Typical exposures are in upper basin of Tatina River (formerly called Rohn River), Alaska Range, southwestern and southern AK. Traced from Tatina River to east fork of Toklat and appears to constitute most of inland slope of mountains. Rocks in part were called Terra Cotta series by Spurr (1900). Consists of blue limestones interbedded with black carbonaceous argillites and thin-bedded siliceous limestones and calcareous slates. Is 4000 to 5000 ft thick. Separated from younger Tonzona group (new) by fault. Age is Ordovician and possibly in part Silurian(?) based on graptolites from lower part of unit. Fossils identified by Charles Schuchert. Upper part of group yielded no fossils.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
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