IGCSE CIE Geography - Coasts
Terms in this set (83)
The border between land and sea.
Why are coasts important?
Oil / gas reserves
Why are coasts under threat?
Rising sea levels
Privatisation increases cost
Oscillations in water formed by the friction between the wind and the sea.
Factors affecting the size of a wave
Duration of wind
Strength of wind
Fetch (the distance travelled by a wave)
Top of a wave.
Bottom of a wave.
Distance between two crests / troughs.
Distance between crest and trough.
Number of waves per unit of time (generally minute).
The speed that a wave is travelling at, influenced by wind, fetch and depth of water.
The movement of water and load onto the beach.
The movement of water and load back down the beach.
As the wave reaches shallower water, the friction with the sea bed increases and thus the wave slows down.
If there is a headland, the waves slow down where the water is shallower, but continue to travel to the bay where water is deeper. As a result, the wave disperses its energy differently and contributes to the forming of a headland.
Waves with a weak swash and a strong backwash that erode and transport material away from beaches.
Waves with a strong swash and a weak backwash that deposit material on beaches.
When sea water and air are trapped in the cracks of rocks, increasing the pressure and causing them to break apart.
Rocks thrown against a cliff by waves.
Acidity of the sea causes small particles to dissolve.
Rocks and particles thrown against each other by the sea.
Immense power of waves crashing into cliffs, causing them to weaken.
Top of cliffs being attacked by the weather (wind, rain, heat, cold etc.), weakening it.
An indented area of land normally found between two headlands. Usually more sheltered so there is less erosion; beaches are commonly found.
A piece of land that sticks out into the sea that also causes waves to refract, forming additional features such as arches and stacks.
A small eroded hole at the bottom of the cliff formed by erosion.
The retreating of a cliff due to erosion, forming a low-lying platform.
A large area under a cliff, formed by erosion (mainly hydraulic pressure).
A cave eroded all the way through a headland.
When the roof of the arch collapses, forming two separate columns of rock.
Stacks eroded by the sea and wind.
When the sea erodes to the top of the headland, forming a large crack and hole.
Process of waves transporting material along a coastline.
Direction a wind normally hits a coastline.
Wooden or concrete fences placed out into the sea to reduce the impacts of longshore drift.
Movement of water caused by differences in temperature, changes in wind or tides.
When small particles (e.g. rocks) are bounced along the beach due to transportation.
Movement of the sea in and out, twice a day, caused by the gravitational pull of the moon.
Area of land between high tide and low tide.
When the sun and moon are in alignment to each other, causing extremely high and low tides.
When the sun and moon are aligned to each other perpendicularly, causing lower high and low tides.
Long, thin stretch of sand connected to mainland but stretching out into the sea.
A low energy, intertidal ecosystem that forms behind a spit containing some salt-resistant vegetation (halophytes).
A spit that joins the mainland with an island.
Main landmass of an area.
A small body of land found in oceans and seas.
A spit that connects two headlands or runs across a small cove / bay.
A salt water lake that develops behind a bar.
Changing Sea Levels
Sea levels are not constant, though currently it is rising. There are two types of sea level change.
Global changes, when the whole level of the sea rises or falls. This is mostly affected by the amount of ice held in glaciers and ice shelves.
Local changes, when the level of the land changes relative to the level of the sea.
Accumulation of material between the lowest spring tides and the highest spring tides. Material can be deposited from longshore drift, constructive waves and river discharge.
A ridge (long thin hill) that forms at the top of the beach where the strand line is.
A line of material (seafood, driftwood etc.) that is deposited by the sea at the furthest point of the high tide.
Extensions of beaches that are formed by dry sand blown onto the beach.
Starting dunes of sand dunes, formed in the sheltered are between the berm and strand line.
Small embryo dunes join together.
Small amounts of vegetation (e.g. sea couch and marram grass) begins to grow on foredunes.
A developing humus layer starts to change the colour of the dune from yellow to grey.
As the humus layer continues to grow, the dune can now support more vegetation, including flowers and trees.
As the size of the dunes develop, water is collected between the dunes where marsh vegetation can grow.
A depression or hole in the dune caused by the wind.
Layer of decaying plant or animal matter that adds nutrients to the ground.
Changing types of plants (e.g. from basic sea couch to trees).
Line between saturated and unsaturated ground.
This building a physical structure, usually out of wood or concrete to protect the coast. This is usually more effective, but it can be very expensive and unsightly.
Examples of Hard Engineering
Working with nature to reduce the impacts of coastal erosion slightly.
Examples of Soft Engineering
It is not possible to protect the entire coastline of every country. Therefore, cost-benefit analysis is often carried out to see if the coast is worth protecting. The economic benefit of a coast will be looked at (e.g. how many jobs are in the area, how much tax the area pays, the value of the buildings in the area) and then the cost of protecting the area (e.g. how much a sea wall or rip-rap will cost).
A line of limestone coral polyp found in warm, shallow areas.
Reef that circles the coastline or islands, often protected by barrier reefs further out to sea, so the plants and animals are suited to low wave-energy environments.
Reefs that occur further from the sea and are commonly separated from the mainland or island by a deep lagoon, normally older and wider than fringing reefs.
Reefs that rise from submerged volcanoes and surround an island.
How coral reefs provide benefits
Support 25% of marine species (about 1 million species of plants and animals)
Protect coastlines from erosion
Natural barrier against tropical storms and tsunamis (they can absorb energy)
Natural recycling agent for carbon dioxide from sea and atmosphere
Contribute material to the formation of beaches (eroded coral reef)
Source of raw material (coral for jewelery and ornaments)
Many species are being found to contain compounds useful in medicine
Benefit the tourism industry because many people like to dive and snorkel over coral reefs
Important fishing grounds
High global value of coral reefs in terms of coastal protection, fishing and tourism: $375 billion.
How coral reefs are being damaged
Rising sea levels
Increases in the global climate
Dynamite, cyanide and trawling fishing techniques
How coral reefs are being managed
Ban damaging fishing practices
Fish stocks can be enhanced and quotas imposed on amount being caught
Sewage outlets can be moved downstream of coral reefs
Banning the dropping of anchors on coral reef
Reduce the use of fertilisers near coral reefs
Alternative Names for Tropical Storms
Hurricane (North America)
Typhoon (East Asia and Pacific)
Cyclone (South Asia)
Temperature Required for the Formation of a Tropical Storm
When a tropical storm hits land.
When an area of low pressure turns into a tropical storm.
When tropical storms breaks up and loses all its strength.
The centre of a tropical storm.
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