Coasts Flashcards
What are coasts shaped by
The sea and the action of waves. The processes that take place are erosion, transportation and deposition.
What is fetch
The distance in which the wind has blown
What are waves caused by
The transfer of energy from the wind
What does a waves energy depend on
It’s fetch, the strength of the wind blowing,, the length of time over which the wind has blown.
How do waves break
A prevailing wind causes waves to start out sea and have a circular orbit, as waves approach the shore friction slows the base of the wave. This causes the orbit to become elliptical until the top of the wave breaks over. Water swashes up the beach and water from previous Wave returns to the sea as back wash.
What is a constructive wave
Waves Created in calm weather that build up the beaches
What is a destructive wave
A wave formed in stormy conditions that erodes the beach.
Height of a constructive wave
Under a metre
Height of destructive wave
Over a metre
Shape of constructive wave
Long in proportion to its height
Shape of a destructive wave
High in proportion to its length
What is the swash and backwash like in a constructive wave
Swash is strong and backwash is weak
What is the swash and backwash like in destructive waves
Swash is weak but backwash is strong
How many constructive waves could occur per minute
Under 11
How many destructive waves could occur in a minute
Over 13
Season in which constructive waves are more common
Summer
Season in which destructive waves are more common
Winter
What is a headland
A cliff promontory which juts out into the sea such that it is surrounded by water on 3 sides
What is a bay
A crescent shaped indention in the coastline found between two headlands. It usually has a beach which may be composed of sand or shingle.
Formation of headland and bays
Waves erode the les resistant rock and the more resistant rock. The less resistant rock erodes due to rapid erosion such as that of abrasion, hydraulic action and some solution.
Once the bay has formed the headlands are left sticking out so sea where their hard rock has been resisted of erosion.
Where and when will the rate of erosion be higher?
Coastline is exposed to a large fetch.
Strong winds blow for a long time creating destructive waves.
An area with no beach to act as a buffer between sea and cliffs.
Areas of soft rock.
A rock has many joints.
Waves converge on a headland (wave refraction) and gain height and erosive energy.
What is wave refraction
Their energy is concentrated Around headlands but reduced around bays.
Waves then tend to approach the coastline parallel to it, and their energy decreases as water depth decreases.
What is a cliff
A steep or vertical face of rock often found at the coast.
Formation of cliffs
Formed by weathering which weakens the top of the cliff whilst the sea attacks and waves erode the base which creates a wave cut notch. The notch increases in size causing the cliff to collapse, the backwash Carries the rubble towards the sea and it is repeated again.
Wave cut notch-undercut at base
What is a wave cut platform
A wide gently sloping surface at the foot of a cliff, left behind when cliff retreats- exposed at low tide.
Formation of wave cut platform
The wave cut notch created, size gradually increases. As there is now nothing to support the cliff face above the force of gravity weakens the rock which is then broken off and eroded by attrition in the sea. The cliff retreats and leaves a wave cut platform, from where the cliff used to be. An area of flat rock is left at the base of the new cliff. This process is repeated resulting in wider wave cut platforms.
Characteristics of wave cut Platform
Slopes gently down to the sea at a 3-5* angle.
Bare rock, smoothed in places by attrition
Deep cracks in some places
Covered at high tide and exposed at low tide
An oval pitted appearance of bare rock interspersed with rock pools.
Formation of caves, arches, stacks and stumps.
A large crack opened up by hydraulic action.
The crack grows into a cave by hydraulic action and abrasion.
The cave becomes larger.
The cave breaks through the headland forming a natural arch.
The arch is eroded and collapses.
This leaves a tall rock stack.
The stack is eroded forming a stump.
What is a beach
A landform of coastal deposition that lies between the High and low tide levels.
Describe the characteristics of a sandy beach Referring to its ... Gradient Dominant wave Distance stretched inland Back of beach
A sandy beach is generally shallow and flat, it’s dominant wave is constructive.
It’s distance stretching inland is a long way and at the back of the beach you will find sand dunes (sometimes).
Low tide In a sandy beach what is formed
Small water filled depressions called runnels form. These are separated by small sandy ridges running parallel to shore. The wet sand may have a rippled appearance.
Describe the characteristics of a pebble beach Referring to its... Gradient Dominant wave Distance inland Back of beach
The gradient on a pebble beach is generally steep, the dominant wave is destructive and the distance inland is not far.
At the back of the beach you can find large pebbles, pebble size increases towards the back of the beach.
How do sandy beaches form
In shelters bays, low energy constructive waves transport material onto the shore. The swash is stronger than the backwash,so sediment is slowly but constantly moved up the beach.
Once the tide has gone out, there is more material on the beach than before.
How do pebble beaches form
In Exposed beaches where there is large fetch.
Destructive waves plunging nature along with their stronger backwash means that pebbles are not moved far up the beach, which makes the beach profile steep.
A storm beach may form when there is wind, stormy weather and waves hurl boulders and large pebbles at the back of the beach.
Why and how do beach profiles change in winter
In winter destructive waves are present as the waves excavates material from the beach creating a concave profile. The beach will become much narrower, steeper and smoother.
Why and how do beach profiles change in summer
The beaches experience constructive waves, sand will slowly return to the beach and berms and sand dunes typically recover, as the sediment isn’t lost by offshore. The key change is the berm as it changes the most seasonally which affects the shape the most.