Is Lushan suitable for visiting in April?
April is a good time to go to Lushan Mountain.
Because April is the season when peach blossoms bloom in Lushan, you can enjoy the blooming peach blossoms and beautiful mountain scenery. In addition, the weather in April is suitable, the temperature is gradually warming up, and it is not as hot as summer, making it very suitable for traveling. For example, you can take a walk in the mountains or ride a bike to experience the beauty of nature. It is worth mentioning that since the peach blossom blooming season in Lushan is the peak tourist season, the number of tourists is relatively large. It is necessary to book hotels and scenic spot tickets in advance to avoid wasting time in queues.
April to May is the best. Because the peach blossoms in Lushan Peach Blossom Spring Scenic Area will bloom from April to May, forming a sea of pink, which is very beautiful. At this time, the climate is also suitable and the travel experience is optimal. In addition, Lushan Peach Blossom Spring Scenic Area also has rich cultural and historical relics, such as Feilaifeng, Huashilou, Longhu Mountain, etc., which are also worth visiting. Therefore, plan your visit beforehand when visiting to fully appreciate the beauty and charm of this place.
Lushan landform features:
The Lushan landform is quite special. It is a composite landform with multiple causes, consisting of fault block mountain tectonic landform, ice erosion landform, and flowing water landform. The landscape is superimposed. During the Late Cretaceous, when the ancient Poyang Lake was formed, the prototype of the Lushan fault-block mountain was formed. It was not until the Himalayan orogeny in the Paleogene and Neogene that the majestic and steep Lushan fault-block mountain was formed.
When the Quaternary Ice Age came three million years later, Lushan Mountain experienced four glaciations. The eroding effect of this type of marine foothill glaciers was particularly strong. On the basis of tall fault-block mountains, , forming a series of glacial landforms, such as blade ridges, cirques, ice cellars, U-shaped valleys, horn peaks, etc.
In the late glacial period of 10,000 years ago, due to abundant rainfall and the development of water systems in Mount Lushan, the fault block mountain structural landforms and ice erosion landforms were strongly transformed under the strong erosion of flowing water, forming a series of unique The flowing water landforms, fault cliffs, and glacial ridges have turned into steep peaks and rocks. The U-valley has formed new peaks and valleys and canyons. The cliffs are lined with majestic cliffs, laying the foundation for the formation of a large number of waterfalls.
Reference for the above content: Baidu Encyclopedia-Lushan