Thursday, February 26, 2026

Say goodbye to the undersea cable that made the global Internet possible

illustration : Rob Vargas
 
From Wired by Jane Ruffind

History was unmade last year, as engineers began the massive project of ripping the first-ever transoceanic fiber-optic cable from the ocean floor.
Just don’t mention sharks.

SHARKS ARE INNOCENT.
Or at least they’re not eating the internet.
As a family of cartilaginous fish, sharks are collectively not guilty of most, if not all, charges of biting, chomping, chewing, or otherwise attacking the underwater network of fiber-optic cables.
The people who build and maintain the nearly 600 subsea cables that carry almost all of our intercontinental traffic—supporting just about every swipe, tap, Zoom, and doomscroll anywhere on the planet—have a love-hate relationship with this myth, which has persisted for decades.
They might even hate that I’m starting this piece with it.

If a cable is suspended over the seabed, a shark might gum it as it explores.
Sometimes they’ll lunge for a cable that’s being pulled out of the water.
But for a shark to actually bite a cable, you’d have to wrap it in fish, much as you’d hide a pill in a hunk of cheese for the dog.
Rats can be a threat on land, because their incisors never stop growing, so they like to file them down on semisoft cables.
But nobody ever asks about rats, maybe because, as a friend of mine pointed out, “sharks make you cool, but rats sound like you have a problem.”

Sometimes people ask about satellites or, especially in Sweden (where I live), about alleged sabotage in the Baltic Sea.
But historically, shark bites have commanded the most attention.
The myth began nearly 40 years ago, with the development of a subsea fiber-optic cable known as TAT-8.
TAT-8 practically invented the concept of an internet cable, and now that it’s ready for retirement, I spent time with the offshore workers, crew members, and engineers who are in the process of pulling it off the seabed.
That’s the real story of subsea cables—not sabotage or sharks, but the humans who take care of the physical stuff that keeps all of our digital communication flowing.

FIBER-OPTIC TRANSMISSION IS a near-magical way of carrying information by pulses of light.
Most people don’t even think about how quickly we’ve accepted instantaneous communication as normal, even those of us who can remember when an international phone call had to be booked in advance.
The more people I meet in this industry, in this network of networks of people and things, the more insulting it sounds to hear that “we” only notice it when it breaks.
(Who is this “we,” I always want to know?)
Billions of people are able to walk around not noticing this infrastructurebecause of the daily work of a few thousand people, sometimes at sea, other times buried under piles of permits, surveys, and purchase orders for thousands of kilometers of cables that will join the millions of kilometers of cables on the seabed that ensure that our planet is continuously being hugged by light.

I also need to clear up something else.
Most people call them “internet cables,” but technically, fiber-optic transmission was developed for telephone calls.
One of the people involved was an English scientist named Alec Reeves, who also spent his time working on psychokinesis and telepathy.
With fiber, voices become light, pulsate across spiderweb-thin strings of glass, and become voices again in your handset on the other end.
Maybe there isn’t that much of a conceptual leap between that and moving things with your mind.

TAT is short for Trans-Atlantic Telephone, and TAT-8—built by AT&T, British Telecom, and France Telecom—was the eighth transoceanic system across the Atlantic.
It was the first to use optical fibers to transmit traffic between Europe and the United States.
Fiber optics for communication had only been worked out in theory in the 1960s, and terrestrial cables were first used in the 1970s.
But using this technology to span continents was practically tantamount to human galactic expansion.

When TAT-8 went into service on December 14, 1988, the science fiction writer Isaac Asimov spoke on video link from New York to audiences in Paris and London: “Welcome everyone to this historic transatlantic crossing,” he said, “this maiden voyage across the sea on a beam of light.” AT&T made a TV ad, in which an earnest voice-over promised a “worldwide intelligent network” where people could send information in any format to anyone they want.
Cue the montage of telephone operators: “This is the AT&T operator. You have a call booked for Poland?” 
“I have your call to Russia.” 
“What city in Cuba are you calling?”
If they were looking to inspire viewers, it wasn’t with the promise of the internet, which was still too niche for most of us to comprehend, but with the end of the Cold War.

TAT-8 would witness the fall of the Berlin Wall, the birth of the World Wide Web, the end of the Soviet Union, the dotcom boom, the end of Tory rule in the UK and the beginning of the Bush years in the US, the September 11 attacks, the dotcom crash, and the dawn of social media (it was Friendster).
Rather than being the last cable ever needed, as had originally been believed, it was full to capacity within 18 months, by which point there were other cables, like PTAT-1 across the Atlantic and TPC-3 in the Pacific.
By 2001, the TAT series was up to number 14.
After developing a fault that was too expensive to be worth fixing, TAT-8 was taken out of service in 2002.

It’s been sitting on the seabed until now.


The MV Maasvliet docks in Portugal to offload recovered fiber-optic cable.
Photograph : Fiona Marron

A view of the monitor in the ship's control area.
Photograph : Fiona Marron
 

Captain's controls on the Maasvliet.
Photograph : Fiona Marron

TAT-8 IS CURRENTLY being pulled up and sent for recycling by Subsea Environmental Services, one of only three companies in the world that’s made cable recovery and recycling its entire business.
Cable companies sometimes recover their own cables after they take them out of service, and some retired cables get new life in scientific research or military use, but most of them—most of the 2 million kilometers of it all—are still right where their former owners left them.
The seabed is a lot busier than you might think, so these operations are clearing space for new cables, along routes that are proven and efficient, rather than disturbing new sections of the sea floor.
And there’s good money in old cables if you know what you’re doing.

It’s after midnight on a cool August night, and my friend Fiona Marron—here to take photos and videos—and I are watching Subsea’s brand-new diesel-electric cable recovery vessel, the MV Maasvliet, dock in the Portuguese port of Leixões, just outside of Porto.
The 14 people on board are two weeks overdue because hurricane season arrived early, and they had to dodge storms Dexter and Erin, which meant they collected more stress and less cable than expected.
During the next week or so, they’ll offload 1,012 kilometers of TAT-8, resupply the ship, then set out again to pick up another load.

They drop the gangway, and there are hugs between the crew and Peter Appleby, operations manager from Subsea.
Up on the bridge, we meet Captain Alex Ivanov, who has been at sea for 30 years and still takes pictures of sunsets.
He scrolls through his phone to show Peter a blazing red and orange sky, then photos of some of the dorado he caught, because when cable ship people aren’t fishing for cable, some of them go fishing for fish.

Peter asks how Alex likes the ship.
Alex helped design it, and this is only its fourth trip out since it left drydock in January 2025.
The captain says he loves the diesel electric—the Maasvliet runs on three industrial Volvo truck engines—even though he says it isn’t as stable as the Rebecca, the company’s other vessel.
The bridge is high-tech and modern, but everything is touchscreens and sensors, and he says if he loses power, he loses everything.
Then he zips off, getting ready for tomorrow, when he’ll hand charge of the ship over to another captain, Vlad.
Vlad will show up wearing a new T-shirt that says “Everything can go wrong at sea” on the front and “Not on my fucking watch!” on the back.

The food serving area aboard the Maasvliet.
Photograph : Fiona Marron
 

The ship's fridge is restocked at port.
Photograph : Fiona Marron

Everyone who has been at sea will tell you that the most important people are the captain and the cook, and all good captains are servant leaders and will concede that the cook is more valuable.
Crew members are from Ukraine, Russia, Poland, Nigeria, and Kenya, and the cook knows everyone’s comfort foods.
Misha, the cook who’s now rotating out, heard one of the crew talking about how much he loved khinkali, Georgian soup dumplings, and the next Sunday they were on the tables.
Peter always brings cottage cheese, cream cheese, and cabbage when he meets a ship in port.
I’m suddenly aware that I’m not just a guest on a ship, I’m a middle-aged mom who has shown up at someone’s home without snacks or a host gift.
Fiona and I are also the first strangers any of these people have seen in two and a half months.

I’M HERE IN Leixões because I’m a researcher in the material culture of the subsea cable industry, and I consider it my business to help people understand that the networks we rely on are made of physical things, created and maintained by people, so that we can stop saying infrastructure is invisible as if the people are invisible too.

Another way to irritate a cable nerd is to suggest that low-Earth-orbit satellites—which are unreliable in bad weather, are harder to repair, and need to be replaced every five years—will one day be our main source of connectivity.
Satellites are still an important component for resilient physical infrastructure, especially in areas with few or no fiber connections, but they haven’t been able to compete on capacity since the 1990s.

Back in the 1970s, though, satellite technology seemed so promising that the Federal Communications Commission made it clear to AT&T: If you don’t do something revolutionary with cables, we’re not going to grant permission for any more intercontinental submarine connections.
At the time, cables relied on copper, and there’s only so much capacity you can cram into a bundle of wires.
So, in 1978, Bell Labs, along with its British counterpart, STC, committed to installing a nearly 6,000-kilometer-long submarine fiber connection between the US, UK, and France.
In Holmdel, New Jersey, Bell Labs began testing out cables, and in 1985 the company deployed its first live test system, known as Optican-1, between two of the Canary Islands.
Optican-1 worked, but it had a series of what are called shunt faults, where damage to the insulation interrupts the electrical signals.

Now, here come the sharks.
Elaine Stafford was the project manager for Optican-1.
In 1986, she was a rare young woman on the scene, on her way to Paris to present an update on the cable at the first of what would become the industry’s main research and development conference.
“I’m supposed to be giving this huge talk, that there’s this wonderful technology and it’s working fine, and it’s going into service, but we had this big question mark,” she recalls.
They didn’t know what had caused the faults.

Jack Sipress, who in Stafford’s recollection was two levels above her at Bell Labs, got on the bus to the conference center.
“And he says, ‘I have the shark teeth,’” Stafford tells me.
“He pulls them out and says, ‘These were pulled out of the faulted cable.’ So we went to the conference and announced to the world that it was shark teeth.”
AT&T even included four pages about shark-bite mitigation in its 36-page press kit for TAT-8.

To be clear, there still isn’t consensus that the sharks caused the shunt fault.
Sipress wasn’t lying about the teeth, but it’s hard to know what really happened.
Stewart Ash, who was part of the UK team at STC, insists that most shark claims really are false.
If the Optican-1 was installed with too little slack, though, and hung above the seafloor in some areas, a shark might’ve munched down.
“While we at STC didn’t believe it,” he says, “we were swept up in the frustration or fear that sharks could interrupt these very important, brand-new cables.”

To be absolutely sure, AT&T funded research at two aquariums: in Mystic, Connecticut, and Sarasota, Florida, where researchers let some dogfish and lemon sharks get a little hungry and then tested to see if they bit any of several different cables that were emitting electrical fields in different patterns.
They didn’t, except in seemingly random cases.
(To be certain about this myself, I took my shark-obsessed 5-year-old to a local aquarium, where we spent 15 minutes trying to figure out how a friendly 3-foot dogfish, whose mouth looks like the coin slot of an old payphone, could do more than give a cable a soft boop.)
Experts also went out into the ocean and pulled different species of sharks onto the deck to force-feed them sections of cable.
Sometimes they bit—wouldn’t you?
But there was absolutely no pattern.

Still, in the 1980s, despite there being no firm evidence that sharks were attracted to anything specific about the cables, the teams decided it wouldn’t hurt to build TAT-8 with a layer of steel between the polyethylene insulation and the fibers.
They sent shark teeth to the NYU School of Dentistry, to have molds made and mounted onto shark jaw simulators, which then chomped on sections of cable.
The result was that lightweight deep-sea fiber was produced, from the start, with what they called “fish bite protection,” which helps against abrasions and other types of everyday damage that can happen in the sea.
Turns out, we owe sharks a thank-you, and probably an apology for the force-feeding.

IT’S MORNING IN Leixões.
On the deck of the Maasvliet, I hover over a pile of TAT-8’s repeaters.
A long-haul submarine telecommunications cable needs repeaters to boost the optical signal to cross the distance, and TAT-8 had more than 100 of them, each encased in a watertight, pressure-tested housing that could survive up to 8,000 meters down.
A rubberized cone stretches from each side of the repeater, sheathing the cable, making the whole piece about 2 meters long.
In a pile, they look like a dead kraken, ready for one last writhe on the dewy deck.

Repeaters weigh about 400 kilograms.
It takes three people to pull one out of the water, cut it free from the cable, and slide it down a special ramp onto the deck.
The rubber casings are stamped with the dates when each one rolled off the line—July 27, 1987, December 23, 1987, February 19, 1988, and so on—and there are identification numbers and instructions painted on them.
Human hands painted the casings before they went into the water 38 years ago, and it’s humans who pull them out, also with their hands.

TAT-8 cable joints strapped to the deck of the Maasvliet.
Photograph : Fiona Marron

Everything about the cable recovery operation needs to be learned on the job, from somebody who carries the knowledge in their body.
A lot of the new crew relies on Stephen, who has chosen to stay at the position of coiler, the rank of ordinary seaman, rather than rising up the ranks as many of the others have.
He’s been with Subsea for 15 years, since the company started, and he trains everyone.
He loves the teamwork and wouldn’t dream of going onto a cargo ship—too much waiting around.

At sea, it’s part of a coiler’s job to stand in the cable tanks in the ship’s hold and grab the cable as it comes through the hatch from the deck above.
You grasp it, and as the ship tosses, you walk backward in slow circles to coil the cable in a neat stack, because fiber cable has to be coiled by hand.
You need to keep it tight, and you don’t want to break the cable.
It’s hard to get used to, Stephen says, because you get dizzy.
Another coiler describes the shifts as 14 cigarettes long.
Eight hours divided into half-hour blocks so you don’t get too woozy: 30 minutes on, 30 minutes off, up the ladder for two cigarettes.

Peter, the operations manager, hands two pairs of utility gloves to Fiona and me.
Do we want to go into the hold? Fiona says yes instantly.
I take longer.
It’s 10 meters down a vertical ladder, but I didn’t travel here to just stand at the top of a ladder and shout “What’s it like down there?”


Peter in one of the cable tanks in the ship's hold.
Photograph : Fiona Marron


Recovered TAT-8 cable.
Photograph : Fiona Marron
 

Fiber-optic cables tend to be skinnier than people expect.
Photograph : Fiona Marron

The ship’s hold has five cable tanks, each about half full.
Most people are surprised when they see how small a submarine telecommunications cable is, but even those are usually the black and yellow steel-armored portions used in shallow water.
This cable, from the deep-sea sections, is the diameter of a taper candle, and it looks like giant cooked spaghetti.
I try to imagine being in here when it’s 30 degrees Celsius, the ship tossing up and down, and trying to walk in slow, backward circles.

Now I want to know how the cable gets from the seabed into the hold in the first place.
Stephen, again, is the person to ask.
He turns down the music—a mix of Ukrainian techno, American classic rock, and a medium dose of death metal—to tell me about what everyone here seems to agree is the most exciting part of cable recovery: catching the cable.

First, you sail to the spot where you’re pretty sure your cable is.
They have a route positioning list, a spreadsheet that shows the precise coordinates of every joint, splice, and repair—along with who did it.
They know where the cable has been plow-buried, where and exactly when a repeater was laid, and the type of cable at every section: double-armored, single-armored, lightweight-armored (the contemporary name for the “fish-bite-proofed” cables).
To take the cable off the seabed, all you get is a hook, a rope, those coordinates, and your senses.
It’s roughly the same method they used in the 19th century when they needed to recover failed telegraph cables from the deep sea.

A flat grapnel hook, known as a “flatfish,” is dropped off the bow.
It falls past blobfish, anglerfish, the giant versions of crab and octopus, and below the deepest-dwelling sharks, down where fish have antifreeze for blood and names like “fangtooth” and “faceless fish.” “When it touches the bottom,” Stephen says, “we stop.” They have to keep the hook flat on the bottom, so they can start what they call the cutting run, sailing slowly toward the cable, at a speed of about one knot, dragging the flatfish.
“The speed matters,” he says.
“When we get to the position, we slow down to keep it from flying or dancing.” 
Everything Stephen tells me sounds like trying to fly a kite in space, except this is all done on the deck of a ship, with ocean swells sometimes over 3 meters—if the swells hit 4, it’s too harsh to work.

Rope, ready to be lowered into the ocean to recover cable.
Photograph : Fiona Marron

Once the hook is in place, you have one job: Keep your eye on the line, watch for a bite.
Someone spots tension in the rope, or the winch makes a move.
Whoever sees it calls out.
Sometimes it’s been three hours, sometimes 24, of rope-dropping and winch-watching.
They cut, pull, start the bow roller and winch, and wait to find out if the flatfish has the right catch.
I repeat a question Fiona has been asking everyone: 
Do you cheer when you catch it?
Of course they do.

Captain Alex has been working with Subsea since its early days.
“In the beginning, I didn’t have any idea how to capture the cable on the ocean floor and bring it on board,” he says.
Cables weren’t laid to be picked up again.
“Sometimes it’s difficult to find.
The cable can shift from its initial position or be blocked by gravel or sand.”
They’re still figuring it all out.
As Subsea cofounder John Theodoracopulos puts it: “I liken a lot of what we do to cleaning up space junk or all the oxygen bottles that are left at base camp at Everest.”

Now that I’ve seen all the planning and experience that goes into an operation to find and recover a cable, it’s even harder to take seriously the idea that enemy saboteurs are regularly pulling this off.
A more legitimate concern is disturbing the seabed, but researchers at the UK’s National Oceanography Center have started looking into the environmental impact of decommissioning, and it’s not as much as you might think.
The biggest impact seems to come from grapnel runs and from the vessels themselves.
Very few cables in service today cross sensitive ocean habitats.
Where that’s the case, they leave those segments in place.
They also only recover cable that’s sitting on the surface of the seabed, and they know exactly where it all is because of that spreadsheet.
Cables don’t even tend to attract sea life colonization very often.
The “reef effect” makes a cool story, but it seems that, just like sharks, most sea life is just not that into cables.


Captains Vlad and Alex aboard the Maasvliet.
Photograph : Fiona Marron

DEPARTING CREW MEMBERS are starting to say their goodbyes.
Captain Vlad is passing out nuts and chocolate; Alex will do the formal handover later today.
Chief engineer Sergei is just about done with the maintenance work needed to hand over to the next chief engineer, also named Sergei.
He barrels through the bridge, beelining to the “good” coffee machine.
“This coffee machine is my wife!” he shouts.
He’s from Crimea, and he’s been a seaman on and off since he was 16.
It’s his hobby, the best job in the world.

In a few days, the cable tanks will be empty.
Next, a cargo ship will arrive.
The bales will be loaded “breakbulk,” as it’s called—directly into the hold, the way it was done before containerization—and brought to South Africa, to Mertech Marine, which also specializes in cable recovery, which Theodoracopulos tells me is a “collegial competitor.”
Mertech is the only cable salvage company with a recycling facility of its own.
It will break the cables down: steel, copper, two kinds of polyethylene.

One of the carousels that spin the cable into bales.
Photograph : Fiona Marron

Cables are stored below decks before coiling.
PHOTOGRAPH: FIONA MARRON


Fiber was the successor to copper, but that’s just the transmission part.
Fiber-optic cables still have plenty of copper in them, and it’s of especially high quality.
The International Energy Agency says we’ll be running short of copper within a decade if the manufacturing world can’t find more of it, so thousands of kilometers of it is nothing to sniff at.
The fiber itself is just about the only part of the cable that doesn’t make sense to recycle, but there’s lots of steel, and that will become things like game and vineyard fencing.
Polyethylene is one of the easiest plastics to recycle, and that will be sent to a facility in the Netherlands, where it will be turned into pellets that can be used for non-food-grade plastics.
By the time you read this, you could be squeezing your shampoo from the remnants of the first fiber-optic cable that crossed the Atlantic, most of which spent 38 years deeper in the sea than the Greenland shark, which is known for being centuries old and extremely sleepy.

And what about the rest of what went into the TAT fiber systems? Bell Labs was eventually sold to the French company Alcatel, which closed the Holmdel facility in 2006.
It spent close to a decade as the largest empty office building in America and is now a mixed-use complex called Bell Works, although it’s probably most recognizable as the headquarters of Lumon Enterprises in the Apple TV show Severance.
The current owners found 18 kilometers of subsea fiber from an early sea trial for TAT-8 in the basement, and they commissioned an architecture firm to come up with ideas for what to do with it, among them a giant slinky.
No one has used the old Ocean Simulation Lab for a production set, but you can also rent that—on a production location website, you’ll find it labeled a “mad scientist’s lair.”

Some of the TAT-8 people are still around because there are two things that keep people in the subsea business: They like people, and they love messy problems.
“Even way back then,” says Stafford, the Optican-1 project manager, “it was connecting the world, doing things right, doing things well.”
The contrast between this world and what’s happening at the application layer isn’t lost on me.
And the shark research makes a lot more sense—they had a big bet, a blank check, and an almost heroic sense of pride in their work that drove them to go down even vanishingly small rabbit holes.

I suppose there’s a third reason a lot of the people are still around: Most people in this tiny industry are Generation X or older, and sometimes they cart around so much institutional knowledge that they can’t retire.
Stafford is near retirement age, and the guy who introduced me to her, Jean Devos, got his start making telegraph cables in the north of France in 1961 and still works as an adviser.
He’s 87.
The first thing Stafford said to me on Zoom was, “How is he? Does he look well?”
The subsea world has been trying to recruit and train younger talent for at least the past decade, so the industry vets can get their rest.

Now it’s my turn to leave, so I’m climbing around the ship, saying my goodbyes, having a few last chats in the smoking area outside the crew quarters—where everyone is when they aren’t working.
I was promised a small piece of TAT-8, and now I have it.
Before I get to the airport, I wrap my cable bundle in a shirtdress and pack it in my carry-on, a little panicked as I realize it looks a lot like a bundle of dynamite.
The Subsea guys also gave me a branded baseball cap, which has a stylized cross-section of submarine cable on it.
I put it on in the airport, in case it can answer questions about what’s in my bag.
Except, how many people know what subsea cables look like?
And you can’t wear a hat through security, so it goes into the bucket.
Nobody asks any questions.

Wednesday, February 25, 2026

Primar reaches milestone proposing more than 25,000 vector nautical charts in the ENC world catalogue


3 years later, a new milestone for Primar with an increase of 25% in the number of active ENCs
(from 20,000 to 25,041 ENCs today from 81 countries)
 
see ENC worldwide coverage with GeoGarage Google Earth plugin
All these charts can be used under conditions with the GeoGarage platform
in webmapping or GIS applications for third parties in B2B mode

IHO member states
 
Existing ENC but non RENC,
 so not provided by Primar
mainly produced by TH Thailand & GB with associated countries
(dual-badge ENCs, so blocked by UKHO for Primar)
 

New analysis hints ancient explorers mapped Antarctic

A map that shows Antarctica nearly 300 years before it was discovered ?
In 1531, French mathematician and cartographer Orontius Finaeus published a world map that included a detailed southern continent resembling Antarctica.
What makes the map so unusual is that Antarctica would not be officially discovered until more than 300 years later.
Even more striking, the landmass is shown with rivers, coastlines, and internal features beneath what is now miles of ice.Some researchers have suggested the map may have been copied from far older source material, possibly preserved through lost charts or ancient geographic knowledge passed down through time.
Others argue the continent was drawn theoretically, based on the long-held belief that a southern landmass must exist to balance the world.Whether advanced guesswork or inherited knowledge, the map raises an uncomfortable question.
How was a continent drawn in such detail long before anyone was supposed to have seen it?
 
 
From NYTimes by Walter Sullivan
 
FOR years a few imaginative authors have argued, based on 16th century maps, that the ice-covered continent of Antarctica was discovered and mapped by an ancient civilization, perhaps one from another planet.
The latter proposition was dismissed by most geographers and historians as preposterous.

Nevertheless, a careful comparison of information appearing on the maps with what is now known of the continent has led a leading geologist and polar specialist to propose that the outlines of Antarctica may, in fact, have been known long before Columbus reached America.

The generally accepted view is that Antarctica was first sighted in 1820 by American seal-hunters as well as by British and Russian explorers.

The suggestion that it may have been discovered many centuries earlier has been made by Dr. John W. Weihaupt, vice chancellor for academic affairs at the University of Colorado at Denver.
His analysis appears as the lead article in the Aug. 28 issue of Eos, the Proceedings of the American Geophysical Union.

Dr. Weihaupt, a specialist in seismic and gravity studies and planetary geology, conducted research at a number of Antarctic stations beginning with the International Geophysical Year of 1957- 58.

Interviewed by telephone recently, Dr. Weihaupt was reluctant to speculate on how the rough outline of Antarctica might have become known to early mapmakers, saying he was not a maritime historian.
He suggested, however, that Bronze Age seafarers from the Mediterranean, trading along the east and west coasts of Africa, might have ventured farther south than previously believed.
 


A Peaking Period of Warming

From 2,600 to 9,000 years ago, he said, the world was warmer than at any time in the last million years, except for the period between the last two ice ages.

Polar ice was presumably reduced, making high latitudes more tempting to explore.

Dr. Weihaupt says that, assuming the outline of Antarctica was known to early cartographers, the source of their information ''remains unanswered.''
Even crude mapping of a large continent would require a knowledge of navigation and geometry presumably beyond the ken of primitive navigators.

Speculation on prehistoric discovery of Antarctica began in 1956, when a map of the Atlantic Ocean purportedly drawn in 1513 by a Turkish admiral named Piri Re'is was shown by a Navy cartographer to Arlington H. Mallery, an engineer.
Mr. Mallery was known for his thesis that Vikings reached American shores five centuries before Columbus.

The map supposedly contained information from voyages made by Columbus.
It showed the western bulge of Africa with considerable accuracy and what seemed a crude outline of the opposite coasts of the Americas.
Those coasts continued unbroken around the southern extremity of the Atlantic, where Antarctica's Queen Maud Land is now known to lie.

This was taken by Mr. Mallery as evidence that the continent at the bottom of the world was already known.
American cartographers had seen the map as early as 1932, but little attention had been paid to its possible implications regarding Antarctica.

Mr. Mallery's argument was picked up by Prof. Charles H. Hapgood, a historian at Keene Teachers College in New Hampshire.
Professor Hapgood had published a controversial book arguing that off-center accumulations of polar ice sometimes caused gradual, but radical changes in the axis of the earth.

His analysis of the Piri Re'is map was published in 1966 under the title ''Maps of the Ancient Sea Kings - Evidence of Advanced Civilization in the Ice Age.''
He also cited several other early maps upon which Dr. Weihaupt now bases his argument.

They are the Orontius Finaeus world map of 1531, the Gerhardus Mercator world map of 1538 and a map of the Americas produced by Ptolomaeus Basilae in 1540.

Professor Hapgood proposed that the Orontius Finaeus map showed the coast of Antarctica as it would appear if the continent were not covered with ice, as may have been the case between the last two ice ages.

The suggestion that Antarctica had been mapped by some civilization that thenvanished won few adherents among historians and geographers.

Two years after the book appeared, however, Erich von D"aniken, a Swiss hotel-keeper turned writer, carried the argument one large step further. In his book ''Chariots of the Gods?'' he proposed that the maps were derived from aerial views obtained by visitors from beyond the earth.

Dr. Weihaupt said he ignored the Piri Re'is map as of questionable authenticity.
He concluded, however, that the Orontius Finaeus and Mercator maps, through their resemblance to the actual outline of Antarctica, ''suggest that man's knowledge of that continent may date from a time somewhat earlier than that century,'' or at least three centuries before the continent's modern discovery.
 

A Modern and Complete Map of the World by the Royal Mathematician Oronce Fine of the Dauphiné.
LOC 
 
Virtually Complete Outline

Both maps show virtually the complete outline and details of a continent that, like Antarctica, is centered on the South Pole.

Generations of scholars have debated over who discovered Antarctica.
The American candidate has been Nathaniel Palmer, captain of a sealing sloop from Stonington, Conn. American and British sealers had begun hunting south of Drake Passage below Cape Horn and on Nov. 17, 1820, Palmer sailed farther south and may have sighted the tip of the Antarctic Peninsula.

The British candidate is Edward Bransfield of the Royal Navy, ordered to explore the area for an outpost to control the south side of that critical waterway between the Atlantic and Pacific.Britain gives Jan. 30, 1820, as the date of Bransfield's discovery.

Two weeks earlier two Russian ships under Adm. Thaddeus von Bellingshausen may have sighted the ice-covered Princess Martha Coast.

Multinational exploration of Antarctica and probing of its ice cover have now produced relatively complete maps of the continent as it would appear free of ice.

Deep fiords would exist where ice streams now reach the sea. An archipelago comparable to the Philippines would lie south of Drake Passage.
The Ross Ice Shelf, an apron of ice 1,000 feet thick and as large as France, would be an open gulf.

The Orontius Finaeus map shows such a gulf, suggesting the possibility it was free of ice at some prehistoric time.
Dr. Weihaupt cites polar specialists who suspect the Ross Ice Shelf may break up into icebergs and vanish if the climate warms and he proposes this may already have happened after the last ice age.

Some ancient Greek philosophers suggested that, to make the world symmetrical, there should be a large land mass at the South Pole to balance the northern continents.
Maps such as that of Orontius Finaeus were explained as flights of imagination based on such reasoning.
But Dr. Weihaupt finds the resemblance to what is now known of the continent, in terms of its size, outline and scattered mountain ranges to be striking.

''The geography of the southern continent,'' he concluded, ''may thus have been known in its broad configuration before the mid-16th century. While the evidence bodes thus, I have no hesitation in reminding the reader, as myself, of Sir Walter Raleigh's admonition that conjectures 'painted on Maps, doe serve only to mislead such discoverers as rashly believe them.' ''
 
Links :

Tuesday, February 24, 2026

Maritime boundary dispute between Ghana and Togo: causes, history, conflict risk, consequences, and scenarios




From RLI Robert Lansing Intitute
 
Ghana has formally notified Togo that it will pursue international arbitration under the United Nations Convention on the Law of the Sea (UNCLOS) to resolve a longstanding dispute over their maritime boundary in the Gulf of Guinea.
 
This move reflects deep-rooted historical disagreements, competing economic interests linked to offshore oil and gas rights, and frustration with failed bilateral negotiations.
By choosing a legal pathway, Accra aims to reduce tensions while preserving peace, but underlying strategic interests still carry the risk of future conflict if the arbitration outcome is contested.


 
Historical Background and Causes of the Dispute

Colonial Legacy and Ambiguous Borders

Like many African maritime disputes, the Ghana–Togo conflict has roots in colonial-era frontier demarcations.
Boundaries drawn by colonial powers in the late 19th and early 20th centuries often lacked precise geographical coordinates, especially offshore.
This ambiguity became more consequential as offshore energy resources gained economic importance.
 
 visualization of Ghana-Togo nautical chart with EEZ in the GeoGarage platform (SHOM raster chart)
 
Ghana Togo EEZ (GeoGarage platform)
 
The dispute centers on how to delimit a maritime boundary that defines sovereign rights over offshore oil, gas, and potentially mineral deposits in the Gulf of Guinea.

Trigger Points

The most salient flashpoint occurred in 2017–2018, when Togolese authorities prevented Ghanaian seismic survey vessels from conducting oil and gas exploration in waters Accra considered its own.
Ghana viewed this as an infringement on its sovereign rights, while Togo asserted competing claims over the same maritime area.

Following the 2017 incident, the two countries formed a Joint Maritime Boundary Technical Committee tasked with developing a mutually acceptable delimitation.
However, persistent differences in methodological approaches, baseline coordinates, and nautical chart interpretations prevented agreement.
Efforts at joint patrols, fishing coordination, and non-invasive exploration were negotiated, but these interim measures did not resolve the core boundary question.

Strategic Stakes and Underlying Drivers

Economic Interests: Oil and Gas Prospects

The disputed area lies offshore in a region with significant hydrocarbon potential.
For Ghana, energy exports have been central to economic growth; securing maritime rights expands access to exploration and production.
For Togo, securing equivalent rights is crucial for diversifying its economy and capturing revenue from offshore energy.
These competing economic imperatives heighten the stakes of any boundary resolution.

Institutional Limitations

Both Ghana and Togo have strong incentives to maintain peaceful bilateral relations, but domestic political considerations complicate compromise.
National pride and political constituencies tied to oil sector expansion make territorial concessions politically sensitive.

Why Arbitration? Possibility of Escalation

Shift to Legal Resolution

By invoking international arbitration under UNCLOS, Ghana is signaling both frustration with bilateral talks and a preference for rules-based settlement.
This move may reduce immediate tensions by placing the dispute in a neutral legal forum rather than a political or military arena.

Risk of Non-Compliance or Contestation

Arbitration results under UNCLOS are legally binding; however, there is no supranational enforcement mechanismother than diplomatic and reputational pressures.
If Togo perceives the outcome as unfavorable, Accra’s reliance on legal authority may still be challenged politically—especially if resource revenues are at stake.

Low Likelihood of Military Escalation—But Not Zero

Historical patterns in the Gulf of Guinea show that maritime disputes between neighbors rarely escalate into armed conflict, largely because of regional institutions (like the African Union) and shared economic interests in cooperative security.
However, localized incidents—such as naval confrontations or fishing vessel detentions—remain possible if either side interprets enforcement actions as provocative.


Consequences of Arbitration and Possible Outcomes
  • Scenario A: Arbitration Decides in Ghana’s FavorClear boundary line defined according to UNCLOS principles.
Ghana gains exclusive rights to the contested offshore area.
Increased investor confidence leads to accelerated oil and gas development.
Togo may attempt to negotiate side agreements for revenue sharing or joint concessions to maintain stability.

-> Implications:
Economic benefits for Accra are substantial.
However, domestic political pressure in Lomé may rise if Togo perceives limited access to resources.
  • Scenario B: Arbitration Favors Togo or Splits the DifferenceThe decision might allocate portions of the contested area to both states.
Togo could claim validation of its sovereign claims.
Ghana may push for shared resource exploitation frameworks.

-> Implications:
This could ease bilateral tensions if framed as fair, but risk domestic backlash in Accra if perceived as a loss.
Cooperative frameworks for exploration and production could emerge.
  • Scenario C: Arbitration Decision Is Contested or RejectedTogo might question the legal basis or fairness of proceedings.
Bilateral tensions could rise again.
Threat of localized maritime incidents increases.

-> Implications:
Renewed diplomatic tensions could undermine regional cooperation and investor confidence.
Third-party mediation by the African Union or United Nations may be required.

Broader Regional Context

African states increasingly face maritime boundary and resource disputes across the continent, particularly in the oil- and gas-rich Gulf of Guinea.
Regional institutions such as the Economic Community of West African States (ECOWAS) and the African Union (AU) have frameworks for peaceful dispute resolution, but practical implementation varies by case.

 
In september 2017, Ghana wins its maritime boundary case n°23 against Cote d’Ivoire when the Special Chamber (SC) of the International Tribunal for Law of the Sea (ITLOS) delivered its judgment
source : Foley Hoag 

Policy Implications and Recommendations
  • Strengthen UNCLOS Implementation: Encourage both states to commit in advance to abiding by arbitration results.
  • Establish Joint Resource Management Zones: Even if boundaries are agreed, mechanisms for shared exploitation can reduce competition and enhance cooperation.
  • Regional Mediation Support: AU and ECOWAS should offer facilitation services to ensure arbitration does not reignite tensions.
  • Transparency Measures: Regular public communication on proceedings can manage domestic expectations and reduce nationalist rhetoric.
The maritime dispute between Ghana and Togo reflects historic boundary ambiguities, economic competition for offshore resources, and frustrated bilateral diplomacy.
Ghana’s decision to seek international arbitration under UNCLOS is a strategic attempt to resolve the dispute within a rules-based framework, lowering the risk of escalation.
While military conflict remains unlikely, diplomatic, economic, and political tensions persist, and outcomes depend heavily on the arbitration ruling and its acceptance by both parties.
The situation underscores broader challenges in African maritime boundary governance and the need for robust regional mechanisms for peaceful dispute resolution.

Links :

Monday, February 23, 2026

Changes in ice volume : Cryosat maps ice volume loss in Antarctica and the Arctic


This animation shows changes in ice volume in Antarctica, Greenland and the Arctic ocean measured by the CryoSat satellite, 2010–15.
CryoSat’s readings also contribute to our knowledge of global ocean depth.

From BBC by Jonathan Amos 

European scientists have found a way to super-charge their study of the ice sheets in Antarctica and Greenland.

The novel technique boosts the data about height changes that are gathered by radar instruments on satellites.
Known as swath altimetry, it permits researchers to see broader regions of the ice sheets in any one pass overhead, and at a much finer scale.
Areas of melting or accumulation can now be investigated with 100 times more information.
The new approach has so far been applied only to a small set of data acquired by the Cryosat spacecraft.
But the intention eventually is to go back and reprocess the entire six-year archive of observations made by this European Space Agency (Esa) mission.
Swath altimetry will totally change the way scientists are able to study some phenomena, says Dr Noel Gourmelen from Edinburgh University, UK.
"The temporal and spatial improvements mean that if we have a surge in a glacier, it now makes it much easier to look at where that event initiated. Did the whole glacier start moving at once?
Or did the change start at the ocean, meaning the ocean was having an impact on the glacier?
Or perhaps it was further back, meaning different processes were involved.
Now, we're better able to trace the history and the causes of the surge," he told BBC News.
To be clear, swath altimetry changes nothing about how Cryosat operates - only in the way its data is processed.
The spacecraft already has a special radar designed to meet the peculiar challenges of observing ice sheets.
With its twin antennas, the instrument can work in an interferometric mode, detecting not just the distance to a spot below it on the ice but also the angle to that location.
Without this ability, it would struggle to map effectively the steep slopes and ridges found at the edges of the ice sheets - the very locations where recent melting and thinning have been most pronounced.

 Cryosat has just super-charged its ability to map the ice sheets

Broader brush

But even in this improved mode, standard data processing concentrates on the nearest radar echo return point and ignores much of the energy in the rest of the signal.
Swath processing, on the other hand, unpacks it all, revealing a line of additional elevation points.
It is now possible to see more of the shape of a depression or valley, not simply the rim or ridge that surrounds it. And because the "brush" of detection is much broader, it takes less time to "paint" the map of an ice sheet.
"We can now see detail that was simply not possible before," said Cryosat's principal scientific advisor, Prof Andy Shepherd.
"We can now map with about 500m spatial resolution the elevation and elevation change of Antarctica and Greenland, and other ice caps and glaciers across the globe."

The power of swath altimetry

The images below of the Petermann Glacier in northwest Greenland show the effect of standard processing versus the new swath approach. The latter pulls out far more elevation information from the radar signal.



The new swath mode has been a major talking point here in Prague at the European Space Agency's Living Planet Symposium, as has the the future of Cryosat itself.
Its radar measurements are highly valued, and are credited with having transformed studies of the Arctic, the Antarctic and Greenland.
But the mission is now operating beyond its design lifetime and could die in orbit at any time.
Researchers have urged Esa and the European Commission to find the means to fund a follow on.
Dr Andrew Fleming from the British Antarctic Survey said if its strand of information was lost with no suitable replacement, it would send many researchers "to bed in tears".
Outgoing Esa Earth observation director, Prof Volker Liebig, said there was no plan for a direct successor, and there was insufficient time to build one even if the money was available.
But the idea that the commission could launch a similar satellite in its Sentinel series of spacecraft in the 2020s was now being discussed, he added.
Prof Liebig said there was no denying the importance of a Cryosat capability, particularly in studying Arctic sea-ice.
"[Cryosat] is a mission that has a geopolitical meaning because the Arctic is the place that will change most in our lifetime as a result of climate change," he told the symposium.
"Plus two degrees [in temperature increase] worldwide means plus six degrees or even 10 degrees at the poles. I've even seen some statements of plus 15 degrees. And this means that by mid-century, in only 30 years from now, Arctic sea-ice will have disappeared completely in summertime."