Exposed in southeast Alaska in three areas. On Chichagof Island in the Sitka quadrangle, the unit consists of a plutonic complex of trondhjemite and subordinate syenite, monzonite amd quartz monzonite. The trondhjemite is dominantly biotite trondhjemite and hornblende-biotite trondhjemite, but includes subordinate hornblende trondhjemite. Syenite is predominantly hornblende syenite, but includes subordinate sodalite syenite and sodalite-nepheline syenite. Also present on Chichagof Island is hornblende-bearing biotite monzonite, hornblende-bearing biotite syenodiorite, and biotite quartz monzonite (Loney and others, 1975). U/Pb TIMS-multigrain zircon dates range between 378 and 353 Ma (S.M. Karl, unpub. data), whereas existing K/Ar dates are significantly younger and discordant, at 121.9±5 and 253.1±10 Ma on biotite and hornblende, respectively (Lanphere and others, 1965). The second area, in the Craig quadrangle, rocks mapped by Eberlein and others (1983) as Cretaceous diorite have yielded a 40Ar/39Ar age of 410 Ma (S.M. Karl, unpub. data) and are included here, presuming the age is a minimum age. In the Dixon Entrance quadrangle on southern Prince of Wales Island, leucocratic biotite ± aegirine ± arfvedsonite ± garnet syenite and subordinate leucodiorite yield a number of U/Pb TIMS-multigrain zircon upper intercept ages in the Ordovician (Gehrels and Saleeby, 1987). The plutons in the Craig and Dixon Entrance quadrangles are part of large igneous complex that consists of Ordovician granitic rocks (unit Ogi), the Bokan Mountain complex of Jurassic age (unit Jag), and these Early Devonian to possibly Ordovician plutons. Finally, in the Ketchikan and Prince Rupert quadrangles on Annette and Gravina Islands, rocks ranging from trondhjemite to granite to quartz diorite form another igneous complex (Loney and others, 1975, Berg and others, 1988, Karl, 1992, Brew, 1996) of Silurian age (Gehrels and others, 1987)