Fig. 1From: Right-lateral offset associated with the most recent earthquake on the Ikeda fault of the Median Tectonic Line, southwest Japan, revealed by ground-penetrating radar profilinga Tectonic map of the Japanese Islands. The plate motion vectors are calculated based on DeMets et al. (2010). Thick red lines indicate the active portion of the MTL. EU: Eurasian plate, NA: North American plate, PA: Pacific plate, PH, Philippine Sea plate, MTL: Median Tectonic Line, ISTL: Itoigawa-Shizuoka Tectonic Line. b Active fault traces of the MTL in central to eastern Shikoku (Tsutsumi and Okada 1996). Locs. 1 and 2 denote the surveyed locations of paleochannel offsets by Okada and Tsutsumi (1997) and Goto et al. (2003), respectively. IzF: Ishizuchi fault, HF: Hatano fault, SgF: Sangawa fault, IkF: Ikeda fault, MF: Mino fault, CF: Chichio fault. The topographic base map is made from the SRTM data (https://www2.jpl.nasa.gov/srtm/). c Geomorphology of the area around the survey site. The Ikeda fault trace is from the Active fault database of Japan (https://gbank.gsj.jp/activefault). The topographic base map is made using the 5-m-mesh digital elevation model of the Geospatial Information Authority of JapanBack to article page