Deep‐seated solution in the Meade basin and vicinity, Kansas and Oklahoma

Eos, Transactions, American Geophysical Union
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Abstract

During the closing years of the 19th century, Haworth [see 1 and 2 of “References” at end of paper] and Johnson [3] noted the abundant depressions resembling sink‐holes in the Southern High Plains, especially in Meade and Clark counties, Kansas, and Beaver County, Oklahoma. Johnson was of the opinion that all the depressions and basins in this region were due to solution, whereas Haworth [1] believed the Meade artesian basin to be structural, although he held to a solutional origin for the Ashland and Englewood basins, which are a few miles to the east. ©1942. American Geophysical Union. All Rights Reserved.

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Additional publication details

Publication type Article
Publication Subtype Journal Article
Title Deep‐seated solution in the Meade basin and vicinity, Kansas and Oklahoma
Series title Eos, Transactions, American Geophysical Union
DOI 10.1029/TR023i001p00035
Volume 23
Issue 1
Year Published 1942
Language English
Publisher American Geophysical Union
Description 5 p.
First page 35
Last page 39
Country United States
State Kansas, Oklahoma
County Meade, Clark, Beaver
Other Geospatial Meade basin
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