Paper 1 Section 1 Flashcards

1
Q

Describe the distribution of UK’s upland and lowland areas

A

The Upland areas are located in the North West of the UK. particularly in Scotland and Wales.
The lowland areas are in the South East of the UK.

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2
Q

Which areas of the UK were glaciated during the last
ice age? (covered by ice)

A

The north west of the UK e.g. Snowdonia and Lake district

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3
Q

What is the climate like in the UK’s upland areas?

A

Relief rainfall = rain surplus
Higher altitude = colder weather
More mist cloud and snow
Windy - exposed

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4
Q

What is the difference between weathering and erosion?

A

Weathering happens ‘in situ’ one place. Erosion happens as sediment is transported/ taken away e.g. moving river or waves

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5
Q

Name 3 different types of weathering.

A

Chemical, biological and mechanical.

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6
Q

How long ago did the last Ice –Age end in the UK?

A

Around 10,000 years ago

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7
Q

Name an example of an igneous rock.

A

Pumice or granite, basalt

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8
Q

Explain how chemical weathering can happen.

A

Some rocks altered by water. limestone. weakened by oxidation.
Sulphur dioxide in the atmosphere makes the rain acidic. It can dissolve chalk and limestone

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9
Q

What is meant by “geomorphic processes?”

A

Earth changing/moving – weathering, erosion, transportation, deposition.

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10
Q

Name three human activities that take place in upland areas.

A

Forestry, reservoirs and dams, tourism: hiking, hill sheep farming

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11
Q

Why are upland areas suitable for building dams and reservoirs? (3 reasons)

A

Steep slopes, high rainfall, sparsely populated, natural deep valleys

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12
Q

Explain how freeze-thaw action works.

A

Water gets into the cracks, freezes, expands puts pressure on the rock. When temperatures rise it thaws and contracts. Repeated over time and the rock breaks down

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13
Q

Why does arable farming take place in lowland areas of the UK?

A

Large areas of flat land, these areas have deep nutrient rich soil which are ideal for farming crops.

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14
Q

What is mass movement? (Give two examples)

A

Large scale movement of material under the influence of gravity
Sliding top down and slumping from the bottom

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15
Q

Name the four processes of erosion. (HA, Ab, At, So)
.

A

Hydraulic action, abrasion, attrition, solution

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16
Q

What are the four processes of Transport? How does a river carry sediment along? (T, S, S, S)

A

Traction, saltation, suspension, solution.

17
Q

A river, glacier or the sea “dumps” sediment. What is a better word than “dumps?”

A

Deposits (deposition)

18
Q

Name four features or landforms that you would expect to see in an area that had been glaciated.

A

Erratic (large boulders), scree slope, corrie, u-shape valley. Tarn lake

19
Q

Explain how a river can erode its bed and banks by hydraulic action

A

The power of the water weakens the rocks, creating cracks in the bank and bed. When water is forced into the cracks it expands, increasing pressure and rock breaks apart.

20
Q

How can the type of rock affect the speed of erosion by the sea?

A

The softer the rock the quicker it is eroded for example clay erodes very quickly

21
Q

Name a rock that can be eroded by solution

A

Limestone

22
Q

Explain how a river creates a V shaped valley near the source.

A

In the upper course of the valley the river is eroding down wards (vertical erosion) this creates a steep sided river channel. Over many years these steep sides are weathered away (e.g. freeze/thaw action) and the sides fall into the river. This leaves a V shape

23
Q

Explain how waterfalls are formed. (4 points)

A

Bands of hard rock over a band of soft rock (sandstone over mudstone)
Soft rock eroded more quickly creating a plunge pool at the bottom of the waterfall. Overtime due to abrasion and hydraulic action the plunge pool undercuts the hard rock and creates an overhang. The overhang eventually collapses as it is unsupported and the whole process repeats.

24
Q

How are large boulders transported along a riverbed?

A

Traction

25
Q

In which stage of the river does it start to meander?

A

Middle

26
Q

Where does the fastest water flow at a meander? (What feature is found here?)

A

The outside bend, a river cliff

27
Q

How are levees formed? (4 points)

A

River floods repeatedly, overtime it drops the heaviest sediment nearest to the riverbank due to loss of energy from friction. As the flooding continues a natural bank of coarse sediment is formed (embankment) . The finer material as it is lighter travels further onto the flood plain.

28
Q

What are floodplains made up of?

A

Alluvium soil from the nutrient rich sediment that has been deposited by the river.

29
Q

Which of the following features are found in the upper course of a river? (3 of them)

A

Mouth Source Rapids Slower Velocity Estuary Levee

30
Q

How are headlands formed along a coastline?

A

When there is hard rock either side of a band of soft rock the waves erode the softer rock at a faster pace. This means it retreats inwards to form a curved bay. The harder rock either side sticks out into the sea to form headlands.

31
Q

Explain how sand is transported along the coastline.

A

Longshore drift. The prevailing wind brings the wave in, (swash) at a angle, back out at 90 degrees to the beach (backwash) This moves sediment along the coastline in the direction of the prevailing wind.

32
Q

Name four features that can be formed when a headland is eroded. (C, A, S and S)
.

A

Cave, arch, stack and stump

33
Q

How are beaches formed?

A

Deposition, often in sheltered areas e.g. bays. Constructive waves add sediment to the shoreline overtime. Beaches are gently sloping towards the sea and can be made up of sand, shingle or pebbles. The finest material is often found closest to the waterline and the larger material towards the back (deposited in storms)

34
Q

Explain how a spit is formed.

A

Longshore drift carries material along the coastline. When there is a curve or change in direction of the coastline longshore drift continues in the direction of the prevailing wind depositing material into the sea. Over time this builds up to create a finger like projection sticking out into the sea. The end of the spit often curves due to wind and wave action. Behind the spit is very sheltered so more deposition occurs, and a salt marsh is formed