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Document Type

Research

Abstract

Lime Creek Shale, containing an Upper Devonian conodont fauna, is exposed below Middle Devonian rocks at a quarry near Springville, Iowa. The occurrence is interpreted as a stratigraphic leak and is cited as further evidence of this condition occurring in a karst Devonian terrain.

Publication Date

1967

Journal Title

Proceedings of the Iowa Academy of Science

Volume

74

Issue

1

First Page

142

Last Page

146

Copyright

© Copyright 1967 by the Iowa Academy of Science, Inc.

Language

EN

File Format

application/pdf

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