Introduction to the Twin Towers: Two symmetrical reed-shaped columnar mountains formed by weathering, denudation and dissolution of Triassic limestone are not connected to each other, but stare at each other. This is because the rock itself has the same properties and regular structural cracks, which are formed by direct erosion along vertical cracks by heavy rain. However, the two mountains are so symmetrical and almost identical in appearance, which is relatively rare in nature.

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