2b - coastal landscapes & change Flashcards

1
Q

COASTAL LANDSCAPES - describe what is meant by the ‘littoral zone’

A
  • a series of sub-zones to represent the features of the wider coastline from sea to land
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2
Q

what does the littoral zone include?

A
  • includes 4 key sub-zones : offshore, nearshore, foreshore and backshore
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3
Q

when does the littoral zone reach dynamic equilibrium?

A
  • when there is a balance between inputs and outputs
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4
Q

state the inputs and outputs of the littoral zone

A
  • sediment is the key input AND output of the system and is determined by :
    —> INPUTS - the action of waves, currents and wind
    —> OUTPUTS - washed into the sea by erosion
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5
Q

what are high energy coasts characterised by?

A
  • destructive waves
  • long fetches
  • high rates of erosion
  • caves
  • arches
  • stacks & stumps
  • cliffs & wave-cut platforms
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6
Q

what are low energy coastlines characterised by?

A
  • constructive waves
  • shorter fetches
  • higher rates of deposition
  • spits & bars
  • beaches
  • sand dunes & salt marshes
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7
Q

GEOLOGICAL STRUCTURE - describe concordant coastlines

A
  • have alternating bands of hard and soft rock parallel to the coast
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8
Q

describe discordant coastlines

A
  • have alternating bands of hard and soft rock at right angles to the coast
    —> erosional landforms are more common on discordant coastlines because erosion happens at different rates along their length
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9
Q

how is Dorset an example of a discordant coast?

A
  • in Dorset, the coastline consists of Portland limestone and Greensands
  • the Greensands is less resistant to erosional processes, and so retreats at a faster rate than the Portland limestone
  • this has resulted in the creation of a bay and headlands
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10
Q

COASTAL MORPHOLOGY - how are Dalmation coasts formed?

A
  • concordant coastlines, also referred to as Pacific coasts, lead to the formation of Dalmation coasts
  • Dalmation coasts are made up of offshore islands and coastal inlets running parallel to the coastline
    —> EXAMPLE : Lulworth Cove, located on the south-west Dorset coastline.
    —> here, the more resistant rock (eg limestone) acts as a barrier to protect the less resistant rock
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11
Q

what landforms form at Atlantic coasts?

A
  • headlands and bays often form on discordant coastlines (also referred to as Atlantic coasts)
  • as the faster eroding, less resistant rock retreats (eg the clays at Swanage Bay), this leaves behind the more resistant rock as headlands
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12
Q

how are headland features formed?

A

—> on discordant coastlines, the retreating, less resistant rock and the exposed resistant rocks cause a change in the shape of the coastline. This leads to WAVE REFRACTION.
—> this change in the way in which waves approach the coastline can cause an increase in the rate of erosion on the headlands
—> this leads to the formation of headland features like caves, arches, stacks and stumps.

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13
Q

GEOLOGICAL STRUCTURE - what causes the geological structure of rocks?

A
  • the geological structure of rocks (the formation of joints, the angle of the dip, faulting and folding) is caused by the deformation and stress placed on them from tectonic processes
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14
Q

why are rocks like sedimentary more susceptible to erosion and weathering?

A
  • these are rocks with the presence of more joints and faults
  • this is because these processes exert forces on the weaknesses found in the layers of the rocks
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15
Q

define the term ‘dip’

A
  • the angle of the rock layer which forms the horizontal bedding plane
  • rocks can dip either towards the land or towards the sea
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16
Q

how is a gentler cliff profile created?

A
  • bedding planes that dip towards the sea create these
  • BUT these cliffs are vulnerable to mass movement processes, like rockfalls
17
Q

how is a steeper cliff profile created?

A
  • bedding planes that dip towards the land tend to create these
  • BUT, these cliffs are more vulnerable to erosion processes, like hydraulic action and abrasion
18
Q

BEDROCK LITHOLOGY - what does this refer to?

A
  • the physical properties of different rocks
  • the existence of sedimentary, igneous and metamorphic rocks affects the rate of recession along a coastline
19
Q

how are igneous rocks formed?

A
  • igneous rocks, such as basalt and granite, form from the crystallisation of magma.
  • they are more resistant to erosion and weathering
20
Q

why are igneous rocks more resistant to erosion and weathering?

A
  • igneous rocks contain crystals which increase the strength of the rocks and reduce the number of lines of weaknesses that would be exploited by physical processes
21
Q

state the difference between intrusive and extrusive igneous rock

A
  • intrusive igneous rock is formed from magma inside the Earth, whereas extrusive igneous rock is formed when magma escapes through vents on the Earth’s surface
  • the average rate of erosion of igneous rock is 0.1-0.5cm per year
22
Q

how are sedimentary rocks formed?

A
  • sedimentary rocks, such as limestone and sandstone, form from the build up, compacting and hardening of sediments into layers over time by lithification
23
Q

why are limestone and chalk more susceptible to erosion and weathering?

A
  • sedimentary rocks that have been formed in a shorter geological time scale tend to be more susceptible and erode at a faster rate compared with those formed over a longer geological time
    —> the average rate of erosion of sedimentary rocks is 2-6cm per year
24
Q

how is metamorphic rock formed?

A
  • metamorphic rocks, such as slate and marble, are formed from the change in the structure of sedimentary and igneous rocks, caused by variations in heat and pressure
  • the process of change is referred to as the rocks having been metamorphosed.
25
Q

how is marble an example of metamorphic rock?

A
  • marble is an example of a metamorphic rock that has been formed from the changing structure of limestone caused by the re-crystallisation of calcite
  • METAMORPHIC ROCKS ARE RESISTANT TO EROSION