Question

The gently sloping accumulation of coarse alluvial deposits by a braided stream is known as

Answer 1

The gently sloping accumulation of coarse alluvial deposits by a braided stream is known as a sand bar.

Explanation:

• Deposition on the sea. Usually, the sediment load of a stream is accumulated, eroded, and redeposited in a stream channel several times, particularly during temperature variations such as flooding.
• The sediments are accumulated as bars or floodplain layers throughout the stream range. Water deposition happens as the current of water can no longer surmount gravity to hold sediments.
• 'An oxbow lake' is a small body of water created by a U-shaped bend in a river that has been cut off by flooding and drainage from the river.

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Answer 2

The gently sloping accumulation of coarse alluvial deposits by a braided stream is known as braid bars.

Explanation:

• The braided rivers consist of a network of river channels that are separated by islands. The braided rivers differ from meandering rivers as they have a threshold level of sediments or slopes and maintain a steep gradient.  

• An increase in the sediments allows for the deposition of the eroded material on the inside the curve that may shift to a meandering profile. Braided rovers are found in Africa an example of Touat Valley.

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