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It is clear that a great range of sediment sizes may be transported by a river. Sediment of small size (e.g., suspended load), when set in motion by erosive agents, may be transported through a river system to the sea, where it may be deposited as a deep-sea clay. Most sedimentary particles, however, have a more eventful journey to their final resting place. (In a geologic context, this may be a temporary resting place; sediment, for example, when it reaches the coast, may be incorporated in a delta at the river mouth or be acted upon by tides, currents, and ...(100 of 32811 words)