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。
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.
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。
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