Cile · Stratovolkan
Monte Burney
Burney, Monte
- Tipe
- Stratovolkan
- Ketinggian
- 1758 m
- Letusan terakhir
- 1910
- Tipe
- Stratovolkan
- Negara
- Cile
- Wilayah
- Amerika Selatan / Austral Andean Volcanic Arc
- Ketinggian
- 1758 m
- Koordinat
- -52.330, -73.400
- Letusan terakhir
- 1910
- Kondisi tektonik
- Zona subduksi / Kerak benua (> 25 km)
- Bentuk lahan
- Komposit
- Batuan utama
- Andesit / Andesit basaltik
Ringkasan geologi
Monte Burney, a large ice-covered volcano in the Patagonian region of Chile, lies about 200 km NW of the town of Punta Arenas. It was constructed on the western rim of a 6-km-wide caldera, which is partially filled with and surrounded by an unglaciated pyroclastic-flow deposit. Flank vents produced andesitic-dacitic lava flows and pyroclastic material. Collapse of the edifice produced a major debris avalanche that traveled to the SSW. Two large Plinian eruptions have been documented during the Holocene. The only known historical eruption took place in 1910.
Ringkasan Wikipedia
Ringkasan InggrisMonte Burney is a volcano in southern Chile, part of its Austral Volcanic Zone which consists of six volcanoes with activity during the Quaternary. This volcanism is linked to the subduction of the Antarctic Plate beneath the South America Plate and the Scotia Plate.
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Riwayat letusan
7 tercatatGlosariumGaris waktu rinci
- 1910VEI 2Teramati1910-03-16 – akhir tidak diketahui
- 90 SM (±100 tahun)VEI ?Perkiraan geologi90 SM – akhir tidak diketahui
- 800 SM (±500 tahun)VEI ?Perkiraan geologi800 SM – akhir tidak diketahui
- 2320 SM (±100 tahun)VEI 5Perkiraan geologi2320 SM – akhir tidak diketahui
- 3740 SM (±10 tahun)VEI ?Perkiraan geologi3740 SM – akhir tidak diketahui
- 7390 SM (±200 tahun)VEI ?Perkiraan geologi7390 SM – akhir tidak diketahui
- 7450 SM (±500 tahun)VEI 5Perkiraan geologi7450 SM – akhir tidak diketahui
Gunung api terdekat
Tautan eksternal
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