AQA A-Level Geography 7037
Water and Carbon Cycles
Hot Desert Systems and LandscapesLandscape
Coastal Systems and LandscapesLandscape
Glacial Systems and LandscapesLandscape
HazardsHazards or ecosystems
Ecosystems Under StressHazards or ecosystems
Global Systems and Global Governance
Changing Places
Contemporary Urban EnvironmentsHuman option
Population and the EnvironmentHuman option
Resource SecurityHuman option
Coastal Systems and Landscapes
Sea Level Change and Coastlines of Submergence
- 5 things to know
- Component 1
Overview
Recall questions on eustatic change through thermal expansion, ice sheets and glaciers, isostatic change and rebound, tectonic change, sea level since the last glacial maximum, coastlines of submergence and emergence, and rias, fjords and Dalmatian coasts.
What you need to know
Answer each one before you reveal it.
How much lower was global sea level at the end of the last glacial maximum compared to present?
Describe the pattern of sea level change since the last glacial maximum.
What is a coastline of emergence?
Describe sea level change since the last glacial maximum and the coastlines it produced.
Questions from this subtopic
Each one with the model answer underneath.
- 1
Define eustatic sea level change.
Model answer
A global change in sea level caused by changes in the volume of water in the oceans.
- 2
How does thermal expansion contribute to eustatic sea level change?
Model answer
As ocean water warms, it expands in volume, raising global sea level.
- 3
How do ice sheets affect eustatic sea level?
Model answer
Melting ice sheets add water to the oceans, raising sea level; growing ice sheets store water, lowering sea level.
- 4
What role do glaciers play in eustatic sea level change?
Model answer
Melting glaciers release stored water into the oceans; growing glaciers remove water from the oceans.
- 5
Define isostatic sea level change.
Model answer
A local or regional change in sea level caused by vertical movement of the land itself.
- 6
What is isostatic rebound?
Model answer
The rising of land after the weight of ice sheets is removed following deglaciation.
Other ways to work this
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