Fig. 6From: Two times lowering of lake water at around 48 and 38 ka, caused by possible earthquakes, recorded in the Paleo-Kathmandu lake, central Nepal HimalayaLithostratigraphy of RB core after Sakai et al. (2001), and AMS14C ages after Hayashi et al. (2009). Change in ratio of phytoliths, sponge spicule, carbonaceous fragments, pollen including spore and others are shown, and change in numbers of sponge spicule, charcoal grain, and Pediastrum in RB core are also shown. Possible range of lake-water fall events are indicated by pink shadow. AP arboreal pollen, NAP non-arboreal pollenBack to article page