“…The majority of isostatic rebound from glacial ice sheets was completed by 9,000-10,000 years ago due to the low viscosity of the mantle below Blakely et al (2009); tsunami data from Atwater andMoore, 1992 andBourgeois andJohnson, 2001; land-level data from Eronen et al, 1987;Beale, 1990;Bucknam et al, 1992;Williams and Hutchinson, 2000;Sherrod, 2001;Williams et al, 2005;and Martin, 2011. (c) Location of mapped marine terraces associated with the A.D. 900-930 Seattle-fault-zone earthquake (Ota et al, 2006;Kelsey et al, 2008); B, Bremerton; RC, Ross Creek; RP, Restoration Point; S, Seattle; SD, Snohomish Delta. Projection of axial surface of Seattle fault zone from Kelsey et al (2008). the Puget Lowland (James et al, 2000).…”