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Reclus

Kerucut piroklastik · Chile · 1403 m

Amalia Glacier flows around the northern flank of Reclus in the Southern Patagonia Ice Field, shown in this 27 February 2018 PlanetScope satellite image (N is at the top; this image is approximately 8 km across). The flanks are heavily eroded and there is a landslide deposit from the northern flank on the glacier surface.
Amalia Glacier flows around the northern flank of Reclus in the Southern Patagonia Ice Field, shown in this 27 February 2018 PlanetScope satellite image (N is at the top; this image is approximately 8 km across). The flanks are heavily eroded and there is a landslide deposit from the northern flank on the glacier surface. · Foto: Satellite image courtesy of Planet Labs Inc., 2018 (https://www.planet.com/). · Wikimedia Commons
Tipe
Kerucut piroklastik
Negara
Chile
Wilayah
Amerika Selatan / Austral Andean Volcanic Arc
Ketinggian
1403 m
Koordinat
-50.940, -73.580
Letusan terakhir
1908
Kondisi tektonik
Subduction zone / Continental crust (> 25 km)
Bentuk lahan
Composite
Batuan utama
Dacite
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.

Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu
1830 BCE~1633 BCE · 1 letusan · VEI maks. ?1711~1908 · 3 letusan · VEI maks. 21830 BCE846 BCE59 BCE9241711

Garis waktu rinci

  1. 1908 (±1 tahun)VEI 1Teramati
    1908-07-02 – Berlangsung
  2. 1879VEI 2Teramati
    1879-07-02 – Berlangsung
  3. 1869VEI 2Teramati
    1869-07-02 – Berlangsung
  4. 1830 SMVEI ?Perkiraan geologi
    BCE 1830 – Berlangsung

Tautan eksternal

⚠ Untuk referensi saja. Bukan untuk tanggap darurat.