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.
Proceedings of the Iowa Academy of Science
© Copyright 1967 by the Iowa Academy of Science, Inc.
Dorheim, Fred H.
"Stratigraphic Leak at Springville Quarry,"
Proceedings of the Iowa Academy of Science: Vol. 74:
, Article 24.
Available at: https://scholarworks.uni.edu/pias/vol74/iss1/24