3- Coastal Landscapes Over Time Flashcards

1
Q

2 process of sea level change

A

Eusatic (change in height of sea)
- more/less water in ocean
- warmer climate = thermal expansion

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2
Q

Process of sea level rise due to warming climate

A
  • melting of terrestrial ice = more water in ocean
  • warmer climate = thermal expansion = water molecules take up more space
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3
Q

Process of sea level fall due to cooling climate

A
  • more water stored on land as terrestrial ice = freezing of rain water= ocean water evaporates = rain = rain freezes = less water in ocean
  • thermal contraction = water molecules take up less space as they vibrate less due to less energy
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4
Q

What is a Ria and how does it form

A

Flooded river estuary , wide + gentle sloping
1- river erodes forming wide valley + floodplain
2- sea level rise
3- river valley is submerged

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5
Q

How can a Ria change over time

A
  • sheltered inlet = low energy environment = allows deposition of sediment = Ria gets shallower
  • erosion at mouth of river = becomes wider
  • in low energy environments flocculation may of or at mouth = deposition
  • narrow inlet = waves have very little energy
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6
Q

What is a Fjord and how does it form

A

Glacial U-shaped valley flooded by rising sea
- steep + narrow with deep channel
1- glacier erodes/ carves gorge by the scraping of sediment in glacier over land
2- sea levels rise
3- glacial valley is submerged

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7
Q

How might a fjord change over time

A
  • weathering + marine erosion break down sides of fjord = gentler sloping gradient
  • deposition at sheltered end of fjord = shallower + change of beach forming
  • erosion at mouth of river (entry to fjord) becomes wider
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8
Q

What is a shingle beach and how does it form

A

Deposited material rolled onshore as sea levels rise , can appear as a straight bar
1-sediment deposited by rivers, waves etc
2- sea levels rise
3- sediment rolled inland as sea rises

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9
Q

How might a shingle beach change over time

A
  • smaller material/sediment is vulnerable to erosion = sorting of sediment by size as longshore drift transports smaller sediment further down coast
  • beach can become steeper due to rising sea level
  • larger sediment is pushed up further and is not eroded due to it requiring a lot of energy = larger sediment at back
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10
Q

What is a raised beach and how does it form

A

Flat area higher than sea level = former wave cut platform
1-erosion of cliff = WCP
2- sea level fall/ regression
3- WCP exposed

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11
Q

How might a raised beach change over time

A
  • colonised by vegetation = hold it together + make more stable
  • could be undercut = raised beach falls + eroded away
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12
Q

What are abandoned cliffs + how do they form

A

-Steep rocky land above present day sea level, often contain other erosion as landforms such as caves or arches
1- steep cliff formed by wave erosion
2- sea level fall/regression
3- cliff left exposed above high tide mark

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13
Q

How might abandoned cliffs change over time

A
  • potential for undercutting + mass movement
  • weathering
    = a chance for a build up of sediment beneath cliffs
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14
Q

What is a marine terrace + how might it form

A

A series of flat areas + sloping areas leading up sea = shows the series of steps in landscape as sea levels fall in stages
1- WCP formed
2- sea level fall
3- another WCP formed at that level
4- sea levels fall again
= series of steps/WCPs

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15
Q

How can a raised beach continue to change over time

A
  • vegetation colonies = strengthens or weakens WCP
  • weathering + mass movement leading to a more gentle profile
  • wave erosion at base
  • sea levels rise could affect via marine proscess
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16
Q

2 types of sea level rise

A

Eustatic = change in water level
Isostatic = change in land level

17
Q

What is Isostatic depression + rebound

A

Depression = build up of material on land = weight of material pushes down on crust = allowing sea to rise further inland

Rebound= removal of sediment of land = land “rebounds” up due to less weight/pressure on it = sea levels fall on local scale

18
Q

How much are sea levels rising a year

A

3.3 mm

19
Q

What could happen to sea levels if greenlands ice sheets melted

A

6m of sea level rise

20
Q

Give an example of a place experiencing isostatic action

A

Scotland undergoing isostatic rebound = land rising due to not being compressed by ice

21
Q

How much lower we’re sea levels in last glacial period - 70,000 years ago

A

100-150 m

22
Q

What is the term for retreating sea levels exposing land

A

Marine regression

23
Q

How much colder was the last glacial period

A

5*C lower

Devensian period

24
Q

How much warming is required for 2m of global sea level rise

A

1•C

25
Q

Name of last glacial period

A

Devensian period
70,000 years ago

26
Q

Name of current interglacial period called

A

Holocene period

27
Q

main reason for changing sea levels

A

Milankovitch cycles

  • However the effect of human activity is accelerating the rise of temps and sea levels beyond natural
28
Q

In the previous Inter-glacial (130,000 years ago) how much higher were sea levels and how much warmer was it

A

20m higher

3.C warmer