Mafic and lesser felsic metavolcanic rocks and greenstone sills interlayered in Hunt Fork Shale and Beaucoup Formation (Brosgé and Reiser, 2000) and, locally, in the Kanayut Conglomerate (Mull and Werdon, 1994). It is mappable as two separate metavolcanic units in most places: a mafic metavolcanic and a felsic metavolcanic unit. Mafic unit consists of pillow basalt, amygdaloidal basalt, and basalt capped by tuffaceous limestone, commonly schistose and altered to calcic greenstone; may, in part, have been olivine basalt flows, about 10 to 80 m thick (Brosgé and others, 1979). Unit also includes younger (presumed Carboniferous) mafic to intermediate metavolcanic rocks in the Howard Pass quadrangle that are associated with limestone of the Lisburne Group and the Nuka Formation (Mull and Werdon, 1994). Felsic rocks, a minor part of the unit, include metamorphosed crystal and lithic tuff, volcanic breccia, and minor porphyry of rhyolitic compositions, now mostly recrystallized to fine crystalline quartz-sericite schist (Brosgé and Reiser, 2000). This unit is distinct form the Ambler sequence (unit Das) in being typically associated with the Hunt Fork Shale (unit Degh) and in being a dominantly mafic unit