Types Of Stream Channels Flashcards

0
Q

Meandering channels: An ox-bow lake is

A

An abandoned meander bend.

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1
Q

Meandering channels: (3)

A

Sinuosity of >1.5
Cut through deposits of fine clay and silt.
Channel and floodplain have moderate gradients.

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2
Q

Meandering channels: Meander is a sine-generated curve,

A

It has the smallest variation in the change of direction. The stream does the least amount of work in turning.

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3
Q

Meandering channels: River minimises resistance to flow and

A

Spreads energy as evenly as possible along its course.

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4
Q

Meandering channels: The speed of the moving water isn’t the same everywhere,

A

On a bend, the zone of high speed is at the outside of the channel.

The water at depth flows slower than the surface water because of the friction from the channel bed.

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5
Q

Meandering channels: Helical flow - Fast moving water

A

Builds up against the outside bank, creating large pressure than the water at depth. The pressure gradient causes the surface water to sink and return to the inner bank, along the river bed.

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6
Q

Meandering channels: Helical flow - Erosion occurs on the

A

Outside of the bend, deposition on the inside bend. This produces point bars on the inside bend.

The point of erosion occurs slightly downstream of meander midpoint, resulting in the meander widening in that direction.

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7
Q

Sinuosity: A measure of

A

How straight a stream is.

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8
Q

Sinuosity: is related to

A

Gradient and composition of stream bed.

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9
Q

Sinuosity (S) =

A

Length of stream channel / Straight distance

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10
Q

Braided channels: Material eroded form banks is

A

Transported a short distance then deposited as a bar. The bar is an obstacle to water flow and eventually builds up above the water surface.

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11
Q

Braided channels: Easily eroded banks,

A

Pushed back due to lateral erosion during floods. The stream widens, becomes shallower and the water velocity drops.

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12
Q

Braided channels: Have steep

A

River gradients, with coarse, uncohesive bank sediments.

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13
Q

Braided channels:

Braiding index =

A

Sum of length of bars in stream section / length of stream section (L)

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14
Q

Straight channels: (5)

A
Steep banks, 
Sinuosity of < 1.5,
Unusual, 
Gentle gradient, 
Fine banks of silt and clay.
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15
Q

Straight channels: Absence of

A

Significant downstream water velocity.

16
Q

Straight channels: Thalweg - The line of

A

Maximum depth and strongest current, usually winds from one side to the other.

17
Q

Straight channels: Thalweg - As it approaches one side

A

Of the bank, sand and mud deposits accumulate on the opposite side.