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4.5. Comparison Between Himalayan and Peninsular Rivers
Difference between the rivers rising in the Himalayas and those rising in the Peninsular plateau are primarily a result of the differences between the two areas in terms of relief and climate. Following table shows major differences between these two groups.
S.N. | Aspects | Himalayan River | Peninsular River | ||||
1 | Place of Origin | Himalayan mountain covered with glaciers | Peninsular plateau highland | and central | |||
2 | Nature of flow | Perennial | Ephemeral | ||||
3 | Type of drainage | Antecedent and Consequent leading to dendritic pattern | Super imposed, resulting in trellis, rectangular Patterns | rejuvenated radial and | |||
4 | Nature of river | Long course, flowing through the rugged mountains experiencing headward erosion and river capturing; In plains meandering and shifting of Course; | Smaller, fixed course with well- adjusted valleys; | ||||
5 | Catchment area | Very large basins | Relatively smaller basin | ||||
6 | Age of the river | Young, active and deepening of valley | Old rivers with graded profile and lateral erosion | ||||
7 | Irrigation | Flows through plains and canal system | Flows over uneven plateau; canals only in deltaic region | ||||
8 | Hydro- electricity | Eastern region potential and building up | has large | very dams | high are | Natural waterfalls for generating electricity |