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Lolo

Stratovolkan · Papua New Guinea · 796 m

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).
Tipe
Stratovolkan
Negara
Papua New Guinea
Wilayah
Southwestern Pacific Volcanic Regions / Bismarck Volcanic Arc
Ketinggian
796 m
Koordinat
-5.466, 150.509
Letusan terakhir
Tidak diketahui
Kondisi tektonik
Subduction zone / Continental crust (> 25 km)
Bentuk lahan
Composite
Batuan utama
Andesite / Basaltic Andesite
Ringkasan geologi

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.

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