An extremenatural event that can cause loss of life, extreme damage to property and disrupt human activity
Types of hazards
Geophysical
Hydrological
Atmospheric
Characteristics of hazards
Clear origins or causes
Distinctive effects
Little or no warning
Exposure may be involuntary
Damage takes place shortly after the hazard, but impacts may last long into the future
Scale and impact requires an emergency response
Disaster
When a hazardous event and a vulnerable population combine
There is no universal agreement on the difference between a disaster and a hazard</b>
A natural hazard only has the potential to cause loss of human life, when it does not it is just a natural event
The UN's criteria for it to be classified as a disaster are: 10+ people killed, 100+ are affected, a state of emergency is declared or international assistance is called for
In 1990, Swiss Re Insurance defined a disaster as an event where at least 20 people die, or insured damage of at least $16 million USD is caused
Disaster
Causes 'significant' impact on a vulnerable population
Factors influencing the relationship between a hazard and a disaster
Natural
Economic
Social
Political
Geographical
Technological
Environmental
Natural factors
Magnitude
Frequency
Duration
Areal extent
Spatial concentration
Speed of onset
Regularity
Earthquake magnitude is now measured in Moment Magnitude Scale (MMS), a modification of the earlier Richter scale
The extent of damage from earthquakes is measured with the Mercalli Scale
Volcano magnitude is measured using the VEI Index, related to the type of lava (basaltic or andesitic) and the type of boundary
Hurricanes are measured using the Saffir-SimpsonHurricaneScale, which measures from 1 to 5, 5 the most severe, based on peak windspeeds
People living in the Asia-Pacific region are 5x more likely to be affected by a natural disaster than those elsewhere
Between 1995 and 2015, America, China and India had the most natural disasters
The annual number of disasters has been rapidly increasing since 1900, peaking at over 400 many years since 2000
Droughts caused the most deaths in the early 20th century, such as the 1928 Chinese Drought killing 3 million
Deaths from natural disasters have been decreasing since the 1920s
Hazard perception
Acceptance
Fear
Adaption
Fatalism
Examples of hazard perception
30% of Americans cite climate change as a motivator to move in 2023
Japan has put up sea walls after the 2011 earthquake
Only 4,000 people moved back to Paradise after the 2018 wildfire
Responses to hazards and management
Modifying the loss (adaptation)
Modify vulnerability (adaptation)
Modify the event (mitigation)
Modify the cause (mitigation)
Hazard Management Cycle

A general plan for recovery and preparation for a hazard
Park Model / Disaster Management Curve

Useful to compare and contrast different hazards and pinpoint different responses needed at different stages
The Hazard Management Cycle and Park Model / Disaster Management Curve are generalised and do not account for differences in development or the fact that some places may never return to 'normal'
Plate tectonic theory

The Earth's crust is split into 7 large plates and several smaller ones, all of which slowly move along Earth's surface
Evidence of continental drift

The east coast of South America and West Africa seem to fit together
Rock layers in the Appalachian Mountains match those of the Caledonian Mountains in Scotland
Rocks in Alaska have fossils of palm tree leaves despite the cold climate, suggesting it was once at lower latitudes and more tropical
Karoo strata in South Africa match the Santa Catarina rocks in Brazil
Paleomagnetism

Provides evidence of seafloor spreading by examining the polarity of rocks
Convection currents
Heat from the core heats the base of the mantle, causing hot rock to rise, cool, and sink, repeating the process and moving the plates
Gravitational sliding

Ridge push and slab pull, where the force of gravity moves the plates
Parts of Earth

Crust
Lithosphere
Asthenosphere
Mantle
Outer core
Inner core
Continental vs oceanic crust
Continental
Oceanic
Types of plate boundaries
Destructive
Constructive
Conservative
Collision
The vast majority of earthquakes happen at plate boundaries
Richter scale
Measures maximum wave amplitude, not total energy released
Moment magnitude (Mw)
Measures the energy released and the amount of movement by rock and the area of the fault
Mercalli scale

Measures the intensity of the earthquake event
Types of waves

Primary waves (P waves)
Secondary waves (S waves)
Love wave
Rayleigh wave
Locating earthquakes

The time between first P and S waves on a seismogram is used to determine the distance from the epicentre