Marine Erosion (Edexcel A Level Geography)
Revision Note
Written by: Bridgette Barrett
Reviewed by: Jenna Quinn
Wave Types
The main source of energy at the coast is the waves
Waves are mainly generated by wind
The friction between wind and the water surface which transfers energy from the wind to the water
Wind occurs because of the rotation of the earth and differences in atmospheric pressure when different parcels of air are heated differently by the sun
Various features of the wind will affect how much energy a wave has: fetch, duration and strength of the wind.
Wave height is the distance from the peak to the trough
Wave length is the distance from crest to crest
Wave frequency is the number of waves which pass a specific point over a given time
Types of wave
There are two main types of wave, constructive and destructive
Impact on beach morphology
Beaches are formed from loose material
Waves alter the morphology (form/shape) of the beach
The morphology is also affected by the size and shape of the beach material
The type of wave in an area can vary depending on the time of year or coastal management
Beach profiles are steeper in summer when there are fewer destructive waves and gentler in winter
Storm berms may develop in winter when large destructive waves carry larger sediment further up the beach than normal
In winter beaches may also have a greater variation in pebble size as larger pebbles are deposited by the destructive waves and smaller pebbles are removed
Offshore ridges/bars are formed due to material being eroded from the beach by destructive waves and deposited offshore
Types of Wave and Their Characteristics
Wave Type | Formation | Wave Form | Break Characteristics | Beach |
---|---|---|---|---|
Constructive | Distant weather systems, calm local weather, short fetch | Long wavelength (up to 100m), low, spilling waves, low energy, low wave frequency | Strong swash, weak backwash | Build up the beach with a gentle beach profile |
Destructive | Local storms, strong winds, high fetch | Short wavelength (Approx. 20m), high, plunging waves, high energy, large wave height | Weak swash, strong backwash | Beach is limited. Steeper beach profile is likely in the short term |
Examiner Tips and Tricks
Ensure that you are familiar with the way in which waves are formed and their different characteristics. It is also important that you are able to explain the differences in beach profile throughout the year.
Erosion Processes
Erosion leads to the formation of a range of landforms at the coast
There are four types of erosion
Abrasion (corrasion) - sediment and stones are picked up by the waves and wear away at the cliff/headland
Hydraulic action - this is the shear force of the waves forcing air at high pressure into cracks in the cliff over time this weakens the rock and causes the joint to widen
Corrosion - weak acids in seawater dissolve the rock particles
Attrition - as rocks are moved around by the water they knock into each other gradually becoming smaller and rounder
Factors affecting erosion
The amount of erosion is influenced by a range of factors
Wave type
Wave size
Lithology
Wave type and size affects the seasonal changes in the amount of erosion
Erosion tends to happen more during the winter due to a greater number of destructive waves
The size and type of waves affects the amount of hydraulic action and abrasion
Lithology influences the rate of erosion
Weaknesses in rocks erode more quickly
More resistant rocks erode more slowly
Coastal Landforms
Wave cut platforms
At high-energy coastlines, hydraulic action and abrasion can cause the formation of wave-cut platforms
Powerful destructive waves attack the base of the cliff at high tide
The hydraulic action and abrasion create a wave-cut notch which over time increases in size
This is called undercutting
Eventually, the overhang created by the undercutting collapses due to weathering and gravity
The cliff retreats, leaving a wave cut platform that is exposed at low tide
At a headland, where the rock is hard, erosion is slow and can lead to a variety of landforms
Wave refraction concentrates wave energy onto the headland and can contribute to the formation of caves, arches, stack and stumps
Joints in the headland are susceptible to erosion by hydraulic action
Over time the joints widen forming a cave that is enlarged by hydraulic action and abrasion
Eventually, erosion cuts through the headland forming an arch
The roof of the cave will eventually collapse due to gravity and the lack of support
This leaves a stack that will over time be eroded by weathering, abrasion, and hydraulic action to form a stump
Examiner Tips and Tricks
When describing landform formation it is helpful to write down the formation as a sequence of steps. This will make the process easier to remember when writing about it in the exam.
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