Seismicity and Earths Interior Flashcards
Focus
The point within earth where the initial slippage generates earthquake energy
Epicenter
Point on earths surface directly above the focus
Seismic waves
Generated by an earthquake shock
Primary waves
First; compressional wave identical in character to sound waves passing through liquid or gas
Secondary waves
Second; particles shear or slide past one another
Shear waves
Cannot pass through liquid
Surface waves
Travel relatively slowly over earths surface
Shallow focus earthquakes
Occur in all seismic belts. Produce larges percentage of earthquakes. Up to 70 km below the surface
Intermediate focus earthquakes
Occur between 70-390 km below surface. Found at convergent plates
Deep focus earthquakes
Between 300-700 km below the surface. Found at convergent plates
Intensity
Destructive power of an earthquake; evaluation of the severity of ground motion at a given location
Magnitude
Objective measure of the amount of energy released
Earthquake hazards
Ground shaking Surface faulting Submergence Liquefaction Tsunamis Landslides Fires Floods
Seismic risk map
Shows past earthquakes in goes of future strikes
Mega thrust earthquakes
Plate of oceanic lithosphere is thrust beneath another at a subduction zone