Biwau Hills

sopka (bez známé erupce za posledních ~12 000 let), Papua New Guinea, Southwestern Pacific Volcanic Regions

Kde

Papua New Guinea, Southwestern Pacific Volcanic Regions

Typ (GVP)

Pyroclastic cone(s)

Nadmořská výška

400 m

Poloha

-7,320°, 143,280°

The Pleistocene Mt. Biwau consists of two coalescing cones surrounded by lavas and probable lahar deposits. The northern cone is capped by a spine-like peak and a dome-like protuberance 1.5 km to the east. A small cinder cone lies 17 km to the west (Mackenzie and Johnson 1984).

Text: Smithsonian Global Volcanism Program.

Údaje o sopce: Smithsonian Global Volcanism Program. Další sopky a průduchy.