Research Sites Image Gallery

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The COVIS instrument is positioned on the seafloor to measure heat output from both chimneys (Mushroom) and diffuse hydrothermal fluids on the seafloor.
The COVIS instrument is positioned on the seafloor to measure heat output from both chimneys (Mushroom) and diffuse hydrothermal fluids on the seafloor.
The undervator as found on the sea floor.  Credit: UW/NSF-OOI/WHOI, V18.
The undervator as found on the sea floor.  Credit: UW/NSF-OOI/WHOI, V18.
Flowmeter taking measurements, Credit: R. Centurion, University of Washington, V18
Flowmeter taking measurements, Credit: R. Centurion, University of Washington, V18
so-hydrate
slope-base1
offshore
shelf
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BO-Endurance-Array-S-Hydrate
BO-Endurance-Array-OR-Line
BO-Endurance-Array-OR-Offshore
BO-Endurance-Array-OR-Slope-Base
BO-Endurance-Array-OR-Shelf
BO-Endurance-Array-OR-Inshore
A variety of geophysical sensors are deployed at the base of Axial Seamount to monitor seismic events on the Juan de Fuca plate.
A variety of geophysical sensors are deployed at the base of Axial Seamount to monitor seismic events on the Juan de Fuca plate.
Axial Seamount is the most magmatically robust volcano on the Juan de Fuca Ridge spreading center. It hosts numerous active hydrothermal fields and abundant sites of diffuse flow.
Axial Seamount is the most magmatically robust volcano on the Juan de Fuca Ridge spreading center. It hosts numerous active hydrothermal fields and abundant sites of diffuse flow.
A good caption about the Central site will go here
A good caption about the Central site will go here
Caption will go here!
Caption will go here!
A good caption will go here.
A good caption will go here.
A real caption will go here in the near future
A real caption will go here in the near future
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caldera-gradient