The Alaknanda river rises mainly from the region near A Satopanth glacier B Gangotri Glacier C Rohtang Pass D Zemu
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Chapter 4: Himalayan River Systems (Set-3)
The Ganga becomes a wide plain river mainly after entering the A Deccan Plateau B Thar Desert C Peninsular hills
Continue readingChapter 4: Himalayan River Systems (Set-1)
The Ganga is officially considered formed after which Himalayan confluence A Rudraprayag confluence B Devprayag confluence C Karnaprayag confluence D
Continue readingChapter 3: Drainage – Concepts and Drainage Systems in India (Set-5)
In a river basin, the boundary line separating one basin from another is called A River mouth point B Delta
Continue readingChapter 3: Drainage – Concepts and Drainage Systems in India (Set-4)
When a river enters a plain from mountains, the most likely immediate change is A Gradient becomes gentler B Tides
Continue readingChapter 3: Drainage – Concepts and Drainage Systems in India (Set-3)
The line joining the highest points of ridges that separates two basins is also called A Meander loop bend B
Continue readingChapter 3: Drainage – Concepts and Drainage Systems in India (Set-2)
In a drainage basin, the highest point on the divide mainly decides A Delta formation speed B Estuary tidal range
Continue readingChapter 3: Drainage – Concepts and Drainage Systems in India (Set-1)
If the longitudinal profile shows a sudden steep drop (knick point), it most strongly suggests A Delta progradation only B
Continue readingChapter 2: Physiographic Divisions of India (Set-5)
The Trans-Himalayan cold desert condition is mainly caused by A Coastal sea influence B Delta sediment spread C Rain shadow
Continue readingChapter 2: Physiographic Divisions of India (Set-4)
The Himalayas create a rain-shadow effect mainly in regions lying A South of Terai B East of Doab C North
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