Loess deposits of Neotoma Valley
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Date
1973-06
Journal Title
Journal ISSN
Volume Title
Publisher
The Ohio State University
Abstract
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.