Case studies for coasts

Changing Landscapes - coasts

·        Sediment cell – South Downs sediment cell

o    Sub-cell 4d along the Sussex coast

o    Between Selsey Bill and Beachy Head

o    Defended with rock reefs, wooden and rock groynes

o    Pebble beeches

o    Dominant drift direction west to east

o    Up to 5000m³ gravel and sand lost round Beachy Head

o    Dredging of Shoreham Harbour, Brighton Marina, Newhaven Harbour

·        Build-up and removal of a beach (system feedback) – Crantock Beach, Cornwall

o    Northwest facing beach in Northern Cornwall

o    River Gannel flows on the northern edge of the beach

o    Ever-changing environment

o    Employs a shoreline management plan

o    Has experienced excessive erosion in recent years (since 2013), especially after the 2013-2014 storms

o    Erosion of up to 3m in depth

o    Mobile zone is degrading, whilst the beach zone is more stable

·        Coast working as a system – Aquitaine Coast

o    Located in the southwest of France

o    Complete shore system composed of beach, dunes and pine tree forest

o    Sandy beaches and dunes

o    Employing hold the line/limited intervention

o    Sea wall, groynes, beach nourishment, dune restoration

o    Stores of the cap ferret spit, arachon estuary, dune du pilat and araguin offshore bar

o    Outputs of the ocean and longshore drift

·        Microtidal range – Eastern Australia

o    Found in parts of New South Wales and Queensland

o    Wave action plays a larger role in Charing the coast than tidal energy

o    Example is Yalimbah Creek

·        Macrotidal range – most of the UK coast

o    Key regions include Bristol Channel and Severn Estuary (up to 15m)

o    Strong tidal currents and dynamic sediment movement

o    Other examples include Humber and Mersey estuaries

o    Drive rapid sediment transport, leading to extensive tidal flats, formation of tidal deltas, and notable erosion/deposition patterns

·        1.1.3 High and low energy environment – Gower Peninsula

o    Mixed energy coastal environment with high and low energy areas

o    High energy areas- Rhossili bay- experiences strong winds and waves, making it popular for surfing

o    Low energy area- Oxwich bay- large, sheltered bay with extensive dunes and salt marshes

·        1.1.5 Headland and Bay – Swanage Bay and Studland Point, Dorset

o    When bands of softer rock on a discordant coastline is eroded faster than the bands of harder rocks, creating areas of lad that stick out form the mainland

o    Has alternating bands of limestone/chalk and clays/sands

o    Ballard point- made of chalk

o    Durlston head- made of limestone

o    Located in Dorset

·        Stacks and stumps – Old Harry and Old Harry’s wife, Dorset

o    The erosion of a cave into an arch, that then collapses to form a stack

o    The stack then gets eroded into a stump

o    Old harry is a stack and his wife is a stump, near Ballard point

o    Made of chalk, which is resistant enough for a cave-arch-stack sequence

·        Cove – Lulworth Cove

o    On the Dorset coast, next to the village of Lulworth

o    Bedrock surrounding the cove is sedimentary, and so was easily erodes

o    Entrance is a breach in the very resistant Portland stone

·        Blowhole – Nakalele Point, Hawaii

o    Northernmost point on the island of Maui

o    Water released by the blowhole can reach up to 100 feet in the air

o    Rock in the area is jet black lava rock

·        Soft rock cliff – Highcliff, Barton-on-Sea (boulder clay rock)

·        Hard rock cliff – Cornish Coastline (basalt rock)

·        1.1.6. Bar – Chesil Beach

o    Spits that extend across two sides of a headland, forming a lagoon behind it

o    Located in Dorset

o    Behind the spit there is The Fleet, which is a lagoon

·        Cuspate foreland – Dungeness foreland, Kent

o    Triangular shaped projections that form from longshore drift moving in two different directions

o    Located in Kent

o    Formed over the last 5000 years

o    Comprised largely of gravel

o    Attracts 1 million tourists annually

·        Spit – Orford Ness

o    Linear deposits of sand and shingle that is attached to land on one end

o    Formed by longshore drift

o    Creates sheltered areas behind that often allows the formation of a salt marsh

o    Largest vegetated shingle spit in Europe

o    Stretches for about 10 miles

o    Located on the Suffolk coast

·        Tombolo – Chesil Beach

o    Longshore drift forming a spit that connects an island to the mainland

o    Connects the isle of Portland to Abbotsbury

o    Largest tombolo in the United Kingdom

·        1.1.7. Sand dunes – Ainsdale Dunes, Sefton

o    On the northwest coast of England

o    Contains a range of habitats

o    Largest dune area in England

·        Mudflat/ salt marsh – Morecambe Bay

o    Northwest coast of England

o    310km^2 of intertidal sand flats

o    Salt marshes develop along the bays margins

o    Makes Morecambe bay a crucial habitat for wildlife

·        Coral reef – Great Barrier Reef

o    Located north-east of Australia

o    Mad up of 2900 individual reefs and 900 islands

o    Threatened by human activity which causes bleaching of coral (global warming)

·        1.1.8. High energy event – December 2013 storm (UK East coast)

o    Gale-force winds of up to 100mph

o    Sea levels peaked at 5.8km and 4.7m in Hull and Dover respectively

·        Rias – Kingsbridge Estuary, Devon

o    A river valley at the coast that has been inundated by the sea as relative sea level rises, resulting in a “drowned valley”

o    Formed on a submergent coastline

o    Has very little freshwater input, high salinity levels and a large tidal range

o    Supports diverse intertidal habitats (mudflats and salt marshes

o    Has steep banks and a relatively deep channel compared to its width

·        Fjord – Sognefjorden, Norway

o    A glaciated valley at the coast that has been inundated by the sea. Has steeper rising walls, a straighter long profile and is deeper than a ria due to glaciers over-deepening the valley

o    Formed on a submergent coastline

o    Located in western Norway

o    205km long, and up to 4,5km wide

·        Raised beach – Isle of Arran, Kings Cave

o    Raised beaches are shore platforms and beaches that are found stranded above the present-day high tide level

o    Formed on an emergent coastline

o    Located in Scotland

o    Kings cave is a notable area which provides evidence of the past sea levels

o    Flat shore platform elevated above the current coastline

·        1.1.9 [Case study] Management of coastal processes – Holderness

o    Located in East Yorkshires coastline

o    Composed predominantly of soft erodible boulder clay

o    Notoriously one of Europe’s fastest eroding cliffs (over 2m/year)

o    Use of sea walls, groynes and revetments

o    Use of managed retreat in certain areas

o    Integrated coastal zone management

o    Decision making involves tradeoffs between protecting property and allowing natural coastal change

·        1.1.10 [Case study] Management of human activity – Ainsdale sand dunes

o    Designated as a national nature reserve and site of special scientific interest (SSSI)

o    Threats from trampling by visitors, off road vehicles and cycling, urban development (encroaching)

o    Managed by fencing and boardwalks, sand dune stabilisation and education and signage