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。
Water-rock debris flow is a main type of debris flow in Qinling mountain with a wide distribution, typical development and serious disaster.
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。
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.
地处西秦岭末端与黄土高原交汇地带，地势西南高、东北低，以山地为主，地形地貌复杂多样。
Terminal is located in the west Qinling Mountains and the Loess Plateau convergence zone, the high-lying south-west, north-eastern low mountain in the main complex and diverse topography.
应用推荐