How can the impacts of tectonic hazards be managed and reduced?
How tectonic hazards are managed using the hazard management cycle, the Park model, prediction and monitoring, mitigation and preparedness at local, national and international scales.
An Edexcel A-Level Geography answer to how tectonic hazards are managed, covering the hazard management cycle, the Park disaster response model, prediction and monitoring, mitigation and preparedness across scales using Japan, Haiti, Iceland and the Indian Ocean.
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What this dot point is asking
Edexcel wants you to explain how the impacts of tectonic hazards can be reduced through management. You need the hazard management cycle, the Park model (disaster response curve), the role of prediction, forecasting and monitoring, the differences between mitigation and preparedness, and how responses operate at local, national and international scales.
The hazard management cycle and the Park model
The Park model, or disaster response curve, plots quality of life against time. After the hazard strikes, the curve plunges, then climbs back through three phases. Relief covers the first hours and days of search, rescue and emergency aid. Rehabilitation spans weeks to months, restoring water, power and temporary shelter. Reconstruction lasts months to years, rebuilding to a normal or improved standard. The shape is diagnostic: a wealthy, well-prepared place dips less and recovers above its original level, while a poorly governed place stays low for years.
This is why management reduces impacts even though it cannot remove the hazard. In Japan after Tohoku 2011, rapid relief and reconstruction to a higher standard, including raised sea walls, produced a shallow dip and strong recovery. In Haiti 2010, a weak state left relief dependent on NGOs and reconstruction stalled, so the curve stayed depressed.
Prediction, forecasting and monitoring
Prediction differs sharply between hazard types, and that difference drives management strategy.
Eyjafjallajokull, Iceland (2010) shows volcanic monitoring in action: seismicity and deformation flagged the eruption, and though the ash cloud grounded European aviation, monitoring guided the response. The 2004 Indian Ocean tsunami, which had no warning system, directly prompted the Indian Ocean tsunami warning system built on DART technology, showing how disasters feed back into the management cycle.
Mitigation, preparedness and scales of response
Mitigation reduces the long-term risk before any event. Land-use zoning keeps housing off the most dangerous ground. Aseismic building techniques include base isolation (bearings that decouple a building from ground motion), cross-bracing and deep foundations anchored into bedrock. Tsunami walls defend low coasts, and lava diversion has been attempted by building barriers and spraying water, as at Mount Etna.
Preparedness turns warnings into safe action through drills, education and evacuation planning. Responses operate across scales: local councils zone land and run drills; national governments fund warning systems and building codes; international actors such as the UN and NGOs like the Red Cross and Oxfam provide relief and reconstruction aid, which dominated the response in Haiti.
Examples in context
Example 1: Japan, integrated management. Japan layers prediction, mitigation and preparedness. After the Tohoku quake of 11 March 2011, an earthquake early-warning system gave seconds of notice, base-isolated buildings limited shaking deaths, and reconstruction raised sea walls above 14 m in places. The roughly deaths were mostly from the tsunami that overtopped older defences, showing both the success and the limits of engineering.
Example 2: Haiti 2010, NGO-led recovery. The quake on 12 January 2010 killed around people. With a weak state, relief and rehabilitation were led by NGOs and the UN, and reconstruction was slow and uneven, with hundreds of thousands still in camps years later. The Park curve stayed low, illustrating how low capacity to cope lengthens recovery.
Try this
Q1. Explain why volcanic eruptions are easier to manage through evacuation than earthquakes. [4 marks]
- Cue. Volcanoes give monitorable precursors (gas, deformation, seismicity, thermal) enabling timed evacuation; earthquakes give no reliable short-term warning, so management relies on building design and preparedness.
Q2. Outline how the Park model can be used to compare recovery in two countries. [4 marks]
- Cue. Compare the depth of the dip and the final level reached through relief, rehabilitation and reconstruction; link a shallow, high-recovering curve to high capacity to cope, as in Japan versus Haiti.
Exam-style practice questions
Practice questions written in the style of Pearson Edexcel exam questions on this dot point, with worked answer explainers. The year tag is the paper they imitate, not the source.
Edexcel Paper 1 (style)12 marksAssess the relative importance of prediction and preparedness in reducing the impacts of tectonic hazards.Show worked answer →
A strong answer uses AO1 to define prediction (forecasting when and where an event will strike) and preparedness (drills, education, evacuation planning, aseismic building), then uses AO2 to weigh them against named cases. Prediction is uneven: volcanoes are increasingly forecastable through gas, ground deformation and seismicity, shown by Eyjafjallajokull 2010 and monitoring in Iceland, but earthquakes remain unpredictable because seismic gaps and strain only narrow the window, not the date. This is why Japan invests so heavily in preparedness instead, with early warning, drills and base-isolated buildings that limited shaking deaths in Tohoku 2011.
The judgement (AO3) should argue that because earthquake prediction is unreliable, preparedness and mitigation usually save more lives, while for volcanoes prediction enables the evacuations that make preparedness effective. A nuanced conclusion notes the two are complementary: the 2004 Indian Ocean tsunami prompted a DART-based warning system, but warnings only work where preparedness translates them into action.
Edexcel 20198 marksExplain how the Park model can be used to understand recovery from a tectonic disaster.Show worked answer →
AO1 and AO2 dominate. Outline the Park model (the disaster response curve) as a graph of quality of life over time through three phases: relief (hours to days, search, rescue and emergency aid), rehabilitation (weeks to months, restoring services and temporary shelter) and reconstruction (months to years, rebuilding to a normal or improved state).
Apply it. In Japan after Tohoku 2011, a wealthy, well-prepared state moved quickly through relief and reconstructed to a higher standard with raised sea walls, so the curve dipped less and recovered above the original level. In Haiti 2010, weak governance and NGO-led relief left the curve low for years, with reconstruction stalling. Conclude that the steepness and final level of the curve reflect capacity to cope, linking management to development.
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Sources & how we know this
- Pearson Edexcel A-Level Geography (9GE0) specification — Pearson Edexcel (2016)