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Top Attractions in Tibet

Lhasa

Lhasa is a prefecture-level city, formerly a prefecture until 7 January 1960, one of the main administrative divisions of the Tibet Autonomous Region of China. It covers an area of 29,274 square kilometres (11,303 sq mi) of rugged and sparsely populated terrain. The consolidated prefecture-level city is divided into five mostly rural counties and three partially urban districts Chengguan District, Doilungdêqên District, and Dagzê District, which contain the main urban area of Lhasa. The prefecture-level city roughly corresponds to the basin of the Lhasa River, a major tributary of the Yarlung Tsangpo River. It lies on the Lhasa terrane, the last unit of crust to accrete to the Eurasian plate before the continent of India collided with Asia about 50 million years ago and pushed up the Himalayas. The terrane is high, contains a complex pattern of faults and is tectonically active. The temperature is generally warm in summer and rises above freezing on sunny days in winter. Most of the rain falls in summer. The upland areas and northern grasslands are used for grazing yaks, sheep and goats, while the river valleys support agriculture with crops such as barley, wheat and vegetables. Wildlife is not abundant, but includes the rare snow leopard and black-necked crane. Mining has caused some environmental problems. The 2000 census gave a total population of 474,490, of whom 387,124 were ethnic Tibetans. The Han Chinese population at the time was mainly concentrated in urban areas. The prefecture-level city is traversed by two major highways and by the Qinghai–Tibet Railway, which terminates in the city of Lhasa. Two large dams on the Lhasa River deliver hydroelectric power, as do many smaller dams and the Yangbajain Geothermal Station. The population is well-served by primary schools and basic medical facilities, although more advanced facilities are lacking. Tibetan Buddhism and monastic life have been dominant aspects of the local culture since the 7th century. Most of the monasteries were destroyed during the Cultural Revolution, but since then many have been restored and serve as tourist attractions.

Norbulingka

Norbulingka is a palace and surrounding park in Lhasa, Tibet, China, built from 1755. It served as the traditional summer residence of the successive Dalai Lamas from the 1780s up until the 14th Dalai Lamas exile in 1959. Part of the "Historic Ensemble of the Potala Palace", Norbulingka is recognized as a UNESCO World Heritage Site, and was added as an extension of this Historic Ensemble in 2001. It was built by the 7th Dalai Lama and served both as administrative centre and religious centre. It is a unique representation of Tibetan palace architecture. Norbulingka Palace is situated in the west side of Lhasa, a short distance to the southwest of Potala Palace. Norbulingka covers an area of around 36 hectares and considered to be the largest man made garden in Tibet. Norbulingka park is considered the premier park of all such horticultural parks in similar ethnic settings in Tibet. During the summer and autumn months, the parks in Tibet, including the Norbulinga, become hubs of entertainment with dancing, singing, music and festivities. The park is where the annual Sho Dun or Yoghurt Festival is held. The Norbulingka palace has been mostly identified with the 13th and the 14th Dalai Lamas who commissioned most of the structures seen here now. During the invasion of Tibet in 1950, a number of buildings were damaged, but were rebuilt beginning in 2003, when the Chinese government initiated renovation works here to restore some of the damaged structures, and also the greenery, the flower gardens and the lakes.

South Summit

The South Summit of Mount Everest is the second-highest peak on Earth, and is a subsidiary peak to the primary peak of Mount Everest. Although its elevation above sea level of 8,749 metres is actually higher than the second-highest mountain on Earth, K2 above sea level), it is only considered a separate peak and not a separate mountain as its prominence is only 11 meters. The peak is a dome-shaped peak of snow and ice, and is connected to the summit of Mount Everest by the Cornice Traverse and Hillary Step. It was first climbed by Charles Evans and Tom Bourdillon on the 1953 British Mount Everest expedition, on May 26, 1953. They were unable to continue on to the primary summit, but Edmund Hillary and Tenzing Norgay, the next pair to make a summit bid, traversed the South Summit to reach the main peak. The distance separating the two summits is approximately 130 metres . A geologist with a 1965 Indian Everest expedition discovered a deposit of fossils of seashells in limestone about 100 feet above the South Summit. This expedition put nine climbers on the main summit. Describing his first ascent of Mount Everest without artificial oxygen in 1978, Reinhold Messner described the South Summit as "quite a milestone for me". During the 1996 Mount Everest disaster, mountain guide Rob Hall and three other people died at the South Summit while descending from the main summit in an unexpected blizzard. Hall survived overnight, and established radio contact the following day, but froze to death later that day, May 11, 1996. His body remains on the South Summit.

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