This report lists the streamflow and reservoir stations in The Great Basin for which records have been or are to be published in reports of the Geological Survey for periods through September 30, 1967. It supersedes Geological Survey Circular 510.
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The study of the watershed described in this report is designated as Project No. 2 in the Joint Federal-State Acid Mine Drainage Pollution Control Demonstration Program. The area studied encompasses the West End mine of the Blue Coal Company.
\nBedrock in the watershed, from oldest to youngest, consists of the Mauch Chunk Formation of Mississippian and, in part, of Pennsylvanian age; the Pottsville Formation of Pennsylvanian age; and the Llewellyn Formation of Pennsylvanian age. The anthracite beds are in the Llewellyn Formation.
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C1-C34, https://doi.org/10.3133/pp605C.","productDescription":"p. C1-C34","costCenters":[],"links":[{"id":119441,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0605c/report-thumb.jpg"},{"id":67386,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0605c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db625626","contributors":{"authors":[{"text":"Spieker, A. 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Soundings were made on the northwestern part of the island of Oahu near the town of Waialua and on the island of Hawaii on the \"saddle\" area near Pohekuloa and the Humuula sheep station. On Oahu, the geoelectrical study indicates that correlation among four stratigraphic units underlain by a vesicular basalt basement is possible. The electrical soundings indicate that it is feasible to determine the approximate depth to the fresh-saline water interface within the basalt. Two Schlumberger soundings with electrode spacings, AB/2, reaching 6,000 feel give sounding curves of the maximum and minimum type whose terminal branches indicate that the true resistivity of basalts saturated with sea water, in the survey area on Oahu, is about 30-40 ohm-m. On the island of Hawaii, an exploratory well drilled in basalt to a depth of 1,001 feet proved to be dry. In the area of this well, two deep soundings were made using the Schlumberger and the equatorial arrays. Although additional soundings at various orientations and larger spacings are needed, there appears to be a conductive layer below 1,600 feet which may represent basalt saturated with fresh water.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr68341","collaboration":"Prepared in cooperation with the Department of Land and Natural Resources of the State of Hawaii and the Institute of Geophysics in Hawaii.","usgsCitation":"Zohdy, A.A., and Jackson, D.B., 1968, Ground-water exploration using the resistivity method on the Hawaiian Islands of Oahu and Hawaii: U.S. Geological Survey Open-File Report 68-341, 39 p., https://doi.org/10.3133/ofr68341.","productDescription":"39 p.","costCenters":[],"links":[{"id":401454,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1968/0341/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":149736,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1968/0341/report-thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Islands of Hawaii and 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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr68307","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1968, Provisional topographic map, Isla Desecheo, Puerto Rico: U.S. Geological Survey Open-File Report 68-307, 1 Plate: 24.23 x 19.66 inches, https://doi.org/10.3133/ofr68307.","productDescription":"1 Plate: 24.23 x 19.66 inches","costCenters":[],"links":[{"id":401305,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0307/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":175531,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1968/0307/report-thumb.jpg"}],"scale":"10000","country":"United States","otherGeospatial":"Isla Desecheo, Puerto Rico","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -67.49382019042969,\n 18.37619363526712\n ],\n [\n -67.46824264526367,\n 18.37619363526712\n ],\n [\n -67.46824264526367,\n 18.39280943659239\n ],\n [\n -67.49382019042969,\n 18.39280943659239\n ],\n [\n -67.49382019042969,\n 18.37619363526712\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a91e4b07f02db65683d","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":530926,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":63916,"text":"gp619 - 1968 - Aeromagnetic map of the Ludlow quadrangle, Hampden and Hampshire Counties, Massachusetts","interactions":[],"lastModifiedDate":"2012-02-10T00:10:52","indexId":"gp619","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"619","title":"Aeromagnetic map of the Ludlow quadrangle, Hampden and Hampshire Counties, Massachusetts","language":"ENGLISH","doi":"10.3133/gp619","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1968, Aeromagnetic map of the Ludlow quadrangle, Hampden and Hampshire Counties, Massachusetts: U.S. Geological Survey Geophysical Investigations Map 619, 1 map., https://doi.org/10.3133/gp619.","productDescription":"1 map.","costCenters":[],"links":[{"id":250239,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0619/report.pdf","size":"33","linkFileType":{"id":1,"text":"pdf"}},{"id":250240,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0619/plate-1.pdf","size":"3048","linkFileType":{"id":1,"text":"pdf"}},{"id":253768,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0619/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -72.5,42.1175 ], [ -72.5,42.25 ], [ -72.36749999999999,42.25 ], [ -72.36749999999999,42.1175 ], [ -72.5,42.1175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691e7d","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":533385,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68439,"text":"ha315 - 1968 - Reconnaissance of the ground-water resources of the Missouri River alluvium between St. Charles and Jefferson City, Missouri","interactions":[],"lastModifiedDate":"2012-02-10T00:11:30","indexId":"ha315","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"315","title":"Reconnaissance of the ground-water resources of the Missouri River alluvium between St. Charles and Jefferson City, Missouri","language":"ENGLISH","doi":"10.3133/ha315","usgsCitation":"Emmett, L.F., and Jeffery, H., 1968, Reconnaissance of the ground-water resources of the Missouri River alluvium between St. Charles and Jefferson City, Missouri: U.S. Geological Survey Hydrologic Atlas 315, 1 map., https://doi.org/10.3133/ha315.","productDescription":"1 map.","costCenters":[],"links":[{"id":185895,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89969,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/315/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"25000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -92.25,38.5 ], [ -92.25,39 ], [ -90.5,39 ], [ -90.5,38.5 ], [ -92.25,38.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db636c50","contributors":{"authors":[{"text":"Emmett, Leo F.","contributorId":67130,"corporation":false,"usgs":true,"family":"Emmett","given":"Leo","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":278216,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jeffery, H. G.","contributorId":74353,"corporation":false,"usgs":true,"family":"Jeffery","given":"H. 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A1-A371, https://doi.org/10.3133/pp600A.","productDescription":"p. A1-A371","costCenters":[],"links":[{"id":119239,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0600a/report-thumb.jpg"},{"id":60530,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0600a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db687803","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":529429,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":58093,"text":"wdrWI6712 - 1968 - Water resources data for Wisconsin, 1967; Part 1. Surface water records and Part 2. Water quality records","interactions":[],"lastModifiedDate":"2012-02-02T00:12:32","indexId":"wdrWI6712","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"WI-67-1-2","title":"Water resources data for Wisconsin, 1967; Part 1. Surface water records and Part 2. Water quality records","language":"ENGLISH","doi":"10.3133/wdrWI6712","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1968, Water resources data for Wisconsin, 1967; Part 1. Surface water records and Part 2. Water quality records: U.S. Geological Survey Water Data Report WI-67-1-2, 228 p., https://doi.org/10.3133/wdrWI6712.","productDescription":"228 p.","numberOfPages":"228","costCenters":[],"links":[{"id":182569,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1967/wi-67-1-2/report-thumb.jpg"},{"id":88322,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1967/wi-67-1-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f1694","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":533206,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":32633,"text":"pp593E - 1968 - Late Eocene nonmarine diatoms from the Beaver Divide area, Fremont County, Wyoming","interactions":[],"lastModifiedDate":"2020-02-28T09:21:21","indexId":"pp593E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"593","chapter":"E","title":"Late Eocene nonmarine diatoms from the Beaver Divide area, Fremont County, Wyoming","docAbstract":"The Beaver Divide is a high escarpment of Tertiary nonmarine strata in central Wyoming separating the Sweetwater Plateau from the relatively low-lying Wind River Basin. The Wagon Bed Formation of middle and late Eocene age and the Beaver Divide Conglomerate Member of the White River Formation-this member being of early Oligocene (Chadronian) age--are exposed near the top of the Beaver Divide in Fremont County, Wyo., about 23 miles southeast of Riverton. The upper part of the Wagon Bed Formation, dated as late Eocene (Uintan) age by Van Houten on the basis of vertebrate fossils, contains a highly silicified fresh-water limestone stratigraphically high in the section with a poorly preserved diatom assemblage. The Beaver Divide Conglomerate Member contains large blocks of similar white limestone, some of which have an assemblage of diatoms the same as that of the Wagon Bed Formation but showing excellent preservation. Both the Wagon Bed limestone and the limestone blocks from the Beaver Divide Conglomerate Member have virtually the same assemblages of nonmarine gastropods. A study of the local geology indicates that a marked erosional topography formed on the Wagon Bed strata before deposition of the Beaver Divide sediments. The Beaver Divide limestone blocks were derived from nearby exposures of the Wagon Bed Formation. The diatom assemblage under consideration was originally deposited in the Wagon Bed limestone and is, therefore, late Eocene rather than early Oligocene in age. This represents the earliest known assemblage of nonmarine diatoms from North America.
The diatom assemblage of the Wagon Bed Formation consists of 27 new species, two species known previously from the upper Miocene of France, and five species still found in living assemblages. One new genus containing two species also occurs in the deposit. The Wagon Bed diatom assemblage is strikingly distinct from later Tertiary fresh-water assemblages in that many diatom genera common to the younger deposits are totally lacking in this Eocene formation. These genera may be absent because of a highly specialized paleoecology during deposition of the Wagon Bed limestone, but the meager evidence provided by the few still-living species suggests nothing more specific than deposition in a temperate circumneutral lake.
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The report area includes about 25,000 square miles of the basin that lie in Nigeria. Most of the area is a featureless plain that slopes gently northeast and east from the uplands of central Nigeria towards Lake Chad. On its eastern side the lake has one surface outlet which overflows only during exceptionally high stages of the lake. This outlet spills into the channel of Bahr al Ghazal, which in turn drains into the Bod616 depression. Because the lake is shallow, the shoreline fluctuates markedly with high and low stages corresponding to the wet and dry seasons. The semiarid climate of Bornu and Dikwa Emirates is characterized by a long dry season and a short wet season that correspond to seasonal winds. Annual rainfall ranges from 15 inches in the northern part of the area to 32 inches in the southern. \r\n\r\nThe Chad Basin in Dikwa and Bornu Emirates is underlain by interbedded sand and clay, collectively termed the Chad Formation. These alluvial and lactustrine sediments were deposited in or near Lake Chad whet it occupied a much greater area during Pliocene and Pleistocene time. The Chad Formation has a very slight primary dip in the direction of Lake Chad and conforms to the gentle slope of land surface. The known thickness of the formation ranges from a few feet where it overlies bedrock on the periphery of the basin to at least 1,800 feet at Maiduguri; however, its total thickness probably exceeds 2,000 feet in the central part of the basin. \r\n\r\nThree water-bearing units termed upper, middle, and lower zones occur within the Chad Formation. The upper zone yields water to numerous dug wells throughout the rural areas and also is .the major source of the Maiduguri municipal water .supply. The middle zone yields water from flowing artesian boreholes that have heads ranging from a few feet to 70 feet above land surface throughout a 13,000 square-mile area of the basin in Nigeria. The lower zone also yields water from flowing boreholes ; however, its areal extent has not been proved beyond the environs of Maiduguri. \r\n\r\nThe present investigation is concerned primarily with the middle zone, which is the source of water for some 190 flowing boreholes used as little-watering points in the Nigerian sector of the Chad Basin. The thickness of loads of waterbearing sand in the middle zone ranges from less than 1 foot to 200 feet, and the artesian head ranges from land surface at Maiduguri to 70 feet above land surface at Lake Chad. The depth to the top of the middle zone in the area of flowing boreholes ranges from 500 to 1,250 feet below land surface. The waterbearing properties of the middle zone differ greatly from place to place. Also, the yields of individual flowing boreholes generally range from 50 to 20,000 imperial gallons per hour (gph). On the basis of water availability, the middle zone can be divided as follows : Areas of high-, moderate-, and low-yield artesian aquifer ; areas of low- and moderate-yield subartesian aquifer ; and an area where the yields from boreholes are insignificant or the aquifer is missing. Recommended maximum rates of long-term withdrawal from individual boreholes for the three artesian areas range from 100 to 5,000 gph with boreholes spaced 5 to 10 miles apart. By limiting flows to the recommended maximum rates, the boreholes should continue to flow for at least 30 years. The present average use per borehole (265 gph in 1965) is considerably less than the recommended maximum rates. \r\n\r\nRecharge to the upper zone occurs in significant but as yet unmeasured quantities, mostly in the vicinity of the major streams. Apparently, however, no significant amount of recharge reaches the middle zone from the Upper zone. Although the middle zone is, in effect, being 'mined' by existing flowing wells, the present (1965) rate of withdrawal i","language":"ENGLISH","publisher":"U.S. Govt. Print. 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(1 folded) :1 map ;27 cm., https://doi.org/10.3133/ofr68116.","productDescription":"22 p. (1 folded) :1 map ;27 cm.","costCenters":[],"links":[{"id":154507,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c7ab","contributors":{"authors":[{"text":"Hadley, R. 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