Coastal systems and processes Flashcards
Main source of energy at a coast
Waves
Three factors affecting how much energy a wave has
Fetch, strength and duration.
Fetch
The distance of open water the wind blows over.
Strength
How forceful the wind is, determined by the pressure difference.
Duration
How long the wind has been blowing.
Tide and Tidal range
Tide is the changes in the level of water due to gravitational pull of the moon.
Tidal range = difference in height between high and low tide.
Constructive waves
Short fetch, long wavelength, low waves, strong swash, weak backwash.
Destructive waves
High fetch, short wavelength, high waves, weak swash and strong backwash,
Wave refraction
Changes the amount of energy reaching the shore on a small local scale.
Sediment budget
The balance between the inputs and outputs of sediment in the system, should be in dynamic equilibrium, natural changes like climate change can disturb this however.
Weathering
The breakdown of rock in its place of origin. (in-situ)
Three main types of weathering.
Physical/mechanical weathering, chemical weathering and biological weathering.
Mechanical/physical weathering
When rocks break up with no chemical changes
Freeze-thaw weathering (physical/mechanical)
Salt crystallisation (mechanical/physical weathering)
Biological weathering
Three methods of chemical weathering
Carbonation, Oxidation and solution
(ChemW) Carbonation
When rain is slightly acidic and reacts with carbonate rocks like limestone, causing them to dissolve.
(ChemW) Oxidation
When iron minerals in the rock react with oxygen in the air to cause rusting and breakdown the rock.
(ChemW) Solution
When other salt minerals in the rock are dissolved.
Mass movement
The downhill movement of material under the influence of gravity.
Including landslides, slumping and rockfalls.
Hydraulic action
Erosional processes that occur due to the power of the waves, with no involvement of the rocks at all.
Abrasion
Occurs when breaking waves that are carrying sediment scrape against the rock surface.
Also known as corrasion.
Dependant on how much sediment is available in the particular coastal system
Attrition
When the size of sediment particles change as sediment held in the waves rub together.
Solution/corrosion
Acids in the seawater wear away the rock.
Marine transportation
Material in the water is moved in 4 ways:
Traction, Saltation, Suspension, Solution.
(MarTrans) Traction
Traction is when pebbles and larger material is rolled along the sea bed.
(MarTrans) Saltation
Saltation is when small pieces of shingle or large sand grains are bounced along the seabed.
(MarTrans) Suspension
Suspension along the coast is when small material such as clay or silt are held in the flow of the seawater.
(MarTrans) Solution
Weak carbonic acid in seawater dissolves minerals in rocks which are then carried in solution.
Longshore drift
Main process of deposition and transportation along the coast.
Influenced by the prevailing wind, waves approach the beach at an angle.