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Global Volcanism Program | Image GVP-07552

The submarine Reykjaneshryggur volcanic system, lying off the SW tip of Iceland at the top of the photo, is part of the Mid-Atlantic Ridge, which extends onto the Reykjanes Peninsula in the foreground.  Numerous submarine eruptions at Reykjaneshryggur dating back to the 12th century have been observed during historical time, some of which have formed ephemeral islands.  Tephra deposits from earlier Holocene eruptions are preserved on the Reykjanes Peninsula in the foreground.     Photo by Oddur Sigurdsson, 1998 (Icelandic National Energy Authority).

The submarine Reykjaneshryggur volcanic system, lying off the SW tip of Iceland at the top of the photo, is part of the Mid-Atlantic Ridge, which extends onto the Reykjanes Peninsula in the foreground. Numerous submarine eruptions at Reykjaneshryggur dating back to the 12th century have been observed during historical time, some of which have formed ephemeral islands. Tephra deposits from earlier Holocene eruptions are preserved on the Reykjanes Peninsula in the foreground.

Photo by Oddur Sigurdsson, 1998 (Icelandic National Energy Authority).


Reykjanes