Sea Level Changes Flashcards

(37 cards)

1
Q

State the 2 types of Sea Level Change.

A

-Isostatic
-Eustatic

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2
Q

Define Eustatic Change.

A

A Sea Level Change caused by a Change in the Volume of Water or a Change in the Shape of Ocean Basins.

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3
Q

State whether Eustatic Change is Local or Global.

A

Global.

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4
Q

State the 3 Factors that influence Eustatic Change.

A

-Thermal Expansion
-Tectonic Movement
-Ice Sheet Melt

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5
Q

Explain the Impact of Thermal Expansion on Eustatic Change.

A

As Ocean Temperatures increase, Water Expands which increases the Volume of Water in the Ocean.

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6
Q

Explain the Impact of Tectonic Movement on Eustatic Change. (3)

A

-The Earth’s Crust is constantly changing Shape and therefore the Capacity of the Ocean Basin.
-Sea Floor Spreading increases the Volume of the Basin and so decreases Sea Level.
-Underwater Volcanism produces large Volumes of Material that Displace Sea Water, causing Sea Level to Rise.

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7
Q

Explain the Impacts of Ice Sheet Melt on Eustatic Change.

A

Global Warming has increased Ocean and Atmospheric Temperatures causing Ice Sheets to Melt and hence Sea Levels have Risen.

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8
Q

Define Isostatic Change.

A

Sea Level Change caused by Vertical Movements of the Land Relative to the Sea.

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9
Q

State 4 Factors that influence Isostatic Change.

A

-Post-Glacial Adjustment
-Accretion
-Subsidence
-Tectonics

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10
Q

Explain the Impacts of Post-Glacial Adjustment on Isostatic Change. (2)

A

-During Glaciation Periods, Heavy Ice Sheets Weight the Land down.
-Post-Glaciation the Ice Sheets Melt and Land Rebounds to a Higher Level causing Sea Level to Fall in Isostaic Rebound.

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11
Q

Explain the Impact of Accretion on Isostatic Change.

A

Acccretion is where there is Net Deposition of Sediment causing Land to Fall realtive to the Sea Level.

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12
Q

Explain the Impact of Subsidence on Isostatic Change.

A

Subsidence of Land is caused by Excess Groundwater Extraction such as the Drainage of Marshland.

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13
Q

Explain the Impact of Tectonics on Isostatic Change.

A

Volcanism releases Lava and Ash causing Land to Rise Relative to Sea Level.

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14
Q

State how many mm a Year Scotland is Rebounding since the last Ice Age.

A

1.5mm a Year.

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15
Q

State how many mm a Year Cornwall is Sinking since the last Ice Age.

A

1.1mm a Year.

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16
Q

Since the last Glacial Maximum 21,000 yrs Ago, How has Sea Level Changed? (3)

A

-Sea Level has Increased by 130m.
-Sea Level has Fluctuated at its Current Level for the last 4000yrs.
-Since 1930’s Sea Level has started to Rise again.

17
Q

State the Global Average Sea Rise per Year.

18
Q

State the 2 types of Coastal Landforms created by Sea Level Changes.

A

-Emergent
-Submergent

19
Q

Define Emergent Landforms.

A

Landforms that arise from Sea Level Falling and Isostatic Rebound.

20
Q

State 2 types of Emergent Landforms.

A

-Raised Beaches
-Fossil Cliffs

21
Q

Explain the Formation and Characteristics of a Raised Beach. (4)

A

-Realtive Sea-Level Rise Primarily due to Isostatic Rebound.
-Beaches are raised above the High Tide Mark.
-They Experience Succession by Vegetation due to no more Erosion occuring from the Sea.
-Raised Beaches also expose Marine Platforms and Erosional Landforms like Caves etc.

22
Q

Cliffs behind Raised Beaches can also be called…?

A

Relict Cliffs.

23
Q

Explain the Formation of a Fossil Cliff. (4)

A

-Isostatic Rebound or Eustatic Change causes Sea Level to rise.
-This exposes the Retreated Wave-Cut Platforms/Notches.
-Erosion stops as the Cliff is too High above Sea Level.
-Cliff loses its Jagged Profile as Vegetation and Soils develop.

24
Q

State a UK Example of a Raised Beach.

A

Corbyn’s Head, Torquay, Devon

25
State a UK EXample of a Fossil Cliff
Lyme Regis, Dorset
26
Define Submergent Features.
Landforms created by a Rise in Sea Level that Floods the Coast.
27
State 3 types of Submergent Landforms.
-Fjords -Dalmation Coasts -Rias
28
Explain the Formation and Characteristics of a Fjord. (6)
-Formed due to Eustatic Change. -River carves a V-Shaped Valley into the Landscape. -During an Ice-Age, a Glacier moves through the Valley eroding it via Plucking and Abrasion to create a U-Shaped Valley. -Global Warming causes Glacial Melt and Retreat Inland. -Due to the Glacier eroding the Valley below Sea Level, the Valley is Flooded creating a Fjord. -Fjords are Narrow with Steep Sides.
29
State an Example of a Fjord in Norway.
Sognefjord which is over 1000m Deep.
30
Explain the Formation of a Dalmation Coast.
Eustatic Change Floods Valleys that lie Parallel to the Coast leaving Islands.
31
State an Example of a Dalmation Coast in Croatia.
The Dalmation Coast, Croatia.
32
Explain the Formation of Rias. (2)
-Eustatic Change partially floods a V-Shaped River Valley. -They're Wide and Deep at the Mouth , becoming Narrower and Shallower the Further Inland they Travel.
33
State an UK Example of a Ria.
Milford Haven, Pembrokeshire, Wales
34
State 2 Stats that highlight Potential Impact of Sea Level rise on Humans.
-75% of the World's Cities are Coastal. -More than 1 Billion People live on High Risk Coasts.
35
State and Explain 4 Impacts of Sea Level Rise on Coastal Areas.
-Storms increasing in Magnitude and Frequency due to Changes in Ocean Temperatures. -Submergence of Low-Lying Coastal Towns/Islands. -Contamination of Water Sources on Farmland can Increase Salinity which can dammage crops and make Land Infertile. -Increased Rates of Coastal Erosion putting Ecosystems, Homes and Buisnesses at Risk.
36
State the Potential Sea Level Rise Depth if the Earth's Ice Sheets Melt.
72m.
37
State 2 Adverse Effects of Climate Change on the UK Coastline.
-Major Transport and Energy Infrastructure is Situated near the Coast on Low-Lying Ground. -High-Grade Agricultural Land and Cities like London are at Risk from Coastal Flooding in the Long-term.