The UKs Evolving Physical Landscape Flashcards
EROSION
The wearing away of the landscape.
STRATA
Layers of rock
GLACIATION
Huge glaciers(blocks of ice) that erode the landscape.
IGNEOUS
Rocks formed from lava and magma.
SEDIMENTARY
Rocks formed from sediments deposited from rivers or the sea.
METAMORPHIC
Sedimentary rocks that were heated and changed under pressure to form a new type of rock.
WEATHERING
The breakdown of rocks by the weather.
DISCORDANT ROCKS
If the rock strata is at right angles to the coast it means it is discordant.
CONCORDANT COASTLINE
If the strata is parallel to the coast then it is concordant.
HEADLANDS
This is where a more resistant rock is sticking out in to the sea.
STACKS
This is a more resistant headland that has been eroded to be left remaining in the water. It was previously a natural arch that got eroded.
FETCH
The distance of water between two bits of land.
SWASH
Waves that go up the beach.
BACKWASH
The movement of water back down the beach after the waves break on the beach.
CONSTRUCTIVE WAVES
Waves that have a strong swash and weak backwash. They build up the beach as a gentle sloping beach.
DESTRUCTIVE WAVE
A wave that has a very strong backwash that creates a steep beach.
ABRASION
For coasts, a type of erosion that is where bits of rock scrape along the cliff like the action of sandpaper and get thrown against the cliff.
For rivers the scratching and scraping of a river bed and banks by the stones and sand in a river
HYDRAULIC ACTION
This is a type of erosion which is the power of the waves against the cliff. Water is forced into cracks and the air in the crack is put under pressure creating a mini explosion.
ATTRITION
Rock falls off the cliff into the water and collide against each other in the sea or river. They get smaller and smaller in size.
SOLUTION
This is a type of erosion where the rock chemically reacts with water.
WAVE CUT PLATFORM
This is a level piece of rock that is left where the cliff once existed. It has rock pools in it often and gets covered in high tide.
LONGSHORE DRIFT
The transportation of sediment along the coastline. The direction is determined by the wind direction.
DEPOSITION
This means the dropping of sediment
BAR
A stretch of sand across the bay, which is caused by longshore drift.
SPIT
A stretch of sand out from the coastline, usually with a curved end.
SALT MARSH
Salt tolerant vegetation growing on mud flats in bays or estuaries.
SAND DUNE
Onshore winds blow sand inland forming a ridge of sand parallel to the shoreline.
COASTAL MANAGEMENT
This is the way in which the coastline is protected from erosion.
SUB AERIAL WEATHERING
This is where there is weathering or mass movement (rock falls, landslides) on a cliff.
CLIFF SLUMPING
This is where the cliff collapses down into the sea.
HARD ENGINEERING
These are traditional, man made types of sea defence like sea walls, revetments, grounds.
GROYNES
A type of sea defence made from wood or concrete that sticks out perpendicular to the coastline into the sea.
RIP RAP (rock armour)
Blocks of limestone, granite that are put at the bottom of a cliff. The wave power is lost on these rather than at the bottom of the cliff.
GABIONS
A type of sea defence that is a cage of small stones. Waves hit these rather than the bottom of the cliff.
HOLD THE LINE
A type of coastal management where there are sea defences stopping erosion.
STRATEGIC RETREAT
Gradually letting the coastline erode and moving businesses and people away from the coast.
DO NOTHING
A type of sea defence where there is no action at all and councils let there be erosion. You do defences where there is a need.
SOFT ENGINEERING
This is natural sea defences that are not man made. These would be beach nourishment or planting vegetation or offshore breakwaters.
SALTATION
In a river material may bounce along the bed of the river downstream.
SOLUTION
In a river some material maybe dissolved and transported downstream.
TRACTION
In a river some material may roll along the bed of the river downstream.
SUSPENSION
In a river some material may be held in suspension within the river as it goes downstream.
UPPER COURSE
This is the top part of a river nearer to the source.
V SHAPE VALLEY
This is the shape of a valley along a river.