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- W2013052024 abstract "The preglacial Teays River, which rose in Tertiary time in the vicinity of the Blue Ridge in North Carolina, flowed across north-central Indiana and turned south through the present lower Wabash Valley to discharge its water into the Gulf Embayment in the vicinity of the southern tip of Illinois. That portion of the valley in northern Indiana, as well as that in western Ohio, was buried beneath the Pleistocene glacial plain. Its route across this area has been traced, by means of well records. Along the west side of Indiana the present Wabash River flows in the deeply alluviated Teays Valley. Well records in the lower Wabash Valley indicate the position of the preglacial valley floor. The Teays Valley in Indiana has a gradient of approximately 8 inches per mile; the buried bedrock floor drops from an altitude of 463 feet in northwestern Jay County to an altitude of 229 feet in southwestern Posey County." @default.
- W2013052024 created "2016-06-24" @default.
- W2013052024 creator A5035505229 @default.
- W2013052024 date "1943-08-01" @default.
- W2013052024 modified "2023-09-25" @default.
- W2013052024 title "The Preglacial Teays Valley in Indiana" @default.
- W2013052024 doi "https://doi.org/10.1086/625164" @default.
- W2013052024 hasPublicationYear "1943" @default.
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