Pg. 47, geol. map. Campagrande formation of Fredericksburg group. Limestone conglomerate, 25 feet thick, overlain by 350 feet of gray limestone, generally massive but locally containing nonpersistent thin-bedded limestone grading into shale. Basal formation of Fredericksburg group. Underlies Cox formation and unconformably overlies Hueco formation [Pennsylvanian] in central part of Finlay Mountains. Age is Early Cretaceous (Comanche).
Named from Campagrande Draw, in Finlay Mountains, El Paso Co. [now in Hudspeth Co.], western TX.
Source: US geologic names lexicon (USGS Bull. 896, p. 324-325).
Transferred this formation to Trinity group. Age is Early Cretaceous (Comanche).
Source: US geologic names lexicon (USGS Bull. 896, p. 324-325).
King, P.B., 1953, IN King, P.B., and Flawn, P.T., Univ. Texas Bur. Econ. Geol. Pub., no. 5301, p. 99-100, pls. 1, 3. Referred to as Campagrande limestone. In Van Horn area, made up of several beds of massive ledge-making light-gray limestone, in part sandy or conglomeratic, and of nodular limestone and marl; at base is conglomerate containing chert and limestone fragments largely derived from the Hueco limestone. Thickness in Streeruwitz Hills 100 to 140 feet; in other areas 30 to 60 feet. Underlies Cox sandstone. Age is Early Cretaceous (Comanche).
Source: US geologic names lexicon (USGS Bull. 896, p. 324-325).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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