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Boundaries and Geologic Events

 

Boundary

Description

Example

Divergent

New crust is generated as the plates move away from each other

Sea floor spreading- Atlantic Ocean

Rift valley- Iceland and Africa

Earthquakes and volcanoes can occur

Convergent

Crust is destroyed as a dense plate subducts (dives) under a less dense plate

(e.g., basaltic ocean plates are denser than granitic continental plates)

Ocean-Continental: volcano formation/ earthquakes

Ocean-Ocean: Trench formation with volcanoes and earthquakes

Continental-Continental: Mountain building, earthquakes possible

Transform (Sliding)

Plates move past each other

Earthquakes such as those along the San Andreas Fault

Original source of this diagram is a USGS poster. It can be found at the USGS Dynamic Earth website.

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Return to Third Marking Period Index