zzzzzPg. 93-94. Fresnal Conglomerate. Pebble- to boulder-size fragments. Interbedded andesites in upper part, possibly the "turkey track" andesite to which Cooper assigned a Miocene age. Thickness about 2,000 feet. Top of section in area under study. Rests unconformably on unit 2 which is composed of andesite, rhyolite, and breccia. Derived from older rocks. Age is Miocene. Report includes columnar section.
Type locality not designated. Present in Fresnal Canyon, Baboqivari Mountains, Pima Co., southeastern AZ.
Source: GNU records (USGS DDS-6; Denver GNULEX); US geologic names lexicon (USGS Bull. 1350, p. 276).
Pg. I11. Unconformably overlies Chiuli Shaik Formation (new).
Source: US geologic names lexicon (USGS Bull. 1350, p. 276).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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