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Document Type

Research

Abstract

Despite the circumstance that in the Iowa part of the Great Plains, lying between the Mississippi River and the Rocky Mountains, the deep well-drillings usually sink only to that famed aquifer, or artesian reservoir, the Peter sandstone, the ancient crystalline basement beneath all of the tall column of sedimentaries is entered in a number of instances. Touching the deeply buried pre-Cambric rocks in the northeastern part of the State is not so surprising inasmuch as soon beyond our boundaries these crystallines rise to the surface.

Publication Date

1928

Journal Title

Proceedings of the Iowa Academy of Science

Volume

35

Issue

1

First Page

220

Last Page

222

Copyright

©1928 Iowa Academy of Science, Inc.

Language

en

File Format

application/pdf

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