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15 Cards in this Set

  • Front
  • Back

Earthquakes

Produce 3 types of waves with different behaviors as they travel through different materials

P Waves (primary waves)

longitudinal (push and pull back and forth motion) fastest, move through solid and liquid,

S Waves (secondary waves)

transverse (move at right angles to primary waves) slower, can move only through solid

surface waves

form when P and S waves reach the surface cause the ground to shake making rock sway side to side and roll like an ocean wave

epicenter

point on Earth's surface directly above where the energy is released in an earthquake; energy that reaches the surface here is greatest then spreads outwards in seismic waves.

seismograph

measures and records seismic waves

seismogram

vibration recorded looks like jagged lines on paperal

distance between the recording seismograph station and earthquake center

measuring the time between the arrival of the P (faster) and S (slower) waves determines

triangulation

plotting circles on a map from 3 seismograph stations, finding where they intersect thus locating the epicenter

San Andreas Fault, Calf

transform boundary

Himalayan MTS

convergent continent to continents

Andes MTs South America

Convergent s contintent and ocean plate subduction

Mid Atlantic Ridge

Divergent oceanic plate boundary sea floor spreading

Ring of Fire

area in Pacific ocean where volcanoes common

Great Rift Valley

divergent continent away from continent