Characteristics of Debris Flows at Houyenshan, Miaoli, Taiwan Hsien-Ter Chou[1]* Hing-Lin Yang[1 Houyenshan, Miaoli, one can classify the debris flow into two different flow patterns such as
-istics of Debris Flows at Houyenshan, Miaoli, Taiwan.” J. of Chinese Soil and Water accumulated rainfall and the traveling distance of gravelly debris flows was established. Gravelly
-istics of Debris Flows at Houyenshan, Miaoli, Taiwan.” Journal of Chinese Soil and Water Houyenshan, Miaoli, Taiwan. The buried depth and covered area exceeded 2.5 m and 100 m2
Characteristics for Debris-Flow Events in Taiwan, Journal of Chinese Soil and Water Conservation, 22 模的影響。 關鍵詞:火炎山、礫石層、土石流、降雨臨界線、潰壩。 The Monitoring and Flow Dynamics of Gravelly Debris
patterns and geophone characteristics of debris flows at Houyenshan, Miaoli, Taiwan.” Journal 石流事件之振幅與時頻分析 Fig.3 Amplitude and time-frequency analysis of historical debris flows at
, J.H. (2015)."The Flow Patterns and Geophone Characteristics of Debris Flows at Houyenshan at higher risk when debris flows occur. Strategies to reduce the vulnerability of
., and Huang, C.H. (2015). “The flow patterns and geophone characteristics of debris flows at Houyenshan, Miaoli, Taiwan.” Journal of Chinese Soil and Water Conservation, 46(2), 71
discussed. To solve the seismo-acoustic stress on the interface of debris flow and bed, as a function of debris flow phase velocity and acoustic wave speed. It means the
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