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.
大关县由于其特殊的地质环境和气候条件，泥石流灾害十分发育。
Because of the particularity of geological environment and climatic conditions in Daguan county, debris flow in Daguan area is well developed.
大巴山区由于特殊的地质构造，滑坡、泥石流和崩塌等地质灾害时有发生。
The complicated geologic structure in Danbashan mountain sometimes resulted in landslide, mudflow and rockfall.
大巴山区由于特殊的地质构造，滑坡、泥石流和崩塌等地质灾害时有发生。
The complicated geologic structure in Danbashan mountain sometimes resulted in landslide, mudflow and rockfall.
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