D","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1962, Short papers in geology, hydrology, and topography; articles 120-179: U.S. Geological Survey Professional Paper 450, vi, 194 p., https://doi.org/10.3133/pp450D.","productDescription":"vi, 194 p.","numberOfPages":"201","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true},{"id":610,"text":"Utah Water Science 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Arizona","linkFileType":{"id":5,"text":"html"}},{"id":480876,"rank":22,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28317.htm","text":"Gravity, volcanism, and crustal deformation in the eastern Snake River Plain, Idaho","linkFileType":{"id":5,"text":"html"}},{"id":480877,"rank":23,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28318.htm","text":"Geohydrologic evidence of a buried fault in the Erda area, Tooele Valley, Utah","linkFileType":{"id":5,"text":"html"}},{"id":480878,"rank":24,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28319.htm","text":"Restudy of the Arrowhead fault, Muddy Mountains, Nevada","linkFileType":{"id":5,"text":"html"}},{"id":480879,"rank":25,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28320.htm","text":"Correlation of granitic plutons across faulted Owens Valley, California","linkFileType":{"id":5,"text":"html"}},{"id":480880,"rank":26,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28321.htm","text":"Structural control of interior drainage, southern San Joaquin Valley, California","linkFileType":{"id":5,"text":"html"}},{"id":480881,"rank":27,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28322.htm","text":"Zinc occurrence in the Serpent Mound structure of southern Ohio","linkFileType":{"id":5,"text":"html"}},{"id":480882,"rank":28,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28323.htm","text":"Faulted Pleistocene strata near Jackson, northwestern Wyoming","linkFileType":{"id":5,"text":"html"}},{"id":480883,"rank":29,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28324.htm","text":"Potential yield of deep water wells in the southern part of the Jicarilla Apache Indian Reservation and vicinity, San Juan Basin, New Mexico","linkFileType":{"id":5,"text":"html"}},{"id":480859,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28300.htm","text":"Precambrian(?) and Cambrian stratigraphy in Esmeralda County, Nevada","linkFileType":{"id":5,"text":"html"}},{"id":480860,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28301.htm","text":"Age and sequence of metasedimentary and metavolcanic formations northwest of New Haven, Connecticut","linkFileType":{"id":5,"text":"html"}},{"id":480861,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28302.htm","text":"The Eagle Valley Evaporite and its relation to the Minturn and Maroon Formations, northwest Colorado","linkFileType":{"id":5,"text":"html"}},{"id":480862,"rank":8,"type":{"id":36,"text":"NGMDB Index 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Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28312.htm","text":"Precambrian gabbro in the central Front Range, Colorado [Keyser Creek area]","linkFileType":{"id":5,"text":"html"}},{"id":480872,"rank":18,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28313.htm","text":"Precambrian gabbro in the central Front Range, Colorado [Apex area]","linkFileType":{"id":5,"text":"html"}},{"id":480873,"rank":19,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28314.htm","text":"Configuration of the bedrock beneath the channel of the lower Merrimack River, Massachusetts","linkFileType":{"id":5,"text":"html"}},{"id":480874,"rank":20,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28315.htm","text":"Geology of Pleistocene deposits of Lake County, Indiana","linkFileType":{"id":5,"text":"html"}},{"id":480875,"rank":21,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28316.htm","text":"Geology of the Vermilion end moraine, Nett Lake Indian Reservation, Minnesota","linkFileType":{"id":5,"text":"html"}},{"id":480884,"rank":30,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_93398.htm","text":"The pre-Bull Lake tills in the Wind River Mountains, Wyoming","linkFileType":{"id":5,"text":"html"}},{"id":480885,"rank":31,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_93399.htm","text":"Cambrian Carrara Formation, Bonanza King Formation, and Dunderberg Shale east of Yucca Flat, Nye County, Nevada","linkFileType":{"id":5,"text":"html"}},{"id":480886,"rank":32,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_93405.htm","text":"Age of the Leadville Limestone in the Glenwood Canyon, western Colorado","linkFileType":{"id":5,"text":"html"}},{"id":480887,"rank":33,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_100150.htm","text":"New members of the Bloyd Formation of Pennsylvanian age, Washington County, Arkansas","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f3f29","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":529442,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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":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":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":32648,"text":"pp500B - 1962 - Geomorphology and general systems theory","interactions":[],"lastModifiedDate":"2012-02-02T00:09:09","indexId":"pp500B","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":"500","chapter":"B","title":"Geomorphology and general systems theory","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Theoretical papers in the hydrologic and geomorphic sciences","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp500B","usgsCitation":"Chorley, R., 1962, Geomorphology and general systems theory: U.S. Geological Survey Professional Paper 500, p. B1-B10, https://doi.org/10.3133/pp500B.","productDescription":"p. B1-B10","costCenters":[],"links":[{"id":160516,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0500b/report-thumb.jpg"},{"id":21957,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0500b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c494","contributors":{"authors":[{"text":"Chorley, R.J.","contributorId":75807,"corporation":false,"usgs":true,"family":"Chorley","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":208855,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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":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":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":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}]}}
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