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National Geologic Map Database
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  • Usage in publication:
    • Hunsaker Member
  • Modifications:
    • Named
  • Dominant lithology:
    • Rhyolite
  • AAPG geologic province:
    • Permian basin
Publication:

Parker, D.F., 1986, Stratigraphic, structural, petrologic development of Buckhorn caldera, northern Davis Mountains, Trans-Pecos Texas, IN Price J.G., and others, eds., Igneous geology of Trans-Pecos Texas; field trip guide and research articles: University of Texas-Austin, Bureau of Economic Geology Guidebook, no. 23, p. 286-302.


Summary:

Named as middle member of the Huelster Formation. Probably named for the old Hunsaker ranch, Jeff Davis Co, TX, in the Permian basin. No type locality designated. Is a massive tuff-breccia occurring in the Madera Canyon, northern Davis Mountains of west-central TX, about 2 km northeast of the old Hunsaker ranch. Composed of angular fragments of up to approximately 25 cm diameter of sparsely porphyritic gray rhyolite. This rhyolite is set in a variable amount of tuffaceous matrix. Mostly the tuff-breccia is structureless, forming rounded, light-brown, moderately rugged outcrop. In several localities crude bedding occurs. A maximum thickness of about 300 m is reached in a small canyon about 1 km south of entrance to Madera Canyon. Overlies mafic lava and sedimentary rock of Huelster Formation; underlies either Gomez Tuff or trachytic lava. Geologic map. Chemical analyses. Correlation chart. Of Oligocene age.

Source: GNU records (USGS DDS-6; Denver GNULEX).


For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.

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