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Papua Nugini · Stratovolkan

Lolo

Tipe
Stratovolkan
Ketinggian
796 m
Letusan terakhir
Tidak diketahui
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 Nugini
Wilayah
Pasifik Barat Daya / Bismarck Volcanic Arc
Ketinggian
796 m
Koordinat
-5.466, 150.509
Letusan terakhir
Tidak diketahui
Kondisi tektonik
Zona subduksi / Kerak benua (> 25 km)
Bentuk lahan
Komposit
Batuan utama
Andesit / Andesit basaltik

Ringkasan geologi

Teks asli bahasa Inggris

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.

Kutipan dari Global Volcanism Program, Smithsonian Institution · Baca ringkasan lengkap di GVP →

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