Earthquakes: Ch 9  Note:  These notes are from my (Dr. Screaton's) lecture notes. I checked with Dr. Smith to confirm that he covered the same material.

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?

Example of intraplate: New Madrid, Missouri, Charleston SC

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

        greater effects on poorly lithified material (liquefaction can occur)
         greater affect on rigid, unreinforced construction


Earthquake prediction
Long range

Short range


Earthquake control ?