Concept Notes 1: Physical Divisions of the Indian Subcontinent

1. Introduction: The Geographical Architecture of India
India encompasses an area of approximately 3.28 million square kilometers, ranking as the seventh-largest country in the world. Its physical landforms showcase extraordinary diversity, spanning from young, active fold mountains in the north to ancient stable shield plateaus in the south.
THE SIX PHYSIOGRAPHIC DIVISIONS
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โผ โผ โผ
[ NORTHERN MOUNTAINS ] [ INDO-GANGETIC PLAINS ] [ PENINSULAR PLATEAU ]
โข 2,400 km Himalayan arc โข 7 lakh sq. km alluvium โข Central Highlands
โข Himadri, Himachal, โข Bhabar, Terai, Bhangar, โข Deccan Trap (Basalt)
Shiwalik ranges Khadar belts โข Western & Eastern Ghats
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โผ โผ โผ
[ THAR DESERT (WEST) ] [ COASTAL PLAINS ] [ ISLAND GROUPS ]
โข Aravalli rain shadow โข Western Coast (Narrow) โข Lakshadweep (Coral)
โข Sand dunes & Luni river โข Eastern Coast (Deltas) โข Andaman & Nicobar (Volcanic)
2. Detailed Characteristics of the Physical Divisions
A. The Northern Mountain Arc (The Himalayas)
The Himalayas are young fold mountains formed by the collision between the Indo-Australian Plate and the Eurasian Plate:
- Himadri (Greater Himalayas): The northernmost and highest continuous range, with an average elevation of 6,000 meters. Contains Mount Everest (8,848 m) and Kanchenjunga (8,586 m). Perennially snow-bound.
- Himachal (Lesser Himalayas): Altitude ranges between 3,700 and 4,500 meters. Famous for hill stations like Shimla, Mussoorie, and Nainital, and valley formations (Kashmir, Kangra, Kullu).
- Shiwaliks (Outer Himalayas): The outermost range with altitude between 900 and 1,100 meters, composed of unconsolidated river sediments prone to landslides. Valleys between Himachal and Shiwaliks are called Duns (e.g., Dehradun).
B. The Northern Plains
Formed by the deposition of alluvium brought by the Indus, Ganga, and Brahmaputra rivers. Morphologically divided into four zones:
- Bhabar: A narrow belt (8โ16 km wide) along the Shiwalik foothills containing pebbles and gravel where streams disappear underground.
- Terai: A wet, marshy, heavily forested plain south of Bhabar where streams re-emerge.
- Bhangar: Older alluvial soil situated above the floodplains, containing calcareous deposits known as Kankar.
- Khadar: Newer, highly fertile alluvial deposits renewed annually by seasonal floods, ideal for intensive agriculture.
C. The Peninsular Plateau
An ancient triangular tableland composed of crystalline igneous and metamorphic rocks:
- Central Highlands: North of the Narmada River, sloping towards the north and east (Malwa Plateau, Bundelkhand, Chota Nagpur Plateau).
- Deccan Plateau: South of the Narmada, bounded by the Satpura Range in the north. Its northwestern part consists of the Deccan Trapโthick sheets of solidified basaltic lava creating nutrient-rich Black Soil (Regur).