Types of Stress
Earthquakes
Volcanic Boundaries
Waves
100

This force pushes the earth's crust in opposite directions (one up and one down)

Shearing 

100

This measures Ground motion during an earthquake

Seismograph 

100

Island arcs occur when two of this type of plate collide

oceanic 

100

this type of waves produce the most severe ground movements

surface waves

200

This type of stress results in a folded mountain range

compression

200

Geologists use the difference in the arrival time of p waves and s waves on a seismograph to determine this

Epicenter 

200

The force that causes magma to erupt at the surface is provided by this

dissolved gases under pressure

200

This type of wave causes the earth to compress

p waves

300

Rocks uplifted by this type of fault create fault block mountains

normal faults

300

This is triggered by earthquakes originating from beneath the ocean floor

Tsunami

300

An eruption of thin, fluid lava would most likely be this

a quiet eruption

300

The richter scale measures the size of these

seismic waves

400

This type of stress makes a strike slip fault

shear

400

An earthquakes this is located deep underground

focus

400

Alternating layers of lava and volcanic ash are found in this

composite volcanos

400

Seismic waves carry energy away from the earthquakes this

focus

500

This type of stress makes a reverse fault

compression

500

The mercalli scale measures this

intensity 

500

Thin runny lava usually hardens into this

lava plateaus or sheilds 

500

This type of wave arrives first during an earthquake

p wave

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