dominantly reverse in type along a 60° north-dipping reverse fault, with up to 10.5 m vertical displacement and at most 1 m horizontal displacement, from the lack of observed offset of river thalwegs. The outcrop pattern of the Aksu segment rupture indicates a low-angle thrust, possibly steepening with depth, with a maximum vertical offset or 3–5 m, decreasing steadily to the east. In total about 200 km of fault surfaces ruptured, although there was no visible faulting joining the two main rupture zones. Landslides Many landslides and rock avalanches were triggered by the earthquake and are associated with the mapped zones of surface rupture. The two largest landslides were the Kaindy rock avalanche and the Ananevo rockslide. The Kaindy landslide, with a volume of 15 x 106 m3, was formed of a mass of limestone that buried a group of yurts and killed 38 people. The Ananevo rockslide also had a volume of about 15 x 106 m3, and was formed of weathered granitic material, with a 250 m high backscarp that is still visible. See also List of earthquakes in 1911 List of earthquakes in Kyrgyzstan 1902 Turkestan earthquake References External links Earthquakes in Russia Earthquakes in Kazakhstan Earthquakes in Kyrgyzstan Earthquake Russia January 1911 events 1911 disasters in the Russian Empire