Can I only use the ticket for Lushan sightseeing bus once?

Tickets for sightseeing bus in Lushan Mountain can be used many times, and sightseeing bus in Lushan Mountain can get on and off at will within seven days at a time, but now it is the peak season, and there is likely to be a long queue. Lushan (Kuangshan) is located in Jiujiang City, Jiangxi Province. It is a world cultural heritage, a world geological park, a national key cultural relic protection unit, a national 5A-level tourist attraction and the first batch of national civilized scenic spots. Known as "Kuangshan is the best in the world".

Lushan Mountain, with majestic mountains and numerous cliffs, extends about 25 kilometers from northeast to southwest, with a width of about 15 kilometers, a total scenic area of 302 square kilometers, a mountainous area of 282 square kilometers, and a relative height of 1200 ~ 1400 meters. The main peak, Hanyang Peak, is 65,438+0,474 meters (4,422 feet) above sea level, with large faults on the east and west sides, which is magnificent. Since ancient times, it has enjoyed the reputation of "the best in the world". The ancients said that the beauty of Lushan Mountain lies in the south of the mountain. The main scenic spot of Lushan Mountain is in the south of the mountain, which has a history of thousands of years. The main attractions are Guanyin Bridge, Bailudong, Xiufeng, Taohuayuan, Zhouyu Dianjiangtai, Ailianchi and Sandiequan. The main scenic spots on the mountain are Xianren Cave, Hanpokou, beauty salon and meeting place. Guling in the mountains, also known as Guniuling, is named after a huge rock-like bull, with an altitude of 1.056 meters.

Lushan Mountain is located at the junction of Jiangnan platform anticline and Lower Yangtze Depression. Except Triassic, all strata in the area are exposed systematically, and the structure is obvious, which shows the main process of crustal evolution. Lushan Mountain has a unique Quaternary glacier relic, which is the birthplace of China's Quaternary Glacier Theory. At the foot of the mountain, on the shore of Poyang Lake, there are unique sand dunes generated by the ancient monsoon circulation in the last glacial period.

The geological structure in Lushan area is complex and obvious, which shows the main process of crustal change. Lushan Mountain rose strongly in Quaternary, and many faults formed many peaks. Lushan Mountain rises and the surrounding area sinks relatively, and the Poyang Lake basin develops further, forming Poyang Lake. The northern part is dominated by fold structures, forming a series of valley landforms; There are a series of fault cliffs in the south and northwest, forming peaks. There are wide valleys and canyons in the mountains, and terraces and valleys are developed around them. Countless peaks, rocks, valleys, waterfalls, rocks, etc. Form a strange and magnificent mountain landscape. Hanyang Peak is1474m above sea level, which is the first peak of Lushan Mountain. Tiechuan Peak, 950 meters above sea level, stands on the precipice, like a huge ship, with a huge scale. There are two waterfalls in Wangjiapo, which are in pairs. Just like two dragons leaning on the sky, spraying pearls and falling jade. Sandie Spring, divided into three stacks, is integrated into one mass, with a drop of 1.55 meters. The wind reflects in the sun and has different shapes.