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,{"id":4,"text":"wsp1659 - 1964 - An appraisal of potential ground-water salvage along the Pecos River between Acme and Artesia, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:05:10","indexId":"wsp1659","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1659","title":"An appraisal of potential ground-water salvage along the Pecos River between Acme and Artesia, New Mexico","language":"ENGLISH","publisher":"U.S. Department of the Interior, Geological Survey ;","doi":"10.3133/wsp1659","isbn":"pbk","usgsCitation":"Mower, R.W., Hood, J.W., Cushman, R., Borton, R., and Galloway, S., 1964, An appraisal of potential ground-water salvage along the Pecos River between Acme and Artesia, New Mexico: U.S. Geological Survey Water Supply Paper 1659, viii, 98 p. :ill., maps, tables ;24 cm., https://doi.org/10.3133/wsp1659.","productDescription":"viii, 98 p. :ill., maps, tables ;24 cm.","costCenters":[],"links":[{"id":110004,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24851.htm","linkFileType":{"id":5,"text":"html"},"description":"24851"},{"id":136272,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1659/report-thumb.jpg"},{"id":246944,"rank":415,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1659/plate-09_sheet_1.pdf","size":"2196","linkFileType":{"id":1,"text":"pdf"}},{"id":246945,"rank":416,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1659/plate-09_sheet_2.pdf","size":"2513","linkFileType":{"id":1,"text":"pdf"}},{"id":246946,"rank":417,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1659/plate-09_sheet_3.pdf","size":"2573","linkFileType":{"id":1,"text":"pdf"}},{"id":246947,"rank":418,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1659/plate-09_sheet_4.pdf","size":"1841","linkFileType":{"id":1,"text":"pdf"}},{"id":246948,"rank":419,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1659/plate-09_sheet_5.pdf","size":"2392","linkFileType":{"id":1,"text":"pdf"}},{"id":246949,"rank":420,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1659/plate-09_sheet_6.pdf","size":"2121","linkFileType":{"id":1,"text":"pdf"}},{"id":24588,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1659/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24589,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1659/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24590,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1659/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24591,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1659/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24592,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1659/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24593,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1659/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24594,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1659/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24595,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1659/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24596,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1659/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24597,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1659/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db6856c7","contributors":{"authors":[{"text":"Mower, Reed W.","contributorId":32503,"corporation":false,"usgs":true,"family":"Mower","given":"Reed","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":141790,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hood, J. W.","contributorId":87908,"corporation":false,"usgs":true,"family":"Hood","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":141793,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cushman, R.L.","contributorId":102859,"corporation":false,"usgs":true,"family":"Cushman","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":141794,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Borton, R.L.","contributorId":75895,"corporation":false,"usgs":true,"family":"Borton","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":141791,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Galloway, S.E.","contributorId":85151,"corporation":false,"usgs":true,"family":"Galloway","given":"S.E.","email":"","affiliations":[],"preferred":false,"id":141792,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":68553,"text":"ha82 - 1964 - Water-table, surface-drainage, and engineering soils map of the Middletown area, Delaware","interactions":[],"lastModifiedDate":"2021-11-04T21:32:37.899859","indexId":"ha82","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"82","title":"Water-table, surface-drainage, and engineering soils map of the Middletown area, Delaware","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha82","usgsCitation":"Boggess, D.H., and Adams, J.K., 1964, Water-table, surface-drainage, and engineering soils map of the Middletown area, Delaware: U.S. Geological Survey Hydrologic Atlas 82, 1 Plate: 46.00 × 28.50 inches, https://doi.org/10.3133/ha82.","productDescription":"1 Plate: 46.00 × 28.50 inches","costCenters":[],"links":[{"id":188886,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":391404,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_16180.htm"},{"id":90181,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/082/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Delaware","otherGeospatial":"Middletown area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -75.75,\n              39.375\n            ],\n            [\n              -75.625,\n              39.375\n            ],\n            [\n              -75.625,\n              39.5\n            ],\n            [\n              -75.75,\n              39.5\n            ],\n            [\n              -75.75,\n              39.375\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f99d6","contributors":{"authors":[{"text":"Boggess, Durward H.","contributorId":28650,"corporation":false,"usgs":true,"family":"Boggess","given":"Durward","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":278449,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Adams, John K.","contributorId":17700,"corporation":false,"usgs":true,"family":"Adams","given":"John","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":278448,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61731,"text":"gq267 - 1964 - Geology of the Central City quadrangle, Colorado","interactions":[],"lastModifiedDate":"2021-11-10T20:29:08.953648","indexId":"gq267","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"267","title":"Geology of the Central City quadrangle, Colorado","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gq267","usgsCitation":"Sims, P., 1964, Geology of the Central City quadrangle, Colorado: U.S. Geological Survey Geologic Quadrangle 267, Report: 1 p.; Plate, https://doi.org/10.3133/gq267.","productDescription":"Report: 1 p.; Plate","costCenters":[],"links":[{"id":102273,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_722.htm","linkFileType":{"id":5,"text":"html"},"description":"722"},{"id":248029,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0267/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":252689,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0267/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Colorado","otherGeospatial":"Central City quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.625,39.75 ], [ -105.625,39.875 ], [ -105.5,39.875 ], [ -105.5,39.75 ], [ -105.625,39.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ae4b07f02db69d125","contributors":{"authors":[{"text":"Sims, P.K.","contributorId":30191,"corporation":false,"usgs":true,"family":"Sims","given":"P.K.","email":"","affiliations":[],"preferred":false,"id":266291,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61634,"text":"gq302 - 1964 - Geology of the Constantine quadrangle, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:35","indexId":"gq302","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"302","title":"Geology of the Constantine quadrangle, Kentucky","language":"ENGLISH","doi":"10.3133/gq302","usgsCitation":"Sable, E.G., 1964, Geology of the Constantine quadrangle, Kentucky: U.S. Geological Survey Geologic Quadrangle 302, 1 map., https://doi.org/10.3133/gq302.","productDescription":"1 map.","costCenters":[],"links":[{"id":102313,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_762.htm","linkFileType":{"id":5,"text":"html"},"description":"762"},{"id":247938,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0302/report.pdf","size":"35","linkFileType":{"id":1,"text":"pdf"}},{"id":252515,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0302/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -86.25,37.6175 ], [ -86.25,37.75 ], [ -86.11749999999999,37.75 ], [ -86.11749999999999,37.6175 ], [ -86.25,37.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db68309d","contributors":{"authors":[{"text":"Sable, Edward G.","contributorId":51273,"corporation":false,"usgs":true,"family":"Sable","given":"Edward","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":266169,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1258,"text":"wsp1618 - 1964 - Use of ground-water reservoirs for storage of surface water in the San Joaquin Valley, California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:13","indexId":"wsp1618","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1618","title":"Use of ground-water reservoirs for storage of surface water in the San Joaquin Valley, California","docAbstract":"The San Joaquin Valley includes roughly the southern two-thirds of the Central Valley of California, extending 250 miles from Stockton on the north to Grapevine at the foot of the Tehachapi Mountains. The valley floor ranges in width from 25 miles near Bakersfield to about 55 miles near Visalia; it has a surface area of about 10,000 square miles. More than one-quarter of all the ground water pumped for irrigation in the United States is used in this highly productive valley. Withdrawal of ground water from storage by heavy pumping not only provides a needed irrigation water supply, but it also lowers the ground-water level and makes storage space available in which to conserve excess water during periods of heavy runoff. A storage capacity estimated to be 93 million acre-feet to a depth of 200 feet is available in this ground-water reservoir. This is about nine times the combined capacity of the existing and proposed surface-water reservoirs in the San Joaquin Valley under the California Water Plan.\r\n\r\nThe landforms of the San Joaquin Valley include dissected uplands, low plains and fans, river flood plains and channels, and overflow lands and lake bottoms. Below the land surface, unconsolidated sediments derived from the surrounding mountain highlands extend downward for hundreds of feet. These unconsolidated deposits, consisting chiefly of alluvial deposits, but including some widespread lacustrine sediments, are the principal source of ground water in the valley. Ground water occurs under confined and unconfined conditions in the San Joaquin Valley. In much of the western, central, and southeastern parts of the valley, three distinct ground-water reservoirs are present. In downward succession these are 1) a body of unconfined and semiconfined fresh water in alluvial deposits of Recent, Pleistocene, and possibly later Pliocene age, overlying the Corcoran clay member of the Tulare formation; 2) a body of fresh water confined beneath the Corcoran clay member, which occurs in alluvial and lacustrine deposits of late Pliocene age or older; and 3) a body of saline connate water contained in marine sediments of middle Pliocene or older age, which underlies the fresh-water body throughout the area. In much of the eastern part of the valley, especially in the areas of the major streams, the Corcoran clay member is not present and ground water occurs as one fresh-water body to considerable depth.\r\n\r\nThe ground-water body is replenished by infiltration of rainfall, by infiltration from streams, canals, and ditches, by underflow entering the valley from tributary stream canyons, and by infiltration of excess irrigation water. In much of the valley, however, the annual rainfall is so low that little penetrates deeply, and soil-moisture deficiency is perennial. Infiltration from stream channels and canals and from irrigated fields are the principal sources of groundwater recharge. The ground-water storage capacity of the San Joaquin Valley has been estimated in an earlier report (Davis and others, 1959) as 93 million acre-feet. This is the quantity of water that would drain by gravity from the valley deposits if the regional water level were lowered from 10 to 200 feet below the land surface. Storage capacity was estimated for only the part of the valley considered to be potentially usable as a ground-water reservoir. In this study, a 200foot depth was selected as a practical valley-wide depth limit for unwatering \r\n\r\nunder full utilization of the ground-water reservoir, even though in localized areas sections in excess of 350 feet in depth have already been dewatered. Some of the factors that locally limit the utilization of the ground-water reservoir are inferior water quality, relatively impermeable surface soils, and relatively impermeable subsurface deposits. On the basis of a detailed analysis of la peg model, the subsurface geology of the San Joaquin Valley was subdivided into predominantly permeable and impermeable zones in the 1","language":"ENGLISH","publisher":"United States Govt. Print. Off.,","doi":"10.3133/wsp1618","usgsCitation":"Davis, G.H., Lofgren, B.E., and Mack, S., 1964, Use of ground-water reservoirs for storage of surface water in the San Joaquin Valley, California: U.S. Geological Survey Water Supply Paper 1618, vii, 125 p. :illus., maps, diagrs., tables. and portfolio ;24 cm., https://doi.org/10.3133/wsp1618.","productDescription":"vii, 125 p. :illus., maps, diagrs., tables. and portfolio ;24 cm.","costCenters":[],"links":[{"id":137412,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1618/report-thumb.jpg"},{"id":26195,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1618/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26196,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1618/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26197,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1618/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26198,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1618/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26199,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1618/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26200,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1618/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26201,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1618/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26202,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1618/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26203,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1618/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26204,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1618/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26205,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1618/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26206,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1618/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604592","contributors":{"authors":[{"text":"Davis, G. H.","contributorId":40963,"corporation":false,"usgs":true,"family":"Davis","given":"G.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":143449,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lofgren, B. E.","contributorId":42579,"corporation":false,"usgs":true,"family":"Lofgren","given":"B.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":143450,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mack, Seymour","contributorId":101247,"corporation":false,"usgs":true,"family":"Mack","given":"Seymour","email":"","affiliations":[],"preferred":false,"id":143451,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":61735,"text":"gq312 - 1964 - Geology of the Portsmouth quadrangle, Kentucky-Ohio, and parts of the Wheelersburg and New Boston quadrangles, Kentucky","interactions":[],"lastModifiedDate":"2022-12-27T20:42:12.709598","indexId":"gq312","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"312","title":"Geology of the Portsmouth quadrangle, Kentucky-Ohio, and parts of the Wheelersburg and New Boston quadrangles, Kentucky","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gq312","usgsCitation":"Sheppard, R.A., 1964, Geology of the Portsmouth quadrangle, Kentucky-Ohio, and parts of the Wheelersburg and New Boston quadrangles, Kentucky: U.S. Geological Survey Geologic Quadrangle 312, Report: 1 p.; 1 Plate: 35.79 x 32.76 inches, https://doi.org/10.3133/gq312.","productDescription":"Report: 1 p.; 1 Plate: 35.79 x 32.76 inches","costCenters":[],"links":[{"id":252693,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0312/report-thumb.jpg"},{"id":248033,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0312/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":102324,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_773.htm","linkFileType":{"id":5,"text":"html"},"description":"773"}],"scale":"24000","country":"United States","state":"Kentucky, Ohio","otherGeospatial":"Portsmouth quadrangle, Wheelersburg and New Boston quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83,\n              38.625\n            ],\n            [\n              -83,\n              38.75\n            ],\n            [\n              -82.8694,\n              38.75\n            ],\n            [\n              -82.8694,\n              38.625\n            ],\n            [\n              -83,\n              38.625\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e8aa","contributors":{"authors":[{"text":"Sheppard, Richard A.","contributorId":41815,"corporation":false,"usgs":true,"family":"Sheppard","given":"Richard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":266298,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":97,"text":"wsp1781 - 1964 - Ground-water levels in the United States, 1957-61, North-central states","interactions":[],"lastModifiedDate":"2012-02-02T00:05:10","indexId":"wsp1781","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1781","title":"Ground-water levels in the United States, 1957-61, North-central states","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1781","usgsCitation":"Hackett, O.M., 1964, Ground-water levels in the United States, 1957-61, North-central states: U.S. Geological Survey Water Supply Paper 1781, v, 148 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1781.","productDescription":"v, 148 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":136215,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1781/report-thumb.jpg"},{"id":24703,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1781/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6675b6","contributors":{"authors":[{"text":"Hackett, O. M.","contributorId":38527,"corporation":false,"usgs":true,"family":"Hackett","given":"O.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":141925,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2253,"text":"wsp1777 - 1964 - Geology and ground-water resources of Washington County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:05:19","indexId":"wsp1777","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1777","title":"Geology and ground-water resources of Washington County, Colorado","docAbstract":"Washington County, in northeastern Colorado, has an area of 2,520 square miles. The eastern two-thirds of the county, part of the High Plains physiographic section, is relatively flat and has been moderately altered by the deposition of loess and dune sand, and by stream erosion. The western one-third is a part of the South Platte River basin and has been deeply dissected by tributary streams. The soils and climate of the county are generally suited for agriculture, which is the principal industry. \r\n\r\nThe rocks that crop out in the county influence the availability of ground water. The Pierre Shale, of Late Cretaceous age, underlies the entire area and ranges in thickness from 2,000 to 4,500 feet. This dense shale is a barrier to the downward movement of water and yields little or no water to wells. The Chadron Formation, of Oligocene age, overlies the Pierre Shale in the northern and central parts of the area. The thickness of the formation ranges from a few feet to about 300 feet. Small to moderate quantities of water are available from the scattered sand lenses and from the highly fractured zones of the siltstone. The Ogallala Formation, of Pliocene age, overlies the Chadron Formation and in Washington County forms the High Plains section of the Great Plains province. The thickness of the Ogallala Formation ranges from 0 to about 400 feet, and the yield from wells ranges from a few gallons per hour to about 1,500 gpm. Peorian loess, of Pleistocene age, and dune sand, of Pleistocene to Recent age, mantle a large pan of the county and range in thickness from a few inches to about 120 feet Although the loess and dune sand yield little water to wells, they absorb much of the precipitation and conduct the water to underlying formations. Alluvium, of Pleistocene and Recent age, occupies most of the major stream valleys in thicknesses of a few feet to about 250 feet. The yield of wells tapping the alluvium ranges from a few gallons per minute to about 3,000 gpm, according to the thickness of saturated material. \r\n\r\nDevelopment of ground water for irrigation has been generally restricted to the South Platte, Arikaree, and Beaver valleys. There were 134 irrigation wells, 3 industrial wells, and 10 municipal wells in the county in 1959. The annual ground-water pumpage from Washington County is estimated to be 18,000 acre-ft; about 10,000 acre-ft is from the High Plains ground-water province. Although some ground water enters the county as underflow, most of the recharge to ground-water reservoirs is from precipitation on the land surface. Recharge to the Ogallala Formation in the county is assumed to be approximately equal to the natural discharge from the county by underflow because ground-water withdrawals are from storage, and no other significant amount of natural discharge is apparent. Undertow in the Ogallala was calculated to be 83,000 acre-ft per year and the rate of recharge from precipitation to be about 0.95 inch per year. Neither recharge nor discharge was calculated for that part of the county in the South Platte River basin. \r\n\r\nAll ground water in Washington County has a high proportion of carbonate and is classed as hard to very hard. The sodium-adsorption-ratio for all samples analyzed was below the limit recommended for irrigation water. All the water from the Ogallala Formation and most of the water from the Chadron Formation is suitable for domestic use. Some water from the alluvial deposits overlying the Pierre Shale was exceptionally high in calcium, magnesium, and sodium sulfates. \r\n\r\nGround water has been heavily developed for irrigation in the South Platte valley and in some parts of the Beaver and Arikaree valleys. Some additional areas, however, could be developed in the latter two valleys. Large quantities of ground water in the Ogallala Formation are available for future development. The quantity of water in storage in the High Plains ground-water province in Washington County is about 6.5 million acre-f","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/wsp1777","usgsCitation":"McGovern, H.E., 1964, Geology and ground-water resources of Washington County, Colorado: U.S. Geological Survey Water Supply Paper 1777, iv, 46 p. :illus., maps (4 fold. 1 col., in pocket) ;24 cm., https://doi.org/10.3133/wsp1777.","productDescription":"iv, 46 p. :illus., maps (4 fold. 1 col., in pocket) ;24 cm.","costCenters":[],"links":[{"id":110015,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24953.htm","linkFileType":{"id":5,"text":"html"},"description":"24953"},{"id":137835,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1777/report-thumb.jpg"},{"id":28024,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1777/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28025,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1777/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28026,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1777/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28027,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1777/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28028,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1777/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db68580b","contributors":{"authors":[{"text":"McGovern, Harold E.","contributorId":9634,"corporation":false,"usgs":true,"family":"McGovern","given":"Harold","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":144901,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61736,"text":"gq289 - 1964 - Geology of the Tygarts Valley quadrangle, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:49","indexId":"gq289","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"289","title":"Geology of the Tygarts Valley quadrangle, Kentucky","language":"ENGLISH","doi":"10.3133/gq289","usgsCitation":"Sheppard, R.A., 1964, Geology of the Tygarts Valley quadrangle, Kentucky: U.S. Geological Survey Geologic Quadrangle 289, 1 map., https://doi.org/10.3133/gq289.","productDescription":"1 map.","costCenters":[],"links":[{"id":102297,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_746.htm","linkFileType":{"id":5,"text":"html"},"description":"746"},{"id":248034,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0289/report.pdf","size":"31","linkFileType":{"id":1,"text":"pdf"}},{"id":252694,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0289/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -83.11749999999999,38.3675 ], [ -83.11749999999999,38.5 ], [ -83,38.5 ], [ -83,38.3675 ], [ -83.11749999999999,38.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67ca77","contributors":{"authors":[{"text":"Sheppard, Richard A.","contributorId":41815,"corporation":false,"usgs":true,"family":"Sheppard","given":"Richard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":266299,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15272,"text":"ofr64122 - 1964 - Geology applied to study of coal mine bumps and mining methods at Sunnyside, Utah","interactions":[],"lastModifiedDate":"2025-06-17T13:45:06.390094","indexId":"ofr64122","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"64-122","title":"Geology applied to study of coal mine bumps and mining methods at Sunnyside, Utah","docAbstract":"<p>Coal mine bumps are a serious hazard to life and property in the mines of east-central Utah. Research into geologic factors associated with these bumps indicates that the bumps are spatially and genetically related to structural and stratigraphic features. Some bumps are directly related to stress accumulation along faults, either from natural causes or as a result of mining. Frictional properties of bedding planes between coal and roof rock, and between some rock units within the roof, directly affect the deformation of coal ribs, and hence the incidence of bumps. These frictional properties are related to the lithology of the roof rocks as well as to the sedimentary structures within the rocks. Commonly a sequence consisting of 1- 3 ft of carbonaceous siltstone, about 2- 3 ft of rider coal, and several feet of massive siltstone or sandstone overlies the main seam. The sequence causes difficult roof conditions in the mines, difficult mining conditions, and directly or indirectly many bumps.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr64122","usgsCitation":"Osterwald, F.W., and Dunrud, C., 1964, Geology applied to study of coal mine bumps and mining methods at Sunnyside, Utah: U.S. Geological Survey Open-File Report 64-122, 8 p., https://doi.org/10.3133/ofr64122.","productDescription":"8 p.","costCenters":[],"links":[{"id":490818,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1964/0122/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148173,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1964/0122/report-thumb.jpg"}],"country":"United States","state":"Utah","city":"Sunnyside","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"id\":\"47\",\"properties\":{\"name\":\"Utah\",\"nation\":\"USA  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,{"id":15043,"text":"ofr64116 - 1964 - Lithologic and radioactivity log of Summit area drill hole, Hardin County, Kentucky","interactions":[],"lastModifiedDate":"2024-08-05T21:55:44.420525","indexId":"ofr64116","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"64-116","title":"Lithologic and radioactivity log of Summit area drill hole, Hardin County, Kentucky","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr64116","usgsCitation":"Moore, F.R., 1964, Lithologic and radioactivity log of Summit area drill hole, Hardin County, Kentucky: U.S. Geological Survey Open-File Report 64-116, Report: 6 p.; 1 Plate: 3.34 x 10.76 inches, https://doi.org/10.3133/ofr64116.","productDescription":"Report: 6 p.; 1 Plate: 3.34 x 10.76 inches","costCenters":[],"links":[{"id":432240,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0116/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":432239,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1964/0116/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148376,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1964/0116/report-thumb.jpg"}],"country":"United States","state":"Kentucky","county":"Hardin County","otherGeospatial":"Summit area drill hole","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -86.1454050949599,\n              37.98329253965666\n            ],\n            [\n              -86.1454050949599,\n              37.5535129289011\n            ],\n            [\n              -85.67869624898441,\n              37.5535129289011\n            ],\n            [\n              -85.67869624898441,\n              37.98329253965666\n            ],\n            [\n              -86.1454050949599,\n              37.98329253965666\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fc270","contributors":{"authors":[{"text":"Moore, Frank R.","contributorId":54582,"corporation":false,"usgs":false,"family":"Moore","given":"Frank","email":"","middleInitial":"R.","affiliations":[{"id":12981,"text":"Department of Biological Sciences, University of Southern Mississippi","active":true,"usgs":false}],"preferred":false,"id":170470,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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