First use of Spor Mountain flows and latite flows. Age is late Tertiary.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Named for Spor Mountain. Type section is in secs 8 and 9, T13S, R12W, Juab Co, UT, Great Basin province. Divided into a beryllium tuff member (base) 20-60 m thick and a porphyritic rhyolite member (top) about 500 m thick. Basal member is a stratified, tan vitric tuff and tuffaceous breccia with abundant clasts of carbonate rocks and a few clasts of quartzite and volcanic rocks. Thin beds of bentonite, ash-flow tuff, epiclastic sandstone and conglomerate also present in basal member. Upper member consists of flows, domes, and plugs of gray to red porphyritic rhyolite and alkali rhyolite erupted from vents around Spor Mountain. Is younger than Needles Range Formation. Is older than Topaz Mountain Rhyolite. Of early Miocene age.
Source: GNU records (USGS DDS-6; Denver GNULEX).
Has an average age of 21.3 +/-0.2 m.y. Minerals dated were sanidine and zircon. Is separated from older rocks and from the younger Topaz Mountain Rhyolite by unconformities. Of early Miocene age. In Great Basin province.
Source: GNU records (USGS DDS-6; Denver GNULEX).
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