About 15,000 years ago, in the place where today a diver descends to see stalactites hanging under the sea, you could walk without wetting your feet: the bottom of the present Great Blue Hole of Belize was a dry limestone cavern, kilometers inland from a coast very different from today's. That's the key to understanding Lighthouse Reef, the most remote and spectacular of Belize's three coral atolls, along with Turneffe and Glover's Reef: nothing in its current geography —the reef ring, the turquoise lagoon, the deep-blue circle in its center— is accidental. It all responds to a geological history of ice, sea and coral written over millennia.
An atoll is a ring- or horseshoe-shaped coral reef formation that surrounds a central lagoon. The classic image of the atoll —a ring of coral crowned by sand cayes, enclosing shallow turquoise waters— is the result of a geological process that extends over millennia.
Most of the world's atolls formed over the edges of ancient sunken volcanoes, according to the model that the naturalist Charles Darwin proposed in the 19th century: the coral grows on the contour of a volcanic island and, as it slowly sinks, the reef keeps growing upward to stay near the surface, until the island disappears and only the ring of coral with its lagoon remains. However, the Caribbean atolls, like those of Belize, have a somewhat different origin: they don't sit over volcanoes, but over foundations of limestone and ancient geological faults, on which the coral grew as the sea level rose after the last glaciation.
Lighthouse Reef is the easternmost of the Belizean atolls and lies outside the main barrier reef, in deep Caribbean waters. Its distance from the coast —about 80 kilometers— and from sources of sediment and pollution is one of the reasons its reefs remain in such good condition. The reef ring encloses a lagoon of clear, shallow waters, dotted with sand banks and a few cayes, among them Half Moon Caye at the southern end.
At the heart of Lighthouse Reef opens the Great Blue Hole, an almost perfect circle of dark-blue water more than 300 meters across and about 124 deep. Although today it's a marine cavity, its origin is terrestrial: the Blue Hole is an ancient limestone cave, a sinkhole, that formed when this area was not underwater.
During the Pleistocene glaciations, tens of thousands of years ago, much of the planet's water was trapped in the polar ice caps and the sea level was much lower than today. What is now the bottom of the Lighthouse Reef lagoon was then solid limestone ground. The slightly acidic rainwater gradually dissolved the limestone and excavated a system of underground caves. Over time, the roof of one of those great caverns collapsed, leaving an open sinkhole.
When the glaciations ended and the sea level rose again, the ocean flooded the sinkhole and turned it into the underwater blue hole we know. The proof of its dry past is the enormous stalactites that hang from its walls from 30 meters deep: these formations can only be created by dripping water in a cave with air, not underwater, which confirms that at some point it was a terrestrial cavern. Studies of the stalactites and the bottom sediments have allowed scientists to reconstruct ancient climatic episodes of the region.
The waters around Lighthouse Reef have a long human history. Long before the arrival of the Europeans, the Maya plied the coast of Belize in canoes, trading products like salt, cacao, obsidian and jade objects along extensive maritime routes that connected the Yucatán Peninsula with the rest of Mesoamerica. The cayes and reefs served as reference points and, in some cases, as stops in that trade network.
After the conquest, the western Caribbean became a scene of Spanish colonial navigation and, above all, of the activity of pirates, buccaneers and smugglers who found ideal hideouts in the labyrinths of reefs and cayes of Belize. The English (the 'Baymen', cutters of logwood and mahogany) settled in the region from the 17th century. The reefs far from the coast, like Lighthouse Reef, were at once a refuge and a deadly trap: many ships wrecked upon crashing into the coral in poorly charted waters.
Precisely to warn of that danger, in the 19th century a lighthouse was built on Half Moon Caye, the caye at the southern end of the atoll. That lighthouse is the one that gave the whole formation its name: 'Lighthouse Reef'. The tower was for a long time one of the few signs of human presence in this remote corner of the Caribbean, guiding navigators away from the coral shoals.
Although local fishermen and navigators had known the blue hole for generations, the Great Blue Hole became famous around the world thanks to the celebrated French explorer and oceanographer Jacques-Yves Cousteau. In 1971, Cousteau brought his famous research ship, the Calypso, to Lighthouse Reef to explore and map the Blue Hole as part of his underwater documentaries.
Cousteau's team carried out dives and soundings that revealed the depth of the hole and, above all, the spectacular stalactites that hang from its inner walls, the proof of its past as a terrestrial cavern. Cousteau declared the site one of the ten best dive sites in the world, a distinction that catapulted the Blue Hole to international fame and made it a dream destination for divers around the planet.
Since then, the Great Blue Hole appears in countless documentaries, reports and lists of natural wonders. In later decades, new scientific and technological expeditions —including the use of submersibles and high-resolution sonar— explored it again, producing three-dimensional maps of its interior and studying the oxygen-free layer of water that occupies its bottom, where sediments and, according to the findings, even remains of ancient dives are preserved. The aura Cousteau gave it remains intact: diving the Blue Hole is, for many, a dream come true.
The extraordinary natural value of Lighthouse Reef led to its legal protection over the course of the 20th century. The key milestone came in 1982, when Half Moon Caye was declared a Natural Monument, becoming one of the first protected areas in Belize. The measure sought to protect the important colony of red-footed boobies that nests on the caye —one of the few large colonies of this species in the Western Hemisphere— along with the frigatebirds, the sea turtles that nest on its beaches and the surrounding reef.
The management of Half Moon Caye was placed in the hands of the Belize Audubon Society, a pioneering conservation organization in the country, which manages several of Belize's most important protected areas. On the caye a bird observation platform, trails and a small station were installed, and rules were established so that tourism and research could coexist with conservation.
The greatest recognition came in 1996, when UNESCO inscribed the Belize Barrier Reef Reserve System on the World Heritage list. This site groups a series of protected areas along the Belizean reef —the second-largest reef system in the world after the Australian Great Barrier— and includes the Natural Monuments of the Blue Hole and Half Moon Caye, on Lighthouse Reef. The distinction recognizes the universal value of these ecosystems and commits Belize to protecting them. In recent years, the site was on the List of World Heritage in Danger due to threats like oil prospecting and coastal development, until the conservation measures adopted by the country made it possible to remove it from that list, a case cited as an example of recovery.