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Field and Laboratory

Publication Date

1-1-1940

Abstract

At many localities along the outcrop of the Austin formation in Dallas County, Texas, channel fillings apparently composed of reworked bedrock occur at levels above the highest stream terraces. If a post-Cretaceous chronology for this portion of Texas is to be formulated, these channel fillings must be taken into account. A more immediate problem, however, is that of the origin of the fillings themselves.

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Creative Commons Attribution-Noncommercial 4.0 License
This work is licensed under a Creative Commons Attribution-Noncommercial 4.0 License

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