Example of a Highland: The Tibetan Plateau — Earth's "Third Pole"
The quintessential highland is the Tibetan Plateau — often called the "Roof of the World" or "Third Pole."
Vitals
- Area: ~2.5 million km² (965,000 sq mi) — 4x France, 3x Texas
- Average elevation: 4,500 m (14,800 ft) above sea level
- Extent: Tibet Autonomous Region + Qinghai + western Sichuan + Ladakh + Bhutan
- Boundaries: Kunlun Mts (N), Himalaya (S), Karakoram (W), Qilian/Hengduan (E)
Why It's the Archetypal Highland
- Scale: Largest, highest plateau on Earth
- Climate engine: Drives Asian monsoon; heats in summer → low pressure → draws moist air from Indian Ocean
- Water tower: Source of 10 major rivers (Indus, Ganges, Brahmaputra, Yangtze, Yellow, Mekong, Salween, Irrawaddy, Tarim, Sutlej) — 1.5B+ people depend on it
- Ecological zones: Alpine steppe, permafrost, wetlands, glaciers (37,000+ km²)
- Biodiversity: Snow leopard, Tibetan antelope (chiru), wild yak, black-necked crane, endemic plants
- Human adaptation: Pastoral nomadism (drokpa), barley agriculture, high-altitude physiology (EPAS1 gene)
Other Notable Highlands (For Comparison)
| Highland | Region | Avg Elev. | Area |
| Altiplano | Bolivia/Peru/Chile/Argentina | 3,750 m | 170,000 km² |
| Ethiopian Highlands | Ethiopia/Eritrea | 2,500 m | 200,000 km² |
| Colorado Plateau | US Four Corners | 2,000 m | 337,000 km² |
| Anatolian Plateau | Turkey | 1,100 m | 500,000 km² |
| Central Massif | France | 800 m | 85,000 km² |
The Tibetan Plateau isn't just an example—it's the type specimen for highland geography, climatology, and human adaptation.