Yuan-Hui Li; Denudation of Taiwan Island since the Pliocene Epoch. Geology ; 4 (2): 105–107. doi: https://doi.org/10.1130/0091-7613(1976)4<105:DOTIST>2.0.CO;2
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The average denudation rate of the Central Range of Taiwan Island has been increasing since the Pliocene Epoch. Today it is at least 1,365 mg/cm2yr, which is probably the highest known value in the world.
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