Rivers Flashcards

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1
Q

What is a watershed of a river?

A

Marks the edge oof a drainage basin ( highest point of land )

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2
Q

What is a source of a river?

A

Starting point of a river

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3
Q

What is the confluence of a river?

A

A point where a smaller river ( like a tributary ) join the main river

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4
Q

What is a tributary of a river?

A

A small stream which joins the main channel

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5
Q

What is the mouth of a river?

A

A point which the river enters the sea

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6
Q

What is meant by the long profile of a river?

A

Long profile of a river is the change in gradient ( steepness ) as the river goes from source to mouth. It starts off steep from the top and becomes more flatter at the lower course ( concave profile )

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7
Q

How and why does the depth of a channel change from source to mouth of a river ?

A

Width and depth increases. Starts of with vertical erosion then followed by lateral erosion as the river moves along the coast.

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8
Q

How does velocity change with distance downstream

A

Speed of flow increases with distance downstream. This is because there’s less friction due to less contact with between the river bed and banks

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9
Q

How does the gradient change with distance downstream?

A

It will decrease as the river flows downstream as it passes from an upland area down to a lowland area where it enters the sea.

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10
Q

How does discharge change with distance downstream?

A

As the river goes downstream it is fed by more tributaries and therefore discharge increases.

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11
Q

What features are found in the upper course of a river?

A

V shaped valleys
Waterfalls
Gorges

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12
Q

What features are found in the middle course of a river?

A

Meanders
Ox bow lakes

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13
Q

What features are found in the lower course of a river?

A

Levees
Floodplains

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14
Q

Which river features are examples of deposition and erosion processes?

A

Floodplains
Meanders
Ox bow lakes

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15
Q

Formation of a waterfall

A

-This is when soft rock is eroded quicker than hard rock, but hard rock is gradually undercut via hydraulic action and abrasion
-(the force of falling water creates a plunge pool)
-Eventually the cap rock is left unsupported due to the undercutting and collapses
-(fallen rock enlarges the plunge pool via abrasion)
-the process repeats itself an da gorge is formed as the waterfall retreats upstream

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16
Q

Formation of a meander

A
  • the swing of the flow of the water within the channel results in water being flung to the outer bank causes faster flow and greater erosion on the outer bank
  • this creates a river cliff due to undercutting by lateral erosion
    -on the inner bend : slow flowing due to shallower, low energy zone and deposition occurs due to low velocity, creating a slip off slope
17
Q

Formation of a floodplain and levee

A
  • when a river floods, water spreads over the surface and there is increased frictional drag resulting in deposition

-Subsequent periods of flooding results in layers of material building up a fertile floodplain
-when a river bursts its bank the largest material is deposited closest to the edge of the river and finer material travels further resulting in levees

18
Q

Formation of ox bow lake

A

-Meanders necks narrow due to erosion on the outer beds
-Eventually the 2 outer bends meet and the river cuts through the neck of the meander ( this is because the water will now take a shorter route rather than flowing around )
-Deposition gradually seals off the old meander bend, forming a straight river
-Old meander bend has been left isolated from the main channel and over time this feature may fill up with sediment.

19
Q

What is the difference in velocity between the inner bend and outer bend of a meander?

A

On the outer bend: it will be faster because its deeper and less frictional drag resulting in erosion.

On the inner bend: it will be slower because there’s more frictional drag and its shallower resulting in deposition.

20
Q

What are the typical characteristics of a waterfall?

A

-deep plunge pool
-Steep sided gorge

21
Q

What are the main changes in a river channel from the upper to the lower course?

A

-Upper course: narrow channel, a few meters wide and very shallow
Middle course: channel becomes wider and will often be over a meter deep
-Lower course: river channel becomes wide and deep

22
Q

Give 3 examples of river management techniques that are hard engineering.

A
  • Dams and reservoirs
  • Channel straightening
  • Flood relief channels
  • Embankments
23
Q

What is a dam and reservoir and how do they help manage rivers?

A

Dams: large concrete barriers built across rivers to impede flow.
Reservoir: formed behind a dam which enables the flow of a river to be controlled and reduces the risk of flow downstream

24
Q

What is a hydrograph?

A

A graph which shows how a rivers discharge changes in response to a precipitation event.

25
Q

Define thee following:
- Lag time
- Rising limb
- Peak discharge
- Base flow

A
  • Lag time: the difference between peak rainfall and peak discharge
  • Rising limb: this shows how quickly the discharge rises after a rain storm
  • Peak discharge: the highest recorded discharge following a rainfall event
  • Base flow: normal flow of a river when its water level is sustained by groundwater flow
26
Q

Give 3 ways in which change rural land-use can increase flood risk

A
  • Forestry: chopping down trees reduces interception and less water is taken up from the soil
  • Farming: soil is bare in the winter so nothing to intercept the rainfall
  • Increase in greenfield sites are being sold off to developers for housing or other human land-use ( increasing impermeable surfaces )
27
Q

Define the following terms:
- Soil moisture
- Evaporation
- Water table

A
  • Soil moisture - water held in soil
  • Evaporation - water lost from the ground ( liquid to vapour )
  • Water table: upper level of saturated zone in the soil
28
Q

How does channel straightening reduce flood risk?

A

It provides a more efficient channel allowing water to pass through quicker reducing the likelihood of a flood. ( flow is slower in meandering channels due to friction )

29
Q

Formation of an interlocking spur

A

The river cuts down into the valley. If there are areas of hard rock which are harder to erode, the river will bend around it.