Key Takeaways: Hazardous Environments (GCSE Geography Revision)
1. Types of Hazards
- Definitions:
- Hazard: Environmental event threatening damage (e.g., earthquakes).
- Natural Disaster: Hazard causing significant destruction (e.g., >10 deaths).
- Categories:GeologicalClimaticBiologicalTechnologicalEarthquakesStormsFiresNuclear explosionsVolcanoesFloodsPestsPollution
Key Rule: Disasters require international criteria (e.g., state of emergency, 100+ injured).
2. Earthquakes
- Causes: Occur at destructive (subduction) and conservative (sliding) plate margins.
- Characteristics:
- Focus: Underground origin.
- Epicentre: Surface point above focus.
- Damage factors: Depth of focus, rock type (soft rocks worsen shaking).
- Measurement:
- Richter Scale: Logarithmic; Energyn=30×Energyn−1Energyn=30×Energyn−1.
- Mercalli Scale: Damage/experience-based (e.g., 5 = objects fall; 10–12 = buildings collapse).
Example: 2011 Tōhoku earthquake (Japan) triggered a tsunami due to undersea focus.
3. Volcanoes
- Distribution: Mostly at plate margins; hotspots (e.g., Hawaii) form within plates.
- Hazards:
- Lava flows (slow-moving but destructive).
- Pyroclastic flows (450 mph, 1000°C).
- Ash clouds (respiratory issues, roof collapses).
- Eruption Types:
- Constructive margins: Gentle eruptions (e.g., Iceland).
- Destructive margins: Violent eruptions (e.g., Mount St. Helens).
Tip: Compare shield vs. composite volcanoes for exam questions.
4. Tropical Storms
- Formation: Requires sea temps >27°C; stages include warm air rising and spiralling winds.
- Characteristics:
- Eye: Calm centre.
- Eyewall: High winds (55–118 km/h).
- Storm surges: Coastal flooding.
- Classification: Saffir-Simpson Scale (Category 5 = >250 km/h winds, catastrophic damage).
Case Studies:
- LIC: Cyclone Nargis (Myanmar, 2008) – 140,000 deaths, poor preparedness.
- HIC: Hurricane Katrina (USA, 2005) – $98bn damage, evacuation failures.
5. Why Live in Hazard Zones?
- Reasons:
- Fertile soils (volcanic ash in Indonesia).
- Economic opportunities (tourism in Iceland).
- Lack of resources to relocate (LICs like Haiti).
- Perceived rarity of disasters.
Example: Naples, Italy, near Mount Vesuvius – high population despite eruption risks.
6. Mitigation Strategies
- Prediction:
- Volcanoes: Monitor earthquakes, gas emissions.
- Earthquakes: Limited warning; focus on building codes (e.g., Japan’s earthquake-proof structures).
- Tropical Storms: Satellite tracking (e.g., NOAA).
- Preparation:
- LICs: Storm shelters, community drills.
- HICs: Levees (New Orleans), early-warning systems.
Exam Tip: Compare prediction (HICs use tech; LICs rely on aid) and preparation (HICs invest in infrastructure).
7. Impacts & Responses
- Primary Effects: Immediate damage (e.g., deaths, destroyed homes).
- Secondary Effects: Long-term consequences (e.g., economic slump, disease).
- Responses:
- Short-term: Emergency aid (e.g., 2004 Asian tsunami – $14bn relief).
- Long-term: Rebuilding (e.g., Banda Aceh’s tsunami warning system).
Case Study: 2004 Asian Tsunami – 230,000 deaths; global aid coordination.
8. Exam Techniques
- Case Studies: Revise one tectonic (e.g., Japan earthquake) and one climatic (e.g., Katrina) event.
- Compare HIC vs. LIC: Use Cyclone Nargis (LIC) and Katrina (HIC) for impacts/responses.
- Math Skills: Calculate population density: Density=PopulationArea (km2)Density=Area (km2)Population.
Top Tips:
- Use PEEL structure (Point, Evidence, Explain, Link).
- For 9-mark questions, include 3 detailed comparisons.
50 GCSE Geography Questions on Hazardous Environments
Section A: Short Answer Questions (1–2 marks)
- Define the term ‘natural hazard’.
- What criteria must be met for a disaster to be listed on the International Disaster Database?
- Name two geological hazards.
- What is the epicentre of an earthquake?
- State two differences between the Richter and Mercalli scales.
- Why do earthquakes at destructive plate margins tend to be more frequent?
- What is a tsunami?
- Name two hazards caused by volcanic eruptions.
- Why do tropical storms form over oceans with temperatures above 27°C?
- What is the ‘eye’ of a tropical storm?
- Identify the wind speed range for a Category 4 tropical storm on the Saffir-Simpson scale.
- Name one method used to monitor tropical storms.
- What is population density?
- Why might people live near volcanoes despite eruption risks?
- Give two examples of short-term responses to earthquakes.
Section B: Case Study Questions (3–4 marks)
- Describe the social impacts of Cyclone Nargis (2008) in Myanmar.
- Explain why Hurricane Katrina (2005) caused severe flooding in New Orleans.
- Outline two long-term responses to the 2004 Asian tsunami.
- Compare the economic impacts of Cyclone Nargis (LIC) and Hurricane Katrina (HIC).
- Why did the 2004 tsunami cause such high casualties in Banda Aceh?
Section C: Data Interpretation (4–6 marks)
- Study Figure 3.1 (tectonic plates). Explain why earthquakes occur at conservative margins.
- Using Figure 3.5 (Saffir-Simpson scale), describe how damage increases with storm category.
- Analyse Figure 3.7 (population density). Why do densely populated areas overlap with hazard zones?
- Calculate population density for a city with 2 million people and an area of 500 km². Use Density=PopulationAreaDensity=AreaPopulation.
- Interpret Figure 3.9. What type of hazard is shown, and how long did it take to move through Honduras?
Section D: Extended Response (6–9 marks)
- Explain why earthquakes are difficult to predict.
- Discuss how volcanic eruptions can have both positive and negative impacts.
- Evaluate the effectiveness of preparation strategies for tropical storms in HICs vs. LICs.
- ‘The impacts of natural disasters are always worse in LICs.’ To what extent do you agree?
- Analyse how human activity can increase the risk of hazards becoming disasters.
Section E: Skill-Based Questions
- Sketch and label the structure of a tropical storm.
- Draw a annotated diagram of a destructive plate margin.
- Map the global distribution of volcanoes using Figure 3.3.
- Create a flowchart showing the stages of tropical storm formation.
- Design a poster advising communities on earthquake preparedness.
Section F: Mathematical Questions
- An earthquake measures 6 on the Richter scale. Calculate how much more energy it releases than a magnitude 5 quake. Use Energyn=30×Energyn−1Energyn=30×Energyn−1.
- Convert 215 km/h (Cyclone Nargis) to mph (1 km ≈ 0.62 miles).
- A volcanic ash cloud spreads 150 miles from a volcano. Convert this distance to kilometres.
- If a tsunami travels at 500 km/h, how long would it take to reach a coast 1000 km away?
- Calculate the storm surge height for a Category 5 storm using Figure 3.5.
Section G: Terminology & Concepts
- Define ‘pyroclastic flow’.
- What is geothermal energy, and how is it linked to volcanic areas?
- Explain the term ‘storm surge’.
- Differentiate between primary and secondary impacts of hazards.
- What is a ‘hotspot’ volcano?
Section H: Comparison Questions
- Compare the characteristics of shield and composite volcanoes.
- Contrast earthquake preparation strategies in Japan (HIC) and Nepal (LIC).
- How do the causes of floods differ from those of tropical storms?
- Compare the roles of satellites and radar in monitoring weather hazards.
- Why might tectonic hazards have more predictable patterns than climatic hazards?
Detailed Answers
- Natural hazard: An event from environmental processes that threatens or causes damage to people, property, or settlements (e.g., earthquakes).
- Criteria: ≥10 deaths, ≥100 injured, state of emergency declared, or international assistance requested.
- Geological hazards: Earthquakes, volcanic eruptions.
- Epicentre: The point on Earth’s surface directly above the earthquake’s focus.
- Richter vs. Mercalli:
- Richter measures energy released (logarithmic scale: Energyn=30×Energyn−1Energyn=30×Energyn−1).
- Mercalli measures observed damage/experience (e.g., Level 5 = objects fall).
- Destructive margins: Intense pressure from subduction causes frequent seismic activity.
- Tsunami: Large ocean waves triggered by undersea earthquakes/volcanic eruptions.
- Volcanic hazards: Lava flows, ash clouds, pyroclastic flows.
- Warm oceans: Provide energy via evaporation, fueling storm development.
- Eye: Calm, low-pressure centre with light winds and no rain.
- Category 4 winds: 210–249 km/h.
- Monitoring method: Satellites, radar, or weather stations.
- Population density: Number of people per km² (Density=PopulationAreaDensity=AreaPopulation).
- Reasons: Fertile soils, economic opportunities, lack of relocation options.
- Short-term responses: Emergency shelters, rescue operations.
Section B: Case Study Questions (3–4 marks)
- Social impacts of Cyclone Nargis (2008):
- At least 140,000 deaths.
- 3 million homeless; 95% of homes destroyed.
- Drinking water polluted, leading to disease outbreaks.
- Hurricane Katrina flooding in New Orleans:
- Storm surge (8.5 m) overwhelmed poorly maintained levees.
- 80% of the city flooded due to low elevation and subsidence.
- Long-term responses to 2004 tsunami:
- Rebuilding projects (e.g., £40 million spent in Sri Lanka/Indonesia).
- Installation of Indian Ocean tsunami warning system (2006).
- Economic impacts comparison:
- Cyclone Nargis (LIC): $10 billion rebuild cost; reliance on foreign aid.
- Hurricane Katrina (HIC): $98 billion rebuild cost; funded domestically.
- 2004 tsunami casualties in Banda Aceh:
- Proximity to epicentre (first hit).
- Lack of warning systems and evacuation plans.
Section C: Data Interpretation (4–6 marks)
- Earthquakes at conservative margins:
- Plates slide past each other, causing friction and sudden jerks (e.g., San Andreas Fault).
- Saffir-Simpson damage escalation:
- Category 1: Minor tree damage → Category 5: Catastrophic building destruction.
- Storm surge increases from 1.0 m (Cat 1) to >5.7 m (Cat 5).
- Dense populations in hazard zones:
- Economic opportunities (e.g., farming on volcanic soils).
- Urbanisation inertia (e.g., Tokyo near tectonic boundaries).
- Population density calculation:
Density=2,000,000500=4000 people/km2Density=5002,000,000=4000 people/km2 - Figure 3.9 interpretation:
- Hazard: Tropical storm.
- Duration in Honduras/El Salvador/Guatemala: 3 days (inferred from date labels).
Section D: Extended Response (6–9 marks)
- Earthquake prediction challenges:
- No reliable precursors (unlike volcanoes).
- Focus is underground; limited technology to monitor plate movements.
- Volcano impacts:
- Negative: Destruction (e.g., Pompeii), ash disrupting air travel.
- Positive: Fertile soils (e.g., Sicily), geothermal energy (e.g., Iceland).
- Storm preparation effectiveness:
- HICs: Advanced tech (e.g., NOAA satellites), levees (e.g., New Orleans).
- LICs: Reliance on aid (e.g., Myanmar’s delayed Cyclone Nargis response).
- Impacts worse in LICs?
- Agree: Poor infrastructure, limited healthcare (e.g., 140,000 deaths in Myanmar vs. 1,800 in USA).
- Disagree: HICs face high economic costs (e.g., Katrina: $98 billion).
- Human activity increasing disaster risk:
- Deforestation → landslides (e.g., Haiti).
- Urbanisation in floodplains → exacerbated flooding (e.g., Bangladesh).
Section E: Skill-Based Questions
- Tropical storm structure:
- Label: Eye (calm), eyewall (high winds), rainbands (heavy rain).
- Destructive plate margin diagram:
- Annotate: Subduction zone, magma rising, volcanic arc.
- Volcano distribution map:
- Plot: Pacific Ring of Fire, mid-Atlantic Ridge, hotspots (e.g., Hawaii).
- Tropical storm formation flowchart:
- Stages: Warm ocean → rising air → spiralling winds → eye formation.
- Earthquake preparedness poster:
- Tips: Secure furniture, emergency kits, evacuation drills.
Section F: Mathematical Questions
- Richter scale energy increase:
Energy6=30×Energy5Energy6=30×Energy5 (30x more energy). - Cyclone Nargis wind speed in mph:
215 km/h×0.62=133.3 mph215 km/h×0.62=133.3 mph - Ash cloud distance in km:
150 miles×1.61=241.5 km150 miles×1.61=241.5 km - Tsunami travel time:
Time=1000500=2 hoursTime=5001000=2 hours - Category 5 storm surge:
>5.7 m>5.7 m (from Saffir-Simpson scale).
Section G: Terminology & Concepts
- Pyroclastic flow: Superheated gas/ash cloud (450 mph, 1000°C).
- Geothermal energy: Heat from magma used for power (e.g., Iceland).
- Storm surge: Sea rise due to low pressure and high winds.
- Primary vs. secondary impacts:
- Primary: Immediate damage (e.g., collapsed buildings).
- Secondary: Long-term effects (e.g., economic recession).
- Hotspot volcano: Forms over mantle plumes (e.g., Hawaii).
Section H: Comparison Questions
- Shield vs. composite volcanoes:
- Shield: Gentle eruptions (basaltic lava), e.g., Mauna Loa.
- Composite: Violent eruptions (viscous lava), e.g., Mount Fuji.
- Earthquake prep: Japan vs. Nepal:
- Japan: Earthquake-proof buildings, drills.
- Nepal: Limited funds, reliance on NGOs.
- Floods vs. tropical storms:
- Floods: Caused by heavy rain/river overflow.
- Tropical storms: Driven by warm ocean temps.
- Satellites vs. radar:
- Satellites: Track cloud patterns globally.
- Radar: Monitors local precipitation movement.
- Tectonic vs. climatic predictability:
- Tectonic: Follow plate boundaries (predictable zones).
- Climatic: Influenced by variable weather systems.