The Himalayas include over a hundred mountains exceeding 7,200 metres (23,600 ft) in height. By contrast, the highest peak outside Asia--Aconcagua, in the Andes-- is 6,961 metres (22,838 ft) tall.
According to the modern theory of plate tectonics, their formation is a result of a continental collision or orogeny along the convergent boundary between the Indo-Australian Plate and the Eurasian Plate abut 50 million years ago. So the Himalayas are among the youngest mountain ranges on the planet.
|
Mountain | m. | ft. | Country |
Everest | 8,848 | 29,035 | Nepal/China |
Lhotse | 8,516 | 27,941 | Nepal/China |
Makalu | 8,463 | 27,767 | Nepal/China |
Cho Oyu | 8,153 | 26,750 | Nepal |
Kangchenjunga | 8,586 | 28,171 | Nepal/India |
Lönpo Gang | 6,979 | 22,898 | |
Ganesh Himal | 7,429 | 24,375 | Nepal/China |
Annapurna | 8,091 | 26,547 | Nepal |
K2 | 8,612 | 28,253 | Pakistan/China |
|
City | Elevation (ft) | Population |
Lhasa, Tibet | 11,900' | 500,000 |
Shigatse, Tibet | 12,660' | 63,000 |
Tingri, Tibet | 14,400' | 523 |
Kathmandu, Nepal | 4,500' | 975,453 |
Lukla, Nepal | 9,383' | 230 |
Pokhara, Nepal | 5,710' | 264,991 |
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