Fig. 2From: Characteristics of landslides triggered by the 2013 ML6.5 Nantou, Taiwan, earthquakeSpatial correlations and bar charts between landslide densities and triggering factors: a PGA, b lithology, c slope roughness, d slope angle, and e aspect. Slope roughness: the standard deviation of the slope within a 3 × 3 cell window, SLS Szeleng Sandstone and Paileng Formation; HT Hsitsun Formation; NK Nankang Formation; KCL Kueichulin Formation; TKS Toukoshan Formation; LS Lushan Formation; PLS Pilushan Formation; TC Tachien Sandstone; TNA Tananao Schist; AL alluviumBack to article page