Rivers Flashcards

1
Q

What is traction?

A

Traction – large pebbles and boulders are rolled along the seafloor.

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2
Q

What is saltation?

A

Saltation – beach material is bounced along the seafloor.

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3
Q

What is suspension?

A

Suspension – beach material is suspended and carried by the waves.

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4
Q

What is solution?

A

Solution – material is dissolved and carried by the water.

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5
Q

What is the long profile of the river?

A

A Long profile shows the gradient of the river from its source to mouth.

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6
Q

Where is the steepest gradient in the long profile of a river?

A

The steepest gradient in the long profile of a river is found in the upper course near to the source.

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7
Q

Why in the upper course is the cross profile of a river valley narrow and steep sided?

A

It becomes narrow and steep sided in the upper course due to vertical erosion.

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8
Q

Why does the river channel become wider and deeper with distance downstream?

A

The river channel becomes deeper due to the increase in discharge and wider due to lateral erosion.

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9
Q

In the middle course of the river valley floor becomes wider why is this?

A

The increase in lateral erosion.

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10
Q

Why do discharge and velocity increase downstream?

A

Discharge increases downstream because of additional water from tributaries. Velocity increases due to the additional water from tributaries and less water is in contact with the bed and banks so there is less friction.

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11
Q

What is vertical erosion?

A

Vertical erosion involves the deepening of the river bed. This is mostly by hydraulic action. It is most common in the upper course of the river.

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12
Q

What is lateral erosion?

A

Lateral erosion erodes the banks of the river. This is more common in the middle and lower courses of a river.

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13
Q

Identify the four Processes of erosion that occur within a river.

A

Abrasion or corrasion, attrition, hydraulic action and solution or corrosion

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14
Q

What is hydraulic action?

A

Hydraulic action is when the force of fast-flowing water hits the bed and banks and forces water and air into cracks in the bedrock. The repeated changes in air pressure cause the river bed to weaken.

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15
Q

What is abrasion?

A

Abrasion, also known as corrasion, is when boulders and stones wear away the river banks and bed. Angular rocks that have entered the channel recently are useful tools of abrasion because they are more angular. Abrasion is responsible for both lateral and vertical erosion of the river channel

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16
Q

What is attrition?

A

Attrition is when sediment particles knock against the bed or each other and break, becoming more rounded and smaller as you move down the river.

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17
Q

What is the solution?

A

Solution (or corrosion) is when acidic water dissolves rocks such as chalk or limestone.

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18
Q

What happens to the shape and size of bed load as you move down the river?

A

It becomes more rounded and smaller.

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19
Q

What is the main process of erosion in the upper course of a river?

A

Hydraulic action.

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20
Q

Identify the four main processes of transportation in a river?

A

Solution, suspension, saltation and traction.

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21
Q

What is traction?

A

Large boulders and rocks are rolled along the river bed.

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22
Q

What is saltation?

A

Small pebbles and stones are bounced along the river bed.

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23
Q

What is suspension?

A

Fine, light material is carried along in the water.

24
Q

What is solution?

A

Minerals are dissolved in the water and carried along in solution.

25
Q

What is deposition?

A

Deposition is the processes by which a river drops its load.

26
Q

Why do rivers deposit sediment?

A

Deposition occurs whenever a river loses energy and velocity falls.

27
Q

Give three examples of where a river may deposit sediment.

A

Deposition occurs: a river enters a shallow area (this could be when it floods and comes into contact with the flood plain)at the base of a waterfall on the inside bend of a meander towards its mouth where it meets another body of water.

28
Q

What is a cross profile?

A

River cross profiles show you a cross-section, taken sideways, of a river channel and/or valley at certain points in the river course.

29
Q

What is a channel cross profile?

A

A channel cross-profile is a cross section of only the river channel.

30
Q

What is a valley cross profile?

A

A valley cross-profile includes the channel, the valley floor and the sides of the valley.

31
Q

How does a channel cross-section change downstream?

A

In the upper course the channel is very narrow and very shallow. By the middle course the channel becomes wider and deeper usually over 1 m. By the lower course the channel becomes wider still and the channel is much deeper.

32
Q

Why does the channel cross-section change downstream?

A

In the upper course, the river erodes its bed by hydraulic action and abrasion. As the river flows downstream it is joined by tributaries, increasing the volume of water, velocity and therefore its erosive power. This enables it to cut a deeper channel as it flows downstream.

33
Q

What are interlocking spurs?

A

Interlocking spurs are fingers of land that jut out into the river valley that streams and rivers are forced to flow around in the upper course.

34
Q

Give three characteristics of interlocking spurs.

A

Steep gradient, convex slopes, project from alternate sides of the family, separated by a narrow valley floor which is mainly taken up by the river channel, sometimes covered in Woodland and may have scree slopes.

35
Q

What are rapids?

A

Rapids are fast flowing, turbulent sections of the river where the bed has a relatively steep gradient. They are found in the upper course of the river.

36
Q

Where are waterfalls and gorges typically found along the long profile of a river?

A

Waterfalls and gorges are typically found in the upper course of the river.

37
Q

What is a waterfall?

A

A waterfall is a step in the long profile of the valley. It is where water falls down the vertical drop in the channel usually from a considerable height.

38
Q

What is a gorge?

A

A gorge is a narrow, steep sided valley, with bare, rocky walls

39
Q

Give three characteristics of a gorge.

A

Characteristics of gorge include: very narrow valley, very steep, high valley sides. Is located immediately downstream of a waterfall. River channel takes up most, if not all, of the valley floor. Boulders litter the river bed. Turbulent, fast flowing whitewater

40
Q

How does a waterfall create a gorge?

A

As a waterfall retreats it leaves behind the steep sided valley which is called gorge. Every time the overhanging Rock breaks off the gorge retreats and grows longer.

41
Q

How is a meander formed?

A

Fast flowing water on the outside bank causes lateral erosion through hydraulic action and abrasion which under cuts the bank, creating a river cliff. Eroded material is then deposited on the inside of the next meander where friction slows the flow, creating a slip-off slope.

42
Q

What is an oxbow lake?

A

An oxbow lake is a small, horseshoe shaped lake that is located several meters from a straight stretch of river.

43
Q

Explain the formation of an oxbow lake.

A

Due to erosion on the outside of a bend and deposition on the inside, the shape of a meander will change over a period of time. Erosion narrows the neck of the land within the meander and as the process continues, the meanders move closer together. When there is a very high discharge (usually during a flood), the river cuts across the neck, taking a new, straighter and shorter route. Deposition will occur to cut off the original meander, leaving a horseshoe-shaped oxbow lake.

44
Q

What is a levee?

A

Levees are naturally raised riverbanks found along the sides of the river channel that has experienced flooding.

45
Q

What are the characteristics of levees?

A

The main characteristics of levees are: raised river banks consist of gravel, stones and small sediment. Steep on the channel side, gentle sloping on the land side. Relatively flat top covered in grass

46
Q

How are levees formed?

A

When a river floods friction with the floodplain leads to a rapid decrease in the velocity of the river and therefore its capacity to transport material. Larger material is deposited closest to the river bank. This often leads to large, raised mounds being formed. Smaller material is deposited further away and leads to the formation of gently sloping sides of the levees.

47
Q

What is a flood plain?

A

A flood plain is a large area of flat land either side of the river that experiences or has experienced flooding.

48
Q

What are the characteristics of a flood plain?

A

Characteristics of a flood plain include: A large area of flat land either side of a river. Layers of alluvium (silt/sand//sediment) cover the flood plain

49
Q

How is a flood plain formed?

A

Floodplains form due to erosion and deposition. Erosion removes any interlocking spurs, creating a wide, flat area on either side of the river. During a flood, material being carried by the river is deposited (as the river loses its speed and energy to transport material). Over time, the height of the floodplain increases as material is deposited on either side of the river. The floodplain is often a wide, flat area caused by meanders shifting along the valley.

50
Q

What is an estuary?

A

Where a river meets the sea

51
Q

How do estuaries form?

A

The river loses energy when it flows into the sea. This causes it to deposit (drop) all the sediment it was carrying. The deposited sediment builds up, forming mudflats.

52
Q

Give an example of a river valley in the UK that you have studied

A

The River Tees

53
Q

Give a feature of the uppercourse of the River Tees

A

High Force waterfall - the waterfall with the highest volume of water in England

54
Q

Give a feature of the middlecourse of the River Tees

A

The meanders near Barnard Castle and surrounding Yarm

55
Q

Give a feature of the lowercourse of the River Tees

A

The Tees estuary