Tibetan Plateau
Tibetan Plateau
The Tibetan Plateau, also known as the Roof of the World, is a vast, elevated plateau in Central Asia covering most of the Tibet region of China, as well as parts of India, Nepal, and Bhutan. It is the world's highest and largest plateau, with an area of 2.5 million square kilometers and an average elevation exceeding 4,500 meters.
Geography[edit | edit source]
The Tibetan Plateau is surrounded by imposing mountain ranges. To the south, it is bordered by the Himalayas, the world's highest mountain range, which includes Mount Everest, the highest peak on Earth. To the north, it is flanked by the Kunlun Mountains and the Qilian Mountains. The plateau also includes several major rivers, including the Yangtze, the Yellow River, and the Mekong, which have their source in the plateau.
Climate[edit | edit source]
The climate of the Tibetan Plateau is harsh and inhospitable. It is characterized by a cold desert climate with low temperatures, strong winds, and low precipitation. The plateau's high elevation results in a thin atmosphere, which leads to intense solar radiation during the day and extremely cold temperatures at night.
Flora and Fauna[edit | edit source]
Despite its harsh climate, the Tibetan Plateau is home to a diverse range of flora and fauna. The plateau's vegetation is mainly composed of hardy grasses and shrubs adapted to the cold desert climate. The plateau is also home to several unique animal species, including the Tibetan antelope, the snow leopard, and the Tibetan wild ass.
Human Settlement[edit | edit source]
The Tibetan Plateau is sparsely populated due to its harsh climate and difficult terrain. The majority of the population is made up of Tibetans, who have adapted to the harsh conditions over centuries. The plateau is also home to several important Buddhist monasteries, including the Potala Palace in Lhasa, the capital of Tibet.
See Also[edit | edit source]
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Contributors: Prab R. Tumpati, MD