在地质历史中,长白山区处于华北地台、中朝准地台构造单元内。早在二亿年前的侏罗纪时代,地球上发生了翻天覆地的变化。巨大的地质动力伴随着地下岩浆活动,把那些曾经在地壳底部沉睡了近10亿年的古老地层从地下推覆到了地表。地幔中的热液岩浆沿着构造裂隙通道滚滚而来,在其最薄弱的地方喷涌而出,形成山崩地裂之势。 In the geological history, Changbai Mountain is located in the North China platform, the Sino-Korean quasi-platform within the unit. As early as 200 million years ago in the Jurassic era, earth-shaking changes took place. Huge geodynamic power accompanied by underground magmatic activity pushed the ancient formations, which had been sleeping for nearly a billion years at the bottom of the crust, from the ground to the surface. The hydrothermal magma in the mantle billowed along the tectonic fissure channels and spewed out in its weakest area, forming the potential for landslide and earth-shattering.