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рддрддреНрд╕рдо рдФрд░ рддрджреНрднрд╡ рд╢рдмреНрдж рдХреА рдкрд░рд┐рднрд╛рд╖рд╛,рдкрд╣рдЪрд╛рдирдиреЗ рдХреЗ рдирд┐рдпрдо рдФрд░ рдЙрджрд╣рд╛рд░рдг - Tatsam Tadbhav

рддрддреНрд╕рдо рд╢рдмреНрдж (Tatsam Shabd) : рддрддреНрд╕рдо рджреЛ рд╢рдмреНрджреЛрдВ рд╕реЗ рдорд┐рд▓рдХрд░ рдмрдирд╛ рд╣реИ тАУ рддрдд +рд╕рдо , рдЬрд┐рд╕рдХрд╛ рдЕрд░реНрде рд╣реЛрддрд╛ рд╣реИ рдЬреНрдпреЛрдВ рдХрд╛ рддреНрдпреЛрдВред рдЬрд┐рди рд╢рдмреНрджреЛрдВ рдХреЛ рд╕рдВрд╕реНрдХреГрдд рд╕реЗ рдмрд┐рдирд╛...

West Flowing Rivers of The Peninsular India

тЬЕThe west flowing rivers of the Peninsular India are fewer and smaller as compared to their east flowing counterparts.

тЬЕThe two major west flowing rivers are the Narmada and the Tapi.

тЬЕThis exceptional behavior is because these rivers didnтАЩt form valleys and instead they flow through faults (linear rift, rift valley, trough) created due to the bending of the northern peninsula during the formation process of Himalayas.

тЬЕThese faults run parallel to the Vindhyas and the Satpuras.

тЬЕThe Sabarmati, Mahi and Luni are other rivers of the Peninsular India which flow westwards.

тЬЕHundreds of small streams originating in the Western Ghats flow swiftly westwards and join the Arabian Sea.

тЬЕIt is interesting to note that the Peninsular rivers which fall into the Arabian Sea do not form deltas, but only estuaries. {Fluvial Depositional Landforms}

тЬЕThis is due to the fact that the west flowing rivers, especially the Narmada and the Tapi flow through hard rocks and hence do not carry any good amount of silt.

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