In January 2022 (very recent!), an underwater volcano erupted near Tonga in the South Pacific Ocean. This is one of the most significant recorded eruptions in over 30 years, and the volcano caused a series of tsunami waves on the shores of Tonga. But what exactly is a volcano? How are they formed? What different types of volcanoes are there? Let’s find out.
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Jetzt kostenlos anmeldenIn January 2022 (very recent!), an underwater volcano erupted near Tonga in the South Pacific Ocean. This is one of the most significant recorded eruptions in over 30 years, and the volcano caused a series of tsunami waves on the shores of Tonga. But what exactly is a volcano? How are they formed? What different types of volcanoes are there? Let’s find out.
Volcanoes are openings of the Earth’s crust to the molten rock below the surface of the Earth. A mixture of hot liquid rock, gases, mineral crystals, and rock fragments – also known as magma – shoots up during a volcanic eruption.
Check out our explanation on Mount Merapi Eruption 2010 to see the damage volcanoes can cause.
The majority of volcanoes are formed at convergent plate margins where subduction occurs. As the denser plate sinks beneath the less dense plate, the temperature and pressure increase. The increase in temperature and pressure causes rocks to release water, resulting in a reduction in the melting point of the rock above. This creates magma, which rises to the surface, forming a volcano.
Certain volcanoes are attributed to hot spots from mantle plumes instead of convergent plate margins. A mantle plume is an area under the crust of the Earth where the magma is hotter than the surrounding magma. The volcano is formed as the hotter magma melts the crust and causes magma to rise to the surface. The mantle plume remains stationary whilst the tectonic plate continues to move (this can cause a chain of volcanoes). Some examples include the Hawaiian Islands that are located far from plate boundaries.
The different states of volcanoes are active, dormant, and extinct.
The different types of volcanoes include cinder cones, composite volcanoes, shield volcanoes, and lava domes.
Cinder cones are formed by the particles from lava that erupt from a single opening. When the gaseous lava is ejected into the air, small fragments solidify and form cinder. This cinder falls around the opening and forms a circular or oval cone.
Example: The Parícutin volcano in Mexico.
Composite volcanoes are formed by alternating layers of lava, volcanic ash, cinders, blocks, and bombs. They are often steep-sided and have symmetrical cones. The cone is often destroyed when the volcano becomes inactive and hardened magma blocks the opening.
Example: Mount Fuji in Japan.
Shield volcanoes consist mostly of fluid lava flow and are shaped (unsurprisingly!) like a shield. Basaltic lava pours out in different directions from the opening or a group of openings. This builds a gently sloping surface. Shield volcanoes are more common in oceanic settings rather than continental.
Example: Mauna Loa, Hawaii, is the world’s largest shield volcano.
Lava domes are formed by lava that is too viscous to flow far. The lava often remains around the vent, building the volcano from within. This process includes the outer surface hardening, breaking, and falling down the volcano’s sides. Lava domes are sometimes formed within the crater of a previous volcanic eruption.
Example: Mount Pelée in Martinique.
Let’s see how different plate margins affect the magnitude and type of volcanic eruption.
Volcanoes are generally small at divergent margins because basalt lava has a high viscosity and low gas content. Currently, there are around 100 volcanoes at divergent plate margins. Some of these are extinct, but over 30 are still active.
Volcanoes at convergent plate margins tend to erupt frequently and with high force. This is because the magma from the process of subduction has high gas and silica content. Ocean-ocean convergent plate margins tend to consist of volcanic islands.
The volcanoes formed at the ocean-ocean convergent plate margins are called island-arc volcanoes. The volcanoes formed at the ocean-continent convergent plate margins are called Andean-type volcanoes.
Volcanoes formed at the ocean-ocean convergent plate margins are called island-arc volcanoes.
The volcanoes formed at the ocean-continent convergent plate margins are called Andean-type volcanoes.
The harmful effects of volcanoes include lava flows, pyroclastic flows, ash falls, gas eruptions, and further secondary hazards.
Volcanoes can erupt with lava flow (molten rock) and damage nearby infrastructure. However, these lava flows tend to travel slowly, which gives time for evacuation. The lava will destroy anything in its path by burning, burying, or knocking it down.
Pyroclastic flows are eruptions of rock, ash, and gas that are superheated. They can travel at 80km/h, significantly faster than lava flows. This means that they can travel a long way with little warning. They can threaten nearby people and cause widespread death and destruction through burning.
Ash falls are eruptions of ash clouds caused by the expansion of gas in the volcano. Ash falls do not tend to endanger human life but can cause issues with aviation, infrastructure, and contamination to water and agriculture.
Gas eruptions escape through soil, lava, or vents and include gases such as carbon dioxide, sulphur dioxide, hydrogen, hydrogen sulphide, and carbon monoxide. These can impact the climate and cause irritations, poisoning, breathing issues, and acidic rain.
Let’s assess two types of secondary hazards from volcanoes: lahars and Jökulhlaups.
Lahars are secondary hazards that are caused by the mixtures of volcanic material and water. They are mud and debris flows that create threats nearby the volcanoes, but they can also travel far from volcanoes along rivers and cause issues further away. They can bury or destroy natural habitats, settlements, and infrastructure. They can also generate tsunamis when they enter the sea.
Jökulhlaups are sudden floods of water from glaciers, which can be caused by volcanic eruptions under a glacier. Therefore, they are potential secondary hazards caused by volcanic eruptions.
See our explanation on Tsunamis and how volcanoes can cause them.
The majority of volcanoes are formed at convergent plate margins where subduction occurs. As the denser plate sinks beneath the less dense plate, the temperature and pressure increase. The increase in temperature and pressure causes rocks to release water, resulting in a reduction in the melting point of the rock above. This creates magma, which rises to the surface, forming a volcano.
Volcanoes are openings of the Earth’s crust to the molten rock below the surface of the Earth.
Volcanoes erupt at convergent plate margins where subduction occurs. As the denser plate sinks beneath the less dense plate, the temperature and pressure increase. The increase in temperature and pressure causes rocks to release water, resulting in a reduction in the melting point of the rock above. This creates magma, which rises to the surface, forming a volcano.
We have volcanoes because of convergent plate margins where subduction occurs.
Volcanoes work by forming at convergent plate margins where subduction occurs. As the denser plate sinks beneath the less dense plate, the temperature and pressure increase. The increase in temperature and pressure causes rocks to release water, resulting in a reduction in the melting point of the rock above. This creates magma, which rises to the surface, forming a volcano.
What are volcanoes?
Volcanoes are openings of the Earth’s crust to the molten rock below the surface of the Earth.
How are volcanoes formed at convergent plate margins?
Volcanoes are formed at convergent plate margins due to the process of subduction. As the denser plate sinks, the temperature and pressure increase. The increase in temperature and pressure causes rocks to release water, resulting in a reduction in the melting point of the rock above. This forms magma, which rises to the surface, forming a volcano.
How are cinder cones formed?
Cinder cones are formed by the particles from lava that erupt from a single opening. In the process of the gaseous lava being ejected into the air, small fragments solidify, forming cinder. This falls around the opening and forms a circular or oval cone.
How are composite volcanoes formed?
Composite volcanoes are formed by alternating layers of lava, volcanic ash, cinders, blocks, and bombs. They are often steep-sided and symmetrical cones.
How are shield volcanoes formed?
Shield volcanoes are formed by fluid lava flow. Lava pours out in different directions from the opening or a group of openings. This builds a gently sloping surface.
How are lava domes formed?
Lava domes are formed by lava that is too viscous to flow far. Therefore, the lava often remains around the vent, building the volcano from within. This process includes the outer surface hardening, breaking, and falling down the sides of the volcano.
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