Pulau Kadovar
Kadovar
Stratovolkan · Papua New Guinea · 365 m
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- Tipe
- Stratovolkan
- Negara
- Papua New Guinea
- Wilayah
- Southwestern Pacific Volcanic Regions / Bismarck Volcanic Arc
- Ketinggian
- 365 m
- Koordinat
- -3.608, 144.588
- Letusan terakhir
- 2023
- Kondisi tektonik
- Subduction zone / Continental crust (> 25 km)
- Bentuk lahan
- Composite
- Batuan utama
- Andesite / Basaltic Andesite
Ringkasan geologi
The 2-km-wide island of Kadovar is the emergent summit of a Bismarck Sea stratovolcano of Holocene age. It is part of the Schouten Islands, and lies off the coast of New Guinea, about 25 km N of the mouth of the Sepik River. Prior to an eruption that began in 2018, a lava dome formed the high point of the andesitic volcano, filling an arcuate landslide scarp open to the south; submarine debris-avalanche deposits occur in that direction. Thick lava flows with columnar jointing forms low cliffs along the coast. The youthful island lacks fringing or offshore reefs. A period of heightened thermal phenomena took place in 1976. An eruption began in January 2018 that included lava effusion from vents at the summit and at the E coast.
Ringkasan Wikipedia
Kadovar adalah sebuah pulau vulkanik di Papua Nugini, tepatnya di timur laut Pulau Papua yang jauh lebih besar. Gunung berapi di pulau ini meletus pada bulan Januari 2018 dan letusan masih berlangsung hingga tahun 2023, meskipun tingkat aktivitasnya secara umum dianggap rendah. Ada beberapa fenomena termal yang meningkat pada tahun 1976.
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Riwayat letusan
Garis waktu rinci
- 2018VEI 2Teramati2018-01-05 – 2023-05-14Summit and SE flank
- 1700VEI ?Perkiraan geologi1700-04 – Berlangsung
Tautan eksternal
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