What's New Archive
The 2017 expedition to Axial Seamount was on R/V Revelle, July 13-23, with ROV Jason and AUV Sentry on board. On this expedition we made measurements to monitor the continued re-inflation of the volcano since its last eruption in 2015 so we can better understand how magma is supplied and stored within the volcano, how it fuels hydrothermal vents and their biological communities, and how we can refine forecasts of future eruptions. We also sampled hydrothermal vents to continue a time-series aimed and understanding the interactions between volcanic events and the hydrothermal and biological systems. A cruise report is in preparation and will be posted here when it is finished.
The expedition website with daily logs from July 12-23 aboard the R/V Revelle with ROV Jason and AUV Sentry is available at:
E/V Nautilus expedition NA080 leg 2 begins the evening of May 22 and continues through June 5 mapping the seafloor and water column in search of methane bubble emission sites. This part of the Ocean Exploration Trust (OET) expedition is a continuation of work that was done last summer for PMEL Earth Ocean Interactions (EOI) Program on the Cascadia Margin, offshore Washington, Oregon, and Northern California. 2016 expeditions NA072 and NA078 resulted in the discovery of 905 individual methane bubble streams that were clustered into 317 emission sites. The vast majority of those sites were previously unknown. The purpose of this exploration is to establish a baseline of methane bubble emission sites and methane-derived habitat (carbonate hardground) for the Cascadia margin. A warming ocean could disassociate some of the solid methane hydrate now locked up in the sediments along continental margins at >~ 500 m depth. Methane is a potent greenhouse gas so there is interest in understanding what happens to the methane as it rises through the water column. Does it make it into the atmosphere? Does it contribute to ocean acidification? There is also interest in the extent of the seep habitat and associated hardgrounds from the perspective of essential fisheries habitat. Those are just a few of the questions EOI scientists are hoping to answer with this research. You can follow the expedition here:
EOI and collaborators are the first scientists using the new Schmidt Ocean Institute’s ROV SuBastian aboard the R/V Falkor as they return to the Mariana back-arc spreading system on an expedition from November 29 to December 20. This year's cruise follows up on discoveries made last year aboard R/V Falkor of new hydrothermal vent sites and lava flows in the Mariana back-arc. EOI also co-directed several NOAA Ship Okeanos ROV Deep Discoverer dives this past summer yielding some additional observations in this relatively unexplored region. ROV SuBastian will provide in-depth exploration and sampling of these systems to characterize their geologic setting, chemical environment, and biological communities. This expedition is supported by Schmidt Ocean Institute, NOAA's Ocean Exploration and Research Program, and the NOAA Pacific Islands Regional Office. (Image courtesy of Schmidt Ocean Institute)
EOI scientists participated in several ROV dives remotely via "telepresence" during the 2016 Deepwater Exploration of the Marianas expedition by the NOAA ship Okeanos Explorer. During Leg 1 of the expedition, EOI co-led three dives in the Mariana backarc, exploring the site of a recent eruption and two newly discovered hydrothermal vent fields. All of these discovered during a recent cruise on R/V Falkor in Nov-Dec 2015, and set the stage for further exploration during a follow-on R/V Falkor cruise in December 2016. During Leg 3 of the Okeanos expedition, EOI co-led three dives in at three volcanically active seamounts, each with its own unique ecosystem. The expedition was supported by the NOAA Ocean Exploration and Research Program.
The Ocean Exploration Trust Inc. ship E/V Nautilus, with several NOAA-PMEL and Oregon State University CIMRS scientists aboard, is using the latest midwater sonar technology to map out methane seeps along the Cascadia continental margin this month. PMEL/CIMRS scientists report that, after locating extensive bubble plumes of methane in Astoria canyon at 850 m, the remotely operated vehicle Hercules visited the site and found an exposure of methane hydrate and gas bubbles streaming out of the seafloor. The hydrate, a mixed water/methane ice phase, is present over extensive areas of continental margins, but has only rarely been observed exposed at the seafloor along the Cascadia margin. Why the hydrate is exposed at this location in association with the methane gas seepage is a topic of discussion among the scientists aboard the Nautilus and those ashore participating remotely via the internet. The E/V Nautilus is a unique platform with extensive telepresence capability that enables scientist aboard to interact with those in the broader scientific community and the public ashore. Dives with the Hercules are broadcast live over the internet and can be viewed at http://www.nautiluslive.org
PMEL scientists from the Earth-Ocean Interactions Program will be on board the E/V Nautilus, which is operated by the Ocean Exploration Trust (OET), during June 1-20. This expedition will explore and characterize habitats and methane seeps along the Cascadia continental margin between northern Washington and Cape Mendocino. Broadband video of the seafloor during the dives from OET remotely operated vehicle Hercules will be broadcast in realtime over the internet. Scientists ashore representing a broad range of expertise will also participate via a realtime link to the ship during the dives.
Follow along live and learn more about the cruise on: http://www.nautiluslive.org
EOI Scientists aboard the Schmidt Ocean Institute’s RV Falkor explored the Mariana back-arc spreading center (November 20 - December 17) and discovered four new hydrothermal vent sites. Researchers from NOAA and its cooperative institutes at the University of Washington and Oregon State University searched for these new hydrothermally active sites to gain a better understanding of the physical, chemical and geological forces that shape the biodiversity in these unique ecosystems. Scientists will return for a second cruise in the Fall of 2016 with a remotely operated vehicle to further characterize and sample the new vent sites.
Learn more about the expedition at:
Hydrothermal Hunt at Mariana (Schmidt Ocean Institute)
UPDATE May 2016: EOI scientists remotely join expedition verifying new hydrothermal vents and lava flows with ROV expedition aboard NOAA Ship Okeanos Explorer. Read more here.
The Schmidt Ocean Institute provided the ship and support for this expedition. Additional support is provided by NOAA Office of Ocean Exploration and Research and NOAA Pacific Island Regional Office.
The 2015 expedition to Axial Seamount was August 15-29 aboard the R/V Thompson. The cruise successfully conducted operations with the underwater vehicles ROV Jason and AUV Sentry. The big excitement this year was exploring the April-May 2015 Axial Seamount eruption and conducting extensive exploration, mapping, and sampling of the new lava flows. Explore the results of the expedition with the Axial 2015 blog (axial2015.blogspot.com).
An eruption appears to have started at Axial Seamount on April 24. The eruption was forecast in September 2014 to occur by the end of 2015, based on seafloor pressure measurements. Axial Seamount is the most active submarine volcano in the NE Pacific and the site of the new OOI cabled observatory. More information on the eruption forecast is HERE, and live data from the seafloor is displayed HERE.