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NotesGeographyTopic 10.2Volcanic and mass-movement hazards
Back to Geography Topics
10.2.28 min read

Volcanic and mass-movement hazards

IB Geography • Unit 10

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Contents

  • Volcanic and mass-movement hazards
  • Reading the distribution of events
  • Why some events are far deadlier - real cases
  • The [10] essay - severity and human well-being
The big idea: A volcanic hazard is any threat from a volcano - lava flows, pyroclastic flows (fast clouds of hot gas and ash), ashfall (tephra), lahars (volcanic mudflows) and toxic gases.

A mass movement is the downslope movement of rock, soil or debris under gravity - rockfalls, landslides, debris flows and slumps. Volcanic eruptions and earthquakes often trigger mass movements, so the two hazards are closely linked.

Reading a hazard map or distribution diagram - lava thickness, ash depth, or the slope angles where slides cluster - is a core Option D skill.

Key terms for this hazard

  • Lava flow - molten rock that flows downhill; slow, so it destroys property but rarely kills.
  • Pyroclastic flow - a fast, super-hot cloud of gas and ash; the deadliest volcanic hazard.
  • Lahar - a volcanic mudflow of ash and water that races down valleys, burying settlements.
  • Tephra / ashfall - fragments thrown out by an eruption; collapses roofs and ruins farmland.
  • Mass movement - downslope movement of rock/soil/debris under gravity.
  • Trigger - the event that sets a slope failing (heavy rain, an earthquake, undercutting, an eruption).
Slow vs fast = deadly or not: Slow hazards (most lava flows, slumps) give people time to escape - they wreck property but kill few.

Fast hazards (pyroclastic flows, lahars, debris flows, sudden landslides) strike with no warning - these cause the mass casualties. Speed, not size, often decides the death toll.

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How this is tested: The stimulus here is usually a shaded hazard map (lava-flow thickness, ashfall depth) or a distribution diagram - a dot diagram of mass movements by altitude and slope, or a triangular graph of movement types. The data marks ask you to State a value (the thickness band covering the most area, a line of longitude), Estimate a count or a ground distance off the scale, or Identify the modal class - the band with the most events. Always read the key or scale first and quote the units.

Read the key first. Which shaded band is darkest (thickest lava) and which is lightest (thinnest)?

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IB-style questionState[2 marks]

Using the lava-thickness map above: (a) state the thickness band that covers the greatest area of lava; (b) estimate the difference in thickness between the thickest and thinnest mapped areas.

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Slope angle bandRockfallsLandslidesDebris flowsTotal events
0-9 degrees0123
10-19 degrees14611
20-29 degrees59822
30-39 degrees127423
40 degrees and over142117
Identify the modal class; count above a threshold: Identify = name the band with the most events (the tallest bar or densest dot cluster). Estimate / Count = add up the events above a threshold line (e.g. all events on slopes of 30 degrees or steeper). Read carefully - one band, or a running total, not the whole dataset.
IB-style questionIdentify[3 marks]

Using the slope table above: (a) identify the slope band with the most mass-movement events; (b) estimate how many events occurred on slopes of 30 degrees or steeper; (c) state the most common type of event on the steepest slopes.

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Real hazard maps work the same way: After Kilauea's 2018 eruption in Hawaii, scientists mapped lava-flow thickness in bands across the lower slopes - you read off which thickness band covers the most ground, or which line of longitude the flow sits near. The same skill reads an ashfall depth map or a lahar inundation map - find the modal band, measure a distance off the scale.

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The severity of a volcanic or mass-movement hazard depends on its type and speed, the warning time, and how vulnerable the people in its path are. A slow lava flow and a fast pyroclastic flow are both volcanic - but their impact on human well-being is worlds apart.

ControlLess severeMore severe
Speed of the hazardSlow lava flow - people escapePyroclastic flow / lahar - no escape
Warning timeMonitored volcano, evacuationSudden landslide, no warning
Population densityRemote slope, few peopleDense settlement on the slope
Vulnerability / wealthStrong buildings, response planWeak housing, poor emergency services
Time of dayDaytime, people alertNight, people asleep indoors

Named events to quote

  • Nevado del Ruiz, Colombia (1985) - a small eruption melted the summit ice and sent lahars down the valleys; the town of Armero was buried and around 23,000 people died, despite warnings that were not acted on.
  • Eyjafjallajokull, Iceland (2010) - a moderate eruption killed nobody, but its ash cloud grounded European flights for days - a huge economic impact with almost no death toll.
  • Haiti earthquake (2010) - the quake triggered widespread landslides on deforested slopes; over 200,000 people died, worsened by weak buildings and deep poverty (high vulnerability).
  • Tohoku, Japan (2011) - an offshore quake and tsunami triggered coastal landslides; strong building codes and warnings limited deaths compared with the wave, showing how preparedness lowers severity.
IB-style questionExplain[4 marks]

Explain why a pyroclastic flow usually causes far more deaths than a lava flow from the same volcano.

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Always tie severity to a cause: Don't just say one event was 'worse'. Explain why - fast + no warning + dense, poor population = high deaths (Nevado del Ruiz); slow + monitored + remote = low deaths. Severity is type plus vulnerability.
How this is tested - the [10] Examine essay: Paper 1 Option D ends with a 10-mark Examine essay, marked on markbands. The recurring version asks how severely different types of mass movement (or volcanic hazard) affect human well-being - across social, health and economic impacts, and how that severity varies over space and time.

Top band needs: accurate terms, two or more types of event developed with named examples and data, a weighing of how and why severity differs, and a clear judgement.
IB-style questionExamine[10 marks]

Examine how severely different types of mass movement affect human well-being.

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IB Exam Questions on Volcanic and mass-movement hazards

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How Volcanic and mass-movement hazards Appears in IB Exams

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Define

Give the precise meaning of key terms related to Volcanic and mass-movement hazards.

AO1
Describe

Give a detailed account of processes or features in Volcanic and mass-movement hazards.

AO2
Explain

Give reasons WHY — cause and effect within Volcanic and mass-movement hazards.

AO3
Evaluate

Weigh strengths AND limitations of approaches in Volcanic and mass-movement hazards.

AO3
Discuss

Present arguments FOR and AGAINST with a balanced conclusion.

AO3

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Related Geography Topics

Continue learning with these related topics from the same unit:

10.1.1Plate tectonics, earthquakes and volcanoes
10.1.2Mass movement processes
10.2.1Earthquake and tsunami hazards
10.3.1Hazard risk and vulnerability
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