Braided channels are typically found in river systems characterized by a high sediment load and variable water flow. These channels consist of multiple intertwining streams or channels that split and rejoin, creating a network resembling braids. Common locations for braided channels include alpine rivers, glacial river systems, and areas with steep gradients where sediment is rapidly eroded and transported. Notable examples can be seen in places like the Brahmaputra River in India and the Yukon River in Canada.
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