Unit consists of poorly known limestone and associated rocks generally found as lenses accompanying rocks of unit |<rqm in central Alaska, in isolated exposures ranging from the southern Brooks Range to the Kaiyuh Mountains south of the Yukon River. Best described part of unit is “gray to white, partly to wholly recrystallized limestone, marble, dark-gray dolomitic marble, and impure schistose limestone. Unit occurs in layers as much as 25 m thick intercalated with quartz-mica schist, mica schist, graphitic schist, metabasite, and quartzite. Some contacts are gradational; others are sharp and may be faulted. Unit contains conodonts of Middle Ordovician age in the Nulato quadrangle and poorly preserved corals of Ordovician to Late Mississippian age in Ruby quadrangle” (Patton and others, 2009). In the Tanana quadrangle, unit is light- to medium-gray or tan platy limestone and massive-bedded silicified limestone and dolostone and has extensive locally developed boxwork silica contains sparse conodonts of Famennian age (J.N. Dover, written commun., 1997). In the southeast Circle quadrangle of central Alaska, small bodies of coarse-grained marble are present in the Paleozoic or Precambrian pelitic schist of the region (unit PzPxyqm)