Inner Mongolia | The Pleistocene Tuo Fengling Tianchi formed 300,000 years ago.

❤Recommended reason: Tuo Fengling Tianchi was formed in the Pleistocene 300,000 years ago. It is a high-altitude lake formed by the accumulation of water in the crater after a volcanic eruption. Tuo Fengling Tianchi is the largest and deepest Tianchi in the Arxan Tianchi group. The altitude is lower than that of Arxan Tianchi. Overlooking from a high place, it lies quietly in the forest in a clear and green color, in the shape of a foot, so it is also called the foot surface lake. 👍Most recommended: On the way, you will pass a colorful floating rock, which is the rock that will not sink when thrown into the water. The wooden plank road between the colorful forests gradually rises, and the wooden plank road between the second viewing platform and the third viewing platform is the best place to shoot the panoramic view of Tuo Fengling Tianchi. The best season to watch Tuo Fengling Tianchi is autumn. When I was in Tuo Fengling, it was cloudy and there was a little sunshine occasionally.