Moshi geopark

Nest within the elevated Tibetan Plateau of western Sichuan, the Moshi Geopark, officially known as the Garze Sedimentary Geopark, presents a stark and otherworldly landscape. Situated approximately 30 kilometres from the town of Xinduqiao at an altitude of around 3500 metres, its defining feature is a 78 km² exposure of unique metamorphic rock formations.
The park's most striking characteristics are its towering, dark-grey pinnacles and pyramidal structures, which are composed primarily of sericite-carbonaceous slate. This specific rock type was formed during the late Yanshanian to early Himalayan orogeny, approximately 65 to 70 million years ago. Its formation resulted from the intense tectonic pressures generated by the collision of the Indian and Eurasian plates, which metamorphosed ancient oceanic sediments. The rock's distinctive fissile, or layered, structure and high calcium content contribute to its susceptibility to erosion.
Active geological processes continue to shape the scenery. The region is part of the seismically active Xianshuihe Fault Zone, with ongoing uplift and frequent seismic activity creating fractures. These fractures are then exploited by water erosion, freeze-thaw cycles, and gravity, which continuously sculpt the sharp, angular ridges and deep gullies. This dynamic interplay of tectonic forces and surface erosion has created one of the most singular and visually arresting geological displays in China, offering a direct view into the powerful subterranean forces that have shaped the Tibetan Plateau.
How to get to Moshi geopark
The only way to reach Moshi is by car or with a tour. It is located half-way between Danba and Xinduqiao.
Accommodation
There is no accomodation at the park. There are hotels in Danba and Xinduqiao.