coastal landscapes Flashcards

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1
Q

what are the characteristics of destructive waves

A
  • Large steep wave plunges over
  • Beach cliff forms
  • Strong backwash
  • Weak smash
  • Little percolation through sand
  • Eroded material deposited
    offshore in longshore bars
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1
Q

what are the characteristics of constructive waves

A
  • Strong swash transports sand up the beach to for a berm
  • Low flat waves spill over
  • Orbital motion of wave becomes more elliptical with sea bed contact
  • Material from offshore bars moved onshore
  • Weak backwash much percolation through sand, little transport of sand down the beach
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2
Q

Why is the process of refraction important?

A

Why is the process of refraction important?
* At a discordant headline, as waves hit the headland they converge and erode the sides of the headlands. As the waves lose energy, they undergo deposition at the bay which leads to the formation of a beach as sediment accumulates.
* At a discordant coastline (alternating bangs of less and more resistant rock) waves converge around the headland as wave refraction occurs (2)
* Waves concentrate their energy around the headland, leading to high levels of erosion and therefore erosional landforms are created (1)
* Wave energy is therefore dispersed and low energy waves reach the bay leading to more deposition and the creation of more beaches (1)

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3
Q

what is a neap tide

A

when the moon and the run are at 90 degrees in relation to the earth

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4
Q

what is spring tide

A

when the moon, earth and sun are in line

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5
Q

define thermohaline

A

Thermohaline = the circulation of ocean water of different densities due to their temperature and salt content.

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6
Q

what are the characteristics of a high energy coastline

A

Waves are powerful

The rate of erosion exceeds the rate of deposition

Characteristics such as cliffs and wave cut platforms

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7
Q

what are the characteristics of a low energy coastline

A

Waves are not powerful

The rate of deposition exceeds the rate of erosion

Characteristic landforms include beaches and spits

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8
Q

what is the littoral zone

A

The littoral zone is the near shore area where sub light penetrates sediments, allowing for aquatic life to flourish, but faces rapid change continually.

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9
Q

how often do spring/neap tides occur

A

twice in a lunar month

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10
Q

what is a sediment cell

A

Sediment cells are distinct areas of coastline separated from other areas by well-defined boundaries, such as headlands and stretches of deep water. Their inputs and outputs of sediment are balanced within each cell. Sediment cells vary in size.

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11
Q

what is the definition of weathering

A

Coastal weathering is the disintegration of rock as it loses its integrity or coherence. The rock mass stays largely the same, but its structure is increasingly fragmented

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12
Q

what are the different types of weathering

A

chemical
mechanical
biological

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13
Q

what is freeze-thaw weathering

A

Primarily occurs in temperature humid climates. Water enters cracks in rocks, freezes and expands by 9%. This causes the rock to crack and pieces to fall off

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14
Q

what is onion skin weathering

A

Usually occurs in arid reasons. Temperature rises, rocks heat. As the rock heats, it expands. At nigh as temperature falls, the rock cools and contracts. This causes the outside layer of the rock to peel away.

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15
Q

what is wetting and drying

A

Coasts are often rich in clay; these clay-rich soils will expand when they are wet and contract when they are dry. This process of expanding and contracting cracks the rocks, making them vulnerable to freeze-thaw and salt crystallisation.

16
Q

salt crystalisation

A

Occurs in semi-arid conditions. Water evaporates from rocks, leaving behind salt. This causes a dramatic increase in volume, leading to the rock cracking and pieces falling off.

17
Q

what is carbonation

A

Coastlines composed of chalk or limestone may be dissolved by acidic rainwater or seawater. The rain/sea absorbs co2 from the atmosphere, creating a weak carbonic acid.
This can convert solid calcium carbonate to soluble calcium bicarbonate and the rock dissolves.

18
Q

what is oxidation

A

Rocks containing iron compounds experience oxidation of the iron into a ferric state (rusting) when oxygen and water are readily available from air or sea. This can lead to disintegration.

19
Q

what are the different types of erosion

A

hydraulic action
abrasion
solution
quarrying
attrition

20
Q

what is the process of hydraulic action

A

The waves force air into the cracks in rocks causing it to break

21
Q

what is the process of abrasion

A

Rock fragments being thrown onto the cliff face, weakening the cliff structure

22
Q

what is the process of quarrying

A

The waves scoop loose rocks out from the cracks formed in rocks

23
Q

what is the process of solution

A

Chalk and limestone is dissolved and rock is removed in solution

24
Q

what are the different types of transportation

A

traction
saltation
suspension
solution

25
Q

what is traction

A

Large particles like boulders are pushed along the sea bed by the force of the water

26
Q

what is suspension

A

Small particles like silt and clay are carrying along in the water

27
Q

what is saltation

A

Pebble sized particles are bounced along the sea bed by the force of the water

28
Q

what is solution

A

Soluble materials dissolve in water and are carried along

29
Q

what is soil creep

A

The slow movement downhill of individual particles due to gravity. Raindrops may dislodge particles, which will slowly move downhill due to gravity

nature of movement: slope

rate: slow

wet/dry: wet

30
Q

what is mudflow

A

Heavy rain can cause large quantities of fine material to flow downhill. As surface layers become saturated, water carries mud downhill.

Nature of movement: slope

rate: fast

wet/dry: wet

31
Q

what is a landslide

A

Occur on cliffs made from softer rocks or deposited material, which slip as a result of failure within it when lubricated, usually following heavy rainfall

nature of movement: diagonal

rate: fast

wet/dry: wet

32
Q

what is slumping

A

Where softer material overlies much more resistant materials, cliffs are subject to slumping. If lubricated, whole sections of the cliff can move downwards

nature of movement: rotational

rate: slow

wet/dry: wet

33
Q

what is rockfall

A

These occur from cliffs undercut by the sea, or on slopes effected by mechanical weathering like frost action

nature of movement: vertical

rate: fast

wet/dry: dry

34
Q

what is solifluction

A

Mass movement of soil and Regolith affected by alternate Freezing and Thawing. Characteristic of Saturated soils in high latitudes, both within and beyond the permafrost zone.

35
Q

what is regolith

A

the layer of unconsolidated solid material covering the bedrock

36
Q

what factors effect coastal landscapes on a spatial and temporal scale

A

Climate

Temperature range
- Freeze thaw especially in places with large diurnal ranges
- Onion skin weathering
- Melting of ice, more sediment

Wet climates
- Weathering - carbonation from acid rain
- More mass movement (slumping landslide)
- Wetting and drying

Tides/waves

Wave steepness
- More plunging waves remove more sediment
- More spilling waves, deposit more sediment

Length of fetch
- Higher energy waves (more destructive waves)

Gradient of sea bed
- Sudden change in gradients make more destructive waves

Humans

Construction of groynes
- Blocks longshore drift, leads to the rest of the sediment cell will be starved from their sediment sources

Dredging
- More dredging decreases fluvial sediment

37
Q

what structural factors effect the coastal landscape

A

dip of cliff
strata
rock resistance
rock type (carbonation/oxidation)
precipitation
vegetation
human interference
tidal range
low/high energy coastline