Coastal Landforms
- Are formed by two processes erosion(27% of coast) and deposition (make 73% of coast)
- Erosion: cliffs, rock platforms, headlands, caves, blowholes, stacks and arches
- Deposition: beaches, spits, dunes, estuaries and lagoons
- Dune blowouts: loose sand blown from dune because vegetation is removed
- Lagoon: formed when sandbar develops, closing estuary
- Estuaries are parts of river that are tidal and occur at sea. They catch mud, sand and nutrients
- Beaches: when material is brought to the shore. Material can be sand, stones or pebbles
- Caves: Formed when waves are refracted (bent towards) a headland and release energy at either side of it.
- Arch: formed when caves erode either side of a headland
- Dunes: Sand is moved to beach in swash. Wind blows sand from beach to fore dune. Grasses bind sand and form a dune. Small plants and shrubs grow to form back dune.
- Cliff: Erosion between low and high tides cut rocks to form a rock platform which then become weak and collapses
- Stack: Further erosion of rock supporting arch will collapse
- Spit: Longshore drift moves sand and other material along a beach and if it occurs in mainly one direction, sand may extend along the coastline
- Blowhole: When caves are exposed by the sea, water rushes in and can cause pressure to build at back of cave. Part of the roof collapses.
- Tombolo: spit joins two land areas
- Headlands: formed when coastal rocks are hard and resist erosion. Softer rocks are eroded and transported elsewhere.
Erosion: Occurs from the wearing away of material by wind, water, etc to form a certain landform
Deposition: Occurs when material is transported by wind, water, etc to form a certain landform.
Transportation: When material is moved from one place to anoter. (i.e by wind, water, etc)