The rock formations of Tianjun Stone Forest share the same geological structure as those of Yunnan’s Stone Forest, both being wonders formed by karst landscapes. They originated during the Carboniferous period, approximately 350 million years ago. However, unlike Yunnan’s Stone Forest, Tianjun Stone Forest underwent a period of drought and water scarcity due to the uplift of the Tibetan Plateau during its formation, which interrupted the water erosion process. Instead, after prolonged wind erosion, it developed into its current unique landscape.
Delingha, Qinghai
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