一切还得从一亿三千万年前说起。今天的四川盆地,那时还是一片浩淼的汪洋大海。由于激烈的喜马拉雅造山运动,这些汪洋所在的地层发生了倾斜,后来随着地壳的持续挤压,原本是汪洋一片的盆地被逐渐抬升,而水流则逐渐在盆地中部的低洼处汇集,并沿着岩层不断侵蚀,从而形成了两壁垂直的深沟,深沟两侧的山体由一层层砖红色的砂岩组成,这些“色如渥丹,灿若明霞”的岩层被地质学家取了一个颇有诗意的名字——丹霞。在这处由地壳运动和岩层沉淀而形成的丹霞地貌之中,一座造型奇特的山峰正在孕育,不过这还是其最原始的状态。直到距今六千五百万年前,这 Everything has to be said from one hundred and thirty million years ago. Today’s Sichuan Basin, was still a vast ocean. Due to the intense Himalayan orogeny, the strata in which the ocean was located were tilted. Later, as the crust continued to crush, the originally extensive basin was gradually lifted and the water gradually gathered in the low-lying central part of the basin and moved along The rock layers are continuously eroded, forming a vertical deep trench with two walls. The mountains on both sides of the deep trench are composed of layers of brick red sandstone. These rock formations are “geologists such as Wodan, Canruo Mingxia” Take a rather poetic name - Danxia. Among the Danxia landform formed by crustal movement and sedimentation, a peculiar mountain is under construction, but this is still its most primitive state. Until sixty-five million years ago, this