Physics of Earthquakes Flashcards
Earthquake
Ground shaking that accompanies sudden movement along a fault, movement of magma underground, a fast-moving landslide, or a large explosion.
First Stage of an Earthquake
Energy buildup: Strain accumulates as rock on either side of the fault is pushed in opposite directions (stress).
Second Stage of an Earthquake
Rapture and Initial Energy Release: Rock breaks in a rupture zone sends vibrations out through the surrounding rock. Vibrations travel out from the epicenter as Primary and Secondary Waves. (P and S waves)
Third Stage of an Earthquake
Continued Release: surface shaking: Earthquake waves reach the surface, traveling as Love and Raleigh waves.
Fourth Stage of an Earthquake
Post Event: After shaking ceases, strain builds up, setting the stage for the next earthquake.
Primary (P) Waves
Body waves that move by compression and expansion.
Secondary (S) Waves
Body waves that move by vertical displacement.
Love Waves
Surface waves that move by lateral (sideways) displacement. They decay slowly and are highly destructive.
What are Love waves named for?
Mathematician A. E. Love.
What is the velocity of a Love wave?
Less than 2.9 kps
Raleigh Waves
Surface waves that move by vertical displacement.
What is the velocity of a Raleigh wave?
Less than 3.0 kps
What are Raleigh waves named for?
Physicist Lord Raleigh
What are the 3 stresses that cause geologic formations?
- Compression
- Extension
- Shearing
Compression
Rock is pushed together
Extension
Rock is stretched
Shearing
Rock is wrenched sideways
How do earthquakes behave?
- Initiation
- Wave travel below the Earth’s surface
- Wave travel at the Earth’s surface
- Aftermath
Body Waves
Waves travel below the Earth’s surface
Surface Waves
Wave travel at the Earth’s surface
Aftermath of an Earthquake
Stress buildup and eventual release
How are earthquakes measured and located?
- Instrumentation
- Measuring scales
- Locating epicenters and hypnocenters
What are the 3 instruments used to measure earthquakes?
- Seismoscope
- Vertical Pendulum
- Seismograph
Seismoscope
A mechanical device that detects vibrations from distant earthquakes. It uses a ball falling from a chute into a cup (frog) indicating direction of principle impulse.