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.

西安翠华山风景地貌由古崩塌性滑坡体高速运动堆积而成,堆积体存在一些反映其运动和动力状况的沉积特征。