Geography Coasts
Coastal Defences
Hard Engineering
Soft Engineering
Dune regeneration
Groynes
Sea Wall
Rock Armour/Rip-Rap
Gabions
Beach nourishment
Marsh creation
Managed retreat
Hornsea
Wooden ones at Bridlington
Spurn Head
Bridlington
Rock ones at Mappleton
Advantages and disadvantages
Very expensive
Not environmentally friendly
Short term
an eyesore
Advantages and disadvantages
More sustainable
Cheaper
Less of an eyesore
Focus on planning and management
Waves
Weathering and erosion
Mass movement and Transportation
Natural shingle beaches
Land forms of coastal erosion
Cave, Arch, Stack, Stump
Wave cut platform
Deposition
Longshore drift
Landforms caused by deposition
Spit
Bar
Tombolo
Coral Reefs
Destructive waves
Constructive waves
Erodes the beach as has a strong backwash pulling the sand off the beach
Deposits onto beach as has a strong swash pushing the sand up the beach
Hydraulic action
Attrition
Solution
Abrasion
Mechanical weathering
Chemical weathering
Biological weathering
Power and size of waves affected by wind power and fetch
Suspension
Solution
Traction
Saltation
Mass movement is the shifting of rocks and loose materials down a slope
Through the erosion of bays, headlands form. These headlands get eroded from the side in by hydraulic action from the wave which refract around the headland. This creates caves which get eroded all the way through the headland creating an arch. Over time the roof of the arch becomes less stable due erosion causing it to fall creating the stack. The bottom of the stack over time will erode until the stack collapses creating a stump.
CSD
Hazards
They can only be seen at low tide
Starts where destructive waves crash at base of cliff forming a wave cut notch eventually causing the cliff to collapse. The part of the cliff that collapses adding to abrasion.
The process whereby material is moved (transported) along a stretch of coastline. Waves approach the shore at an angle (usually in line with prevailing wind direction) and swash moves material up the beach in this direction. Backwash pulls material strait down the beach at right angle due to gravity. The result is that material is transported in a zig-zag fashion along the beach.
The formation of a spit begins due to a change in the direction of a coastline, or a change in the prevailing wind direction. Where there is a break in the coastline and a slight drop in energy, longshore drift which has been occurring further up the coastline, will deposit material at a faster rate than it can be removed. A ridge (new land) will form out at sea. If the wind direction changes, or the spit begins to form over an estuary, the sand will start to curve forming a hook and recurved laterals. Sand dunes and vegetation can form on the hook. Eventually water will become trapped behind the spit and it will become marshy and muddy, this is known as a salt marsh. If the spit traps water behind it, this is known as a lagoon. If the spit is at right angle to the land, it is known as a divergent spit.
Beaches
Build-up of sediment along a coastline from sediment that has been eroded
Sand dunes
Conditions needed for formation
An obstacle
Strong onshore prevailing winds
A wide expanse of sand that is not covered in low tide.
Formation
An obstacle like a shrub disrupts the onshore wind flow reducing its speed and energy due to the friction of it rubbing the obstacle, causing the wind to deposit grains of sand.
A small dune forms behind the shelter of the obstacle. This is called an embryo dune.
The embryo dune grows larger to about 1-meter tall classifying it as a yellow dune or fore dune.
Plant life like marram grass colonises the top of the dune as sand hold water and nutrients.
The dune grows to about 10m and the grass dies to form a layer of hummus giving the sand more nutrients. This is called a Semi-fixed dune.
The dune grows even taller and the sand starts to turn to rich and moist soil. This allows much larger vegetation and some climax trees to grow. This is called a fixed dune or grey dune.
Conditions for coral reefs to form
Sunlight - Needed for the algae, which is in symbiosis with the polyps, to photosynthesise.
Shallow water - Water not exceeding 25 meters are needed
Clean, clear water - They grow faster in clear water as sunlight is allowed to penetrate more easily
High Salinity - A salinity range of 32–40% is needed
Mangrove swamps
Mangroves are shrubs or small trees that grow in costal environments. They are a tropical vegetation, commonly found in the intertidal zone; the area that is above water at low tide and below water at high tide. They are the only trees that are capable of thriving in saltwater and have adapted to living in these conditions in a number of ways.
Erosion rates from 3 feet per year to 30 feet per year
Holbeck hall hotel, Scarborough collapsed in 1993
Oppertunities
Holderness is the Europes fastest eroding coastline
House near edge of cliff sold for £1
Tourism – Bridlington and spurn head as is an SSSI
Gas terminal – 3,000 jobs
Headlands and bays
Cliffs
Tropical Stroms
Start over water in low pressure zones. Water needs to be 26oC or higher. Heat and humidity rise from the ocean. Converging winds force air to rise. The Earth’s rotation causes the storm to spin. Northern hemisphere storm spins anticlockwise, Southern hemisphere storm spins clockwise. Wind at 74mph is a tropical storm like a cyclone, hurricane or typhoon. Tropical storms dissipate when over cold water or land.