` China's Sub Breaches 'Forbidden Ground' 3 Miles Below Arctic Ice—First Footage From Hidden Ridge Surfaces - Ruckus Factory

China’s Sub Breaches ‘Forbidden Ground’ 3 Miles Below Arctic Ice—First Footage From Hidden Ridge Surfaces

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In 2025, China’s crewed deep-sea submersible Fendouzhe completed a historic series of dives beneath Arctic pack ice to the eastern Gakkel Ridge, reaching a maximum depth of 5,277 meters—more than three miles below the surface.

Supported by the research vessel Tan Suo San Hao, the expedition marked the first time a crewed submersible explored this section of the ridge. Scientists described the mission as closing one of the final gaps in global mid-ocean ridge exploration, transforming a long-inaccessible region into a directly observed environment.

The Gakkel Ridge — Earth’s Most Remote Mid-Ocean Ridge

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Wikimedia Commons – 37ophiuchi BrucePL


The Gakkel Ridge is a 1,800-kilometer-long underwater mountain chain running between Greenland and Siberia beneath permanent or near-permanent Arctic ice. It is the slowest-spreading mid-ocean ridge on Earth, making it geologically distinct and difficult to study.

While parts of the western ridge were explored remotely in earlier decades, the eastern Gakkel Ridge remained unreachable by crewed vehicles due to extreme depth, ice cover, and logistical constraints—until this mission.

Mission Scale — A Record Arctic Deep-Sea Campaign

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The Arctic expedition lasted roughly three months at sea and included 43 total dives, 32 of which were conducted beneath dense pack ice exceeding 80 percent surface coverage. Fendouzhe operated at depths few human-occupied vehicles have ever reached, repeatedly descending to more than 5,000 meters.

The mission ranks among the longest and most sustained crewed deep-sea operations ever conducted in polar conditions, validating China’s ability to maintain precision operations in one of Earth’s harshest environments.

Why “Forbidden Ground” Was More Than a Metaphor

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For decades, the eastern Gakkel Ridge was effectively unreachable. Permanent ice cover limited surface support, while extreme depth ruled out most conventional submersibles. Even autonomous vehicles faced navigation and communication challenges under ice.

Scientists referred to the region as “forbidden ground” not because of secrecy, but because physical conditions made direct human observation impractical. The 2025 dives removed that barrier, allowing scientists to see, sample, and document terrain previously known only through indirect measurements.

What the Submersible Collected

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During its dives, Fendouzhe collected sediment cores, rock samples, seawater, and biological specimens from the seafloor.

These materials are essential for understanding ridge geology, deep-ocean chemistry, and life adapted to extreme cold, pressure, and darkness. The samples are now undergoing laboratory analysis, with researchers emphasizing that full scientific interpretation will take years. Officials described the data as potentially reshaping existing maps and theories of Arctic seafloor formation.

Completing the Global Ridge Puzzle

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Mid-ocean ridges form a continuous volcanic system encircling the planet, yet the eastern Gakkel Ridge remained the last major segment unexplored by crewed submersibles.

Chinese scientists involved in the mission referred to this area as the “last piece of the puzzle” in understanding the global ridge network. By directly observing this section, researchers can now compare Arctic ridge processes with those in warmer oceans, improving models of plate tectonics and mantle dynamics.

Hydrothermal Possibilities Beneath the Ice

PIA19059 Trapping of Methane In Enceladus Ocean This illustration depicts potential origins of methane found in the plume of gas and ice particles that sprays from Saturn s moon Enceladus based on research by scientists working with the Ion and Neutral Mass Spectrometer on NASA s Cassini mission Scientists believe the plumes originate from an internal liquid-water ocean beneath the moon s south polar region Recent findings from Cassini suggest hydrothermal activity as one of two likely sources of methane in the plume of gas and ice particles that erupts from the south polar region of Enceladus The finding is the result of extensive modeling to address why methane as previously sampled by Cassini is curiously abundant in the plume Researchers with Cassini s Ion and Neutral Mass Spectrometer INMS determined that at the high pressures expected in the moon s ocean icy materials called clathrates could form that imprison methane molecules within a crystal structure of water ice Their models indicated that this process could be so efficient at depleting methane from Enceladus ocean that they still needed an explanation for the methane abundance in the plume In one scenario hydrothermal processes supersaturate the ocean with methane This could occur if methane is produced faster than it is converted into clathrates A second possibility is that methane clathrates from the ocean are dragged along into the erupting plumes and release their methane as they rise like bubbles forming in a popped bottle of champagne The authors agree that both scenarios are likely occurring to some degree but they note that the presence of nanosilica grains as documented by Cassini s Cosmic Dust Analyzer CDA instrument favors the hydrothermal scenario The Cassini-Huygens mission is a cooperative project of NASA the European Space Agency and the Italian Space Agency NASA s Jet Propulsion Laboratory a division of the California Institute of Technology in Pasadena manages the mission for NASA s Science Mission Directorate Washington The Cassini CDA instrument was provided by the German Aerospace Center the instrument team led by Ralf Srama is based at the University of Stuttgart in Germany The INMS team is based at Southwest Research Institute San Antonio Texas For more information about the Cassini-Huygens mission visit and
Photo by NASA JPL-Caltech SwRI on Wikimedia


A 2003 expedition identified hydrothermal vents on the western Gakkel Ridge, revealing life sustained by chemical energy rather than sunlight.

Scientists believe similar systems may exist on the eastern ridge, though confirmation requires careful analysis of collected samples and imagery. Hydrothermal vents are of high scientific interest because they support unique ecosystems and offer clues about how life might arise in extreme environments, including icy moons such as Europa and Enceladus.

Operating Under 80 Percent Ice Coverage

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One of the expedition’s defining challenges was operating beneath thick, shifting pack ice. Ice cover limits emergency surfacing, complicates navigation, and restricts communication with surface vessels.

Successfully completing 32 under-ice dives demonstrated precise coordination between the submersible and its support ship. While the mission was scientific, the operational achievement itself represents a major advance in polar deep-sea capability, proving that sustained human activity is possible under dense Arctic ice.

Ship–Submersible Coordination in Extreme Conditions

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The research vessel Tan Suo San Hao played a critical role, maintaining position, tracking ice movement, and supporting recovery operations.

Under Arctic conditions, even small errors can lead to vehicle loss. The expedition validated procedures for positioning, timing, and risk management in ice-covered waters. Scientists emphasized that such coordination is essential not only for Arctic research but for any future missions requiring precise operations far from conventional ports or rescue infrastructure.

Mapping What Satellites Cannot See

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Satellite observations provide invaluable data on ice extent and surface conditions, but they cannot reveal fine-scale seafloor structure.

The Gakkel Ridge dives produced high-resolution imagery and measurements of terrain, slopes, and volcanic features previously inferred only indirectly. These data will improve bathymetric maps and help scientists understand how Arctic ridges differ from those in faster-spreading ocean basins, refining global geological models.

Climate Science at the Seafloor

The seasonal melting of sea ice across the central Arctic Ocean and surrounding basins peaks in July the region s warmest month In Foxe Basin currents tidal motion and winds can stir up the now-fragile pieces of ice producing art-like patterns on the water s surface One such moment of seasonal beauty was on full display on July 15 2024 when the OLI-2 Operational Land Imager-2 on Landsat 9 captured this image Foxe Basin off the west coast of Baffin Island in Nunavut Canada measures about 400 kilometers 250 miles across at its widest point Hudson Bay lies to the south connected to the basin by Foxe Channel and additional waterways within the Canadian Arctic Archipelago lie to the west The image above shows the northeastern part of Foxe Basin and several of its largest islands The basin s waters are often clogged with first-year sea ice-seasonal ice that is less than a year old New ice begins to form each year around October according to Environment and Climate Change Canada and it continues to spread and thicken through the winter until melting begins in late May or early June As of August 2024 the basin was nearly ice-free except for areas west of Baffin Island and within Foxe Channel The images above show detailed views of patterns in the ice on July 15 The basin s ice is often in motion producing the wispy tendrils of ice and paths of open water that trail some of the larger pieces All of this motion also helps stir up sediment which is the main reason for the ice s muddy appearance Pieces of eroded soil and debris-sloughed from the surrounding land and stirred up from the shallow seafloor-mix with the seawater and stain the ice brown Algae which can grow under the ice and wash onto its surface might also be contributing to the discoloration The basin is a haven for an array of wildlife Several polynas-areas of open water within the sea ice-are an important gathering place for species such as bowhead whales and polar bears Walrus migrating birds and other creatures also rely on the basin s resources NASA Earth Observatory images by Wanmei Liang using Landsat data from the U S Geological Survey Story by Kathryn Hansen
Photo by NASA Earth Observatory images by Wanmei Liang using Landsat data from the U S Geological Survey Story by Kathryn Hansen on Wikimedia


The Arctic is warming faster than any other region on Earth, yet deep-ocean processes remain poorly understood.

Samples from the Gakkel Ridge will help scientists study how deep waters circulate, store heat, and interact with seafloor geology. Such processes influence long-term climate regulation. Researchers stress that understanding the deep Arctic Ocean is essential for improving climate models, which currently rely heavily on surface and atmospheric data.

A Technological Milestone for Crewed Submersibles

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Fendouzhe is designed to reach depths exceeding 10,000 meters, making it one of the world’s most capable crewed submersibles.

The Arctic mission tested its systems in low-temperature, high-pressure conditions far from conventional support. Successful performance across dozens of dives provides engineers with real-world data on materials, life-support systems, and maneuverability, informing future upgrades and designs for extreme-environment exploration vehicles.

Scientific Mission, Strategic Attention

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While the expedition was conducted under a scientific mandate, it attracted international attention due to its location and capabilities demonstrated.

Analysts note that data on seafloor topography, ice behavior, and under-ice operations can have broader applications beyond science. Chinese officials emphasize peaceful research goals, but the mission nonetheless highlights how advanced polar science and national technological capacity increasingly intersect in regions of growing geopolitical interest.

The Arctic as a Zone of Renewed Interest

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U.S. Department of Defense Current Photos, Public domain, via Wikimedia Commons


As sea ice declines seasonally, Arctic regions are drawing increased attention from governments, researchers, and industry. Scientific access is often the first step in long-term engagement.

By conducting one of the most ambitious Arctic deep-sea missions to date, China positioned itself among a small group of nations capable of operating at extreme depths under ice. This presence adds momentum to broader international interest in the region’s future.

What Makes This Different From Past Expeditions

A person using a map for navigation inside a vehicle hinting at exploration and travel
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Previous exploration of the Gakkel Ridge relied on sonar mapping and uncrewed vehicles, which, while valuable, cannot fully replace direct human observation.

Crewed dives allow real-time decision-making, detailed sampling, and adaptive exploration. The eastern ridge’s first crewed survey therefore represents a qualitative shift, not just an incremental advance, in how scientists can study one of Earth’s most inaccessible geological systems.

From Raw Data to Years of Analysis

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YouTube – CGTN


Despite dramatic imagery and headlines, researchers caution that scientific conclusions will emerge slowly. Processing rock chemistry, biological specimens, and sediment records takes time, and results must be compared with data from other ridges worldwide.

Officials involved in the mission stress that its greatest value lies not in immediate discoveries, but in the long-term contribution of high-quality data to Arctic and global ocean science.

International Norms and Open Waters

A diver in a dry suit holding a spiny sea urchin underwater Close-up view
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The dives were conducted in international waters, where marine scientific research is broadly permitted under existing legal frameworks.

Such missions are common among deep-sea research nations, though under-ice operations remain rare. As activity in the Arctic increases, scientists and policymakers alike acknowledge that transparency and data sharing will be important for maintaining cooperation in a region where monitoring is inherently difficult.

Why the Eastern Ridge Matters Scientifically

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Photo by PHYS ORG


Because the Gakkel Ridge spreads at an exceptionally slow rate, it offers a natural laboratory for studying how Earth’s crust forms under minimal magma supply.

Comparing its eastern and western sections may reveal how volcanic and tectonic processes adapt to extreme conditions. Insights gained here could refine theories that apply not only to Earth, but to other rocky bodies with limited internal heat.

Redefining What Is “Inaccessible”

Aerial high-angle shot of an offshore platform in the clear waters of the Maldives
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For much of modern science, the deep Arctic seafloor symbolized the limits of human reach. The success of this expedition challenges that assumption.

By combining advanced submersible design with careful logistical planning, researchers demonstrated that even the most hostile environments can be studied directly. This does not eliminate risk, but it significantly expands the practical boundaries of ocean exploration.

A Door Opened Beneath the Ice

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Facebook – Global Times


China’s descent to the eastern Gakkel Ridge did not merely add another data point to oceanography; it opened a door to a region long considered unreachable.

The mission delivered samples, imagery, and operational lessons that will shape Arctic research for decades. While broader implications will continue to be debated, one fact is clear: three miles beneath the Arctic ice, one of Earth’s final unexplored frontiers is now, for the first time, within human reach.

Sources:
“Chinese Scientists Pioneer ‘Ship-Submersible Collaboration’ in the Central Arctic Ocean” – Chinese Academy of Sciences (CAS)
​“China’s manned submersibles report success of joint Arctic Ocean expedition” – The State Council Information Office of the People’s Republic of China
“Pioneering deep-sea mission ends” – China Daily
“China conducts ongoing manned deep dives in the Arctic” – CGTN (China Global Television Network)
“China’s 3 deep-sea manned submersibles have made over 200 dives this year” – SCIO (State Council Information Office)
“China’s scientific team makes history with first Arctic manned deep-sea exploration” – Global Times