The UCSB scientists are making new contributions to this field of inquiry in their studies of
seafloor hydrothermal fluid discharge into the Earth's oceans, which has been occurring ever since the oceans first formed four billion years ago.
Not exact matches
In Pescadero Basin, however,
hydrothermal - vent
fluids pass through thick layers of
seafloor mud.
The second spot was Axial Seamount, an active underwater volcano, along with its associated
hydrothermal vents, where the team could study the transfer of minerals from beneath the
seafloor into the water and access hardy microbes that thrive in the vent
fluids, which can reach 250 degrees Fahrenheit.
Eventually, the hot, mineral - rich
fluid rises again and gushes out of openings in the
seafloor —
hydrothermal vents — at temperatures up to about 400 degrees Centigrade.