Earthquakes: Can't be Monitoring the Earth's movement
Volcanoes: Small earthquakes, Escaping gas, Change in the volcano's shape
Planning
1. Earthquakes: Buildings with shockabsorbancy, Automatic shut off switches to prevent fires
2. Volcanoes: Strengthen buildings, Trenches and barriers
Can't afford to move
Doesn't happen very often
Prediction
Earthquakes: Can't be reliablypredicted
Volcanoes: Can be predicted by monitoring the volcano
Protection
1. Earthquakes: Avoid high risk areas, Prepared emergency services, Educate locals, Practice evacuationdrills, Emergency supplies
2. Volcanoes: Can't be protected
Tropical Storms Case Study: Typhoon Haiyan
Made landfall in the Philippines on 8th November 2013
The most affected areas were Tacloban and Cebu
Up to 280 mm of rain
Up to 314 km/hour winds
Storm surge with 2.3m waves
One of the most powerful storms recorded
Disasters also have significant economic impacts, including damage to infrastructure, loss of productivity, increased healthcare costs, and decreased tourism revenue.
In addition to these immediate effects, disasters often lead to long-term consequences such as displacement, poverty, and social unrest.
Natural Hazard
A natural process which could cause death, injury or disruption to humans or destroy property and possessions
Two Main Types of Natural Hazard
Geological Hazards
Meteorological Hazards
Geological Hazards
Caused by land and tectonicprocesses, including volcanoes and earthquakes, landslides and avalanches
Meteorological Hazards
Caused by weather and climate, including tropical storms and other extreme weather (e.g. heatwaves and cold spells)
Hazard Risk
The probability of people being affected by a hazard in a particular area
Factors Affecting Hazard Risk
Vulnerability - the more people in an area exposed to natural hazards, the greater the probability they will be affected
Capacity to Cope - the better a population can cope with an extreme event, the lower the risk of them being severely affected
Factors Affecting Hazard Risk
Type - the risk from some hazards is greater than others (e.g. tropical storms can be predicted and monitored, but earthquakes happen suddenly with no warning)
Frequency - natural hazards that occur more often may carry a higher risk
Magnitude - more severe natural hazards tend to have the greatest effects
Natural hazards are extreme events that pose a threat to people
Tectonic plates are constantly moving and the Earth's surface is separated into these plates
Continental Crust
Thicker (30-50 km) and less dense
Oceanic Crust
Thinner (5-10 km) and more dense
Plates are moving because of convection currents in the mantle
Three Types of Plate Margin
Destructive Margins
Constructive Margins
Conservative Margins
Destructive Margins
1. Oceanic plate is subducted (forced down into the mantle) and destroyed, creating gas-rich magma, volcanoes and ocean trenches
2. Where continental plates meet, the ground is folded upwards, creating fold mountains
Constructive Margins
Magma rises from the mantle to fill the gap and cools, creating new crust
Conservative Margins
Crust isn't created or destroyed, plates move sideways past each other or in the same direction at different speeds
Volcanoes at Destructive Margins
Denser oceanic plate moves down into the mantle, melts, and magma rises through cracks in the crust to form a volcano
Volcanoes at Constructive Margins
Magma rises up into the gap created by the plates moving apart, forming a volcano
Volcanic Eruptions
Volcanoes emit lava and gases, and some erupt lots of ash which can cover land, block out the sun, and cause pyroclastic flows
Earthquakes
1. Caused by the tension that builds up at all three types of plate margin as the plates move
2. The plates eventually jerk past each other, sending out shockwaves which are the earthquake
Focus
The point in the Earth where the earthquake starts
Epicentre
The point on the Earth'ssurface straight above the focus
Moment Magnitude Scale
Measures the amount of energy released by an earthquake (magnitude)
A logarithmic scale, so a magnitude 7 earthquake causes 10 times as much ground shaking as a magnitude 6
Earthquakes of magnitude 6 and below normally only cause slight damage, while those of magnitude 7 and above can cause major damage and deaths
Global Atmospheric Circulation
The overall movement of air between the equator and the poles that affects the Earth's climate
Global Atmospheric Circulation
1. Air moves due to differences in air pressure, creating high and low pressure belts and cells
2. Air rises at the equator, sinks at 30° and 60° north/south, and moves back towards the equator or poles