Loess deposits of Neotoma Valley
Advisor:White, Sidney E.
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Publisher:The Ohio State University
Series/Report no.:The Ohio State University. Department of Geology and Mineralogy Senior Theses; 1973
Neotoma Valley contains deposits of Illinoian and Wisconsin waterlaid loess which form various topographic features throughout the valley. Illinoian lake clays occupy the flat valley bottom. These lake sediments formed as a result of damming of the valley by lllinoian outvash gravels. Topographic features in the valley are partially due to post-Illinoian erosion.