Bristol Island
Stratovolkan · United Kingdom · 1100 m

- Tipe
- Stratovolkan
- Negara
- United Kingdom
- Wilayah
- Antarctic-Scotia Volcanic Regions / South Sandwich Volcanic Arc
- Ketinggian
- 1100 m
- Koordinat
- -59.017, -26.533
- Letusan terakhir
- 2016
- Kondisi tektonik
- Subduction zone / Oceanic crust (< 15 km)
- Bentuk lahan
- Composite
- Batuan utama
- Basalt / Picro-Basalt
Ringkasan geologi
The 9 x 10 km Bristol Island near the southern end of the South Sandwich arc lies across Fortser's Passage from the Southern Thule Islands and forms one of the largest islands of the chain. Largely glacier-covered, it contains a horseshoe-shaped ridge at the interior extending northward from the highest peak, 1100-m-high Mount Darnley. A steep-sided flank cone or lava dome, Havfruen Peak, is located on the east side, and a young crater and fissure are on the west flank. Three large sea stacks lying off Turmoil Point at the western tip of the island may be remnants of an older now-eroded volcanic center. Both summit and flank vents have been active during historical time. The latest eruption, during 1956, originated from the west-flank crater, and deposited cinder over the icecap. The extensive icecap and the difficulty of landing make it the least explored of the South Sandwich Islands.
Ringkasan Wikipedia
Ringkasan InggrisBristol Island is an uninhabited island in the South Sandwich Islands, an archipelago in the Southern Ocean. The island is almost entirely surrounded by ice cliffs and largely covered with ice. It features both the oldest rocks of this archipelago and an active volcano that last erupted in 2016.
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Riwayat letusan
Garis waktu rinci
- 2016VEI 1Teramati2016-04-24 – 2016-07-26Main crater, Mt. Sourabaya
- 1956VEI 3Teramati1956-01-11 – 1956-01-19West flank
- 1950VEI 2Teramati1950-03-27 – Berlangsung
- 1936VEI 2Teramati1936-12-18 – 1937-01-01
- 1935VEI 2Teramati1935-12-31 – Berlangsung
- 1823VEI 2Teramati1823 – Berlangsung
Tautan eksternal
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