Large prehistoric earthquakes are preserved in the geological record. Paleoseismology is the discipline concerned with reconstructing past earthquakes from this record, and mainly draws on offsets in fault scarps and river channels, deformed sediments, soil liquefaction, landslide and tsunami deposits (Ludwig, 2015), and archeological records (Nur, 2007). Biological archives recognize that the sudden subsidence of coasts during earthquakes may submerge and kill near-shore vegetation (Atwater & Yamaguchi, 1991), while shaking-induced damage to roots and damage from debris may suppress tree growth and be recorded in annual growth rings (