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27 Cards in this Set

  • Front
  • Back

Fault and force at a divergent boundary

Normal and tension

Fault and force at a transform boundary

Strike slip and shearing

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

Triangulation

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

Make up and size of the layer

Vibration caused by energy released when a break at a fault

Seismic waves

Earthquake waves that arrives at the surface first

Primary

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

Surface

The movement of rocks particles during the passage of S waves

Right angles

The movement of rock particles during the passage of P waves

Back and forth

The sequence of waves during an earthquake from first to last

Primary secondary and surface

Force that causes plates to move sideways past each other

Shearing

Type of stress that produces reverse faults

Compressional

What type of fault is created by tensional forces

Normal Fault

A fault where rocks slip past each other sideways

Strike slip

Type of force at a strike-slip fault

Sheering

Force that pushes rock in opposite directions

Tension

Changes in Earth’s interior have been detected due to

Seismic Wave

The force that squeezes rock together

Compression

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

Earthquake

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

Faults

Measuring the time between the epicenter and the

Recording seismic graph

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

Focus

Point B is called the earthquake

Epicenter

What type of fault is illustrated in this diagram

Normal

A layer of hot rock

Mantle

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

Convergent

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

Divergent