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History of Great Blue Hole

What a 'blue hole' is

In December 2018, a submarine descended to the bottom of the Great Blue Hole with Richard Branson and Jacques Cousteau's grandson aboard, broadcasting live for the whole planet. At 120 meters deep, where neither light nor oxygen reaches, they found stalactites formed when this was a dry cave, dead conchs… and plastic bottles. That perfect circular abyss, visible from space, is at once an archive of the Earth's climate and an uncomfortable mirror of our present. But let's start at the beginning: what exactly is a blue hole?

To understand the Great Blue Hole of Belize it's worth starting with the general phenomenon. A 'blue hole' is a type of marine sinkhole: a vertical cavity, generally with a circular mouth, that opens in the seabed and stands out for its dark blue color, much more intense than that of the turquoise, shallow waters that surround it. That color contrast, so well appreciated from the air, is due to the difference in depth: the very deep blue of the hole reveals that there the bottom drops suddenly by tens or hundreds of meters.

These sinkholes form in limestone terrain (karst relief), where water gradually dissolves the rock and creates underground caves and galleries. Blue holes exist in various places around the world, especially in the Caribbean, the Bahamas and the Red Sea, but the one in Belize is one of the largest, most perfect and most famous of all, to the point of becoming synonymous with the concept itself.

What's fascinating about Belize's Great Blue Hole is that its formation is tied to the great changes in sea level in the planet's recent geological history. It's not a whim of the landscape, but a natural archive: its walls and its internal formations hold the memory of when this area of the Caribbean was not underwater, but out in the open air. That history, written in the rock, is what makes it so special to geologists and divers alike.

Blue holes as karst sinkholes
The accepted definition describes blue holes as marine sinkholes formed in limestone, whose dark color contrasts with the surrounding shallow waters because of the greater depth. The one in Belize is one of the largest and best-known examples in the world.
Source: https://en.wikipedia.org/wiki/Blue_hole
Wikipedia (EN) — «Blue hole»: https://en.wikipedia.org/wiki/Wikipedia (EN) — «Great Blue Hole»: https://en.wikipedia.orgWikipedia (EN) — «Karst»: https://en.wikipedia.org/wiki/Kars

The geological formation: a cavern that the sea flooded

The history of the Great Blue Hole is, in reality, the history of the changes in sea level during the glaciations. During the great ice ages of the Quaternary, enormous masses of water were trapped in the glacial ice caps of the poles and continents, so the sea level was much lower than today. In those times, much of what is now the Lighthouse Reef atoll and its surrounding waters was not underwater, but solid ground exposed to the air.

In that dry landscape, over the limestone, rainwater gradually dissolved the stone and, over millennia, excavated a system of underground caves and caverns, like those we see today on solid ground in so many parts of the world. Inside those caves, stalactites (the formations that hang from the ceiling) and stalagmites formed, drop by drop, in a very slow process characteristic of dry karst environments.

When the glaciations ended and the ice melted, the sea level rose drastically, and the ocean flooded those lands and those caves. At some point, the roof of the great cavern collapsed, and the sea filled the void: thus was born the circular sinkhole we know today. The stalactites that divers contemplate suspended in the gloom, tens of meters deep, are the direct testimony of that terrestrial past: they formed in the dry, in a cave with air, long before the Caribbean covered them. The Great Blue Hole is, in that sense, a fossil of the landscape.

Collapse of a cavern and rise in sea level
The accepted geological explanation holds that the Great Blue Hole formed as a system of karst caves during periods of low sea level (glaciations); as the sea level rose after the glaciations, the caves flooded and the roof collapsed, leaving the stalactites underwater. The exact datings of the different phases are the subject of scientific study.
Source: https://en.wikipedia.org/wiki/Great_Blue_Hole
Wikipedia (EN) — «Great Blue Hole»: https://en.wikipedia.orgWikipedia (ES) — «Gran agujero azul»: https://es.wikipedia.oWikipedia (EN) — «Last Glacial Period»: https://en.wikipedia

The Lighthouse Reef atoll, its home

The Great Blue Hole is not isolated: it lies in the center of the Lighthouse Reef atoll, the easternmost of Belize's three coral atolls (along with Turneffe and Glover's Reef). An atoll is a ring-shaped coral formation that surrounds an inner lagoon, and Belize's are singular: unlike most atolls in the world (which form over ancient sunken volcanoes, especially in the Pacific), the Belizean ones sit over different geological structures, which makes them especially interesting for science.

Lighthouse Reef owes its name to the lighthouse on Half Moon Caye, one of its cayes. The atoll is home, besides the hole, to some of the most valuable natural corners of Belize: Half Moon Caye itself —the country's first natural monument, with its famous colony of red-footed boobies— and reefs of extraordinary health and beauty, highly sought after by divers from all over the world. The whole ensemble is protected and part of the Barrier Reef reserves.

The atoll's remoteness from the coast (about 70 km) explains why visiting it is always a full-day excursion and why its waters are among the best in visibility and best-conserved in the country. That same distance kept it relatively safe for centuries, making it a natural sanctuary in the middle of the Caribbean. The Great Blue Hole is the star, but the entire atoll that surrounds it is, as a whole, one of the natural treasures of Belize.

Belize's atypical atolls
Belize's three atolls (Lighthouse Reef, Turneffe and Glover's Reef) are usually described as atypical, since they didn't form over sunken volcanoes like most Pacific atolls, but over different geological structures, which makes them of special scientific interest. The precise geological details are still being researched.
Source: https://en.wikipedia.org/wiki/Lighthouse_Reef
Wikipedia (EN) — «Lighthouse Reef»: https://en.wikipedia.orgWikipedia (EN) — «Half Moon Caye»: https://en.wikipedia.org/Wikipedia (EN) — «Atoll»: https://en.wikipedia.org/wiki/Atol

Jacques Cousteau and worldwide fame (1971)

If the Great Blue Hole is today one of the most famous diving icons on the planet, much of the credit belongs to a legendary figure: the French explorer and oceanographer Jacques-Yves Cousteau. In 1971, Cousteau brought his legendary research ship, the Calypso, to the Lighthouse Reef atoll to explore and study the sinkhole, as part of his famous oceanographic expeditions that the world followed on television.

Cousteau and his team dived in the hole, mapped its shape and studied the formations of its interior, confirming the karst origin of the sinkhole from the stalactites found at depth. The expedition publicized the geological wonder of that blue abyss and, according to tradition, Cousteau included it among the best dive sites in the world, an endorsement that catapulted its international fame.

From then on, the Great Blue Hole went from being a geographical curiosity known above all to geologists and local fishermen to becoming a dream destination for divers around the world. Cousteau's media exposure transformed it into a brand, a tourist magnet and, over time, one of the visual symbols of Belize. It's a good example of how science communication can change the destiny of a place: that voyage of the Calypso in 1971 still brings travelers to the atoll half a century later.

The story had an almost cinematic sequel in December 2018, when an Aquatica Submarines expedition —with the oceanographer Erika Bergman as pilot, the businessman Richard Branson and Fabien Cousteau, Jacques's grandson, as crew members— descended to the bottom of the sinkhole in the Stingray 500 submarine, in a live broadcast on the Discovery Channel. Using sonar from the company Kongsberg, they produced the first complete three-dimensional map of the hole and confirmed that its last 30 meters are an anoxic zone, without oxygen and laden with hydrogen sulfide, where they found dead conchs, intact stalactites… and plastic bottles: a reminder that not even the most remote corner of the Caribbean escapes the human footprint.

The 1971 Calypso expedition
It's widely reported that Jacques Cousteau explored the Great Blue Hole with the Calypso in 1971 and contributed decisively to its worldwide fame, including it among the great dive sites. Some specific details of the expedition come from popular accounts and should be taken with caution.
Source: https://en.wikipedia.org/wiki/Great_Blue_Hole
Wikipedia (EN) — «Great Blue Hole»: https://en.wikipedia.orgWikipedia (EN) — «Jacques Cousteau»: https://en.wikipedia.orWikipedia (ES) — «Gran agujero azul»: https://es.wikipedia.o

UNESCO World Heritage (1996) and conservation

The international recognition of the value of the Great Blue Hole and its surroundings culminated in 1996, when UNESCO inscribed the Belize Barrier Reef Reserve System on the World Heritage list. This declaration does not protect a single point, but a set of seven marine protected areas that represent the best of the Mesoamerican Reef System in Belizean waters, and it includes the Lighthouse Reef atoll with the Great Blue Hole and the Half Moon Caye reserve.

UNESCO highlighted the exceptional value of this ecosystem: the second-longest coral reef in the world, with its atolls, reefs, mangroves and lagoons, home to an extraordinary marine biodiversity, which includes threatened species like sea turtles, manatees and the American crocodile. The Great Blue Hole, besides its beauty, adds to this ensemble a singular geological value as a window onto the planet's climatic past.

That World Heritage status carries the responsibility of conserving the site for future generations. The Belizean reef came to be included on the List of World Heritage in Danger due to threats like coastal development and oil exploration, until protective measures (among them a moratorium on oil activity in its waters) made it possible to remove it from that risk list. Today, visiting the Great Blue Hole also means understanding it as a fragile treasure: respecting the rules of the operators and the protected areas, not touching the coral or the formations and choosing responsible tourism is part of ensuring that this blue eye keeps amazing those who come after.

The 1996 inscription and the removal from the danger list
The Belize Barrier Reef Reserve System was inscribed as a UNESCO World Heritage Site in 1996 and includes Lighthouse Reef with the Great Blue Hole. The site was on the List of World Heritage in Danger until conservation measures (including an oil moratorium) made it possible to remove it. It's worth verifying the current status in official sources.
Source: https://whc.unesco.org/en/list/764/
UNESCO — «Belize Barrier Reef Reserve System» (#764): https:Wikipedia (EN) — «Belize Barrier Reef»: https://en.wikipediaWikipedia (EN) — «Great Blue Hole»: https://en.wikipedia.org

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