Fluvial Processes Flashcards
Suspended load: (4)
Fine particles.
In turbulent eddies.
Can remain suspended for long period of time.
A lot of S load can determine the river colour - China’s yellow river.
Bed load: (3)
Measured by average particle size.
Intermediate particles move by saltation.
Large particles bounce / slide along the floor.
Dissolved load: (3)
Amount and type of material is influenced by the rocks in the area.
Consists of ions.
Limestones dissolve more readily than basalt.
Precipitation deposited high
Journeys back down by the pull of gravity.
Pe = Mgh
g - acceleration due to gravity, m s-2.
90% of Pe in rivers is dissipated as internal turbulence in the water itself. Less than 10% of Pe is available to erode and transport rock particles.
Potential energy ➡️ Kinetic energy in
Flows of streams on land.
Graded stream: A progressively lower
Gradient is needed to transport the stream load.
Graded stream: The inputs and
Outputs of the stream load are balanced.
Graded stream: Achieves
Equilibrium with its surroundings.
Graded stream: Steeper profile at
The top, gentle at the bottom.
Graded stream: Shallow water on a
Steep slope can transport the same load as deep water on a shallow slope.
Graded profile: Dependent on
The base level of the river.
Graded profile: If the base level changes,
The gradient will either increase or decrease.
Graded profile: A change in the base level may
Be from a change in sea level or from regional uplift.
Graded profile: Streams respond to base level changes by
Altering how much they erode and depositing new material until a new grade is achieved.