“…While bedrock and coarse sediment such as boulders form the rigid channel boundary, fine sediments comprise a dynamic and transient part of the river corridor (e.g., Skalak & Pizzuto, 2010). Fine sediments provide substrate for riparian vegetation, morphological complexity for the aquatic ecosystem, protection of archeological resources, and important recreational areas for visitors (Butterfield et al., 2020; East et al., 2017; Grams et al., 2010; Kaplinski et al., 2005; Korman et al., 2004; Meshkova & Carling, 2012). In canyon rivers where flow is strongly affected by bedrock or relatively immobile talus, flow hydraulics are often dictated by these fixed obstructions (Alvarez et al., 2016; Rennie et al., 2018; Venditti et al., 2014; Wright & Kaplinski, 2011).…”