Eduqas A-Level Geography A110QS
Coastal LandscapesLandscape
Glaciated LandscapesLandscape
Changing Places
Water and Carbon Cycles
Global Migration
Global Governance of the Oceans
Tectonic Hazards
EcosystemsContemporary theme
Economic Growth and Challenge: IndiaContemporary theme
Economic Growth and Challenge: ChinaContemporary theme
Development in an African ContextContemporary theme
Energy Challenges and DilemmasContemporary theme
Weather and ClimateContemporary theme
Geographical Skills
Tectonic Hazards
Primary volcanic hazards
- 3 things to know
- Component 3 Section A
Overview
Primary volcanic hazard, pyroclastic flow and lava flows as a hazard.
What you need to know
Answer each one before you reveal it.
What is a pyroclastic flow?
Why are pyroclastic flows the deadliest volcanic hazard?
Questions from this subtopic
Each one with the model answer underneath.
- 1
Define a primary volcanic hazard.
Model answer
A primary volcanic hazard is caused directly by the eruption itself. Lava flows, pyroclastic flows, ash falls, volcanic bombs and gas emissions are all primary hazards.
- 2
What is a pyroclastic flow?
Model answer
A pyroclastic flow is a fast, ground-hugging current of hot gas, ash and rock fragments. Temperatures can exceed 500 °C and speeds commonly pass 100 km h⁻¹.
- 3
Why are pyroclastic flows the deadliest volcanic hazard?
Model answer
A pyroclastic flow is too fast to outrun and kills by heat, asphyxiation and impact. Survival within the path of a flow is almost impossible.
- 4
Give a named example of deaths caused by a pyroclastic flow.
Model answer
Pyroclastic flows from Soufrière Hills on Montserrat killed 19 people on 25 June 1997. The victims had returned to farm inside the exclusion zone.
- 5
Describe lava flows as a hazard.
Model answer
Lava flows destroy everything in their path but usually move slowly enough for people to escape. Basaltic flows travel fastest because they are the least viscous.
- 6
Give an example of an unusually fast lava flow.
Model answer
Nyiragongo in the Democratic Republic of the Congo produces exceptionally fluid, low-silica lava. Flows entering Goma in January 2002 destroyed much of the city centre and killed an estimated 150 people.
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