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Abstract
The bedrock in Iowa (Hershey, 1969) is generally overlain by deposits of glacial drift and alluvium, which range in thickness from less than 1 foot (0.3 m) to more than 400 ft (18 m), respectively. The configuration of the bedrock surface is the result of a complex system of ancient drainage courses when were developed during a long period of preglacial erosion and during shorter, but more intense, periods of interglacial erosion.
Study Area
Publication type | Report |
---|---|
Publication Subtype | USGS Numbered Series |
Title | Bedrock topography of northeast Iowa |
Series title | IMAP |
Series number | 933 |
DOI | 10.3133/i933 |
Year Published | 1975 |
Language | English |
Publisher | U.S. Geological Survey |
Publisher location | Iowa City, IA |
Contributing office(s) | Iowa Water Science Center |
Description | 2 plates: 27.49 x 47.04 inches and 30.91 x 47.01 inches |
Country | United States |
State | Iowa |
Scale | 25000 |
Online Only (Y/N) | N |
Additional Online Files (Y/N) | N |
Google Analytic Metrics | Metrics page |