Earthquakes Flashcards
Displacement
The offset of segments or points that were once continuous or adjacent.
Stick-slip
Movement starts, but quickly stops due to friction
Stress builds, causing failure
Hypocenter vs. Epicenter
Hypocenter (or focus): The spot within the Earth where earthquake waves originate
Epicenter: Land surface above the hypocenter
Seismicity
Motion along a newly formed fault
Motion on an existing fault
*Body Waves
Primary (P) Waves: Compressional waves, (Push Pull) travels through solids, liquids, and gases
Secondary (S) Waves: Shear waves, (Shaking) travels through solids only
Surface Waves
Travel along Earth’s surface
Love (L) waves – Move back and forth like a snake
Rayleigh (R) waves – Move like ripples on a pond
Magnitude
The amount of energy released
Shallow Earthquakes
0-60km subduction trace
Earthquakes are rare below 660 km (mantle is ductile)
Intermediate & Deep Earthquakes
Intermediate and deep earthquakes occur along the subduction trace
Soil Liquefaction
Waves liquefy H2O-filled sediments
High pore pressures force grains apart, reducing friction
Liquefied sediments flow as a slurry
Tsunamis
Result when earthquakes change the seafloor (Not Tidal Waves)
Normal faulting drops seabed; reverse faulting raises it