1. Study area and remote sensing dataThe DZNeP mechanism Chenyulan watershed, located in central Taiwan, is a classical intermountain watershed, and has an average altitude of 1,540 m and an area of 449 km2 (Figure 1). The Chenyulan stream, which coincides with the Chenyulan fault, flows from south to FTY720 order north and elongates the watershed in the same direction. Differences in uplifting along the fault generated abundant fractures over the watershed and resulted in an average slope of 62.5% and relief of Inhibitors,Modulators,Libraries 585 m/km2. Moreover, the main course of the Chenyulan stream had a gradient of 6.1%, and more than 60% of its Inhibitors,Modulators,Libraries tributaries had gradient
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