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Key Points at a Glance
Six Major Physiographic Divisions
- Himalayan Mountains, Indo-Gangetic Plain, Peninsular Plateau
- Great Indian Desert (Thar), Coastal Plains, Islands
- Each division differs in geological age, origin, and economic use
- Together they cover all of India's 32.87 lakh sq km
Himalayas — Stretch and Dimensions
- Extend 2,500 km from Indus Gorge (west) to Brahmaputra Gorge (east)
- Average width 150–400 km
- India's highest peak is Kangchenjunga (8,586 m) on the Sikkim-Nepal border
- Still rising at ~5 mm per year due to ongoing plate collision
Three Parallel Himalayan Ranges
- Greater Himalayas (Himadri) — avg height 6,000 m; perpetually snow-covered
- Lesser Himalayas (Himachal) — avg 3,700–4,500 m; hill stations and forests
- Outer Himalayas (Shiwaliks) — 600–1,500 m; youngest; prone to erosion
Indo-Gangetic Plain — World's Largest Alluvial Plain
- 2,400 km long, 150–300 km wide, covering ~7.5 lakh sq km
- Divided into four zones: Bhabar, Terai, Bangar (old alluvium), Khadar (new alluvium)
- Khadar is the most fertile — renewed annually by Himalayan rivers
- Supports over 40% of India's food grain output
Peninsular Plateau — Ancient Gondwana Origin
- One of the oldest and most stable landmasses (Gondwanaland origin)
- Composed mainly of Deccan Trap basalts and Archaean gneisses and schists
- Average elevation 600–900 m; covers ~16 lakh sq km (half of India)
- Source of India's richest coal, iron ore, bauxite, and manganese deposits
Western Ghats (Sahyadri) — Key Facts
- Run 1,600 km from the Tapi River (north) to Kanyakumari (south)
- Highest peak Anamudi (2,695 m) in Kerala — highest south of the Himalayas
- Form a continuous watershed separating the narrow Konkan coast from Deccan Plateau
- UNESCO World Heritage biodiversity hotspot (2012)
Eastern Ghats — Discontinuous Range
- Discontinuous, averaging 600 m height
- Cut across by Mahanadi, Godavari, Krishna, and Kaveri rivers
- Highest peak Jindhagada (1,690 m) in Andhra Pradesh
- Rich in bauxite (Visakhapatnam) and iron ore deposits
Shivaliks and Dun Valleys
- Shivalik Hills (Outer Himalayas) are geologically youngest
- Intermontane valleys between Shivaliks and Lesser Himalayas are called Duns
- Key Duns: Dehra Dun (85 km long, 25 km wide), Patli Dun, Kotli Dun
- Formed ~5–2 million years ago from debris eroded from younger Himalayas
Coastal Plains — East vs West
- Eastern coastal plain is wider (100–120 km) with major deltas of Mahanadi, Godavari, Krishna, and Kaveri
- Western coastal plain is narrower (10–80 km)
- Western plain divided into Konkan (north), Goa, and Malabar (south) sections
- Total coastline: 7,516 km (including island territories)
India's Two Island Groups
- Andaman & Nicobar (Bay of Bengal) — 572 islands, 8,249 sq km
- Southern tip Indira Point at 6°45'N is India's southernmost point
- Lakshadweep (Arabian Sea) — 36 coral atolls, 32 sq km (smallest UT)
- A&N commands the Malacca Strait; strategically vital
Important Mountain Passes (PYQ 2023)
- Nathu La (Sikkim, 4,310 m), Shipki La (Himachal, 3,933 m)
- Rohtang Pass (Himachal, 3,978 m), Zoji La (J&K, 3,529 m)
- Pal Ghat (Kerala, 150 m) — lowest gap in Western Ghats
Thar Desert — Key Characteristics
- Lies west of the Aravallis in Rajasthan; area ~2.09 lakh sq km in India
- Extends into Pakistan as the Cholistan Desert
- Landforms: sandy plains (Erg), barren rocky plateaus (Reg), shifting barchan dunes
- Salt lakes: Sambhar, Didwana, Pachpadra; India's highest solar energy potential
Shivalik Formation — PYQ 2021 Q3
- Formed through continental collision of Indian and Eurasian plates
- Tethys Sea sediments were folded and uplifted
- Shivaliks are the youngest range, formed 5–2 million years ago
- Debris eroded from the younger Himalayas built up the Shivalik structure
