78. Physiography of India
भारत की भू-आकृतिCORE 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
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PREDICTED Predicted RAS Questions
Based on PYQ trends and 2026 syllabus analysis
1 5M How were the Himalayas formed? Distinguish between Himadri, Himachal, and Shiwaliks.
Model Answer
The Himalayas are fold mountains formed by the collision of the Indian and Eurasian plates, compressing Tethys Sea sediments upward (~70–40 million years ago). Himadri (Inner Himalayas) is the highest range, averaging 6,000 m, with perpetual snow. Himachal (Middle Himalayas) averages 3,700–4,500 m; contains hill stations like Shimla. Shiwaliks (Outer Himalayas) are youngest, 600–1,500 m, formed from eroded debris; Duns (like Dehra Dun) lie between them and Himachal.
~50 words • 5 marks
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