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Papua New Guinea · Stratovolcano

Lolo

Type
Stratovolcano
Elevation
796m
Last eruption
Unknown
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. · Photo: Photo by Elliot Endo, 2002 (U.S. Geological Survey).
Type
Stratovolcano
Country
Papua New Guinea
Region
Southwestern Pacific / Bismarck Volcanic Arc
Elevation
796m
Coordinates
-5.466, 150.509
Last eruption
Unknown
Tectonic setting
Subduction zone / Continental crust (> 25 km)
Landform
Composite
Major rock type
Andesite / Basaltic andesite

Geological summary

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.

Excerpt from the Global Volcanism Program, Smithsonian Institution · Read the full summary on GVP →

Eruption history

Glossary

Detailed timeline

No eruption records available.

Nearby volcanoes

External links

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