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Bristol Island

Stratovolcano · United Kingdom · 1100m

The largely glacier-covered, 9 x 10 km Bristol Island is one of the largest of the South Sandwich Islands.  Both summit and flank vents on Bristol Island 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 on Bristol Island and the difficulty of landing make it the least explored of the South Sandwich Islands.
The largely glacier-covered, 9 x 10 km Bristol Island is one of the largest of the South Sandwich Islands. Both summit and flank vents on Bristol Island 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 on Bristol Island and the difficulty of landing make it the least explored of the South Sandwich Islands. · Photo: ASTER satellite image, 2002 (National Aeronautical and Space Administration, courtesy of ASTER science team). · Wikimedia Commons
Type
Stratovolcano
Country
United Kingdom
Region
Antarctic-Scotia Volcanic Regions / South Sandwich Volcanic Arc
Elevation
1100m
Coordinates
-59.017, -26.533
Last eruption
2016
Tectonic setting
Subduction zone / Oceanic crust (< 15 km)
Landform
Composite
Major rock type
Basalt / Picro-Basalt
Geological summary

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.

From Wikipedia

Bristol 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.

Wikipedia · CC BY-SA · Read full article

Eruption history

Summary (VEI over time)
Click a bar to see individual eruptions
1823~1842 · 1 eruptions · max VEI 21920~1939 · 2 eruptions · max VEI 21939~1958 · 2 eruptions · max VEI 31997~2016 · 1 eruptions · max VEI 118231862192019581997

Detailed timeline

  1. 2016VEI 1Observed
    2016-04-24 – 2016-07-26
    Main crater, Mt. Sourabaya
  2. 1956VEI 3Observed
    1956-01-11 – 1956-01-19
    West flank
  3. 1950VEI 2Observed
    1950-03-27 – Ongoing
  4. 1936VEI 2Observed
    1936-12-18 – 1937-01-01
  5. 1935VEI 2Observed
    1935-12-31 – Ongoing
  6. 1823VEI 2Observed
    1823 – Ongoing

External links

⚠ For reference only. Not for emergency response.