Tibet Travel Information

Tibet is a Plateau region in Central Asia and the indigenous home to the Tibetan people. With an average elevation of 4,900 metres (16,000 ft), it is the highest region on Earth and is commonly referred to as the "Roof of the World."

Tibet is comprised of the three provinces of Amdo (now split by China into the provinces of Qinghai, Gansu & Sichuan), Kham (largely incorporated into the Chinese provinces of Sichuan, Yunnan and Qinghai), and U-Tsang (which, together with western Kham, is today referred to by China as the Tibet Autonomous Region).

The Tibet Autonomous Region (TAR) comprises less than half of historic Tibet and was created by China in 1965 for administrative reasons. It is important to note that when Chinese officials and publications use the term "Tibet" they mean only the TAR.

Tibetans use the term Tibet to mean the three provinces described above, i.e., the area traditionally known as Tibet before the 1949-50 invasion.

Despite over 40 years of Chinese occupation of Tibet, the Tibetan people refuse to be conquered and subjugated by China. The present Chinese policy, a combination of demographic and economic manipulation, and discrimination, aims to suppress the Tibetan issue by changing the very character and the identity of Tibet and its people.

Tibet is located on the Tibetan Plateau, the world's highest region. Most of the Himalaya mountain range, one of the youngest mountain ranges in the world at only 4 million years old, lies within Tibet. Its most famous peak, Mount Everest, is on Nepal's border with Tibet. The average altitude is about 3,000 m in the south and 4,500 m in the north.

The atmosphere is severely dry nine months of the year, and average snowfall is only 18 inches, due to the rain shadow effect whereby mountain ranges prevent moisture from the ocean from reaching the plateaus. Western passes receive small amounts of fresh snow each year but remain traversable all year round. Low temperatures are prevalent throughout these western regions, where bleak desolation is unrelieved by any vegetation beyond the size of low bushes, and where wind sweeps unchecked across vast expanses of arid plain. The Indian monsoon exerts some influence on eastern Tibet. Northern Tibet is subject to high temperatures in the summer and intense cold in the winter.