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- W168285909 abstract "The late Wisconsin boundary at Paint Creek valley west of Chillicothe is anomalous. An inlier of Illinoian age drift lies north of the valley and within it is ground moraine complexes of late Wisconsin age surrounding Illinoian age kames. Moreover Illinoian age lake deposits are intermixed with Wisconsin age outwash units. This problematic distribution prompted recent mapping and stratigraphic analysis which identified at least five major ice marginal complexes. North to south they are: High Paint Creek (NW or N source), Owl Creek (NE source), Biers Run (N source), Dry Run (NE source), Deer Creek ( ). The areal distribution of these marginal complexes indicates that recession was incremental with limited meltwater drainage. Radiocarbon ages place the age of the Biers Run drift after 17.8 ka. The distribution of landforms allows at least two hypotheses: either extremely low profile ice-tongues flowed into the Paint Creek Valley from either side or thicker, cold based ice overtopped the Illinoian ridgeline'' filling the valley. Given the altitudinal control on drift limits and the presence of fresh moraine on the uplands south of the Paint Creek valley, the author adopts the later hypothesis and if true, it implies a cold based ice margin atmore » the southernmost limit of the Laurentide Ice Sheet.« less" @default.
- W168285909 created "2016-06-24" @default.
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- W168285909 date "1993-03-01" @default.
- W168285909 modified "2023-09-28" @default.
- W168285909 title "The late Wisconsin boundary of the Scioto sublobe near Chillicothe, Ohio" @default.
- W168285909 hasPublicationYear "1993" @default.
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