Earthquakes occur at all plate boundaries as they all experience some degree of movement. Frequent movement means there is a constant release of energy and pressure, so earthquakes here are less severe
Earthquake- as the crust of the earth is constantly moving, there tends to be a slow build up of stress within the rocks. When this pressure is released, parts of the surface experience intense shaking.
Retrofitting is when, in earthquake prone areas, buildings and other structures can be fitted with devices such as shock absorbers and cross-bracing to make them more earthquake proof.
A tsunami is a giant sea wave generated by a shallow focus under water earthquakes, violent volcanic eruptions, under water debris slides and landslides into the sea. It is a displacement of water.
An epicentre is the point on the earths surface immediately above the focus of the earthquake.
The focus is the point where the pressure release occurs withing the crust.
Magnitude is the size of an earthquake using amplitude of seismic waves. This is measures with a seismometer.
The Richter Scale is a logarithmic scale proportional to the magnitude. Mostly replaced by the moment magnitude scale (MMS) which identifies energy released
The Mercalli Scale is a human scale which measures the intensity of an event and its impact using a 12-point scale
Landslides and avalanches are slope failures as a result of ground shaking
Liquefaction: when violently shaken, soils with a high water content loose their mechanical strength and behave like a fluid. The water particles move to the surface.
P waves are vertical. Buildings are built to withstand vertical weight
S waves are horizontal. These are more destructive, especially to buildings that have not been built/retrofitted to withstand this movement
Tsunami- water is quickly vertically displaced which forms waves. These can reach 500-600 inland. P waves uplift under the sea. Wave gets taller is water shallows and wave slows. Generated by a shallow focus underwater.
Drawdown is the reduction in sea level (tide goes out).
Management of seismic hazards involves preparation, mitigation, prevention and adaptation
Preparation includes securing things to the wall or floor and making a plan (where to meet, where emergency kit is and what's in it, emergency radio or beacon)
Mitigation involves deploying the army (Gov), education (gov) and earthquake proof beds.
Prevention cannot truly be done so it is better to prepare and mitigate. But, it can involve early warning systems of magnitude and location.
Adaptation includes retrofitting (pendulums, deep foundations, early warning systems, making buildings flexible through dampeners)
Examples of management: EQ drills, fire prevention, emergency services, land-use planning, insurance, aid, tsunami protection.