EQ4 Flashcards

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1
Q

What is meant by the long profile of the river

A

The long profile of a river shows river gradient changes as it flows from the source to mouth

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2
Q

How does the river landscape change along its profile

A

As you go down the river the gradient will decrease , it will be highest at the source and slowly decrease

As you go down the flood plain becomes a lot wider because there is more river discharge that erodes away at the edges of the river

Bed load size will also decrease because there is a higher velocity downstream meaning the rocks will erode quicker and become smoother

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3
Q

Compare hydraulic action and abrasion

A

Hydraulic action is when water hits the cliff face eroding it while abrasion is when the water body chucks the rocks at the cliff face . Or when the water erodes the water bed

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4
Q

Define weatherinb

A

When rocks are slowly worn away due to physical, human or chemical factors

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5
Q

Compare freeze thaw weathering and biological weathering

A

Freeze thaw is when water gets into permeable rock and slowly freezes over time due to this the rock cracks while biological weathering has nothing to do with water it is about when animals or roots wear away from the rock

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6
Q

What is traction

What is suspension

A

Large boulders rolling on the sea bed

Water transports small rocks

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7
Q

How is waterfalls formed

A

Often in upper stages of river . Water flows over different bands of soft and hard rock. It erodes over time meaning the soft rock can no longer keep up the hard rock . The overhang collpases forming a plungepool. The waterfall retreats back over time due to constant erosion

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8
Q

How are u shaped valleys formed

A

Rivers high in the mountains flow down eroding the landscape vertically. The river cuts a deep notch into the landscape. As the river erodes more the valleys rock is exposed to more freeze thaw weathering which will loosen it . When the rock falls the valley sides begin to steepen helping with erosion . The rocks are transported downstream and the channel becomes wider creating a v-shape with interlocking spurs

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9
Q

How do interlocking spurs form

A

As the river erodes the landscape in the upper course bit begins winding and and swerving trying to avoid soft rock creating a zipper shape .

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10
Q

How do meanders form

A

In the middle course in the river there is more energy and a high volume of water in a narrow space . Due to this it erodes lateral to the right and left which eventually forms a bend .

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11
Q

How does an oxbow lake form

A

After a long period of time the meander becomes very curved and eventually turns narrower and the river cuts off forming an oxbow lake

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12
Q

How does a flood plain form

A

They are made by a meander eroding sideways as it travels downstream , when a river breaks its banks it leaves behind alluvium . This gradually builds up forming a flood plain

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13
Q

How do levees form

A

The natural movement of a water body pushes sediment up to the side creating a natural levee . The banks of a river are often elevated

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14
Q

How do deltas form

A

When a river reaches a lake or the sea water it slows down and drops the sediment it was carrying if not transported it will build up forming deltas

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15
Q

How does climate change effect the river landscape

A

FOR every one degree of increase you are able to store 6 percent more water vapor. More water vapor will lead to higher concentrations of precipitation which will fill up water bodies quicker leading to an increase of floods

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16
Q

How does geology effect the river landscape

A

Steep relief means that less infiltration will occur and speed up the rate of surface runoff
Impermeable rocks will lead to an increase of throughflow and suface runoff as the water cannot penetrate it. The water will fill the rivers quicker causing quicker floods and accelerating the speed of ground saturation

17
Q

How do slope processes change the river landscape

A

Mass movement will cause sediment to enter the rivers reducing its velocity and sometimes blocking up rivers

18
Q

Compare a flashy hydrograph and a subdued hydrograph

A

Flashy-
Will have a shorter lag time from peak rainfall to peak discharge . Its rising limb will also be very steep up and a slow gradual falling limb . This is opposite to a subdued hydrograph with longer lag times and its rising limb will be a gradual up while its falling limb will be a gradual down.

19
Q

What effects hydrographs

A

Farming
Impermeable surfaces
Urbanisation

20
Q

What were the causes of the eden flood

A
Farming
Drains filled up
High urbanisation
Storm desmond 
Climate change .