“…Most studies have shown that lateral subsurface flow occurs either because of temporary saturation above an impeding layer or because the water table rises into a more permeable layer near the surface (Weiler et al., 2005). Soil development leads to an increase in fine particles due to physical weathering (He & Tang, 2008; Mavris et al., 2010; Righi et al., 1999) and chemical weathering (i.e., clay formation; Crocker & Dickson, 1957; Román‐Sánchez et al., 2021; Schaaf et al., 2017; Young et al., 2004). Illuviation of this fine‐textured material leads to a lower permeability layer that promotes ponding and lateral SSF (e.g., Dahlke et al., 2012; Lohse & Dietrich, 2005).…”