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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]
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 ]
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 ...
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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 ...
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.
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.