Traditional Culture Encyclopedia - Traditional festivals - What geographical knowledge is contained in the different heights of the mountainside peak prospect?
What geographical knowledge is contained in the different heights of the mountainside peak prospect?
The extension structure specially developed in Lushan Mountain has formed the metamorphic core complex structure and fault block mountain in Lushan Mountain. Lushan Mountain is located at the northern end of the Yangtze block in the south of China. From Jurassic to Paleogene, the continental crust was in a state of intense extension, and large-scale remelted granite invaded the continental crust. Under the action of this horizontal and vertical force, Lushan Mountain is in a rising state and in the development stage of basin ridge structure. In the late Himalayan movement more than 20 million years ago, Lushan Mountain formed the present form of fault block mountain. The extensional structure as the main body, the fault-block mountain structure and metamorphic core complex structure accompanying Lushan Mountain constitute another feature of Lushan Mountain's geoscience landscape.
The unique multi-gene complex landscape of Lushan Mountain. Neotectonic movement made Lushan Mountain form a block mountain structure, and cliff landforms can be seen everywhere around the mountain, especially on the east and west sides, which is the embodiment of the rising mountain structure. The top of Lushan Mountain is relatively gentle, and the ancient erosion surface is obvious. After Lushan entered the Pleistocene, Quaternary glacial activity appeared. Due to the Quaternary erosion, various glacial landforms such as ice buckets, ice chambers, U-shaped valleys, ice ridges, ice steps, ice blade ridges and tinder have appeared in the whole mountain. The superposition of tectonic movement and ice erosion makes Lushan Mountain look more majestic and steep.
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