The guide for visiting Lushan is as follows: 1. Transportation: To travel to Lushan, you can first take a train or plane to Jiujiang City.
From Jiujiang City to Lushan Scenic Area, you can choose to take a bus or a taxi.
In addition, you can also take the train directly to Lushan Station. After getting off, you can take a bus or taxi to the Lushan Scenic Area.
2. Tickets and opening hours: Tickets for Lushan Scenic Area are open all day long, and the recommended visit time is 2-3 days.
3. Tour route: Day 1: North Gate of Mount Lushan→Lushan Scenic Area→Ruqin Lake→Huajing→Overpass→Xianren Cave→Da Tianchi→Longshou Pavilion→Wulao Peak→South Gate of Mount Lushan; Day 2: South Gate of Mount Lushan
Gate → Sandiequan → Xiufeng → Poyang Lake.
4. Accommodation: There are many hotels and B&Bs in Lushan Scenic Area. Visitors can choose suitable accommodation according to their own budget and preferences.
5. Catering: Lushan specialties include Lushan tofu, stewed chicken with stone fungus, Poyang Lake whitebait, etc.
During your trip to Lushan, you can taste these special delicacies and experience the food culture of Lushan.
Characteristics of Lushan Mountain 1. Coolness: Lushan Mountain is located in the subtropical humid monsoon zone, with abundant rainfall and a mild and pleasant climate. In midsummer, it is a cool island suspended in the hot sea in the middle and lower reaches of the Yangtze River.
The annual precipitation in Lushan Mountain can reach 1950-2000 mm, so the temperature difference in the mountain is large, there are many clouds and fog, and the mountains are varied and ever-changing.
2. Landform characteristics: The most important stratigraphic relics in Lushan Mountain are the stratigraphic relics of the Paleoproterozoic Xingzi Group. There are two main exposures: the section from Qixian Temple to Ruanjiapeng, located in the river valley.
Along the way, you can see various schists, metamorphic rocks, quartzites and marbles of the Xingzi Group.
From Guizong to the Jinlun Peak section, you can see various granulites, schists and amphibolites (basic volcanic lava) of the Xingzi Group along the way.
Its ruins are not only complete, but also preserved naturally.
3. Geological characteristics: The geological formation of Lushan Mountain is a fault block mountain formed by fault gaps. There are many faults around it, especially in the southeast and northwest. The northeast-southwest trending faults are large in scale. Due to this fault block structure,
The mountains formed have many strange peaks, steep cliffs, and various shapes. Some are as round as a canopy, some stretch like the Great Wall, some are as high as the sky, some overlook the waves, some are like ships sailing on the sea, and some are like turtles.
Traveling across the earth, it is majestic and magnificent.
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