
Lhasa, which signifies "Place where there is the Gods" and is more than 1,300 years of age, sits in a valley right beside the Lhasa River. In the eastern part of the city, close to the Jokhang Temple and Barkhor neighborhood, Tibetan impact is still solid and clear and it is basic to see generally dressed Tibetans connected with on a kora (a clockwise circumambulation or stroll around the Jokhang Temple), regularly turning petition wheels. The western piece of Lhasa is all the more ethnically Han Chinese in character. It is occupied and present day and seems to be like numerous other Chinese urban areas. A significant part of the framework, for example, banks and government workplaces is to be found there.
History

A Tibetan custom says that after Songtsän Gampo's demise in 649 C.E., Chinese troops caught Lhasa and smoldered the Red Palace.Chinese and Tibetan researchers have noticed that the occasion is said neither in the Chinese archives nor in the Tibetan compositions of Dunhuang.
Atmosphere
Because of its high rise, Lhasa has a cool semi-bone-dry atmosphere (Köppen: BSk) with chilly winters and gentle summers, yet the valley area shields the city from serious frosty or heat and solid winds. Month to month conceivable daylight ranges from 53 percent in July to 84 percent in November, and the city gets
about 3,000 hours of daylight every year. It is in this way infrequently called the "sunlit city" by Tibetans. The coldest month is January with a normal temperature of −1.6 °C (29.1 °F) and the hottest month is June with a day by day normal of 16.0 °C.
Topography
Lhasa has a rise of around 3,600 m (11,800 ft)and lies in the focal point of the Tibetan Plateau with the encompassing mountains ascending to 5,500 m (18,000 ft). The air just contains 68 percent of the oxygen contrasted with ocean level.The Kyi River (or Kyi Chu), a tributary of the Yarlung Zangbo River, goes through the southern part of the city. This waterway, referred to neighborhood Tibetans as the "joyful blue waves", courses through the snow-secured tops and chasms of the Nyainqêntanglha mountains, developing 315 km (196 mi), and exhausting into the Yarlung Zangbo River at Qüxü, shapes a region of incredible picturesque magnificence. The marshlands, generally uninhabited, are toward the north.Ingress and departure streets run east and west, while toward the north, the street base is less created.
No comments:
Post a Comment