Home > Iowa Academy of Science > Journals & Newsletters > Proceedings of the Iowa Academy of Science > Volume 21 (1914) > Annual Issue
Document Type
Research
Abstract
It is well known that several systems of drainage lines have been impressed upon the surface of the present state of Iowa, only to be successively wiped out by the hand of time. Not to mention possible earlier ones, a well-marked drainage system was cut into the Saint Louis and older strata prior to Des Moines time. Upon the (relative) subsidence of the land during Des Moines time the valleys were filled and drainage lines obliterated to the farthest limits of deposition of Coal Measures rocks. Differences of nearly 400 feet in the altitude of the Saint Louis surface near Des Moines give evidence of the vigor of the erosive forces and the lapse of time during which degradation was active. At least some of the Coal Measures outliers of eastern Iowa may occupy depressions cut during this period, and, as Doctor Calvin pointed out, the land surface of that time, probably stood higher than at present, since the base of the Coal Measures sandstones of the Iowa City outlier is sixty feet below present river level. Beyond the eastern limits of the Des Moines strata the drainage systems doubtless continued for a long time, though at times sluggish and ineffective as erosive agents.
Publication Date
1914
Journal Title
Proceedings of the Iowa Academy of Science
Volume
21
Issue
1
First Page
173
Last Page
181
Copyright
©1914 Iowa Academy of Science, Inc.
Language
en
File Format
application/pdf
Recommended Citation
Lees, James H.
(1914)
"Earth Movements and Drainage Lines in Iowa,"
Proceedings of the Iowa Academy of Science, 21(1), 173-181.
Available at:
https://scholarworks.uni.edu/pias/vol21/iss1/25