Originates as Tsangpo in Tibet. Enters India via Arunachal Pradesh (Dihang). Peninsular Rivers: Non-perennial, rain-fed rivers.
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This section focuses on the Earth's natural processes and landforms.
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Formed by the alluvial deposits of the Indus, Ganga, and Brahmaputra rivers. Divided into Bhabar (pebble-studded), Terai (marshy), Bhangar (older alluvium), and Khadar (newer, fertile alluvium). Originates as Tsangpo in Tibet
Divided into Crust, Mantle, and Core. The lithosphere comprises the crust and uppermost solid mantle. The asthenosphere is the highly viscous, mechanically weak zone upper mantle where magma originates.
Driven by wind, gravity, and density differences.
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Kharif: Sown with the onset of monsoons (Rice, Maize, Cotton, Jowar, Bajra).