Land counterpart of a delta . An assemblageof sediments marking place where a stream moves from a steep gradientto a flatter gradient and suddenly loses transporting power. Typicalof arid and semiarid climates but not confined to them.
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Land counterpart of a delta . An assemblageof sediments marking place where a stream moves from a steep gradientto a flatter gradient and suddenly loses transporting power. Typicalof arid and semiarid climates but not confined to them.