Rock avalanches, debris flows, and pyroclastic flows surge down steep canyons at high velocities in response to gravitational attraction (Jakob et al., 2005), posing a potential threat to human lives and facilities downstream (Choi et al., 2014;Jakob et al., 2012). The destructive potential of these granular phenomena can be greatly enhanced through erosion and entrainment of bed material controlled by the stresses between the flow base and the channel bed (Iverson et al., 2011;Song & Choi, 2021). Basal stress generated by granular flows can drive near-bed grain dynamics and energy dissipation (Hsu et al., 2014). Sediment entrainment is related to the largest mean and fluctuating basal stress (Berger et al., 2011b) and the maximum erosion depth scales with the depth to which force fluctuations can propagate (McCoy et al., 2012). High-magnitude force fluctuations weaken the apparent friction coefficients of granular flows, enhancing flow mobility (Cagnoli & Romano, 2012;Li et al., 2022). Therefore, to better understand the flow-bed interaction mechanisms, and relevant hazard assessment, it is essential to provide physical insights into the basal stresses generated by granular flow.