Named Betheden formation for Betheden, Winston Co., MS. Unit includes all residual material at top of Midway and below Midway-Wilcox unconformity. Consists of deposits of bauxite, kaolin, bauxitix, and kaolinitic clays and the overlying lignite. Thickness is approximately 25 feet. It gradationally overlies the Porters Creek formation and unconformably underlies the Fearn Springs formation, or the Ackerman formation where the Fearn Springs is absent. The Betheden is of Paleocene or Eocene age.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Fearn Springs and Betheden appear to be intraformational. Author recommends that name Betheden be abandoned and that Fearn Springs include both units.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Betheden Formation is stratigraphic equivalent of Naheola Formation and is discarded by some workers in favor of Naheola. Described in this report as 25 ft of mostly nonmarine quartzose sands. Age generalized as Paleogene.
Source: GNU records (USGS DDS-6; Reston GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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