Axial Image Gallery

Axial-Caldera-International-District
Axial-Caldera-Eastern
Axial-Caldera-Central
Axial-Caldera-ASHES
Axial-base-basemap-sm
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.
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The cabled geophysical array at the Central Caldera Site is focused on measuring the inflation and deflation of the volcano, earthquakes, and the movement of of molten lava within the core of the volcano. Bathymetric data are from D. Clague and D. Caress, MBARI. Image Credit: University of Washington.
The cabled geophysical array at the Central Caldera Site is focused on measuring the inflation and deflation of the volcano, earthquakes, and the movement of of molten lava within the core of the volcano. Bathymetric data are from D. Clague and D. Caress, MBARI. Image Credit: University of Washington.
Axial Slope Base Image
Axial Slope Base Image
Axial Caldera Image
Axial Caldera Image
ASHES Vent Field Caption
ASHES Vent Field Caption
A good caption about the Central site will go here
A good caption about the Central site will go here
A real caption will go here in the near future
A real caption will go here in the near future
Caption will go here!
Caption will go here!
During Jason Dive J2-980, the remnants of multiple lava lakes from the April 2011 eruption of Axial Seamount were encountered. The bathtub rings mark the progressive lowering of the "lake". Credit: UW/OOI-NSF/WHOI; J2-980; V17.
During Jason Dive J2-980, the remnants of multiple lava lakes from the April 2011 eruption of Axial Seamount were encountered. The bathtub rings mark the progressive lowering of the "lake". Credit: UW/OOI-NSF/WHOI; J2-980; V17.
Tubeworms with red plumes grow on the side of an odd basalt formation formed as part of a fossilized lava lake at the summit of Axial Seamount in 2011. Depth is ~1500 m. UW/OOI-NSF/WHOI; J2-980; V17.
Tubeworms with red plumes grow on the side of an odd basalt formation formed as part of a fossilized lava lake at the summit of Axial Seamount in 2011. Depth is ~1500 m. UW/OOI-NSF/WHOI; J2-980; V17.
A glass-coated sheet flow sample recovered on Jason Dive J2-980 from the April 2011 lava flow on Axial Seamount. Credit. Mitch Elend, University of Washington, V17.
A glass-coated sheet flow sample recovered on Jason Dive J2-980 from the April 2011 lava flow on Axial Seamount. Credit. Mitch Elend, University of Washington, V17.
A dense colony of tube worms awash in warm diffusely venting fluids grow on the April 2011 lava flow at the summit of Axial Seamount. UW/OOI-NSF/WHOI; J2-980; V17.
A dense colony of tube worms awash in warm diffusely venting fluids grow on the April 2011 lava flow at the summit of Axial Seamount. UW/OOI-NSF/WHOI; J2-980; V17.
This science pod was cut loose from the Axial Base Shallow Profiler mooring on Sunday morning and was throughly cleaned by an eager group of students. The growth visible on the pod comes after just one year in the water, and since many of the instruments on the pod require unobstructed intake lines for sampling, the pods must be replaced yearly. 
This science pod was cut loose from the Axial Base Shallow Profiler mooring on Sunday morning and was throughly cleaned by an eager group of students. The growth visible on the pod comes after just one year in the water, and since many of the instruments on the pod require unobstructed intake lines for sampling, the pods must be replaced yearly. 
Healthy tube worms grow along a venting fracture in the 2011 glassy lava flow at the summit of Axial Seamount. Credit: UW/OOI-NSF/WHOI; J2-980; V17.
Healthy tube worms grow along a venting fracture in the 2011 glassy lava flow at the summit of Axial Seamount. Credit: UW/OOI-NSF/WHOI; J2-980; V17.
A small cluster of blue cilliates intermixed with limpets grow in a diffuse flow site on the the 2011 lava flow at the summit of Axial Seamount. Credit: UW/OOI-NSF/WHOI; J2-980; V17.
A small cluster of blue cilliates intermixed with limpets grow in a diffuse flow site on the the 2011 lava flow at the summit of Axial Seamount. Credit: UW/OOI-NSF/WHOI; J2-980; V17.
A beautiful ropey, jumbled sheet flow covers the seafloor at ~1500 m beneath the oceans' surface at the summit of Axial Seamount. The lava was erupted in April 2011. Credit: UW/OOI-NSF/WHOI; J2-980; V17.
A beautiful ropey, jumbled sheet flow covers the seafloor at ~1500 m beneath the oceans' surface at the summit of Axial Seamount. The lava was erupted in April 2011. Credit: UW/OOI-NSF/WHOI; J2-980; V17.
The Cabled Array high power and bandwidth fiber optic cables extend from coastal to blue water environments, that include the Cascadia Subduction Zone and the largest volcano off of the Washington-Oregon coast, Axial Seamount. The ~ 900 km of cable provides two-way communications and data flow at the speed of light to 140 instruments and 2900 m-tall moorings with instrumented profilers that have been operational since 2015. Credit: University of Washington.
The Cabled Array high power and bandwidth fiber optic cables extend from coastal to blue water environments, that include the Cascadia Subduction Zone and the largest volcano off of the Washington-Oregon coast, Axial Seamount. The ~ 900 km of cable provides two-way communications and data flow at the speed of light to 140 instruments and 2900 m-tall moorings with instrumented profilers that have been operational since 2015. Credit: University of Washington.
Modifications to the RSN cabled observatory suggested at the RSN-Axial Workshop in Seattle, WA October 5-7, 2011. 
Modifications to the RSN cabled observatory suggested at the RSN-Axial Workshop in Seattle, WA October 5-7, 2011. 
2011 Bathymetry of Axial Seamount Caldera (first draft), using the R/V Thompson's EM302.  Data were processed by UW undergraduate student Brendan Philip using CARIS HIPS and SIPS software.  
2011 Bathymetry of Axial Seamount Caldera (first draft), using the R/V Thompson's EM302.  Data were processed by UW undergraduate student Brendan Philip using CARIS HIPS and SIPS software.