Pg. 29-40. Coonewah bed of Annona Chalk. Name applied to a 2-ft bed of relatively pure chalk near the top of the Annona. Age is Late Cretaceous.
Type locality: west valley wall of Coonewah Creek, 2.5 mi west of Verona, approx. at southeast corner of SW/4 sec. 22, T. 10 S., R. 5 E., Lee Co., northern MS.
[Coonewah Bed now (ca. 1960) included in Demopolis Formation; Annona restricted from MS.]
Source: US geologic names lexicon (USGS Bull. 1200, p. 927).
Assigned to lower portion of Demopolis Formation along with the X-point of Stearns (1957). Shown in fig. 4 as occurring in MS and TN.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Coonewah Bed of Demopolis Formation. Lies within "middle chalk member" of Demopolis Formation. Intertongues with Selma Chalk (Selma Group) of downdip (south) area. Age is Late Cretaceous (late Campanian; Tayloran Provincial Age); planktic foram zone G. CALCARATA (of Caron, 1985), calcareous nannofossil zones CC21 to CC22.
Source: Publication.
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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