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Papúa Nueva Guinea · Estratovolcán

Lolo

Tipo
Estratovolcán
Altitud
796 m
Última erupción
Desconocido
Lolo rises to the N beyond lava flows producing gas plumes during the 2002 eruption of Pago. Lolo is located N of Pago volcano along the N coast of New Britain, near Cape Hoskins. It is of late Pleistocene or Holocene age and overlaps the older Kapberg volcano on its W side. Lolo contains a 250-m-wide and 60-m-deep crater.
Lolo rises to the N beyond lava flows producing gas plumes during the 2002 eruption of Pago. Lolo is located N of Pago volcano along the N coast of New Britain, near Cape Hoskins. It is of late Pleistocene or Holocene age and overlaps the older Kapberg volcano on its W side. Lolo contains a 250-m-wide and 60-m-deep crater. · Foto: Photo by Elliot Endo, 2002 (U.S. Geological Survey).
Tipo
Estratovolcán
País
Papúa Nueva Guinea
Región
Pacífico Suroccidental / Bismarck Volcanic Arc
Altitud
796 m
Coordenadas
-5.466, 150.509
Última erupción
Desconocido
Contexto tectónico
Zona de subducción / Corteza continental (> 25 km)
Forma volcánica
Compuesto
Roca principal
Andesita / Andesita basáltica

Resumen geológico

Original en inglés

Lolo is a nearly symmetrical andesitic stratovolcano, ~3.5 km in diameter, located N of Witori volcano along the N coast of New Britain near Cape Hoskins.

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.