KERALA PSC / INDIAN GEOGRAPHY / DIFFERENCE BETWEEN THE HIMALAYAN AND THE PENINSULAR RIVERS / NOTES / OBJECTIVE QUESTIONS / STUDY MATERIALS / GENERAL KNOWLEDGE
KERALA PSC / INDIAN GEOGRAPHY / DIFFERENCE BETWEEN THE HIMALAYAN AND THE PENINSULAR RIVERS / NOTES / OBJECTIVE QUESTIONS / STUDY MATERIALS / GENERAL KNOWLEDGE
|
Himalayan
rivers |
Peninsular
Rivers |
|
·
Extensive
catchment area |
·
Comparatively
small catchment area |
|
·
Rain-fed and
snow-fed so perennial |
·
Rain-fed, non-perennial
seasonal in nature |
|
·
High erosive
capability |
·
Low erosive
capability |
|
·
Develop gorges
in the mountains and meanders in the plains |
·
Deep valleys are
not produced as they flow through hard crystalline rocks |
|
·
They are
slow-moving and are generally free from rapids and waterfalls in their lower
courses through the plains. So they are useful in inland waterways |
·
They have
waterfalls and rapids in their courses. These observations make the
peninsular rivers less useful in inland waterways. |
KERALA PSC / INDIAN GEOGRAPHY / DIFFERENCE BETWEEN THE HIMALAYAN AND THE PENINSULAR RIVERS / NOTES / OBJECTIVE QUESTIONS / STUDY MATERIALS / GENERAL KNOWLEDGE

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