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Papúa Nueva Guinea · Campo volcánico

Garua Harbour

Tipo
Campo volcánico
Altitud
565 m
Última erupción
Desconocido
The Garua (Talasea) Harbour volcanic field (upper right center) consists of a group of mostly rhyolitic lava domes and ash cones that ring the harbor on the west and form Garua Island (right center) to the east. Active hot springs ring the shores of Garua Harbour, including a large group of boiling pools, fumaroles, and mudpots located near the Talasea Government Station on the south shore of the bay, directly opposite the western tip of Garua Island.
The Garua (Talasea) Harbour volcanic field (upper right center) consists of a group of mostly rhyolitic lava domes and ash cones that ring the harbor on the west and form Garua Island (right center) to the east. Active hot springs ring the shores of Garua Harbour, including a large group of boiling pools, fumaroles, and mudpots located near the Talasea Government Station on the south shore of the bay, directly opposite the western tip of Garua Island. · Foto: NASA Landsat image, 2000 (courtesy of Hawaii Synergy Project, Univ. of Hawaii Institute of Geophysics & Planetology).
Tipo
Campo volcánico
País
Papúa Nueva Guinea
Región
Pacífico Suroccidental / Bismarck Volcanic Arc
Altitud
565 m
Coordenadas
-5.300, 150.070
Última erupción
Desconocido
Contexto tectónico
Zona de subducción / Corteza continental (> 25 km)
Forma volcánica
Grupo volcánico
Roca principal
Riolita

Resumen geológico

Original en inglés

The Garua (Talasea) Harbour volcanic field consists of a group of lava domes and ash cones of possible Holocene age.

Extracto del Global Volcanism Program, Smithsonian Institution · Leer el resumen completo en el GVP →

Historial de erupciones

Glosario

Línea de tiempo detallada

No hay registros de erupciones disponibles.

Volcanes cercanos

Enlaces externos

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