Seismic profiling data indicate that the thickness of an accreted ocea
nic terrane of Paleocene and early Eocene age, which forms the basemen
t of much of the forearc beneath western Oregon and Washington, varies
by approximately a factor of 4 along the strike of the Cascadia subdu
ction zone. Beneath the Oregon Coast Range, the accreted terrane is 25
to 35 kilometers thick, whereas offshore Vancouver Island it is about
6 kilometers thick. These variations are correlated with variations i
n are magmatism, forearc seismicity, and long-term forearc deformation
. It is suggested that the strength of the forearc crust increases as
the thickness of the accreted terrane increases and that the geometry
of the seaward edge of this terrane influences deformation within the
subduction complex and controls the amount of sediment that is deeply
subducted.