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Dawson Strait Group

Medan gunung api · Papua New Guinea · 500 m

The Dawson Straits, seen in this NASA Landsat image, is located between eastern Fergusson Island (upper left) and northwestern Normanby Island (lower left) in the D'Entrecasteaux island group. The area contains a volcanic field with several young volcanic centers that erupted rhyolitic obsidian flows. Mount Oiau is located on the narrow peninsula (left center) forming the southernmost point on Fergusson Island. A large crater is visible on Dobu Island, southeast of Oiau. Young volcanic rocks are also found on Sanaroa Island (upper right).
The Dawson Straits, seen in this NASA Landsat image, is located between eastern Fergusson Island (upper left) and northwestern Normanby Island (lower left) in the D'Entrecasteaux island group. The area contains a volcanic field with several young volcanic centers that erupted rhyolitic obsidian flows. Mount Oiau is located on the narrow peninsula (left center) forming the southernmost point on Fergusson Island. A large crater is visible on Dobu Island, southeast of Oiau. Young volcanic rocks are also found on Sanaroa Island (upper right). · Foto: NASA Landsat 7 image (worldwind.arc.nasa.gov)
Tipe
Medan gunung api
Negara
Papua New Guinea
Wilayah
Southwestern Pacific Volcanic Regions / Trobriand Volcanic Province
Ketinggian
500 m
Koordinat
-9.620, 150.880
Letusan terakhir
1350
Kondisi tektonik
Subduction zone / Continental crust (> 25 km)
Bentuk lahan
Cluster
Batuan utama
Rhyolite
Ringkasan geologi

The Dawson Straits, located between eastern Fergusson and western Normanby Islands in the D'Entrecasteaux island group, contains a volcanic field with several centers that define a possible partly submerged caldera. There have been no historical eruptions, but morphology suggests an extremely young age for some lava flows, and the area displays vigorous thermal activity. The most prominent volcanic centers are Mounts Lamonai and Oiau, located about 10 km apart on the SW tip of Fergusson Island. The summit of Lamonai is capped by a steep-walled crater, and rhyolitic lava flows are exposed on the NE side of the cone. The dominantly volcaniclastic Oiau cone has also produced obsidian lava flows. Dobu Island to the south is formed of coalescing volcanic centers and likewise has produced youthful rhyolitic obsidian flows.

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Ringkasan (VEI dari waktu ke waktu)
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1350~1350 · 1 letusan · VEI maks. ?13501350135113511351

Garis waktu rinci

  1. 1350VEI ?Perkiraan geologi
    1350 – Berlangsung
    Oiau

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