The tourist landscape in Xi an Cuihua Mountain, is generated from a large paleo-avalanchine landslide, with the special deposit structures showing indirectly information of high speed block movement.
西安翠华地貌由古崩塌性滑坡体高速运动堆积而成,堆积体在一些反映其运动和动力状况的沉积特征。
The tourist landscape in Xi an Cuihua Mountain, is generated from a large paleo-avalanchine landslide, with the special deposit structures showing indirectly information of high speed block movement.
西安翠华地貌由古崩塌性滑坡体高速运动堆积而成,堆积体在一些反映其运动和动力状况的沉积特征。
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