Dell Tuff. Gray to pink rhyolitic ash-flow tuff. Chiefly crystals of quartz, sanidine, biotite, and plagioclase in a poorly welded to unwelded matrix of devitrified shards and pumice. Thickness 180 m. Unconformably overlies Drum Mountains Rhyodacite, or locally overlies Oligocene(?) breccia at Spor Mountain or Paleozoic rocks; unconformably underlies Spor Mountain Formation. Age is Oligocene, based on average fission-track age of 32 Ma.
Type locality: The Dell, in secs. 23 and 24, T. 12 S., R. 12 W., Thomas Range, Juab Co., western UT. Named from The Dell.
Source: US geologic names lexicon (USGS Bull. 1564, p. 44-45).
Is an Oligocene unit--a simple cooling unit--limited to Thomas Range and Key Mountains, in the Great Basin province. Has an average isotopic age of 32.0+/-0.6 Ma.
Source: GNU records (USGS DDS-6; Denver GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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