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Himalayan and Peninsular Rivers Compared

Himalayan and Peninsular Rivers Compared

Drainage · 1 min read
FeatureHimalayan riversPeninsular rivers
SourceGlaciers and snowRain-fed, from plateau and Ghats
FlowPerennialSeasonal (dry in summer)
AgeYoung, still eroding (V-shaped valleys, gorges, waterfalls)Old, graded; broad shallow valleys
Length / basinLong, huge basinsShorter, smaller basins
CourseMeanders, braids, shift course; floodsStable course, rift valley (Narmada, Tapi)
MouthDeltas (Ganga-Brahmaputra)Deltas (east) and estuaries (west)
Navigation and irrigationHigh potentialLimited navigation, tanks, dams
HydropowerHugeModerate (Western Ghats), many dams
ExamplesIndus, Ganga, BrahmaputraGodavari, Krishna, Kaveri, Narmada, Tapi

East-flowing vs west-flowing peninsular rivers

East-flowingWest-flowing
Many, long, big basinsFew, short (except Narmada, Tapi)
DeltasEstuaries
Mahanadi, Godavari, Krishna, Kaveri, Pennar, SubarnarekhaNarmada, Tapi, Mahi, Sabarmati, Luni, Periyar
Rise in Western GhatsRise in Satpura-Vindhya-Aravalli or the Ghats
Flow through the Eastern Ghats gapsFlow through rifts or steep slope

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Prepared for exam revision from NCERT, standard geography textbooks, the Census of India 2011, the India State of Forest Report, IMD, Ministry of Agriculture and other official sources. Maps are schematic teaching maps, not Survey of India maps, and zone boundaries are approximate. Figures such as production, capacity, counts of parks and ports, and census status change, so check the latest official source before relying on them. Found a mistake? Tell us.