“…(3) are influenced by many factors including hillslope-channel coupling, physical linkages among channel reaches, and hydrological regimes; (4) can follow many trajectories; (5) are intricately intertwined with ecological recovery; and (6) that systems may not return to predisturbance states (e.g., Bellmore et al, 2019;Cluer & Thorne, 2014;East et al, 2018;Foley et al, 2017;Gellis et al, 2017;Gran et al, 2011Gran et al, , 2013James, 1991;James & Lecce, 2013;Kasai, 2006;Kasai et al, 2004;Major et al, 2018;Moody & Meade, 2014, 2018Pierson & Major, 2014;Schumm, 2005;Swanson & Major, 2005). But we can further exploit records of physical responses to profound fluvial disturbances to gain richer geomorphic insights.…”