The Memory of Sichuan Emei Tour

The late Mesozoic geological history of China Yanshan movement, laying the Emei Mountain geological outline of the new phase of the Himalayan tectonic movement, and accompanied by the uplift of Qinghai-Tibet Plateau, creating the Emei Mountain. As the summit Mount Emei is a large spray of Paleozoic basalt rock under the protection and to maintain a high degree, because of the mountains within the "Bao Liu cutting strong", thus forming a high 2000 meters above the "valley peaks terrain." Mountain terrain along the way due to the formation of the co-existence of sub-and multi-appearance: If there is limestone in the Tibet Guro-dong landscape like caves; by granite and metamorphic rock, and the formation of deep gorges of the position; the top of the hill is solid basalt some lava platform scene.

Emei scenic area with altitude difference, and show different climate characteristics. Qingyinge following low mountains, lush vegetation, clean air cool spring temperatures with no major differences in the plain, a little sooner or later you can add clothing. Qingyinge to Xixiangchi of the mountain, the temperature is lower than the foot of the mountain plains 4 ℃ -5 ℃, visitors need an ample supply of clothing. Xixiangchi to the golden dome of high mountains, people line the clouds, cold rain at first, the temperature lower than the foot of the mountain at Temple, etc. about 10 ℃. Hill prepared for tourists a large number of cotton coat, available for visitors to rent. Emeishan the middle of a "boundary", mountain known as "yang", the mountain known as the "underworld." Cumulus clouds have a certain weight, so the location of the boundaries to which the Emei. Thus, visitors will hear often when the golden dome thunder, but only the "yang" in the rain, "hell" will not rain.