Topography of Peninsular Plateau
The topography of the peninsular plateau comprises several small as well as big plateaus with smoother surfaces and also broadly rounded tops that seldom rise up to 600 meters.
Denudation and its effects have been stopped by the hard rocks and the subordinate hills are remnants of the previous systems of mountains like the Aravalli hills or the stricter elements of the same plateau which have weathered erosion. Volcanic eruptions have been occurring for several places and also cover broad swaths of northwest Deccan having a thick volcanic lava mantle.
Peninsular Plateau of India
Peninsular Plateau: Peninsular plateau refers to the tableland of crystalline, igneous, and metamorphic rocks from the past and is produced by a breakup and drifting of the Gondwana continent, making it one of the oldest landmasses. The plateaus are characterized by vast and shallow valleys and rounded hills. The two important sections include the Central Highlands and the Deccan Plateau.
Central Highlands refers to the section of the Peninsular plateau to the north of the Narmada River, which covers a major portion of the Malwa plateau. Both Satpura ranges as well as Aravallis define the Vidhya range. The sandy, as well as the stony desert of Rajasthan, blends in a farther westward extension.
Table of Content
- Peninsular Plateau of India Map
- Characteristics of Peninsular Plateau
- Two Important Plateaus
- Importance of the Peninsular Plateau
- The Stretch of Peninsular Plateau
- Topography of Peninsular Plateau
- Central Highlands
Contact Us