Mount Kunlun UNESCO Global Geopark

Mount Kunlun UNESCO Global Geopark is located in the southwest part of Golmud, Qinghai Province.

Situated at the northeastern part of the Qinghai-Tibet Plateau hinterland, the tectonic setting of the UNESCO Global Geopark belongs to the colliding zone of Kangxiwar-South Kunlun-Madoi-Maqin. The UNESCO Global Geopark has experienced multiple times of complicated crustal evolution, ocean development, as well as ocean-land transformation, developing a tectonic mix of Mesoproterozoic-Neoproterozoic-Jurassic strata, with active and intense magmatic activities. It is one of the important mountain systems in inland Asia as well as an important window for geological evolution research of the Eurasia continent. Rare as it is, Mount Kunlun UNESCO Global Geopark also retains the geological relics left in the evolution history of the Paleo Asian tectonic system and Tethyan tectonic system. The suture zone and rock pieces inside it faithfully record the complicated geological history such as several times of Tethys Ocean-land conversion, magmatic activity, crustal extension, subduction and collision of the plate, making the UNESCO Global Geopark play a unique and irreplaceable role in earth science in China and even Eastern Asia.