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The Work of Rivers ,[object Object],[object Object],[object Object],[object Object],[object Object]
The Work of Rivers ,[object Object],[object Object],[object Object],[object Object],[object Object]
The Work of Rivers ,[object Object],[object Object],[object Object]
The Work of Rivers ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
The Work of Rivers ,[object Object],[object Object],[object Object],[object Object]
The Work of Rivers Relationship of velocity and sediment size to erosion
The Work of Rivers B. Transportation (4 ways)
The Work of Rivers B. Transportation (4 ways) ,[object Object],[object Object]
The Work of Rivers B. Transportation (4 ways) 2.  Saltation ( saltim: by leaps/jumps) Smaller and lighter rock fragments and sand hop and bounce along the river bed. At times, the distinction between traction and saltation may be difficult to determine.
The Work of Rivers B. Transportation (4 ways) 3.  Suspension Some of the load like silt and clay (fine-grained) will float along. They may only be deposited when stream velocity reaches near 0. Turbulence in the water is crucial in holding a load of sediments.
The Work of Rivers B. Transportation (4 ways) 4.  Solution Some minerals are transported in dissolved form. Especially chemical solution derived from minerals like limestone or dolomite.
The Work of Rivers ,[object Object],[object Object],[object Object],[object Object]
The Work of Rivers ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
The Work of Rivers ,[object Object],[object Object],[object Object],[object Object],[object Object]
The Work of Rivers ,[object Object],[object Object],[object Object],[object Object]

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The work of rivers

  • 1.
  • 2.
  • 3.
  • 4.
  • 5.
  • 6. The Work of Rivers Relationship of velocity and sediment size to erosion
  • 7. The Work of Rivers B. Transportation (4 ways)
  • 8.
  • 9. The Work of Rivers B. Transportation (4 ways) 2. Saltation ( saltim: by leaps/jumps) Smaller and lighter rock fragments and sand hop and bounce along the river bed. At times, the distinction between traction and saltation may be difficult to determine.
  • 10. The Work of Rivers B. Transportation (4 ways) 3. Suspension Some of the load like silt and clay (fine-grained) will float along. They may only be deposited when stream velocity reaches near 0. Turbulence in the water is crucial in holding a load of sediments.
  • 11. The Work of Rivers B. Transportation (4 ways) 4. Solution Some minerals are transported in dissolved form. Especially chemical solution derived from minerals like limestone or dolomite.
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