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Anak Krakatau [notes 1] is a volcanic island in Indonesia. On 29 December 1927, Anak Krakatau first emerged from the caldera formed in 1883 by the explosive volcanic eruption that destroyed the island of Krakatoa .
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.
Krakatau; Metadata. This file contains additional information, probably added from the digital camera or scanner used to create or digitize it.
In the months leading up to the 2018 tsunami, Anak Krakatau had seen increased activity. Starting in June 2018, Anak Krakatau saw an increase of volcanic activity with a Strombolian eruption, producing lava flows and ash plumes as high as 5 km. One day prior to the collapse, on 21 December, an eruption was observed which lasted more than two ...
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The eruptions were initially of pumice and ash, and that island and the two islands that followed were quickly eroded away by the sea. Eventually a fourth island named Anak Krakatau (meaning "child of Krakatoa" in Indonesian) broke water in August 1930, and produced lava flows more quickly than the waves could erode them.
The Loudon and the W.H. Besse, at ~65 km north-northeast and ~80 km east-northeast of Krakatau respectively, were hit by strong winds and tephra. They were farther away than the scorched victims of the hot flows in Sumatra, so the ships and crew survived. [ 13 ]
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.