{"pageNumber":"6653","pageRowStart":"166300","pageSize":"25","recordCount":184900,"records":[{"id":63556,"text":"gp491 - 1965 - Aeromagnetic map of the Columbus-Dayton area, Ohio and Indiana","interactions":[],"lastModifiedDate":"2012-02-10T00:10:43","indexId":"gp491","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"491","title":"Aeromagnetic map of the Columbus-Dayton area, Ohio and Indiana","language":"ENGLISH","doi":"10.3133/gp491","usgsCitation":"Philbin, P.W., Long, C.L., and Moore, F., 1965, Aeromagnetic map of the Columbus-Dayton area, Ohio and Indiana: U.S. Geological Survey Geophysical Investigations Map 491, 1 map ;52 x 106 cm., https://doi.org/10.3133/gp491.","productDescription":"1 map ;52 x 106 cm.","costCenters":[],"links":[{"id":253277,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0491/report-thumb.jpg"},{"id":249724,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0491/report.pdf","size":"31","linkFileType":{"id":1,"text":"pdf"}},{"id":249725,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0491/plate-1.pdf","size":"9960","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -85.25,39.3675 ], [ -85.25,42.5 ], [ -82.25,42.5 ], [ -82.25,39.3675 ], [ -85.25,39.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696d82","contributors":{"authors":[{"text":"Philbin, P. W.","contributorId":25915,"corporation":false,"usgs":true,"family":"Philbin","given":"P.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":269121,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Long, C. L.","contributorId":98699,"corporation":false,"usgs":true,"family":"Long","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":269122,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moore, F.C. Jr.","contributorId":105795,"corporation":false,"usgs":true,"family":"Moore","given":"F.C.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":269123,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":63030,"text":"gq412 - 1965 - Geology of the Cadiz quadrangle, Trigg County, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:46","indexId":"gq412","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"412","title":"Geology of the Cadiz quadrangle, Trigg County, Kentucky","language":"ENGLISH","doi":"10.3133/gq412","usgsCitation":"Fox, K., 1965, Geology of the Cadiz quadrangle, Trigg County, Kentucky: U.S. Geological Survey Geologic Quadrangle 412, 1 map., https://doi.org/10.3133/gq412.","productDescription":"1 map.","costCenters":[],"links":[{"id":102431,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_880.htm","linkFileType":{"id":5,"text":"html"},"description":"880"},{"id":249162,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0412/report.pdf","size":"35","linkFileType":{"id":1,"text":"pdf"}},{"id":252163,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0412/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87.86749999999999,36.75 ], [ -87.86749999999999,36.8675 ], [ -87.75,36.8675 ], [ -87.75,36.75 ], [ -87.86749999999999,36.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db683271","contributors":{"authors":[{"text":"Fox, Kenneth F.","contributorId":29804,"corporation":false,"usgs":true,"family":"Fox","given":"Kenneth F.","affiliations":[],"preferred":false,"id":268220,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":63159,"text":"gq379 - 1965 - Geology of the Mount Aire quadrangle, Salt Lake County, Utah","interactions":[],"lastModifiedDate":"2012-02-10T00:10:43","indexId":"gq379","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"379","title":"Geology of the Mount Aire quadrangle, Salt Lake County, Utah","language":"ENGLISH","doi":"10.3133/gq379","usgsCitation":"Crittenden, M., 1965, Geology of the Mount Aire quadrangle, Salt Lake County, Utah: U.S. Geological Survey Geologic Quadrangle 379, 1 map., https://doi.org/10.3133/gq379.","productDescription":"1 map.","costCenters":[],"links":[{"id":102393,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_842.htm","linkFileType":{"id":5,"text":"html"},"description":"842"},{"id":249280,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0379/report.pdf","size":"28","linkFileType":{"id":1,"text":"pdf"}},{"id":252596,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0379/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.75,40.6175 ], [ -111.75,40.75 ], [ -111.61749999999999,40.75 ], [ -111.61749999999999,40.6175 ], [ -111.75,40.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e977","contributors":{"authors":[{"text":"Crittenden, Max D.","contributorId":43404,"corporation":false,"usgs":true,"family":"Crittenden","given":"Max D.","affiliations":[],"preferred":false,"id":268421,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52450,"text":"ofr6533 - 1965 - New Mexico State Planning Office Report - Western closed basins","interactions":[{"subject":{"id":52450,"text":"ofr6533 - 1965 - New Mexico State Planning Office Report - Western closed basins","indexId":"ofr6533","publicationYear":"1965","noYear":false,"title":"New Mexico State Planning Office Report - Western closed basins"},"predicate":"SUPERSEDED_BY","object":{"id":70046983,"text":"70046983 - 1967 - Water resources of New Mexico: occurrence, development, and use","indexId":"70046983","publicationYear":"1967","noYear":false,"title":"Water resources of New Mexico: occurrence, development, and use"},"id":1}],"supersededBy":{"id":70046983,"text":"70046983 - 1967 - Water resources of New Mexico: occurrence, development, and use","indexId":"70046983","publicationYear":"1967","noYear":false,"title":"Water resources of New Mexico: occurrence, development, and use"},"lastModifiedDate":"2013-07-15T13:43:42","indexId":"ofr6533","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-33","title":"New Mexico State Planning Office Report - Western closed basins","language":"ENGLISH","doi":"10.3133/ofr6533","usgsCitation":"Cooper, J., 1965, New Mexico State Planning Office Report - Western closed basins: U.S. Geological Survey Open-File Report 65-33, 25 p., https://doi.org/10.3133/ofr6533.","productDescription":"25 p.","costCenters":[],"links":[{"id":100183,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1965/0033/report.pdf","size":"13555","linkFileType":{"id":1,"text":"pdf"}},{"id":179272,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1965/0033/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697948","contributors":{"authors":[{"text":"Cooper, J.B.","contributorId":92316,"corporation":false,"usgs":true,"family":"Cooper","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":245363,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52476,"text":"ofr6587 - 1965 - The Area B flood-control plan--its influence on the future water resources of the Miami area, Florida","interactions":[{"subject":{"id":52476,"text":"ofr6587 - 1965 - The Area B flood-control plan--its influence on the future water resources of the Miami area, Florida","indexId":"ofr6587","publicationYear":"1965","noYear":false,"title":"The Area B flood-control plan--its influence on the future water resources of the Miami area, Florida"},"predicate":"SUPERSEDED_BY","object":{"id":70046926,"text":"70046926 - 1967 - Hydrologic effects of area B flood control plan on urbanization of Dade County, Florida","indexId":"70046926","publicationYear":"1967","noYear":false,"title":"Hydrologic effects of area B flood control plan on urbanization of Dade County, Florida"},"id":1}],"supersededBy":{"id":70046926,"text":"70046926 - 1967 - Hydrologic effects of area B flood control plan on urbanization of Dade County, Florida","indexId":"70046926","publicationYear":"1967","noYear":false,"title":"Hydrologic effects of area B flood control plan on urbanization of Dade County, Florida"},"lastModifiedDate":"2013-07-09T13:38:52","indexId":"ofr6587","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-87","title":"The Area B flood-control plan--its influence on the future water resources of the Miami area, Florida","language":"ENGLISH","doi":"10.3133/ofr6587","usgsCitation":"Kohout, F.A., and Hartwell, J., 1965, The Area B flood-control plan--its influence on the future water resources of the Miami area, Florida: U.S. Geological Survey Open-File Report 65-87, 95 p., https://doi.org/10.3133/ofr6587.","productDescription":"95 p.","costCenters":[],"links":[{"id":179705,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6833f2","contributors":{"authors":[{"text":"Kohout, F. A.","contributorId":11593,"corporation":false,"usgs":true,"family":"Kohout","given":"F.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":245401,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hartwell, J.H.","contributorId":98356,"corporation":false,"usgs":true,"family":"Hartwell","given":"J.H.","email":"","affiliations":[],"preferred":false,"id":245402,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":63158,"text":"gq378 - 1965 - Geology of the Dromedary Peak quadrangle, Utah","interactions":[],"lastModifiedDate":"2012-02-10T00:10:43","indexId":"gq378","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"378","title":"Geology of the Dromedary Peak quadrangle, Utah","language":"ENGLISH","doi":"10.3133/gq378","usgsCitation":"Crittenden, M., 1965, Geology of the Dromedary Peak quadrangle, Utah: U.S. Geological Survey Geologic Quadrangle 378, 1 map., https://doi.org/10.3133/gq378.","productDescription":"1 map.","costCenters":[],"links":[{"id":102392,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_841.htm","linkFileType":{"id":5,"text":"html"},"description":"841"},{"id":249279,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0378/report.pdf","size":"31","linkFileType":{"id":1,"text":"pdf"}},{"id":252443,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0378/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.75,40.5 ], [ -111.75,40.6175 ], [ -111.61749999999999,40.6175 ], [ -111.61749999999999,40.5 ], [ -111.75,40.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682f9b","contributors":{"authors":[{"text":"Crittenden, Max D.","contributorId":43404,"corporation":false,"usgs":true,"family":"Crittenden","given":"Max D.","affiliations":[],"preferred":false,"id":268420,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68130,"text":"ha150 - 1965 - Floods in Barrington Quadrangle, Northeastern Illinois","interactions":[],"lastModifiedDate":"2012-02-10T00:11:29","indexId":"ha150","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"150","title":"Floods in Barrington Quadrangle, Northeastern Illinois","language":"ENGLISH","doi":"10.3133/ha150","usgsCitation":"Noehre, A.W., Walter, G.L., and Allen, H., 1965, Floods in Barrington Quadrangle, Northeastern Illinois: U.S. Geological Survey Hydrologic Atlas 150, 1 col. map ;58 x 43 cm., on sheet 82 x 112 cm., https://doi.org/10.3133/ha150.","productDescription":"1 col. map ;58 x 43 cm., on sheet 82 x 112 cm.","costCenters":[],"links":[{"id":186673,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89430,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/150/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.25,42.1175 ], [ -88.25,42.25 ], [ -88.11749999999999,42.25 ], [ -88.11749999999999,42.1175 ], [ -88.25,42.1175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e71d4","contributors":{"authors":[{"text":"Noehre, Allen W.","contributorId":17659,"corporation":false,"usgs":true,"family":"Noehre","given":"Allen","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":277699,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walter, Gerald L.","contributorId":59880,"corporation":false,"usgs":true,"family":"Walter","given":"Gerald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":277700,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Allen, Howard E.","contributorId":17274,"corporation":false,"usgs":true,"family":"Allen","given":"Howard E.","affiliations":[],"preferred":false,"id":277698,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":52470,"text":"ofr6568 - 1965 - Description and analysis of the geohydrologic system in western Pinal County, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:11:23","indexId":"ofr6568","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-68","title":"Description and analysis of the geohydrologic system in western Pinal County, Arizona","docAbstract":"Western Pinal County is between Phoenix and Tucson in the Basin and Range physiographic province of southern Arizona and consists of about 2,000 square miles of valley floor with low relief surrounded by mountains. It is the second largest agricultural area in the State, and about 25 percent of the ground water pumped in the State is from this area. \r\n\r\nThe study area has been divided into four parts. Three of these--the Casa Grande-Florence area, the Eloy area, and the Stanfield-Maricopa area--are in the lower Santa Cruz basin; the fourth--the Gila River area--is a long narrow strip along the Gila River from the Ashurst-Hayden Dam to the confluence of the Gila and Santa Cruz Rivers. The project was undertaken to provide a better understanding of the ground-water supply in relation to the present and potential water use in this area of extensive ground-water development. The arid climate of western Pinal County--combining high temperatures and low humidity--causes most of the precipitation to be returned to the atmosphere by evapotranspiration, which leaves only a very small part for recharge to the ground-water reservoir. The computed potential evapotranspiration--44. 97 inches--is five times greater than the average precipitation. \r\n\r\nIn general, the subsurface materials in western Pinal County are unconsolidated alluvial deposits underlain by consolidated alluvium and crystalline rocks and bounded by mountains consisting of crystalline and minor sedimentary rocks. The crystalline and sedimentary rocks of the mountains are not known to be water bearing in western Pinal County. The impermeable rocks underlying the basin are called the hydrologic bedrock unit in this report. Although the unit may consist of several different rock types, the distinction between them is relatively unimportant in this study because none of them yield appreciable amounts of water. The lower Santa Cruz basin in western Pinal County is divided into two sections by a buried ridge of the hydrologic bedrock unit, referred to in this report as the Casa Grande ridge. The ridge trends in a north-south direction from the Sacaton to the Silver Reef Mountains. \r\n\r\nThe unconsolidated deposits constitute the main storage reservoir for ground water in western Pins/ County. The deposits are divided into four units---the local gravel unit, the lower sand and gravel unit, the silt and clay unit, and the upper sand and gravel unit--all of which are major water-yielding units except the silt and clay unit. The local gravel unit, which is present only in the western section of the lower Santa Cruz basin, ranges in thickness from 0 to nearly 1,000 feet and is generally a productive aquifer. The lower sand and gravel unit, Which is a heterogeneous mixture of sand, gravel, and clay, ranges in thickness from 0 to about 500 feet. Where the lower sand and gravel unit is overlain by the silt and clay unit, it generally contains water under artesian conditions; where it is not overlain by the silt and clay unit, it is indistinguishable from the upper sand and gravel unit, and the water is under water-table conditions. The silt and clay unit is the least permeable deposit of the unconsolidated alluvium, and ranges in thickness from 0 to about 2, 000 feet. Generally it is less productive than the other units of the unconsolidated alluvium, although it yields moderate amounts of water from numerous thin stringers and lenses of highly permeable sand and gravel. The upper sand and gravel unit is at the land surface in most of the area; it ranges in thickness from less than 50 to about 600 feet. The unit has the highest average permeability of all the unconsolidated alluvial units; however, the permeability of the unit varies vertically and laterally, which results in a wide range of well yields. As of 1964, the static water levels in most wells in the basin were still in the upper sand and gravel unit. However, the unit is being dewatered in most of the basin, and water levels in","language":"ENGLISH","doi":"10.3133/ofr6568","usgsCitation":"Hardt, W.F., and Cattany, R., 1965, Description and analysis of the geohydrologic system in western Pinal County, Arizona: U.S. Geological Survey Open-File Report 65-68, 111 p., https://doi.org/10.3133/ofr6568.","productDescription":"111 p.","costCenters":[],"links":[{"id":179267,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1965/0068/report-thumb.jpg"},{"id":86900,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86901,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86902,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86903,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86904,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86905,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86906,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86907,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86908,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86909,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86910,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86911,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86912,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86913,"rank":413,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86914,"rank":414,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86915,"rank":415,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-16.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86916,"rank":416,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-17.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86917,"rank":417,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-18.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86918,"rank":418,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-19.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86919,"rank":419,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-20.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86920,"rank":420,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-21.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86921,"rank":421,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-22.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86922,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1965/0068/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66dce1","contributors":{"authors":[{"text":"Hardt, W. 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,{"id":52479,"text":"ofr65100 - 1965 - Logs of test holes and wells in the Red River Valley in Lafayette, Little River, and Miller Counties, Arkansas","interactions":[],"lastModifiedDate":"2012-02-02T00:11:27","indexId":"ofr65100","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-100","title":"Logs of test holes and wells in the Red River Valley in Lafayette, Little River, and Miller Counties, Arkansas","language":"ENGLISH","doi":"10.3133/ofr65100","usgsCitation":"May, J., Emmett, L.F., and Ludwig, A.H., 1965, Logs of test holes and wells in the Red River Valley in Lafayette, Little River, and Miller Counties, Arkansas: U.S. Geological Survey Open-File Report 65-100, 55 p., https://doi.org/10.3133/ofr65100.","productDescription":"55 p.","costCenters":[],"links":[{"id":179708,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ae4b07f02db63ccad","contributors":{"authors":[{"text":"May, J.R.","contributorId":67158,"corporation":false,"usgs":true,"family":"May","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":245410,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Emmett, L. F.","contributorId":43332,"corporation":false,"usgs":true,"family":"Emmett","given":"L.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":245408,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ludwig, A. H.","contributorId":63007,"corporation":false,"usgs":true,"family":"Ludwig","given":"A.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":245409,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2990,"text":"wsp1792 - 1965 - Ground water in Permafrost regions--an annotated bibliography","interactions":[{"subject":{"id":52376,"text":"ofr63140 - 1963 - Ground water in permafrost regions - an annotated bibliography of publications through 1960, with glossary of terms","indexId":"ofr63140","publicationYear":"1963","noYear":false,"title":"Ground water in permafrost regions - an annotated bibliography of publications through 1960, with glossary of terms"},"predicate":"SUPERSEDED_BY","object":{"id":2990,"text":"wsp1792 - 1965 - Ground water in Permafrost regions--an annotated bibliography","indexId":"wsp1792","publicationYear":"1965","noYear":false,"title":"Ground water in Permafrost regions--an annotated bibliography"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:36","indexId":"wsp1792","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1792","title":"Ground water in Permafrost regions--an annotated bibliography","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/wsp1792","usgsCitation":"Williams, J.R., 1965, Ground water in Permafrost regions--an annotated bibliography: U.S. Geological Survey Water Supply Paper 1792, iii, 294 p. :fold. map (in pocket) ;24 cm., https://doi.org/10.3133/wsp1792.","productDescription":"iii, 294 p. :fold. map (in pocket) ;24 cm.","costCenters":[],"links":[{"id":139447,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1792/report-thumb.jpg"},{"id":29762,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1792/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29763,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1792/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66daf0","contributors":{"authors":[{"text":"Williams, John R.","contributorId":107260,"corporation":false,"usgs":true,"family":"Williams","given":"John","email":"","middleInitial":"R.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":146111,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2639,"text":"wsp1784 - 1965 - Quality of surface waters in the lower Columbia River Basin","interactions":[],"lastModifiedDate":"2017-02-03T13:41:22","indexId":"wsp1784","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1784","title":"Quality of surface waters in the lower Columbia River Basin","docAbstract":"This report, made during 1959-60, provides reconnaissance data on the quality of waters in the lower Columbia River basin ; information on present and future water problems in the basin; and data that can be employed both in water-use studies and in planning future industrial, municipal, and agricultural expansion within this area. \r\n\r\nThe lower Columbia River basin consists of approximately 46,000 square miles downstream from the confluence of the Snake and Columbia Rivers The region can be divided into three geographic areas. The first is the heavily forested, sparsely populated mountain regions in which quality of water in general is related to geologic and climatological factors. The second is a semiarid plateau east of the Cascade Mountains; there differences in geology and precipitation, together with more intensive use of available water for irrigation, bring about marked differences in water quality. The third is the Willamette-Puget trough area in which are concentrated most of the industry and population and in which water quality is influenced by sewage and industrial waste disposal. \r\n\r\nThe majority of the streams in the lower Columbia River basin are calcium magnesium bicarbonate waters. In general, the rivers rising in the. Coast Range and on the west slope of the Cascade Range contain less than 100 parts per million of dissolved solids, and hardness of the water is less than 50 parts per million. Headwater reaches of the streams on the east slope of the Cascade Range are similar to those on the west slope; but, downstream, irrigation return flows cause the dissolved-solids content and hardness to increase. Most of the waters, however, remain calcium magnesium bicarbonate in type. \r\n\r\nThe highest observed dissolved-solids concentrations and also some changes in chemical composition occur in the streams draining the more arid parts of the area. In these parts, irrigation is chiefly responsible for increasing the dissolved-solids concentration and altering the chemical composition of the streams. The maximum dissolved-solids concentration and hardness of water observed in major irrigation areas were 507 and 262 parts per million, respectively, for the. Walla Walla River near Touchet, Wash. \r\n\r\nIn terms of the U.S. Salinity Laboratory Staff classification (1954, p. 80), water in most streams in the basin has low salinity and sodium hazards and is suitable for irrigation. A salt-balance problem does exist in the Hermiston-Stanfield, Oreg., area of the Umatilla River basin, and because of poor drainage, improper irrigation practices could cause salt-balance problems in the Willamette River Valley, Oreg., in which irrigation is rapidly increasing.\r\n\r\nPollution by sewage disposal has reached undesirable levels in the Walla Walla River, in the Willamette River from Eugene to Portland, Oreg., and in the Columbia River from Portland to Puget Island. In the lower reaches of the Willamette River, the pollution load from sewage and industrial-waste disposal at times depletes the dissolved oxygen in the water to concentrations below what is considered necessary for aquatic life. \r\n\r\nWater in most of the tributaries to the lower Columbia River is of excellent quality and after some treatment could be used for industrial and municipal supplies. The principal treatment required would be disinfection and turbidity removal.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1784","usgsCitation":"Santos, J.F., 1965, Quality of surface waters in the lower Columbia River Basin: U.S. Geological Survey Water Supply Paper 1784, iv, 78 p. :illus., maps. ;24 cm., https://doi.org/10.3133/wsp1784.","productDescription":"iv, 78 p. :illus., maps. ;24 cm.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":28958,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1784/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138744,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1784/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651877","contributors":{"authors":[{"text":"Santos, John F.","contributorId":21530,"corporation":false,"usgs":true,"family":"Santos","given":"John","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":145543,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":63343,"text":"gq458 - 1965 - Geologic map of the South Pass City quadrangle, Fremont County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-10T00:10:59","indexId":"gq458","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"458","title":"Geologic map of the South Pass City quadrangle, Fremont County, Wyoming","language":"ENGLISH","doi":"10.3133/gq458","usgsCitation":"Bayley, R.W., 1965, Geologic map of the South Pass City quadrangle, Fremont County, Wyoming: U.S. Geological Survey Geologic Quadrangle 458, 1 map., https://doi.org/10.3133/gq458.","productDescription":"1 map.","costCenters":[],"links":[{"id":102477,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_926.htm","linkFileType":{"id":5,"text":"html"},"description":"926"},{"id":249445,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0458/report.pdf","size":"32","linkFileType":{"id":1,"text":"pdf"}},{"id":252844,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0458/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.86749999999999,42.3675 ], [ -108.86749999999999,42.5 ], [ -108.75,42.5 ], [ -108.75,42.3675 ], [ -108.86749999999999,42.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae6e4b07f02db68b2e5","contributors":{"authors":[{"text":"Bayley, Richard W.","contributorId":106084,"corporation":false,"usgs":true,"family":"Bayley","given":"Richard","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":268700,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":64122,"text":"gp500 - 1965 - Aeromagnetic map of Findlay, Ohio, and vicinity","interactions":[],"lastModifiedDate":"2022-12-23T19:53:14.861576","indexId":"gp500","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"500","title":"Aeromagnetic map of Findlay, Ohio, and vicinity","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp500","usgsCitation":"Bromery, R.W., and McCaslin, W.E., 1965, Aeromagnetic map of Findlay, Ohio, and vicinity: U.S. Geological Survey Geophysical Investigations Map 500, Report: 1 p.; 1 Plate: 29.007 x 21.90 inches, https://doi.org/10.3133/gp500.","productDescription":"Report: 1 p.; 1 Plate: 29.007 x 21.90 inches","costCenters":[],"links":[{"id":411015,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3451.htm","linkFileType":{"id":5,"text":"html"}},{"id":254090,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0500/report-thumb.jpg"},{"id":250579,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0500/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":250578,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0500/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"125000","country":"United States","state":"Ohio","city":"Findlay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84.125,\n              40.75\n            ],\n            [\n              -84.125,\n              41.25\n            ],\n            [\n              -83.25,\n              41.25\n            ],\n            [\n              -83.25,\n              40.75\n            ],\n            [\n              -84.125,\n              40.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db6982eb","contributors":{"authors":[{"text":"Bromery, R. W.","contributorId":11676,"corporation":false,"usgs":true,"family":"Bromery","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":269992,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCaslin, W. E.","contributorId":37002,"corporation":false,"usgs":true,"family":"McCaslin","given":"W.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":269993,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":63342,"text":"gq460 - 1965 - Geologic map of the Miners Delight quadrangle, Fremont County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-10T00:10:59","indexId":"gq460","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"460","title":"Geologic map of the Miners Delight quadrangle, Fremont County, Wyoming","language":"ENGLISH","doi":"10.3133/gq460","usgsCitation":"Bayley, R.W., 1965, Geologic map of the Miners Delight quadrangle, Fremont County, Wyoming: U.S. Geological Survey Geologic Quadrangle 460, 1 map., https://doi.org/10.3133/gq460.","productDescription":"1 map.","costCenters":[],"links":[{"id":102480,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_929.htm","linkFileType":{"id":5,"text":"html"},"description":"929"},{"id":249444,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0460/report.pdf","size":"32","linkFileType":{"id":1,"text":"pdf"}},{"id":252843,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0460/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.75,42.5 ], [ -108.75,42.6175 ], [ -108.61749999999999,42.6175 ], [ -108.61749999999999,42.5 ], [ -108.75,42.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696982","contributors":{"authors":[{"text":"Bayley, Richard W.","contributorId":106084,"corporation":false,"usgs":true,"family":"Bayley","given":"Richard","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":268699,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":63341,"text":"gq461 - 1965 - Geologic map of the Louis Lake quadrangle, Fremont County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-10T00:10:59","indexId":"gq461","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"461","title":"Geologic map of the Louis Lake quadrangle, Fremont County, Wyoming","language":"ENGLISH","doi":"10.3133/gq461","usgsCitation":"Bayley, R.W., 1965, Geologic map of the Louis Lake quadrangle, Fremont County, Wyoming: U.S. Geological Survey Geologic Quadrangle 461, 1 map :col. ;on sheet 71 x 71 cm. fold. in envelope 31 x 24 cm., https://doi.org/10.3133/gq461.","productDescription":"1 map :col. ;on sheet 71 x 71 cm. fold. in envelope 31 x 24 cm.","costCenters":[],"links":[{"id":102481,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_930.htm","linkFileType":{"id":5,"text":"html"},"description":"930"},{"id":249443,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0461/report.pdf","size":"32","linkFileType":{"id":1,"text":"pdf"}},{"id":252842,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0461/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.86749999999999,42.5 ], [ -108.86749999999999,42.6175 ], [ -108.75,42.6175 ], [ -108.75,42.5 ], [ -108.86749999999999,42.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696d85","contributors":{"authors":[{"text":"Bayley, Richard W.","contributorId":106084,"corporation":false,"usgs":true,"family":"Bayley","given":"Richard","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":268698,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68184,"text":"ha148 - 1965 - Floods in Wheaton quadrangle, northeastern Illinois","interactions":[],"lastModifiedDate":"2012-02-10T00:11:29","indexId":"ha148","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"148","title":"Floods in Wheaton quadrangle, northeastern Illinois","language":"ENGLISH","doi":"10.3133/ha148","usgsCitation":"May, V.J., and Allen, H., 1965, Floods in Wheaton quadrangle, northeastern Illinois: U.S. Geological Survey Hydrologic Atlas 148, 1 map :col. ;58 x 44 cm., on sheet 78 x 122 cm., https://doi.org/10.3133/ha148.","productDescription":"1 map :col. ;58 x 44 cm., on sheet 78 x 122 cm.","costCenters":[],"links":[{"id":186468,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89494,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/148/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.11749999999999,41.75 ], [ -88.11749999999999,41.8675 ], [ -88,41.8675 ], [ -88,41.75 ], [ -88.11749999999999,41.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dee4b07f02db5e30c8","contributors":{"authors":[{"text":"May, V. Jeff","contributorId":80358,"corporation":false,"usgs":true,"family":"May","given":"V.","email":"","middleInitial":"Jeff","affiliations":[],"preferred":false,"id":277797,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Allen, Howard E.","contributorId":17274,"corporation":false,"usgs":true,"family":"Allen","given":"Howard E.","affiliations":[],"preferred":false,"id":277796,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":63347,"text":"gq428 - 1965 - Geologic map of the Blackcap Mountain quadrangle, Fresno County, California","interactions":[],"lastModifiedDate":"2012-02-10T00:10:59","indexId":"gq428","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"428","title":"Geologic map of the Blackcap Mountain quadrangle, Fresno County, California","language":"ENGLISH","doi":"10.3133/gq428","usgsCitation":"Bateman, P.C., 1965, Geologic map of the Blackcap Mountain quadrangle, Fresno County, California: U.S. Geological Survey Geologic Quadrangle 428, 1 map., https://doi.org/10.3133/gq428.","productDescription":"1 map.","costCenters":[],"links":[{"id":101807,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27.htm","linkFileType":{"id":5,"text":"html"},"description":"27"},{"id":249449,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0428/report.pdf","size":"32","linkFileType":{"id":1,"text":"pdf"}},{"id":252931,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0428/report-thumb.jpg"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -119,37 ], [ -119,37.25 ], [ -118.75,37.25 ], [ -118.75,37 ], [ -119,37 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ce4b07f02db69ee1a","contributors":{"authors":[{"text":"Bateman, Paul Charles","contributorId":54586,"corporation":false,"usgs":true,"family":"Bateman","given":"Paul","email":"","middleInitial":"Charles","affiliations":[],"preferred":false,"id":268706,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5712,"text":"pp498C - 1965 - Relation of electrochemical potentials and iron content to ground-water flow patterns","interactions":[],"lastModifiedDate":"2017-04-25T14:05:37","indexId":"pp498C","displayToPublicDate":"1993-01-01T10:00:00","publicationYear":"1965","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":"498","chapter":"C","title":"Relation of electrochemical potentials and iron content to ground-water flow patterns","docAbstract":"<p>This study was undertaken to develop means of measuring oxidation potentials in aquifer systems and to use the measured values in interpreting the behavior of iron in ground water. Anne Arundel County, Md., was selected as the area of study because of the wide range of concentration of iron-nearly zero to about 35 ppm-in the ground water and the rather complete information on the geology and hydrology. The regional geology consists of coastal plain sediments ranging in age from Early Cretaceous through the Recent. Most of the pH and oxidation-potential measurements were made in nonmarine Cretaceous deposits, only a few in the marine Eocene. Iron-bearing minerals in the area are primarily hematite or limonite and glauconite with a small amount of pyrite. </p><p>Equipment was developed that permits the measurement of oxidation potentials by use of saturated calomel and platinum electrodes in ground-water samples uncontaminated by oxygen of the atmosphere. Measured Eh values range from about +700 mv to -40 mv. Approximately 2 to 3 hours are required to measure a stable or nearly stable oxidation potential. </p><p>The mineralogy and organic content of the deposits and the ground-water flow pattern are the primary controls on the oxidation potential and pH of the water. A correlation exists between the oxidation potential and the concentration of iron in ground water; the higher concentrations occur in waters with the lowest values of Eh. The concentration of iron in the water tested shows little correlation with the pH of the water. The highest oxidation potentials were measured in water produced from shallow wells and those wells in recharge areas. The lowest potentials were measured farthest downgradient in water associated with gray and green sediments. The Eh values measured in the field are between values predicted from the solubility of Fe(OH)<sub>2</sub>(c) and values predicted from the solubility of hematite.</p>","largerWorkTitle":"Hydrology of aquifer systems","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp498C","usgsCitation":"Back, W., and Barnes, I., 1965, Relation of electrochemical potentials and iron content to ground-water flow patterns: U.S. Geological Survey Professional Paper 498, Report: iii, p. C1-C16; 3 Plates: 10.09 x 17.13 inches or less, https://doi.org/10.3133/pp498C.","productDescription":"Report: iii, p. C1-C16; 3 Plates: 10.09 x 17.13 inches or less","costCenters":[],"links":[{"id":32284,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0498c/report.pdf","text":"Report","size":"4.44 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":139891,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0498c/report-thumb.jpg"},{"id":340291,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0498c/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":340289,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0498c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":340290,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0498c/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Maryland","county":"Anne Arundel County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.87957763671875,\n              38.69408504756833\n            ],\n            [\n              -76.387939453125,\n              38.69408504756833\n            ],\n            [\n              -76.387939453125,\n              39.25352462727606\n            ],\n            [\n              -76.87957763671875,\n              39.25352462727606\n            ],\n            [\n              -76.87957763671875,\n              38.69408504756833\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c2c3","contributors":{"authors":[{"text":"Back, William","contributorId":59007,"corporation":false,"usgs":true,"family":"Back","given":"William","email":"","affiliations":[],"preferred":false,"id":151472,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barnes, Ivan","contributorId":56619,"corporation":false,"usgs":true,"family":"Barnes","given":"Ivan","email":"","affiliations":[],"preferred":false,"id":151471,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":6378,"text":"pp498B - 1965 - Variations in chemical character of water in the Englishtown Formation, New Jersey","interactions":[{"subject":{"id":52280,"text":"ofr62123 - 1962 - Variations in the chemical character of the water in the Englishtown formation, New Jersey","indexId":"ofr62123","publicationYear":"1962","noYear":false,"title":"Variations in the chemical character of the water in the Englishtown formation, New Jersey"},"predicate":"SUPERSEDED_BY","object":{"id":6378,"text":"pp498B - 1965 - Variations in chemical character of water in the Englishtown Formation, New Jersey","indexId":"pp498B","publicationYear":"1965","noYear":false,"chapter":"B","title":"Variations in chemical character of water in the Englishtown Formation, New Jersey"},"id":1}],"lastModifiedDate":"2017-03-15T12:57:36","indexId":"pp498B","displayToPublicDate":"1992-01-01T08:00:00","publicationYear":"1965","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":"498","chapter":"B","title":"Variations in chemical character of water in the Englishtown Formation, New Jersey","docAbstract":"<p>This investigation describes the variations in the chemical character of the water in the Englishtown Formation of Late Cretaceous age in the Atlantic Coastal Plain of New Jersey, and demonstrates the application of the concept of hydrochemical mapping to the study and evaluation of water-bearing materials.&nbsp;The chemistry of ground water is responsive to the physical environment and lends support to available geologic and hydrologic data. A study of the ground-water chemistry may even suggest concepts for which additional geologic or hydrologic data may not be obtainable by conventional methods of study. Hydrochemical mapping is particularly important in evaluating an aquifer satisfactorily, but it could be equally useful in regional geologic studies concerned with continuity of units or mineralogic differences and similarities.</p>","largerWorkTitle":"Hydrology of aquifer systems","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp498B","collaboration":"Prepared in cooperation with New Jersey Division of Water Policy and Supply","usgsCitation":"Seaber, P.R., 1965, Variations in chemical character of water in the Englishtown Formation, New Jersey: U.S. Geological Survey Professional Paper 498, iii, p. B1-B35, https://doi.org/10.3133/pp498B.","productDescription":"iii, p. B1-B35","costCenters":[],"links":[{"id":33751,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0498b/report.pdf","text":"Report","size":"5.30 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":121598,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0498b/report-thumb.jpg"}],"country":"United States","state":"New Jersey","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -74.28955078125,\n              40.50753459933616\n            ],\n            [\n              -74.72351074218749,\n              40.13899044275822\n            ],\n            [\n              -75.1519775390625,\n              39.882342585755744\n            ],\n            [\n              -75.3497314453125,\n              39.806426117299374\n            ],\n            [\n              -75.44860839843749,\n              39.688167045890395\n            ],\n            [\n              -75.42938232421875,\n              39.58029027440865\n            ],\n            [\n              -75.3826904296875,\n              39.56970506644249\n            ],\n            [\n              -74.11651611328125,\n              39.816975090490004\n            ],\n            [\n              -74.05334472656249,\n              39.87391156801293\n            ],\n            [\n              -74.0093994140625,\n              40.134790883048524\n            ],\n            [\n              -73.97918701171875,\n              40.361195540839\n            ],\n            [\n              -73.99566650390625,\n              40.40094763151963\n            ],\n            [\n              -74.058837890625,\n              40.44276659332215\n            ],\n            [\n              -74.15496826171874,\n              40.478292268560175\n            ],\n            [\n              -74.28955078125,\n              40.50753459933616\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602af9","contributors":{"authors":[{"text":"Seaber, Paul R.","contributorId":67492,"corporation":false,"usgs":true,"family":"Seaber","given":"Paul","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":152609,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70112256,"text":"70112256 - 1965 - Resource understanding: a challenge to aerial methods","interactions":[],"lastModifiedDate":"2017-03-27T13:42:24","indexId":"70112256","displayToPublicDate":"1990-06-12T10:05:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3051,"text":"Photogrammetric Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Resource understanding: a challenge to aerial methods","docAbstract":"<p>Aerial survey methods are speeding acquisition of survey data needed to provide and manage the nation's resources. These methods have been applied to topographic mapping for a number of years and the record clearly shows their advantages in terms of cost and speed in contrast to the ground methods that have been historically employed. Limited use is now being made of aerial methods to assist cadastral surveys, in location, acquisition and development of National Parks, in mapping the geology of the nation, in locating and developing water resources, and in surveys of the oceans. It is the purpose of this paper to call attention to these uses and to encourage the scientific community to further refine aerial methods so that their use may be increased and the veracity of data improved.</p>","language":"English","publisher":"American Society of Photogrammetry","publisherLocation":"Falls Church, VA","usgsCitation":"Udall, S.L., 1965, Resource understanding: a challenge to aerial methods: Photogrammetric Engineering, v. 31, no. 1, p. 63-75.","productDescription":"13 p.","startPage":"63","endPage":"75","numberOfPages":"13","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288447,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 173.0,16.916667 ], [ 173.0,71.833333 ], [ -66.95,71.833333 ], [ -66.95,16.916667 ], [ 173.0,16.916667 ] ] ] } } ] }","volume":"31","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"539acc13e4b0e83db6d08fdb","contributors":{"authors":[{"text":"Udall, Stewart L.","contributorId":9968,"corporation":false,"usgs":true,"family":"Udall","given":"Stewart","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":494583,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70112254,"text":"70112254 - 1965 - Infrared photography and imagery in water resources research","interactions":[],"lastModifiedDate":"2025-01-07T16:16:02.375348","indexId":"70112254","displayToPublicDate":"1990-06-12T09:49:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2136,"text":"Journal - American Water Works Association","active":true,"publicationSubtype":{"id":10}},"title":"Infrared photography and imagery in water resources research","docAbstract":"<p><span>This article briefly describes the characteristics of infrared radiation and demonstrates how infrared photography and infrared imagery can be applied to water resources research, specifically to the identification and description of hydrologic features.</span></p>","language":"English","publisher":"American Water Works Association","publisherLocation":"Denver, CO","doi":"10.1002/j.1551-8833.1965.tb01472.x","usgsCitation":"Robinove, C.J., 1965, Infrared photography and imagery in water resources research: Journal - American Water Works Association, v. 57, no. 7, p. 834-840, https://doi.org/10.1002/j.1551-8833.1965.tb01472.x.","productDescription":"7 p.","startPage":"834","endPage":"840","numberOfPages":"7","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288445,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"57","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"539acc04e4b0e83db6d08f6f","contributors":{"authors":[{"text":"Robinove, Charles J.","contributorId":16983,"corporation":false,"usgs":true,"family":"Robinove","given":"Charles","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":494582,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70112253,"text":"70112253 - 1965 - Photointerpretation of Alaskan post-earthquake photography","interactions":[],"lastModifiedDate":"2017-03-27T13:40:15","indexId":"70112253","displayToPublicDate":"1990-06-12T09:35:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3051,"text":"Photogrammetric Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Photointerpretation of Alaskan post-earthquake photography","docAbstract":"<p>Aerial photographs taken after the March 27, 1964, Good Friday, Alaskan earthquake were examined stereoscopically to determine effects of the earthquake in areas remote from the towns, highways, and the railroad.  The two thousand black and white photographs used in this study were taking in April, after the earthquake, by the U. S. Coast & Geodetic Survey and were generously supplied to the U. S. Geological Survey.  Part of the photographs, at a scale of 1/24,000, provide blanket coverage of approximately 2,000 square miles of land area north and west of Prince William Sound, including parts of the mainland and some of the adjacent islands.  The epicenter of the earthquake, near the head of Unakwik Inlet, is located in this area.  The rest of the photographs, at scales ranging from 1/17,000 to 1/40,000, cover isolated strips of the coastline of the mainland and nearby islands in the general area of Prince William Sound.</p>\n<br/>\n<p>Figure 1 shows the area of new photo coverage used in this study.  The objective of the study was to determine quickly whether geological features resulting from the earthquake, such as faults, changes in shoreline, cracks in surficial material, pressure ridges in lake ice, fractures in glaciers and lake ice, and rock slides and avalanches, might be identifiable by photointerpretation.  The study was made without benefit of comparisons with older, or pre-earthquake photography, which was not readily available for immediate use.</p>","language":"English","publisher":"American Society of Photogrammetry","publisherLocation":"Falls Church, VA","usgsCitation":"Hackman, R., 1965, Photointerpretation of Alaskan post-earthquake photography: Photogrammetric Engineering, v. 31, no. 4, p. 604-610.","productDescription":"7 p.","startPage":"604","endPage":"610","numberOfPages":"7","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288442,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -150.0122,59.6906 ], [ -150.0122,61.8408 ], [ -144.9482,61.8408 ], [ -144.9482,59.6906 ], [ -150.0122,59.6906 ] ] ] } } ] }","volume":"31","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"539acc05e4b0e83db6d08f77","contributors":{"authors":[{"text":"Hackman, R.J.","contributorId":95086,"corporation":false,"usgs":true,"family":"Hackman","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":686346,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70112252,"text":"70112252 - 1965 - Geological exploration from orbital altitudes","interactions":[],"lastModifiedDate":"2017-03-27T13:39:05","indexId":"70112252","displayToPublicDate":"1990-06-12T09:18:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1829,"text":"Geotimes","active":true,"publicationSubtype":{"id":10}},"title":"Geological exploration from orbital altitudes","docAbstract":"The National Aeronautics & Space Administration is planning geologic exploration from orbiting spacecraft. For that purpose it is evaluating new and refined exploration tools, often called remote sensors, including devices that are sensitive to force fields, such as gravity gradient systems, and devices that record the reflection or emission of electromagnetic energy. Both passive electromagnetic sensors (those that rely on natural sources of illumination, such as the Sun) and active electromagnetic sensors (which use an artificial source of illumination) are being considered.","language":"English","publisher":"American Geological Institute","publisherLocation":"Alexandria, VA","usgsCitation":"Badgley, P.C., Fischer, W., and Lyon, R.J., 1965, Geological exploration from orbital altitudes: Geotimes, v. 10, no. 2, p. 11-14.","productDescription":"5 p.","startPage":"11","endPage":"14","numberOfPages":"5","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288438,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"539acc00e4b0e83db6d08f43","contributors":{"authors":[{"text":"Badgley, Peter C.","contributorId":33625,"corporation":false,"usgs":true,"family":"Badgley","given":"Peter","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":494579,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fischer, William A.","contributorId":47787,"corporation":false,"usgs":true,"family":"Fischer","given":"William A.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":494580,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lyon, Ronald J. P.","contributorId":75067,"corporation":false,"usgs":true,"family":"Lyon","given":"Ronald","email":"","middleInitial":"J. P.","affiliations":[],"preferred":false,"id":494581,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70106998,"text":"70106998 - 1965 - Water resources data for Indiana, 1965","interactions":[],"lastModifiedDate":"2014-06-02T06:09:13","indexId":"70106998","displayToPublicDate":"1966-01-01T14:16:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"IN-65-1","title":"Water resources data for Indiana, 1965","docAbstract":"<p>The surface-water records for the 1965 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of Indiana are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering States. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey, under the direction of Malcolm D. Hale, district engineer, Surface Water Branch.</p>\n<br/>\n<p>This report marks the beginning of a new method of presenting, annually, basic data on surface-water records by States. Through September 30, 1960, the records of discharge and stage of streams and contents and stage of lakes or reservoirs were published in an annual series of U.S. Geological Survey water-supply papers entitled \"Surface Water Supply of the United States.\" Since 1951 there have been 20 volumes in the series; each volume covered an area whose boundaries coincided with those of certain natural drainage areas. The records in Indiana were contained in Parts 3A, 4 and 5 of that series.</p>\n<br/>\n<p>Beginning with the 1961 water year, streamflow records and related data will be released by the Geological Survey in annual reports on a State-boundary basis. Distribution of these basic-data reports will be limited and primarily for local needs. The records later will be published in Geological Survey water-supply papers at 5-year intervals. These 5-year water-supply papers will show daily discharge and will be compiled on the same geographical areas previously used for the annual series; however, some of the 14 parts of coterminous United States will be further subdivided.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70106998","collaboration":"Prepared in cooperation with Indiana Department of Natural Resources; Indiana State Board of Health; Indiana State Highway Commission; Corps of Engineers, U.S. Army","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1965, Water resources data for Indiana, 1965: U.S. Geological Survey Water Data Report IN-65-1, viii, 249 p., https://doi.org/10.3133/70106998.","productDescription":"viii, 249 p.","numberOfPages":"258","temporalStart":"1964-10-01","temporalEnd":"1965-09-30","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":287928,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":287927,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70106998/report.pdf"}],"country":"United States","state":"Indiana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.0979,37.7717 ], [ -88.0979,41.7607 ], [ -84.7847,41.7607 ], [ -84.7847,37.7717 ], [ -88.0979,37.7717 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"537b280de4b0929ba496abd5","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":535655,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70207281,"text":"70207281 - 1965 - Osmotic equilibrium and overthrust faulting","interactions":[],"lastModifiedDate":"2019-12-15T16:22:01","indexId":"70207281","displayToPublicDate":"1965-12-31T16:15:09","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Osmotic equilibrium and overthrust faulting","docAbstract":"<p><span>The two principal suggested modes of facilitating overthrust faulting are (1) lubrication at the sole by evaporite beds or micaceous shales and (2) flotation due to anomalously high (&gt; hydrostatic) pore-water pressures. Past rapid sedimentation and tectonic compression have been suggested as important causes of anomalously high water pressure (Hubbert and Rubey, 1959). We suggest osmosis as another important possibility. Field data on shale beds and experimental studies on compacted clays show that such material can act as semipermeable membranes that greatly retard passage of dissolved electrolytes relative to H</span><sub>2</sub><span>O. Equilibrium osmotic pressure, π, across an ideal membrane is given by (a, activity; V</span><sub>H2O</sub><sup>0</sup><sub>1</sub><span>, molar volume of distilled water). At 80°C, π is 470 bars between saturated halite solution and distilled water; it is 360 bars between saturated and 10 per cent solutions. At 25°C the values are 20 per cent lower. Other dissolved components, if present in similar proportions, will enhance the effect. Anomalous water pressures of at least 400 bars above hydrostatic have been measured in oil wells; many of these wells penetrate evaporites and/or shales which separate formation waters of differing salt concentrations. These pressures are explicable by assuming osmotic equilibrium across a membrane which separates saturated halite solution from solutions up to 10 weight per cent NaCl. Thus, osmotic equilibrium may be an important mechanism for floating thrust sheets. Lubrication of thrust sheets by shales or evaporites and flotation by anomalously high pressures may be simply different manifestations of the same geologic milieu. © 1965, The Geological Society of America, Inc.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1965)76[1379:OEAOF]2.0.CO;2","issn":"00167606","usgsCitation":"Hanshaw, B., and Zen, E., 1965, Osmotic equilibrium and overthrust faulting: Geological Society of America Bulletin, v. 76, no. 12, p. 1379-1385, https://doi.org/10.1130/0016-7606(1965)76[1379:OEAOF]2.0.CO;2.","productDescription":"7 p. ","startPage":"1379","endPage":"1385","costCenters":[],"links":[{"id":370288,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"76","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hanshaw, B.B.","contributorId":25928,"corporation":false,"usgs":true,"family":"Hanshaw","given":"B.B.","email":"","affiliations":[],"preferred":false,"id":777530,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zen, E-An","contributorId":47064,"corporation":false,"usgs":true,"family":"Zen","given":"E-An","email":"","affiliations":[],"preferred":false,"id":777531,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}