State the 2 types of Sea Level Change.
-Isostatic
-Eustatic
Define Eustatic Change.
A Sea Level Change caused by a Change in the Volume of Water or a Change in the Shape of Ocean Basins.
State whether Eustatic Change is Local or Global.
Global.
State the 3 Factors that influence Eustatic Change.
-Thermal Expansion
-Tectonic Movement
-Ice Sheet Melt
Explain the Impact of Thermal Expansion on Eustatic Change.
As Ocean Temperatures increase, Water Expands which increases the Volume of Water in the Ocean.
Explain the Impact of Tectonic Movement on Eustatic Change. (3)
-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.
Explain the Impacts of Ice Sheet Melt on Eustatic Change.
Global Warming has increased Ocean and Atmospheric Temperatures causing Ice Sheets to Melt and hence Sea Levels have Risen.
Define Isostatic Change.
Sea Level Change caused by Vertical Movements of the Land Relative to the Sea.
State 4 Factors that influence Isostatic Change.
-Post-Glacial Adjustment
-Accretion
-Subsidence
-Tectonics
Explain the Impacts of Post-Glacial Adjustment on Isostatic Change. (2)
-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.
Explain the Impact of Accretion on Isostatic Change.
Acccretion is where there is Net Deposition of Sediment causing Land to Fall realtive to the Sea Level.
Explain the Impact of Subsidence on Isostatic Change.
Subsidence of Land is caused by Excess Groundwater Extraction such as the Drainage of Marshland.
Explain the Impact of Tectonics on Isostatic Change.
Volcanism releases Lava and Ash causing Land to Rise Relative to Sea Level.
State how many mm a Year Scotland is Rebounding since the last Ice Age.
1.5mm a Year.
State how many mm a Year Cornwall is Sinking since the last Ice Age.
1.1mm a Year.
Since the last Glacial Maximum 21,000 yrs Ago, How has Sea Level Changed? (3)
-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.
State the Global Average Sea Rise per Year.
2mm.
State the 2 types of Coastal Landforms created by Sea Level Changes.
-Emergent
-Submergent
Define Emergent Landforms.
Landforms that arise from Sea Level Falling and Isostatic Rebound.
State 2 types of Emergent Landforms.
-Raised Beaches
-Fossil Cliffs
Explain the Formation and Characteristics of a Raised Beach. (4)
-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.
Cliffs behind Raised Beaches can also be called…?
Relict Cliffs.
Explain the Formation of a Fossil Cliff. (4)
-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.
State a UK Example of a Raised Beach.
Corbyn’s Head, Torquay, Devon