Unit is named the Hull meta-andesite. Consists of greenish to reddish meta-andesite resembling the Fant meta-andesite. Prevailing type is greenish and essentially non-porphyritic; occasionally in the Little Grizzly Creek region it is decidedly amygdaloidal. Is only partially crystalline. Much of it is in more or less well-defined sheets representing lava flows and tuff. In places is decidedly slaty. It penetrates the Mormon sandstone and Foreman formation. Age is most likely Late Jurassic. (B896)
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Age of the Hull Meta-andesite is revised from Late Jurassic to: Middle Jurassic (Bathonian).
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Hull Meta-andesite is abandoned as it is a mixture of volcanic rocks of widely divergent ages that serves only to confuse the stratigraphic an structural relations on Mt. Jura. Its rocks are reassigned to the Fant Meta-andesite and as unnamed rocks.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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