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Lithograph of the eruption c. 1888. The 1883 eruption of Krakatoa (Indonesian: Letusan Krakatau 1883) in the Sunda Strait occurred from 20 May until 21 October 1883, peaking in the late morning of 27 August when over 70% of the island of Krakatoa and its surrounding archipelago were destroyed as it collapsed into a caldera.
Krakatoa (/ ˌ k r ɑː k ə ˈ t oʊ ə, ˌ k r æ k-/), also transcribed Krakatau (/-ˈ t aʊ /), is a caldera [1] in the Sunda Strait between the islands of Java and Sumatra in the Indonesian province of Lampung.
Rakata (/ r ə ˈ k ɑː t ə / rə-KAH-tə), also called Greater Krakatau, is a partially collapsed and uninhabited stratovolcano on the Indonesian island of Krakatoa (Indonesian: Krakatau) in the Sunda Strait between the islands of Sumatra and Java.
Krakatoa is an active stratovolcano located in Indonesia, and lying on the far western rim of the Pacific Ring of Fire. Krakatoa is a notably powerful volcano, with the 1883 eruption being one of the deadliest and most destructive volcanic events in all of recorded history.
A new parasitic cone, called Anak Krakatau (or the child of Krakatau), rose from the sea at the centre of the caldera in 1930. [14] The other Krakatau islets from the 1883 eruptions are known as Sertung, Panjang and Rakata. Java is a relatively small island compared to Sumatra, but it has a higher concentration of active volcanoes.
Molten lava and boulders rained down from the sides of Anak Krakatau – dubbed the “child” of the legendary Indonesian volcano – on July 18.A tour group from Aventure et Volcans were on ...
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The New Flora of the Volcanic Island of Krakatau, (reissued by Cambridge University Press 2009, ISBN 978-1-108-00433-6) [1] C. A. Backer; The Problem of Krakatao as Seen By a Botanist (1929). Examines the "Krakatau problem"- whether or not all life was destroyed by the 1883 eruption. [2] Rupert Furneaux; Krakatoa (1964).