Physical (Long profile) Flashcards

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1
Q

In general, what is the long profile of a river

A

It is usually smoothly concave, with the gradient being steeper in the upper course + becoming progressively gentler towards the mouth

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2
Q

How are irregularities in the gradient (which frequently occur) sometimes represented

A

As rapids, waterfalls and lakes

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3
Q

What are knickpoints

A

Marked breaks/changes in the slope of the long profile of a river, which is generally the product of rejuvenation

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4
Q

How does dynamic equilibrium occur

A

Irregularities in the long profile are eventually worn away by river erosion to give a smooth graded profile

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5
Q

What is dynamic equilibrium

A

Where balance has been achieved between processes of erosion and deposition

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6
Q

What do some geographers say about how a graded profile is achieved

A

They say it is when the river uses up all of its energy in the movement of water and sediment so that no free energy is left to undertake further erosion.

But if the volume and load of the river change over the long term, the river channel and its long profile will adjust to new conditions.

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7
Q

What is long profile (of a river)

A

It illustrates the changes in altitude of the course of the river

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8
Q

Which stage of the river has the most energy

A

Lower (as it is wider and there is more water increasing the velocity and therefore energy)

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9
Q

What does hydraulic radius show

A

The efficiency of the channel (ability is the channel to move water)

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10
Q

How do you calculate hydraulic radius

A

X-Sectional area / wetted perimeter

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11
Q

The higher the hydraulic radius..

A

The higher the efficiency

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12
Q

What is wetted perimeter

A

The length of the ned and banks in contact with the water

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13
Q

What is channel shape

A

The size of the channel (width : depth ratio) - it increases downstream

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14
Q

In which part of the river does velocity increases

A

Downstream

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15
Q

Why does velocity increase downstream

A

Upper course- narrow and shallow so a large proportion of the water is in contact with the bed and banks thus hydraulic radius is low; whereas in the lower course the channel becomes wider and deeper.
Although the wetted perimeter increases, there is less water in contact with bed + banks compared to cross area

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16
Q

What erosion and transportation is in the upper course

A

Vertical- erosion hydraulic action and attrition.

Transportation- Traction and suspension, solution.

17
Q

What deposition is in the upper course

A

It is limited to large bed load

18
Q

What erosion is in the middle course of the river

A

Attrition and hydraulic action, more lateral erosion

19
Q

What transportation and deposition is in the middle course of the river

A

Smaller traction bed load, more suspension and little solution.
Courser material is deposited and is deposited on slopes.

20
Q

What erosion and transportation is in the lower course

A

Erosion is reduced- some lateral erosion on meanders.

Pebble bed load and suspension

21
Q

What deposition is in the lower course

A

Deposition is fine, forms slip off slopes, levées and floodplains