Black argillite, thin-bedded black chert, thin-bedded black limestone, brown calcareous and carbonaceous wacke sandstone, graywacke, and dull green pillow basalt. The chert, argillite, and limestone contain radiolarians. Graywacke clasts include mainly chert, with subordinate limestone, sandstone, argillite, and volcanic rock fragments. Pillow basalts have interbeds of argillite and gray green tuffaceous siltstone. Karl and others (2010, p. 2) indicated that deformed, quartz-veined black chert and argillite containing Ordovician graptolites (Carter, 1977) grade upward to carbonaceous argillite, chert, chert sandstone grit, meter-scale lenses of pillow basalt, and thinly laminated black limestone containing Silurian-Devonian conodonts (A.G. Harris, written commun., 1995). Crisscrossing quartz veinlets in the Hood Bay Formation, which are absent in the Cannery Formation (unit PDcf), are inferred to represent a pre-Cannery deformation event