Lolobau Island
Lolobau
Kaldera · Papua New Guinea · 878 m
- 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 InggrisLolobau Island is an island in the Bismarck Sea, within the West New Britain Province of the Islands Region, in northern Papua New Guinea.
Wikipedia · CC BY-SA · Baca artikel lengkap →
Riwayat letusan
Garis waktu rinci
- 1911VEI 4Teramati1911 – 1912East flank (Sili)
- 1908VEI ?Perkiraan geologi1908 – Berlangsung
- 1904VEI 4Teramati1904-08-09 – 1905-10-18East flank (Sili, Malo), Hulu ?
- 1100 (±30 tahun)VEI 4Perkiraan geologi1100 – BerlangsungHulu
Tautan eksternal
⚠ Untuk referensi saja. Bukan untuk tanggap darurat.