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Antarktika · Stratovolkan

Penguin Island

Tipe
Stratovolkan
Ketinggian
180 m
Letusan terakhir
1905
Penguin Island
Foto: NSF · Public domain · Wikimedia Commons
Tipe
Stratovolkan
Negara
Antarktika
Wilayah
Antarktika & Scotia / South Shetlands Volcanic Arc
Ketinggian
180 m
Koordinat
-62.100, -57.930
Letusan terakhir
1905
Kondisi tektonik
Intralempeng / Kerak benua (> 25 km)
Bentuk lahan
Komposit
Batuan utama
Basal / Pikrobasal
Ringkasan geologi

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.

Ringkasan Wikipedia

Ringkasan Inggris

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

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Riwayat letusan

3 tercatatGlosarium
Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu · Gunakan tombol panah untuk berpindah batang, Enter untuk membuka
1683~1705 · 1 letusan · VEI maks. ?1838~1861 · 1 letusan · VEI maks. ?1883~1905 · 1 letusan · VEI maks. ?16831727179418381883

Garis waktu rinci

  1. 1905VEI ?Perkiraan geologi
    1905-07-02 – akhir tidak diketahui
    NE flank (Petrel Crater)
  2. 1850VEI ?Teramati
    1850-07-02 – akhir tidak diketahui
    Deacon Peak
  3. 1683VEI ?Perkiraan geologi
    1683 – akhir tidak diketahui
    Deacon Peak

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