Hazardous enviroments
HAITI EARTHQUAKE (2010)
LIC (Low-Income Country)
Key Facts:
Date: 12 January 2010
Magnitude: 7.0 on the Richter scale
Epicentre: Near Léogâne, ~25 km from Port-au-Prince (capital)
Depth: 13 km (shallow = more destructive)
Tectonic Setting: Conservative boundary – Caribbean Plate and North American Plate
Impacts:
Primary:
230,000 deaths
300,000+ injured
1.5 million homeless
50% of buildings collapsed in Port-au-Prince (incl. Presidential Palace & UN HQ)
Critical infrastructure destroyed (roads, hospitals, airports)
Secondary:
Cholera outbreak (over 10,000 deaths)
Looting and civil unrest
Over-reliance on international aid
Economy crippled – damage cost estimated at $8 billion
Long-term displacement in refugee camps
Responses:
Short-term:
International aid sent (US, UN, NGOs)
Rescue teams & medical aid flown in
Temporary shelters established
Long-term:
Debris removal and rebuilding projects
Infrastructure slowly rebuilt, but corruption and poor planning slowed progress
International aid continued for years
CHRISTCHURCH EARTHQUAKE (2011)
HIC (High-Income Country)
Key Facts:
Date: 22 February 2011
Magnitude: 6.3 on the Richter scale
Epicentre: Near Lyttelton, ~10 km from Christchurch
Depth: 5 km (very shallow)
Tectonic Setting: Conservative boundary – Pacific Plate and Australian Plate
Impacts:
Primary:
185 deaths
2,000+ injured
Extensive damage to central Christchurch (cathedral collapsed)
50% of buildings in central business district severely damaged or destroyed
Liquefaction affected infrastructure
Secondary:
$40 billion in damage
Ongoing aftershocks caused psychological stress
Economic impact on tourism and education sectors
Insurance claims caused delays in rebuilding
Long-term displacement of residents
Responses:
Short-term:
Rapid emergency services response
National state of emergency declared
International help (Australia, Japan, UK)
Long-term:
Extensive insurance coverage supported rebuilding
New building regulations introduced
Christchurch Rebuild Authority established
Infrastructure and zoning improvements
Key Strengths:
Strong government coordination
High preparedness level (earthquake drills, building codes)
Good communication and access to resources
🔍 Comparison Points between Haiti and Christchuch:
Factor | Haiti (2010) – LIC | Christchurch (2011) – HIC |
|---|---|---|
Economic Capacity | Very limited; reliant on aid | Strong; insured economy, fast response |
Death Toll | Extremely high (230,000) | Lower (185) despite high magnitude impact |
Building Quality | Poor construction, unregulated | Strict building codes in place |
Emergency Response | Slow, chaotic | Fast, organised |
Long-Term Recovery | Still ongoing, hindered by politics | Effective, although costly |
A volcano is an opening in the Earth's surface through which magma (molten rock), gases, and ash escape.
7. Volcano Case Study: Mt. Pinatubo, Philippines (1991)
Date: June 1991
VEI: 6 (Colossal)
Cause: Convergent boundary (Eurasian plate subducting under Philippine plate)
Primary Hazards:
Ash plume reached 34 km into atmosphere
Pyroclastic flows destroyed villages
Secondary Hazards:
Lahars continued for years due to monsoon rains
Global temperatures dropped by 0.5°C due to ash
Impacts:
847 killed, over 1 million displaced
$700 million in damage
Responses:
Early evacuation saved lives
Long-term resettlement and monitoring system improvements
8. Hazard Perception
Wealth: Poorer residents more at risk due to lack of resources to evacuate.
Experience: Locals underestimated risk—eruption was dormant for 600+ years.
Education: Education and science-based communication by USGS helped save lives.
Beliefs: Some indigenous people delayed evacuation due to cultural beliefs.
Mobility: Many in rural areas lacked transport to evacuate quickly.
Volcano-Eyjafjallajökull Eruption, Iceland – 2011
Type of Hazard:
Volcanic eruption (stratovolcano)
Lava, ash cloud, and glacial melt causing flooding
Background:
Location: Southern Iceland, on the Mid-Atlantic Ridge (constructive plate boundary)
Type of volcano: Stratovolcano beneath a glacier
Eruption Date: Major event in April 2010, but volcanic activity continued into 2011
Impacts:
Environmental:
Ash cloud ejected 9 km into the atmosphere
Flooding from glacial melt (jökulhlaup)
Ash fall affected farmland and air quality
Social:
No fatalities, but significant disruption to daily life
500 people evacuated from rural areas
Economic:
Estimated cost to the aviation industry: $1.7 billion
Over 100,000 flights cancelled across Europe
Affected global supply chains (e.g., Kenya’s flower exports)
Management & Response:
Real-time monitoring by the Icelandic Meteorological Office
Airspace closed proactively (EU coordination)
Use of satellite and seismic monitoring
Effective communication through social and mainstream media
Volcanic gas Lake Nyos Disaster, Cameroon – 1986
Type of Hazard:
Limnic eruption (CO₂ gas burst from lake)
Rare gas-based geophysical disaster
Background:
Location: Northwest Cameroon
Volcanic crater lake overlying magma, slowly accumulating CO₂
Date of event: August 21, 1986
Trigger: Possibly a landslide or overturn from heavy rain
Impacts:
Environmental:
Release of ~1.6 million tonnes of CO₂
Suffocated livestock and vegetation over a wide area
Social:
1,746 people killed in surrounding villages
3,500 livestock dead
Survivors suffered trauma and respiratory issues
Economic:
Collapse of local agriculture
Displacement of rural communities
Long-term socio-economic impacts due to fear and relocation
Management & Response:
International scientific response (USGS, French experts)
Degassing project started: Pipes installed to release CO₂ gradually
Education programs for local communities
🌪 tropical storm Case Study: Typhoon Haiyan, Philippines (2013)
📍 Location and Background
Typhoon Name: Haiyan (locally called Yolanda)
Date: November 8, 2013
Location: Central Philippines
Category: Category 5 Super Typhoon
Winds: Up to 314 km/h (195 mph)
Storm Surge: Up to 6 meters high
Affected Areas: Primarily Tacloban City, Leyte, Samar, Cebu, and surrounding islands
🌀 Causes of the Typhoon
Warm ocean temperatures over the Pacific (above 26.5°C) provided energy for the storm.
Low wind shear allowed the storm to intensify rapidly.
Coriolis force near the equator enabled the storm to rotate.
High humidity in the atmosphere contributed to storm development.
Climate change may have played a role in increasing sea surface temperatures, intensifying the typhoon.
Primary Impacts
Death toll: Over 6,300 people officially confirmed dead.
Homes destroyed: Over 1.1 million homes.
Storm surge: Caused widespread flooding, especially in Tacloban.
Wind damage: Entire towns flattened, especially coastal communities.
Injuries: Over 28,000 people injured.
Power and communications down across many islands.
Agriculture destroyed: Rice and sugarcane fields wiped out.
Secondary Impacts
Disease outbreaks due to contaminated water (e.g., cholera, dysentery).
Looting and civil unrest in affected areas.
Displacement: Over 4 million people left homeless.
Livelihoods lost: Especially in farming and fishing communities.
Long-term economic damage: Estimated at $5.8 billion USD.
Infrastructure damage delayed aid and rescue efforts.
Increased poverty due to job losses and destruction of property.
📊 Key Statistics for Typhoon Haiyan
Metric | Data |
|---|---|
Date | November 8, 2013 |
Wind Speed | 314 km/h |
Storm Surge Height | Up to 6 meters |
Death Toll | ~6,300 |
People Affected | 14 million |
Homes Damaged/Destroyed | 1.1 million |
Economic Damage | $5.8 billion USD |
Displaced Persons | 4.1 million |
🆘 Responses
Short-term (Immediate):
Evacuation centers set up in safer areas.
International aid sent (e.g., USA, UK, UN).
UK sent £77 million and the HMS Illustrious carrier with supplies.
Emergency supplies: food, water, and medicine distributed.
Search and rescue teams deployed.
Long-term:
"Build Back Better" policy introduced by the Philippine government.
New storm shelters built and planning regulations improved.
Replanting of mangroves to buffer future storm surges.
Aid from NGOs like Red Cross helped rebuild homes and infrastructure.
Education on disaster preparedness improved in schools and communities.
Hurricane Case Study: Hurricane Katrina, USA (2005)
Location: Gulf Coast (Louisiana, Mississippi)
Magnitude: Category 5; landfall as Category 3
Impacts:
Social: 1,833 deaths, 1 million displaced
Economic: $125 billion in damages
Environmental: Levee failure, flooding of New Orleans
Political: Criticism of FEMA and federal response
Response:
Slow, inadequate evacuation; poor coordination
Rebuilding led to gentrification and community displacement
8. Hazard Perception
Wealth: Poor communities affected most
Experience: Previous storms didn’t prepare residents for scale
Education: Risk miscommunication
Beliefs: Distrust in government delayed evacuation
Tornado Case Study: Joplin Tornado, Missouri (2011)
Date: May 22, 2011
EF Rating: EF5 with winds > 320 km/h
Impacts:
Social: 158 deaths, over 1,100 injured
Economic: $2.8 billion in damage, 7,000 homes destroyed
Environmental: Debris scattered for miles
Political: Declared federal disaster; highlighted need for improved emergency response
Response:
Emergency shelters activated, federal aid mobilized quickly
Criticism of siren delay and lack of warning comprehension by public
8. Hazard Perception
Wealth: Determines shelter availability
Experience: Frequent tornadoes may lead to underestimation of risk
Education: Affects comprehension of warnings
Mobility: Elderly/disabled more vulnerable
Case Study Mass movement: Vargas Tragedy, Venezuela (1999)
Date: December 1999
Trigger: 911 mm of rainfall in a few days
Type: Debris flows, landslides down coastal mountains
Impacts:
Social: Over 30,000 deaths, 75,000 homeless
Economic: Billions in damages, loss of infrastructure
Environmental: River channels changed, massive sediment deposition
Political: Criticism of urban development policies and lack of early warning
Response:
Military aid, emergency housing
Long-term resettlement efforts faced challenges
8. Hazard Perception
Wealth: Poorer communities often located on unstable slopes
Experience: Lack of memory or records led to poor preparedness
Education: Residents unaware of early warning signs
Mobility: Steep, informal settlements hindered evacuation
Bohol Earthquake, Philippines (2013)
Location and Date
Epicenter: Near Carmen, Bohol Island, Central Visayas region, Philippines
Date: October 15, 2013
Magnitude: 7.2 on the Richter scale
Depth: 12 km (shallow-focus quake)
Causes
Tectonic setting: The Philippines lies on the Pacific Ring of Fire, a zone of frequent seismic activity.
The earthquake was caused by movement along a previously unknown fault line (North Bohol Fault).
It was a reverse fault movement (compressional stress)—typical of convergent boundaries.
The Philippines is situated between the Eurasian Plate and the Philippine Sea Plate.
Primary Impacts:
Deaths: Over 220 people killed
Injured: Around 1,000
Displaced: Over 340,000 people
Homes destroyed: Over 73,000 structures damaged, including 14,500 totally collapsed
Historical heritage sites were badly affected (e.g., Loboc and Baclayon churches—centuries-old Spanish colonial buildings)
Secondary Impacts:
Landslides blocked roads and isolated communities
Disruption of power and communication
Water shortages due to damaged infrastructure
Tourism declined—many tourists evacuated the area
Responses
Short-term:
State of Calamity declared in Bohol and Cebu
Emergency relief from the Philippine government and international NGOs (e.g., Red Cross, UN)
Temporary shelters set up for displaced populations
Medical assistance and food distribution coordinated
Military helicopters used for aid in remote areas
Long-term:
Infrastructure rehabilitation (roads, bridges, schools)
Disaster risk reduction programs strengthened (e.g., Earthquake drills, early warning systems)
Geo-hazard mapping improved to identify unknown faults
Community education on emergency preparedness
Evaluation
Despite the magnitude, the death toll was relatively low compared to similar quakes, thanks in part to:
It occurring in the morning when people were awake
Rapid emergency response and coordination
Improved disaster management systems post-2009 typhoons
Challenges included reaching isolated rural areas, especially due to landslides and damaged bridges.