Pg. 24, 31, 39; see also Univ. Texas Bull., no. 2132, p. 161-166. Belknap limestone member of Harpersville formation. Lies 30 to 50 feet below top of formation. Is traceable a long distance.
Source: US geologic names lexicon (USGS Bull. 896, p. 150).
Pg. 161-166; see also Jour. Geol., v. 30, p. 24, 31, 39, 1922. Belknap limestone lentil of Harpersville formation. Yellow to buff limestone, nodular, 2 to 4 feet thick, locally very fossiliferous. Lies 60 to 80 feet above Crystal Falls limestone lentil of Harpersville formation and 30 to 50 feet below top of formation. [Age is Pennsylvanian.]
Named from old Fort Belknap, Young Co., Bravos River region, central northern TX; typical exposures in vicinity of Newcastle, Young Co., where it lies above the workable coal bed. [Absent from Colorado River Valley.]
Source: US geologic names lexicon (USGS Bull. 896, p. 150).
Belknap limestone member of Thrifty formation. The USGS currently [ca. 1966] classifies the Belknap as a member of the Thrifty Formation. Term Harpersville abandoned. Recognized in central northern Texas. Age is Late Pennsylvanian.
Source: US geologic names lexicon (USGS Bull. 1200, p. 283).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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