The Coastal Zone Flashcards
How is sediment moved at the coast? Give a small definition for each transportation method.
Traction: when pebbles and larger sediment is rolled along the sea bed
Saltation: load is bounced along the seabed
Suspension: small particles are carried in water
Solution: minerals are dissolved and carried in solution
How is the coast eroded? Give an explanation for each type
Solution: acids contained in the sea water dissolve rock such as chalk and limestone
Attrition: waves smash rocks and pebbles on the shore into each other, they break and become smoother
Abrasion: bits of rock and sand in waves grind down cliff and surfaces
Hydraulic action: air may become trapped in joints and crack of a cliff which then freezes breaking the cliff by freeze-thaw
Describe the qualities of a destructive wave.
High wave
Breaks in a downward movement onto the shore
Weak swash
Strong backwash
Occurs when wave energy is high or there is a storm
Describe the qualities of a constructive wave.
Low wave Strong wash Weak backwash They break on the shore and deposit material Created in calm weather
Give some examples of depositional landforms.
Beaches
Spits
Tombolos
What are beaches and how are they formed?
Beaches are mad up of eroded material that has been transported from elsewhere and deposited by the sea.
What are spits and how are they formed?
A spit is an extended stretch of beach material and is joined to mainland at one end.
Longshore drift moves material along the coastline
A spit forms when the material is deposited
Overtime the spit grows and develops a hook if the wind direction changes further out
Waves can’t get past a spit, which create a sheltered are where silt is deposited and mud last or salt marshes form
What are Tombolos and how are they formed?
A Tombolo is a spit connecting an island to the mainland, they are formed the same way spits are.
Give an example of a tombolo
Chenille beach connects the isle of Portland to the mainland Dorset coast.
It stretches for 18 miles.
Lagoons have formed behind the stretch of beach.
List some erosion landforms
Caves, arches, stacks and stumps
Headlands and bays
Cliffs
How are caves, arches, stack and stumps formed?
Caves occur when waves force their way into cracks in the cliff face. The water contains sand and other ,are rials that grind way at the rock until the cracks become a cave. Hydraulic action is the predominant process.
If the cafe is formed in a headland, it may eventually break through the other side forming an arch.
The arch will gradually become bigger until it can no longer support the top of the arch. When the arch collapses, it leaves the headland on one side and a stack on the other.
The stack will be attacked at the base which weakens the structure.
Eventually it will collapse to form a stump.
How are headlands and bays formed?
They are formed when the sea arak a a section of coast with alternating bands of hard and soft rock.
The sea will erode the soft rock quicker, which creates a bay and the hard rock will stick out crating a headland.
How are cliffs eroded?
Weather weakens the top of the cliff.
The sea attacks the base of the cliff forming a wave-cut notch
The notch increases in size causing the cliff to collapse.
The backwash carries the rubble towards the sea forming a wave-cut platform
The process repeats and the cliff continues to retreat.
List some examples of hard engineering solutions.
Sea walls
Groynes
Rock armour
List some advantages and disadvantages of building a sea wall
Advantages: protects the base of cliffs, land and buildings against erosion. Can also prevent coastal flooding in some areas.
Disadvantages: expensive to build (can be up to £6 million per kilometre to construct), reflects wave energy back to sea so they remain powerful, overtime they will begin to erode so cost of maintenance is high.