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。
Mudslides develop when water rapidly accumulates in the ground and results in a surge of water-saturated rock, earth, and debris.
当雨水迅速累积在土地上并且产生了大量被水浸透的岩石，泥土与碎屑时，泥石流就形成了。
Because ice restricted to high altitudes and to polar regions, running water moves far more rock debris each year than ice does.
由于冰只局限在高地和极区，所以每年流水搬运的岩屑比冰所运走的多得多。
Because ice restricted to high altitudes and to polar regions, running water moves far more rock debris each year than ice does.
由于冰只局限在高地和极区，所以每年流水搬运的岩屑比冰所运走的多得多。
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