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Antarctica · Stratovolcano

Penguin Island

Type
Stratovolcano
Elevation
180m
Last eruption
1905
Penguin Island
Photo: NSF · Public domain · Wikimedia Commons
Type
Stratovolcano
Country
Antarctica
Region
Antarctic & Scotia / South Shetlands Volcanic Arc
Elevation
180m
Coordinates
-62.100, -57.930
Last eruption
1905
Tectonic setting
Intraplate / Continental crust (> 25 km)
Landform
Composite
Major rock type
Basalt / Picro-basalt
Geological summary

The 1.4 x 1.7 km Penguin Island is located off the SE coast of King George Island in Antarctica's South Shetland Islands, west of the axis of the Bransfield Rift. The most prominent feature is Deacon Peak, a basaltic scoria cone with a 350-m-wide summit crater on the SW side of the island. A small plug of basaltic lava occupies the 75-m-deep crater. Petrel Crater, a 300-m-wide maar, is located near the east coast. The formation of Deacon Peak was dated by lichenometry at about 300 years ago, and the younger Petrel Crater maar was dated at about 100 years (Birkenmajer, 1979). Some reports of fumarolic activity on nearby Bridgeman Island are attributed to the more youthful Penguin Island.

From Wikipedia

Penguin Island is one of the smaller of the South Shetland Islands of Antarctica.

Wikipedia · CC BY-SA · Read full article →

Eruption history

3 recordedGlossary
Summary (VEI over time)
Click a bar to see individual eruptions · Use arrow keys to move between bars, Enter to open
1683~1705 · 1 eruptions · max VEI ?1838~1861 · 1 eruptions · max VEI ?1883~1905 · 1 eruptions · max VEI ?16831727179418381883

Detailed timeline

  1. 1905VEI ?Geological estimate
    1905-07-02 – end unknown
    NE flank (Petrel Crater)
  2. 1850VEI ?Observed
    1850-07-02 – end unknown
    Deacon Peak
  3. 1683VEI ?Geological estimate
    1683 – end unknown
    Deacon Peak

Nearby volcanoes

External links

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