Costal systems and landscapes. Flashcards
Heysham and Morecambe- four defence options:
Hold the line- retain the existing coastline by maintaining current defences or building new ones where existing structures no longer provide sufficient protection.
Do nothing but monitor- on some stretches of coastline, it is not technically economically or environmentally viable to undertake defence works.
Retreat the line- actively manage the rate and process of the coast retreats.
Advance the line- build new defences seaward of the existing line.
Heysham and Morecambe- Background.
Current defences along the 8.5km stretch of coastline are the results of an improvement scheme of existing structures during a multi-phase programme between 1989-2018- costing £30m.
The mix of traditional hard engineering with more contemporary methods to improve the potential for sustainable management.
Heysham and Morecambe- Strategy 1.
Rock armour/rip rap to enhance and protect the existing sea wall.
Boulders of locally sourced limestone are placed along the existing promenade and sea walls from the west to 1km east of the town centre.
Heysham and Morecambe- Strategy 2.
Breakwaters or rock groynes.
Around ten breakwaters and rock groynes were built at intervals in front of the town.
Heysham and Morecambe- Strategy 3.
Repaired and replaced sea walls.
The traditional sea wall was repaired and reinforced. Cost £11m and protects 11,400 homes and 2,246 commercial properties.
Design to last 100 years.
Holderness- Case study:
- How long is the coastline?
61km long- Flamborough head to Spurn Head.
Holderness- Case study:
- What are the cliffs made of and what type of wave are there?
-Boulder clay ‘till’.
-Destructive waves.
Holderness- Case study:
-Coastal process operating in the area.
-Erosion: soft boulder is easily eroded, Great Cowden 10m/year.
-Mass Movement: boulder clay is prone to slumping when wet.
-Transportation: prevailing winds transport material southwards. Winds also create an ocean current that transports material south by longshore drift.
-Deposition: where ocean current meets the outflow of the Humber River, the flow becomes turbulent and sediment is deposited.
Holderness- Case study:
-Headland and wave-cut platforms.
To the north the boulder clay overlies chalk. Chalk is harder and less easily eroded so it forms a headland and wave-cut platforms. Flamborough head has features such as stacks, caves and arches.
Holderness- Case study:
-Slumping cliffs.
Frequent slumps give the boulder clay cliffs a distinctive shape. In some locations several slumps have occurred and have not yet been eroded, making the cliff tiered.
Holderness- Case study:
Beaches.
The area to the south of Flamborough Head is sheltered from wind and waves, and a wide sand and pebble beach has formed.
Holderness- Case study:
Sand dunes.
Around Spurn Head, material transported by the wind is deposited, forming dunes.
Holderness- Case study:
Spit.
Erosion and longshore drift have created a spit with a recurved end across the mouth of the Humber Estuary- this is called Spurn Head. On the landward side of the spit, estuarine mudflats and saltmarshes have formed.
Holderness- Case study:
How much has the coastline retreated i the past 2K years?
How many villages have been lost?
4km
30 villages.
Holderness- Case study:
Social, economic and environmental problems.
-Loss of settlements and livelihoods-farmland.
-Loss of infrastructure- gas terminal at Easington only 25m from the cliff edge.
-Loss sites of Special Scientific Interest (SSSIs)- the lagoons near Easington,