Home > Iowa Academy of Science > Journals & Newsletters > Proceedings of the Iowa Academy of Science > Volume 55 (1948) > Annual Issue
Document Type
Research
Abstract
The silt bottomed prairie lakes of Clay and Palo Alto Counties, Iowa, have shallow, hard, alkaline, turbid waters. They are located in the youngest of the glacial drifts, in which the soils are highly calcareous and rich in mineral salts. The more shallow lakes with relatively flat, saucer-like basins, support a rich population of rooted, submerged, and emergent vegetation which minimizes wave action. The lakes whose basins are deeper than four feet are unfavorable to the growth of emergent vegetation and rooted submerged types do not survive the wave action except in the shallow waters along the depositing shores.
Publication Date
1948
Journal Title
Proceedings of the Iowa Academy of Science
Volume
55
Issue
1
First Page
171
Last Page
177
Copyright
©1948 Iowa Academy of Science, Inc.
Language
en
File Format
application/pdf
Recommended Citation
Hayden, Ada
(1948)
"A Quarterly Standard Mineral Analysis of the Waters of Four Iowa Lakes in the Ruthven Area,"
Proceedings of the Iowa Academy of Science, 55(1), 171-177.
Available at:
https://scholarworks.uni.edu/pias/vol55/iss1/21