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台怀景区地理地质学专家认为,五台山堪称地球早期地质历史博物馆,是华北大陆古老基底受新生代构造活动形成的断块山脉,地质遗迹包含了太古代花岗岩、绿岩带、古元古代地层、中元古代地层、古生代地层、第三纪古夷平面及第四纪冰缘地貌,跨越超过25亿年的时空,为世界山脉所罕见。连绵的山体形成北邻恒山、东接太行的殊胜气势,其间出现了华北大陆基底大面积的地质露头。也因地貌高差巨大,形成了峰岭交错、沟谷纵横的
According to the geology and geology experts at Taiwan Huaijing Scenic Spot, Wutaishan is called Earth’s Early Geological History Museum and is a fault block mountain formed by the Cenozoic tectonic activity of the ancient basement of North China continent. The geological relics include Archean granite, greenstone belt, ancient Paleozoic strata , The Middle Proterozoic strata, the Paleozoic strata, the Tertiary paleo-level and the Quaternary rim geology, span more than 2.5 billion years of space and time and are rarely seen in the world mountains. Rolling hills form the north adjacent to Hengshan, the eastern side of Taihang’s extraordinary victory momentum, during which there has been a large area of North China continental basement geological outcrop. Also due to the huge terrain elevation, forming a staggered peaks Ridge, vertical and horizontal valleys