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The AAPG/Datapages Combined Publications Database
AAPG Bulletin
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The Travis Peak formation and its members were named and described by Hill in 1889. At the type locality in Travis County, the formation consists of the Sycamore sands and conglomerates, composing the lowest member, the Cow Creek limestones and shell beds forming the middle member, and the Hensell sands and marls comprising the upper member. The Travis Peak thickens in the subsurface east, south, and southwest of the type locality. With the exception of the basal conglomerates, the beds of the Travis Peak are uniform throughout the exposures. The fossiliferous Cow Creek is the most persistent of the three members.
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