Is Lushan Mountain suitable for playing in April?

Lushan Mountain is suitable for sightseeing in April.

Because April is the season of peach blossoms in Lushan Mountain, you can enjoy the blooming peach blossoms and beautiful mountain scenery. In addition, the weather in April is suitable, and the temperature gradually warms up, which is not as hot as summer, so it is very suitable for traveling. For example, you can take a walk on the mountain or ride a bike to feel the beauty of nature. It is worth mentioning that because the peach blossom season in Lushan Mountain is the peak of tourism and the number of tourists is relatively large, it is necessary to book tickets for hotels and scenic spots in advance to avoid wasting time in the queue.

April to May is the best. Because the peach blossoms in Lushan Taohuayuan Scenic Area will bloom in April and May, forming a pink ocean, which is very beautiful. At this time, the climate is also suitable and the travel experience is the best. In addition, Lushan Taohuayuan Scenic Area is rich in cultural and historical relics, and Feilai Peak, Huashi Mountain Villa and Longhu Mountain are also worth visiting. Therefore, it is necessary to make a tour plan in advance before fully appreciating the beauty and charm of this place.

Geomorphological features of Lushan Mountain:

Lushan Mountain is a special landscape, which is a multi-genetic composite landscape composed of structural landscape, ice erosion landscape and running water landscape. While the ancient Poyang Lake was formed in the Late Cretaceous, the embryonic form of Lushan fault block mountain was formed. It was not until the Himalayan orogeny of Paleogene and Neogene that the magnificent Lushan fault block mountain was formed.

Three million years later, the Quaternary Great Ice Age came, and there were four ice ages in Lushan Mountain. This kind of marine piedmont glacier has a particularly strong cutting effect. On the basis of the tall fault-block mountain, a series of glacial landforms such as ridge, ice bucket, ice room, U-shaped valley and ice mound have been formed.

During the Late Glaciation since 65438+100000 years, due to the abundant rainfall and well-developed water system in Lushan Mountain, under the strong erosion of flowing water, the structural landforms and glacial landforms of the fault block mountain were strongly transformed, forming a series of unique flowing water landforms. Cliffs and glacier ridges become steep peaks and valleys, and U valley forms new peaks and valleys. There are many cliffs and great momentum, which lays the foundation for the formation of a large number of waterfalls.

Reference: Baidu Encyclopedia-Lushan Mountain