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Global Volcanism Program | Image GVP-05811

Hakusan, seen here from the WNW, contains multiple vents along a roughly N-S line. Holocene eruptions have consisted of phreatic or phreatomagmatic explosions from several summit craters. Partial collapse of the summit produced a debris avalanche down the E flank. Historical eruptions were recorded over almost a thousand-year period until the 17th century. Photo by Ishikawa Prefecture, 1994 (courtesy Toshio Higashino, Haku-san Nature Conservation Center).

Hakusan, seen here from the WNW, contains multiple vents along a roughly N-S line. Holocene eruptions have consisted of phreatic or phreatomagmatic explosions from several summit craters. Partial collapse of the summit produced a debris avalanche down the E flank. Historical eruptions were recorded over almost a thousand-year period until the 17th century.

Photo by Ishikawa Prefecture, 1994 (courtesy Toshio Higashino, Haku-san Nature Conservation Center).

Keywords: stratovolcano


Hakusan