Pg. 121-122. Cassel Hill member of Catahoula formation. Loose, noncalcareous sands and sandy clays which commonly contain considerable silicified wood; occurs at base of the Catahoula. Thickness as much as 45 feet; near Cassel Hill 15 to 25 feet thick. Unconformably overlies Vicksburg formation. Separated from overlying Chalk Hills member (new) by an interval of massive sandstone and gray tuff. Age is Miocene.
Well developed in vicinity of Cassel Hill, in NE/4 sec. 9, T. 10 N., R. 5 E., Catahoula Parish, east-central LA.
Source: US geologic names lexicon (USGS Bull. 1200, p. 661).
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