This movie highlights some of the remarkable animals that thrive deep beneath the oceans surface in the absence of sunlight and in waters that are at near freezing temperatures. The move was produced by Boston University undergraduate student, Caitlin Russell as part of the University of Washington's School of Oceanography student at-sea program. This effort was part of the VISIONS'13 program to install the US's first underwater cabled observatory.
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', sources: [ {'file': 'https://stream.ocean.washington.edu:443/rsn/mp4:r1615highlights-broadband.m4v/playlist.m3u8'}, {'file': 'https://stream.ocean.washington.edu:443/rsnPhone/mp4:R1615Highlights-Wi-Fi.m4v/playlist.m3u8'}, {'file': 'rtmp://stream.ocean.washington.edu/rsn/mp4:r1615highlights-broadband.m4v'} ]} , {'height':'540', 'width':'960', 'image':'/files/screenshot2013-07-27am_med.jpg', 'title':'Dive 1614 First View of ASHES ', 'description':'Dive 1614 was a short trip down and back to survey locations for instruments & junction boxes near, and in, the ASHES hydrothermal field. The imagery starts with close-ups of microbial experiments deployed in 2011 in a beautiful diffusely venting area at the base of 4-m-tall ‘Mushroom’ chimney, which is marked by highly friable ‘chimlets’ that emit particle-poor high-temperature fluids. This area is a target for a high-definition camera that will provide real-time imaging of this animal-covered edifice. ROPOS also visited > 1 m-tall, new black smoker spires at the summit of Inferno. In 2011, Inferno's top was sampled for microbial analyses, so this new growth is only ~ 2 years old. ROPOS then visited the base of Mushroom again, and the dive ended with placement of Markers 8 and 10, which will be used as target sites for placement of secondary infrastructure on Leg 4 of VISIONS'13. Video credit: OOI-NSF/UW/CSSF
', sources: [ {'file': 'https://stream.ocean.washington.edu:443/rsn/mp4:r1614highlights-broadband.m4v/playlist.m3u8'}, {'file': 'https://stream.ocean.washington.edu:443/rsnPhone/mp4:R1614Highlights-Wi-Fi.m4v/playlist.m3u8'}, {'file': 'rtmp://stream.ocean.washington.edu/rsn/mp4:r1614highlights-broadband.m4v'} ]} , {'height':'540', 'width':'960', 'image':'/files/screenshot2013-07-27at7.41.25am_med.jpg', 'title':'Dive 1613 Cable Lay Eastern Caldera ', 'description':'This dive installed a 4140 ft electrical extension cable (ECALW7) deployed at Eastern Caldera secondary node site and running north to its termination point that will include a short-period seismometer. The medium power junction box (MJ03E) was deployed at this site on a previous dive. After setting ROCLS on the seafloor, ROPOS plugged the extension cable into the J-Box, hooked up a strain line (kellum grip) running from the cable to the J-Box, unfurled the figure-8 cable on the ROCLS horns, and then began laying cable. The run ended in a small sediment pond, perfect for follow-on deployment of the short-period seismometer. ROPOS pulled the two pins to release the flange box protecting the wet mate connector at the end of the cable, and then surveyed the cable. During the survey, the vehicle transited over a few small collapse zones. At the end of the dive, ROPOS went back and relatched into ROCLS for recovery.
Video credit: OOI-NSF/UW/CSSF
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Video credit: OOI-NSF/UW/CSSF
', sources: [ {'file': 'https://stream.ocean.washington.edu:443/rsn/mp4:R1611Highlights-Broadband.m4v/playlist.m3u8'}, {'file': 'https://stream.ocean.washington.edu:443/rsnPhone/mp4:R1611Highlights-Wi-Fi.m4v/playlist.m3u8'}, {'file': 'rtmp://stream.ocean.washington.edu/rsn/mp4:R1611Highlights-Broadband.m4v'} ]} , {'height':'540', 'width':'960', 'image':'/files/screenshot2013-07-27at7.44.57am_med.jpg', 'title':'Dive 1610 Eastern Caldera Dive Ended', 'description':'The goal of dive 1610 was to deploy 1262 m of electrical extension cable (ECALW7) from the medium power J-Box, MJ03E, to an area north of the J-Box. On a follow-on dive, a short-period seismometer will be deployed at the end of this cable as part of a network to detect earthquakes in real-time in the volcano. ROPOS descended to the seafloor near this site and unlatched the remotely operated cable laying system (ROCLS) from the vehicle's underbelly. ROPOS examined the cable in preparation for removing the section of cable on the front 'horns' of ROCLS, which hold cable splayed in a figure-8 fashion, and the wet-mate connector. Upon inspection of an oil-filled hose that is part of the cable termination, it was found that this section lacked oil. The dive was ended, ROPOS relatched into ROCLS and brought the system to the surface. This section of hose was filled on deck, and the cable was deployed successfully on a follow-on dive. Video credit: OOI-NSF/UW/CSSF
', sources: [ {'file': 'https://stream.ocean.washington.edu:443/rsn/mp4:R1610Highlights-Broadband.m4v/playlist.m3u8'}, {'file': 'https://stream.ocean.washington.edu:443/rsnPhone/mp4:R1610Highlights-Wi-Fim4v/playlist.m3u8'}, {'file': 'rtmp://stream.ocean.washington.edu/rsn/mp4:R1610Highlights-Broadband.m4v'} ]} , {'height':'540', 'width':'960', 'image':'/files/screenshot2013-07-27at7.46.12am_med.jpg', 'title':'Dive 1609 JBox at Eastern Caldera', 'description':'The medium-power J-Box (MJ03E) was deployed during this dive at the Eastern Caldera site, which is located ~ 600 m southeast of the Primary Node 3B. The J-Box was landed in an area of low- to moderate-relief lobate flows with a few pillows. During the dive, ROPOS connected a ~ 600 m electro-optical cable running from near PN3B to the J-Box in port 1, which had been laid on a previous dive. ROPOS cleaned up the area a bit by storing the flange box under MJ03E. ROPOS then imaged the surrounding seafloor, including a small collapse zone. There is a fair amount of marine snow in this area, as seen when ROPOS starts its return to the surface. This material rains down from the shallow surface waters, with some contribution from hydrothermal plume material in the caldera. Video credit: OOI-NSF/UW/CSSF
', sources: [ {'file': 'https://stream.ocean.washington.edu:443/rsn/mp4:r1609highlights-broadband.m4v/playlist.m3u8'}, {'file': 'https://stream.ocean.washington.edu:443/rsnPhone/mp4:R1609Highlights-Wi-Fi.m4v/playlist.m3u8'}, {'file': 'rtmp://stream.ocean.washington.edu/rsn/mp4:r1609highlights-broadband.m4v'} ]} , {'height':'540', 'width':'960', 'image':'/files/screenshot2013-07-27at7.47.14am_med.jpg', 'title':'Dive R1608 Highlights', 'description':'R1608 Highlights
Video credit: OOI-NSF/UW/CSSF
', sources: [ {'file': 'https://stream.ocean.washington.edu:443/rsn/mp4:R1608Highlights-Broadband.m4v/playlist.m3u8'}, {'file': 'https://stream.ocean.washington.edu:443/rsnPhone/mp4:R1608Highlights-Wi-Fi.m4v/playlist.m3u8'}, {'file': 'rtmp://stream.ocean.washington.edu/rsn/mp4:R1608Highlights-Broadband.m4v'} ]} , {'height':'540', 'width':'960', 'image':'/files/r1606highlightscut2_med.jpg', 'title':'Dive 1606 Southern Hydrate Ridge and Pinnacle', 'description':'Dive 1606 focused on the recovery of a flow meter (called a Mosquito designed by Evan Solomon at the UW), deployed during the VISION'11 expedition. The flow meter is used to calculate the flow of seawater into the sediments, and flow of methane-rich fluids out of the seeps. Sediment samples were also taken with a push core. ROPOS transited to a ~ 60 foot tall carbonate pinnacle a few hundred meters west of the seeps. It is a place of remarkable beauty, hosting 100’s of soft corals that inhabit the hard substrate. Small nooks and crannies in the carbonate provide homes to shrimp and hiding places for crabs, squat lobsters and velvety, blue hag fish. ROPOS found a very large transient bubble plume at the seeps - the bubbles could be followed for > 600 ft into the water column and are of interest because of their potential to transfer methane into the atmosphere, should the bubbles reach the surface.
', sources: [ {'file': 'https://stream.ocean.washington.edu:443/rsn/mp4:R1606HighlightsCut2-Broadband.m4v/playlist.m3u8'}, {'file': 'https://stream.ocean.washington.edu:443/rsnPhone/mp4:R1606HighlightsCut2-Wi-Fi.m4v/playlist.m3u8'}, {'file': 'rtmp://stream.ocean.washington.edu/rsn/mp4:R1606HighlightsCut2-Broadband.m4v'} ]} , {'height':'540', 'width':'960', 'image':'/files/r1605highlights_med.jpg', 'title':'Dive 1605 Instrument Deployment Southern Hydrate ', 'description':'This ROPOS dive focusedd on deploying a CAT flow meter, and two 'Mosquito' flow meters at Southern Hydrate Ridge new Einstein's Grotto. The seeps host red rock fish, abundant clams, and white bacterial mats. The hummocky, sedimented areas are marked by broad expanses of clam shell chaff. At the end of the dive, Niskin bottles on ROPOS were triggered to take samples of the methane-rich fluids. These will be analyzed onshore.
', sources: [ {'file': 'https://stream.ocean.washington.edu:443/rsn/mp4:R1605Highlights-Broadband.m4v/playlist.m3u8'}, {'file': 'https://stream.ocean.washington.edu:443/rsnPhone/mp4:R1605Highlights-Wi-Fi.m4v/playlist.m3u8'}, {'file': 'rtmp://stream.ocean.washington.edu/rsn/mp4:R1605Highlights-Broadband.m4v'} ]} , {'height':'540', 'width':'960', 'image':'/files/r1604_thumb_med.jpg', 'title':'Dive R1604', 'description':'Dive 1604 with ROPOS focused on installing over 15,000 feet of cable across the summit of Axial Volcano. With this much cable, the drum weighed over 6,000 lbs, making it too heavy to be latched into the underbelly of ROPOS. Instead the cable drum was lowered over the starboard side of the ship using one of the ship’s wires and winches. ROPOS was also launched and about 600 feet below the ship it imaged the drum with its forward-looking sonar. Carefully, the ROPOS pilot and navigator drove the vehicle toward the drum until they were close enough to image the drum directly with the ROV's high-definition camera. ROPOS and the drum then descended to the seafloor, 5,000 feet below the ocean's surface. The cable drum was gently placed on the seafloor with the winch as ROPOS ensured there was a safe landing zone. ROPOS then attached cable to the junction box, and began laying cable on the seafloor.
', sources: [ {'file': 'https://stream.ocean.washington.edu:443/rsn/mp4:R1604HighlightsEds-Broadband.m4v/playlist.m3u8'}, {'file': 'https://stream.ocean.washington.edu:443/rsnPhone/mp4:R1604HighlightsEds-Wi-Fi.m4v/playlist.m3u8'}, {'file': 'rtmp://stream.ocean.washington.edu/rsn/mp4:R1604HighlightsEds-Broadband.m4v'} ]} , {'height':'540', 'width':'960', 'image':'/files/r1603_thumb_med.jpg', 'title':'Dive 1603 Installing Cable to Eastern Caldera ', 'description':'
Dive 1603 marked the first installation of an extension cable onto the seafloor at the summit of Axial Volcano. The 2083 feet of cable was installed from near Primary Node 3B to a southern site known as Eastern Caldera. This cable will be connected to a junction box that will provide power and communication to seismometers that will detect earthquakes in real-time and a bottom pressure-tilt instrument that will measure the inflation and deflation of the volcano's floor. ROPOS surveyed the cable route, transiting over lobate flows, bulbous pillow flows, and a few skylights. The cable was then installed and ROPOS set the cable laying system ROCLS (Remotely Operated Cable Laying System) onto the seafloor near marker W. ROPOS then removed the flange box from ROCLS so that the wet-mate connector would be available for follow-on connection to the J-Box later in the cruise. A few rat tail fish were observed along the way.
', sources: [ {'file': 'https://stream.ocean.washington.edu:443/rsn/mp4:R1603Highlights-Broadband.m4v/playlist.m3u8'}, {'file': 'https://stream.ocean.washington.edu:443/rsnPhone/mp4:R1603Highlights-Wi-Fi.m4v/playlist.m3u8'}, {'file': 'rtmp://stream.ocean.washington.edu/rsn/mp4:R1603Highlights-Broadband.m4v'} ]} , {'height':'540', 'width':'960', 'image':'/files/r1602_thumb_med.jpg', 'title':'Dive R1602', 'description':'Dive R1602
', sources: [ {'file': 'https://stream.ocean.washington.edu:443/rsn/mp4:r1602highlights.m4v/playlist.m3u8'}, {'file': 'https://stream.ocean.washington.edu:443/rsnPhone/mp4:R1602Highlights-Wi-Fi.m4v/playlist.m3u8'}, {'file': 'rtmp://stream.ocean.washington.edu/rsn/mp4:r1602highlights.m4v'} ]} , {'height':'540', 'width':'960', 'image':'/files/r1601_thumb_med.jpg', 'title':'Dive R1601', 'description':'Dive R1601
', sources: [ {'file': 'https://stream.ocean.washington.edu:443/rsn/mp4:R1601Highlights-Broadband.m4v/playlist.m3u8'}, {'file': 'https://stream.ocean.washington.edu:443/rsnPhone/mp4:R1601Highlights-Wi-Fi.m4v/playlist.m3u8'}, {'file': 'rtmp://stream.ocean.washington.edu/rsn/mp4:R1601Highlights-Broadband.m4v'} ]} , {'height':'540', 'width':'960', 'image':'/files/r1600_thumb_med.jpg', 'title':'Dive R1600', 'description':'Dive R1600
', sources: [ {'file': 'https://stream.ocean.washington.edu:443/rsn/mp4:R1600Highlights-Broadband.m4v/playlist.m3u8'}, {'file': 'https://stream.ocean.washington.edu:443/rsnPhone/mp4:R1600Highlights-Wi-Fi.m4v/playlist.m3u8'}, {'file': 'rtmp://stream.ocean.washington.edu/rsn/mp4:R1600Highlights-Broadband.m4v'} ]} , {'height':'394', 'width':'700', 'image':'/files/r1596_med.jpg', 'title':'Dive Highlights R1596', 'description':'During the beginning of ROPOS dive 1596 at the summit of Axial Seamount, we drove south towards the hydrothermal field 'International District'. East of the field, we first encountered lobate flows and a few collapse basins, but closer to the field the lava flows transitioned into rough, jumbled hackley flows. As ROPOS entered the field, we encountered a small, partially extinct chimney with weak diffuse venting at its top, which hosted small tube worms. ROPOS transited to the largest black smoker chimney 'El Guapo', which rises > 50 feet above the surrounding seafloor. We started at the base of the massive edifice and slowly transited to the top of the structure, which hosts numerous small orifices venting jets of hot hydrothermal fluid. In 2011, the fluids were boiling at 349°C, and at a water depth of 5000 m. Dive Highlights R-1596 (Credit: NSF-OOI/UW/CSSF)
', sources: [ {'file': 'https://stream.ocean.washington.edu:443/rsn/mp4:r1596-broadband.m4v/playlist.m3u8'}, {'file': 'https://stream.ocean.washington.edu:443/rsnPhone/mp4:R1596-Wi-Fi.m4v/playlist.m3u8'}, {'file': 'rtmp://stream.ocean.washington.edu/rsn/mp4:r1596-broadband.m4v'} ]} , {'height':'540', 'width':'960', 'image':'/files/Dive_Highlight_1471_med.jpg', 'title':'Dive 1471 Highlights', 'description':'Sensorbot system instrument recovery
', sources: [ {'file': 'https://stream.ocean.washington.edu:443/rsn/mp4:Dive_Highlight_1471_Computer.m4v/playlist.m3u8'}, {'file': 'https://stream.ocean.washington.edu:443/rsnPhone/mp4:Dive_Highlight_1471_iPhone.m4v/playlist.m3u8'}, {'file': 'rtmp://stream.ocean.washington.edu/rsn/mp4:Dive_Highlight_1471_Computer.m4v'} ]} , {'height':'540', 'width':'960', 'image':'/files/Dive_Highlight_1470_med.jpg', 'title':'Dive 1470 Highlights', 'description':'Site survey, sample collection, and instrument recovery
', sources: [ {'file': 'https://stream.ocean.washington.edu:443/rsn/mp4:Dive_Highlight_1470_Computer.m4v/playlist.m3u8'}, {'file': 'https://stream.ocean.washington.edu:443/rsnPhone/mp4:Dive_Highlight_1470_iPhone.m4v/playlist.m3u8'}, {'file': 'rtmp://stream.ocean.washington.edu/rsn/mp4:Dive_Highlight_1470_Computer.m4v'} ]} , {'height':'540', 'width':'960', 'image':'/files/Dive_Highlight_1469_med.jpg', 'title':'Dive 1469 Highlights', 'description':'Sensorbot System Deployment, Hydrothermal Vent Imaging, and Current Sensor Recovery
', sources: [ {'file': 'https://stream.ocean.washington.edu:443/rsn/mp4:Dive_Highlight_1469_Computer.m4v/playlist.m3u8'}, {'file': 'https://stream.ocean.washington.edu:443/rsnPhone/mp4:Dive_Highlight_1469_iPhone.m4v/playlist.m3u8'}, {'file': 'rtmp://stream.ocean.washington.edu/rsn/mp4:Dive_Highlight_1469_Computer.m4v'} ]} , {'height':'540', 'width':'960', 'image':'/files/Dive_Highlight_1468_med.jpg', 'title':'Dive 1468 Highlights', 'description':'Hydrothermal vent imaging, sample collection, and current meter deployment
', sources: [ {'file': 'https://stream.ocean.washington.edu:443/rsn/mp4:Dive_Highlight_1468_Computer.m4v/playlist.m3u8'}, {'file': 'https://stream.ocean.washington.edu:443/rsnPhone/mp4:Dive_Highlight_1468_iPhone.m4v/playlist.m3u8'}, {'file': 'rtmp://stream.ocean.washington.edu/rsn/mp4:Dive_Highlight_1468_Computer.m4v'} ]} , {'height':'540', 'width':'960', 'image':'/files/Dive_Highlight_1467_med.jpg', 'title':'Dive 1467 Highlights', 'description':'Exploring recent eruption changes to Axial Seamount
', sources: [ {'file': 'https://stream.ocean.washington.edu:443/rsn/mp4:Dive_Highlight_1467_Computer.m4v/playlist.m3u8'}, {'file': 'https://stream.ocean.washington.edu:443/rsnPhone/mp4:Dive_Highlight_1467_iPhone.m4v/playlist.m3u8'}, {'file': 'rtmp://stream.ocean.washington.edu/rsn/mp4:Dive_Highlight_1467_Computer.m4v'} ]} , {'height':'540', 'width':'960', 'image':'/files/Dive_Highlight_1466_med.jpg', 'title':'Dive 1466 Highlights', 'description':'Cable inspection done on August 22, 2011
', sources: [ {'file': 'https://stream.ocean.washington.edu:443/rsn/mp4:Dive_Highlight_1466_Computer.m4v/playlist.m3u8'}, {'file': 'https://stream.ocean.washington.edu:443/rsnPhone/mp4:Dive_Highlight_1466_iPhone.m4v/playlist.m3u8'}, {'file': 'rtmp://stream.ocean.washington.edu/rsn/mp4:Dive_Highlight_1466_Computer.m4v'} ]} , {'height':'540', 'width':'960', 'image':'/files/Dive_Highlight_1465_med.jpg', 'title':'Dive 1465 Highlights', 'description':'Cable inspection done on August 21, 2011
', sources: [ {'file': 'https://stream.ocean.washington.edu:443/rsn/mp4:Dive_Highlight_1465_Computer.m4v/playlist.m3u8'}, {'file': 'https://stream.ocean.washington.edu:443/rsnPhone/mp4:Dive_Highlight_1465_iPhone.m4v/playlist.m3u8'}, {'file': 'rtmp://stream.ocean.washington.edu/rsn/mp4:Dive_Highlight_1465_Computer.m4v'} ]} , {'height':'540', 'width':'960', 'image':'/files/Dive_Highlight_1464_med.jpg', 'title':'Dive 1464 Highlights', 'description':'Instrument recovery using ROPOS
', sources: [ {'file': 'https://stream.ocean.washington.edu:443/rsn/mp4:Dive_Highlight_1464_Computer.m4v/playlist.m3u8'}, {'file': 'https://stream.ocean.washington.edu:443/rsnPhone/mp4:Dive_Highlight_1464_iPhone.m4v/playlist.m3u8'}, {'file': 'rtmp://stream.ocean.washington.edu/rsn/mp4:Dive_Highlight_1464_Computer.m4v'} ]} , {'height':'540', 'width':'960', 'image':'/files/Dive_Highlight_1463_med.jpg', 'title':'Dive 1463 Highlights', 'description':'Hydrate Ridge photo mosaic
', sources: [ {'file': 'https://stream.ocean.washington.edu:443/rsn/mp4:Dive_Highlight_1463_Computer.m4v/playlist.m3u8'}, {'file': 'https://stream.ocean.washington.edu:443/rsnPhone/mp4:Dive_Highlight_1463_iPhone.m4v/playlist.m3u8'}, {'file': 'rtmp://stream.ocean.washington.edu/rsn/mp4:Dive_Highlight_1463_Computer.m4v'} ]} , {'height':'540', 'width':'960', 'image':'/files/Dive_Highlight_1462_med.jpg', 'title':'Dive 1462 Highlights', 'description':'Dive 1462 Highlights
', sources: [ {'file': 'https://stream.ocean.washington.edu:443/rsn/mp4:Dive_Highlight_1462_Computer.m4v/playlist.m3u8'}, {'file': 'https://stream.ocean.washington.edu:443/rsnPhone/mp4:Dive_Highlight_1462_iPhone.m4v/playlist.m3u8'}, {'file': 'rtmp://stream.ocean.washington.edu/rsn/mp4:Dive_Highlight_1462_Computer.m4v'} ]} , {'height':'540', 'width':'960', 'image':'/files/Dive_Highlight_Life_med.jpg', 'title':'ROPOS Dive Highlights Leg 1 Biology', 'description':'ROPOS dive highlights of biology at Southern Hydrate Ridge (VISIONS'11 Leg 1).
', sources: [ {'file': 'https://stream.ocean.washington.edu:443/rsn/mp4:Dive_Highlight_Life_Computer.m4v/playlist.m3u8'}, {'file': 'https://stream.ocean.washington.edu:443/rsnPhone/mp4:Dive_Highlight_Life_iPhone.m4v/playlist.m3u8'}, {'file': 'rtmp://stream.ocean.washington.edu/rsn/mp4:Dive_Highlight_Life_Computer.m4v'} ]} , {'height':'540', 'width':'960', 'image':'/files/Dive_Highlight_1461_med.jpg', 'title':'ROPOS Dive 1461 Highlights Core Samples', 'description':'ROPOS dive 1461 involved taking push core samples from an active methane hydrate seep at Southern Hydrate Ridge. A secondary node test frame that was deployed in 2010 and left at this site for a year to test the material properties of the frame was also recovered.
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