Krakatau archipelago in the context of "Rakata"

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⭐ Core Definition: Krakatau archipelago

The Krakatoa Archipelago is a small uninhabited archipelago of volcanic islands formed by the Krakatoa stratovolcano located in the Sunda Strait, nestled between the much larger islands of Java and Sumatra. As of 2018, the archipelago consists of four main islands: Verlaten (a.k.a. Sertung) to the northwest, Lang (a.k.a. Rakata Kecil, or Panjang) to the northeast, Rakata (what remains the main island) to the south, and the currently volcanically active Anak Krakatoa in the north-centre. Together, the islands are a part of the Indonesian island arc system, created by the northeastward subduction of the Indo-Australian Plate. As part of a dynamic volcanic system, the islands have been continuously reshaped throughout recorded history, most notably in the 1883 eruption of Krakatoa.

Administratively, the Krakatoa Archipelago lies entirely within Lampung, Indonesia and forms a part of Ujung Kulon National Park.

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👉 Krakatau archipelago in the context of Rakata

Rakata (/rəˈkɑːtə/ 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. Standing 813 m (2,667 ft) tall, it was the largest and southernmost of three volcanoes that formed the island of Krakatoa (the others being Danan (volcano) and Perboewatan) and the only one of the volcanoes not totally destroyed in the 1883 eruption. Rakata is the last remnant of the original island prior to its destruction. However, Rakata did lose its northern half in that eruption, leaving just its southern half. The exposed cliff is quite striking visually, partially of a large exposed dike terminating in a large lenticular extrusion at the middle of the almost vertical cliff. The feature has been called "the Eye of Krakatoa."

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Krakatau archipelago in the context of 1883 eruption of Krakatoa

Between 20 May and 21 October 1883, the volcanic island of Krakatau, located in the Sunda Strait, erupted. On 27 August, the island had its most significant eruption, which destroyed over 70% of the island and its surrounding archipelago, afterwards collapsing itself into a caldera. The 27 August eruption had an estimated Volcanic Explosivity Index (VEI) of 6, and is one of the deadliest and most destructive volcanic events in recorded history; the third explosion of that day, which occurred at 10:02 am, remains the loudest known sound in history.

The explosion was heard 3,110 kilometres (1,930 mi) away in Perth, Western Australia, and Rodrigues near Mauritius, 4,800 kilometres (3,000 mi) away. The acoustic pressure wave circled the globe more than three times. At least 36,417 deaths are attributed to the eruption and the tsunamis it created. Significant additional effects were felt worldwide in the days and weeks after the volcano's eruption. Additional seismic activity was reported until February 1884, but any reports after October 1883 were dismissed by Rogier Verbeek's subsequent investigation into the eruption.

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