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  2. Mount Sunda - Wikipedia

    en.wikipedia.org/wiki/Mount_Sunda

    The volcano formed the northern ridge of the Bandung Basin. The ancient volcano is the predecessor of today's Tangkuban Perahu, Burangrang, and Bukit Tunggul volcanoes. The Sunda volcano was a stratovolcano and is estimated to have reached up to 3,000–4,000 metres (9,850–13,100 ft) above sea level during the Pleistocene age. [1]

  3. Sunda Arc - Wikipedia

    en.wikipedia.org/wiki/Sunda_Arc

    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. The Sunda Arc begins at Sumatra and ends at Flores , and is adjacent to the Banda Arc . [ 1 ]

  4. List of volcanoes by elevation - Wikipedia

    en.wikipedia.org/wiki/List_of_volcanoes_by_elevation

    Mountain Metres Feet Location and Notes Ojos del Salado: 6,893: 22,615: Argentina/Chile – highest dormant volcano on Earth: Monte Pissis: 6,793: 22,287: Argentina Nevado Tres Cruces

  5. Galunggung - Wikipedia

    en.wikipedia.org/wiki/Galunggung

    Mount Galunggung is part of the Sunda Arc extending through Sumatra, Java and the Lesser Sunda Islands, which has resulted from the subduction of the Australian Plate beneath the Eurasian Plate. For the first time since 1982 after eruptions finished and conditions seemed normal, on February 12, 2012, the status was upgraded to Alert based on ...

  6. Timeline of volcanism on Earth - Wikipedia

    en.wikipedia.org/wiki/Timeline_of_volcanism_on_Earth

    Active volcanoes such as Stromboli, Mount Etna and KÄ«lauea do not appear on this list, but some back-arc basin volcanoes that generated calderas do appear. Some dangerous volcanoes in "populated areas" appear many times: Santorini six times, and Yellowstone hotspot 21 times.

  7. 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]

  8. Bandung - Wikipedia

    en.wikipedia.org/wiki/Bandung

    Geological data show that the Bandung Basin is located on an ancient volcano, known as Mount Sunda, erected up to 3,000–4,000 metres (9,800–13,100 feet) during the Pleistocene age. [32] Two large-scale eruptions took place; the first formed the basin, and the second (est. 55,000 BCE) blocked the Citarum river, turning the basin into a lake ...

  9. 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.