The Peninsular Plateau
The Peninsular Plateau is an ancient tableland in India, largely formed by the fragmentation of Gondwana land, making it one of the oldest landmasses in the country. Composed primarily of crystalline, igneous, and metamorphic rocks, it displays a unique topography of rounded hills and broad valleys. It can be subdivided into two primary regions:
1. Central Highlands
This region lies north of the Narmada River and constitutes the larger portion of the Malwa plateau.
- Geographical Features: Bounded by the Vindhyan and Satpura ranges, it features rivers such as Chambal and Betwa flowing from southwest to northeast.
- Key Divisions: The eastern extensions include Bundelkhand and Baghelkhand, while the Chotanagpur plateau serves as the further eastern extension, known for being drained by the Damodar River.
2. Deccan Plateau
This triangular area lies south of the Narmada River and is flanked by the Western and Eastern Ghats.
- Geographical Orientation: Higher elevation on the western side, sloping gently eastward, with notable hills including the Western Ghats approaching 1600 meters.
- Ecological Importance: The plateau's geological setting contributes to the black soil formation, crucial for agriculture.
Importance in Context
The Peninsular Plateau plays a crucial role as a mineral storehouse, influences agricultural viability due to its black soil, and affects the climatic conditions due to its elevated geography.