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Plate boundaries, earthquakes and volcanoes
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Most earthquakes and volcanoes happen where plates meet. What happens depends on how the plates move.
Types of plate boundary
Destructive (convergent): oceanic crust sinks under continental crust. This causes explosive volcanoes and strong earthquakes. Example: the west coast of South America (the Andes) and Japan.
Collision: two continental plates push together and fold up into mountains, such as the Himalayas.
Conservative: plates slide past each other. No volcanoes, but earthquakes. Example: the San Andreas Fault in California.
Earthquakes
The point underground where it starts is the focus; the point on the surface above it is the epicentre.
Scientists measure earthquake strength on the moment magnitude scale. Undersea earthquakes can cause tsunamis, as in Japan in 2011.
Volcanoes
The Pacific Ring of Fire is a ring of volcanoes and earthquake zones around the Pacific Ocean.
In 2010 ash from the Icelandic volcano Eyjafjallajokull stopped many flights across Europe for days.
Why are earthquakes and volcanoes common in Japan?
- Japan lies on destructive plate boundaries.
- Oceanic plates sink beneath the plates Japan sits on, which melts rock and forms magma: volcanoes.
- The plates stick and slip as they move, releasing energy: earthquakes.
Answer: It sits on destructive boundaries where plates sink, causing both volcanoes and earthquakes.
Constructive: apart (Iceland). Destructive: oceanic plate sinks (Andes, Japan): explosive volcanoes and big earthquakes. Collision: fold mountains (Himalayas). Conservative: slide past (San Andreas), earthquakes only. Focus underground; epicentre above it. Ring of Fire around the Pacific.
The interactive lesson includes the diagrams for this topic.
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