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Dawson Strait Group

Campo vulcanico · 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)
Tipo
Campo vulcanico
Paese
Papua New Guinea
Regione
Southwestern Pacific Volcanic Regions / Trobriand Volcanic Province
Altitudine
500 m
Coordinate
-9.620, 150.880
Ultima eruzione
1350
Contesto tettonico
Subduction zone / Continental crust (> 25 km)
Forma vulcanica
Cluster
Roccia principale
Rhyolite
Sintesi geologica

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.

Storia delle eruzioni

Riepilogo (VEI nel tempo)
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1350~1350 · 1 eruzioni · VEI max. ?13501350135113511351

Cronologia dettagliata

  1. 1350VEI ?Stima geologica
    1350 – In corso
    Oiau

Link esterni

⚠ Solo a scopo informativo. Non adatto a situazioni di emergenza.