Fig. 9From: Late Quaternary eruption of the Ranau Caldera and new geological slip rates of the Sumatran Fault Zone in Southern Sumatra, IndonesiaExposure of the distal Ranau Tuff along the trace of the Pauh Fault, 20 km from the eruptive center near Sukabumi village (Lat,Lon: −4.61433, 103.88004). a Top of Ranau Tuff overlain by old alluvial deposit. b Base of Ranau Tuff overlying the Tertiary sandstone. RAN-06B sample is collected from a thin, light gray paleosolBack to article page