[Presumably named for Nabesna River, Wrangell Mountains, southern AK]. Type not designated. Consists of generally thick-bedded, mostly white limestone and darker gray or bluish dolomitic limestone comprising a "series of limestones occurring on the upper Nabesna and Chisana rivers ... almost entirely restricted to the Wrangell Mountains". No age-diagnostic fossils found within unit; age regarded as Permian based on regional biostratigraphic correlations.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Unit thickness at White Mountain is approximately 2000 ft. Age is considered to be Late Triassic [overall] based on occurrence of age-diagnostic fossils (including MONOTIS) from correlative limestones to the east in Snag Creek valley and nearby locales.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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