Seismic Hazards Flashcards
Focus
The breaking point
Epicentre
The point on the surface directly above the focus
Depth of focus and its effects
Shallow focus earthquakes (0-70km deep) tend to cause the greatest damage and account for
75% of all earthquake energy released.
Intermediate focus earthquakes occur between 70-300km
Deep focus earthquakes occur at depths of 300-700km.
Body waves
Are shockwaves that travel through the earth
There are two types of body waves: primary and secondary
Primary (P) waves
travel through both liquids and solids and are the fastest waves, reaching the surface first.
Secondary (S) waves
also travel through the Earth, but unlike primary waves, they cannot travel through solids such as the core.
Surface waves
travel along the Earth’s surface. Because they cannot travel through the mantle and core
Love (L) waves
are the slowest waves but they are the most destructive.
Rayleigh (R) waves
travel out from the epicentre near the surface.
Tsunamis
These are giant sea waves generated by shallow-focus underwater earthquakes involving movements of the seabed
Liquefaction
occurs in unconsolidated sediments that are saturated with water. Such sediments are made of loosely arranged particles that are not joined together and behave like a liquid when shaken by seismic waves.
Landslides
is a rapid movement of earth materials down a slope, the materials ranging from huge boulders to soil.
Magnitude of earthquakes
The Richter scale is a logarithmic scale. The scale starts at 0 and each number is ten times the magnitude of the one before it.