Describe the topography of Malwa Plateau.

Introduction: The Malwa Plateau (मालवा का पठार) is a triangular-shaped, elevated tableland situated in western Madhya Pradesh, covering 88,222 sq. km (~28.62%) of the state's geographical area, bounded by the Vindhyan scarps in the south and the Aravalli hills in the northwest.

1. Geological Formation and Topographic Origin:

• Formed during the late Cretaceous era by fissure eruptions of basic basaltic lava of the Deccan Traps.
• Centuries of denudation and weathering transformed original step-like volcanic terraces into a flat-topped, undulating, rolling peneplain tableland.

2. Relief, Elevation, and Major Mountain Peaks:

• General elevation averages between 300 and 600 metres above sea level, with a gentle, consistent slope towards the north and north-east.
• Prominent Mountain Peaks of Malwa:
  1. Sigar Peak (881 metres): Highest mountain peak of the Malwa Plateau situated in the Mandu-Janapav ridge.
  2. Janapav Peak (854 metres): Historic hill near Mhow (sacred origin of Chambal River and Parashurama hermitage).
  3. Dhajari Peak (810 metres): Another prominent peak near Indore.
  4. Gomanpur Peak (510 metres).

3. Hydrographic Drainage Topography:

• Rivers follow the gentle north-easterly structural slope into the Yamuna basin:
  • Chambal River: Cuts magnificent gorges and waterfalls (Patalpani, Chulia).
  • Shipra River: Sacred meandering river draining into Chambal.
  • Kali Sindh, Parbati, Nevaj, Gambhir, and Betwa.

4. Edaphic and Soil Characteristics:

• Covered with deep and medium fertile Black Cotton Soil (Regur) formed by basalt weathering, supporting intensive cultivation of GI Sharbati Wheat, Soybean, and Cotton.

Conclusion: Malwa Plateau's distinct flat-topped basaltic relief, fertile black soil, and temperate climate constitute the agricultural and economic core of Madhya Pradesh.