Haiyuan Earthquake, China

Historical co-seismic landslide inventory with Google Earth A case study of 1920 Haiyuan Earthquake, China [Pg.179]

State Key Laboratory of Geohazard Prevention and Geoenvironment Protection, [Pg.179]

Although a great deal of research has been made on the landslides triggered by Haiyuan Earthquake in recent years, they are mainly aimed at several representative landslides or landslides in typical areas (such as Xiji County), with little attention [Pg.179]

The central part of the study area is Liupan Mountain with the elevation of 2000 to 3000 m, exposing bedrocks in Pliocene series. Near the mountain is the loess hill, with the elevation of 1200 to 2000 m. The study area is characterized by temperate continental monsoon climate, with the annual average temperature of 5 to 7°C. This area is fairly dry. [Pg.180]

The surface ruptures of Haiyuan Earthquake were 273 km long, which can be divided into two segments with the east end of Nanhuashan as the boundary. The seismic fault was the sinistral strike-slip fault, where the maximum horizontal displacement was approximately 10 m and the maximum vertical displacement was approximately 7.6 m. [Pg.180]

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