“…(1) freeze-thaw, which can cause frost shattering of bedrock (Dredge, 1992) and generation of talus, or weakening or creep of unconsolidated sediment (Daanen et al, 2012;Zhou et al, 2018); (2) sustained rainfall or snowmelt, which can destabilize soils (Cui et al, 2019); (3) chemical weathering, which can weaken bedrock and generate talus (Avtar et al, 2011); (4) thinning of glaciers and debuttressing (removal of the physical support) of moraines or weakened bedrock or tributary glaciers (Kääb et al, 2006); (5) thawing of permafrost or ice-cored moraines; (6) gully erosion by surface streams or subsurface piping, which can undermine glaciers, debris, or bedrock; (7) prior earthquakes or joint fracturing of bedrock ; (8) deforestation and other vegetation changes (Pathak, 2016;Hashim et al, 2017); (9) construction (Pathak, 2016); and commonly a combination, e.g., bedrock weathering, deforestation, land use conversion and construction, and sustained precipitation (Cui et al, 2019), or bedrock fracturing, vegetation change, and sustained precipitation . Commonly, minor landsliding itself can destabilize slopes and condition them for larger subsequent failures triggered by earthquakes or rainfall (Pathak, 2016).…”