Fig. 11From: Late Quaternary eruption of the Ranau Caldera and new geological slip rates of the Sumatran Fault Zone in Southern Sumatra, IndonesiaConsistent right-lateral offsets of isochronous river channels deeply incised into the Ranau Tuff near Liwa. The total offset is estimated from three channels that cross the fault at high angle, and is consistent with the offset of channels that cross the fault trace at low angle. The digital terrain is developed from SRTM 1 Arc-Second. Location of these offsets is marked in Fig. 3 Back to article page