Ch2 Flashcards
Seismic Waves
When earthquakes occur, energy is released that travels through Earth in the form of vibrations, or Seismic waves
2 kinds of waves
Surface waves and body waves
Surface Waves
They move over Earth’s surface a little like ocean waves, but travel much faster. These do the most property damage
Body Waves
Cause less damage but are more useful in studying Earth’s interior bc they travel beneath the surface
Refract
As body waves travel from one type of material into another, their speed can change and they will change direction, or refract.
2 kinds of body waves
primary-waves and secondary-waves
Primary waves (travel through solid, liquid, gas)
p-waves travel faster than any other kind of seismic wave & are the first to arrive to a location.
Compressional Waves
P-waves are also known as compressional waves bc they cause the material they pass through to compress and stretch parallel to the direction the waves travel.
Secondary Waves (travel through solids)
s-waves travel slower than s-waves but faster than surface waves. 2nd to arrive to location
Shear Waves
s-waves are also known as shear waves bc they cause the material they pass through to shake from side-to-side, perpendicular to direction they travel.
Body waves cont.
Travel downward from the location of earthquake, reach some max depth, then return to surface.
Earth’s interior
3 layers: curst, mantle, core.
Crust
Thin, rocky layer that comprises about 0.4% of Earth’s mass and less than 1% of its volume.
2 kinds of crust
Continental crust & Oceanic crust
2 kinds of crust
Continental crust & Oceanic crust