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http://www.livescience.com/28186-krakatoa.html

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the 1883 eruption of Krakatua is thought of as the loudest sound heard in modern history. It killed 36,000 people because it triggered tsunamis and destroyed two thirds of the island.

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Krakatua is known for it's frequent and violent eruptions. It's last eruption was on March 31, 2014.

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Krakatua is an example of a tall stratovolcano. Meaning it is built up from previous eruptions and made from layers of lava and ash and has a steep incline upward.

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The Indo-Australian Plate and the Sunda Plate are the two plates involved. The Indo-Australian Plate is being subducted under the Sunda Plate because the two plates are converging.

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Rhyolite is found at convergent plate boundaries therefore; we can incur that Krakatua was formed as a result of rising crust material that has been melted in the core.

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Krakatua has a silica value of 67.3%. This means it's rock type is rhyolite.

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Krakatua is located in the Lampung Province in Indonesia.