Types of volcanoes | Some infamous volcanic eruptions

A volcano is an opening in a planet’s crust through which hot lava, tephra and gases come out from a magma reservoir. Magma refers to the molten or semi-molten rocks inside the Earth’s surface. There are 3 types of volcanoes classified based on activity.

  • Active
  • Dormant
  • Extinct

Active volcanoes are those which erupt frequently.
Dormant volcanoes are those which show signs of a future eruption.
Extinct volcanoes are those which show no signs of eruption.

Types of Volcanoes classified on the basis of extrusive landforms

Stratovolcanoes (composite volcanoes)

These are the most common types of volcanoes. Stratovolcanoes have an almost conical shape e.g., Mount Fuji, Mount Vesuvius. These cones are built up by several eruptions of volcanic materials from the main conduit. Each eruption adds a new layer to the sides of the volcano.

The lava that comes out of these volcanoes is acidic having a very high viscosity and a high silica content.

Stratovolcanoes - Types of volcanoes

The lava doesn’t spread out far because of the high viscosity and a conical landform is formed around the conduit. These volcanoes may have various dykes feeding other vents on the sides of the volcano.

Stratovolcano eruptions are often explosive. A large amount of gas and pyroclastic material is thrown up in the atmosphere.

Shield volcanoes

The less viscous lava forms the shield volcanoes. The less viscous basic lava flows easily and forms a shield like landform. The eruptions are generally non-explosive (effusive eruption). The basic lava that flows out of the shield volcanoes has a low silica percentage.

Shield volcanoes - types of volcanoes

Quick question

Which is the highest active volcano in the world (above sea-level)?

Cinder cones

These are simple volcanoes having a single vent. Cinder cone hills have steep slopes and there is a bowl-shaped crater at the top. Pyroclastic materials such as volcanic ash and cinder are thrown up in the air during the eruption of the lava fountain. The pyroclastic material cools and settles down to form loose conical hills. The highly viscous molten lava flows beneath the cinder cones. These volcanoes roughly reach a height of 1000 ft.

Cinder cones - types of volcanoes

Lava domes

These are formed by the very viscous lava. Due to its high viscosity, the lava does not flow easily and starts piling up to form lava domes.


Caldera is a hollow formed when the magma reservoir is emptied and the ground above it collapses.

Now we know about the types of volcanoes. Let’s discuss about some infamous volcanic eruptions.

Some infamous volcanic eruptions

The explosivity of volcanic eruptions varies indefinitely. Some eruptions cause minimal damage while others can affect global weather. Volcanic explosivity index (VEI) gives us the relative measure of explosiveness of a volcanic eruption. It is a number ranging from 0-8. Greater the index, greater is the amount of tephra thrown out. Tephra refers to any solid material thrown out of the volcano.

Material coming out of the volcano is basically of three types – molten lava, tephra (solid rocks and ash), and gases. Lava flows closer to the surface and hence causes less damage than the tephra that travels far and causes widespread damage.

Mount Tambora eruption in 1815

Mount Tambora is an active stratovolcano in Sumbawa, Indonesia. 1815 eruption of Mount Tambora is the deadliest volcanic eruption in recorded history. The volcanic explosivity index was 7 for the eruption.

Volcanic ash covered many parts of Indonesia, burnt crops creating food shortages. The volcanic eruption shot the volcanic clouds up in the stratosphere. The aerosols traveled across the world and decreased the average global temperatures. Temperatures dropped because the sunlight was reflected by the sulphur aerosols present in the clouds.

The city of Chennai (then Madras) on the eastern shore of India experienced temperatures below freezing which is unusual for a South Indian coastal city. Moreover, some say, it even snowed in Madras.

An estimated 90,000 people lost their lives because of the eruption.

Mount Vesuvius eruption of 79 AD

Mount Vesuvius is a stratovolcano located on the Gulf of Naples. It has an elevation of 1,281 meters. The eruption of Mount Vesuvius on 24 August 79 AD is one of the deadliest volcanic eruptions in recorded history. The eruption had a VEI of 5. The city of Pompeii southwest of Vesuvius and the city of Herculaneum west of Vesuvius were completely buried under volcanic ash. The explosive eruption shot the gases and other volcanic materials up in the stratosphere more than 30 kilometers.

Mount Vesuvius Pompeii
Pompeii with Mount Vesuvius in the background

The number of casualties are unknown but were estimated in several thousands.

The city of Pompeii buried under the volcanic ash was rediscovered in 1748. Most of the things in the city were found unharmed as they were preserved by the volcanic ash.

The letters written by Pliny the younger, a Roman author give an eye witness account of the actual explosion.

Krakatoa 1883 eruption

Krakatoa is a volcanic island in the Sunda Strait between the Indonesian islands of Java and Sumatra. 1883 explosion of Krakatoa claimed the lives of more than 36,000 people. Several towns were buried under the hot volcanic ash. The eruption was so loud that it was heard thousands of kilometers away in Perth, Australia.

Like the Mount Tambora eruption, it also decreased the average global temperatures. The VEI for the eruption was 6. The eruption triggered a Tsunami which did more damage than the explosion itself.

Mount Pelee explosion in 1902

Another infamous volcanic explosion took place in Martinique. Mount Pelee which is a stratovolcano erupted in 1902 completely obliterating the town of Saint-Pierre. 30,000 people lost their lives and there were only 2 survivors from Saint-Pierre.

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Answer to quick question

Ojos del Salado in the Andes is the highest active volcano in the world. It has an elevation of 6,893 m above sea-level. It is a stratovolcano.

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