A braided stream is indicative of excess sedimentation.

Name: A braided stream is indicative of excess sedimentation.
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Braided streams are formed when there is an excess of sediment in the river, causing the formation of multiple channels that weave and braid around each other. The sediment can come from sources such as erosion, landslides, or heavy rainfall. The braided pattern allows for the river to carry the heavy load of sediment without becoming blocked or flooding.

A Braided Stream Is Indicative of Excess Sedimentation