Ch. 8: Earthquakes Flashcards
Earthquake
Earth shaking caused by a rapid release of energy
tectonic stresses cause rocks to break
energy moves outward as an expanding sphere of waves
What are the causes of most Seismicity?
• Most seismicity (earthquake activity) occurs due to…
o Motion along a fault
o Inflation of a magma chamber
o Volcanic eruptions
• Lesser causes:
o Giant landslides
o Meteorite impacts
o Nuclear explosions
What is the focus of an earthquake?
the break along an earthquake fault within the
earth from which seismic waves originate
What is the epicenter?
the point on the earth’s surface directly above
the focus of an earthquake
What is the Elastic Rebound Theory?
Strain builds up until rock’s strength is exceeded
Stress is released, blocks are displaced across fault, then snap back to original shape.
This elastic rebound releases energy as seismic waves.
Primary or P waves
Compressional, or primary (P), waves
• Push-pull (compress and expand) motion
• Fastest type of seismic waves
• Travel through solids AND liquids
Secondary or S waves:
Shear, or secondary (S), waves
• Sideways motion
• Slower than P waves
• Travel only through solids, not liquids
Surface waves:
Travel along Earth’s surface
These waves are the slowest and most destructive type of seismic waves.
What are Seismographs/seismometers?
– Instruments that record seismic waves
– detect earthquakes anywhere on Earth
– reveal size and location of earthquakes
What is the Richter magnitude M? How is that determined?
The Richter scale represents the energy released
by an earthquake.
Each increase in magnitude corresponds to 30X more energy released
What is the Mercalli intensity? What do the Roman numerals mean?
• Mercalli intensity scale - Degree of shaking
damage
– Roman numerals I-XII assigned to different levels of damage.
– Damage occurs in zones related to local geology, bedrock vs. water-saturated soils
Where do most earthquakes occur? along plate boundaries (interplate)
Divergent and transform: shallow
ex) San Andreas
Convergent: shallow to deep (≤700 km); Wadati-Benioff zone
ex) Japan
But some earthquakes occur within a plate (intraplate)
ex) New Madrid, MO; Charleston SC
What are the hazards of earthquakes:
Ground shaking Building collapse Liquefaction Landslides Tsunami Fire
Earthquake prediction (short-term)
Precursors: clusters of foreshocks strain build-up and deformation of crust changes in water level, gasses in wells animal behavior (may hear ultrasonic micro-cracking)
stick-slip history of a fault
Stress builds up until rock’s strength is exceeded
• Micro-fractures form (→ foreshocks)
• When fault moves → main shock
• Minor movement later → aftershocks