Heterogeneous rupture in the great Cascadia earthquake of 1700 inferred from coastal subsidence estimates

Abstract Past earthquake rupture models used to explain paleoseismic estimates of coastal subsidence during the great A.D. 1700 Cascadia earthquake have assumed a uniform slip distribution along the megathrust. Here we infer heterogeneous slip for the Cascadia margin in A.D. 1700 that is analogous t... View More