Coasts, 10 Flashcards
(36 cards)
Destructive waves
- they are created in storm conditions.
- they are also created from big , strong waves when the wind is powerful.
- they occurs when wave energy is high and the wave has travelled over a long fetch
Swash of the wave
Swash goes up at the angle of the wind ( on the direction of the wind ).
Wave
A wave is a body of water moving towards a coastline at higher than average level.
Backwash of the wave
The backwash is always at right angles to the sea.
Constructive waves
- they are created in calm weather and are less powerful than destructive waves.
- they break on the share and deposit material, building up reaches.
- they have a Swash that is stronger than the backwash.
Formation of wave cut platform
- Erosion occurs at high water / high tide.
- The processes of erosion must be mentioned ie. Corrasion, solution and hydraulic action.
- Undercutting occurs.
- A wave cut notch is formed at the base of the cliff.
- The resulting overhang collapses and the cliff.
- A large area of flat rock is left at the base of the new cliff line. This is the wave-cut platform.
Caves, Arches and stacks
- CRACK
a large crack is enlarged by the pressure on / off effect of hydraulic action. - NOTCH
the crack grows into a notch and then a cave as destructive waves coverage on the headland and continue to erode it. - CAVE
over time, the cave becomes larger. Wave refraction draws waves to all sides of the headland so caves may form back-to-back. - ARCH
the sea breaks through the back of the cave forming a natural arch is widened as notches form. - HEAVY TOP OF THE ARCH
weathering such as freeze-throw continues to weaken the top of the arch, making it
less stable. - ROCKS FELL
top of the arch eventually collapses. - STACK
this leaves a pillar of detached rock called a stock. - STACK STARTS TO FALL
notches from at the base of the stack, which eventually makes it unstable. - STUMP
the stack will eventually topple into the sea, leaving only its base. This stump is normally only visible at low tide.
Transportation and LSD( long shore drift ),
Solution
Solution = dissolved chemicals ( often derived from chalk or limestone) in sea water and carried in solution. The load is not visible.
Transportation and LSD( long shore drift), suspension
Suspension = small particles are carried (suspended) in water, eg slits and clays, which can make the water look cloudy.
Transportation and LSD( long shore drift ), saltation
Saltation = load is bouncing or hopping along the sea bed, eg small pieces of shingle or large sand grains. Particles which are too heavy to be suspended.
Transportation and LSD( long shore drift ), traction
Traction = pebbles and larger sediment are rolled along the sea bed.
Long shore drift
Long shore drift = transport of sediment along a stretch of coastline caused by waves approaching the beach at an angle.
The land forms, types (3)
- Beaches
- Splits
- Bars
Coastal deposition.
Deposition is likely to occur when:
- waves enter an area of shallow water.
- waves enter a shelter area, eg a cove or bay, where low energy means constructive waves are dominant.
- there is little wind.
- wide expanse of flat beach, so swash spreads out, weaking the wave, so backwash is weak.
- there is a good supply of material from up drift erosion.
Beach
A beach is the gently sloping area of land between the right and low water marks.
Beaches ARE NOT permanent features as their shapes are alternated by waves.
Split
A split is a narrow coastal land formation that is tied to the coast at one end
Formation of Bar
Because of wind creates long shore drift and sand bank is carrying on the beach. At the end of it, it starts deposition and split forms. Split joins with headlands and creating the bar behaving and it creates lagoon.
Formation of Tombolo
Tombolos are formed where a split continues to grow outwards joining land to an offshore island to be located in the path of the land of the long shore drift for the split to latch onto as it grows.
Tombolos, like all deposition features can be removed during large storm but are often permanent and used.
Location of Dune
Essential conditions, large flat beach, large supply of sand, onshore wind, large tidal range and an obstacle such as drift wood.
Similarities and differences between the bars and splits.
Similarities: they creating in the same way( long shore drift)
Differences: bars going to lagoon, split goes to the sea.
Sand dunes
Sand dunes are often found at the back of a beach. However, they need very specific contact to form and are therefore not uniformly seen
Sand movement
Sand movement = the sand used to create dunes is transported to the back of the beach by the wind in 3 main ways, creep, saltation, suspension
Formation of dune
- At the back of the beach is an obstacle such as drift wood.
- Heaviest grains settle against the obstacle, lighter ones settle on other side of obstacle.
- Side facing the wind begins to form a crest.
- This is because the pile of sand become too steep to build ups and falls under its own weight .
- Sand stops slipping when slope reaches a gradient of 30-34 degrees.
- Repeated movement of material up windward side and down leeward side causes dunes to migrate inland.
- Sand dune its self becomes and obstacle and other dunes from in front of it.
Concordant
Concordant = where bands of different rock type run parallel to the coastline.