Fig. 3From: Mass accumulation rate of detrital materials in Lake Suigetsu as a potential proxy for heavy precipitation: a comparison of the observational precipitation and sedimentary recordFine-tuned age model of SG12LM3 (black). Probability range (dashed lines) is estimated based on Bayesian analysis. Varve count age, 137Cs control points, and 12 pairs of event layers (blue solid lines) and historically recorded flood events (red solid lines) are also shownBack to article page