Acoustic signals (T-waves) from a seismic swarm were detected in 1990 from a source along the Udintsev fracture zone at about 143°W, along the segment that corresponds with the Pacific-Antarctic Ridge (Global Volcanism Network Bulletin, 1990). The seismicity may have been linked to volcanic activity.
Udintsev Transform Volcano — Undersea Features
Fissure ventType
HoloceneLast eruption
-5700 mElevation
Undersea FeaturesCountry
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