Home > Iowa Academy of Science > Journals & Newsletters > Proceedings of the Iowa Academy of Science > Volume 4 (1896) > Annual Issue
Document Type
Research
Abstract
Until very recently, geologists working in Iowa have been content to refer the various boulder clays represented in the state to two till sheets, a so called "upper" and "lower," separated in many places by the "forest beds" of McGee, or in other localities by gravels, often in conjunction with a vegetal horizon, the Aftonian of Chamberlin.
Publication Date
1896
Journal Title
Proceedings of the Iowa Academy of Sciences
Volume
4
Issue
1
First Page
58
Last Page
62
Copyright
©1896 Iowa Academy of Science, Inc.
Language
en
File Format
application/pdf
Recommended Citation
Beyer, S. W.
(1896)
"Evidence of a Sub-Aftonian Till Sheet in Northeastern Iowa,"
Proceedings of the Iowa Academy of Science, 4(1), 58-62.
Available at:
https://scholarworks.uni.edu/pias/vol4/iss1/11