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  2. Mount Sunda - Wikipedia

    en.wikipedia.org/wiki/Mount_Sunda

    Mount Sunda was an ancient volcano that once stood in Priangan highlands in today's West Java province, Java island, Indonesia. The Sunda volcano existed during the Pleistocene age before a violent Plinian eruption caused its summit to collapse.

  3. Sunda Arc - Wikipedia

    en.wikipedia.org/wiki/Sunda_Arc

    Major Volcanoes - Merapi, Krakatoa, Mount Sinabung, Semeru The Sunda Arc is a volcanic arc that produced the volcanoes that form the topographic spine of the islands of Sumatra , Nusa Tenggara , Java , the Sunda Strait , and the Lesser Sunda Islands .

  4. Tangkuban Perahu - Wikipedia

    en.wikipedia.org/wiki/Tangkuban_Perahu

    Together with Mount Burangrang and Bukit Tunggul, it is a remnant of the ancient Mount Sunda after the plinian eruption caused the Caldera to collapse. In April 2005, the Directorate of Volcanology and Geological Hazard Mitigation raised an alert, forbidding visitors from going up the volcano.

  5. Krakatoa - Wikipedia

    en.wikipedia.org/wiki/Krakatoa

    A thundering sound was heard from the mountain Batuwara [now called Pulosari, an extinct volcano in Bantam, the nearest to the Sunda Strait] which was answered by a similar noise from Kapi, lying westward of the modern Bantam [ is the westernmost province in Java, so this seems to indicate that Krakatoa is meant]. A great glowing fire, which ...

  6. Mount Tambora - Wikipedia

    en.wikipedia.org/wiki/Mount_Tambora

    Mount Tambora, also known as Tomboro, [6] is situated in the northern part of Sumbawa island, part of the Lesser Sunda Islands. [7] It is a segment of the Sunda Arc, a chain of volcanic islands that make up the southern chain of the Indonesian archipelago. [8] Tambora forms its own peninsula on Sumbawa, known as the Sanggar peninsula.

  7. Lake Bandung - Wikipedia

    en.wikipedia.org/wiki/Lake_Bandung

    Lake Bandung (Sundanese: Situ Hiang) was a prehistoric lake located in and around the city of Bandung, Parahyangan highlands, West Java, Indonesia. believed to exist between 126,000 and 20,000 BCE in the Pleistocene due to the violent eruption of Mount Sunda that blocked the Citarum River, causing the lowlands to begin to be inundated with water, eventually forming a lake.

  8. 1883 eruption of Krakatoa - Wikipedia

    en.wikipedia.org/wiki/1883_eruption_of_Krakatoa

    A large area of the Sunda Strait and places on the Sumatran coast were affected by pyroclastic flows from the volcano. Verbeek and others believe that the final major Krakatoa eruption was a lateral blast, or pyroclastic surge. Material shot out of the volcano at 2,575 kilometres per hour (715 metres per second). [10]

  9. List of volcanoes in Indonesia - Wikipedia

    en.wikipedia.org/wiki/List_of_volcanoes_in_Indonesia

    Mahameru (Semeru) above Mount Bromo, East Java. East Indonesia Islands from ISS.Seven active volcanoes are visible: 5 in East Java, Agung in Bali and Rinjani in Lombok.. The geography of Indonesia is dominated by volcanoes that are formed due to subduction zones between the Eurasian plate and the Indo-Australian plate.