Earthquakes: vibrations of the ground caused by the sudden release
of energy stored in rocks
Mostly due to sudden movement along faults
also, can be due to volcanism
elastic rebound theory: rocks bend until their strength exceed, break and "snap back"
vibrations (seismic waves) radiate through the earth
focus: location within the earth where rupture begins
epicenter: point on earth's surface directly above the focus
two types of seismic waves:
body waves travel through the earth:
Primary (P) waves, compression
and expansion, travel fastest
Secondary (S) waves. shear
waves, don't travel through liquids
surface waves move only on the surface of the earth
Seismographs: measure and record seismic waves
Earthquake distribution
95% of earthquakes are located along plate boundaries.
two major belts: circum-Pacific, Meditterranean-Asiatic
5% intraplate. Why intraplate?
Earthquake and Plate Tectonics
divergent boundaries: shallow (< 70 km), due to tension
transform: San Andreas fault system
convergent:
collision: due to compression
subduction zones: due to friction between subducting plate and overlying
plate.
Earthquake intensity and magnitude
Damage due to earthquakes
depends on magnitude and duration of shaking
Earthquake prediction
Long range
Earthquake control ?