Cile · Kerucut piroklastik
Reclus
- Tipe
- Kerucut piroklastik
- Ketinggian
- 1403 m
- Letusan terakhir
- 1908
- Tipe
- Kerucut piroklastik
- Negara
- Cile
- Wilayah
- Amerika Selatan / Austral Andean Volcanic Arc
- Ketinggian
- 1403 m
- Koordinat
- -50.940, -73.580
- Letusan terakhir
- 1908
- Kondisi tektonik
- Zona subduksi / Kerak benua (> 25 km)
- Bentuk lahan
- Komposit
- Batuan utama
- Dasit
Ringkasan geologi
Reclus, the source of several Patagonian Holocene tephra layers, was recognized to be an independent volcanic edifice in 1987. The volcano consists of a large dacitic pyroclastic cone with a crater about 1 km in diameter. As many as six tephra layers overlie a peat layer dated at 3,780 years before present. Research has also revealed evidence for eruptions in the 19th and early 20th centuries.
Ringkasan Wikipedia
Ringkasan InggrisReclus, also written as Reclús, is a cinder cone and stratovolcano located in the Southern Patagonian Ice Field, Chile. Part of the Austral Volcanic Zone of the Andes, its summit rises 1,000 metres (3,300 ft) above sea level and is capped by a crater about 1 kilometre (0.62 mi) wide. Close to the volcano lies the Amalia Glacier, which is actively eroding Reclus.
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Riwayat letusan
4 tercatatGlosariumGaris waktu rinci
- 1908 (±1 tahun)VEI 1Teramati1908-07-02 – akhir tidak diketahui
- 1879VEI 2Teramati1879-07-02 – akhir tidak diketahui
- 1869VEI 2Teramati1869-07-02 – akhir tidak diketahui
- 1830 SMVEI ?Perkiraan geologi1830 SM – akhir tidak diketahui
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