Eruptions occur predominately from the central conduit and have also produced lava flows that travel far down the flanks.
Pyroclastic flows and mudflows have commonly swept down many of the approximately 40 ravines that radiate from the summit and have often devastated populated lowland areas.
www.volcanodiscovery.comAusbrüche haben auftreten, überwiegend aus den zentralen Conduit und auch Lavaströme, die weit nach unten an den Flanken zu reisen.
Pyroklastische Ströme und Schlammlawinen haben sich viele der etwa 40 Schluchten häufig gefegt, die Strahlen vom Gipfel und besiedelten Flachland oft verwüstet haben.
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