How are costal landscapes developed? Flashcards

1
Q

How does climate impact weathering?

A

In warmer climates chemical weathering occurs at higher rates

In colder climates weathering such as freeze-thaw & carbonation occur more

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2
Q

How can Landslides change the coastal landscape?

A

if a large mass of sediment falls in a short period of time it can result in a dramatic change in the shape of a coastline

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3
Q

How does rock fall impact the coastal landscape?

A

when rocks become loose and fall due to gravity they can be taken away by the waves or stay at the bottom of the cliff as scree

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4
Q

What are rotational slides?

A

this is when mass movement occur on a curved plane

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5
Q

How can humans impact fluvial erosion?

A

Activities such as deforestation and building dams can impact the amount of sediment that is transported to the coast

also the effectiveness of the river to erode the sediment due to impacted levels of energy

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6
Q

What is traction?

A

This is when boulders roll along the sea bed

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7
Q

What is saltation?

A

when small pebbles or rocks roll along the sea bed

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8
Q

What is suspension?

A

this is when the sediment is moved along in flow

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9
Q

When does deposition take place?

A

this happens when the energy of the wave/wind drops due to a loss of velocity or decrease in volume of water

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10
Q

When does deposition take place?

A

this happens when the energy of the wave/wind drops due to a loss of velocity or decrease in volume of water

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11
Q

What is settling velocity?

A

This is the speed at which sediment of a certain size will be deposited

Larger particles deposited first with the smaller particles being deposited last

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12
Q

Where do Headlands and bays form?

A

they form along discordant coastlines

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13
Q

how do Headlands and bays form?

A

The weaker rock gets eroded back by erosional processes and results in bays being formed

the stronger rock is left stick out as a Headland

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14
Q

What is wave refraction?

A

Wave refraction is what occurs at uneven coastlines such as headlands and bays

it is when the waves hit the headlands first and then bend the waves into the bays where energy expended is less

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15
Q

How do caves form?

A

As a headland faces side erosion due to wave refraction and orthogonal converging

Faults/joints of weakness are exposed due to erosional processes such as abrasion, hydraulic action and solution

Caves form when these faults widen and damage is concentrated at low and high tide marks

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16
Q

How does an arch form?

A

If the wave angle or refraction is right then it can cause erosion through the headland or the cave joining another cave on the other side

Creating an arch

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17
Q

How does an stack form?

A

the base of the arch continues to widen as it is further eroded

eventually this results in the arch collapsing forming a stack

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17
Q

How does an stack form?

A

the base of the arch continues to widen as it is further eroded

eventually this results in the arch collapsing forming a stack

18
Q

How does a stump form?

A

The base of the stack continues to be eroded until it collapses leading to a stump being left

19
Q

What are the 3 types of rock strata?

A

?

20
Q

How are shore platforms formed?

A

Destructive waves break on relatively steep cliffs, between low and high tide marks creating a wave cut notch

continual undercutting removes the support for the rock strata above so it collapses

As the cliff retreat continues, a gently seaward sloping shore platform is created at the base of the cliff. Normally between 0 and 3 degrees in angle

the platform becomes so wide (approx. 500m) that the friction from the platform slows the waves and they break on the platform itself, ceasing the undercutting

21
Q

What is an example of an shore platform?

A

Flamborough Head on the Holderness Coastline

22
Q

What is an example of an arch?

A

Durdle Door, Jurassic coast, Dorset

23
Q

Example of a stack and stump?

A

Old harry and his wife in Dorest

24
Q

What are Geos?

A

narrow, steep sided inlets formed by weakness in the rock (e.g
joints/faults) that have eroded more rapidly thanthe surrounding rock

25
Q

How do Geos form?

A

Joints/faults cause rock to be eroded quicker than surroundings

Or

tunnel like caves can have a total collapse causing a geo to form

Hydraulic action & abrasion are main erosional processes involved with this

26
Q

How does a blowhole form?

A

when a cave only has a partial collapse it can result in a blowhole forming

in storm like conditions water can be forced up the vertical blowhole

27
Q

Whats an example of a Geo?

A

35m deep Huntsman’s Leap in Pembrokeshire which is formed
in a joint in carboniferous limestone

28
Q

What is an example of a Blowhole?

A

Trevane, Cornwall

29
Q

What are beaches?

A

They are accumulations of material between the lowest tide and highest storm waves

They are influenced by the wind strength and therefore the wave energy

30
Q

How do different wave types influence a beach?

A

destructive waves will carry sediment away from the beach creating a flatter beach

Constructive waves will bring sediment onto the beach which creates a steeper beach profile

31
Q

How do beaches vary with angle?

A

sandy beaches have a gentle gradient of less than 5 degrees, sad is very compact when wet which means that there is little energy lost from percolation allowing the backwash to pull sand down off the beach

Pebble beaches are much steeper at around 20 degrees as they have high levels of percolation through the pebbles which means the backwash loses energy and cant pull and material back

32
Q

Which beaches have LSD?

A

Drift aligned beaches have LSD

Swash aligned beaches don’t have LSD as the swash goes up at right angles

33
Q

How do spits form?

A

Most common when tidal range <3m as it allows sediment to be readily transported

Where the longshore drift current enters deeper water near the distal end, wave energy is dispersed throughout more water.

Rates of transport are reduced and deposition increases.

34
Q

Why are spits curved?

A

spits are curved due to wave refraction around the coastline and the presence of a secondary wind/wave direction influencing the coastline

35
Q

what happens to the area behind a spit?

A

it is a low energy environment so allowing deposition to continue

can lead to the formation of a lagoon or salt marsh

36
Q

Why are spits dynamic?

A

they exist as long as deposition > erosion so can be easily influences by events such as storms

37
Q

How do on-shore bars form?

A

it is formed as a spit grows across an indentation in the coastline (e.g a cove or bay)

It is also dynamic due to it being reliant on deposition > erosion & vulnerable to sea level rises and storms

At the landward side of the bar a salt water lagoon forms

38
Q

How do tombolos form?

A

A tombolo is a beach that connects the mainland to an offshore island.

It often develops first as a spit, as longshore drift (usually in one dominant direction) transports and then deposits material where the coastline changes direction and wave energy is lost.

39
Q

Where are salt marshes found?

A

They are features of low energy environments

E.g estuaries or landward sides of spits

They are vegetated areas of deposited silts and clay

40
Q

Example of salt marshes

A

Welwick Saltmarsh on the River Humber

41
Q

How does vegetation impact salt marshes

A

The greater the density of vegetation, the more sediment that is subsequently trapped, helping to stabilise the saltmarsh.

The lower marsh will be submerged by highly salty water so biodiversity is poor in such harsh conditions, inundation twice a day by high and low tides

Further inland, a greater variety of species will thrive, including reeds and rushes.

42
Q

How do Salty marshes Drain?

A

Small creeks help to drain the marsh when at low tide, but can trap salt water which are often too salty for vegetation to grow, these areas are called saltpans.