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Geologic Unit: Powwow
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Map showing publication footprint
  • Usage in publication:
    • Powwow conglomerate member
  • Modifications:
    • Original reference
  • Dominant lithology:
    • Conglomerate
    • Red beds
Publication:

King, P.B., and King, R.E., 1929, Stratigraphy of outcropping Carboniferous and Permian rocks of Trans-Pecos Texas: American Association of Petroleum Geologists Bulletin, v. 13, no. 8, p. 907-926. [Available online, with subscription, from AAPG archives: http://www.aapg.org/datasystems or http://search.datapages.com]


Summary:

Pg. 909, 911. Powwow conglomerate member of Hueco limestone restricted. Above the beds of Strawn age are limestones containing Canyon and Cisco fossils. CHAETETES is absent, and a zone of FUSULINELLA MEEKI occurs at base. Uppermost beds contain Cisco fusulinids (identifications of C.O. Dunbar). Near top is a member of conglomerate and red beds, which is folded with the rest of the Carboniferous. The red beds are well exposed 2 to 5 miles south of Hueco Canyon along main escarpment of Hueco Mountains. [Age is considered Permian(?).]
Named from Powwow Canyon [now spelled Pow Wow Canyon] 3.5 mi south of Hueco Canyon, which is followed by the new El Paso-Carlsbad highway [U.S. Route 62 / 180], Hueco Mountains, [Helms West Well and Phone Line Canyon 7.5-min quadrangles, El Paso and Hudspeth Cos.], western TX.
[Additional locality information from USGS GNIS database and USGS historical topographic map collection TopoView, accessed on September 10, 2023.]

Source: Modified from US geologic names lexicon (USGS Bull. 896, p. 1724).


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

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