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Teays River

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Series: GSA Special Papers
Published: 01 January 1991
DOI: 10.1130/SPE258-p29
... The Old Kentucky River system was a major contributor to the Teays River, draining southwestern Ohio and much of eastern Kentucky. The trunk river flowed northward from southeastern Kentucky throughout Frankfort and Carrollton, and then past Cincinnati and Dayton, joining the Teays River near...
Series: GSA Special Papers
Published: 01 January 1991
DOI: 10.1130/SPE258-p19
... Three transects were conducted across the main channel of the abandoned Teays River valley in Pike, Jackson, and Scioto Counties, Ohio, to evaluate the lithology and general stratigraphy of valley-fill deposits. Field observations obtained from both deep borings and surface excavations indicate...
Series: GSA Special Papers
Published: 01 January 1991
DOI: 10.1130/SPE258-p9
... At some time during the Pleistocene Epoch, a part of the modern Ohio River drainage system in Ohio and West Virginia developed in response to impoundment of the ancestral Teays River drainage system. Rhythmites formed in the lacustrine slackwaters and remain today, extending as much as 150...
Journal Article
Journal: GSA Bulletin
Published: 01 November 1973
GSA Bulletin (1973) 84 (11): 3677–3688.
...JAMES T. TELLER Abstract The preglacial rivers of southwestern Ohio, northern Kentucky, and southeastern Indiana flowed toward the north and joined with the west-flowing trunk river, the Teays, in central Ohio. The main tributary valleys to the Teays River in this region—containing the Old Kentucky...
Series: GSA Special Papers
Published: 01 January 1991
DOI: 10.1130/SPE258-p43
... Configuration of the buried part of the Teays Valley system across western Ohio, Indiana, and eastern Illinois suggests that the Teays is not a preglacial system, but rather, that it was formed marginal to a major glacier earlier than that which created the Ohio River, probably in similar...
Journal Article
Journal: GSA Bulletin
Published: 01 March 1963
GSA Bulletin (1963) 74 (3): 251–274.
...EDWARD C RHODEHAMEL; CHARLES W CARLSTON Abstract The segment of the abandoned pre-Pleistocene Teays Valley between Scary and Huntington, W. Va. stands 130–240 feet above the Ohio and Kanawha rivers, and its bedrock floor slopes westward at about 0.6 foot per mile. The bedrock floor is overlain...
Journal Article
Published: 01 September 1961
Journal of Sedimentary Research (1961) 31 (3): 456–466.
...Constantine Manos Abstract Samples of sediments from just above the bedrock of the valley bottom of the ancient Teays and Mahomet rivers were taken in unglaciated regions of West Virginia and Ohio, and from beneath glacial drift in Ohio and Illinois and analyzed for heavy mineral content. Analysis...
Series: GSA Field Guide
Published: 10 December 2018
DOI: 10.1130/2018.0051(07)
EISBN: 9780813756516
... Episode in the Middle Pleistocene, the Sangamon interglacial, and the Late Pleistocene Wisconsin Episode. The Old Kentucky River was tributary to the Teays, depositing sands at ca. 1.5 Ma, confirmed by multiple 10 Be- 26 Al cosmogenic radionuclide burial ages. Glacial till uncoformably overlies Old...
FIGURES | View All (11)
Series: GSA Field Guide
Published: 10 December 2018
DOI: 10.1130/2018.0051(12)
EISBN: 9780813756516
... of the upper Wabash River, to the confluence with the late Tertiary Teays Bedrock Valley, with major emphasis on how the depositional framework and diagenetic history of the Late Silurian reef archipelago continue to reverberate in the modern geomorphic response of the valley to Pleistocene events. The first...
FIGURES | View All (46)
Journal Article
Journal: GSA Bulletin
Published: 01 July 2001
GSA Bulletin (2001) 113 (7): 825–836.
... on the Mississippi fan increased at this time, consistent with extensive glaciation in the watershed. It is possible that the Teays River formed along the glacial margin at this time at the latitude of central Indiana and Ohio ( Fig. 1 ; Gray, 1991 ). Although ice lobes reached far south, they did not reach...
FIGURES | View All (5)
Journal Article
Journal: AAPG Bulletin
Published: 01 August 2004
AAPG Bulletin (2004) 88 (8): 1041–1047.
... Pleistocene valleys that are buried by as much as 182 m (600 ft) of till sand and silt form world-class aquifers ( Goldthwait, 1979 ), the best known of which is the buried Teays Valley that extends northwest from Chillicothe to Celina, Ohio. Channels filled by the Mississippian Berea Sandstone are commonly...
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Series: Geological Society, London, Special Publications
Published: 02 December 2019
DOI: 10.1144/SP488-2018-166
EISBN: 9781786204639
.... ( a ) Interpreted Pliocene drainage, where an ancestral Wisconsin River (W) and ancestral upper Ohio system (T and P for the Teays and Pittsburgh rivers, respectively) drained to the St Lawrence Seaway and the Atlantic Ocean, and a smaller upper Mississippi (UMi) and Ohio (O) drainage contributed to the Missouri...
FIGURES | View All (20)
Series: GSA Special Papers
Published: 01 January 2006
DOI: 10.1130/2006.2404(05)
... for the ancient Teays River system before its destruction during a major glacial cycle. Utilization of the sediment record in cave regions west of the Mississippi River may independently date Pliocene-Pleistocene drainage changes in the Upper Mississippi River basin associated with the development of ice lobes...
Series: GSA Field Guide
Published: 01 January 2012
DOI: 10.1130/2012.0027(03)
EISBN: 9780813756271
...-scale changes in tributary streams in response to human impacts and land use change over 10 1 –10 2 years, to diurnal and event-driven changes in water quality over 10 –2 to 10 –3 years. Drainage network changes in the Little Miami River and Mad River systems occurred through stream capture and were...
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Series: GSA Field Guide
Published: 01 January 2017
DOI: 10.1130/2017.0046(02)
EISBN: 9780813756462
... Allegheny River). White (1896) calculated that the surface of Lake Monongahela could not have risen much above 335 m (1100 ft) based on cols identified in Salem and Weston, West Virginia. He suggested that these cols formed spillways allowing lake water to flow into the ancient Teays River basin, the “pre...
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Series: GSA Field Guide
Published: 10 December 2018
DOI: 10.1130/2018.0051(11)
EISBN: 9780813756516
... sedimentation in the West Fork White River valley and tributaries began ca. 27 k cal yr B.P. and continued until ca. 20.5 k cal yr B.P., representing the timing of ice sheet advance into and out of the paleo–White River drainage basin. Ice sheet advance and retreat rates average ~40 m/yr before and after...
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Series: GSA Special Papers
Published: 01 January 1991
DOI: 10.1130/SPE258-p79
..., discontinuous lentils of sand confined within lacustrine clays. Valley-fill aquifers are confined by capping till units, except where exhumed at the crossings of the Maumee-Wabash Trough (modern Wabash River Valley). A variety of aquifers typically are available within the valley-capping sediments...
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1998
AAPG Bulletin (1998) 82 (5): 701–728.
... increases occurred as the Ohio, western Appalachian, upper Missouri, and Great Plains rivers changed course ( Figure 4 ). Permanent capture of these drainage systems by the Mississippi River started around the beginning of the Pleistocene with the paleo-Ohio (Teays) River and western Appalachians drainage...
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Journal Article
Journal: GSA Bulletin
Published: 01 July 2010
GSA Bulletin (2010) 122 (7-8): 1047–1066.
... Mahomet aquifer, except near a river where stacked sands may have created a hydrologic window to the Mahomet aquifer. It appears that most of the Mahomet aquifer is well protected from surficial contamination. The approach used in this study enabled us to better understand and identify the processes...
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Journal Article
Journal: GSA Bulletin
Published: 01 March 2014
GSA Bulletin (2014) 126 (3-4): 447–458.
... studies below the St. Maurice (Québec, Fig. 1 ; Crosby, 1932 ), Hudson (New York; Kemp, 1908 ), Mohawk (New York, Fig. 2 ; Simpson, 1949 ), Teays (Indiana; Fidlar, 1943 ), Mahomet (Illinois; Horberg, 1945 ), Kennebec (Maine; Crosby, 1945 ), and Connecticut (New Hampshire; Crosby, 1945 ) river...
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