Predominantly medium-grained composite plutons of granite and quartz monzonite and lesser granodiorite and quartz syenite. Biotite is the chief mafic mineral and hornblende is locally present, especially in the granodiorite phases. Muscovite is a common component of the granite. Unit is widespread, although the bulk of the exposure is in the western Alaska Range and Tyonek quadrangle or spatially associated with the Alaska-Aleutian Range batholith of Reed and Lanphere (1973) in the Lake Clark and Iliamna quadrangles. It is primarily distinguished from unit Tkg by age determinations. Unit includes the Styx River batholith of Reed and Elliott (1970), rocks of map units Ti7, Ti10, and Ti11 of Nelson and others (1983), much of the McKinley series of Reed and Nelson (1980) and unit Tbgd of Csejtey and others (1978). Outliers occur in Unalakleet and Table Mountain quadrangles. In the Lime Hills and western Tyonek quadrangles, it is difficult to distinguish between this map unit and unit TKg; without additional mapping and data, the density of lithologically similar plutons makes distinction of these two units especially difficult