Distributaries form when a river splits into multiple smaller channels as it approaches a delta or an area with low gradient. This splitting occurs due to sediment buildup, which reduces the river's capacity to carry its flow, causing it to branch out. Distributaries typically develop in regions where sediment deposition is significant, allowing the river to distribute its water across a wider area. Over time, these channels can evolve and change course due to ongoing sedimentation and shifting water flow patterns.
Distributary
Tributary - flows into Distributary - flows out of
the rivers in their lower coures split into numerous channels due to the deposition of slit these channels are known as distributaries
A distributary
Padma
Distributary
A confluence.
A distributary.
hugli is not a tributary. it is distributary of ganga river
Distributary
A tributary is a river or stream that flows into a larger river or body of water, while a distributary is a branch of a river that flows away from the main channel. Tributaries add water to the main river, while distributaries branch off from it.
Hoogly river which is a distributary of ganga