The process of the formation of the ancient bridge isolation road is that in the process of tens of millions of years of change, the crustal plates are constantly undergoing tectonic movements, and the crust is also undergoing fault activities, which leads to the collision between plates and forms the deep and large fault valley where the ancient bridge isolation road is located.

The ancient Jogory Road is an important channel for ancient trade and cultural exchanges, which runs through the southwest border of China, the Sichuan-Yunnan-Tibet Plateau and the Qinghai-Tibet Plateau.