Thin- to thick-bedded lithic graywacke, siltstone, and argillite turbidites, and interbedded conglomerate, limestone, and volcanic rocks (Rossman, 1963; Muffler, 1967; Loney and others, 1975; Eberlein and others, 1983; Brew, 1996). Turbidite beds commonly have laminar, cross-bedded, graded, and load cast structures typical of full and partial Bouma sequences (Muffler, 1967; Karl and Giffen, 1992). The olistostromal conglomerate is commonly polymictic and contains clasts of granitic and gabbroic rocks, greenstone, graywacke, chert, and limestone blocks thought to have been derived from local sources, but is locally monomictic (Muffler, 1967; Brew and others, 1984; Karl and Giffen, 1992; Brew, 1996; Karl and others, 1999). Sandstone grains consist of volcanic rock fragments, mudstone, slate, chert fragments, and grains of plagioclase, calcite, and quartz (Muffler, 1967; Karl and Giffen, 1992). Mafic to intermediate flows, breccia, and tuff are reported by several sources (Brew and others, 1984; Brew, 1996; Karl and others, 1999); where separately mapped, they are included in unit Sv here. Includes clastic rocks of the Rendu and Tidal Formations in Glacier Bay (Rossman, 1963), the Point Augusta Formation on Chichagof Island (Loney and others, 1975), Bay of Pillars Formation on Kupreanof Island (Muffler, 1967; Brew, 1996), and polymictic olistostromal conglomerate interbedded within the Heceta Limestone (unit DSl) in the Prince of Wales Island area (Brew, 1996; Karl and others, 1999). Also includes shallow water carbonaceous sedimentary rocks of the Staney Creek area on Prince of Wales Island, which consists of limestone, siltstone, calcareous mudstone, and polymictic conglomerate (Eberlein and others, 1983). Age is primarily derived from Silurian graptolites in the Bay of Pillars and Point Augusta Formations (Muffler, 1967; Loney and others, 1975) and the sedimentary rocks of the Staney Creek area (Eberlein and others, 1983), but the unit is also locally interbedded with fossiliferous Silurian limestone (Shpa). Poorly preserved Early Jurassic radiolarians (C.D. Blome, written commun. (1996), reported by D.A. Brew, written commun., 2004), in an argillite and chert section of rocks unconformably overlying this unit in the northwestern Juneau quadrangle, are unique to southeast Alaska. As the outcrop area is extremely small, and documentation of this occurrence is lacking or conflicting, it is not shown separately here