Likuruanga | |
---|---|
Highest point | |
Elevation | 904 m (2,966 ft) |
Coordinates | 4°57′11″S 151°23′06″E / 4.953°S 151.385°E |
Geography | |
Location | West New Britain, Papua New Guinea |
Geology | |
Mountain type | Stratovolcano |
Last eruption | Pleistocene |
Likuruanga is a stratovolcano in easternmost West New Britain Province on the island of New Britain, Papua New Guinea. Its low, dissected edifice contains a large volcanic crater that is breached to the north. The last known eruption from Likuruanga is prehistoric in age, having taken place during the Pleistocene epoch. [1]
A fatality occurred on Likuruanga's northern flank in September 2006 when a boy died in a hole at the village of Bakada. The cause of death was carbon dioxide asphyxiation. [1]
Likuruanga | |
---|---|
Highest point | |
Elevation | 904 m (2,966 ft) |
Coordinates | 4°57′11″S 151°23′06″E / 4.953°S 151.385°E |
Geography | |
Location | West New Britain, Papua New Guinea |
Geology | |
Mountain type | Stratovolcano |
Last eruption | Pleistocene |
Likuruanga is a stratovolcano in easternmost West New Britain Province on the island of New Britain, Papua New Guinea. Its low, dissected edifice contains a large volcanic crater that is breached to the north. The last known eruption from Likuruanga is prehistoric in age, having taken place during the Pleistocene epoch. [1]
A fatality occurred on Likuruanga's northern flank in September 2006 when a boy died in a hole at the village of Bakada. The cause of death was carbon dioxide asphyxiation. [1]