【摘要】 目的进一步研究翠华山山崩地貌的形态特征、成因、发育过程,以及地质公园的建没。方法应用地质地貌学工作方法,野外实地考察,参阅相关资料,从区域地质构造、岩性、地貌、风化和地震作用力诸因素,结合航片分析,对地震山崩进行较全面的科学研究。结果翠华山地震之前,山坡受结构面控制,形成了潜在不稳定的岩体,受强大地震力的作用,以滑崩的方式运动,形成崩塌壁、崩积物和堰塞湖等地貌,特别是地表崩积物的岩块,在滑崩过程中,受反弹力影响,形成千姿百态的山崩裂石,是罕见的山崩地貌奇观现象。结论翠华山山崩地貌的形成是多种因素综合作用的结果,主要与地震强度,以及与地质地貌等环境因素有关。更多还原

【Abstract】 Aim To study the characteristics of Cuihua Mountain landslides geography,its growth process and tour geology park construction.Methods Use the method of applied geology and geography,open investigates on the spot,reading related data,from structure,rock,geography,morals and custom in the district and earthquake function and various factors,together with aviation films analysis and more overall scientific research on the earthquake landslide.Results The function of earthquake and the characteristics of Cuihua Mountain formed the rare,geographical spectacular sight.Conclusion Cuihua Mountains landslidesing the formation of geography is result that various factor cooperates,eventually earthquake intensity and geology geography environment factor relevant.更多还原