Image Archive

A sea pen (a colonial, stalked cnidarian, related to jellyfish) at Slope Base. Photo Credit: UW/NSF-OOI/WHOI, V19

A fringed sea cucumber next to the Slope Base junction box in 2019. Photo Credit: UW/NSF-OOI/WHOI, V19.

Barnacles, tunicates, and anemones biofouling the digital still camera at the Oregon Shelf site. Photo Credit: M. Vardaro, UW, V19

Close-up shot of white anemones on top of Oregon Shelf junction box MJ01C. Photo Credit: M. Vardaro, UW, V19

Close-up shot of shrimp hiding among the anemones encrusting Oregon Shelf junction box MJ01C. Photo Credit: M. Vardaro, UW, V19

A shrimp hiding among the anemones biofouling junction box MJ01C at the Oregon Shelf Site, deployed since 2014. Photo Credit: M. Vardaro, UW, V19

Deep-sea octopus (Muusoctopus sp.) at Axial Base 2600 m; Photo Credit: UW/NSF-OOI/WHOI, V19

A pom-pom anemone at Axial Base, moving around the legs of the HPIES instrument. Photo Credit: UW/NSF-OOI/WHOI; V19

A Graneledone octopus peeking at Jason around the side of the Axial Base HPIES instrument. Photo Credit: UW/NSF-OOI/WHOI; V19

A rattail fish swimming near the Axial Base junction boxes during a CTD deployment. Photo credit: UW/NSF-OOI/WHOI; V19

Organisms colonize the outer walls of the 16 m-tall hydrothermal edifice called El Guapo. The community structure changes with height above seafloor. Here, limpets, red scale worms and blue protists (ciliates) colonize the outer sulfide walls of the structure. Credit: UW/NSF-OOI/WHOI, V18.

Near the summit of the ~16 m-tall El Guapo chimney, sulfide worms, and tubeworms colonize the younger part of the new sulfide growth. Credit: UW/NSF-OOI/WHOI, V18.

Once again the Smokey Caverns (or Taverns as it is also known) has changed remarkably since we visited it with Jason last year. The area is significantly more rugged, marked by large hummocks. An eelpout, sole, clams and orange rock fish dot the landscape. Credit: UW/NSF-OOI/WHOI, V18.

A hagfish with mouth wide open slithers around the Southern Hydrate Ridge methane seep site. Credit: UW/NSF-OOI/WHOI, V18.

An old Ocean Drilling Program hole serves as a nursery for hagfish and crabs at the summit of Southern Hydrate Ridge. Credit: UW/NSF-OOI/WHOI, V18.

This Corallimorph anemone was spotted on the seafloor at Southern Hydrate Ridge at a depth of 774 meters. Photo Credit: NSF-OOI/UW/CSSF; Dive 1772; V14.

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 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 small cluster of healthy Ridgeia tube worms grow near Skadis' Cauldron, a highly active snowblower in 2011. Credit: UW/OOI-NSF/WHOI; J2-980; V17.

A 3D temperature (thermistor) array housing 24 sensors rests above a small diffuse flow site a few meters away from the actively venting black smoker edifice called Mushroom in the ASHES hydrothermal field on Axial Seamount. This cabled instrument was designed and built by G. Proskurowski, UW School of Oceanography. Limpets have colonized the frame and cable housing the thermistors. An osmotic fluid sampler is inserted into the diffuse flow site to obtain chemistry coregistered with temperature. Credit: UW/NSF-OOI/WHOI; V16. 

A digital still camera (left), mass spectrometer (middle) and a fluid and microbial DNA sampler at the El Gordo vent in the International District Hydrothermal Field measure and sample fluids, animals, and microbes in this active processes within this hydrothermal system to understand linkages amoung seismicity (seismometers extend away from the field), venting and life in this extreme environment. Credit: UW/OOI-NSF/WHOI; Dive J2-212, V16.

Krill surroung the small "cage" housing the cable connection from the Shallow Profiler at Axial Base to the extension cable connecting the Profiler to the power and communications. Credit: UW/OOI-NSF/WHOI, Dive J910, V16.

The float atop the Deep Profiler Mooring at the base of Axial Seamount has become a habitat for schools of fish. Credit: NSF-OOI/UW/CSSF; ROPOS Dive R1860, V15.

A skate swims gently past ROPOS at the base of Axial Seamount, greater than 9000 ft beneath the ocean's surface. Credit: UW/NSF-OOI/CSSF; ROPOS DIve R1841, V15.

A huge rattail, ~ 5 feet in length, swims slowly in front of the ROV ROPOS near the International District Hydrothermal Field at a depth of 5000 ft beneath the ocean's surface. This area has a higher abundance of these fish than observed elsewhere in the caldera, perhaps because of the larger size of the vent field and hence food source. Credit: UW/NSF-OOI/CSSF; ROPOS Dive R1729; V15.

Pyconogonids are abundant on many sulfide structures in the vent fields within the caldera of Axial Seamount. These 8-legged anthropods are commonly found in areas where venting has stopped, leaving variably oxidized edificies. Here, they are associated with snails an a small scale worm ~ 1 cm; in length. Credit: UW/NSF-OOI/CSSF; ROPOS Dive R1836; V15.

The Poralia rufescens jellyfish.