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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]
Sangeang Api (Gunung Api or Gunung Sangeang) is an active complex volcano on the island of Sangeang in Indonesia. It consists of two volcanic cones, 1,949 metres (6,394 ft) Doro Api and 1,795 m (5,889 ft) Doro Mantoi. [1] Sangeang Api is one of the most active volcanoes in the Lesser Sunda Islands.
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 ...
Location and Notes Mount Klabat: 1,995: ... Lesser Sunda Islands, Indonesia Mount Lamongan: ... A list (incomplete) of volcanoes on Earth arranged by elevation in ...
Mount St. Helens. Washington Elevation: 8,363 feet Mount St. Helens surprised locals and the world alike when it erupted on May 18, 1980, as many thought the volcano was extinct.A plume of ash and ...
Rajabasa is an isolated 1281-m-high conical volcano along the Sunda Strait at the most southeastern point of Sumatra. It has a well-preserved 500 x 700 m summit crater with a swampy floor. The volcano is covered with vegetation.
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.
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.