Worldwide distribution of known hydrothermal vent fields (InterRidge 2009)
Hydrothermal vent fields discovered on the Portuguese seafloor
Max temperatures: ~270 °C
Setting: Basaltic MOR system at the slow-spreading Reykjanes Ridge, hosted within a volcanic rift valley.
Max temperatures: not yet measured
Setting: Basalt-hosted vent field on the Menez Gwen segment, associated with recent volcanic activity in the Azores region.
Max temperatures: ~285 °C
Setting: E-MORB basalt-hosted field located at the summit caldera of a young axial volcano, with focused black-smoker venting.
Max temperatures: ~333 °C
Setting: E-MORB basalt-hosted field situated within a central volcano caldera on the axial graben of the MAR.
Max temperatures: <10 °C
Setting: Ultramafic-hosted, low-temperature diffuse venting site with strong CH₄ discharge, located near a non-transform offset.
Max temperatures: ~9 °C
Setting: Ultramafic-influenced diffuse field on a non-volcanic ridge massif, characterized by serpentinized peridotites and a tectonic mélange.
Max temperatures: ~365 °C
Setting: Ultramafic-hosted black-smoker system, extremely rich in H₂ and CH₄, located on the western flank of a non-transform offset between the AMAR ridge segments.