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파푸아뉴기니 · 성층화산

Lolo

화산 유형
성층화산
해발
796m
마지막 분화
미확인
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. · 사진: Photo by Elliot Endo, 2002 (U.S. Geological Survey).
화산 유형
성층화산
국가
파푸아뉴기니
지역
남서태평양 / Bismarck Volcanic Arc
해발
796m
좌표
-5.466, 150.509
마지막 분화
미확인
판구조 환경
섭입대 / 대륙 지각 (> 25 km)
화산 지형
복성화산체
주요 암석
안산암 / 현무암질 안산암
지질학적 요약

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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