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Lolo

Stratovolcano · Papua New Guinea · 796m

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 Volcanic Regions / 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. It is of very late Pleistocene or Holocene age and overlaps the older Kapberg volcano to the west (Blake and McDougall, 1973). Lava flows are prominent on its flanks, and a well-preserved crater 250 m wide and 60 m deep truncates the summit.

Eruption history

Detailed timeline

No eruption records available.

External links

⚠ For reference only. Not for emergency response.