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Lushan tension resume
C

This topic studies geological structure and tectonic geomorphology. Geological structures are divided into folds (anticlines and synclines) and faults. The topography of fold formation is generally as follows: (1) anticlines form mountains; Syncline into the valley.

Reversed terrain: the top of anticline is eroded into a valley by tension; Synclinal trough is hard and not easy to be eroded, but becomes a mountain. Faults lift rocks into mountains or highlands (Huashan, Lushan and Taishan).

Rockfall (graben) forms valleys or lowlands (Weihe Plain and Fenhe River Basin). The geological structure in the valley is a graben formed by fault subsidence, and the formation of sediments in the valley reflects flowing water deposition. So this question chooses option C.