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Different types of volcanoes erupt differently due to different compositions of the magma chambers as well as differnt magma types being present within the volcanoes. The three main types of magma are Basalt, Andesite, and Rhyolite. These erupt in very different manners.

  1. Basalt - Basalt eruptions are ften known as Hawaiian style eruptions, they are categorized by curtains of fire and long rift zones. The magma itself is very fluid in nature, it does not readily trap gasses to explosive levels and therefore has very placid and erupts in flows and layers. Volcanoes of this type are known as shield volcanoes.
  2. Andesite - This is an intermediate magma in its viscosity, it will flow but not as well as basalt does. This magma also has the ability to trap dissolved gasses to explosive levels. It is an intermediate viscosity and a volcano of this type would be a stratovolcano or cinder cones.
  3. Rhyolite - The most viscous basic form of magma, it does not want to flow and will build into lava domes around active vents. This magma is known for its ability to drive very powerful explosions through its ability to maintian dissolved gas and only let it escape through explosive decompression. A volcano of this type can be a Stratovolcano or a Caldera.
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Q: Why eruption of each volcano different?
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