Your answer is correct. Even if the flow no longer has enough energy for a full transport of solids, they are still in the sediment and suspension state. The resulting transport bodies (ripples, dunes, banks) can become solidified deposits.

Your answer is partially correct. Even if the flow no longer has enough energy for a full transport of solids, they are still in the sediment and suspension state. The resulting transport bodies (ripples, dunes, banks) can become solidified deposits.

Unfortunately, your answer is not correct. Even if the flow no longer has enough energy for a full transport of solids, they are still in the sediment and suspension state. The resulting transport bodies (ripples, dunes, banks) can become solidified deposits.

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