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Geological Formation

Krakatoa

Volcanic Formations

Krakatoa is a caldera in the Sunda Strait between Java and Sumatra, in Indonesia's Lampung province, sitting above a subduction zone where the Eurasian and Indo-Australian plates meet at a sharp bend that leaves the crust there unusually weak. Its catastrophic eruption of August 26-27, 1883, ejected an estimated 25 cubic kilometers of rock, was heard as far away as Australia, and killed at least 36,417 people, mostly through tsunamis, destroying two-thirds of the original island; Rakata is the only remnant of that island to survive. In 1927 a new volcanic cone, Anak Krakatau, meaning Child of Krakatoa, emerged from the caldera and has erupted periodically since, including a 2018 flank collapse that triggered a deadly tsunami, with further eruptive activity recorded into the 2020s.

Facts
Classification
Protected Status
National Park or Reserve 1
Protected Status
UNESCO World Heritage Site 1
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Caused By

Volcanism, Processes
Source Krakatoa (Wikipedia)

In Discipline

Source Krakatoa (Wikipedia)
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Sources
1. Krakatoa (Wikipedia)
  • Protection
    In 1991, "Ujung Kulon National Park and Krakatau Nature Reserve" was inscribed as an UNESCO World Heritage Site, matching Natural criteria (vii) and (x).
  • In Discipline: Volcanology, Lead paragraph
    Krakatoa (), also transcribed Krakatau (), is a caldera in the Sunda Strait between the islands of Java and Sumatra in the Indonesian province of Lampung
  • Caused By: Volcanism, Lead paragraph
    Krakatoa (), also transcribed Krakatau (), is a caldera in the Sunda Strait between the islands of Java and Sumatra in the Indonesian province of Lampung
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Wikidata: Krakatoa
Wikidata Q82613, class allow-list match (w-wdresolver-0926)View the Source
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