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1883 Eruption of Krakatoa

Volcanology

The volcanic island's most violent eruption on August 27, 1883, rated 6 on the Volcanic Explosivity Index, was heard thousands of kilometers away and generated tsunamis that caused the great majority of its recorded deaths. It remains a reference case for how a single eruption can affect global climate and ocean behavior. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

Facts
Event Date
1883-08-27 1
Magnitude or Scale
Volcanic Explosivity Index (VEI) 6 1
Death Toll
At least 36,417, most from the tsunamis the eruption generated 1
Location
Krakatoa, Sunda Strait, Dutch East Indies (present day Indonesia) 1
Connections

Associated With

Volcanic Explosivity Index, Concepts

Rated Volcanic Explosivity Index 6.

Source Volcanic Explosivity Index (Wikipedia)
Volcano, Phenomena

The 1883 eruption of Krakatoa is a defining case study in explosive volcanism and global climatic effects.

Caused By

Volcanism, Processes

Read from this phenomenon's own Wikipedia article (1883 Eruption of Krakatoa); earth5 pass cause judgment: Volcanism.

Source 1883 Eruption of Krakatoa (Wikipedia)

In Discipline

Source 1883 Eruption of Krakatoa (Wikipedia)
In the Other Atlases

Found In

Also in Geography Atlas: where this subject is found.

Sources
1. 1883 Eruption of Krakatoa (Wikipedia)
Wikimedia Foundation
  • Lead section
    Between 19 May and 21 October 1883, the volcanic island of Krakatoa (located in the Sunda Strait, then part of the Dutch East Indies-modern-day Indonesia) began erupting, lasting more than five months.
  • In Group: Major Volcanic Eruptions, Lead sentence
    On 27 August, the island had its most significant eruption, which destroyed over 70% of the island and its surrounding archipelago, the island collapsing into a caldera.
View the Source
Volcanic Explosivity Index (Wikipedia)
Wikimedia FoundationAssociated With: Volcanic Explosivity IndexView the Source
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