8.2 Types of Volcanoes


What does an active volcano look like?

Climbing up Mount St. Helens and looking into the crater at the steaming dome is an incredible experience. The slope is steep and the landscape is like something from another planet. Nothing’s alive up there, except maybe a bird. When you’re standing on the top you can see off to others of the Cascades volcanoes: Mt. Adams, Rainier, Hood, Jefferson, and sometimes more.


A volcano is a vent through which molten rock and gas escape from a magma chamber. Volcanoes differ in many features, such as height, shape, and slope steepness. Some volcanoes are tall cones and others are just cracks in the ground ( Figure below ). As you might expect, the shape of a volcano is related to the composition of its magma.

Composite Volcanoes

Composite volcanoes are constructed of felsic to intermediate rock. The viscosity of the lava means that eruptions at these volcanoes are often explosive.

Mt. Fuji in Japan is one of the world’s most easily recognized composite volcanoes.

Mount St. Helens was a beautiful, classic, cone-shaped volcano. In May 1980 the volcano blew its top off in an explosive eruption, losing 1,300 feet off its summit.

Eruptions at Composite Volcanoes

Viscous lava cannot travel far down the sides of the volcano before it solidifies, which creates the steep slopes of a composite volcano. In some eruptions the pressure builds up so much that the material explodes as ash and small rocks. The volcano is constructed layer by layer, as ash and lava solidify, one upon the other ( Figure below ). The result is the classic cone shape of composite volcanoes.

A cross section of a composite volcano reveals alternating layers of rock and ash: (1) magma chamber, (2) bedrock, (3) pipe, (4) ash layers, (5) lava layers, (6) lava flow, (7) vent, (8) lava, (9) ash cloud. Frequently there is a large crater at the top from the last eruption.

Shield Volcanoes

Shield volcanoes get their name from their shape. Although shield volcanoes are not steep, they may be very large. Shield volcanoes are common at spreading centers or intraplate hot spots ( Figure below ). Hawaii has some spectacular shield volcanoes including Mauna Kea, which is the largest mountain on Earth from base to top. The mountain stands 33,500 ft high, about 4,000 feet greater than the tallest mountain above sea level, Mt. Everest.

Mauna Kea on the Big Island of Hawaii is a classic shield volcano.

Eruptions at Shield Volcanoes

The lava that creates shield volcanoes is fluid and flows easily. The spreading lava creates the shield shape. Shield volcanoes are built by many layers over time and the layers are usually of very similar composition. The low viscosity also means that shield eruptions are non-explosive.

This “Volcanoes 101″ video from National Geographic discusses where volcanoes are found and what their properties come from (3e) :http://www.youtube.com/watch?feature=player_profilepage&v=uZp1dNybgfc(3:05).

Cinder Cones

Cinder cones are the most common type of volcano. A cinder cone has a cone shape, but is much smaller than a composite volcano. Cinder cones rarely reach 300 meters in height, but they have steep sides. Cinder cones grow rapidly, usually from a single eruption cycle. These volcanoes usually flank shield or composite volcanoes. Many cinder cones are found in Hawaii.

A lava fountain erupts from Pu’u O’o, a cinder cone on Kilauea.

Eruptions at Cinder Cones

Cinder cones are composed of small fragments of rock, such as pumice, piled on top of one another. The rock shoots up in the air and doesn’t fall far from the vent. The exact composition of a cinder cone depends on the composition of the lava ejected from the volcano. Cinder cones usually have a crater at the summit. Most cinder cones are active only for a single eruption.


  • Magma composition determines both eruption type and volcano type.
  • Composite cones are built of felsic to intermediate lava and shield volcanoes of mafic lava.
  • Cinder cones are made of small fragments of a variety of compositions usually from a single eruption.

Making Connections


Use these resources to answer the questions that follow.

http://www.hippocampus.org/Earth%20Science \rightarrow Environmental Science \rightarrowSearch: Composite Volcanoes

1. What is another name for composite volcanoes?

2. Explain the composite volcano’s typical structure.

3. List two examples of composite volcanoes. What is the location of each?

http://www.hippocampus.org/Earth%20Science \rightarrow Environmental Science \rightarrowSearch: Cinder Cones

4. How is a cinder cone formed?

5. What is cinder cone’s typical maximum height?

6. Where is Lava Butte located?

7. When did Izalco last erupt?

http://www.hippocampus.org/Earth%20Science \rightarrow Environmental Science \rightarrowSearch: Shield Volcanoes

8. Describe a shield volcano’s structure.

9. What is the height of Mauna Loa?

10. Where is Mount Washington located? How old is it?


1. Why do mafic lavas produce shield-shaped volcanoes and felsic lavas produce cone-shaped volcanoes?

2. From what does a composite volcano get its name?

3. Describe how a cinder cone forms.


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