Q.There is no formation of deltas by rivers of the Western Ghats. Why?

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Reasons for No Delta Formation by West-Flowing Rivers

• Short River Courses: West-flowing rivers (such as the Mandovi, Sharavati, and Periyar) have very short distances to travel before emptying into the Arabian Sea. Consequently, they have limited catchment areas and insufficient time to erode rocks and accumulate the massive volume of sediment required for delta building.
• Steep Gradients and High Velocity: The Western Ghats present a steep western escarpment. Rivers flowing down these steep slopes have high kinetic energy and flow with great velocity. This rapid flow allows the rivers to carry sediment directly into the deep sea rather than depositing it at the coast.
• Narrow Continental Shelf: The western coast of India is characterized by a very narrow continental shelf that drops off sharply into the deep waters of the Arabian Sea. Any sediment brought down by the rivers is quickly swept into deep oceanic trenches, preventing coastal accumulation.
• High Tidal and Wave Energy: The Arabian Sea experiences strong wave action, high-energy tides, and powerful coastal currents. These forces continuously scrub the river mouths, dispersing and transporting any deposited sediment away from the coast, which prevents the formation of deltaic lobes.
• Rocky Coastline and Hard Rock Geology: The western coast is predominantly a submerged, rocky coastline with hard basaltic rock formations. The rivers flow over hard, crystalline rocks that resist erosion, resulting in a very low initial sediment load.
• Absence of Floodplains: Due to the steep terrain and short courses, these rivers do not develop extensive floodplains or meandering courses where sediment deposition typically occurs before reaching the sea.
• Rapid Drainage: The proximity of the Western Ghats to the Arabian Sea ensures that rivers drain almost immediately into the sea, bypassing the gradual, slow-moving coastal phase essential for deltaic deposition.