Acoustic T-waves from a seismic swarm, possibly associated with magmatic activity, were recorded in 1991 from a location 130 km S of the Eltanin Fracture Zone (Bulletin of the Global Volcanism Network, 1991). The source was near a seamount shallower than 1,000 m in depth near the Pacific-Antarctic Ridge.
Hollister Ridge Volcano — Undersea Features
Fissure ventType
HoloceneLast eruption
-1000 mElevation
Undersea FeaturesCountry
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