What makes an earthquake hazardous, and how can the risk be reduced?
Earthquake hazards, risk and mitigation: the primary and secondary hazards of earthquakes (ground shaking, liquefaction, landslides, tsunami, fire); the distinction between hazard, vulnerability, exposure and risk; the factors controlling the severity of impact; and the prediction, monitoring and mitigation strategies (building design, hazard mapping, early warning and planning).
A focused answer to the Eduqas Geology geohazards statement on earthquakes. Covers primary and secondary earthquake hazards, the distinction between hazard, vulnerability, exposure and risk, the controls on severity, and the prediction, monitoring and mitigation strategies that reduce impact.
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What this dot point is asking
This is part of the Geohazards theme examined in Component 3. Eduqas wants you to distinguish the primary and secondary hazards of earthquakes, to define and relate hazard, vulnerability, exposure and risk, to explain the controls on the severity of impact, and to describe prediction, monitoring and mitigation strategies. It applies the earthquake science (seismic waves, magnitude and intensity) to the human consequences and how to reduce them.
The answer
Primary and secondary hazards
The primary hazard of an earthquake is the ground shaking produced directly by the seismic waves, which damages and collapses buildings, bridges and infrastructure. The secondary hazards are triggered by that shaking:
- Liquefaction: saturated, loose, fine sediment loses its strength when shaken and behaves like a liquid, so buildings sink, tilt or topple and buried tanks float upwards.
- Landslides and rockfalls on slopes, which can bury settlements and dam rivers.
- Tsunami: if the sea floor is suddenly displaced (by a submarine fault or landslide), a series of long-wavelength ocean waves is generated.
- Fires: ruptured gas mains and power lines ignite fires that are hard to fight when water mains are also broken.
The secondary hazards often cause more deaths than the shaking itself (for example tsunami).
Hazard, vulnerability, exposure and risk
These four terms are precise and frequently tested:
Controls on the severity of impact
For a given magnitude, the damage varies enormously depending on:
- Focal depth: shallow-focus earthquakes do far more surface damage than deep ones.
- Distance from the epicentre: intensity falls with distance.
- Local ground conditions: soft, saturated sediment amplifies shaking and can liquefy, while hard bedrock shakes less.
- Building design and quality: engineered, reinforced structures survive where unreinforced masonry collapses.
- Population density, time of day and preparedness: a dense, unprepared population suffers more casualties.
This is why a large earthquake in a well-prepared region can cause fewer deaths than a smaller one in a poorly built, densely populated region.
Prediction, monitoring and mitigation
Earthquakes cannot yet be predicted precisely in time, but the hazard can be managed:
- Monitoring: seismometers, GPS measurement of crustal strain, and historical records identify active faults and recurrence intervals.
- Hazard mapping and land-use planning: maps of fault zones and liquefaction-prone ground steer development away from the worst sites, reducing exposure.
- Earthquake-resistant design: flexible frames, cross-bracing, base isolation and tying walls to frames reduce vulnerability.
- Early-warning systems: detecting the fast P wave gives seconds of warning before the damaging surface waves, enough to stop trains and shut off gas.
- Education, drills and emergency planning: prepare the population and the response.
Examples in context
Example 1. Liquefaction damage. In earthquakes affecting cities built on reclaimed or river-delta sediment, liquefaction tilts and sinks well-built structures whose foundations were sound, showing that ground conditions can outweigh building quality.
Example 2. Early warning saving seconds. Systems that detect the fast P wave and broadcast an alert before the slower surface waves arrive give enough time to halt high-speed trains and shut off gas, reducing secondary hazards even though the earthquake itself was not predicted.
Try this
Q1. State one primary and two secondary hazards of an earthquake. [3 marks]
- Cue. Primary: ground shaking. Secondary (any two): liquefaction, landslides, tsunami, fire.
Q2. Explain the difference between hazard and risk. [2 marks]
- Cue. The hazard is the natural event with the potential to harm; risk is the likelihood of harmful consequences, which also depends on exposure and vulnerability.
Q3. Describe one mitigation strategy that reduces vulnerability and one that reduces exposure. [2 marks]
- Cue. Reduce vulnerability with earthquake-resistant building design; reduce exposure with hazard mapping and land-use planning that keeps development off the worst ground.
Exam-style practice questions
Practice questions written in the style of WJEC Eduqas exam questions on this dot point, with worked answer explainers. The year tag is the paper they imitate, not the source.
Eduqas 20196 marksDistinguish between the primary and secondary hazards of an earthquake, and explain why two earthquakes of the same magnitude can cause very different levels of damage.Show worked answer →
A levels-of-response answer; separate the hazard types, then explain the variable impact.
- Primary hazard
- The primary hazard is the ground shaking caused directly by the seismic waves, which damages and collapses buildings and infrastructure.
- Secondary hazards
- These are triggered by the shaking: liquefaction (saturated loose sediment loses strength and behaves like a liquid, so foundations sink and tilt), landslides on slopes, tsunami if the sea floor is displaced, and fires from ruptured gas and power lines.
- Why damage varies
- For the same magnitude, the impact depends on the depth of focus (shallow focus does more surface damage), the distance from the epicentre, the local ground (soft saturated sediment amplifies shaking and can liquefy, hard bedrock shakes less), the building design and quality (engineered versus unreinforced), the population density and time of day, and the level of preparedness.
Top-band answers separate the direct shaking (primary) from the triggered secondary hazards, and give several valid reasons (focal depth, ground conditions, building quality, preparedness) for the variable damage.
Eduqas 20215 marksExplain the difference between hazard, vulnerability and risk, and describe two mitigation strategies that reduce earthquake risk.Show worked answer →
Define the terms, then give mitigation linked to them.
- Hazard
- The natural process or event with the potential to cause harm (here the earthquake and its shaking).
- Vulnerability
- How susceptible the people and structures are to harm (for example poorly built housing, an unprepared population), with exposure being the number of people and assets in the hazard zone.
- Risk
- The likelihood of harmful consequences, combining the hazard with the exposure and vulnerability. Risk can be reduced by lowering vulnerability or exposure even though the hazard itself cannot be removed.
- Mitigation (any two)
- Earthquake-resistant building design (flexible frames, cross-bracing, base isolation, tying walls to frames) reduces vulnerability. Hazard mapping and land-use planning keep development off the worst ground (avoiding liquefaction-prone or fault-zone sites), reducing exposure. Early-warning systems, drills and education reduce casualties.
Markers reward correct definitions (hazard the process, vulnerability susceptibility, risk the combined likelihood of harm) and two valid mitigation measures linked to reducing vulnerability or exposure.
Related dot points
- Earthquakes and seismic waves: the focus and epicentre; the elastic rebound mechanism; the P, S and surface waves and their properties; the difference between magnitude (the logarithmic Richter scale and its saturation, and the moment magnitude scale) and intensity (the Modified Mercalli scale); the use of P and S wave arrival times and travel-time graphs to locate an epicentre by triangulation.
A focused answer to the Eduqas Geology statement on earthquakes. Covers the focus and epicentre, the elastic rebound mechanism, P, S and surface waves and their properties, the difference between magnitude (Richter saturation and moment magnitude) and intensity (Modified Mercalli), a worked example using the P-S travel-time gap, and how triangulation from three stations locates an epicentre.
- Volcanic hazards and monitoring: the primary and secondary hazards of volcanic eruptions (lava flows, pyroclastic flows, tephra and ash fall, lahars, gases, sector collapse); the control of magma composition on eruption style and hazard; and the monitoring and prediction methods (seismicity, ground deformation, gas emissions, thermal and historical records) used to forecast eruptions.
A focused answer to the Eduqas Geology geohazards statement on volcanoes. Covers primary and secondary volcanic hazards, how magma composition controls eruption style and hazard, and the monitoring methods (seismicity, ground deformation, gas, thermal) used to forecast eruptions and reduce risk.
- Mass movement and landslide hazards: the types of mass movement (rockfall, slide, slump, flow and creep); the factors controlling slope stability (slope angle, rock and soil strength, water, bedding orientation, vegetation and undercutting); the triggers of slope failure; and the engineering and planning methods used to reduce landslide hazards.
A focused answer to the Eduqas Geology geohazards statement on mass movement. Covers the types of mass movement, the factors controlling slope stability, the triggers of slope failure, and the engineering and planning methods used to reduce landslide hazards.
- Plate margins and their features: the processes and characteristic features of constructive (divergent), destructive (convergent) and conservative (transform) margins; the sub-types of destructive margin (ocean-ocean island arcs, ocean-continent margins and continent-continent collision); the Benioff zone, subduction and decompression melting; the diagnostic rocks, structures, earthquakes and volcanoes of each margin type.
A focused answer to the Eduqas Geology statement on plate margins. Covers constructive (divergent), destructive (convergent) and conservative (transform) margins, the ocean-ocean, ocean-continent and continent-continent sub-types, the Benioff zone, subduction and decompression melting, and the diagnostic rocks, structures, earthquakes and volcanoes that identify each margin in the exam.
- Groundwater, aquifers and hydrogeology: the storage and movement of water in rocks; porosity and permeability; aquifers, aquicludes and the water table; artesian conditions; Darcy's law for groundwater flow; and the practical issues of abstraction, recharge, over-abstraction and groundwater pollution.
A focused answer to the Eduqas Geology statement on groundwater. Covers the storage and movement of water in rocks, porosity and permeability, aquifers, aquicludes and the water table, artesian conditions, Darcy's law for groundwater flow, and the issues of abstraction, recharge and pollution.
Sources & how we know this
- Eduqas A Level Geology Specification (A220QS) — Eduqas (2017)