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Dawson Strait Group

Campo volcánico · 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 volcánico
País
Papua New Guinea
Región
Southwestern Pacific Volcanic Regions / Trobriand Volcanic Province
Altitud
500 m
Coordenadas
-9.620, 150.880
Última erupción
1350
Contexto tectónico
Subduction zone / Continental crust (> 25 km)
Forma volcánica
Cluster
Roca principal
Rhyolite
Resumen geológico

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.

Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
1350~1350 · 1 erupciones · VEI máx. ?13501350135113511351

Línea de tiempo detallada

  1. 1350VEI ?Estimación geológica
    1350 – En curso
    Oiau

Enlaces externos

⚠ Solo como referencia. No apto para respuesta ante emergencias.