The Peninsular Plateau: Overview
The Peninsular Plateau is a tableland of old crystalline, igneous and metamorphic rocks. It is the oldest and most stable part of India, a broken part of Gondwanaland.
Key facts
- Shape: an irregular triangle with its base along the Delhi ridge / Aravalli-Rajmahal line and its apex at Kanyakumari.
- Area: about 16 lakh sq km; average height 600-900 m.
- Slope: generally west to east, shown by the east-flowing Godavari, Krishna, Kaveri (the exceptions are Narmada and Tapi, which flow west through rift valleys).
- Rocks: Archaean gneiss and schist, Dharwar, Gondwana, Deccan Trap.
- Frame: Aravalli (north-west), Vindhya-Satpura (north), Western Ghats (west), Eastern Ghats (east), Rajmahal hills (north-east).
- The plateau has been eroded, peneplained and later uplifted and faulted many times; many hills are relict (residual) mountains.
Two big divisions
| Division | Where | Features |
|---|---|---|
| Central Highlands | North of the Narmada | Aravalli, Malwa, Bundelkhand, Baghelkhand, Vindhya, Chotanagpur |
| Deccan Plateau | South of the Narmada, between the Ghats | Maharashtra, Karnataka and Telangana plateaus |
Keep practising
Notes are only half the work. Test yourself with questions and discuss doubts with other aspirants.
Prepared for exam revision from NCERT, standard geography textbooks, the Census of India 2011, the India State of Forest Report, IMD, Ministry of Agriculture and other official sources. Maps are schematic teaching maps, not Survey of India maps, and zone boundaries are approximate. Figures such as production, capacity, counts of parks and ports, and census status change, so check the latest official source before relying on them. Found a mistake? Tell us.