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Researching the effects of underwater hydrothermal venting systems |
Northern Gorda Ridge | ||
The Gorda Ridge has been an active spreading ridge with three SOSUS-detected seismic events: The T-phase swarm in February/March 1996 lead to the emission of Event Plumes and the eruption of a new lava flow onto the seafloor. For more information on the northern Gorda Ridge, see the VENTS Gorda Geology Page or the above event sites. updated 4/12/2001 |
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