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27 Cards in this Set

  • Front
  • Back

Normal / tension

Fault and force at a divergent boundary

Strike- slip / shearing

Faults and forces at a transform boundary

Triangulation

Locating the earthquake epicenter by drawing three circles and finding where the three intersect is called

Make- up and size layer

Scientist have been able to use earthquake waves to find out what about the earth

Seismic wave

Vibrations caused by energy released when q break occurs at a fault is

Primary wave

Earthquake wave that arrive at the surface first

Surface waves

Earthquake waves that cause the ground to shake and make rocks roll like an ocean wave

Right angles

The movement of rock particles during the passage of S waves

Back and Forth

The movement of rock particles during the passage of P waves

Primary / secondary / surface waves

The sequence of waves during an earthquake from first to last

Shearing

Force that causes plates to move sideways past each other

Compression

Type of stress that produces reverse faults

Normal

What type of fault is created by tensional forces

Strike - slip

A fault where rocks slip past each other sideways

Shear

Type of force at a strike slip fault

Tension

Force that pushes rock in opposite directions

Seismic wave

Changes in Earth’s interior have been detected due to

Compression

The force that squeezes rocks together

Earthquakes

When the force on rocks is great enough , they break, producing vibrations called

Faults

Once the elastic limit of rocks is passed , they break and move along surface called

Seismograph

Measuring the time between the arrival of P and s waves determine the distance between the epicenter and the

Focus

Point A where energy is initially released during the earthquake is called the

Epicenter

Point B is called the earthquake

Normal

What type of fault is illustrated in this diagram

Mantle

A layer of hot rock

Convergent

When arrows at a plate boundaries are point towards each other it is a

Divergent

When arrows are pointed away from teach other at plate boundaries it is