How to evaluate the relationship between Mount Emei’s tourist landscape and geological processes

The relationship between Mount Emei’s tourist landscape and geological processes is mainly reflected in the following aspects:

1. Geological structure: From the perspective of geological structure, Mount Emei is an anticlinal fault block mountain. , belonging to the Emei-Wa(Wushan) fault block zone. After a long period of geological tectonic action, unique fault-block mountains were formed in Mount Emei, such as Sheshen Cliff, Ten Thousand Buddhas Peak, Thousand Buddhas Peak, etc., thus forming the unique natural landscape of Mount Emei.

2. Karst landforms and flowing water landforms: Mount Emei has a variety of karst landforms, flowing water landforms, etc., which constitute the beautiful natural landscape of Mount Emei. Among them, Jiulao Cave is a typical landform of karstification, while "Shuangqiao Qingyin", "Longmen Waterfall" and "One Line of Sky" are representatives of flowing water landforms.

3. Faults and fold structures: Mount Emei also has many faults and fold structures, which also constitute unique natural scenery, such as the Emeishan fault, the Wanniansi fault, the Emeishan anticline, and the Er'emei anticline.

4. Exposed strata: Mount Emei has many exposed strata, which are of great scientific investigation and research value. Among them, the "Triassic Geological Section of Longmen Cave in Mount Emei" is a natural science protection site in Sichuan Province, providing good field practice conditions for geography and geology majors in many universities.

To sum up, the tourism landscape of Mount Emei is closely related to geological processes. Its unique natural landscape is composed of geological structures, karst landforms and flowing water landforms, faults and fold structures, and stratigraphic exposures. The functions are formed in the same way.