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
Hazards
Where Vulcanicity Occurs
- 2 things to know
- Component 1
Overview
Recall questions on vulcanicity at constructive and destructive plate margins and why eruptions there are effusive or explosive, on hotspots, magma plumes and the volcanic island chains that record plate movement, and on magma viscosity and eruption style.
What you need to know
Answer each one before you reveal it.
At which type of plate boundary does vulcanicity occur when plates collide and one subducts beneath the other?
Questions from this subtopic
Each one with the model answer underneath.
- 1
At which type of plate boundary does vulcanicity occur when plates move apart?
Model answer
Constructive (divergent) margins
- 2
At which type of plate boundary does vulcanicity occur when plates collide and one subducts beneath the other?
Model answer
Destructive (convergent) margins
- 3
What term describes locations where mantle plumes rise independently of plate boundaries to produce volcanic activity?
Model answer
Hotspots
- 4
Explain why eruptions at constructive margins are typically effusive rather than explosive.
Model answer
Magma rises to fill the gap as plates diverge, producing basaltic lava with low viscosity that allows gases to escape easily, resulting in effusive eruptions
- 5
Why are eruptions at destructive margins typically more explosive than those at constructive margins?
Model answer
Subducting oceanic crust melts to produce magma that is more viscous and gas-rich, trapping gases until pressure causes explosive release; the magma is andesitic or rhyolitic in composition
- 6
How do volcanic chains form at hotspots?
Model answer
Hotspots are stationary plumes of rising magma from deep in the mantle; as the tectonic plate moves over the fixed plume, a chain of volcanoes forms
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