{"pageNumber":"2528","pageRowStart":"63175","pageSize":"25","recordCount":68801,"records":[{"id":33127,"text":"b1232 - 1966 - Bibliography of North American geology, 1962","interactions":[],"lastModifiedDate":"2012-02-02T00:09:10","indexId":"b1232","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1232","title":"Bibliography of North American geology, 1962","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1232","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1966, Bibliography of North American geology, 1962: U.S. Geological Survey Bulletin 1232, 834 p, https://doi.org/10.3133/b1232.","productDescription":"834 p","costCenters":[],"links":[{"id":247372,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1232/report.pdf","size":"39396","linkFileType":{"id":1,"text":"pdf"}},{"id":251819,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1232/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db6298a0","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":529453,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14023,"text":"ofr6658 - 1966 - Seismic refraction surveys in the vicinity of Eagle City, Clark County, Ohio","interactions":[],"lastModifiedDate":"2016-11-07T10:16:41","indexId":"ofr6658","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"66-58","title":"Seismic refraction surveys in the vicinity of Eagle City, Clark County, Ohio","docAbstract":"<p>As part of a continuing program to define the thickness and extent of water-bearing sand and gravel deposits in southwestern Ohio, the U.S. Geological Survey, in cooperation with the Ohio Division of Water, in the summer of 1964 completed a seismic refraction survey in the vicinity of Eagle and Tremont Cities, Ohio (fig. 1). Similar surveys were completed in 1962 of the lower Great Miami River and Whitewater River Valleys (Watkins, 1963); in 1963 of the upper Great Miami River Valley (Watkins and Spieker, 1964) and of the Scioto River Valley (Watkins and Bailey, 1964). </p><p>The area of the survey includes known or inferred portions of an interglacial drainage system which is deeply entrenched into bedrock. Ohio was covered by glaciers at least twice during the Pleistocene Epoch. As the last glacier retreated from Clark County, floods of meltwater deposited up to 300 ft of sand and gravel, now forming the lowlands of the Mad River Valley. </p><p>The sand and gravel is highly permeable and saturated with large quantities of water of good quality. The underlying bedrock consists of limestone and dolomite, and limestone interbedded with shale. The limestone and dolomite sequence is the principal source of water along the edges of the buried valley where the sand and gravel thins. The city of Springfield has recently developed wells in the glacial deposits, and many industries in the area rely on wells in these deposits as their principal source of water. The purpose of the present survey is to define the thickness and extent of the important water-bearing sand and gravel deposits. Such information will make possible a more accurate evaluation of the area's water resources than has previously been possible.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6658","usgsCitation":"Hassemer, J.H., Watkins, J.S., and Bailey, N.G., 1966, Seismic refraction surveys in the vicinity of Eagle City, Clark County, Ohio: U.S. Geological Survey Open-File Report 66-58, 7 p., https://doi.org/10.3133/ofr6658.","productDescription":"7 p.","numberOfPages":"11","costCenters":[],"links":[{"id":147209,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":330800,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1966/0058/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Ohio","county":"Clark County","city":"Eagle City","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.86053085327148,\n              39.95185892663005\n            ],\n            [\n              -83.86053085327148,\n              40.016834928010034\n            ],\n            [\n              -83.79632949829102,\n              40.016834928010034\n            ],\n            [\n              -83.79632949829102,\n              39.95185892663005\n            ],\n            [\n              -83.86053085327148,\n              39.95185892663005\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb6b7","contributors":{"authors":[{"text":"Hassemer, Jerry H.","contributorId":8103,"corporation":false,"usgs":true,"family":"Hassemer","given":"Jerry","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":168807,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Watkins, Joel S.","contributorId":10788,"corporation":false,"usgs":true,"family":"Watkins","given":"Joel","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":168808,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bailey, Norman G.","contributorId":59439,"corporation":false,"usgs":true,"family":"Bailey","given":"Norman","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":168809,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":68254,"text":"ha165 - 1966 - Availability of ground water in parts of Hamlin and Paris Landing quadrangles, Jackson Purchase Region, Kentucky","interactions":[],"lastModifiedDate":"2022-10-07T19:50:11.184896","indexId":"ha165","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"165","title":"Availability of ground water in parts of Hamlin and Paris Landing quadrangles, Jackson Purchase Region, Kentucky","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha165","usgsCitation":"Lambert, T.W., 1966, Availability of ground water in parts of Hamlin and Paris Landing quadrangles, Jackson Purchase Region, Kentucky: U.S. Geological Survey Hydrologic Atlas 165, 1 Plate: 47.68 × 35.00 inches, https://doi.org/10.3133/ha165.","productDescription":"1 Plate: 47.68 × 35.00 inches","costCenters":[],"links":[{"id":189680,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":408122,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15526.htm","linkFileType":{"id":5,"text":"html"}},{"id":89640,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/165/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Kentucky","otherGeospatial":"Hamlin and Paris Landing quadrangles, Jackson Purchase region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.125,\n              36.5\n            ],\n            [\n              -88.042,\n              36.5\n            ],\n            [\n              -88.042,\n              36.625\n            ],\n            [\n              -88.125,\n              36.625\n            ],\n            [\n              -88.125,\n              36.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db6608c4","contributors":{"authors":[{"text":"Lambert, T. William","contributorId":40574,"corporation":false,"usgs":true,"family":"Lambert","given":"T.","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":277917,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56299,"text":"wdrNV651 - 1966 - Water resources data for Nevada, 1965","interactions":[],"lastModifiedDate":"2012-02-02T00:12:01","indexId":"wdrNV651","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"NV-65-1","title":"Water resources data for Nevada, 1965","language":"ENGLISH","doi":"10.3133/wdrNV651","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1966, Water resources data for Nevada, 1965: U.S. Geological Survey Water Data Report NV-65-1, NA, https://doi.org/10.3133/wdrNV651.","productDescription":"NA","costCenters":[],"links":[{"id":181327,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f0e4b07f02db5edea4","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":532490,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68502,"text":"ha220 - 1966 - Water resources of the Pomme de Terre River Watershed, West-central Minnesota","interactions":[],"lastModifiedDate":"2018-03-05T12:30:00","indexId":"ha220","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"220","title":"Water resources of the Pomme de Terre River Watershed, West-central Minnesota","docAbstract":"<p>The watershed is underlain by water-bearing glacial drift, cretaceous rocks, and Precambrian crystalline rocks. &nbsp;It is an elongate basin 92 miles long and has a drainage area of 977 square miles. &nbsp;The Pomme de Terre River flows within an outwash valley discharging into the Minnesota River at Marsh Lake.</p>","language":"English","publisher":"U.S. Geological 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-96.45172119140624,\n              45.30387083299528\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f065d","contributors":{"authors":[{"text":"Cotter, R. D.","contributorId":89874,"corporation":false,"usgs":true,"family":"Cotter","given":"R.","email":"","middleInitial":"D.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":278332,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bidwell, L. E.","contributorId":100029,"corporation":false,"usgs":true,"family":"Bidwell","given":"L.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":627606,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Oakes, E.L.","contributorId":38652,"corporation":false,"usgs":true,"family":"Oakes","given":"E.L.","email":"","affiliations":[],"preferred":false,"id":627607,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hollenstein, G.H.","contributorId":168893,"corporation":false,"usgs":false,"family":"Hollenstein","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":627608,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":2447,"text":"wsp1683 - 1966 - Magnitude and frequency of floods in the United States: Part 9. Colorado River Basin","interactions":[],"lastModifiedDate":"2022-01-25T22:14:55.973665","indexId":"wsp1683","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1683","title":"Magnitude and frequency of floods in the United States: Part 9. Colorado River Basin","docAbstract":"<p>This report outlines methods by which the magnitude and frequency of expected floods of any recurrence interval from 1.1 to 50 years can be determined at most points in the Colorado River basin.</p><p>Composite frequency curves were drawn showing the relation of the mean annual flood to floods having recurrence intervals from 1.1 to 50 years. Other curves express the relation of the mean annual flood to basin characteristics. In the northern part of the basin (north of about lat 37° N.) both drainage area and mean altitude were important factors influencing the magnitude of the mean annual flood. Only drainage area was used as an independent variable in the southern part of the basin.</p><p>By combining data from the composite frequency curves and curves showing the relation of the mean annual flood to basin characteristics, flood-frequency curves can be drawn for streams in the report area not materially affected by regulation or diversion within the range and recurrence interval defined by base data.</p><p>Some of the larger streams in the basin do not lend themselves to regional analysis. These streams are given special treatment in this report. Owing to the paucity of streamflow data, flood-frequency relations are not defined in some of the more arid parts of the report area. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C","doi":"10.3133/wsp1683","usgsCitation":"Patterson, J.L., and Somers, W., 1966, Magnitude and frequency of floods in the United States: Part 9. Colorado River Basin: U.S. Geological Survey Water Supply Paper 1683, Report: xvii, 475 p.; Plate: 29.50 x 44.45 inches, https://doi.org/10.3133/wsp1683.","productDescription":"Report: xvii, 475 p.; Plate: 29.50 x 44.45 inches","numberOfPages":"491","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":394849,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24892.htm"},{"id":28521,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1683/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138127,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1683/report-thumb.jpg"},{"id":28520,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1683/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona, California, Colorado, Nevada, Nevada, Utah, Wyoming","otherGeospatial":"Colorado River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -115,\n              31.329\n            ],\n            [\n              -105.833,\n              31.329\n            ],\n            [\n              -105.833,\n              43.417\n            ],\n            [\n              -115,\n              43.417\n            ],\n            [\n              -115,\n              31.329\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6495a4","contributors":{"authors":[{"text":"Patterson, James L.","contributorId":17593,"corporation":false,"usgs":true,"family":"Patterson","given":"James","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":145219,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Somers, William P.","contributorId":47346,"corporation":false,"usgs":true,"family":"Somers","given":"William P.","affiliations":[],"preferred":false,"id":145220,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68492,"text":"ha221 - 1966 - Map showing altitude of the base of fresh water in coastal plain aquifers of the Mississippi embayment","interactions":[],"lastModifiedDate":"2022-07-20T18:14:20.665265","indexId":"ha221","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"221","title":"Map showing altitude of the base of fresh water in coastal plain aquifers of the Mississippi embayment","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha221","usgsCitation":"Cushing, E.M., 1966, Map showing altitude of the base of fresh water in coastal plain aquifers of the Mississippi embayment: U.S. Geological Survey Hydrologic Atlas 221, 1 Plate: 31.50 × 29.50 inches, https://doi.org/10.3133/ha221.","productDescription":"1 Plate: 31.50 × 29.50 inches","costCenters":[],"links":[{"id":185568,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":404145,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15587.htm","linkFileType":{"id":5,"text":"html"}},{"id":90045,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/221/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","country":"United States","state":"Alabama, Arkansas, Kentucky, Louisiana, Mississippi, Missouri, Tennessee","otherGeospatial":"Mississippi embayment","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -94.767,\n              32\n            ],\n            [\n              -87.25,\n              32\n            ],\n            [\n              -87.25,\n              37.317\n            ],\n            [\n              -94.767,\n              37.317\n            ],\n            [\n              -94.767,\n              32\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a94e4b07f02db658e6d","contributors":{"authors":[{"text":"Cushing, E. M.","contributorId":94273,"corporation":false,"usgs":true,"family":"Cushing","given":"E.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":278320,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2969,"text":"wsp1806 - 1966 - Ground-water resources and geology of northern and central Johnson County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:05:41","indexId":"wsp1806","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1806","title":"Ground-water resources and geology of northern and central Johnson County, Wyoming","docAbstract":"Northern and central Johnson County, Wyo., is an area of about 2,600 square miles that lies principally in the western part of the Powder River structural basin but also includes the east flank of the Bighorn Mountains. Sedimentary rocks exposed range in age from Cambrian to Recent and have an average total thickness of about 16,000 feet. Igneous and metamorphic rocks of Precambrian age crop out in the Bighorn Mountains. Rocks of pre-Tertiary age, exposed on the flanks and in the foothills of the Bighorns, dip steeply eastward and lie at great depth in the Powder River basin. The rest of the project area is underlain by a thick sequence of interbedded sandstone, siltstone, and shale of Paleocene and Eocene age. Owing to the regional structure, most aquifers in Johnson County contain water under artesian pressure. \r\n\r\nThe Madison Limestone had not been tapped for water in Johnson County at the time of the present investigation (1963), but several wells in eastern Big Horn and Washakie Counties, on the west flank of the Bighorn Mountains, reportedly have flows ranging from 1,100 to 2,800 gallons per minute. Comparable yields can probably be obtained from the Madison in Johnson County in those areas where the limestone is fractured or cavernous. The Tensleep Sandstone reportedly yields 600 gallons per minute to a pumped irrigation well near its outcrop in the southwestern part of the project area. Several flowing wells tap the formation on the west flank of the Bighorn Mountains. The Madison Limestone and the Tensleep Sandstone have limited potential as sources of water because they can be developed economically only in a narrow band paralleling the Bighorn Mountain front in the southwestern part of the project area. \r\n\r\nOverlying the Tensleep Sandstone is about 6,000 feet of shale, siltstone, and fine-grained sandstone that, with a few exceptions, normally yields only small quantities of water to wells. The Cloverly Formation and the Newcastle Sandstone may yield moderate quantities of water to wells; but, in some areas, properly constructed wells tapping both formations might yield large quantities of water. The Shannon Sandstone Member of the Cody Shale will probably yield only small quantities of water to Wells, but it is the best potential source of ground water in the stratigraphic interval between the Newcastle and Parkman Sandstones. \r\n\r\nThe Parkman Sandstone and the Lance Formation yield water to relatively shallow wells principally in the southwestern part of the project area. The Fort Union Formation yields adequate supplies of water for stock and domestic use from relatively shallow wells near its outcrop almost everywhere in the county. A few deep wells tap the Fort Union along the Powder River valley in the northeastern part of Johnson County. Some of these wells flow, but their flows rarely exceed 10 gallons per minute; larger yields could be undoubtedly be obtained by pumping. \r\n\r\nThe Wasatch Formation is the principal source of ground water in Johnson County. It yields adequate supplies to many relatively shallow stock and domestic wells, some of which flow, but much larger yields probably would require pumping lifts that are prohibitive for most purposes. The Kingsbury Conglomerate and Moncrief Members of the Wasatch Formation, though, may yield moderate quantities of water in some places. \r\n\r\nAlluvial deposits underlying the valleys of the Powder River and Crazy Woman, Clear, and Piney Creeks are potential sources of moderate to large supplies of water in the Powder River drainage basin. The permeability of these deposits decreases with distance from the Bighorn Mountain front, so that largest yields can probably be obtained along the upper reaches of these streams. \r\n\r\nMost ground water utilized in the project area is for domestic and stock supplies and is obtained from drilled wells and from springs. Water for irrigation is obtained almost entirely by diverting flows of perennial streams. The discharge of wel","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/wsp1806","usgsCitation":"Whitcomb, H.A., Cummings, T.R., and McCullough, R.A., 1966, Ground-water resources and geology of northern and central Johnson County, Wyoming: U.S. Geological Survey Water Supply Paper 1806, v, 90 p. :illus., maps. ;24 cm., https://doi.org/10.3133/wsp1806.","productDescription":"v, 90 p. :illus., maps. ;24 cm.","costCenters":[],"links":[{"id":139273,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1806/report-thumb.jpg"},{"id":29704,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1806/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db666f87","contributors":{"authors":[{"text":"Whitcomb, Harold A.","contributorId":102868,"corporation":false,"usgs":true,"family":"Whitcomb","given":"Harold","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":146066,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cummings, T. Ray","contributorId":20722,"corporation":false,"usgs":true,"family":"Cummings","given":"T.","email":"","middleInitial":"Ray","affiliations":[],"preferred":false,"id":146064,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McCullough, Richard A.","contributorId":78712,"corporation":false,"usgs":true,"family":"McCullough","given":"Richard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":146065,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2007,"text":"wsp1869B - 1966 - Effect of vertical motion on current meters","interactions":[],"lastModifiedDate":"2012-02-02T00:05:22","indexId":"wsp1869B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1869","chapter":"B","title":"Effect of vertical motion on current meters","docAbstract":"The effect of vertical motion on the performance of current meters at various stream velocities was evaluated to determine whether accurate discharge measurements can be made from a bobbing boat. \r\n\r\nThree types of current meters--Ott, Price, and vane types--were tested under conditions simulating a bobbing boat. A known frequency and amplitude of vertical motion were imparted to the current meter, and the related effect on the measured stream velocity was determined. One test of the Price meter was made under actual conditions, using a boat and standard measuring gear. The results of the test under actual conditions verified those obtained by simulating the vertical movements of a boat. \r\n\r\nThe tests show that for stream velocities below 2.5 feet per second the accuracy of all three meters is significantly affected when the meters are subjected to certain conditions of vertical motion that can occur during actual field operations. Both the rate of vertical motion and the frequency of vertical oscillation affect the registration of the meter. \r\n\r\nThe results of these tests, presented in the form of graphs and tables, can be used as a guide to determine whether wind and stream flow are within an acceptable range for a reliable discharge measurement from a boat.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1869B","usgsCitation":"Kallio, N.A., 1966, Effect of vertical motion on current meters: U.S. Geological Survey Water Supply Paper 1869, iv, 20 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1869B.","productDescription":"iv, 20 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":138395,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1869b/report-thumb.jpg"},{"id":27452,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1869b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db625434","contributors":{"authors":[{"text":"Kallio, Nicholas A.","contributorId":15992,"corporation":false,"usgs":true,"family":"Kallio","given":"Nicholas","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":144517,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":187,"text":"wsp1883 - 1966 - Quality of surface waters of the United States, 1961, Parts 5 and 6, Hudson Bay and upper Mississippi River basins and Missouri River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:10","indexId":"wsp1883","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1883","title":"Quality of surface waters of the United States, 1961, Parts 5 and 6, Hudson Bay and upper Mississippi River basins and Missouri River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1883","usgsCitation":"Love, S.K., 1966, Quality of surface waters of the United States, 1961, Parts 5 and 6, Hudson Bay and upper Mississippi River basins and Missouri River basin: U.S. Geological Survey Water Supply Paper 1883, viii, 315 p. :tables ;23 cm., https://doi.org/10.3133/wsp1883.","productDescription":"viii, 315 p. :tables ;23 cm.","costCenters":[],"links":[{"id":136331,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1883/report-thumb.jpg"},{"id":24798,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1883/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651b77","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":142058,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68415,"text":"ha218 - 1966 - Fresh-water springs of Hawaii from infrared images","interactions":[],"lastModifiedDate":"2012-02-10T00:11:14","indexId":"ha218","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"218","title":"Fresh-water springs of Hawaii from infrared images","language":"ENGLISH","doi":"10.3133/ha218","usgsCitation":"Fischer, W., Davis, D.A., and Sousa, T.M., 1966, Fresh-water springs of Hawaii from infrared images: U.S. Geological Survey Hydrologic Atlas 218, 1 map ;30 x 27 cm. on sheet 85 x 134 cm. folded to 22 x 27 cm., https://doi.org/10.3133/ha218.","productDescription":"1 map ;30 x 27 cm. on sheet 85 x 134 cm. folded to 22 x 27 cm.","costCenters":[],"links":[{"id":188723,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89937,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/218/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"506800","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -156,18.916666666666668 ], [ -156,20.5 ], [ -154.83333333333334,20.5 ], [ -154.83333333333334,18.916666666666668 ], [ -156,18.916666666666668 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a85f7","contributors":{"authors":[{"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":278179,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davis, Dan A.","contributorId":81188,"corporation":false,"usgs":true,"family":"Davis","given":"Dan","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":278180,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sousa, Theresa M.","contributorId":99642,"corporation":false,"usgs":true,"family":"Sousa","given":"Theresa","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":278181,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":37659,"text":"tp3 - 1966 - Observations on the marine cladoceran Penilia avirostris in northwestern Atlantic waters","interactions":[],"lastModifiedDate":"2012-02-02T00:09:57","indexId":"tp3","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":89,"text":"Technical Paper","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"3","title":"Observations on the marine cladoceran Penilia avirostris in northwestern Atlantic waters","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Croce, N.D., 1966, Observations on the marine cladoceran Penilia avirostris in northwestern Atlantic waters: Technical Paper 3, 37 p. : ill. ; 26 cm.","productDescription":"37 p. : ill. ; 26 cm.","costCenters":[],"links":[{"id":164821,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db696417","contributors":{"authors":[{"text":"Croce, Norberto Della","contributorId":61483,"corporation":false,"usgs":true,"family":"Croce","given":"Norberto","email":"","middleInitial":"Della","affiliations":[],"preferred":false,"id":218424,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":1953,"text":"wsp1869C - 1966 - Velocity-head coefficients in open channels","interactions":[],"lastModifiedDate":"2012-02-02T00:05:22","indexId":"wsp1869C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1869","chapter":"C","title":"Velocity-head coefficients in open channels","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1869C","usgsCitation":"Hulsing, H., Smith, W., and Cobb, E.D., 1966, Velocity-head coefficients in open channels: U.S. Geological Survey Water Supply Paper 1869, v, 45 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1869C.","productDescription":"v, 45 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":138543,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1869c/report-thumb.jpg"},{"id":27293,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1869c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db6022a8","contributors":{"authors":[{"text":"Hulsing, Harry","contributorId":62200,"corporation":false,"usgs":true,"family":"Hulsing","given":"Harry","email":"","affiliations":[],"preferred":false,"id":144428,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, Winchell","contributorId":20311,"corporation":false,"usgs":true,"family":"Smith","given":"Winchell","email":"","affiliations":[],"preferred":false,"id":144426,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cobb, Ernest D.","contributorId":25139,"corporation":false,"usgs":true,"family":"Cobb","given":"Ernest","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":144427,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2792,"text":"wsp1809T - 1966 - Hydrology of the alluvium of the Arkansas River, Muskogee, Oklahoma, to Fort Smith, Arkansas","interactions":[],"lastModifiedDate":"2012-02-02T00:05:28","indexId":"wsp1809T","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1809","chapter":"T","title":"Hydrology of the alluvium of the Arkansas River, Muskogee, Oklahoma, to Fort Smith, Arkansas","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1809T","usgsCitation":"Tanaka, H.H., Hollowell, J.R., and Murphy, J.J., 1966, Hydrology of the alluvium of the Arkansas River, Muskogee, Oklahoma, to Fort Smith, Arkansas: U.S. Geological Survey Water Supply Paper 1809, iv, 42 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1809T.","productDescription":"iv, 42 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":138873,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1809t/report-thumb.jpg"},{"id":29278,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809t/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29279,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809t/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29280,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809t/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29281,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1809t/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdbf7","contributors":{"authors":[{"text":"Tanaka, Harry H.","contributorId":13604,"corporation":false,"usgs":true,"family":"Tanaka","given":"Harry","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":145798,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hollowell, Jerrald R.","contributorId":51278,"corporation":false,"usgs":true,"family":"Hollowell","given":"Jerrald","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":145799,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Murphy, John Joseph","contributorId":8453,"corporation":false,"usgs":true,"family":"Murphy","given":"John","email":"","middleInitial":"Joseph","affiliations":[],"preferred":false,"id":145797,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":3665,"text":"cir530 - 1966 - Gravimetric effects of petroleum accumulations--A preliminary summary","interactions":[],"lastModifiedDate":"2017-08-27T18:00:43","indexId":"cir530","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"530","title":"Gravimetric effects of petroleum accumulations--A preliminary summary","docAbstract":"Negative gravity anomalies of very local extent and with amplitudes of 1.2 milligals or less have been observed over some known petroleum and natural gas fields in southern California and South Dagestan, U.S.S.R. Field evidence, laboratory measurements, and theory indicate that these anomalies are mainly the result of hydrocarbon pore fluids of densities significantly lower than that of water. Gravity meters already available have the precision necessary to detect some of these anomalies from surface measurements. In addition, a high-precision borehole gravity meter has been developed, by the industrial firm of LaCoste and Romberg, Inc., that can be used in wells with a casing 7 inches or more in diameter and at temperatures below 100?C. Field tests indicate that the prototype attains a precision in wells of ? 0.015 milligal for a single measurement. These observations and the new gravimeter should aid in the search for new petroleum fields and for new reservoirs in known fields that are incompletely explored.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir530","usgsCitation":"McCulloh, T.H., 1966, Gravimetric effects of petroleum accumulations--A preliminary summary: U.S. Geological Survey Circular 530, iii, 4 p. ;27 cm., https://doi.org/10.3133/cir530.","productDescription":"iii, 4 p. ;27 cm.","costCenters":[],"links":[{"id":117687,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1966/0530/report-thumb.jpg"},{"id":30705,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1966/0530/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db6722b8","contributors":{"authors":[{"text":"McCulloh, Thane Hubert","contributorId":101625,"corporation":false,"usgs":true,"family":"McCulloh","given":"Thane","email":"","middleInitial":"Hubert","affiliations":[],"preferred":false,"id":147366,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3820,"text":"cir524 - 1966 - The changing pattern of ground-water development on Long Island, New York","interactions":[],"lastModifiedDate":"2017-08-27T17:57:37","indexId":"cir524","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"524","title":"The changing pattern of ground-water development on Long Island, New York","docAbstract":"Ground-water development on Long Island has followed a pattern that has reflected changing population trends, attendant changes in the use and disposal of water, and the response of the hydrologic system to these changes. The historic pattern of development has ranged from individually owned shallow wells tapping glacial deposits to large-capacity public-supply wells tapping deep artesian aquifers. Sewage disposal has ranged from privately owned cesspools to modern large-capacity sewage-treatment plants discharging more than 70 mgd of water to the sea. \r\n\r\nAt present (1965), different parts of long Island are characterized by different stages of ground-water development. In parts of Suffolk County in eastern long Island, development is similar to the earliest historical stages. Westward toward New York City, ground-water development becomes more intensive and complex, and the attendant problems become more acute. The alleviation of present problems and those that arise in the future will require management decisions based on the soundest possible knowledge of the hydrologic system, including an understanding of the factors involved in the changing pattern of ground-water development on the island.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir524","usgsCitation":"Heath, R., Foxworthy, B., and Cohen, P.M., 1966, The changing pattern of ground-water development on Long Island, New York: U.S. Geological Survey Circular 524, iii, 10 p. :illus., maps. ;27 cm., https://doi.org/10.3133/cir524.","productDescription":"iii, 10 p. :illus., maps. ;27 cm.","costCenters":[],"links":[{"id":30890,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1966/0524/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139237,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1966/0524/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a68e4b07f02db63b226","contributors":{"authors":[{"text":"Heath, Ralph C.","contributorId":53359,"corporation":false,"usgs":true,"family":"Heath","given":"Ralph C.","affiliations":[],"preferred":false,"id":147671,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Foxworthy, B. L.","contributorId":45686,"corporation":false,"usgs":true,"family":"Foxworthy","given":"B. L.","affiliations":[],"preferred":false,"id":147670,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cohen, Philip M.","contributorId":67860,"corporation":false,"usgs":true,"family":"Cohen","given":"Philip","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":147672,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":40711,"text":"ofr66157 - 1966 - Effect of treated effluent diversion on Yahara River flow, Wisconsin","interactions":[],"lastModifiedDate":"2015-10-13T12:32:32","indexId":"ofr66157","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"66-157","title":"Effect of treated effluent diversion on Yahara River flow, Wisconsin","docAbstract":"<p>Before December 1958 the treated sewage effluent from the Madison, Wisconsin, metropolitan area was discharged into the Yahara River at the north end of Lake Waubesa, which is upstream from the USGS gaging station on the Yahara River near McFarland, Wis. Since December 1958 the effluent has been diverted southward from the sewage treatment plant into Badfish Creek and enters the lower reach of Yahara River, thus byrpassing the gaging station. The purpose of this report is to demonstrate the effect that this diversion seems to have on the flow of the Yahara River near McFarland. Indirectly, it also demonstrates the effect on streamflow of withdrawing ground water for use in the Madison metropolitan area since the treated effluent is primarily the major portion of the used ground water.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr66157","usgsCitation":"Young, K., 1966, Effect of treated effluent diversion on Yahara River flow, Wisconsin: U.S. Geological Survey Open-File Report 66-157, 23 p., https://doi.org/10.3133/ofr66157.","productDescription":"23 p.","numberOfPages":"23","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":98243,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1966/0157/report.pdf","size":"1509","linkFileType":{"id":1,"text":"pdf"}},{"id":171098,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1966/0157/report-thumb.jpg"}],"country":"United States","state":"Wisconsin","otherGeospatial":"Yahara River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.36965942382812,\n              43.3101903843356\n            ],\n            [\n              -89.55230712890624,\n              43.17814279946058\n            ],\n            [\n              -89.65805053710938,\n              43.08995208151042\n            ],\n            [\n              -89.44244384765625,\n              42.943355168255806\n            ],\n            [\n              -89.25979614257812,\n              42.898100636939276\n            ],\n            [\n              -89.22821044921875,\n              42.819580715795915\n            ],\n            [\n              -89.15817260742188,\n              42.78129125156277\n            ],\n            [\n              -89.11148071289062,\n              42.78431496548022\n            ],\n            [\n              -89.07852172851562,\n              42.790361950280925\n            ],\n            [\n              -89.0716552734375,\n              42.81353658623225\n            ],\n            [\n              -89.0936279296875,\n              42.89105805581562\n            ],\n            [\n              -89.17739868164062,\n              42.99761672705504\n            ],\n            [\n              -89.32159423828125,\n              43.17513839170044\n            ],\n            [\n              -89.36141967773438,\n              43.26020603533185\n            ],\n            [\n              -89.36965942382812,\n              43.3101903843356\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db62543f","contributors":{"authors":[{"text":"Young, K.B.","contributorId":77997,"corporation":false,"usgs":true,"family":"Young","given":"K.B.","email":"","affiliations":[],"preferred":false,"id":223836,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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