Physical landscapes in the UK - section c Flashcards
what is weathering and erosion
weathering is where rocks are broken down where they are
erosion is when rocks are broken down and carried away by something
what is freeze-thaw weathering
It happens when the temp alternates above and below 0*c. Water fills the cracks of rock and eventually freezes (when water freezes it expands) which puts pressure on the rock. One the water thaws it contracts which releases the pressure on the rock. Repeated freezing and thawing widens the crack into the rock breaks up.
What is chemical weathering
Rainwater contains dissolved carbon dioxide making it a weak carbonic acid. Carbonic acid reacts with the rock that contains calcium carbonate so the rock is dissolved by the rainwater
what is mass movement
its the shifting of rocks and loose materials down a slope and can cause coasts to retreat rapidly. Its more likely to happen when the material is full of water as water acts as a lubricant and makes the rock heavier. When material shifts it can create a scarp (steep cut in slope).
Explain destructive and constructive waves
When wind blows over the surface of the sea it creates waves. The greater the fetch ( the distance the wind blows over the sea) the greater the wave. Storms can cause storm surges where the sea level is temporary risen caused as strong winds push water onshore.
Destructive waves erode the coast:
- high frequency and high and steep
-Their backwash is more powerful (water moving down the beach) than their swash (water moving up the beach) so material is removed.
Constructive waves deposit material:
-low frequency and are low and long
-swash is more powerful then backwash
what three ways do waves wear away coasts.
Hydraulic power - waves crash against rocks and compress the air in their cracks this put pressure on the rocks. repeated compression widen the cracks and breaks the rock off
Abrasion - eroded particles in the water scrape and rub against rock removing small pieces.
Attrition - eroded particles in the water collide, break into smaller pieces and become more rounded
Explain longshore drift
waves follow the direction of the mot common wind they usually don’t hit the coast at a right angle. The swash carries material up the beach in the same direction as the waves but the backwash carries material down the beach at a right angle eventually creating a zig zag of material over time.
Explain traction
large particles like boulders are pushed along the sea bed by the force of water
explain saltation
pebble -sized particles are bounced along the sea bed by the force of the water
explain suspension
small particles like silt and clay are carried along in the water
explain solution
soluble materials dissolve in the water and are carried along
what is deposition and what causes it
deposition occurs when water carrying material loses energy and slows down.
-coasts build up when the deposition is greater then the erosion
the amount of material deposited is increased when:
-there lots of erosion elsewhere on the coast (more material available)
-lots of material is transported into the area
-constructive waves as they drop more then remove.
what is a discordant and concordant coastline
discordant coastline is made up of alternating bands of hard and soft rocks at right angles to the cost
concordant - the alternating bands of rocks it parallel to the coast
How are headlands and bays formed
Headlands and bays are formed on concordant coastline so the erosion happens faster on the softer rock than the hard rock. This causes the soft rock to be eroded faster creating a bay with a gentle slop whereas the hard rock is eroded slowly meaning it juts out forming a headland with steep sides.
How are headlands eroded in to caves, arches and stacks
The resistant rocks that form a headland often have weaknesses likes cracks so when waves crashes against these cracks hydraulic action and abrasion erodes it. repeated erosion causes a cave to form. Then the cave is further eroded until it breaks through creating an arch. The rock that supports the arch continues to be eroded until it collapse leaving a stack (an isolated rock separate from headland).
How are cliffs eroded to form wave-cut platforms.
Erosion happens at the foot off a cliff over time eventually creating a wave-cut notch. This is the enlarged over time until the rock above the notch is unstable and collapses. The fallen material is then washed away and a new notch begins to form. After repeated collapsed the cliff retreats leaving behind a wave-cut platform
How are beaches formed
Beaches are formed by constructive waves and can form either a sand beach or a shingle beach.
Sand beaches are created by low energy waves that are flat and wide. Sand particles are small so the weak backwash can move them back down the beach, creating a long gentle slope.
Shingle beaches are created by high energy waves that are steep and narrow. Sand particles are washed away but larger shingles are left behind. The shingles particle build up to create a steep slope
How is a spit formed
Spits form at sharp bends at rivers. Long shore drift transport sand and shingle past the bend and deposits it in the sea. Strong winds and waves can curve the end of the spit creating a recurved end. The area behind the spit is sheltered from waves so material can accumulate over time. Over time the sheltered area can become a mud flat or saltmarsh
How are bars formed
A bar forms when a spit joins two headlands together. The bay behind the bar is cut off from the sea meaning a lagoon behind the bar can form. Offshores bars can form if the coast has a gentle slope - friction with the sea bed causes waves to slow down and deposit sediment offshore creating a bar that is not connected to the coast.
How is a sand dune formed
When sand is deposited by longshore drift is moved up the beach by wind. Obstacles cause the wind speed to decrease so sand is deposited, forming small embryo dunes. Embryo dunes are then colonised by plants e.g. marram grass. The roots of the plants stabilise the sand encouraging more sand to accumulate their this form foredunes and eventually mature dunes. New embryo dunes form in front of stabilised dunes. Dune slacks (small pools) can form in hollows between dunes
what is hard engineering
man-made structure built to control flow of the sea and reducing flooding and erosion
what is soft engineering
Schemes set us using knowledge of the sea and its processes to reduce the effects of flooding and erosion
What is a sea wall and its benefits
hard engineering
A wall made up out of a hard material like concrete that reflects waves back to the sea.
It prevents erosion of the coast and acts as a barrier to prevent flooding. However it creates a strong backwash that erodes under the wall and its expensive to build and maintain