Friday, May 8, 2026

Alaska’s near‑record landslide tsunami sent a wave 1,580 feet up the fjord walls – and left clues for building a warning system

The Tracy Arm landslide sent a tsunami wave far up the opposite side of the fjord near South Sawyer Glacier.
John Lyons/U.S. Geological Survey

From The Conversation by Michale E. West & Ezgi Karasözen

On the evening of Aug. 9, 2025, passengers on the Hanse Explorer finished taking selfies and videos of the South Sawyer Glacier, and the ship headed back down the fjord.
Twelve hours later, a landslide from the adjacent mountain unexpectedly collapsed into the fjord, initiating the second-highest tsunami in recorded history.
 
Localization with the GeoGarage platform (NOAA nautical raster chart)

We conduct research on earthquakes and tsunamis at the Alaska Earthquake Center, and one of us serves as Alaska state seismologist.
In a new study with colleagues, we detail how that landslide sent water and debris 1,580 feet (481 meters) up the other side of the fjord – higher than the top floor of the Taipei 101 skyscraper – and then continued down Tracy Arm.
The force of the water stripped the fjord’s walls down to bare rock.
 

The Tracy Arm landslide generated a tsunami that sent a wave so high up the opposite fjord wall that it would have overtopped some of the world’s tallest buildings.
Here’s how it compares to other large tsunamis around the world. 
Steve Hicks/University College London

It was just after 5 o’clock in the morning on a dreary day, and fortunately, no ships were nearby.
In the months after, some cruise lines started avoiding Tracy Arm.
However, the conditions that led to this event are not at all unique to this fjord.

Landslides are common in the coastal mountains of Alaska where rapid uplift, caused by tectonic forces and long-term ice loss, converges with the erosive forces of precipitation and moving glaciers.
But a curious pattern has emerged in recent years: Multiple major landslides have occurred precisely at the terminus of a retreating glacier.

Though the mechanics are still poorly understood, these mountains appear to become unstable when the ice disappears.
When the landslide hits the water, the momentum of millions of tons of rock is transferred into tsunami waves.
 

Maps show how the glacier has retreated over the years, moving past the section of mountain that collapsed (outlined in white on the right) in the days prior to the slide.
The map on the right shows the height the tsunami reached on the fjord walls.
Planet Labs


This same phenomenon is playing out from Alaska to Greenland and Norway, sometimes with deadly consequences.
Across the Arctic, countries are trying to come to terms with this growing hazard.
The options are not attractive: avoid vast swaths of coastline, or live with a poorly understood risk.
We believe there is an obvious role for alert systems, but only if scientists have a better understanding of where and when landslides are likely to occur.

Signs that a landslide might be coming

The Tracy Arm landslide is a powerful example.

The landslide occurred in August, when warm ocean waters and heavier precipitation favor both glacier retreat and slope failure.
The glacier below the landslide area had experienced rapid calving – large chunks of ice breaking off and falling into the water – and it had retreated more than a third of a mile in the two months prior.
Heavy rain had been falling.
Rain enters fractures in the mountain and pushes them closer to failure by increasing the water pressure in cracks.

Most provocative are the thousands of small seismic tremors that emanated from the area of the slide in the days prior to the mountainside collapsing.

 
The view from the deck of the Hanse Explorer on Aug. 9, 2025, shows the mountain where the landslide occurred just 12 hours before it happened.
Hanse Explorer


We believe that this combination of signs would have been sufficient to issue progressive alerts to any ships in the vicinity and homes and businesses that could have been harmed by a tsunami at least a day prior to the failure – had a monitoring program existed.

Escalating alerts are used for everything from terrorism and nuclear plant safetyto avalanches and volcanic unrest.
They don’t remove the risk, but they do make it easier for people to safely coexist with hazards.

For example, though people are still killed in avalanches, alert systems have played an essential role in making winter backcountry travel safer for more people.
The collapse at Tracy Arm demonstrates what could be possible for landslides.

What an alert system could look like

We believe that the combination of weather and rapid glacier retreat in early August 2025 was likely sufficient to issue an alert notifying people that the hazard may be temporarily elevated in a general area.
On a yellow-orange-red scale, this would be a yellow alert.

In the hours prior to the landslide, the exponential increase in seismic events and telltale transition to what is known as seismic tremor – a continuous “hum” of seismic energy – were sufficient to communicate a time-sensitive warning for a specific region.
 
Seismic data from the closest monitoring station to the landslide, about 60 miles (100 kilometers) away, shows the “hum” of seismic energy increasing just ahead of the landslide, indicated by the tall yellow spike shortly after 5 a.m.
Source: Alaska Earthquake Center.


These observations, recorded as a byproduct of regional earthquake monitoring, warranted an “orange” alert noting immediate concern.
The signs were arguably sufficient to recommend keeping boats and ships out of the fjord.

Our research over the past few years has demonstrated that once a large landslide has started, it is possible to detect and measure the event within a couple of minutes.
In this amount of time, seismic waves in the surrounding area can indicate the rough size of the landslide and whether it occurred near open water.

A monitoring program that could quickly communicate this would be able to issue a red alert, signaling an event in progress.

The National Oceanic and Atmospheric Administration’s tsunami warning program has spent decades fine-tuning rapid message dissemination.
A warning system would have offered little help for ships in the immediate vicinity, but it could have provided perhaps 10 minutes of warning for those who rode out the harrowing tsunami farther away.

An animation showing the tsunami’s reach up the fjord walls after the landslide, as well as the large cresting wave as it heads down Tracy Arm.
Credit: Shugar et al., 2026.


There is no landslide monitoring system operating yet at this scale in the U.S.
Building one will require cooperation across state and federal agencies, and strengthened monitoring and communication networks.
Even then, it will not be fail-proof. 

Understanding risk, not removing it

Alert systems do not remove the risk entirely, but they are a better option than no warning at all.
Over time, they also build awareness as communities and visitors get used to thinking about these hazards.

Many of the most alluring places on Earth come with significant hazards.
Arctic fjords are among them.
The same processes that create this hazard – glacier retreat, steep terrain, dynamic geology – are also what make these landscapes so compelling.
The mix of glaciers, ice-choked waters and steep mountains is exactly what draws people to these places.
People will continue to visit and experience them.
 

The last view of Tracy Arm, taken from the Hanse Explorer motoring away from the South Sawyer glacier, before a landslide from a mountain just out of view on the left crashed into the fjord.
The landslide generated a tsunami that sent a wave nearly 1,600 feet (about 490 meters) up the mountain on the right.


The question is not whether these places should be avoided altogether, but how to help people make more informed decisions.
We believe that stronger geophysical and meteorological monitoring, coupled with new research and communication channels, is the first step.

On Aug. 9, visitors unknowingly passed through a landscape on the cusp of failure.
An alert system might have given tour companies and people in the area the information they needed to make more informed choices and avoid being caught by surprise.
 

Thursday, May 7, 2026

UKHO : changes in standard nautical charts (SNC) produced from ENC


 
This document provides an overview of changes to the display treatment of selected features on ADMIRALTY Standard Nautical Charts (SNCs) produced from Electronic Navigational Chart (ENC) data. 
As part of the ongoing evolution of the ADMIRALTY paper chart portfolio, some new edition SNCs are now being generated using ENC data. Certain chart elements may therefore appear differently from previous editions, reflecting a more standardised and consistent approach to chart presentation. 
The purpose of this guide is to help users understand what has changed, what remains the same, and how to interpret these features when using ADMIRALTY SNCs produced from ENCs. These changes relate only to how information is displayed and do not affect the underlying safety, accuracy or compliance of ADMIRALTY Standard Nautical Charts. 
This document should be used as a reference alongside the chart to support familiarisation with updated chart presentation.


Science has just discovered “oases” of clams and tube worms at a depth of 9,533 meters, where sunlight does not exist and yet life thrives in abundance


From Ecoticias

A last-minute detour nearly six miles down has led scientists to what they call the deepest known ecosystem on Earth, a long stretch of seafloor communities that don’t depend on sunlight at all.
Instead, clams and tube worms appear to survive on chemical energy from methane and other gases leaking out of cracks in the ocean floor.

The discovery, described in a new Nature study, comes from dives in two remote trenches in the northwest Pacific, including areas between Russia and Alaska.
It also adds a fresh twist to a big question in ocean science: how far down can life really go, and what keeps it going when there’s no light, little food, and crushing pressure?

A “one-more-look” moment in the hadal zone


The hadal zone is the deepest part of the ocean, starting around 6,000 meters down and running to the bottom of the deepest trenches.
Think of it as Earth’s underwater canyons, where pressure is so extreme that ordinary submarines cannot go.

During a 2024 expedition that ran from July 8 to August 17, researchers used the deep-diving submersible Fendouzhe to explore the Kuril-Kamchatka Trench and the western Aleutian Trench.
Geochemist Mengran Du, working with Xiaotong Peng, reported seeing dense groups of animals at depths from about 5,800 to 9,533 meters, spanning roughly 2,500 kilometers.

How methane replaces sunlight

Most life on Earth ultimately runs on sunlight, because plants and algae use it to make food.
In these trenches, there’s no light at all, so the system runs on chemosynthesis, which is basically “making food from chemicals” instead of from sunlight.

Here’s the simple version.
Cold seeps are cracks in the seafloor that leak chemicals like methane and hydrogen sulfide, and NOAA’s cold seep overview explains how bacteria can use those chemicals for energy.
Some of these bacteria live inside animals like clams and tube worms, feeding their hosts in a kind of built-in food factory.

A new clue about carbon cycling in the deepest ocean

What surprised the team wasn’t just the animals, but the chemistry under them.
The researchers reported unusually high methane in trench sediments, and they suggest microbes may be producing methane locally by processing buried organic material and recycling carbon on site.

In practical terms, that means the trenches may act less like a dead-end storage pit and more like a “recycling center” for carbon in the deep ocean.

That matters because methane and carbon dioxide are powerful greenhouse gases in the atmosphere, and understanding where carbon ends up, and how long it stays there, helps scientists build better climate and ocean models.

Why this matters beyond the trenches


Experts who were not part of the work say the size and depth of the communities stand out.
Johanna Weston of Woods Hole Oceanographic Institution has pointed out that deep trenches are remote, but they’re still connected to the surface, including through food pulses and pollution that sinks.

That connection keeps showing up in other research.
Weston’s team recently described a deep-sea scavenger that feeds on sinking seaweed in the Atlantic in a Woods Hole press release, and earlier work linked trench life to plastic pollution through an Eurythenes plasticus report.

Meanwhile, methane-based partnerships aren’t limited to trenches, as shown by a methane-powered sea spiders study that found deep-sea spiders hosting methane-eating microbes on their bodies.

What comes next for exploring the deepest ocean

The big takeaway is that these chemical-powered communities may be more widespread than scientists once thought.
If similar cold seep conditions exist in other trenches, there may be more “dark ecosystems” waiting, and some species may be new to science.

That’s one reason international efforts are ramping up, including the Global Hadal Exploration Programme, which aims to coordinate deep-ocean research across countries and disciplines.
It fits a broader surge in species discovery, highlighted by the Ocean Census announcement that reported hundreds of newly documented marine species.

Links :

Wednesday, May 6, 2026

NOAA releases first images of nodules from waters near American Samoa


Image of geological samples from the seafloor that were collected via box core on April 14, 2026, in U.S. waters off American Samoa. (Image credit: USGS)
Download Image

From NOAA
 
New images and samples were collected during 2026 efforts to map and characterize the seafloor in federal waters off American Samoa 

NOAA released today the first images of geologic seafloor samples from a hydrographic survey project to map and characterize more than 30,000 square nautical miles of federal waters in the U.S. exclusive economic zone (EEZ) beyond the territorial waters of American Samoa. The box core samples will allow for further analysis to understand the composition of deep sea resources and the environments in which they are found.

“NOAA’s mapping missions serve as a reminder that ocean exploration is a vital piece of our nation’s economic development,” said NOAA Administrator Neil Jacobs, Ph.D. “These images highlight the outstanding work of our NOAA team and partners to characterize the seafloor, and the data gathered during this historic project will enable science-based decision-making to support responsible development.”

The new images were collected as part of a Department of Commerce initiative to implement the U.S. Offshore Critical Minerals Mapping Plan as defined by President Trump’s Executive Order 14285: Unleashing America's Offshore Critical Minerals and Resources. In developing the mapping plan, NOAA, in consultation with the Department of Interior’s Bureau of Ocean Energy Management(BOEM) identified the federal waters near American Samoa as a priority area of the seabed for mapping and analyzing nodules that may contain critical minerals.

“NOAA’s work to map and characterize these areas reflects the strength of interagency collaboration under President Trump’s Executive Order to unleash America’s offshore critical minerals,” said BOEM Acting Director Matt Giacona. “For BOEM, NOAA’s high-resolution mapping and characterization are essential inputs that will provide the foundational data needed to assess resource potential, inform leasing and environmental reviews, and reduce uncertainty as we evaluate future offshore mineral activities in a responsible, science-based manner.”

As the mission remains underway, images of the seafloor and box core samples will be posted online on a rolling basis, serving as an initial indication of mineral resource potential and the deep-ocean marine environment in the federal waters off American Samoa. Scientists from the U.S. Geological Survey (USGS) will conduct analyses of the seafloor composition, which will enhance scientific understanding of the deep seabed in the region and inform future exploration and activities related to deep seabed minerals. USGS plans to release the initial analyses from this work early this summer.

Presumed polymetallic nodules on the seafloor off American Samoa at a depth of 5,498 meters (3.42 miles) prior to the collection of a box core. (Image credit: NOAA)
Download Image


“USGS is excited for the opportunity to study the composition of these unique mineral samples in U.S. waters within the Samoa Basin,” said Ned Mamula, director, USGS. “We will continue providing the actionable science our partner agencies need for decision-making.”

NOAA’s Office of Coast Survey is leading the project contract, with NOAA Ocean Exploration, BOEM, and USGS providing additional scientific expertise and guidance.

About deep seabed mineral development

Deep seabed mining is the extraction of nodules containing critical minerals from the ocean floor. Some regions of the deep seabed contain an abundance of valuable resources like manganese, nickel, cobalt, copper and rare earth elements. Critical minerals are used in everything from defense systems and batteries to smartphones and medical devices and are increasingly important components for American manufacturing. Access to these minerals is a key factor in the resilience of U.S. supply chains. Learn more by visiting NOAA’s National Ocean Service website.

Tuesday, May 5, 2026

The seabed doctrine: when commercial infrastructure gets drafted

 
 
From Pulse by Dize Kandu
 
There is a sentence buried on page seventeen of the U.S. Strategic Subsea Cables Act of 2026 that I cannot stop thinking about.
It quotes NATO: undersea cables carry an estimated ten trillion dollars in transfers every day, and around ninety-five percent of global data flows are transmitted through them.
The number is doing the work of an argument.
You read it and you feel, viscerally, that something so vital must be protected and whatever protection looks like, it must be worth the cost.

That is how doctrine gets written now.
Not with tanks, not with treaties, but with statistics placed so precisely that the conclusion appears to arrive on its own.

I have been watching the subsea cable file for a while as a maritime security professional, but also as someone who lives in a country where several of the world's critical digital arteries surface.
What is happening in Washington right now is not, properly speaking, a cable protection bill.
It is the quiet legislative reclassification of a global commercial network into a strategic military asset, and it is being done through a door almost no one is watching: the door of narrative.

What the Act Actually Does

Let me walk through the legislation, because most of the summaries floating around have been written by people who read the press release and stopped there.

The Strategic Subsea Cables Act of 2026, introduced in March by Representatives Wilson and Meeks with Senate companions from Shaheen and Barrasso, pairs with H.R.2503, an export control bill that industry analysts have already started calling "the shield" to the Act's "sword."
The shield keeps subsea cable manufacturing and maintenance technology out of Chinese hands, accelerating what submarine industry observers describe as a formal split between "trusted" Western cable supply chains and "untrusted" Chinese ones.
The sword, this new Act, does four things.



It mandates sanctions against any foreign person who intentionally damages undersea infrastructure.
It creates ten full-time State Department positions dedicated to cable diplomacy, with instructions to work the International Cable Protection Committee harder and to build a multinational fleet of dedicated repair ships.
It establishes a presidential interagency committee to coordinate U.S.cable policy across the Department of State, Homeland Security, the Department of War, the Department of Commerce, and others.
And it requires federal agencies to share threat information directly with private cable operators, who are, let us remember, commercial telecommunications companies.

Read those four elements together, and something becomes clear that the summaries do not state.
The Act is not designed to protect cables.
It is designed to enroll them.
A commercial fiber-optic line laid by a consortium of private carriers becomes, under this framework, a node in an American-led enforcement architecture, one whose operating concept is sanctions, whose intelligence-sharing moves in one direction, and whose legal theory rests on intentional state-sponsored sabotage.

And here is where the architecture starts to show its seams.

Of the roughly six hundred active cables on the planet, around four private firms; SubCom (United States), Alcatel Submarine Networks (France), NEC (Japan), and HMN Technologies (China), manufacture and install the overwhelming majority.
Consortiums own most of the cables.
Landings are scattered across dozens of jurisdictions.
The repair fleet, such as it is, is chronically undersized and aging.
No single government commands this system.
No single government can.
The Act does not attempt to build shared governance; it attempts to install U.S. jurisdiction over the parts that can be reached through sanctions, licensing, and the threat of private litigation.
It is, functionally, a workaround for the fact that the actual system is bigger than any one state.
Juha Martelius and the Inconvenient Problem of Evidence

Which brings me to a name most people in the defense community outside Europe have never heard.

Juha Martelius is the director of Supo, Finland's Security and Intelligence Service, an agency whose sole job is to understand what is actually happening on and under the water between Finland and Russia.
In March of this year, Supo published its National Security Overview for 2026, and Martelius put something on the record that Washington has not yet fully absorbed.
Direct quote, publicly delivered: "Our understanding has been that there has been no deliberate Russian state activity in the background.
It is a very broadly shared view in the other European intelligence community."

Let that sit for a moment.

Source: Dmitri Fedotkin/ERR

The country that lost the Estlink 2 power cable on Christmas Day 2024.
The country that seized the Eagle S tanker, spent months investigating it, charged its officers with aggravated criminal mischief, and then watched its own courts struggle with the fundamental legal question of whether anchor drag outside territorial waters could even be prosecuted as sabotage under existing law.
The country that knows exactly how to run a cable incident to ground, because it has done it, that country, through the agency best positioned to know, is saying: slow down.
Not every cable fault is a hybrid warfare attack.
And labeling every incident as Kremlin-directed sabotage, Supo warns explicitly in its assessment, "may actually amplify the fear and perceived reach of Russian power, which serves Russian strategic interests."

In intelligence terms, this is a devastating observation.
Finland is essentially telling the rest of the Western alliance that the narrative around subsea cable incidents is running ahead of the evidence, and that the narrative itself is doing Moscow's work for it.

There is a deeper technical point embedded in Supo's caution that deserves attention.
The Baltic Sea, where most of the recent incidents have clustered, sees an enormous volume of commercial traffic through shallow, cable-dense waters.
Of the roughly 150 to 200 cable faults that occur worldwide every year, the overwhelming majority are caused by fishing trawlers and anchor drops in waters under two hundred meters.
Seven cable cuts in the Baltic between November 2024 and January 2025 sounds alarming, and it is.
But it is also statistically consistent with what happens when shadow fleet vessels, poorly maintained, crewed by people working under opaque ownership structures, operating tankers with documented equipment failures transit one of the world's most cable-dense shallow seas.
Some of those incidents are almost certainly deliberate.
Some are almost certainly not.
Distinguishing between the two requires forensic patience that a sanctions-driven policy framework actively discourages.



The Eagle S case is the case study nobody wants to talk about.
Finnish prosecutors could not prove intent.
They pivoted to a clever argument, that operating a vessel so poorly maintained that its windlass could malfunction constituted criminal recklessness but the court was unmoved on the jurisdictional question of damage occurring in the exclusive economic zone rather than territorial waters.
The tanker was eventually released.
The crew returned home.
The cable was repaired.
And Finland was left with a legal system that had tried, in good faith, to prosecute suspected cable sabotage under the rule of law and run aground on structural limitations that international maritime law never contemplated when it was written.

The Strategic Subsea Cables Act does not solve that problem.
It routes around it.
If the courts cannot prove intent, sanction the ship's beneficial owner.
If the flag state is useless, target the registry itself.
If the evidence is ambiguous, let the cable owner file a civil suit that does not require the same burden of proof.
This is not the rule of law being strengthened.
It is the rule of law being supplemented by the rule of unilateral economic pressure, and the supplement is quickly becoming the main instrument.

The Attribution Problem



Here is the gap that most Western defense commentary is refusing to address.
It is not a question of whether Russia has the capability and intent to damage subsea infrastructure.
It plainly does.
The GUGI fleet, Russia's Main Directorate for Deep Sea Research, maintains special-purpose vessels at Olenya Guba that are explicitly designed for seabed operations, including deep-diving submersibles, oceanographic surveillance ships, and nuclear-powered auxiliary submarines built for exactly this kind of work.
The reconnaissance patterns in the Baltic are real and have been documented for years.
No serious analyst disputes any of that.

The question is whether a legislative and sanctions architecture should be built on the assumption that every incident is confirmed sabotage, when the country with the most operational experience is telling us that sometimes a dragged anchor is a dragged anchor, and sometimes a windlass really does malfunction on a rusty tanker owned by a brass-plate company at a Dubai hotel address.
There is, of course, a middle category that deserves its own scrutiny: incidents that are not state ordered but are state tolerated, recklessness that Moscow neither commands nor prevents because the resulting chaos serves its interests regardless of who initiated it.
That distinction matters enormously, and it is precisely the kind of distinction that a sanctions first framework is structurally incapable of drawing.

This matters because attribution, once codified into policy, becomes self-reinforcing.
Every subsequent incident gets read through the attributed framework.
Every ambiguity resolves in favor of the conclusion already reached.
Supo has seen this before, in a different context, admittedly, but the institutional memory is relevant.
Finnish intelligence spent much of the Cold War learning how to distinguish between what Moscow was actually doing, what Moscow wanted Helsinki to think it was doing, and what Helsinki's allies were projecting onto the relationship.
That kind of analytical discipline is rare, and it is exactly what the current moment requires.

The American framework does not have that discipline built into it.
It has the opposite: a bipartisan consensus that adversary attribution is politically cheap and politically useful, combined with a legal architecture that rewards speed over accuracy.

The Classical Problem: What a Cable Actually Is

There is an older debate hiding underneath this new one.
In classical international law, subsea cables are commercial infrastructure, and their protection has been governed since 1884 by a convention whose enforcement mechanism is basically "the courts of the flag state will probably do something, eventually." 
UNCLOS adds some overlay but does not fundamentally change the commercial character of the assets.



The Strategic Subsea Cables Act does not amend either framework.
What it does instead is create a parallel, unilateral enforcement regime grafted onto commercial assets, one where the U.S.
government shares "threat information" with private operators, imposes sanctions on suspected saboteurs, and encourages cable owners to pursue private lawsuits against anonymous defendants in the style of Google's recent "Does 1 through 25" case, a civil action in which the company sued unnamed defendants operating fraudulent online advertising schemes linked to Chinese networks, using discovery mechanisms to unmask anonymous actors.
CSIS has been admirably candid about this framework, calling it "deterrence by detection" and "deterrence by punishment," and crediting it with a novel virtue: eliminating "plausible deniability."

I understand the appeal.
I really do.
Faced with a string of cable incidents in the Baltic and growing nervousness about Chinese behavior in the South China Sea, something has to be done.
But "deterrence by detection" is only as good as the attribution regime underneath it.
And if Finland, whose intelligence service is paid to be paranoid about exactly this question, is publicly saying the attribution is shakier than the headlines suggest, then what the Act is actually deterring may not be sabotage.
It may be deniability itself.

Which is a different, more interesting, and considerably more aggressive thing.

Deniability, in the grammar of international relations, is what allows states to act in the grey zone without triggering formal escalation.
Stripping it away sounds like a pure good, who, after all, is in favor of plausible deniability? The counter argument is not frivolous: deniability is also an enabler, the very mechanism that allows grey zone operations to continue without consequence, and reasonable analysts can disagree about which function predominates.
But in practice, deniability also functions as a shock absorber.
It creates space for quiet de-escalation, backchannel resolution, and the slow work of attribution that Finnish courts, for all their failures, have at least tried to do properly.
A regime that eliminates deniability through pre-attributed sanctions does not reduce hybrid warfare.
It simply relocates the escalation from the water to the courtroom, from the courtroom to the sanctions list, and from the sanctions list to wherever comes next.
What This Looks Like From Outside Washington



For countries positioned at the intersection of multiple cable corridors, Türkiye being one of them, with Mediterranean and Black Sea systems landing and transiting through our jurisdiction, a legislative architecture that converts commercial cables into strategic U.S.
assets is not a neutral development.
It is the extraterritorial extension of American maritime authority over infrastructure that touches our territorial waters, exclusive economic zones, and landing stations.

The Act does not ask Türkiye's permission to sanction a vessel that happens to drag its anchor near a cable running through our seabed.
It does not require coordination with the countries whose forensic intelligence services may have reached different conclusions about a given incident.
It simply installs Washington as the primary adjudicator of what counts as sabotage, what counts as accident, and what penalties attach to each.

Consider what this means in practice.
A Russian-linked tanker damages a cable in the Black Sea.
Under the Act, the U.S.
Treasury can move against the vessel's beneficial owner, freeze its assets, and pressure its insurers and classification society, all before a Turkish investigation has even begun.
Cable owners, many of them American companies, can file civil suits in U.S.
courts for damages that occurred in our waters.
Sanctions packages can be built on intelligence we did not participate in collecting and attribution judgments we did not review.
The enforcement architecture operates regardless of whether the coastal state agrees with the underlying analysis.

This is STRATCOM in legislative form, not the discipline of strategic communications as commonly understood, but its older sibling, the construction of an interpretive framework so dense, so pre-populated with conclusions, that disagreement sounds naive.
When every cable incident arrives with its attribution already attached, the policy response becomes automatic.
When the policy response becomes automatic, the policy framework becomes permanent.
When the policy framework becomes permanent, the cables themselves stop being commercial infrastructure in any meaningful sense.
They become something else.
They become a theatre.

And theatres, as anyone who has studied maritime security knows, are never neutral spaces.
What Can Be Done



What is to be done, then, by those of us who are not writing the legislation in Washington but who will have to operate inside its consequences?

First, build independent analytical capacity.
Every coastal state with significant cable exposure should develop its own forensic and attribution expertise, separate from whatever Washington's interagency committee decides to share.
Finland's Supo is a model precisely because it is willing to say "we do not see what you say you see." That kind of epistemic independence is now a strategic asset, not a diplomatic inconvenience.
For Türkiye specifically, with our existing maritime intelligence infrastructure and our geographic position at the chokepoints of two cable theatres, this capacity is achievable within a realistic timeframe if the institutional will exists to build it.

Second, insist on the older framework.
Subsea cables are commercial infrastructure under the 1884 convention and under UNCLOS.
They are also strategic in effect, yes, but collapsing the distinction between commercial and military in legal terms is exactly the move that allows unilateral enforcement to masquerade as international law.
Countries with cable landings should resist the collapse, not because sabotage is fine, but because the legal categories still matter and because once they are collapsed, it will be very difficult to uncollapse them.
International maritime law evolves at the speed of consensus, and unilateral reclassification by the most powerful actor in the system is not consensus.

Third, and this is the part that defense sector LinkedIn will find uncomfortable: recognize that "deterrence by detection" is a narrative weapon before it is a technical one.
The AI, the predictive analytics, the cued satellite imagery, all of it is real and useful.
I have no quarrel with the technology, and the detection architecture has produced real operational value in tracking vessel movements and identifying suspicious transit patterns that would otherwise go unnoticed.
But what gets detected depends on what you are looking for, and what gets reported depends on who is writing the press release.
A maritime security architecture in which only Washington gets to name the saboteurs is not a security architecture.
It is a content strategy with sonar attached.

Fourth, invest in regional cooperation that does not run through Washington.
The Mediterranean cable cluster, the Black Sea landings, the Red Sea transit routes through Egypt, each of these is a theatre where coastal states have direct interest and insufficient coordination.
The European Union's 2025 cable security action plan is a start, but it remains overwhelmingly Atlanticist in its framing.
What is missing is a genuinely regional attribution and response framework that reflects the intelligence priorities and legal traditions of the states whose waters actually hold the cables.

The Argument, in the End



I will end with the sentence that started this piece.
Ten trillion dollars in transfers every day, ninety-five percent of global data.
Those numbers are real.
But they describe a commercial network that serves everyone, built mostly by four private companies, maintained by repair ships crewed by labour from a dozen countries, funded by consortiums that cross every geopolitical fault line on the planet.
It is one of the few genuinely shared pieces of infrastructure that the modern world still has.
The fact that my bank transaction and a Chinese financial transfer and a Russian diplomatic cable all ride the same fiber-optic strand for part of their journey is not a vulnerability to be eliminated.
It is a rare, dwindling piece of functional interdependence.

The question is whether we protect it as something shared, or whether we let it be drafted into somebody else's war.

Finland, quietly, is arguing for the former.
The Strategic Subsea Cables Act is quietly delivering the latter.
And the rest of us are going to have to decide, sooner than we think, which architecture we actually want to live inside.