Murray

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)

Stratovolcano

Nadmořská výška

2 254 m

Poloha

-6,750°, 144,020°

The Pleistocene Mt. Murray stratovolcano straddles WNW-trending limestone ridges and contains a 6-km-wide crater breached to the south that may have originated from slope failure (Johnson, 1987). Two cones are situated on the NE and SE flanks.

Text: Smithsonian Global Volcanism Program.

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