2b - coastal landscapes & change Flashcards
COASTAL LANDSCAPES - describe what is meant by the ‘littoral zone’
- a series of sub-zones to represent the features of the wider coastline from sea to land
what does the littoral zone include?
- includes 4 key sub-zones : offshore, nearshore, foreshore and backshore
when does the littoral zone reach dynamic equilibrium?
- when there is a balance between inputs and outputs
state the inputs and outputs of the littoral zone
- 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
what are high energy coasts characterised by?
- destructive waves
- long fetches
- high rates of erosion
- caves
- arches
- stacks & stumps
- cliffs & wave-cut platforms
what are low energy coastlines characterised by?
- constructive waves
- shorter fetches
- higher rates of deposition
- spits & bars
- beaches
- sand dunes & salt marshes
GEOLOGICAL STRUCTURE - describe concordant coastlines
- have alternating bands of hard and soft rock parallel to the coast
describe discordant coastlines
- 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
how is Dorset an example of a discordant coast?
- 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
COASTAL MORPHOLOGY - how are Dalmation coasts formed?
- 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
what landforms form at Atlantic coasts?
- 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
how are headland features formed?
—> 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.
GEOLOGICAL STRUCTURE - what causes the geological structure of rocks?
- 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
why are rocks like sedimentary more susceptible to erosion and weathering?
- 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
define the term ‘dip’
- the angle of the rock layer which forms the horizontal bedding plane
- rocks can dip either towards the land or towards the sea