River Systems: Fluvial Processes and Geomorphological Evolution
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The River System
Much of the rainwater that falls on the Earth's surface is concentrated in flows or channeled river currents.
Fluvial Processes: Load, Capacity, and Competence
The action of a river (erosion, transport, and sedimentation) for a given speed depends on the size of the particles. The action of a river is defined by:
- Load (Freight): The actual amount of sediment a river carries at a certain time and place. This may include:
- Bed Load: Larger particles carried by rolling (pebbles and gravel) or saltation (sand).
- Suspended Load: Finest materials (clay and silt) carried within the water column.
- Dissolved Load (Transport in Solution): Materials transported as soluble compounds (carbonates, sulfates, chlorides).
- Capacity: The theoretical maximum