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Cinder conesĬinder cones are relatively small volcanoes made from loose volcanic material. This type of eruption can produce lava fountains that can be hundreds of metres tall and travel at speeds of up to 100 metres per second. Other volcanoes around the world also exhibit gentle Hawaiian eruptions. The best known are the Hawaiian volcanoes such as Mauna Loa, Mauna Kea and Kīauea. Shield volcanoes are typically located on hot spots found across tectonic plates rather than at the boundaries. This type of eruption is known as strombolian and is exhibited by other volcanoes around the world, such as by Mount Erebus in Antarctica. Mildly explosive blasts of magma - called fire fountains - consistently occur from a few minutes to a few hours apart. This island volcano has been exhibiting a pattern of eruption for 2,000 years.

Stromboli is another of Italy's active stratovolcanoes, but it behaves differently to Vesuvius. These types of eruptions can last for several days and cause a plume of superheated ash and gas that can expand and reach a height of 55 kilometres. This was a Plinian eruption, with jets of magma and gases emerging from the volcano at high speeds. Pyroclastic flow is a very hot mixture of ash, gases and other volcanic materials that moves at high speed along the flank of the volcano. Several settlements were destroyed by its pyroclastic flow, the most famous being the ancient Roman city of Pompeii. It may have killed more than 16,000 people in total. The violent 79 AD eruption of the still-active stratovolcano Mount Vesuvius in Italy is regarded as the deadliest in European history. Their lava is sticky (viscous), which means that it doesn't usually spread too far before cooling on the surface, giving the volcano a tall and cone-shaped profile. They mostly produce explosive eruptions and are most commonly associated with convergent plate boundaries. They are also known as composite volcanoes. Stratovolcanoes are steep-sloped and cone-shaped. Stratovolcanoes are the most common and perhaps most recognisable type of volcano. Volcanoes come in a variety of shapes and sizes, primarily caused by the different types of magma, but also by how volcanoes behave and where they're located. Volcanoes are typically high ground or mountains, sometimes with very steep sides made from the magma that erupted.

This mixture of materials is called magma while it's underground, lava when it is erupted and igneous rock once it's cooled and solidified on the surface. Volcanoes are an opening of the Earth's crust through which molten rock, gases and ash can escape.

How to cook coke without baking soda using vinegar