Himalayas
The Himalayas are a vast east–west mountain system in Asia, forming a high barrier between the Tibetan Plateau and the plains of the Indian subcontinent. Extending across parts of India, Nepal, Bhutan, Pakistan and China, the range includes Mount Everest and many other high peaks. Formed by the continuing convergence of the Indian and Eurasian plates, the Himalayas also shape regional climate, river systems, ecosystems and human life.
Location and extent
The Himalayas arc across southern Asia between the Tibetan Plateau to the north and the plains of the Indian subcontinent to the south. Encyclopaedia Britannica describes the uninterrupted range as about 2,500 kilometres long from west to east and roughly 200–400 kilometres wide. It crosses borderlands in India, Nepal, Bhutan, Pakistan and China. The exact lines used to define a mountain system can vary; the term Hindu Kush Himalaya (HKH), used in regional research, describes a broader 3,500-kilometre region extending across parts of eight countries, from Afghanistan to Myanmar. The HKH region should not be confused with the Himalayas alone.
Relief and structure
The Himalayan system is made up of several roughly parallel belts with distinct landforms and geological histories. From south to north, Britannica groups them as the Outer or Sub-Himalayas (the Siwalik Range), the Lesser Himalayas, the Great Himalaya Range and the Tethys or Tibetan Himalayas. The region's landscape includes steep peaks, deep valleys and gorges, glaciers and high plateaus. Mount Everest is its highest summit and the highest point on Earth above sea level.
Formation and continuing tectonic activity
The mountains formed as the Indian continental plate moved north and collided with the Eurasian plate, closing the Tethys Ocean between them. The collision began about 50–40 million years ago. Because neither thick continental plate could readily sink beneath the other, compression folded and thickened the crust and pushed rock upward, building the Himalayas and the Tibetan Plateau. The plates continue to converge, so tectonic deformation and earthquakes remain part of the region's geology; uplift, erosion and landslides continually reshape the landscape.
Water, climate and ecosystems
Snowfields and glaciers feed many rivers that descend from the mountains. The Indus and Brahmaputra have extensive catchments in the Himalayan region, while the Ganges is also closely linked to Himalayan waters. These rivers carry water and sediment toward the South Asian plains. Sharp changes in elevation produce a succession of climatic and ecological zones, from lower slopes to alpine terrain and the high snow zone. The broader HKH region is the headwater area for ten major Asian river systems, according to the International Centre for Integrated Mountain Development (ICIMOD).
People and regional significance
The Himalayas are inhabited and crossed by many communities whose languages, livelihoods and traditions reflect the region's varied environments. For thousands of years the mountains have held religious and cultural importance in South Asia, appearing in literature, mythologies and religious practice. Their elevation and rugged terrain have also shaped routes and contact between the subcontinent and the Tibetan Plateau. Because the Himalayas form part of a wider, interconnected mountain and river region, their environmental changes can affect communities both in high valleys and far downstream.
Key facts
- Region
- South Asia, between the Tibetan Plateau and the plains of the Indian subcontinent.
- Extent
- About 2,500 km east–west and 200–400 km north–south, using Britannica's definition of the uninterrupted range.
- Countries and territories
- Parts of India, Nepal, Bhutan, Pakistan and China.
- Highest summit
- Mount Everest.
- Geological origin
- Collision of the Indian and Eurasian continental plates beginning roughly 50–40 million years ago.
- Major rivers
- The Indus, Ganges and Brahmaputra are among the major river systems linked to Himalayan waters.
Timeline
About 225 million years ago
India was a large island off the Australian coast, separated from Asia by the Tethys Ocean, according to the USGS reconstruction.
About 80 million years ago
India was still moving north toward Asia; the USGS estimates it was roughly 6,400 km south of the Asian continent.
About 50–40 million years ago
The Indian and Eurasian continental plates began colliding, initiating rapid Himalayan uplift; convergence continues today.
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References
- 1.Himalayas Definition, Location, History, Countries, Mountains, Map, & Facts
Encyclopaedia Britannica · encyclopedia · reliability: high · retrieved 15 October 2026
Supports: Regional location and extent, major physiographic belts, mountain and river features, ecological zones, and cultural significance.
- 2.The Himalayas: Two continents collide
U.S. Geological Survey, This Dynamic Earth · other · reliability: high · retrieved 15 October 2026
Supports: Geological reconstruction of the India–Eurasia collision, its approximate timing, and the ongoing tectonic forces affecting the region.
- 3.Continental/Continental: The Himalayas
The Geological Society of London · other · reliability: high · retrieved 15 October 2026
Supports: Explains continental collision, crustal thickening, mountain uplift and continued tectonic activity in the Himalayas.
- 4.The Hindu Kush Himalaya
International Centre for Integrated Mountain Development (ICIMOD) · other · reliability: high · retrieved 15 October 2026
Supports: Defines the broader HKH region and describes its extent across eight countries and its connection to ten major Asian river systems.
- 5.Himalayas — Drainage
Encyclopaedia Britannica · encyclopedia · reliability: high · retrieved 15 October 2026
Supports: Describes Himalayan drainage and the region's major rivers.
- 6.Himalayas — People
Encyclopaedia Britannica · encyclopedia · reliability: high · retrieved 15 October 2026
Supports: Provides reference coverage of peoples and cultural life in the Himalayan region.
References are suggested by the research engine and may be incomplete. Unverified URLs are omitted rather than guessed.
Article history
- Version 115 October 2026 · EditorCreated by Zapia