The Himalayas are divided longitudinally into four distinct parallel mountain ranges from north to south, each with unique geological and structural features.
- Trans-Himalayas (Tethys Himalayas): Located north of the Great Himalayas, containing the Karakoram, Zaskar, Ladakh, and Kailash ranges. Mount Godwin-Austen (K2, 8611m) lies in the Karakoram range.
- Greater Himalayas (Himadri): The northernmost and highest continuous range with an average elevation of 6,000 meters. Composed of central crystalline rocks (granites and gneisses) and houses peaks like Mt. Everest, Kanchenjunga, and Nanga Parbat.
- Lesser Himalayas (Himachal): Rugged range running parallel to the south of Himadri, averaging 3,700 to 4,500 meters. Features famous hill stations and valleys like Kashmir Valley, Kangra, and Kullu Valley.
- Outer Himalayas (Shiwaliks): The outermost southern foothills composed of unconsolidated sediments brought down by rivers. Altitude varies from 900 to 1,100 meters, featuring flat-structural valleys called Duns (Dehra Dun) in the west and Duars in the east.
| Range / Region | Key Feature / Valley | Important Pass / Peak |
|---|---|---|
| Greater Himalayas | Perennial snowline, source of major rivers | Zoji La, Shipki La, Nathu La |
| Lesser Himalayas | Kashmir & Kathmandu Valleys | Pir Panjal, Banihal Pass |
| Trans-Himalayas | Rain shadow zone, cold desert | Karakoram Pass, Khardung La |
| Shiwalik Range | Dun formations (Dehra Dun, Patli Dun) | Mohand Pass |