Image Archive




























These samples were collected from a lava flow with an age of about 3 months.
r2205_720p
ROPOS being deployed off the port side of the R/V Thompson.
The ROV ROPOS gently flew into a small collapse basin marked by pillars, arches and isolated columns of basalt. These areas form as lava drains out from deep lava pools. The surface of the lava lake or channel very rapidly cools as it interacts with near freezing seawater. As the lava drains out, the roof is not strong enough to maintain its weight, and collapses into a pile of talus. Credit: UW/NSF-OOI/CSSF; V11.
A small pillar marked by bathtub rings is encased by broken slabs of the sheet flow that erupted in April 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.
Dean2-poster
Black, glassy basalt marks the edge of the new 2011 lava flow on the eastern edge of the caldera. Credity: UW/NSF-OOI/CSSF; V11.
Theme IV banner
Dean
The ROV ROPOS is controlled from this room.
ROPOS, operated by the Canadian Scientific Submersible Facility, is the remotely operated vehicle onboard.
When camera stands become hats!
On the bow of the boat
ROPOS's crane
blue
Sunset Day 4
Camera team testing equipment off the side
Matt Knight relaxing at the bow of the ship
ROPOS equipment
The bridge
Beautiful day above Axial Seamount
To highlight the impacts of pressure and for relaxing downtime, it is a common tradition on ROV cruises to color styrofoam heads and cups and take them down to the seafloor. Styrofoam cups come up about 1 inch tall. This head has not yet been "shrunk" but will go down in a few days.
Overlapping pillow flows are enclosed by islands of sediment along the flanks of Axial Seamount. Credit: NSF-OOI/CSSF; V11.
This Flapjack Octopus floated gently above the seafloor for several minutes as we watched it through the eyes of the ROV ROPOS. Credit: UW/OOI-NSF/CSSF, V11.
Pillow basalts, interspersed with sediment ponds, mark old lava flows on the flanks of Axial Seamount. The rocks and sediment are host to occasional deep sea corals.
This Flapjack Octopus was imaged by the Canadian robotic vehicle ROPOS at a water depth of 5728 feet on Axial Seamount. Photo credit: OOI-NSF/UW/CSSF, V11
This Roughtail skate was photographed by the ROV ROPOS at 1756 m (5761 feet) beneath the ocean's surface on the flank of Axial Seamount. Credit: UW/NSF-OOI/CSSF; ROPOS Dive R1466; V11.
- Anemone
- Animal
- Arthropod
- ASHES
- Axial
- Axial Base
- Axial Biology
- Axial Caldera
- Bacteria
- Basalt Lava
- BEP
- Biofouling
- Biology
- Camds
- Camera
- Camhd
- Central Caldera
- Ciliates
- Cnidaria
- Coastal Biology
- Crab
- Deep Profiler Mooring
- Dive Highlights
- Eastern Caldera
- Echinoderms
- Endurance Array
- Engineering Team
- ENLIGHTEN 10
- Exploratorium
- Fish
- Geology
- HD Camera
- HPIES
- Hydrate Ridge
- Hydrates
- Hydrophone
- Hydrothermal Vents
- Illustration
- Inshore 80 Meters
- Instrument
- International District
- J-BOX
- Jason
- Jellyfish
- Junction Box
- K12
- Lava
- Mollusk
- Moorings
- Nodes
- Nudibranch
- Octopus
- OOI
- Oregon Offshore
- Oregon Offshore 600 m
- Oregon Shelf
- Oregon Slope Base
- People
- PN1B
- PN1D
- Polychaetes
- PPSDN
- Primary Node
- RASFL
- ROCLS
- ROPOS
- ROPOS Dives
- ROV Team
- RV Revelle
- RV Sikuliaq
- RV Thompson
- Salp
- Sample
- SC13
- Science Team
- Sea Cucumber
- Sea Star
- Sea Urchin
- Seafloor
- Seismometer
- Sensors
- Shallow Profiler Mooring
- Shark
- Shipboard
- Shore Station
- Slope Base
- Smoker
- Soft Coral
- Southern Hydrate Ridge
- Sponge
- Squid
- Students
- Students & Guest Participants
- Tmpsf
- Tubeworms
- VISIONS 11 Leg 1
- VISIONS 11 Leg 2
- VISIONS 11 Viewers
- VISIONS 13
- VISIONS 14
- VISIONS 15
- VISIONS 16
- VISIONS 17
- VISIONS 18
- VISIONS 20
- VISIONS 22
- VISIONS 23
- visions 26
- Visualization