Reason (R): These rivers do not carry any alluvial sediments.
Explanation
Assertion (A) is true: The west-flowing rivers of Peninsular India, such as the Narmada, Tapi, Mahi, and Mandovi, generally do not form deltas due to the following reasons:
Steep Gradient and Short Course: These rivers flow through steep slopes of the Western Ghats and have a short course before reaching the Arabian Sea. This rapid flow prevents sediment deposition. Narrow Continental Shelf: The western coast has a narrow continental shelf, causing sediments to be quickly carried into deeper waters rather than accumulating near the mouth to form deltas. High Energy Waves and Currents: The Arabian Sea experiences strong wave action and currents that disperse sediments away from river mouths, further inhibiting delta formation. Reason (R) is false: While some west-flowing rivers might carry less alluvial sediment compared to east-flowing rivers that tra-verse vast plains, it’s not accurate to say they carry no alluvial sediments. The absence of deltas is due to the factors like the steep gradient of the rivers, the nature of the terrain they flow through, and the lack of a significant continental shelf where sediment could be deposited to form a delta. Thus, Assertion (A) is true and Reason (R) is false.