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National Geologic Map Database
Geologic Unit: Rodessa
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  • Usage in publication:
    • Rodessa Formation
  • Modifications:
    • Overview
  • AAPG geologic province:
    • Mid-Gulf Coast basin
Publication:

Warner, A.J., and Moody, J.S., 1992, West Raymond field [Mississippi]: Mississippi Office of Geology, Mississippi Geology, v. 13, no. 2, p. 13-22.


Summary:

Rodessa Formation consists primarily of land-derived detrital material. In Raymond Field, unit is a 600 to 700-ft section. The lower Rodessa consists of 145 to 275 ft of alternating sands and shales. Sands are 20 to 60 ft thick, white to gray, fine- to medium-grained, and moderately well cemented. The middle Rodessa is 125- to 200 ft thick and consists predominantly of shales and mudstones. Upper Rodessa is referred to in this report as Rodessa Consolidated and contains three distinct sands. Overlies the Pine Island Formation and underlies the Ferry Lake Formation. Age is Early Cretaceous (Comanchean).

Source: GNU records (USGS DDS-6; Reston GNULEX).


For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.

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