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Wave action and coastal landforms. PART TWO!. Yesterday, we learned about…. Waves friction Wave length , height , crest , trough Wave action: constructive and destructive Swash and backwash Longshore drift Wave refraction. Coastline Erosion. Four types: 1) Corrosion - PowerPoint PPT Presentation
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Wave action and coastal landforms
PART TWO!
Yesterday, we learned about…Waves frictionWave length,
height, crest, trough
Wave action: constructive and destructive
Swash and backwash
Longshore driftWave refraction
Coastline ErosionFour types:
1) Corrosion
2) Corrasion/ Abrasion
3) Attrition
4) Hydraulic action
Corrosion (also sometimes called solution)A type of chemical weathering where
material is dissolved by seawaterThere are weak acids in the sea which wear
rock down (especially some types of rock such as chalk or limestone)
http://www.bbc.co.uk/schools/gcsebitesize/geography/coastal/coastalprocessesrev3.shtml
Corrasion/ AbrasionScouring of the rockSand and rock particles in waves wear
down rock surfaces (usually at the base of a cliff)
Leaves rock very smoothLike sandpaper
http://www.bbc.co.uk/schools/gcsebitesize/geography/coastal/coastalprocessesrev3.shtml
AttritionRock particles in suspension erode each
otherRock hits rock particles break downHitting each other and getting smaller in size
http://www.bbc.co.uk/schools/gcsebitesize/geography/coastal/coastalprocessesrev3.shtml
Hydraulic ActionWhen waves hit the base of a cliff, air is
compressed into cracks. When the wave retreats the air rushes out of the gap cliff material breaks away.
Basically, water and air are compressed into rock fractures water and air in and out of the rock breaks it apart
http://www.bbc.co.uk/schools/gcsebitesize/geography/coastal/coastalprocessesrev3.shtml
Undercutting (52-53)Rock eroded and removed at the base of a
cliff Creates a very steep, vertical cliff
Cliff erosion featuresCavesBaysHeadlandsTunnelsArchesStacksWave-cut platforms
Caves, Bays, HeadlandsCAVES: Indentation in the
weakest rock surface of cliff caused by wave refraction and hydraulic action
BAYS: soft rock wears away faster bay between headlands
HEADLANDS: Hard rock more resistant to erosion erodes into jagged shape that juts out from land
Erosion of cliffs caves bays and headlands caves tunnels arch stack wave-cut
platform
Arch: hole in headland caused by wave refractionStack: isolated rock pillar after arch cavesWave-cut platform: undercutting creates a rock
debris platform in water
http://www.geography.learnontheinternet.co.uk/topics/coasts_erosional_landforms.html#baysandheadlands
Shoreline depositional features
Spits
Tombolos
Spit Long ridge of sand created by longshore
drift
Linear accumulation of sediment attached to land at one end.
Spits are typically elongate, narrow features built to several dozen feet by wind and waves.
Where there is an obstruction or the power of the waves is reduced the material is deposited. The sediment which is deposited usually builds up over the years to form a long ridge of material
TomboloWhen sand spit
grows long enough that it joins an island to the mainland
Types of coasts (54) Ria: lower part of V-shaped valley flooded
with water A drowned river valley that remains open to
the seaFjord: Lower part of U0shaped valley flooded
with waterEstuary: lower part of a river valley filled
with sediment and submerged by the sea depending on the tides; mix of salt and fresh water; funnel shape with gently sloping sides
Coastal Protection1) Sea wall: man-made wall to prevent wave erosion
2) Groynes: artificial barriers built into ocean to stop movement of sand by longshore drift