Is Earth the only planet to have volcanoes?
On Earth, active volcanoes are found on all continents except Australia. Volcanoes even erupt under the ice on Antarctica! Volcanoes are also common elsewhere in the solar system. In fact, the biggest volcano is on Mars. This image is of Olympus Mons, which is a shield volcano. Olympus Mons is three times the height of Mt. Everest. But its slopes are very gentle.
A volcano is a vent from which the material from a magma chamber escapes. This may include lava, rock fragments, ash and gases. Volcanic eruptions can come from many types of structures. Most people think of volcanoes as large, peaky cones. But volcanoes can be large and broad, or tiny little cones. Volcanic eruptions can come from fractured domes, a vent in the ground, or from a giant hole in the ground.
Where They Are
Volcanoes are a vibrant manifestation of plate tectonics processes. Volcanoes are common along convergent and divergent plate boundaries. Volcanoes are also found within lithospheric plates at hotspots. Wherever mantle is able to melt, volcanoes are likely to be the result.
The Pacific Ocean basin is a good place to look for different types of volcanoes. The light blue wavy line that goes up the right-center of the diagram is the East Pacific Rise. The rise is made of volcanoes at a divergent plate boundary. Trenches due to subduction are on the west and east sides of the basin. Subduction creates island arcs that are seen in the western Pacific. Subduction also creates continental arcs seen along Central and South America. Hawaii is the line of volcanoes trending southeast-northwest near the center-top of the image. The Hawaiian volcanoes are due to a hotspot.
Volcanoes at divergent plate boundaries are in the East Pacific Rise. Convergent plate boundaries, where there are trenches, have volcanoes. Hotspot volcanoes are in chains in the middle of the ocean basin.
Volcanoes erupt because mantle rock melts. This is the first stage in creating a volcano. How can rock melt? One way is if the temperature rises. Another way is if the pressure on the rock decreases; this will lower the rock's melting temperature. The melting temperature of a rock also goes down if water is added. Every time there is a volcanic eruption one or more of these things happens. For each type of volcano mentioned in these lessons, think about how and why melting occurs.
Volcanoes can be active, dormant, or extinct.
Of all the volcanoes in the world, very few are erupting at any given time. Scientists question whether a volcano that is not erupting will ever erupt again and then describe it as active, dormant, or extinct.
Active: currently erupting or showing signs of erupting soon.
Dormant: no current activity, but has erupted recently.
Extinct: no activity for some time; will probably not erupt again.
active volcano: A volcano that is currently erupting or is just about to erupt.
dormant volcano: A volcano that is not currently erupting, but that has erupted in the recent past.
extinct volcano: A volcano that has not erupted in recorded history, and is unlikely to erupt again.
- Volcanoes are located along convergent and divergent plate boundaries. They can be found in the middle of plates at hot spots.
- Magma can be created when temperature rises, pressure lowers, or water is added.
- Volcanoes may be active, dormant, or extinct. This depends on whether there is the possibility of magma in their magma chambers.
Use this resource to answer the questions that follow.
- How are volcanoes formed?
- Where do volcanoes occur?
- What is the Ring of Fire? Where is it located?
- Where is Mount St. Helen's located?
- Where is Mount Pinatubo located?
- Where do most volcanoes occur? Why?
- What is needed for magma to form?
- If a volcano is dormant, can it become active? Can it become extinct?