VISIONS 13 Images

The temperature-resistivity instrument measures, in real-time, the temperature of black smoker fluids (>400°C) and the resistivity of the fluids as a proxy for chlorinity. Vents at Axial Seamount are boiling, producing fluids that are very low in chloride content (salts). Boiling is an important processes because it enhances precipitation of precious metals in seafloor black smokers.
The temperature-resistivity instrument measures, in real-time, the temperature of black smoker fluids (>400°C) and the resistivity of the fluids as a proxy for chlorinity. Vents at Axial Seamount are boiling, producing fluids that are very low in chloride content (salts). Boiling is an important processes because it enhances precipitation of precious metals in seafloor black smokers.
The digital still camera (with pan/tilt and LED lights) will be positioned at the International District in Axial volcano's caldera.
The digital still camera (with pan/tilt and LED lights) will be positioned at the International District in Axial volcano's caldera.
A variety of geophysical sensors will be deployed at the base of Axial Seamount to monitor seismic events on the Juan de Fuca plate.
A variety of geophysical sensors will be deployed at the base of Axial Seamount to monitor seismic events on the Juan de Fuca plate.
The HD video camera (with pan/tilt and LED lights) will be positioned near the Mushroom Vent at the Ashes Vent site in Axial volcano.  The goal is to image the physical and biological activity on this vent.
The HD video camera (with pan/tilt and LED lights) will be positioned near the Mushroom Vent at the Ashes Vent site in Axial volcano.  The goal is to image the physical and biological activity on this vent.
Axial Caldera Image
Axial Caldera Image
Axial Slope Base Image
Axial Slope Base Image
Short-period seismometers provide real-time information on earthquakes at mid-ocean ridges. In 2003, an array of seismometers was deployed on the Endeavour Segment of the Juan de Fuca Ridge, north of Axial Seamount. The one shown here, was deployed inside a borehole in a pillow basalt in the Mothra Hydrothermal Field, providing better coupling to the seafloor. This project was funded by the W.M. Keck Foundation.
Short-period seismometers provide real-time information on earthquakes at mid-ocean ridges. In 2003, an array of seismometers was deployed on the Endeavour Segment of the Juan de Fuca Ridge, north of Axial Seamount. The one shown here, was deployed inside a borehole in a pillow basalt in the Mothra Hydrothermal Field, providing better coupling to the seafloor. This project was funded by the W.M. Keck Foundation.
'Osmo' samplers draw hydrothermal fluids into small capillary-like tubing and allow long-term sampling of diffuse and black smoker hydrothermal fluids, as well as fluids from methane seeps. Osmo samplers in this image (white canisters) are attached in an in situ 'microbial' incubator deployed inside the walls of a black smoker chimney called Gremlin. The osmo samplers allowed collection of vent fluids for 1-year, while the microbial incubator collected hundreds of temperature measurements inside the wall of the black smoker. Novel microbes colonized mineral wafers and new sulfide precipitates inside 4 discrete chambers within the incubator. This experiment, lead by D. Kelley, University of Washington, was designed to look at the upper temperature limit of life. Osmo samplers will be deloyed at the ASHES hydrothermal field and at the summit of Southern Hydrate Ridge during the VISIONS'13 expedition.
'Osmo' samplers draw hydrothermal fluids into small capillary-like tubing and allow long-term sampling of diffuse and black smoker hydrothermal fluids, as well as fluids from methane seeps. Osmo samplers in this image (white canisters) are attached in an in situ 'microbial' incubator deployed inside the walls of a black smoker chimney called Gremlin. The osmo samplers allowed collection of vent fluids for 1-year, while the microbial incubator collected hundreds of temperature measurements inside the wall of the black smoker. Novel microbes colonized mineral wafers and new sulfide precipitates inside 4 discrete chambers within the incubator. This experiment, lead by D. Kelley, University of Washington, was designed to look at the upper temperature limit of life. Osmo samplers will be deloyed at the ASHES hydrothermal field and at the summit of Southern Hydrate Ridge during the VISIONS'13 expedition.
The Offshore Endurance site at 600 m water depth will host two cabled moorings and a Benthic Experiment Platform with numerous physical, chemical and biological sensors, as well as a digital still camera.
The Offshore Endurance site at 600 m water depth will host two cabled moorings and a Benthic Experiment Platform with numerous physical, chemical and biological sensors, as well as a digital still camera.
The Benthic Experiment Package (BEP) is composed of a hazard-resistant frame (shown here), the inside of which hosts an UW-APL-designed Low Power communications housing, and a variety of sensors to measure oceanographic properties that include acidity (pH), carbon dioxide, salinity and oxygen concentrations, and currents. A hydrophone that will be mounted outside of the frame will be used to detect sounds in the ocean. The BEP is scheduled for installation in 2014 at the Endurance Offshore site that is part of the Endurance Array's Newport Line. This site is also the location of one of the RSN Primary Nodes, which is the power and data hub for the BEP Low-Power Junction Box, which is in turn the power and data hub for a variety of instrument platforms.
The Benthic Experiment Package (BEP) is composed of a hazard-resistant frame (shown here), the inside of which hosts an UW-APL-designed Low Power communications housing, and a variety of sensors to measure oceanographic properties that include acidity (pH), carbon dioxide, salinity and oxygen concentrations, and currents. A hydrophone that will be mounted outside of the frame will be used to detect sounds in the ocean. The BEP is scheduled for installation in 2014 at the Endurance Offshore site that is part of the Endurance Array's Newport Line. This site is also the location of one of the RSN Primary Nodes, which is the power and data hub for the BEP Low-Power Junction Box, which is in turn the power and data hub for a variety of instrument platforms.
A variety of extension cables with underwater wet-mateable connectors plug into the junction boxes and nodes. In concert, these assets will provide power and communications to >100 instruments on the RSN. The drums are prespooled and on the ship they are loaded onto the the remote cable laying system on ROPOS (ROCLS).
A variety of extension cables with underwater wet-mateable connectors plug into the junction boxes and nodes. In concert, these assets will provide power and communications to >100 instruments on the RSN. The drums are prespooled and on the ship they are loaded onto the the remote cable laying system on ROPOS (ROCLS).
During the VISIONS'13 expedition the ROV ROPOS, installed >22,000 m of extension cables onto the seafloor using the remotely operated cable laying system (ROCLS) shown here attached to its underbelly. The cables will provide power and real-time, two-way communication to a diverse array of instruments and junction boxes.
During the VISIONS'13 expedition the ROV ROPOS, installed >22,000 m of extension cables onto the seafloor using the remotely operated cable laying system (ROCLS) shown here attached to its underbelly. The cables will provide power and real-time, two-way communication to a diverse array of instruments and junction boxes.
This low voltage node will be deployed during Leg 2 of the VISIONS'13 expedition at the Offshore site west of Newport Oregon at a water depth of ~600 m. It will provide a connection for the Endurance array Benthic Experiment Platform (BEP).
This low voltage node will be deployed during Leg 2 of the VISIONS'13 expedition at the Offshore site west of Newport Oregon at a water depth of ~600 m. It will provide a connection for the Endurance array Benthic Experiment Platform (BEP).
Some of the special capabilities of ROPOS are that it can lift up to 4,000 lbs and directly couple to Junction Boxes for deployment to the seafloor, such as the one shown here. This was a test deployment of a Junction Box "shell", not yet fully outfitted with electronics, cables and sensors conducted in 2011.
Some of the special capabilities of ROPOS are that it can lift up to 4,000 lbs and directly couple to Junction Boxes for deployment to the seafloor, such as the one shown here. This was a test deployment of a Junction Box "shell", not yet fully outfitted with electronics, cables and sensors conducted in 2011.
Over 22 km of extension cables were deployed by the robotic vehicle ROPOS during the VISIONS'13 expedition.The cables were spooled onto drums and installed using the Remotely Operated Cable Laying System (ROCLS) latched beneath ROPOS.
Over 22 km of extension cables were deployed by the robotic vehicle ROPOS during the VISIONS'13 expedition.The cables were spooled onto drums and installed using the Remotely Operated Cable Laying System (ROCLS) latched beneath ROPOS.
The R/V Thompson holds station in Nootka Sound, an inlet on the west coast of Vancouver Island.
The R/V Thompson holds station in Nootka Sound, an inlet on the west coast of Vancouver Island.
Battery-operated thermistor array. VISIONS '13, Leg 3. Photo by Ryan Cox.
Battery-operated thermistor array. VISIONS '13, Leg 3. Photo by Ryan Cox.
Passing through the Ballard Locks (photo: Judy Twedt)
Passing through the Ballard Locks (photo: Judy Twedt)
Dense macrofaunal communities cover the actively venting black smoker edifice called El Guapo. Here, tube worms are covered with filamentous bacteria. Also in this area are blue ciliates, palm worms, and thick colonies of limpets.   Photo credit: OOI/UW/CSSF
Dense macrofaunal communities cover the actively venting black smoker edifice called El Guapo. Here, tube worms are covered with filamentous bacteria. Also in this area are blue ciliates, palm worms, and thick colonies of limpets.   Photo credit: OOI/UW/CSSF
RSN Cables 1   Photo by Ben Fundis
RSN Cables 1   Photo by Ben Fundis
ROPOS begins dive 1592 at the summit of Axial Seamount. Photo by Mitch Elend.
ROPOS begins dive 1592 at the summit of Axial Seamount. Photo by Mitch Elend.
The gangway is taken up at the UW dock as the R/V Thompson prepares to set sail on the first leg of VISIONS '13. Photo by Nancy Penrose
The gangway is taken up at the UW dock as the R/V Thompson prepares to set sail on the first leg of VISIONS '13. Photo by Nancy Penrose
Having just cast off from the UW dock, the R/V Thompson heads out on the first leg of VISIONS '13 Photo by Nancy Penrose
Having just cast off from the UW dock, the R/V Thompson heads out on the first leg of VISIONS '13 Photo by Nancy Penrose
Perhaps there are future ocean scientists and engineers among those watching as the Thompson waits in the Ballard Locks. Photo by Mike Mulvihill
Perhaps there are future ocean scientists and engineers among those watching as the Thompson waits in the Ballard Locks. Photo by Mike Mulvihill
The top of the the Escargot Vent in the International District Hydrothermal Vent Field at Axial Seamount. (credit: OOI/UW/CSSF)
The top of the the Escargot Vent in the International District Hydrothermal Vent Field at Axial Seamount. (credit: OOI/UW/CSSF)
A wave from Chief Scientist John Delaney, with Allison Fundis, as the Thompson passes through the Ballard Locks. Photo by Mike Mulvihill
A wave from Chief Scientist John Delaney, with Allison Fundis, as the Thompson passes through the Ballard Locks. Photo by Mike Mulvihill
ROPOS pilots guide the robotic vehicle as it enters the water above Axial Volcano.
ROPOS pilots guide the robotic vehicle as it enters the water above Axial Volcano.
RSN Cables 6 Photo by Ben Fundis
RSN Cables 6 Photo by Ben Fundis
With the railroad bridge up, the Thompson leaves the Ballard Locks and heads for Puget Sound. Photo by Mike Mulvihill
With the railroad bridge up, the Thompson leaves the Ballard Locks and heads for Puget Sound. Photo by Mike Mulvihill
Entering the Ballard Locks Photo by Mike Mulvihill
Entering the Ballard Locks Photo by Mike Mulvihill
Waiting at the Ballard Locks Photo by Mike Mulvihill
Waiting at the Ballard Locks Photo by Mike Mulvihill
ROPOS vans and spools with OOI extension cables (orange) on aft deck of the R/V Thompson at the UW dock, Sunday 30 June 2013
ROPOS vans and spools with OOI extension cables (orange) on aft deck of the R/V Thompson at the UW dock, Sunday 30 June 2013
ROPOS dunk test in Puget Sound, Seattle in background. Photo by Ben Fundis
ROPOS dunk test in Puget Sound, Seattle in background. Photo by Ben Fundis
View of downtown Seattle from Lake Union during out departure. (photo: Judy Twedt)
View of downtown Seattle from Lake Union during out departure. (photo: Judy Twedt)
Beginning a nearly mile long descent to the seafloor (photo: Judy Twedt)
Beginning a nearly mile long descent to the seafloor (photo: Judy Twedt)
Spools of extension cables (orange) on fantail of the R/V Thompson at UW dock, Sunday, 30 June 2013
Spools of extension cables (orange) on fantail of the R/V Thompson at UW dock, Sunday, 30 June 2013
RSN Cables 7 Photo by Ben Fundis
RSN Cables 7 Photo by Ben Fundis
Drums holding extension cables and a secondary node are loaded onto the fantail of the R/V Thompson in preparation for deployment. Photo by Skip Denny.
Drums holding extension cables and a secondary node are loaded onto the fantail of the R/V Thompson in preparation for deployment. Photo by Skip Denny.
Spare commissioning support hardware is plugged into Primary Node 3B while it is fully powered up from >350 miles away at Pacific City, Oregon. A tool basket on the left holds the hardware, as well as other equipment that may have been needed for testing. The manipulator arms of ROPOS are in the foreground, waiting for the test to be completed. Photo: OOI/UW/CSSF
Spare commissioning support hardware is plugged into Primary Node 3B while it is fully powered up from >350 miles away at Pacific City, Oregon. A tool basket on the left holds the hardware, as well as other equipment that may have been needed for testing. The manipulator arms of ROPOS are in the foreground, waiting for the test to be completed. Photo: OOI/UW/CSSF
Preparing to the ROPOS for the first dive (photo: Judy Twedt)
Preparing to the ROPOS for the first dive (photo: Judy Twedt)
Peparing for the ROPOS dunk test in Puget Sound. Photo by Ben Fundis
Peparing for the ROPOS dunk test in Puget Sound. Photo by Ben Fundis
Small 'chimlet' on the chimney Escargot in the International District hydrothermal field. Photo credit: OOI/UW/CSSF
Small 'chimlet' on the chimney Escargot in the International District hydrothermal field. Photo credit: OOI/UW/CSSF
Fire and boat drill aboard the R/V Thompson during Leg 1 of the VISIONS'13 expedition. Steve. Jason, and Jonathan from the ROPOS Team raced to get survival suits on. Photo by M. Elend.
Fire and boat drill aboard the R/V Thompson during Leg 1 of the VISIONS'13 expedition. Steve. Jason, and Jonathan from the ROPOS Team raced to get survival suits on. Photo by M. Elend.
RSN Cables 4   Photo by Ben Fundis
RSN Cables 4   Photo by Ben Fundis
A close up of the diverse ecosystems hydrothermal vents, such as El Guapo pictured here, support. (credit: OOI/UW/CSSF)
A close up of the diverse ecosystems hydrothermal vents, such as El Guapo pictured here, support. (credit: OOI/UW/CSSF)
Primary Node 1B will connect instruments at the summit of Southern Hydrate Ridge to the Ocean Observatories Initiative's cabled network. (credit: OOI/UW/CSSF)
Primary Node 1B will connect instruments at the summit of Southern Hydrate Ridge to the Ocean Observatories Initiative's cabled network. (credit: OOI/UW/CSSF)
Julie and Allison at the logging station in the control room, making meticulous records of the dive (photo: Judy Twedt)
Julie and Allison at the logging station in the control room, making meticulous records of the dive (photo: Judy Twedt)
Applied Physics Lab engineers Geoff Cram and Skip Denny (left to right) prepare the secondary node for deployment at primary node 1A. (photo: Allison Fundis) 
Applied Physics Lab engineers Geoff Cram and Skip Denny (left to right) prepare the secondary node for deployment at primary node 1A. (photo: Allison Fundis) 
ROCLS, the remotely operated cable laying system, stand ready on R/V Thompson's fantail to deploy the extension cable at primary node 1A. (photo: Allison Fundis) 
ROCLS, the remotely operated cable laying system, stand ready on R/V Thompson's fantail to deploy the extension cable at primary node 1A. (photo: Allison Fundis) 
Students Julie Ann Koehlinger, Claire Knox (left to right), Owen Coyle, and Adrian Rembold (background) in the main lab during the transit out of Newport. (photo: Allison Fundis) 
Students Julie Ann Koehlinger, Claire Knox (left to right), Owen Coyle, and Adrian Rembold (background) in the main lab during the transit out of Newport. (photo: Allison Fundis) 
Co-chief Scientists, John Delaney and Deb Kelley enjoy a laugh (photo: Allison Fundis)
Co-chief Scientists, John Delaney and Deb Kelley enjoy a laugh (photo: Allison Fundis)
Videographer Ben Fundis captures action on the fantail. (photo: Allison Fundis) 
Videographer Ben Fundis captures action on the fantail. (photo: Allison Fundis) 
Undergraduate student Brendan Philip looks at data collected with the ship's multibeam sonar to image methane bubble plumes in the water column. (photo: Allison Fundis) 
Undergraduate student Brendan Philip looks at data collected with the ship's multibeam sonar to image methane bubble plumes in the water column. (photo: Allison Fundis) 
Graduate student Rick Berg, readies the Mosquito instrument that will be deployed at Hydrate Ridge to measure fluid flow out of and into the sedimented seafloor. (photo: Allison Fundis) 
Graduate student Rick Berg, readies the Mosquito instrument that will be deployed at Hydrate Ridge to measure fluid flow out of and into the sedimented seafloor. (photo: Allison Fundis) 
Chief Scientist, John Delaney, updates the whiteboard that serves as the primary message center. It is affectioately nicknamed "The Board of Lies" due to continuously changing and shifting plans at sea. (photo: Allison Fundis) 
Chief Scientist, John Delaney, updates the whiteboard that serves as the primary message center. It is affectioately nicknamed "The Board of Lies" due to continuously changing and shifting plans at sea. (photo: Allison Fundis) 
Applied Physics Lab engineers Tim McGinnis, James Tilley, and Jesse Dosher look over deployment plans. (photo: Allison Fundis) 
Applied Physics Lab engineers Tim McGinnis, James Tilley, and Jesse Dosher look over deployment plans. (photo: Allison Fundis) 
Co-chief Scientist, Deb Kelley, enjoys the view as R/V Thompson sets sail for VISIONS'13 Leg 2. (photo: Allison Fundis)
Co-chief Scientist, Deb Kelley, enjoys the view as R/V Thompson sets sail for VISIONS'13 Leg 2. (photo: Allison Fundis)
Capt. Russ Devaney manuevers the Thompson out of Newport, OR to set sail for Leg 2. (photo: Allison Fundis)
Capt. Russ Devaney manuevers the Thompson out of Newport, OR to set sail for Leg 2. (photo: Allison Fundis)
Leslie and Rick watch the first CTD cast of Leg 2. Photo by Allison Fundis
Leslie and Rick watch the first CTD cast of Leg 2. Photo by Allison Fundis
Marine Tech Brandy shows Julie, Owen, and Judy how to deploy the CTD. Photo by Allison Fundis
Marine Tech Brandy shows Julie, Owen, and Judy how to deploy the CTD. Photo by Allison Fundis
Seconday Node 3A awaits on deck to be deployed at the base of Axial Seamount, where it will eventually be connected to the primary node previously deployed there. Photo by Allison Fundis
Seconday Node 3A awaits on deck to be deployed at the base of Axial Seamount, where it will eventually be connected to the primary node previously deployed there. Photo by Allison Fundis
Primary Node 3A is installed at the base of Axial Volcano and connected to the backbone cable, which is connected to a terrestrial shore station in Pacific City, Oregon. This node provides 10,000 volts of power and 10 Gbs bandwidht for real-time communication. The node is located >300 miles off the coast. Photo Credit: Photo credit: NSF-OOI/UW/CSSF
Primary Node 3A is installed at the base of Axial Volcano and connected to the backbone cable, which is connected to a terrestrial shore station in Pacific City, Oregon. This node provides 10,000 volts of power and 10 Gbs bandwidht for real-time communication. The node is located >300 miles off the coast. Photo Credit: Photo credit: NSF-OOI/UW/CSSF
A medium power Junction Box (MJ01A), was deployed on July 10 near Primary Node 1A at the Slope Base. Photo credit: NSF-OOI/UW/CSSF
A medium power Junction Box (MJ01A), was deployed on July 10 near Primary Node 1A at the Slope Base. Photo credit: NSF-OOI/UW/CSSF
Chief Scientist John Delaney (right) narrates the live video stream as ROPOS pilot Josh Chernov approaches ROCLS, the remotely operated cable laying system, on the seafloor. Photo by Allison Fundis
Chief Scientist John Delaney (right) narrates the live video stream as ROPOS pilot Josh Chernov approaches ROCLS, the remotely operated cable laying system, on the seafloor. Photo by Allison Fundis
ROPOS goes into the water in the early morning of July 10, prior to descending 2600 m (~7800 ft) to the seafloor. Directly latched below the vehicle is the medium-powered junction box, MJ01A. Photo credit: NSF-OOI/UW/CSSF
ROPOS goes into the water in the early morning of July 10, prior to descending 2600 m (~7800 ft) to the seafloor. Directly latched below the vehicle is the medium-powered junction box, MJ01A. Photo credit: NSF-OOI/UW/CSSF
Vincent Auger of ROPOS watches over the ROV and secondary node as they are deployed over the base of Axial Seamount in preparation for deploying ~500 meters of extension cable. Photo by Allison Fundis
Vincent Auger of ROPOS watches over the ROV and secondary node as they are deployed over the base of Axial Seamount in preparation for deploying ~500 meters of extension cable. Photo by Allison Fundis
ROPOS lights up the water column as it begins its descent to the base of Axial Seamount 2600 meters deep. Photo by Allison Fundis
ROPOS lights up the water column as it begins its descent to the base of Axial Seamount 2600 meters deep. Photo by Allison Fundis
An albatross comes in for a landing near R/V Thomas G. Thompson. (photos by Allison Fundis, University of Washington, V13)   
An albatross comes in for a landing near R/V Thomas G. Thompson. (photos by Allison Fundis, University of Washington, V13)   
During dive R-1600, ROPOS connects the 600 m cable deployed at the base of Axial Seamount to a test box on the vehicle to the secondary node at the other end. (credit: NSF-OOI/UW/CSSF)
During dive R-1600, ROPOS connects the 600 m cable deployed at the base of Axial Seamount to a test box on the vehicle to the secondary node at the other end. (credit: NSF-OOI/UW/CSSF)
Leaving Newport Oregon for Southern Hydrate Ridge, the Cascadia Margin, and Axial Volcano.
Leaving Newport Oregon for Southern Hydrate Ridge, the Cascadia Margin, and Axial Volcano.
Brittle stars (Ophiuroids) are very common in the sediments at the base of Axial Seamount, 2609 meters deep.  (credit: NSF-OOI/US/CSSF)
Brittle stars (Ophiuroids) are very common in the sediments at the base of Axial Seamount, 2609 meters deep.  (credit: NSF-OOI/US/CSSF)
Julie Nelson and Orest Kawka sample the CTD water cast after collecting samples from the base of Axial Seamount. Photo by Allison Fundis
Julie Nelson and Orest Kawka sample the CTD water cast after collecting samples from the base of Axial Seamount. Photo by Allison Fundis
ROPOS approaches the cable laying system ROCLS at the base of Axial Seamount. The drum hosts 600 m of extension cable. Photo credit: NSF-OOI/UW/CSSF
ROPOS approaches the cable laying system ROCLS at the base of Axial Seamount. The drum hosts 600 m of extension cable. Photo credit: NSF-OOI/UW/CSSF
Applied Physics Lab engineers (from left to right) Tim McGinnis, Jesse Dosher, and James Tilley look over tests results as ROPOS connects to a secondary node on the seafloor and sends real-time data back to the surface. Photo by Ed McNichol 
Applied Physics Lab engineers (from left to right) Tim McGinnis, Jesse Dosher, and James Tilley look over tests results as ROPOS connects to a secondary node on the seafloor and sends real-time data back to the surface. Photo by Ed McNichol 
Mitch Elend works on creating maps that the ROPOS team will use as a guide as they lay OOI-RSN extension cables. Photo by Ed McNichol 
Mitch Elend works on creating maps that the ROPOS team will use as a guide as they lay OOI-RSN extension cables. Photo by Ed McNichol 
ROPOS pilot and engineer, Josh Chernov, works on the ROV. Photo by Ed McNichol 
ROPOS pilot and engineer, Josh Chernov, works on the ROV. Photo by Ed McNichol 
A small flapjack octopus (one of the species of the genus Opisthoteuthis) doesn't seem to mind being on camera. Credit: UW/OOI-NSF/CSSF, ROPOS Dive R1608, V13.
A small flapjack octopus (one of the species of the genus Opisthoteuthis) doesn't seem to mind being on camera. Credit: UW/OOI-NSF/CSSF, ROPOS Dive R1608, V13.
A small Flapjack octopus sits atop a lobate flow at the summit of Axial Seamount - water depth ~ 1500 m (nearly 5000 feet beneath the surface). Credit: UW/OOI-NSF/CSSF, V13.
A small Flapjack octopus sits atop a lobate flow at the summit of Axial Seamount - water depth ~ 1500 m (nearly 5000 feet beneath the surface). Credit: UW/OOI-NSF/CSSF, V13.
Close up of a soft coral at the southern end of an ~ 60 m tall carbonate Pinnacle at Southern Hydrate Ridge.
Close up of a soft coral at the southern end of an ~ 60 m tall carbonate Pinnacle at Southern Hydrate Ridge.
A purple-hued hagfish weaves its way through the rugged limestone rock at the Pinnacle at South Hydrate. A pink octocoral and orange squat lobster complete the trio. Credit: UW/NSF-OOI/CSSF; ROPOS Dive R1606
A purple-hued hagfish weaves its way through the rugged limestone rock at the Pinnacle at South Hydrate. A pink octocoral and orange squat lobster complete the trio. Credit: UW/NSF-OOI/CSSF; ROPOS Dive R1606
Many of the collapse areas have lava pillars that support remnants of the roof that originally covered a lava pond. Credit: UW/NSF-OOI/CSSF; ROPOS Dive R1608; V13.
Many of the collapse areas have lava pillars that support remnants of the roof that originally covered a lava pond. Credit: UW/NSF-OOI/CSSF; ROPOS Dive R1608; V13.
A young smoker near the base of the suflide edifice called 'Mushroom' emits particle-poor, shimmering water at temperatures  >100oC.  Tube worms, palm worms and limpets bathe in diffusely flowing fluids that vent out of the porous chimney walls and mix with the surrounding, nearly freezing seawater. A high definition camera will be installed at this site providing real-time live imagery in 2014. (VISIONS '13 Dive R-1614) Photo credit:  OOI-NSF/UW/CSSF
A young smoker near the base of the suflide edifice called 'Mushroom' emits particle-poor, shimmering water at temperatures  >100oC.  Tube worms, palm worms and limpets bathe in diffusely flowing fluids that vent out of the porous chimney walls and mix with the surrounding, nearly freezing seawater. A high definition camera will be installed at this site providing real-time live imagery in 2014. (VISIONS '13 Dive R-1614) Photo credit:  OOI-NSF/UW/CSSF
This sulfide chimney, known as Mushroom, rises ~ 4 m (12 ft) above the seafloor. It is located in the ASHES Vent Field and will be the site for deployment of a cabled high definition video camera in 2014 and three-dimensional temperature array, as well as an uncabled vent fluid sampler. Credit: OOI-NSF/UW/CSSF; ROPOS Dive R1614; V13.
This sulfide chimney, known as Mushroom, rises ~ 4 m (12 ft) above the seafloor. It is located in the ASHES Vent Field and will be the site for deployment of a cabled high definition video camera in 2014 and three-dimensional temperature array, as well as an uncabled vent fluid sampler. Credit: OOI-NSF/UW/CSSF; ROPOS Dive R1614; V13.
Live Visions 13 show with John Delaney and Mary Miller from the Exploratorium in the museum's Observatory Gallery on July 30, 2013.
Live Visions 13 show with John Delaney and Mary Miller from the Exploratorium in the museum's Observatory Gallery on July 30, 2013.
First earthquake data from Eastern Caldera subnet. Seen here are two sets of patterns, three panels from each seismometer. VISIONS '13, Leg 3.
First earthquake data from Eastern Caldera subnet. Seen here are two sets of patterns, three panels from each seismometer. VISIONS '13, Leg 3.
VISIONS '13 & Exploratorium interactive broadcast, July 28, 201 Mary Miller, Director of Public Understanding of Science at the Exploratorium in San Francisco, interviews VISIONS '13 Co-Chief Scientist Giora Proskurowski before an audience in the Wired Pier exhibit at the Exploratorium. Photo courtesy of the Exploratorium.
VISIONS '13 & Exploratorium interactive broadcast, July 28, 201 Mary Miller, Director of Public Understanding of Science at the Exploratorium in San Francisco, interviews VISIONS '13 Co-Chief Scientist Giora Proskurowski before an audience in the Wired Pier exhibit at the Exploratorium. Photo courtesy of the Exploratorium.
The thermistor array connected to the computer and power supply.
The thermistor array connected to the computer and power supply.
This thermistor array, designed by Giora Proskurwoski, a Project Scientist as part of the UW cabled observatory team, will allow 3-D measurements to be made in diffuse flow sites over time, with real-time transmission of the data to shore via the cable. Temperature, in part, governs where animals and microbes thrive, expire, and evolve at vent sites. Photo by Mary Levin, UW.
This thermistor array, designed by Giora Proskurwoski, a Project Scientist as part of the UW cabled observatory team, will allow 3-D measurements to be made in diffuse flow sites over time, with real-time transmission of the data to shore via the cable. Temperature, in part, governs where animals and microbes thrive, expire, and evolve at vent sites. Photo by Mary Levin, UW.
Students on VISIONS '13 Leg 3 Left to right: Trevor Uptain, Ryan Cox, Fredrik Ryden, Cody Turner, Marisa Gedney, Montgomery Taylor, Isaac Stockdale, Brendan Philip, Owen Coyle, J.R. Rembert
Students on VISIONS '13 Leg 3 Left to right: Trevor Uptain, Ryan Cox, Fredrik Ryden, Cody Turner, Marisa Gedney, Montgomery Taylor, Isaac Stockdale, Brendan Philip, Owen Coyle, J.R. Rembert
An at-sea tradition is to send styrofoam cups and wig-heads (usually embellished with stylistic artwork) down to the depths so that the overwhelming pressure in the deep sea compresses the objects into miniature versions. (Photo by Leslie Sautter)
An at-sea tradition is to send styrofoam cups and wig-heads (usually embellished with stylistic artwork) down to the depths so that the overwhelming pressure in the deep sea compresses the objects into miniature versions. (Photo by Leslie Sautter)
This relatively small (<1 m) inactive chimney recently toppled over, becoming an excellent sample for collection. (ROPOS Dive #1617, VISIONS '13, Leg 3) Photo credit:  OOI-NSF/UW/CSSF
This relatively small (<1 m) inactive chimney recently toppled over, becoming an excellent sample for collection. (ROPOS Dive #1617, VISIONS '13, Leg 3) Photo credit:  OOI-NSF/UW/CSSF
Deployment of short-period seismometers on the seafloor requires special consideration in terms of the sensors being level. Here, a special platform hosting the seismometer is being leveled by ROPOS through turning of adjustment bolts on the legs. These instruments will provide important real-time data on seismic activity inside the volcano, and associated with microfracturing events around the plumbing system for hydrothermal vents. VISIONS 13, Dive 1617 Photo credit: NSF-OOI/UW/CSSF
Deployment of short-period seismometers on the seafloor requires special consideration in terms of the sensors being level. Here, a special platform hosting the seismometer is being leveled by ROPOS through turning of adjustment bolts on the legs. These instruments will provide important real-time data on seismic activity inside the volcano, and associated with microfracturing events around the plumbing system for hydrothermal vents. VISIONS 13, Dive 1617 Photo credit: NSF-OOI/UW/CSSF
Several crabs dine on a jellyfish buffet on Axial Seamount. (VISIONS '13 Dive R-1615) Photo credit:  OOI-NSF/UW/CSSF
Several crabs dine on a jellyfish buffet on Axial Seamount. (VISIONS '13 Dive R-1615) Photo credit:  OOI-NSF/UW/CSSF
Students Brendan Philip and and Cody Turner work with Professor Julie Nelson in the computer lab.  They are monitoring the temperature and salinity profiles created during the downcast of the CTD to determine the depths for triggering Niskin bottles for seawater collections. VISIONS '13, leg 3 (Photo by Leslie Sautter)
Students Brendan Philip and and Cody Turner work with Professor Julie Nelson in the computer lab.  They are monitoring the temperature and salinity profiles created during the downcast of the CTD to determine the depths for triggering Niskin bottles for seawater collections. VISIONS '13, leg 3 (Photo by Leslie Sautter)
The summit of the actively venting chimney Inferno in 2013, located in the ASHES hydrothermal field at the summit of Axial Seamount. Credit: UW/NSF-OOI/CSSF; V13. Photo credit: NSF-OOI/UW/CSSF
The summit of the actively venting chimney Inferno in 2013, located in the ASHES hydrothermal field at the summit of Axial Seamount. Credit: UW/NSF-OOI/CSSF; V13. Photo credit: NSF-OOI/UW/CSSF
Snail-shaped top of the Escargot hydrothermal vent sulfide structure in the Internationl District area. ROPOS Dive 1617, VISIONS '13, Leg 3. Photo credit NSF-OOI/UW/CSSF
Snail-shaped top of the Escargot hydrothermal vent sulfide structure in the Internationl District area. ROPOS Dive 1617, VISIONS '13, Leg 3. Photo credit NSF-OOI/UW/CSSF
Eight students participated on both Legs 1 and 2.  In the front row, from left:  Adrian Rembold (2nd), Owen Coyle (5th), Claire Knox (6th), Julie Nelson (in pink), Judy Twedt (in blue), Julie Ann Koehlinger (in yellow), and Rick Berg (on the end).  In the back row, from left:  Brendan Philip (1st).  
Eight students participated on both Legs 1 and 2.  In the front row, from left:  Adrian Rembold (2nd), Owen Coyle (5th), Claire Knox (6th), Julie Nelson (in pink), Judy Twedt (in blue), Julie Ann Koehlinger (in yellow), and Rick Berg (on the end).  In the back row, from left:  Brendan Philip (1st).  
Purple protists, ciliates, on hdyrothermal sulfide structure in the International District. White bacterial mats outline diffuse flow cracks. Credit: UW/NSF-OOI/CSSF; ROPOS DIve R1617; V13.
Purple protists, ciliates, on hdyrothermal sulfide structure in the International District. White bacterial mats outline diffuse flow cracks. Credit: UW/NSF-OOI/CSSF; ROPOS DIve R1617; V13.
Part of the work required to properly install a seismometer on the seafloor is to ensure that the instrument is level. The yellow disk, shown here, is placed on the seismometer by ROPOS. The legs of the seismometer platform are then adjusted until a level reading is achieved. Credit: UW/NSF-OOI/CSSF; ROPOS, Dive 1617, V14. Credit: NSF-OOI/UW/CSSF
Part of the work required to properly install a seismometer on the seafloor is to ensure that the instrument is level. The yellow disk, shown here, is placed on the seismometer by ROPOS. The legs of the seismometer platform are then adjusted until a level reading is achieved. Credit: UW/NSF-OOI/CSSF; ROPOS, Dive 1617, V14. Credit: NSF-OOI/UW/CSSF
This resistivity-temperature probe was deployed in the 270°C hydrothermal vent called 'Escargot' at the summit of Axial Volcano in 2013. Resistivity is an analoge for chlorinity or "saltiness' of the hydrothermal fluids. Boiling is common in these venting environments, governing gas concentrations, metal deposition, and perhaps life. A cabled version will be installed in 2014 providing real-time 24/7 data. ROPOS dive #1618, VISIONS '13, Leg 3. Photo credit: NSF-OOI/UW/CSSF.
This resistivity-temperature probe was deployed in the 270°C hydrothermal vent called 'Escargot' at the summit of Axial Volcano in 2013. Resistivity is an analoge for chlorinity or "saltiness' of the hydrothermal fluids. Boiling is common in these venting environments, governing gas concentrations, metal deposition, and perhaps life. A cabled version will be installed in 2014 providing real-time 24/7 data. ROPOS dive #1618, VISIONS '13, Leg 3. Photo credit: NSF-OOI/UW/CSSF.
Students Brendan Philip and Montgomery Taylor use all their strength to position the chimney on the examination table. VISIONS '13, Leg 3 (Photo by Leslie Sautter)
Students Brendan Philip and Montgomery Taylor use all their strength to position the chimney on the examination table. VISIONS '13, Leg 3 (Photo by Leslie Sautter)
Deep Sea Skate sketch, drawn by Montgomery Taylor, a College of Charleston undergraduate student who participated on Leg 3 of VISIONS '13.
Deep Sea Skate sketch, drawn by Montgomery Taylor, a College of Charleston undergraduate student who participated on Leg 3 of VISIONS '13.
ROPOS collects vent chimney sample
ROPOS collects vent chimney sample
This 90 cm, ~100 lbs. chimney was collected from the base of the El Guapo sulfide chimney at the International District Hydrothermal Vent Field on Axial Seamount (ROPOS Dive 1617).  (Photo by Leslie Sautter)
This 90 cm, ~100 lbs. chimney was collected from the base of the El Guapo sulfide chimney at the International District Hydrothermal Vent Field on Axial Seamount (ROPOS Dive 1617).  (Photo by Leslie Sautter)
Crabs eating. VISIONS '13, LEG 3 Photo credit: NSF-OOI/UW/CSSF
Crabs eating. VISIONS '13, LEG 3 Photo credit: NSF-OOI/UW/CSSF
ROV Pilots in the control room, as we examine the black smoker known as Escargot. (photo: Judy Twedt)
ROV Pilots in the control room, as we examine the black smoker known as Escargot. (photo: Judy Twedt)
John Delaney Leg 3 Poetry NIght, VISIONS '13. Photo by Ben Fundis
John Delaney Leg 3 Poetry NIght, VISIONS '13. Photo by Ben Fundis
Fredrik Ryden created a prototype 3D visualization of ROPOS dives for his student project.  This image shows 15 dives simultaneously on Axial Caldera's bathymetry.  The black lines are the RSN cable routes extending from Primary Node PN3B (on the lower right of the image).
Fredrik Ryden created a prototype 3D visualization of ROPOS dives for his student project.  This image shows 15 dives simultaneously on Axial Caldera's bathymetry.  The black lines are the RSN cable routes extending from Primary Node PN3B (on the lower right of the image).
ROPOS was sent down to retrieve a seismometer at the end of VISIONS '13 Leg 3 Photo credit: NSF-OOI/UW/CSSF
ROPOS was sent down to retrieve a seismometer at the end of VISIONS '13 Leg 3 Photo credit: NSF-OOI/UW/CSSF
Cody gaining outreach experience during a live broadcast on the R/V Thompson during Leg 3 of VISIONS'13.
Cody gaining outreach experience during a live broadcast on the R/V Thompson during Leg 3 of VISIONS'13.
Deployment of the Bottom Pressure and Tilt meter off the side of the R/V Thompson in 2013. Credit: M. Elend, University of Washington. V13.
Deployment of the Bottom Pressure and Tilt meter off the side of the R/V Thompson in 2013. Credit: M. Elend, University of Washington. V13.
First day at the Fire and Safety drill onboard the R/V Thompson, I got to practise the 'art' of putting on a survivial suit.
First day at the Fire and Safety drill onboard the R/V Thompson, I got to practise the 'art' of putting on a survivial suit.
Upon leaving Axial Seamount, only one cable reel remains on deck. Leg 3 Visions 13. Photo by Mary Miller.
Upon leaving Axial Seamount, only one cable reel remains on deck. Leg 3 Visions 13. Photo by Mary Miller.
Giora Proskurowski planning a cable route on Axial Seamount during leg 3 during Visions 13. 
Giora Proskurowski planning a cable route on Axial Seamount during leg 3 during Visions 13. 
As her student project, Marisa Gedney is developing an outreach-oriented web site filled with information on Axial Seamount.
As her student project, Marisa Gedney is developing an outreach-oriented web site filled with information on Axial Seamount.
ROPOS termination box.  The fiber optical connections are in front with the BNC like connectors.
ROPOS termination box.  The fiber optical connections are in front with the BNC like connectors.
Iron-rich basalts quickly oxidize in the O2-rich atmosphere once on deck. (Photos by Leslie Sautter)
Iron-rich basalts quickly oxidize in the O2-rich atmosphere once on deck. (Photos by Leslie Sautter)
ROPOS Control Room on R/V Thompson, VISIONS '13 Photo by Fredrik Ryden
ROPOS Control Room on R/V Thompson, VISIONS '13 Photo by Fredrik Ryden
Samples of fresh basalt were collected from Axial Seamount's caldera floor.  When fresh, the outer surface of the rock is glassy due to the very rapid cooling and crystallization that occurs when the hot lava comes in contact with the 2oC seawater.  This glass - known as obsidian - is very sharp and crumbles easily. (Photos by Leslie Sautter)
Samples of fresh basalt were collected from Axial Seamount's caldera floor.  When fresh, the outer surface of the rock is glassy due to the very rapid cooling and crystallization that occurs when the hot lava comes in contact with the 2oC seawater.  This glass - known as obsidian - is very sharp and crumbles easily. (Photos by Leslie Sautter)
Cable draped on pillar at Axial Seamount on leg 3, Visions 13.  Photo credit: NSF-OOI/UW/CSSF
Cable draped on pillar at Axial Seamount on leg 3, Visions 13.  Photo credit: NSF-OOI/UW/CSSF
Empty ROCLS spools on Thompson fantail at end of VISIONS '13, Leg 3, are emblematic of the cable-laying work accomplished.   Photo by Nancy Penrose
Empty ROCLS spools on Thompson fantail at end of VISIONS '13, Leg 3, are emblematic of the cable-laying work accomplished.   Photo by Nancy Penrose
Montgomery Taylor created a portion of a laboratory exercise as her student project.
Montgomery Taylor created a portion of a laboratory exercise as her student project.
A strong plume of methane-rich bubbles issue from the seafloor at the Summit of Southern Hydrate Ridge. This area collapsed sometime between 2010 and 2011, probably due to methane release from the subsurface. VISIONS '13, Leg 4 Photo credit: NSF-OOI/UW/CSSF
A strong plume of methane-rich bubbles issue from the seafloor at the Summit of Southern Hydrate Ridge. This area collapsed sometime between 2010 and 2011, probably due to methane release from the subsurface. VISIONS '13, Leg 4 Photo credit: NSF-OOI/UW/CSSF
The remotely operated vehicle ROPOS used a snap hook connected to a line on its underbelly, hooked into the frame of the CTD for recovery to the surface. The CTD wire failed as the sensor-sampling package was being recovered onto the deck of the Thompon. Luckily, after its >9000 free descent to the seafloor, it landed upright in the soft sediment. Photo credit: NSF-OOI/UW/CSSF.
The remotely operated vehicle ROPOS used a snap hook connected to a line on its underbelly, hooked into the frame of the CTD for recovery to the surface. The CTD wire failed as the sensor-sampling package was being recovered onto the deck of the Thompon. Luckily, after its >9000 free descent to the seafloor, it landed upright in the soft sediment. Photo credit: NSF-OOI/UW/CSSF.
The CTD is recovered from a water depth of 2902 m at the base of the subduction zone at a site where full water column moorings will be deployed next year and connected to the cable. The ROV ROPOS attached a snaphook to the top of the CTD frame, securing it under the ROV for transport to the surface. Photo credit: NSF-OOI/UW/CSSF.
The CTD is recovered from a water depth of 2902 m at the base of the subduction zone at a site where full water column moorings will be deployed next year and connected to the cable. The ROV ROPOS attached a snaphook to the top of the CTD frame, securing it under the ROV for transport to the surface. Photo credit: NSF-OOI/UW/CSSF.
The ROV ROPOS vacuums out sediment in a caisson at the summit of Southern Hydrate Ridge. In 2014, a broadband seismometer will be placed in the caisson and covered in silica beads to optimize acquisition of acoustic signals by lowering ocean "noise" (e.g. currents). Credit: UW/NSF-OOI/CSSF.
The ROV ROPOS vacuums out sediment in a caisson at the summit of Southern Hydrate Ridge. In 2014, a broadband seismometer will be placed in the caisson and covered in silica beads to optimize acquisition of acoustic signals by lowering ocean "noise" (e.g. currents). Credit: UW/NSF-OOI/CSSF.
Judy leaviing Seattle to begin the VISIONS'13 adventure.
Judy leaviing Seattle to begin the VISIONS'13 adventure.
This caisson is buried to about 1 m depth beneath the sediments. Next year a broadband seismometer will be placed in it and connected to the cable, providing real-time detection and location of earthquakes. A cover was placed over the caisson to keep sediment from falling into it and animals out. Credit: UW/NSF-OOI/CSSF. V13.
This caisson is buried to about 1 m depth beneath the sediments. Next year a broadband seismometer will be placed in it and connected to the cable, providing real-time detection and location of earthquakes. A cover was placed over the caisson to keep sediment from falling into it and animals out. Credit: UW/NSF-OOI/CSSF. V13.
Graneledone Octopus on lava dlows at the summit of Axial Seamount. Credit: UW/OOI-NSF/CSSF, ROPOS Dive R1617, V13.
Graneledone Octopus on lava dlows at the summit of Axial Seamount. Credit: UW/OOI-NSF/CSSF, ROPOS Dive R1617, V13.
ROV ROPOS with MJ03E. VISIONS '13, Leg 3
ROV ROPOS with MJ03E. VISIONS '13, Leg 3
The seafloor records where a small lava river once flowed.  The "banks" are pieces of the solidified lava that were shoved and broken by the swifter, central stream. (VISIONS '13 Dive R-1613) Photo credit:  OOI-NSF/UW/CSSF
The seafloor records where a small lava river once flowed.  The "banks" are pieces of the solidified lava that were shoved and broken by the swifter, central stream. (VISIONS '13 Dive R-1613) Photo credit:  OOI-NSF/UW/CSSF
Flattened oil-filled hose on the horn of the ROV ROPOS Remotely Operated Cable Laying System (ROCLS), VISIONS '13 Dive 1610 Photo credit: OOI-NSF/UW/CSSF
Flattened oil-filled hose on the horn of the ROV ROPOS Remotely Operated Cable Laying System (ROCLS), VISIONS '13 Dive 1610 Photo credit: OOI-NSF/UW/CSSF
Octopus on a lava flow in the caldera of Axial Volcano at a depth of ~ 1500 m (nearly 5000 ft beneath the oceans surface). Credit; UW/NSF-OOI/CSSF; V13.
Octopus on a lava flow in the caldera of Axial Volcano at a depth of ~ 1500 m (nearly 5000 ft beneath the oceans surface). Credit; UW/NSF-OOI/CSSF; V13.
This orange, secondary cable was laid about one week ago by ROPOS. The image, taken during the cable inspection portion of Dive 1608, shows the cable on top of pillow basalts on the seafloor at Axial Volcano. Photo credit: OOI-NSF/UW/CSSF
This orange, secondary cable was laid about one week ago by ROPOS. The image, taken during the cable inspection portion of Dive 1608, shows the cable on top of pillow basalts on the seafloor at Axial Volcano. Photo credit: OOI-NSF/UW/CSSF
A cable that will link an instrument to a Secondary Node is buoyant enough so that it easily spans across a large collapse area without danger of abrasion. (VISIONS '13 Dive R-1611) Photo credit:  OOI-NSF/UW/CSSF
A cable that will link an instrument to a Secondary Node is buoyant enough so that it easily spans across a large collapse area without danger of abrasion. (VISIONS '13 Dive R-1611) Photo credit:  OOI-NSF/UW/CSSF
Cooling lava takes on different shapes, depending on the temperature and vigor of the flow.  Here, lava lobes, sheet flow and jumbled flow types fill the frame near to the Ashes vent site on Axial. (VISIONS '13 Dive R-1613) Photo credit:  OOI-NSF/UW/CSSF
Cooling lava takes on different shapes, depending on the temperature and vigor of the flow.  Here, lava lobes, sheet flow and jumbled flow types fill the frame near to the Ashes vent site on Axial. (VISIONS '13 Dive R-1613) Photo credit:  OOI-NSF/UW/CSSF
The thermistor array will be deployed at the base of the hydrothermal vent Mushroom, on the lower right side of this image on top of the yellow incubators.
The thermistor array will be deployed at the base of the hydrothermal vent Mushroom, on the lower right side of this image on top of the yellow incubators.
The testing box on ROPOS was used to plug into a 4356 m (14291 ft!) long extension cable (RS03W7) that starts at  Primary Node 3B on the northern side of the caldera, runs clear across the caldera, and ends just west of the black smokers in a zone of safety. It will provide power and communication to two short-period seismometers and a three dimensional temperature array deployed in a diffuse flow site at the base of the chimney called Mushroom. VISIONS '13, Leg 3
The testing box on ROPOS was used to plug into a 4356 m (14291 ft!) long extension cable (RS03W7) that starts at  Primary Node 3B on the northern side of the caldera, runs clear across the caldera, and ends just west of the black smokers in a zone of safety. It will provide power and communication to two short-period seismometers and a three dimensional temperature array deployed in a diffuse flow site at the base of the chimney called Mushroom. VISIONS '13, Leg 3
Safety is a priority aboard the R/V Thompson, and part of that is learing to rapidly put on an emergency life suit.
Safety is a priority aboard the R/V Thompson, and part of that is learing to rapidly put on an emergency life suit.
Moon over Newport upon our departure Photo by Montgomery Taylor
Moon over Newport upon our departure Photo by Montgomery Taylor
Sunset   Photo by Fredrik Ryden
Sunset   Photo by Fredrik Ryden
Sunset at NOAA Dock in Newport, Oregon from the Thompson Photo by Montgomery Taylor
Sunset at NOAA Dock in Newport, Oregon from the Thompson Photo by Montgomery Taylor
One of ROPOS’ “claws” that can be manipulated from the ship to do many tasks on the infrastructure deployed to the seafloor. Photo by Montgomery Taylor
One of ROPOS’ “claws” that can be manipulated from the ship to do many tasks on the infrastructure deployed to the seafloor. Photo by Montgomery Taylor
Sketch of Graneledone Octopus by Montgomery Taylor, College of Charleston student onboard Leg 3 of VISIONS '13.
Sketch of Graneledone Octopus by Montgomery Taylor, College of Charleston student onboard Leg 3 of VISIONS '13.
Fiber Optic Cable we are using to connect all of the pieces of our Regional Scale Nodes puzzle Photo by Montgomery Taylor
Fiber Optic Cable we are using to connect all of the pieces of our Regional Scale Nodes puzzle Photo by Montgomery Taylor
The bow of the Thompson, with the bridge in the background Photo by Montgomery Taylor
The bow of the Thompson, with the bridge in the background Photo by Montgomery Taylor
John and James check out the caisson on the tool sled prior to deployment. VISIONS '13, Leg 4 Photo by Mitchell Elend
John and James check out the caisson on the tool sled prior to deployment. VISIONS '13, Leg 4 Photo by Mitchell Elend
A great learning experience regarding the impact of pressure on materials is provided by placing styrofoam cups and heads in mesh bags on the CTD and deploying them >9000 feet beneath the oceans surface. This image shows a very small head that experienced a 'free fall' event when the CTD wire parted after a prior 9000 foot planned trip to the seafloor during routine CTD operations. A wig head that has not yet made it to the seafloor is shown on the right for comparison. Oh, and Deb Kelley's head is used for scale.
A great learning experience regarding the impact of pressure on materials is provided by placing styrofoam cups and heads in mesh bags on the CTD and deploying them >9000 feet beneath the oceans surface. This image shows a very small head that experienced a 'free fall' event when the CTD wire parted after a prior 9000 foot planned trip to the seafloor during routine CTD operations. A wig head that has not yet made it to the seafloor is shown on the right for comparison. Oh, and Deb Kelley's head is used for scale.
A holothurian forages at 9000 ft at the base of the continental margin ~ 125 km off Newport Oregon. VISIONS '13, Leg 4 Photo credit: NSF-OOI/UW/CSSF.
A holothurian forages at 9000 ft at the base of the continental margin ~ 125 km off Newport Oregon. VISIONS '13, Leg 4 Photo credit: NSF-OOI/UW/CSSF.
I got to collect fluid samples with Colin from the Niskin bottles on the CTD for follow-on shore-based analyses.  Photo Credit: Mitch Elend
I got to collect fluid samples with Colin from the Niskin bottles on the CTD for follow-on shore-based analyses.  Photo Credit: Mitch Elend
The CTD was safely brought onboard after its freefall >9000 feet to the seafloor below. A follow-on test showed it was ok.
The CTD was safely brought onboard after its freefall >9000 feet to the seafloor below. A follow-on test showed it was ok.
Beautiful striated pillow basalts form a thick flow on the floor of Axial Seamount. Credit: UW/NSF-OOI/CSSF, ROPOS Dive R1630; V13
Beautiful striated pillow basalts form a thick flow on the floor of Axial Seamount. Credit: UW/NSF-OOI/CSSF, ROPOS Dive R1630; V13
A crab picks its way across a glassy, jumbled lava flow in the caldera of Axial Seamount. VISIONS '13, Leg 4 Photo credit: NSF-OOI/UW/CSSF
A crab picks its way across a glassy, jumbled lava flow in the caldera of Axial Seamount. VISIONS '13, Leg 4 Photo credit: NSF-OOI/UW/CSSF
During Leg 4 of the VISIONS'13 cruise, old battery-powered transponders were recovered because they present navigation hazards. A sharp knife held in the manipulator is used to cut the 150-200 m tether at its base, and it and the transponder come to the surface where they are recovered on the ship. Photo credit: NSF-OOI/UW/CSSF
During Leg 4 of the VISIONS'13 cruise, old battery-powered transponders were recovered because they present navigation hazards. A sharp knife held in the manipulator is used to cut the 150-200 m tether at its base, and it and the transponder come to the surface where they are recovered on the ship. Photo credit: NSF-OOI/UW/CSSF
Small sulfide chimneys vent high temperature fluids at the base of the Mushroom sulfide edifice. Dense tubeworm (red plumes), palm worm (brown red plumes), and limpet macrofaunal assemblages completely cover most of the edifice. Credit: UW/NSF-OOI/CSSF. V13.
Small sulfide chimneys vent high temperature fluids at the base of the Mushroom sulfide edifice. Dense tubeworm (red plumes), palm worm (brown red plumes), and limpet macrofaunal assemblages completely cover most of the edifice. Credit: UW/NSF-OOI/CSSF. V13.
A fossilized lava pond reflects past circulation of melt on the seafloor in a small lava lake. The surface is glass, and fine sediments highight the whirl. VISIONS '13, Leg 4 Photo credit: NSF-OOI/UW/CSSF
A fossilized lava pond reflects past circulation of melt on the seafloor in a small lava lake. The surface is glass, and fine sediments highight the whirl. VISIONS '13, Leg 4 Photo credit: NSF-OOI/UW/CSSF
My first time sampling fluid on Leg 4 from a water cast at the base of the continental slope.
My first time sampling fluid on Leg 4 from a water cast at the base of the continental slope.
Beautiful sheet flow swirl with broken hackly edges. Credit: UW/NSF-OOI/CSSF; V13.
Beautiful sheet flow swirl with broken hackly edges. Credit: UW/NSF-OOI/CSSF; V13.
The R/V Thompson crew watches from the bow as the Thompson transits through the channel our of Newport Oregon into the Pacific for the start of Leg 4 of the VISIONS'13 Expedition. Photo Credit: Mitch Elend, University of Washington.
The R/V Thompson crew watches from the bow as the Thompson transits through the channel our of Newport Oregon into the Pacific for the start of Leg 4 of the VISIONS'13 Expedition. Photo Credit: Mitch Elend, University of Washington.
A large Fried Egg Jellyfish (Phacellophora cantschatica) hugs the basalts along the floor of Axial Seamount. The jellyfish is likely a 'fried egg' jelly. Credit: UW/NSF-OOI/CSSF; ROPOS Dive R1635, V11.
A large Fried Egg Jellyfish (Phacellophora cantschatica) hugs the basalts along the floor of Axial Seamount. The jellyfish is likely a 'fried egg' jelly. Credit: UW/NSF-OOI/CSSF; ROPOS Dive R1635, V11.
The 3D thermistor array designed by RCA Project Scientist Giora Proskurowski is attached to the Medium Powered J-BOx (MJ03B) in the ASHES hydrothermal field. The array will be tested on a follow-on dive, and in 2014 it will be deployed in a diffuse flow site at the base of the vent called Mushroom, along with a high-definition video camera and an osmo vent fluid sampler. Credit: UW/NSF-OOI/CSSF; V13.
The 3D thermistor array designed by RCA Project Scientist Giora Proskurowski is attached to the Medium Powered J-BOx (MJ03B) in the ASHES hydrothermal field. The array will be tested on a follow-on dive, and in 2014 it will be deployed in a diffuse flow site at the base of the vent called Mushroom, along with a high-definition video camera and an osmo vent fluid sampler. Credit: UW/NSF-OOI/CSSF; V13.
Caitlin and Andrew take water samples from a CTD cast ~ 125 km off the coast of Oregon to characterize fluids up to 9000 ft beneath the oceans surface.
Caitlin and Andrew take water samples from a CTD cast ~ 125 km off the coast of Oregon to characterize fluids up to 9000 ft beneath the oceans surface.
A bit of relaxation time on a cloudy, but mild Sunday morning...Day 41 on the R/V Thompson for Brendan Philip. Photo Credit: Mitch Elend, University of Washington.
A bit of relaxation time on a cloudy, but mild Sunday morning...Day 41 on the R/V Thompson for Brendan Philip. Photo Credit: Mitch Elend, University of Washington.
University of Washington undergraduate student Colin Katagiri and RSN Project Scientist Orest Kawka process fluids collected from ~ 125 off the coast of Newport Oregon at water depths from as great as 9000 ft beneath the oceans surface. Chemical and biological data collected on these samples will be used to optimize sampling strategies of sensors on cabled moorings to be installed at this site next year as part of the Ocean Observatories Initiative. VISIONS '13, Leg 4 Photo Credit: Mitch Elend, University of Washington.
University of Washington undergraduate student Colin Katagiri and RSN Project Scientist Orest Kawka process fluids collected from ~ 125 off the coast of Newport Oregon at water depths from as great as 9000 ft beneath the oceans surface. Chemical and biological data collected on these samples will be used to optimize sampling strategies of sensors on cabled moorings to be installed at this site next year as part of the Ocean Observatories Initiative. VISIONS '13, Leg 4 Photo Credit: Mitch Elend, University of Washington.
A 3D thermistor array designed by RSN Project Scientist Dr. Giora Proskurowski is deployed in the ASHES vent field for testing. A similar system will be deployed and powered up next summer, providing real-time 24/7 temperature data over the Internet for all to use/see. The blue cable holds 24 temperature sensors and was provided by RBR Ltd. The array will be placed in a diffuse flow site at the base of the vent called Mushroom, a site hosting abundant vent fauna. These data, coupled with seismic information, fluid chemistry, and HD imagery will be used to see how these systems evolve over time and how earthquakes influence chemical and biological processes. VISIONS '13, Leg 4   Photo credit: NSF-OOI/UW/CSSF
A 3D thermistor array designed by RSN Project Scientist Dr. Giora Proskurowski is deployed in the ASHES vent field for testing. A similar system will be deployed and powered up next summer, providing real-time 24/7 temperature data over the Internet for all to use/see. The blue cable holds 24 temperature sensors and was provided by RBR Ltd. The array will be placed in a diffuse flow site at the base of the vent called Mushroom, a site hosting abundant vent fauna. These data, coupled with seismic information, fluid chemistry, and HD imagery will be used to see how these systems evolve over time and how earthquakes influence chemical and biological processes. VISIONS '13, Leg 4   Photo credit: NSF-OOI/UW/CSSF
This 60-m extension cable will soon host a high-definition video camera to be deployed at the Mushroom hydrothermal vent (far left). White microbial mats along narrow fractures in the lobate lava flows mark areas where low-temperature diffuse hydrothermal fluids issue from the seafloor. The 7-function manipulator arms of the Canadian ROV ROPOS gently place the wet-mate connector holding plate on the seafloor. VISIONS '13 Leg 4 Photo credit: NSF-OOI/UW/CSSF.
This 60-m extension cable will soon host a high-definition video camera to be deployed at the Mushroom hydrothermal vent (far left). White microbial mats along narrow fractures in the lobate lava flows mark areas where low-temperature diffuse hydrothermal fluids issue from the seafloor. The 7-function manipulator arms of the Canadian ROV ROPOS gently place the wet-mate connector holding plate on the seafloor. VISIONS '13 Leg 4 Photo credit: NSF-OOI/UW/CSSF.
Several members of the Leg 3 VISIONS'13 team gaze to the west upon leaving Newport at the start of VISIONS '13 Leg 3. Photo by Mary Miller
Several members of the Leg 3 VISIONS'13 team gaze to the west upon leaving Newport at the start of VISIONS '13 Leg 3. Photo by Mary Miller
Putting on an immersion suit is harder than it seems!
Putting on an immersion suit is harder than it seems!
Julie Ann and Claire sit on the upper deck of the R/V Thompson as it goes through the Ballard locks on Leg 1 of VISIONS'13.
Julie Ann and Claire sit on the upper deck of the R/V Thompson as it goes through the Ballard locks on Leg 1 of VISIONS'13.
Issac on Leg 3 of the VISIONS'13 Expedition.
Issac on Leg 3 of the VISIONS'13 Expedition.
Brendan Philip, VISIONS '13 Leg 3 Poetry Night, gets a laugh from Brian Clampitt while reading his poem. Photo by Ben Fundis
Brendan Philip, VISIONS '13 Leg 3 Poetry Night, gets a laugh from Brian Clampitt while reading his poem. Photo by Ben Fundis
Fredrik Ryden (holding Neruda poetry book) and Thompson Captain Russ Devaney, VISIONS '13, Leg 3 Poetry Night
Fredrik Ryden (holding Neruda poetry book) and Thompson Captain Russ Devaney, VISIONS '13, Leg 3 Poetry Night
Ed McNichol, VISIONS 13, Leg 3 Poetry Night, tells the girl, the boy, and the pig story.  Photo by Ben Fundis
Ed McNichol, VISIONS 13, Leg 3 Poetry Night, tells the girl, the boy, and the pig story.  Photo by Ben Fundis
Leg 3 included a wonderful mix of scientists, engineers, ROPOS crew, educators and students.
Leg 3 included a wonderful mix of scientists, engineers, ROPOS crew, educators and students.
Ryan Cox, performs for the VISIONS '13, Leg 3 Poetry Night. Photo by Ben Fundis
Ryan Cox, performs for the VISIONS '13, Leg 3 Poetry Night. Photo by Ben Fundis
Left to right: Julie Nelson, Montgomery Taylor, and J. Ryan Rembert, VISIONS '13 Leg 3 Poetry night. Photo by Ben Fundis
Left to right: Julie Nelson, Montgomery Taylor, and J. Ryan Rembert, VISIONS '13 Leg 3 Poetry night. Photo by Ben Fundis
Ship's crew member, Dana Africa, reads a shaggy dog story on Poetry Night, Leg 3, VISIONS '13. Photo by Ben Fundis
Ship's crew member, Dana Africa, reads a shaggy dog story on Poetry Night, Leg 3, VISIONS '13. Photo by Ben Fundis
Owen Coyle showing student Adrian Rembold how to collect water samples during VISIONS'13, Leg 2. Photo by Mitchell Elend
Owen Coyle showing student Adrian Rembold how to collect water samples during VISIONS'13, Leg 2. Photo by Mitchell Elend
Cody Turner and John Delaney conduct a live broadcast from aboard the R/V Thompson during the VISIONS '13 Expedition, Leg 3. (Photos by Leslie Sautter)
Cody Turner and John Delaney conduct a live broadcast from aboard the R/V Thompson during the VISIONS '13 Expedition, Leg 3. (Photos by Leslie Sautter)
Sketch of “Castle” Hydrothermal Vent (International District, Axial Seamount) Sketch and photo by Montgomery Taylor
Sketch of “Castle” Hydrothermal Vent (International District, Axial Seamount) Sketch and photo by Montgomery Taylor
The bottom pressure and tilt instrument (BOPT), designed by Bill Chadwick of Oregon State University, being deployed onto the seafloor at Axial Seamount by ROPOS as part of the VISIONS'13 expedition. Credit: UW/OOI-NSF/CSSF; V13.
The bottom pressure and tilt instrument (BOPT), designed by Bill Chadwick of Oregon State University, being deployed onto the seafloor at Axial Seamount by ROPOS as part of the VISIONS'13 expedition. Credit: UW/OOI-NSF/CSSF; V13.
ROPOS enters the water on dive 1604 during VISIONS'13. Photo Credit. Mitch Elend.
ROPOS enters the water on dive 1604 during VISIONS'13. Photo Credit. Mitch Elend.
Water streams off ROPOS as it is being recovered onto the deck of the R/V Thompson - it was a beautiful blue-sky day. Photo Credit: Mitch Elend, University of Washington. VISIONS '13, Leg 4
Water streams off ROPOS as it is being recovered onto the deck of the R/V Thompson - it was a beautiful blue-sky day. Photo Credit: Mitch Elend, University of Washington. VISIONS '13, Leg 4
A break in the overcast days brings on great sunny weather for sampling water from the CTD. Photo Credit: Mitch Elend, University of Washingotn.
A break in the overcast days brings on great sunny weather for sampling water from the CTD. Photo Credit: Mitch Elend, University of Washingotn.
Close-up view of a microbial experiment (tubes at right) being conducted by Harvard University. The experiment is located in a diffuse flow site, surrounded by limpets, small tube worms and palm worms. In part, this study is designed to look at microbial utilization of sulfur in these systems. The green lasers from the ROV ROPOS are 10 cm apart. VISIONS '13, Leg 4 Photo credit: NSF-OOI/UW/CSSF.
Close-up view of a microbial experiment (tubes at right) being conducted by Harvard University. The experiment is located in a diffuse flow site, surrounded by limpets, small tube worms and palm worms. In part, this study is designed to look at microbial utilization of sulfur in these systems. The green lasers from the ROV ROPOS are 10 cm apart. VISIONS '13, Leg 4 Photo credit: NSF-OOI/UW/CSSF.
During the UW-OOI-NSF VISIONS'13 Expedition, the remotely operated vehicle ROPOS installed three medium power J-Boxes (secondary nodes) utilizing their special 4,000 lb heavy lift capabilities. ROPOS took this RSN J-Box down on dive R1601. The broad feet on the J-Box are used for installation in heavily sedimented areas. This was an unusually calm day at sea in the NE Pacific. Photo Credit: Mitch Elend, University of Washington.
During the UW-OOI-NSF VISIONS'13 Expedition, the remotely operated vehicle ROPOS installed three medium power J-Boxes (secondary nodes) utilizing their special 4,000 lb heavy lift capabilities. ROPOS took this RSN J-Box down on dive R1601. The broad feet on the J-Box are used for installation in heavily sedimented areas. This was an unusually calm day at sea in the NE Pacific. Photo Credit: Mitch Elend, University of Washington.
ROPOS decends to the seafloor during the VISIONS'13 expedition. Photo Credit: Mitch Elend, University of Washington
ROPOS decends to the seafloor during the VISIONS'13 expedition. Photo Credit: Mitch Elend, University of Washington
The RCA high definition camera at the base of the hydrothermal vent called Mushroom. Credit: UW/NSF-OOI/CSSF; ROPOS Dive R1636; V13.
The RCA high definition camera at the base of the hydrothermal vent called Mushroom. Credit: UW/NSF-OOI/CSSF; ROPOS Dive R1636; V13.
Dr. Danny Grumbaum and Owen Coyle are developing this sea-going, flow-through system. VISIONS '13, Leg 3
Dr. Danny Grumbaum and Owen Coyle are developing this sea-going, flow-through system. VISIONS '13, Leg 3
Numerous spools of extension cables await deployment on Leg 3. When completed, the VISIONS13 program will have installed ~23,000 m of cable on the seafloor.
Numerous spools of extension cables await deployment on Leg 3. When completed, the VISIONS13 program will have installed ~23,000 m of cable on the seafloor.
High-temperature, near-boiling fluids jet from small spigots on the top of the metal-sulfide, black-smoker chimney called El Guapo (the handsome one) in the International District Hydrothermal Field. VISIONS '13, Leg 4. Photo credit: NSF-OOI/UW/CSSF
High-temperature, near-boiling fluids jet from small spigots on the top of the metal-sulfide, black-smoker chimney called El Guapo (the handsome one) in the International District Hydrothermal Field. VISIONS '13, Leg 4. Photo credit: NSF-OOI/UW/CSSF
A Mola mola (or sunfish) gently passes by the R/V Thompson - they are the heaviest known bony fish. The other day we saw albatross picking parasites off of them as they wafted by. Credit: Mitch Elend, University of Washington, V13.
A Mola mola (or sunfish) gently passes by the R/V Thompson - they are the heaviest known bony fish. The other day we saw albatross picking parasites off of them as they wafted by. Credit: Mitch Elend, University of Washington, V13.
The ROV ROPOS powers up the RSN-OOI camera for the first time at the hydrothermal chimney called Mushroom. This image is from ROPOS with the vehicle lights off, and only the RSN-OOI HD camera providing illumination of the chimney while collecting the first video imagery from the seafloor, which was then streamed live over the Internet. Photo credit: NSF-OOI/UW/CSSF.
The ROV ROPOS powers up the RSN-OOI camera for the first time at the hydrothermal chimney called Mushroom. This image is from ROPOS with the vehicle lights off, and only the RSN-OOI HD camera providing illumination of the chimney while collecting the first video imagery from the seafloor, which was then streamed live over the Internet. Photo credit: NSF-OOI/UW/CSSF.
This high resolution bathymetric map of the ASHES hydrothermal field shows the location of small, ~ 4 m tall, actively venting sulfide structures. The field is located near the steep western caldera wall. The field is likely fed by fluids circulating up along faults associated with this wall. 
This high resolution bathymetric map of the ASHES hydrothermal field shows the location of small, ~ 4 m tall, actively venting sulfide structures. The field is located near the steep western caldera wall. The field is likely fed by fluids circulating up along faults associated with this wall. 
Paul gives a tour of the T/V Thompsons engine room to VISIONS'13 students.
Paul gives a tour of the T/V Thompsons engine room to VISIONS'13 students.
Caitlin looks at a microbial experiment brought up from hydrothermal diffuse flow site at the base of the chimney called Mushroom: water depth ~ 5000 ft. Photo Credit: Mitch Elend, University of Washington.
Caitlin looks at a microbial experiment brought up from hydrothermal diffuse flow site at the base of the chimney called Mushroom: water depth ~ 5000 ft. Photo Credit: Mitch Elend, University of Washington.
The summit of this hydrothermal chimney, called 'Eascargot', has a striking resemblance to a snail. A 270°C actively venting site (two small white chimneys mid structure) will host a cabled temperature-resistivity sensor there in 2014. This sensor will provide real-time data on the fluid chemistry (chlorinity) -temperature relationships inside the vent. The instrument was designed by Marv Lilley, University of Washington. VISIONS '13, Leg 4. Photo credit: NSF-OOI/UW/CSSF
The summit of this hydrothermal chimney, called 'Eascargot', has a striking resemblance to a snail. A 270°C actively venting site (two small white chimneys mid structure) will host a cabled temperature-resistivity sensor there in 2014. This sensor will provide real-time data on the fluid chemistry (chlorinity) -temperature relationships inside the vent. The instrument was designed by Marv Lilley, University of Washington. VISIONS '13, Leg 4. Photo credit: NSF-OOI/UW/CSSF
This short-period seismometer was deployed on a flat sheet flow ~ 1.3 km east of the ASHES hydrothermal field in 2013. The black ball in the yellow circle shows that it is perfectly level, helping to insure that the highest quality data comes off of this network. Axial Volcano is likely to be quite seismically active and we are anxious to get the real-time data on shore next year. This will help us understand magma and fluid migration in the subsurface of the volcano...and eventually these data may help us predict an eruption. Several earthquakes were detected in real-time during testing of these seismometers in 2013. Credit: UW/NSF-OOI/CSSF, ROPOS Dive R1635; V13.
This short-period seismometer was deployed on a flat sheet flow ~ 1.3 km east of the ASHES hydrothermal field in 2013. The black ball in the yellow circle shows that it is perfectly level, helping to insure that the highest quality data comes off of this network. Axial Volcano is likely to be quite seismically active and we are anxious to get the real-time data on shore next year. This will help us understand magma and fluid migration in the subsurface of the volcano...and eventually these data may help us predict an eruption. Several earthquakes were detected in real-time during testing of these seismometers in 2013. Credit: UW/NSF-OOI/CSSF, ROPOS Dive R1635; V13.
A Deep-Sea Cucumber (Holothurian) is shown with brittle stars and a seastar on a lobate flow on Axial Volcano. This is likely the species Pannychia moseleyi. Photo credit: NSF-OOI/UW/CSSF; V13
A Deep-Sea Cucumber (Holothurian) is shown with brittle stars and a seastar on a lobate flow on Axial Volcano. This is likely the species Pannychia moseleyi. Photo credit: NSF-OOI/UW/CSSF; V13
An Argo Float just being released from the R/V Thompson during the VISIONS'13 program. It will collect chemical measurements to depths of 1000 m, surfacing every 5-10 days to transmit these data back to shore via a satellite. Photo Credit: Mitch Elend, University of Washington.
An Argo Float just being released from the R/V Thompson during the VISIONS'13 program. It will collect chemical measurements to depths of 1000 m, surfacing every 5-10 days to transmit these data back to shore via a satellite. Photo Credit: Mitch Elend, University of Washington.
Charlie watches an Argo Float drift past the R/V Thompson following his deployment of it 200 m northeast of the Primary Node location for the Regional Scale Nodes program. We are especially anxious to see the results of the ISUS nitrate sensor on it as it makes measurements above Axial Seamount. Photo Credit: Mitch Elend, University of Washington.
Charlie watches an Argo Float drift past the R/V Thompson following his deployment of it 200 m northeast of the Primary Node location for the Regional Scale Nodes program. We are especially anxious to see the results of the ISUS nitrate sensor on it as it makes measurements above Axial Seamount. Photo Credit: Mitch Elend, University of Washington.
A resistivity-temperature probe, developed by Dr. Marv Lilley at the University of Washington, was deployed into a 270°C actively venting orifice on the chimney called Escargot. Resistivity is an analogue for chlorinity. Some of the vents in the International District are boiling, causing release of very gas-rich, low-salinity fluids. This instrument, recovered on ROPOS dive 1638, was deployed on a small ledge on the structure a few weeks previously with power provided by batteries in the titanium housing. The orange-white taped cable leads to the wand that is inserted into the chimney (not shown in this image). The white, feathery material on the outside of the chimney is filamentous bacteria, supported by low-temperature diffuse fluids that waft up the side of the chimney. Photo credit: NSF-OOI/UW/CSSF
A resistivity-temperature probe, developed by Dr. Marv Lilley at the University of Washington, was deployed into a 270°C actively venting orifice on the chimney called Escargot. Resistivity is an analogue for chlorinity. Some of the vents in the International District are boiling, causing release of very gas-rich, low-salinity fluids. This instrument, recovered on ROPOS dive 1638, was deployed on a small ledge on the structure a few weeks previously with power provided by batteries in the titanium housing. The orange-white taped cable leads to the wand that is inserted into the chimney (not shown in this image). The white, feathery material on the outside of the chimney is filamentous bacteria, supported by low-temperature diffuse fluids that waft up the side of the chimney. Photo credit: NSF-OOI/UW/CSSF
University of Washington, School of Oceanography undergraduate student - Charlie Parker- deploys an Argo float over Axial Seamount during the VISIONS'13 program. The float wil submerge to 1000 m beneath the surface, taking chemical measurements along the way, and every 5-10 days will surface and transmit these data over a satellite to shore. Photo Credit: Mitch Elend, University of Washington.
University of Washington, School of Oceanography undergraduate student - Charlie Parker- deploys an Argo float over Axial Seamount during the VISIONS'13 program. The float wil submerge to 1000 m beneath the surface, taking chemical measurements along the way, and every 5-10 days will surface and transmit these data over a satellite to shore. Photo Credit: Mitch Elend, University of Washington.
Brittle stars of the species Spinophiura jolliveti are very abundant on all the lava rocks at Axial Seamount within the caldera. Photo credit: NSF-OOI/UW/CSSF.
Brittle stars of the species Spinophiura jolliveti are very abundant on all the lava rocks at Axial Seamount within the caldera. Photo credit: NSF-OOI/UW/CSSF.
The Diva hydrothermal vent, is a 277°C small, fragile anhydrite (CaSO4) structure in the International District vent field on Axial Volcano. The chimney is of interest because it has the highest carbon dioxide concentrations of any of the chimneys within the Axial caldera. In 2014, it will host an instrument developed by Dr. Bill Seyfried, University of Minnesota,  that will provide real-time streaming data on acidity, hydrogen sulfide, hydrogen and temperature of the vent fluids. VISIONS '13, Leg 4. Photo credit: NSF-OOI/UW/CSSF
The Diva hydrothermal vent, is a 277°C small, fragile anhydrite (CaSO4) structure in the International District vent field on Axial Volcano. The chimney is of interest because it has the highest carbon dioxide concentrations of any of the chimneys within the Axial caldera. In 2014, it will host an instrument developed by Dr. Bill Seyfried, University of Minnesota,  that will provide real-time streaming data on acidity, hydrogen sulfide, hydrogen and temperature of the vent fluids. VISIONS '13, Leg 4. Photo credit: NSF-OOI/UW/CSSF
A short-period seismometer (OBSSPA301) is installed ~1.3 km east of the ASHES hydrothermal field. A cable connects to a medium power junction box in the field. During testing with ROPOS, this seismometer recorded a small earthquake. Credit: UW/NSF-OOI/CSSF, ROPOS Dive R1640; V13.
A short-period seismometer (OBSSPA301) is installed ~1.3 km east of the ASHES hydrothermal field. A cable connects to a medium power junction box in the field. During testing with ROPOS, this seismometer recorded a small earthquake. Credit: UW/NSF-OOI/CSSF, ROPOS Dive R1640; V13.
Inside the ROV ROPOS control room, the science and engineering team watches in amazement at the life that thrives around the hydrothermal vents. Here, microbial experiements are being recovered from the structure Mushroom using the 7 manipulator function arm of ROPOS. The experiments will be used by Harvard graduate student H. Olins to study the metabolisms of microbes in these extreme environments. Photo Credit: Caitlin Russell, Boston University.
Inside the ROV ROPOS control room, the science and engineering team watches in amazement at the life that thrives around the hydrothermal vents. Here, microbial experiements are being recovered from the structure Mushroom using the 7 manipulator function arm of ROPOS. The experiments will be used by Harvard graduate student H. Olins to study the metabolisms of microbes in these extreme environments. Photo Credit: Caitlin Russell, Boston University.
The ~ 4 m tall chimney called Inferno in the ASHES hydrothermal field sprouts a very young (< 2 year old) fragile beehive. The beehive structure is composed of very fine-grained sulfide minerals and anhydrite. Lush assemblages of tube worms, palm worms and limpets grow on the outer walls of the edifice. VISIONS '13, LEG 4. Photo credit: NSF-OOI/UW/CSSF
The ~ 4 m tall chimney called Inferno in the ASHES hydrothermal field sprouts a very young (< 2 year old) fragile beehive. The beehive structure is composed of very fine-grained sulfide minerals and anhydrite. Lush assemblages of tube worms, palm worms and limpets grow on the outer walls of the edifice. VISIONS '13, LEG 4. Photo credit: NSF-OOI/UW/CSSF
The summit of Axial Volcano will host myriad geophysical, chemical and biological instruments connected in real-time to the Internet via an array of junction boxes and extension cables. During the VISIONS'13 Expedition, three subnets were completed at this site (highlighted in blue). They include: 1) a medium-powered J-box MJ03B in the ASHES hydrothermal field, which is connected to two short-period seismometers; 2) an HD camera also in the ASHES hydrothermal field; and 3) a medium powered J-box MJ03E connected to two short-period seismometers. Over 20 km of extension cables, with lengths up to ~ 5 km, were successfully installed in 2013 using the ROV ROPOS. All extension cables and subnets were fully tested and are functional, awaiting to be connected to Primary Node PN3B. The remaining infrastructure will be deployed in during VISIONS'14, next year.
The summit of Axial Volcano will host myriad geophysical, chemical and biological instruments connected in real-time to the Internet via an array of junction boxes and extension cables. During the VISIONS'13 Expedition, three subnets were completed at this site (highlighted in blue). They include: 1) a medium-powered J-box MJ03B in the ASHES hydrothermal field, which is connected to two short-period seismometers; 2) an HD camera also in the ASHES hydrothermal field; and 3) a medium powered J-box MJ03E connected to two short-period seismometers. Over 20 km of extension cables, with lengths up to ~ 5 km, were successfully installed in 2013 using the ROV ROPOS. All extension cables and subnets were fully tested and are functional, awaiting to be connected to Primary Node PN3B. The remaining infrastructure will be deployed in during VISIONS'14, next year.
A cable termination assembly (CTA) is removed from the cable drum that was just released from the Remotely Operated Cable Laying System (ROCLS) during the ROV ROPOS dive 1599. The CTA, held in ROPOS's manipulator, provides a termination/connection between wetmate connectors and extension cables. An RSN wetmate hybrid connector (RS03W3-PA) is shown in the background, still attached to an extension cable that is figure 8'ed on the front horns of the cable drum. Photo credit: NSF-OOI/UW/CSSF.
A cable termination assembly (CTA) is removed from the cable drum that was just released from the Remotely Operated Cable Laying System (ROCLS) during the ROV ROPOS dive 1599. The CTA, held in ROPOS's manipulator, provides a termination/connection between wetmate connectors and extension cables. An RSN wetmate hybrid connector (RS03W3-PA) is shown in the background, still attached to an extension cable that is figure 8'ed on the front horns of the cable drum. Photo credit: NSF-OOI/UW/CSSF.
With ROPOS's heavy lift capabilities and industry style latch system on its underbelly, it is able to safely take heavy loads to the seafloor. During the VISIONS'13 Expedition, ROPOS takes two short-period seismometers to the seafloor in the tool basket at the start of Dive 1617 to the caldera of Axial Seamount.
With ROPOS's heavy lift capabilities and industry style latch system on its underbelly, it is able to safely take heavy loads to the seafloor. During the VISIONS'13 Expedition, ROPOS takes two short-period seismometers to the seafloor in the tool basket at the start of Dive 1617 to the caldera of Axial Seamount.
Before and after images of the fantail of the R/V Thompson during the VISIONS'13 expedition - at the end of the cruises there was nothing else left to deploy.
Before and after images of the fantail of the R/V Thompson during the VISIONS'13 expedition - at the end of the cruises there was nothing else left to deploy.
This medium powered junction-box (MJ03B) in the ASHES hydrothermal field was installed during the VISIONS'13 expedition. The titanium cylinder inside the frame hosts the power converters, data ports, and communication capabilities to shore via the Primary Nodes. A 4.3 km cable extends from this J-Box across the caldera to PN3B, where it awaits future connection. MJ03B was installed as a 'subnet' during VISIONS'13 - two short-period seismometers are now connected to it via a 50 m and 1.2 km extension cable, respectively. A also host a cabled 3D thermistor array (a test instrument is shown in this image - triangular shaped frame with blue cables) was also deployed for testing. MJ03B, and all cables and connected sensors were fully tested during VISIONS'13, and are fully functional. During the several hour test period, several earthquakes were detected. 
This medium powered junction-box (MJ03B) in the ASHES hydrothermal field was installed during the VISIONS'13 expedition. The titanium cylinder inside the frame hosts the power converters, data ports, and communication capabilities to shore via the Primary Nodes. A 4.3 km cable extends from this J-Box across the caldera to PN3B, where it awaits future connection. MJ03B was installed as a 'subnet' during VISIONS'13 - two short-period seismometers are now connected to it via a 50 m and 1.2 km extension cable, respectively. A also host a cabled 3D thermistor array (a test instrument is shown in this image - triangular shaped frame with blue cables) was also deployed for testing. MJ03B, and all cables and connected sensors were fully tested during VISIONS'13, and are fully functional. During the several hour test period, several earthquakes were detected. 
An ODI hybrid wet-mate connector provides > 1 Gbs video transmission capabilities and power to the RSN-OOI-NSF high definition camera that was deployed during the VISIONS'13 Expedition. The wetmate connectors allow an ROV to connect and disconnect infrastructure underwater without having to recover the equipment. The camera shown here is at a water depth of ~ 5000 ft at the summit of Axial Seamount. The orange extension cable (on right of camera) was powered up by the ROV ROPOS through an ~ 4 km extension cable that traverses eastward across the caldera at Axial Seamount. Live video video from the HD camera was streamed over the Internet for several hours during testing of the camera. In 2014, the extension cable will be connected to Primary Node 3B for 365 day access. The camera was installed at the base of the hydrothermal chimney called Mushroom in the ASHES hydrothermal field. Photo credit: NSF-OOI/UW/CSSF.  
An ODI hybrid wet-mate connector provides > 1 Gbs video transmission capabilities and power to the RSN-OOI-NSF high definition camera that was deployed during the VISIONS'13 Expedition. The wetmate connectors allow an ROV to connect and disconnect infrastructure underwater without having to recover the equipment. The camera shown here is at a water depth of ~ 5000 ft at the summit of Axial Seamount. The orange extension cable (on right of camera) was powered up by the ROV ROPOS through an ~ 4 km extension cable that traverses eastward across the caldera at Axial Seamount. Live video video from the HD camera was streamed over the Internet for several hours during testing of the camera. In 2014, the extension cable will be connected to Primary Node 3B for 365 day access. The camera was installed at the base of the hydrothermal chimney called Mushroom in the ASHES hydrothermal field. Photo credit: NSF-OOI/UW/CSSF.  
During ROPOS Dive 1611, the ROV latched into the remotely operated cable laying system (ROCLS) hosting a drum with an RSN extension cable ready to be installed. In concert, these two systems successfully installed >22,000 m of extension cables on the seafloor during the UW-OOI-NSF VISIONS'13 expedition.
During ROPOS Dive 1611, the ROV latched into the remotely operated cable laying system (ROCLS) hosting a drum with an RSN extension cable ready to be installed. In concert, these two systems successfully installed >22,000 m of extension cables on the seafloor during the UW-OOI-NSF VISIONS'13 expedition.
A dolphin streams ahead of the R/V Thompson as the ship transits home from 47 days at sea. Credit: Cody Turner, University of Washington, V13.
A dolphin streams ahead of the R/V Thompson as the ship transits home from 47 days at sea. Credit: Cody Turner, University of Washington, V13.
During VISIONS'13 ROPOS Dive R1636, the battery-powered version of the thermistor array was deployed at a small diffuse flow site at the base of the hydrothermal chimney called Mushroom. The thermistor array will provide a 3-dimensional view of the temperature structure at this site, which will help inform the community about the environmental conditions under which the biological assemblages thrive and evolve. Credit: UW/OOI-NSF/CSSF; ROPOS Dive R1636, V13.
During VISIONS'13 ROPOS Dive R1636, the battery-powered version of the thermistor array was deployed at a small diffuse flow site at the base of the hydrothermal chimney called Mushroom. The thermistor array will provide a 3-dimensional view of the temperature structure at this site, which will help inform the community about the environmental conditions under which the biological assemblages thrive and evolve. Credit: UW/OOI-NSF/CSSF; ROPOS Dive R1636, V13.
The students on Leg 4 gather on the bow of the R/V Thompson. From left to right - Charlie Parker,  Andrew Baird, Vega Shaw, Cody Turner, Caitlin Russell, Teos Bisbee, Brendan Philip, and Colin Katagiri....oh,and to the far right is 'Mr. Chicken,' a fine member of the science party who was the only one to dive to 5000 ft beneath the oceans surface. During the VISIONS'13 program, 20 undergraduate and graduate students participatied in the sea-going experience onboard the R/V Thompson using the Canadian ROV ROPOS.
The students on Leg 4 gather on the bow of the R/V Thompson. From left to right - Charlie Parker,  Andrew Baird, Vega Shaw, Cody Turner, Caitlin Russell, Teos Bisbee, Brendan Philip, and Colin Katagiri....oh,and to the far right is 'Mr. Chicken,' a fine member of the science party who was the only one to dive to 5000 ft beneath the oceans surface. During the VISIONS'13 program, 20 undergraduate and graduate students participatied in the sea-going experience onboard the R/V Thompson using the Canadian ROV ROPOS.
ROPOS Control Room VISIONS '13, Leg 3 Photo by Ryan Cox
ROPOS Control Room VISIONS '13, Leg 3 Photo by Ryan Cox
During VISIONS'13 two types of flow meters (CAT and Mosquito) were deployed at the summit of Southern Hydrate Ridge near the Einstein's Grotto active seep site - each instrument has specific ranges of flow that they measure. They will be recovered in 2014, providing year-long records of flow into and out of the sediment. Credit: UW/OOI-NSF//CSSF; V13
During VISIONS'13 two types of flow meters (CAT and Mosquito) were deployed at the summit of Southern Hydrate Ridge near the Einstein's Grotto active seep site - each instrument has specific ranges of flow that they measure. They will be recovered in 2014, providing year-long records of flow into and out of the sediment. Credit: UW/OOI-NSF//CSSF; V13