泥石流是由于短历时高强度的大雨激发而形成的。
Debris flow was triggered by the short duration and high intensity rainstorm.
但由于降水比较集中的特点，致使新疆的泥石流也比较发育。
But due to falling concentration, generate a lot of debris flow in Xinjiang.
泥石流堆积体边坡失稳现象由于其组成物质、形成年代和堆积部位等方面的特点，与其他岩土边坡失稳有不同的表现。
Failure of debris flow fan is distinct from the common rock and soil slope failure due to the unique geotechnical features of debris flow sediment.
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