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Geography

Key Points at a Glance

Physiography of India

Paper II · Unit 3 Section 1 of 11 0 PYQs 28 min

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Key Points at a Glance

  1. 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
  2. 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
  3. 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
  4. 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
  5. 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
  6. 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)
  7. 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
  8. 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
  9. 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)
  10. 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
  11. 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
  12. 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
  13. 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