Penguin Island
Stratovolkan · Antarctica · 180 m
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- Tipe
- Stratovolkan
- Negara
- Antarctica
- Wilayah
- Antarctic-Scotia Volcanic Regions / South Shetlands Volcanic Arc
- Ketinggian
- 180 m
- Koordinat
- -62.100, -57.930
- Letusan terakhir
- 1905
- Kondisi tektonik
- Intraplate / Continental crust (> 25 km)
- Bentuk lahan
- Composite
- Batuan utama
- Basalt / Picro-Basalt
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 InggrisPenguin Island is one of the smaller of the South Shetland Islands of Antarctica.
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Riwayat letusan
Garis waktu rinci
- 1905VEI ?Perkiraan geologi1905 – BerlangsungNE flank (Petrel Crater)
- 1850VEI ?Teramati1850 – BerlangsungDeacon Peak
- 1683VEI ?Perkiraan geologi1683 – BerlangsungDeacon Peak
Tautan eksternal
⚠ Untuk referensi saja. Bukan untuk tanggap darurat.