The Taklamakan Desert is a desert in Southwestern Xinjiang in Northwest China. Located inside the Tarim Basin in Southern Xinjiang, it is bounded by the Kunlun Mountains to the south, the Pamir Mountains to the west, the Tian Shan range to the north, and the Gobi Desert to the east.
View of the Taklamakan desert
Desert life near Yarkand
The Molcha (Moleqie) River forms a vast alluvial fan at the southern border of the Taklamakan Desert, as it leaves the Altyn-Tagh mountains and enters the desert in the western part of the Qiemo County. The left side appears blue from water flowing in many streams. The picture is taken in May, when the river is full with the snow/glacier meltwater.
A desert is a landscape where little precipitation occurs and, consequently, living conditions create unique biomes and ecosystems. The lack of vegetation exposes the unprotected surface of the ground to denudation. About one-third of the land surface of the Earth is arid or semi-arid. This includes much of the polar regions, where little precipitation occurs, and which are sometimes called polar deserts or "cold deserts". Deserts can be classified by the amount of precipitation that falls, by the temperature that prevails, by the causes of desertification or by their geographical location.
Sand and dunes of the Libyan Desert
Valle de la Luna ("Moon Valley") in the Atacama Desert of Chile, the world's driest non-polar desert
Atacama, the world's driest non-polar desert, part of the Arid Diagonal of South America
Flash flood in the Gobi