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GCSE AQA Geography Paper 1 Physical Landscapes Revision notes

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A detailed summary of all the key processes named on the AQA specification for all the coastal and river processes as well as case study information for potential 6 markers. Written by a grade 9 student.

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  • May 15, 2024
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Paper 2: UK Physical Landscapes

Lesson 1: Physical Landscape of the UK


The Tees-Exe line divides upland Britain in the N & W from lowland
Britain in the S & E.
Igneous rocks are cooled molten magma.
Sedimentary rocks are eroded material compressed in layers.
Metamorphic rocks are I or S rocks changed by heat or pressure.
Sandstone forms in hot desert climates, whilst coal forms in tropical
swamps.
Igneous rocks form in areas of active volcanoes: they are cooled,
solidified lava.
Igneous and metamorphic rocks are more resistant to erosion and
weathering.
Sedimentary rocks are less resistant to erosion and weathering,
although the degree of resistance varies from rock to rock.




3.1.3.2: Coastal landscapes in the UK
Erosional Processes
Hydraulic action: The pressure of the water being thrown against the cliffs by the wave. It includes the
compression of air in cracks, which can cause the pieces of rock to break off.
Abrasion: Sand and pebbles carried within the waves are thrown against the cliff face with considerable force.
Corrosion: This is a type of chemical reaction between certain rock types and the acids in the seawater.
Attrition: This process involves the wearing away of rocks that are in the sea.


Weathering processes
Chemical weathering is caused by rainwater that contains weak acids that can react with certain rock types.
Biological weathering is the action of plants and animals on the land.

Physical weathering: Caused by temperature and precipitation. Freeze-thaw weathering is when water gets into
cracks in the rocks.
Mass movement processes

Rockfall occurs from steep rocky cliffs when the cliffs are undercut by marine erosion at their base; this is when
material moves down a slope due to the pull of gravity.

Soil creep is the slowest downhill movement of soil. Gravity will pull the water that is contained in the soil
down a slope.

Slumping, also known as rotational slipping, involves a large area of land moving down a slope in a landslide.

, Transportation Processes

Traction: Larger pebbles and cobbles are rolled along the sea bed.
Saltation: Smaller pebbles are moved when one pebble hits another, causing it to bounce. This bouncing can set
up a chain reaction
Suspension: Very fine sediment, sand, silt and clay, is carried as a suspension in the water, making it look
murky or muddy
Solution: Dissolved material from corrosion is carried in a solution, so it cannot be seen.

Longshore drift: Waves approach the coast at an angle because of the direction of the prevailing wind. The
swash will carry the material towards the beach at an angle. The backwash then flows back to the sea, down the
slope of the beach. The process repeats itself along the coast in the zigzag movement.

Sediment Deposition

Deposition happens during the BACKWASH (as the wave travels back down the beach towards the sea). The
largest material is deposited first at the top of the beach and the deposition is then graded by size from this point
towards the sea: graded deposition.

Wave Types and Characteristics



Constructive Destructive

Wave height Low Tall

Wave length Long Short

Wave frequency 6-8 per minute 10-14 per minute

Beach gradient Gentle gradient Steep gradient

Stronger swash/ backwash Stronger swash Stronger backwash

Net movement Onto/ up the beach Off/ down the beach

Breaking point Early on the beach due to Further inland on the beach due to
shallower coastline deeper coastline

Feature formed Berms Storm beach

Season most common Summer Winter

Coastline types:

A concordant coastline has the same type of rock along its length. The alternating bands of soft and hard rock
run parallel to the coastline.
A discordant coastline is where the rock type alternate between the bands of soft and hard rock which are
perpendicular to the coast.

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