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OCR GCSE Geography B · J384
OCR J384 · 1.2b Check the specification (PDF) (opens in a new tab)
In April 2015, a magnitude struck Nepal, a landlocked country between India and China. Its was approximately , in the Gorkha district. Around and more than .
An earthquake is a physical event, but the scale of the disaster also depends on the people and buildings exposed to it and their ability to cope. Nepal had limited financial resources, and in 2015 about 80% of its population lived in rural communities, many of them remote. This made reaching survivors and supplying aid difficult.
Nepal lies at a collision boundary between the Indian and Eurasian plates. As the plates move towards one another, the crust is compressed. Movement is not always smooth: friction can prevent rocks from moving while stress builds. When rocks suddenly slip along a fault, stored energy is released as seismic waves, causing the ground to shake.
The earthquake began at a shallow focus, approximately 15 km beneath the surface. A shallow focus means that seismic waves travel a relatively short distance before reaching the surface, helping explain the damaging shaking. More than 300 aftershocks followed, creating further danger for survivors and rescuers.
Plate movement caused the earthquake; shaking produced both direct damage and further hazards.
Plate movement explains why the earthquake occurred. It does not, on its own, explain the death toll. Building vulnerability also mattered: the Dharahara Tower in Kathmandu, which had not been retrofitted to improve its earthquake resistance, collapsed.
Primary effects resulted directly from the shaking. Buildings collapsed, killing and injuring people and leaving almost 3.5 million people homeless. Approximately 7,000 schools and 1,000 health facilities were damaged or destroyed. Electricity and water supplies were cut.
These losses affected more than buildings. Damaged health facilities reduced access to treatment when large numbers of people needed medical help. Damage to schools disrupted education, while the destruction of offices, shops and factories prevented people from earning a living.
Many temples and UNESCO World Heritage sites were also destroyed. This was both a cultural loss and an economic problem because Nepal relied on income from tourism.
Secondary effects were triggered by the earthquake or developed from its initial damage. Shaking triggered avalanches on Mount Everest and in the Langtang Valley, as well as landslides that blocked roads and rivers.
Blocked roads made an already difficult relief operation harder: supplies and rescue teams could not easily reach isolated communities. The combination of damaged tourist attractions and disruption to mountain tourism reduced tourist income, affecting livelihoods beyond the places where buildings had collapsed.
Damage was estimated at US$7–10 billion, around 35% of Nepal's GDP. GDP measures the value of goods and services produced in a country in a year. This comparison shows the enormous scale of the damage relative to Nepal's economy, helping explain why international assistance was important.
The first priority was to find survivors, treat injuries and provide shelter and supplies. Around 90% of the Nepalese army was mobilised. Other countries sent search-and-rescue teams, medical staff, medicines, food, water, clothing and temporary shelters.
Tent cities in Kathmandu provided temporary accommodation for people whose homes were unsafe or destroyed. A GIS crisis-mapping tool helped coordinate the response by organising location-based information. This supported decisions about where assistance was needed.
The Asian Development Bank provided a US$3 million emergency relief grant. Emergency relief addressed urgent needs; it could not replace all the homes, services and livelihoods that had been lost.
Recovery involved restoring access and essential services. Landslides were cleared and roads repaired so that remote rural communities could be reached again. Schools were rebuilt, and the Asian Development Bank provided US$200 million for rebuilding.
Other responses aimed to reduce the consequences of future earthquakes. Stricter building codes and stronger enforcement sought to improve building safety. Earthquake drills taught people what to do during an earthquake, and a new government task force was established to plan for future events.
These measures could not stop the Indian and Eurasian plates moving. Their purpose was to make people and buildings less vulnerable. Nepal therefore illustrates the connection between a physical hazard, social and economic vulnerability, emergency relief and longer-term risk reduction.
Immediate: 90% of the army mobilised; international rescue teams and supplies; Kathmandu tent cities; GIS crisis mapping; US$3 million Asian Development Bank emergency grant.
Long-term: roads cleared and repaired; schools rebuilt; US$200 million Asian Development Bank rebuilding support; stricter building codes and enforcement; earthquake drills; government planning task force.
Use Nepal-specific evidence to support explanations, rather than listing facts without showing why they matter.
Distinguish the physical cause of the earthquake from factors that increased its consequences, such as vulnerable buildings and difficult access to remote settlements.
Magnitude describes earthquake size; it is not the same as intensity, which describes shaking and its effects at a particular location.
Separate immediate relief from long-term recovery, and explain what each response achieved.
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Tectonic hazard
An event caused by movement of the Earth's crust that threatens people, property or livelihoods.
Collision boundary
A plate boundary where two continental plates move towards one another, compressing and deforming the crust.
Focus
The point within the Earth where an earthquake begins.
Epicentre
The point on the Earth's surface directly above an earthquake's focus.
Magnitude
A measure of the size of an earthquake, related to the energy released.
Aftershock
A smaller earthquake that follows the main earthquake in the affected region.
Primary effect
An effect caused directly by the earthquake's shaking, such as the collapse of a building.
Secondary effect
An effect triggered by the earthquake or resulting from its initial damage, such as a landslide or loss of tourist income.
Put your knowledge into practice — try past paper questions for Geography B
Tectonic hazard
An event caused by movement of the Earth's crust that threatens people, property or livelihoods.
Collision boundary
A plate boundary where two continental plates move towards one another, compressing and deforming the crust.
Focus
The point within the Earth where an earthquake begins.
Epicentre
The point on the Earth's surface directly above an earthquake's focus.
Magnitude
A measure of the size of an earthquake, related to the energy released.
Aftershock
A smaller earthquake that follows the main earthquake in the affected region.
Primary effect
An effect caused directly by the earthquake's shaking, such as the collapse of a building.
Secondary effect
An effect triggered by the earthquake or resulting from its initial damage, such as a landslide or loss of tourist income.