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Lolobau Island

Lolobau

Kaldera · Papua New Guinea · 878 m

Lolobau is located on the western rim of a 6-km-wide caldera, which formed about 12,000 years ago on the 8 x 13 km Lolobau Island. It is seen here from the south beyond the lower flanks of Ulawun. The smaller peak to the right is located along the eastern caldera rim.
Lolobau is located on the western rim of a 6-km-wide caldera, which formed about 12,000 years ago on the 8 x 13 km Lolobau Island. It is seen here from the south beyond the lower flanks of Ulawun. The smaller peak to the right is located along the eastern caldera rim. · Foto: Photo by Robert Citron, 1970 (Smithsonian Institution; courtesy of William Melson) · Wikimedia Commons
Tipe
Kaldera
Negara
Papua New Guinea
Wilayah
Southwestern Pacific Volcanic Regions / Bismarck Volcanic Arc
Ketinggian
878 m
Koordinat
-4.916, 151.162
Letusan terakhir
1912
Kondisi tektonik
Subduction zone / Continental crust (> 25 km)
Bentuk lahan
Caldera
Batuan utama
Basalt / Picro-Basalt
Ringkasan geologi

Lolobau volcano has grown over the W rim of a 6-km-wide caldera which formed about 12,000 years ago. The 8 x 13 km island is located just off the coast of eastern New Britain. A small lake occupies the SW part of the caldera. A small lava dome (Hulu) caps Mount Lolobau, which has a 0.8 x 1.1 km summit crater breached to the NE. Flank cones are found along the coast of the largely submerged volcano. Several vents within the caldera, on the E flank of the main edifice, have been active during historical time. The latest eruptions took place during the early 20th century.

Ringkasan Wikipedia

Ringkasan Inggris

Lolobau Island is an island in the Bismarck Sea, within the West New Britain Province of the Islands Region, in northern Papua New Guinea.

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Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu
1100~1181 · 1 letusan · VEI maks. 41830~1911 · 3 letusan · VEI maks. 411001262150616681830

Garis waktu rinci

  1. 1911VEI 4Teramati
    1911 – 1912
    East flank (Sili)
  2. 1908VEI ?Perkiraan geologi
    1908 – Berlangsung
  3. 1904VEI 4Teramati
    1904-08-09 – 1905-10-18
    East flank (Sili, Malo), Hulu ?
  4. 1100 (±30 tahun)VEI 4Perkiraan geologi
    1100 – Berlangsung
    Hulu

Tautan eksternal

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