Water-rock debris flow is a main type of debris flow in Qinling mountain with a wide distribution, typical development and serious disaster.
水石流是秦岭山地泥石流主要类型之一。 分布广泛，发育典型，灾害严重。
The movement characteristics of water-rock debris flow and its mechanics of movement starting in Qinling mountain have been analyzed through investigations on the spot.
笔者通过实地考察资料，对秦岭山地水石流的运动特性进行了研究，并对其起动的力学性能作了初步分析。
Rock debris is often carried into TAP during rainstorms by water draining the volcano summit around the lake.
在暴风雨的季节，水冲刷着湖泊周围的火山顶峰，岩石碎片常常随之落入TAP湖中。
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