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Gunung berapi Pusikbukit (+ 1982 m) naik lebih dari 1000 m di atas danau, hampir 200 m di atas dinding kaldera barat. Gunung berapi komposit ini sebagian besar terdiri dari 2 piroksen andesit (61-65 wt.% SiO2) dan beberapa aliran lava hornblende dacite (68-69 wt.% SiO2, Gbr. 3B). Berdasarkan ekspresi geomorfologis mereka, lava dasit adalah yang termuda. Tidak ada letusan bersejarah yang tercatat di Pusikbukit, tetapi solfatera aktif hadir di sisi timur lautnya
Pusikbukit volcano (+ 1982 m) rises over 1000 m above the lake, almost 200 m above the western caldera wall. This composite volcano consists mostly of 2 pyroxene andesite (61-65 wt. % SiO2) and a few hornblende dacite lava flows (68-69 wt. % SiO2, Fig. 3B). Based upon their geomorphological expression, the dacitic lavas are the youngest. No historic eruptions have been recorded at Pusikbukit, but an active solfatera is present on its northeastern flank
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