Pg. 75-91. Arkansas marls. In valley of Arkansas north of Poncha Pass, [Freemont County], central southern Colorado, is a fine development of light-colored marls, doubtless of same age as Santa Fe marls, which I have designated by name of Arkansas marls. They occupy entire valley of the Arkansas, which is about 40 miles long and 5 to 10 miles wide. Assigned to Pliocene.
[GNC remark (ca. 1936, US geologic names lexicon, USGS Bull. 896, p. 72): †Arkansas marls abandoned. Same as Santa Fe formation, of late Miocene and Pliocene age.]
Source: US geologic names lexicon (USGS Bull. 896, p. 72).
Rocks in Eagle basin assigned to Arkansas marl by Hayden (1869) are reassigned to the Miocene and Pliocene Dry Union Formation in this report.
Source: GNU records (USGS DDS-6; Denver GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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