2.Coastal Erosion & Deposition Flashcards
Constructive Waves
- happen at low frequency
- long and low
- overtime form gently sloping beaches
- constructive waves deposit material on coasts as backwash less powerful that swash
Destructive Waves
- responsible for erosional processes
- high frequency (10-15 per min)
- circular motion so waves break at a greater height
- destructive waves remove material from coasts as swash less powerful than backwash
Abrasion
Where pieces of rock are picked up by waves and hit against the bead, beach or cliffs which wears them away over time
Attrition
Where pieces of bedload are hit against one another causing them to break apart and become smaller and more rounded
Corrosion
When there is a chemical reaction between the seawater and susceptible rocks like limestone
Hydraulic Power
- causes the breakdown of cliffs due to the force of water being compressed into cracks of rock
- repeated action of the water forced in and out of the cracks in the rock leads to surrounding cliff
Spits
- when coast changes direction at and estuary, longshore drift continues to move sediment across the inlet
- the rives doesn’t let spit completely join to the coast on the other side as river has energy to move sediment
- spits are long fingers of sand sticking out from one side in a coastline that have been curved by secondary winds
Bars
- bar is formed when a spit grows across a bay
- lagoons often form behind bars
Beaches
- made by constructive waves moving and depositing sand or shingle inland
- more gently sloping beach tends to be formed from sand than steeper pebbles beaches
Tombolos
If a spit stretches across the mainland and joins an offshore island, this causes a Tombolo to form
Cuspate Forelands
- form when sediment is deposited across a bay caused by longshore drift transporting sediment in two directions
- leads to formation of two spits which eventually meet, resulting in trapping of sediment until eventually new land is formed
Sediment Cell Concept
- describes a closed system operated by sources, transfers and sinks driven by erosion, transportation and deposition processes
- the uk has 11 key sediment cells and sub-cells, each with its own shoreline management plan
Mechanical Weathering
- when rocks are broken down without their chemical composition being changes
- salt weathering is the main type of mechanical weathering affecting coasts
Biological Weathering
- when rocks are broken down by living things
- the activity of animals near the coast is also an example of biological weathering
Chemical Weathering
- when rocks are broken down because of their chemical composition being changed
- carbon weathering is a a type of chemical weathering that takes place when it’s warm and wet