Tombolo example
Chesil beach
St ninians island
Bar example
Slapton ley
Devon
Spit example
Humber estuary
Haloseres
Ecological succession that develops in a highly saline environment
On mud flats
Needs low energy and constant supply of mud
Roots stabilise with salt tolerant plants
Land rise and vegetation wit grow
Sand dunes types from foreshore to backshore
Embryo
Fore
Yellow
Grey
Ridges
Dune slack
Blowout
Embryo dune
Metre high
80% sand exposed
Fore and yellow dunes
5m high
20% sand exposed
grey dunes and dune ridges
8-10m high
Less than 10% exposed sand
How are sand dunes formed
Deposits of sand in inter tidal zone
Dries
Blown by wind and move by saltation up beach
Trapped by debris
If not eroded then builds and is colonised by plants
Positive feedback as continues to grow
Roots make it stable
Berms
Spring tides form a storm ridge so following tides can’t reach features further back remain untouched
Berms are smaller ridges formed beneath rudge marking successive high tides following the spring tide into the near tide
Example on Hornsea beach
Ridges and runnels
Form parallel to the shoreline in the foreshore zone
Ridges are areas of the foreshore that are raised above the adjacent shore which dips into a runnel
Runnels are disrupted by channels that help to drain water down the beach
Cusps
Crescent shaped indentations that form on beaches which have mix of sand and shingle
Formed where there is a junction between the two
Swash concentrated in small bay that forms in the centre of the cusp
Stronger backwash that removes sediment
Offshore bars
Elongated ridges and mounds of sand or gravel deposited beyond a shoreline by currents and waves
Both submerged bars and emergent islands separated from the shore which are exposed at different times
Submerged bars constructed by …
Constructed by longshore, tidal and fluvial currents in shallow water coastal environments
Can migrate
Steep shore facing slopes of berms