Coasts Flashcards
Littoral zone
The wider coastal zone including adjacent land areas and shallow parts of the sea just offshore
Primary coasts
Dominated by land based processes such as deposition from rivers or new land from lava flows
Secondary coasts
Dominated by marine erosion or deposition processes from the sea
Emergent coasts
Where the coasts are rising relative to sea level eg due to tectonic uplift
Submergent coasts
Where coasts are being flooded by the sea either due to rising sea levels or subsiding land
Low energy coastlines
Sheltered coasts with limited fetch and low wind speeds resulting in small waves
High energy coastlines
Exposed coasts facing prevailing winds with long wave fetches resulting in powerful waves
Cliff profile
The height and angle of a cliff face as well as it’s features such as wave cut notches or changes in slope angle
Dynamic equilibrium
The balanced state of a system when inputs and outputs balance over time
Short term factors showing the littoral zone is constantly changing
Individual waves
Daily tides
Seasonal storms
Long term factors showing the littoral zone is constantly changing
Changes to sea level
Climate change
3 features of a marine erosion dominated cliff
Steep face
Active undercutting
Limited cliff base debris
3 features of a sub-aerial process dominated cliff
Curved slope profile
Lower angle face
Accumulated debris
Faults
Major fractures that have moved rocks from their original positions
Formed when the pressure to which a rock is subjected exceeds its internal strength causing it to fracture
Deformation
Folds and dips caused by tectonic activity
Strata
Different layers with bedding planes
Joints
Fractures caused either by contraction as sediments dry out or by earth movements during uplift
Concordant coastline
Rock strata run parallel to the coastline
Discordant coastline
Different rock strata run at right angles to the coastline
Bands of more and less resistant rock
Headlands and bays
Deposition
The laying down of sediment carried by wind or water
Coastal erosion
The process in which cliffs are worn away and transported by the sea
Traction
Large materials such as boulders are rolled along the sea bed
As they are heavy so waves don’t have enough energy to carry them
Saltation
Pebbles or small stones are lifted by the sea but dropped when energy is lost.
As a result pebbles are bounced along sea bed
Suspension
Smaller particles such as sand float in the sea
Solution
Particles such as clay are dissolved in the sea and constantly move with water
Abrasion
Material is hurled against the cliff by waves wearing away at it
Attrition
A pieces of material knock each other they get smaller smoother and more rounded
Hydraulic action
Where waves crash into base of cliff forcing air into cracks. This exerts a pressure, cracks grow until rock detatches
Solution (erosion)
Soluble particles dissolved by acids in sea water
Lithology
The characteristics of the rock including the type, whether it’s permeable or impermeable, how porous it is
Isle of Purbeck, Jurassic coast
Resistant Portland limestone lies parallel to the coast
At points where this limestone is weaker erosion causes small coves eg Lulworth cove
Igneous rock erosion rate
Very slow
Interlocking crystals make rock strong and resistant
Few joints and therefore limited areas of weakness to exploit
Metamorphic rock erosion rate
slow
Crystallised sedimentary rock
Some folds and fractures to exploit
Sedimentary erosion rate
Moderate to fast
If cement between layers is weak then it will be weak
Younger rocks are weaker
Permeability (lithology)
The ability of water to pass through the rock.
Related to its previousness and porosity.
Pervious rocks
Eg limestone
Joints and bedding planes that water can flow through
How can groundwater flow weaken rocks
Flows through rocks layers removing binding cement
Carbonation
Acidic rainwater slowly dissolved the calcium carbonate in the limestone or chalk creating calcium bicarbonate which is taken away in solution
Hydrolysis
Water combines with minerals like granite and the chemical reaction creates salts and clay
Eg in Devon it has created Kaolin (porcelain china clay)
Freeze thaw
Water goes into cracks and freezes
This expands and breaks the rock
Horizontal bedding plane
1)Erosional processes
2)Main mass movement type
Undercutting by wave action can lead to development of wave cut notches and platforms
Main mass movement=rock fall
Sloping bedding plane (towards sea)
1)Weathering
2)Sub aerial processes
Large slabs of rock loosened by weathering slide off easily along bedding planes.
Sub aerial processes have a greater influence than marine processes leading to shelling cliffs
Sloping bedding plane (away from sea)
Rocks loosened by weathering and wave action are difficult to dislodge
Slope profile lowered by mass movement and weathering
Cliff face is rugged and uneven
Marram grass
Helps stabilise the unconsolidated sediment of the dunes and encourages other plants to grow there as well so helping plant succession