Fluvial Processes Flashcards
How do rivers erode?
- downwards (vertical erosion) and sideways (lateral erosion).
- requires large amounts of energy
Name 4 types of erosion
- abrasion / corrasion
- attrition
- hydraulic action
- solution / corrosion
Abrasion
The scraping, scouring and wearing away of the bed and banks by rock fragments carried by the river flow.
Attrition
Wearing down of the river load itself as particles strike each other and the bed and banks.
Hydraulic action
Process of river bed and bank erosion; it involves the energy of the flowing water itself.
Solution
Material chemically dissolved in water.
Name 4 types of transportation
- traction
- saltation
- suspension
- solution
Traction
Involves bed load material rolling downstream
Saltation
Process by which material is transported in a bouncing motion
Suspension
Light particles are held and carried in the flowing water
Solution
Material chemically dissolved in water
When will a river deposit its load?
If there is not enough energy to transport the particles. Larger
particles are dropped off first, then smaller.
What logic does the Hjulström curve follow?
a) the larger the particle, the more energy needed to erode or transport it
b) erosion will need more energy than transport
Anomalies in the Hjulström curve
- clay or silt have a natural cohesion and stick together, requiring more energy to lift them. Once separated the individual particles are easily carried and clay will remain suspended even at low velocities
- clay and silt particles can be very tightly packed, making the water flow smooth with little friction. The clay is less likely to be disturbed by water flow