Fluvial Processes Flashcards

0
Q

Suspended load: (4)

A

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.

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1
Q

Bed load: (3)

A

Measured by average particle size.
Intermediate particles move by saltation.
Large particles bounce / slide along the floor.

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2
Q

Dissolved load: (3)

A

Amount and type of material is influenced by the rocks in the area.
Consists of ions.
Limestones dissolve more readily than basalt.

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3
Q

Precipitation deposited high

A

Journeys back down by the pull of gravity.

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4
Q

Pe = Mgh

g - acceleration due to gravity, m s-2.

A

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.

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5
Q

Potential energy ➡️ Kinetic energy in

A

Flows of streams on land.

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6
Q

Graded stream: A progressively lower

A

Gradient is needed to transport the stream load.

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7
Q

Graded stream: The inputs and

A

Outputs of the stream load are balanced.

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8
Q

Graded stream: Achieves

A

Equilibrium with its surroundings.

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9
Q

Graded stream: Steeper profile at

A

The top, gentle at the bottom.

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10
Q

Graded stream: Shallow water on a

A

Steep slope can transport the same load as deep water on a shallow slope.

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11
Q

Graded profile: Dependent on

A

The base level of the river.

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12
Q

Graded profile: If the base level changes,

A

The gradient will either increase or decrease.

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13
Q

Graded profile: A change in the base level may

A

Be from a change in sea level or from regional uplift.

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14
Q

Graded profile: Streams respond to base level changes by

A

Altering how much they erode and depositing new material until a new grade is achieved.

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