Geography ✿ Distinctive landscapes

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37 Terms

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Landscape

an area of land with both physical features and human features

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Where are upland areas usually found?

north and west of the UK

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Where are lowland areas usually found?

south and west of the UK

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Where are glaciated areas usually found?

north-west of the UK

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state 4 characteristics of upland areas

  • formed of harder rocks (slate, granite, limestone)

  • climate is usually cool and wet

  • thin soils due to harsh climate

  • land used for farming and tourism

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state 4 characteristics of lowland areas

  • formed of softer rocks (chalk, clay, sandstone)

  • climate is usually warmer and drier

  • fertile soils

  • land used for industries and farming

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state 2 characteristics of glaciated areas

  • ice causes erosion of the landscape causing valleys

  • ice also melts which deposits material

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weathering

break down or dissolving of rocks

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erosion

transportation of rocks or minerals

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biological weathering

the breakdown of rock caused by the movement of animals and plants

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chemical weathering

the breakdown of rock by changing it’s chemical composition

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mechanical weathering

process of physical changes such as wind, temperature and waves which breakdown rock

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3 upper course landforms

  • v shaped valley

  • waterfalls

  • gorges

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3 middle course landforms

  • wide valleys

  • meanders

  • ox-bow lakes

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3 lower course landforms

  • ox-bow lakes

  • flood plains

  • levees

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flood plain

flat land next to a river, material is deposited here when river is flooded

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hard engineering

using artificial structures to control nature

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soft engineering

working with natural coastal processes

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<p><span>solution (erosion)</span></p>

solution (erosion)

dissolved carbon dioxide making waters acidic, the acid reacts with rocks

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<p>abrasion</p>

abrasion

when rocks scrape against the seabed, removing small pieces

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<p>attrition </p>

attrition

rocks smashing into each other, breaking them into smaller fragments

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<p>hydraulic action</p>

hydraulic action

the force of water crashing into headlands/ river banks

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<p><span>how are </span><strong><u>caves</u></strong><span> formed?</span></p>

how are caves formed?

  • waves crash into the headlands, forming cracks by hydraulic action

  • repeated erosion causes the cracks to open, forming a cave

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<p>how are <strong><u>arcs</u></strong> formed?</p>

how are arcs formed?

a cave becomes larger and eventually breaks through the headland

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<p>how are <strong><u>stacks</u></strong> formed?</p>

how are stacks formed?

the base of an arch becomes wider through further erosion, the roof becomes too heavy and collapses

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<p>how are <strong>spits</strong> formed?</p>

how are spits formed?

  • sediment is carried by longshore drift

  • a change in wind direction occurs and forms a hooked end

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<p>How are <strong>v shaped valleys</strong> formed?</p>

How are v shaped valleys formed?

  • a river that flows through a mountain, its land is eroded vertically

  • overtime this deepens the river bed, creating deep v shape valley

  • mass movement and weathering on valley sides cause lose material to fall which the river transports down stream, deepening its shape

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how is a river levee formed?

  • a river is flooded and spreads out on the floodplain

  • as water overflows, heavy sediment is deposited closest to banks

  • this repeats overtime which creates build up of sediment, creating raised embankments

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how are headlands and bays formed?

  • erosion occurs at more harder rocks which erodes slower than the softer rock

  • as the soft rock is eroded away quicker it creates a bay leaving the harder rock sticking out into the sea as headlands

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describe the 2 types of waves

  • constructive → low frequency waves

  • destructive

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deposition

when material is being carried by the water (in rivers or seas) and dropped off

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describe the 2 types of mass movement

  • slumps → material shifts with a rotation

  • slides → material shifts in a line

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mass movement

the shifting of rocks and loose material down a slope

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traction

rocks are pushed along the river seabed by force of the water

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saltation

rocks being bounced along the seabed

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suspension

rocks like silt and clay are carried along by water

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solution (transportation)

soluble material dissolved in the water are carried along