The best season to play in Sailimu Lake is from June to July every year. At this time, there are wild flowers blooming on the green grassland around the lake area, taking care of the blue lake under the snow-capped mountains. The scenery is the most beautiful, and the photos around the lake are very good.

The flowers around the lake area also have their own distribution, with purple flowers in Hubei, yellow flowers in the west and blue flowers in the east, with their own characteristics. In addition, in July every year, the "Nadam" event on the lakeside grassland makes Sailimu Lake even more icing on the cake.

Sailimu Lake is located in the alpine basin in the western section of Tianshan Mountain in Bole City, Xinjiang. It is called "Sailimu Zhuoer" in Mongolian, which means "the lake on the back of the mountain". Provincial-level tourist attractions, the fifth batch of national-level scenic spots, are the highest altitude, largest area and beautiful alpine lakes in Xinjiang, and also the last place where the warm and humid air currents in the Atlantic Ocean care, so there is the saying that "the last tear in the Atlantic Ocean".

Formation and evolution of sailimu lake;

The assembling process of many ancient blocks before Sinian. By the Sinian, the main body began to form a unified craton block, and generally accepted the unified caprock deposits represented by the Sinian moraine and the phosphorus-bearing rock series in the early CAMBRIAN.

Evolution process of cracking and reassembling of Xinjiang plate in early and middle Paleozoic. From the mid-CAMBRIAN to the end of the late Carboniferous, the complicated and diverse history of continental plates spreading and separating, subduction and collision was completed.

Finally, the basic tectonic framework of Xinjiang today was formed, ending the tectonic evolution stage of separation and combination of multi-plates and land in early and middle Paleozoic, and entering the same plate, that is, the tectonic evolution stage in the land.

The evolution stage of Xinjiang intracontinental structure from late Paleozoic to present. At the end of Carboniferous and the beginning of Permian, the embryonic form of Eurasian plate has been formed, and Xinjiang has become a part of this global giant plate. However, on its south side, it is still facing the closure of the Paleo-Tethys Ocean, the opening and final closure of the NeoTethys and the formation of the Qinghai-Tibet Plateau, which finally contributed to the tectonic subsidence lake-Sailimu Lake.

Reference to the above content: Baidu Encyclopedia-Sailimu Lake