Krakatoa is a volcano in Indonesia.
Krakatoa may also refer to:
Krakatoa, also transcribed Krakatau, is a caldera in the Sunda Strait between the islands of Java and Sumatra in the Indonesian province of Lampung. The caldera is part of a volcanic island group comprising four islands. Two, Lang and Verlaten, are remnants of a previous volcanic edifice destroyed in eruptions long before the famous 1883 eruption; another, Rakata, is the remnant of a much larger island destroyed in the 1883 eruption.
The Sunda Strait is the strait between the Indonesian islands of Java and Sumatra. It connects the Java Sea with the Indian Ocean.
A phreatic eruption, also called a phreatic explosion, ultravulcanian eruption or steam-blast eruption, occurs when magma heats ground water or surface water. The extreme temperature of the magma causes near-instantaneous evaporation of water to steam, resulting in an explosion of steam, water, ash, rock, and volcanic bombs. At Mount St. Helens in Washington state, hundreds of steam explosions preceded the 1980 Plinian eruption of the volcano. A less intense geothermal event may result in a mud volcano.
Rakata, also called Greater Krakatau, is a partially collapsed stratovolcano on the Indonesian island of Krakatoa 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 Krakatoa and the only one 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."
Anak Krakatoa is an volcanic islands in the Sunda Strait between the islands of Java and Sumatra in the Indonesian province of Lampung. On 29 December 1927, Anak Krakatoa emerged from the caldera formed in 1883 by the explosive volcanic eruption that destroyed the island of Krakatoa.
Krakatoa, East of Java is a 1968 American disaster film starring Maximilian Schell and Brian Keith. During the 1970s, the film was re-released under the title Volcano.
A volcano is a geological landform usually generated by the eruption through a vent in a planet's surface of magma.
Krakatoa: The Last Days is a BBC Television docudrama that premiered on 7 May 2006 on BBC One. The program is based upon four eyewitness accounts of the 1883 eruption of Krakatoa, an active stratovolcano between the islands of Sumatra and Java, present day Indonesia.
Lang Island lies in the Sunda Strait, between Java and Sumatra, in Indonesia. It is one of the Krakatoa Archipelago, above the famous Krakatoa volcano. Lang suffered only slightly in the 1883 eruption of Krakatoa; it actually grew in area from massive pumice fall, although most of the additional area washed away within several years.
Sebesi is an Indonesian island in the Sunda Strait, between Java and Sumatra, and part of the province of Lampung. It rises to a height of 844 metres (2,769 ft) and lies about 12 kilometres (7.5 mi) north of the Krakatoa Archipelago; it is the closest large island to Krakatoa, about the same area and height as the remnant of Rakata. Like Krakatoa, it too is volcanic, although there are no dated eruptions known. Unlike the Krakatoa Archipelago, Sebesi has permanent streams and is inhabited.
Gouverneur Generaal Loudon was a mail steamer and excursion vessel which survived the 1883 eruption of Krakatoa.
Rogier Diederik Marius Verbeek was a Dutch geologist and natural scientist.
Panaitan is an island in the Sunda Strait, between Java and Sumatra, and in the Indonesian province of Banten. It is the largest island in the strait, and is located near the westernmost tip of Java. Like the nearby Krakatoa, it too is volcanic in origin, although there are no known historic eruptions. The name 'Prince's Island' apparently is because the island was considered the property of Javan princes. Administratively, the island is a part of Pandeglang Regency.
Sebuku is an island in the Sunda Strait between Java and Sumatra. It is one of the larger islands in the strait and lies just 2.5 kilometres (1.6 mi) to the north of Sebesi and 2.3 kilometres (1.4 mi) south of Sumatra. It is administratively part of South Lampung Regency, Lampung.
Krakatoa, in the Sunda Strait in Indonesia, has attracted a significant literature and media response to the 1883 eruption and subsequent events in the vicinity.
The 1883 eruption of Krakatoa in the Sunda Strait began on 20 May 1883 and peaked on the late morning of Monday, 27 August 1883, when over 70% of the island of Krakatoa and its surrounding archipelago were destroyed as it collapsed into a caldera.
Fair Wind to Java is a 1953 American adventure film in Trucolor from Republic Pictures, produced and directed by Joseph Kane, that stars Fred MacMurray and Vera Ralston. With special effects by the Lydecker brothers, the film was based on the 1948 novel of the same name by Garland Roark.
Drama dari Krakatau is a 1929 vernacular Malay novel written by Kwee Tek Hoay. Inspired by Edward Bulwer-Lytton's 1834 novel The Last Days of Pompeii and the 1883 eruption of Krakatoa, the sixteen-chapter book centres on two families in 1920s Batam that are unknowingly tied together by siblings who were separated in 1883. The brother becomes a political figure, while the sister marries a Baduy priest-king. Ultimately these families are reunited by the wedding of their children, after which the priest sacrifices himself to calm a stirring Krakatoa.
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, Lang, Rakata, and the currently volcanically active Anak Krakatoa. 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.