The big idea: Volcanoes and mass movements are two closely linked hazards: eruptions and earthquakes often trigger mass movements.
Volcanic hazard
- Any threat from a volcano.
- Lava flows, pyroclastic flows (fast clouds of hot gas and ash), ashfall (tephra), lahars (volcanic mudflows) and toxic gases.
Mass movement
- The downslope movement of rock, soil or debris under gravity.
- Rockfalls, landslides, debris flows and slumps.
A core Option D skill: 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.
Kinds of distribution diagram
- A dot diagram of mass movements by altitude and slope.
- A triangular graph of movement types.
What the data marks ask
- State a value (the thickness band covering the most area, a line of longitude).
- Estimate a count or a ground distance off the scale.
- Identify the modal class - the band with the most events.
Read the key first: 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)?
Interactive diagram
Explore the labelled diagram, charts and maps for this topic in full study mode.
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.
Model answer plan
See the answer broken into clear points, with guidance on how each point earns marks.
Recorded mass-movement events by slope angle (mountain valley, 10-year record)
| Slope angle band | Rockfalls | Landslides | Debris flows | Total events |
|---|---|---|---|---|
| 0-9 degrees | 0 | 1 | 2 | 3 |
| 10-19 degrees | 1 | 4 | 6 | 11 |
| 20-29 degrees | 5 | 9 | 8 | 22 |
| 30-39 degrees | 12 | 7 | 4 | 23 |
| 40 degrees and over | 14 | 2 | 1 | 17 |
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.
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.
Model answer plan
See the answer broken into clear points, with guidance on how each point earns marks.
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.
Practice with exam-style questions
Answer exam-style questions and get AI feedback that shows you exactly what examiners want to see in a full-marks response.
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.
Same hazard family, different impact: A slow lava flow and a fast pyroclastic flow are both volcanic - but their impact on human well-being is worlds apart.
Why severity varies between events
| Control | Less severe | More severe |
|---|---|---|
| Speed of the hazard | Slow lava flow - people escape | Pyroclastic flow / lahar - no escape |
| Warning time | Monitored volcano, evacuation | Sudden landslide, no warning |
| Population density | Remote slope, few people | Dense settlement on the slope |
| Vulnerability / wealth | Strong buildings, response plan | Weak housing, poor emergency services |
| Time of day | Daytime, people alert | Night, 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.
A contrasting mass movement: Holbeck Hall, Scarborough (UK, 1993): In June 1993, after a dry spell and then heavy rain, the glacial-till cliff below the Holbeck Hall Hotel slumped towards the sea in a rotational slide. Over several days the hotel's lawn and then part of the building collapsed down the slope. Nobody died: the movement was slow enough for everyone to leave. The cause was water soaking into the clay, raising its weight and lowering its strength, while waves had removed material at the cliff foot.
Vargas, Venezuela (1999)
- Fast debris flow
- Days of torrential rain on steep, deforested slopes
- Dense, poor settlements on the fans below
- A huge death toll; whole towns buried
Holbeck Hall, UK (1993)
- Slow rotational slump
- Rain soaking a clay (till) cliff undercut by waves
- One hotel on the cliff top
- No deaths; property lost; later cliff protection
Explain why a pyroclastic flow usually causes far more deaths than a lava flow from the same volcano.
Model answer plan
See the answer broken into clear points, with guidance on how each point earns marks.
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.
- 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.
- A clear judgement.
Examine how severely different types of mass movement affect human well-being.
Model answer plan
See the answer broken into clear points, with guidance on how each point earns marks.