Varve dating method
The main factor controlling varve formation is climate variability; there must be large seasonal differences in both temperature and precipitation.This sets up the succession of biotic life and the physical and chemical structure of the lake necessary to form the contrasting layers.With the exception of tree rings, which were previously discussed on this post by Erin our reconstructions are often limited by errors in dating methods.However in some lakes, sediments are deposited in visible annual layers called varves.The sedimentation or annual varve thickness is relatively uniform, typically 1.2 mm per yr for present conditions in Lake Suigetsu which is located near the coast of the Sea of Japan.
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