The 8 October 2005 Kashmir earthquake triggered several thousand landslides. These were mainly rock falls and debris falls, although translational rock and debris slides also occurred. In addition, a sturzstrom (debris avalanche) comprising ∼80 million m3 buried four villages and blocked streams to create two lakes. Although landsliding occurred throughout the region, covering an area of N7500 km2, the failures were highly concentrated, associated with six geomorphic–geologic anthropogenic settings, including natural failures in (1) highly fractured carbonate rocks comprising the lowest beds in the hanging wall of the likely earthquake fault; (2) Tertiary siliciclastic rocks along antecedent drainages that traverse the Hazara–Kashmir Syntaxis; (3) steep (N50°) slopes comprising Precambrian and Lower Paleozoic rocks; (4) very steep (»50°) lower slopes of fluvially undercut Quaternary valley fills; and (5) ridges and spur crests. The sixth setting was associated with road construction. Extensive fissuring in many of the valley slopes together with the freshly mobilized landslide debris constitutes a potential hazard in the coming snowmelt and monsoon seasons. This study supports the view that earthquake-triggered landslides are highly concentrated in specific zones
associated with the lithology, structure, geomorphology, topography, and human presence.