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Types of Volcanoes

A volcano is an opening on the earth’s surface through which molten rocks, lava, volcanic ash, debris, and gases from the magma chamber reach the earth’s surface.

Earth’s crust is broken into 17 major tectonic plates, which float on its mantle (the layer beneath the earth’s surface). Since these plates are always converging or diverging, sometimes they collide or pull apart, and volcanoes may erupt in these active zones. During a volcanic eruption, molten rock or lava come out through vents in Earth’s crust. When the lava is beneath the earth’s surface, it is called magma.

Mount St. Helens (USA), Mauna Loa (Hawaii), Mount Cotopaxi (South America), Mount Pinatubo (Philippines) are some famous volcanoes in the world.

How Many Types of Volcanoes Are There

There are four types of volcanoes based on the nature of their eruption and the kind of lava they release – cinder cone, composite, shield, and lava dome volcanoes.

Based on their frequency of eruption, volcanoes can be of three types – active, dormant, and extinct volcanoes.

What are the Different Types of Volcanoes Based on Their Eruption Characteristics

Types of Volcanoes

1. Cinder Cone Volcano

Cinder Cone is the simplest, most common type, and has a characteristic cone shape. It forms when volcanic cinder, blobs of congealed lava of basaltic composition, come out from a single vent. It has explosive eruptions caused by gas rapidly expanding and escaping from the molten lava that comes out like a fountain. The lava cools quickly and falls as cinders that build up around the vent forming a cone shape, leaving a crater at the summit. These volcanoes can be as high as 100 to 400 meters.

Lava Type: Less viscous, quite fluid basaltic lava (enriched in iron and magnesium and depleted in silica)

Examples: Lava Butte in Oregon (USA), Cerro Negro in Nicaragua (Central America), Parícutin in Mexico.

Parícutin in Mexico Cinder Cone Volcano Types

2. Composite Volcano

Also referred to as strato-volcanoes, it includes some of the world’s grandest mountains. It is a tall conical mountain composed of an alternating layer of lava-flow, which justifies the name composite volcano. It can have a cluster of vents, with lava breaking through walls or issuing from fissures on the sides of the mountain. The eruptions are extremely explosive and dangerous. Pressure builds in the magma chamber as gases under immense heat and pressure are dissolved within the magma. When the magma reaches the vents, the pressure is released, and the gases explode violently. These can be up to 100 to 3500 meters high.

Lava Type: Highly viscous rhyolitic lava that hardens before it can spread far (high content of silica and low iron and magnesium contents)

Examples: Mount St. Helen and Mount Rainier in the USA, Mount Etna and Stromboli in Italy, Mount Fuji in Japan, Cotopaxi in Ecuador, Mount Vesuvius in Italy, Mount Pinatubo and Mayon in the Philippines, Volcan de Colima in Mexico, Eyjafjallajokull in Iceland, Popocatepetl in Mexico, Arenal Volcano in Costa Rica, Mount Shasta (White Mountain) in USA.

Mount St. Helen in the USA Composite Volcano Types

3. Shield Volcano

Shield volcanoes are huge, gently sloped volcanoes that almost exclusively erupts basaltic lava and include some of the largest volcanoes in the world. The eruptions are not explosive; the lava oozes out from the central vent or a group of vents and spreads far, building a dome shape profile like a warrior’s shield. They can be as high as 9000 meters from the base.

Lava Type: Less viscous, quite fluid basaltic lava

Examples: The volcanoes in the Hawaiian Island, including Kilauea, Diamond Head, Mauna Loa, and Mauna Kea

Mauna Loa in Hawaii Shield Volcano Types

4. Lava Dome

These are relatively small, circular mounds formed as the lava is too viscous to flow, which makes it piles over and around the vents. As the lava oozes out, its outer surface cools and hardens, then shatters, spilling loose fragments down its side. Lava domes are found within the crater or on the sides of large composite volcanoes. Their height depends on the size of the composite volcanoes they appear around.

Lava Type: Highly viscous, less fluid rhyolitic lava

Examples: Lassen Peak and Mono domes in California (USA), Novarupta lava dome in Alaska (USA)

The Lava Dome at the Crater of Mount St. Helen in the USA

What are the Different Types of Volcanoes Based on Their Frequency of Eruptions

1. Active Volcanoes

Those that have erupted in the last 10,000 years and are expected to erupt again at any time.

Examples: Mount Etna in Italy and Mauna Loa in Hawaii.

2. Dormant Volcanoes

Those that have not erupted in the last 10,000 years, but are likely to erupt after remaining inactive for a long period.

Examples: Mt. Kilimanjaro in Africa and Mt. Fuji in Japan.

3. Extinct Volcanoes

Those that were active in the past, but have not erupted in the last 10,000 years and are not likely to erupt in the present or the future.

Examples: Mt. Kenya in Africa and Mt. Aconcagua in South America.


Q 1.  What is a caldera?

Ans. Caldera is a bowl-shaped depression formed when a volcano collapses shortly after emptying the magma chamber in a volcanic eruption. Though sometimes considered a separate type of volcano, it is actually formed as an after-effect of an eruption. Yellowstone Caldera in the USA is one such example.

Q 2. What are pyroclasts or pyroclastic materials?

Ans. Pyroclasts refer to the rocks, lava fragments, ash, vapor expelled during volcanic eruptions.

Q 3. What is the world’s largest active shield volcano?

Ans. Mauna Loa (Hawaii).

Article was last reviewed on Friday, December 13, 2019

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