Stone of Gela Alta

The Stone of Gela Alta is a meteorite buried beneath the ice of Gela Alta whose steady heat has formed a lake and an enclosed chamber within the glacier. The stone’s material properties are investigated across successive expeditions, but the evidence does not establish that it is alive. Instead, its heat, the Arctic worm associated with the site, and the prospect of a world-changing discovery become entangled with scientific uncertainty, commercial appetite, and the power of belief.

Discovery and Expeditions

The stone’s history reaches back to an expedition in the thirties, when Loyen came with a German party planning preliminary work for an airport on a narrow coastal strip. The expedition included Thule Inuit; people from West Greenland would not join because of the island’s bad reputation. Following Knud Rasmussen’s example of taking Inuit accounts seriously, Loyen found the meteorite. He returned in 1966 with Ving and Andreas Fine Licht. That party built a permanent passageway to the stone, but the expedition ended before they could solve the technical problems they faced. A later return in 1991 was also cut short, and Smilla’s group was forced to go home.

The earlier expeditions left physical traces of their work. In an underground room, gray ice covers laboratory instruments that appear to date from the 1960s or 1991: chromatographs, microscopes, crystallization jars, an incubator, and an electrophoresis apparatus. Tørk identifies the electrophoresis equipment as something Loyen brought in 1966, when the researchers still thought they were dealing with a form of organic life. The abandoned apparatus makes the history of inquiry tangible: the stone has repeatedly drawn scientists into the glacier, while each return inherits the unresolved questions and material remains of the last.

The Stone Beneath the Glacier

At the glacier’s ablation zone, a white rock knob interrupts the ice flow. Near it, the snow is stamped down where the ground slopes toward a crevasse, marking the place where Tørk had turned back to meet Smilla. Farther inside, the stone lies in the middle of a lake about a hundred feet across. The water is slightly milky with bubbles dissolving into the surrounding ice; the chamber has little water circulation and an apparent balance between freezing and melting. The place seems lifeless, apart from the heat coming from the stone.

The heat is not merely a theory: Tørk says the stone produces it, and that it melts the walls around it at a rate comparable to the glacier’s movement. The expedition examined cut-off fragments and found a mixture of iron, nickel, peridotite, magnesium, and silicates, with no unusual substance identified in them. Tests found no radioactivity. These observations establish notable physical effects and a recorded mineral composition, but do not settle whether the meteorite is alive or what produces its heat.

The Arctic Worm and Its Ecology

The stone’s setting is also the site of research into the Arctic worm, identified by Tørk as Dracunculus borealis, a large nematode parasite. In a laboratory beneath the ice, a specimen is observed in a water flea, Cyclops marinus. The flea has been treated with hydrochloric acid and is still beneath the microscope; what first looks like part of its digestive system is identified as a worm. Tørk describes the parasite’s established cycle in marine mammals: larvae enter water fleas, develop there over several weeks, and can reach a larger mammal when the flea is ingested. The worm matures in its host, mates, and the female moves beneath the skin to form a nodule and release larvae into the water. In this account, the parasite is well adapted to its hosts, which ordinarily are not seriously harmed.

Tørk contrasts that cycle with the Guinea worm, whose spread depends on environmental conditions such as heat and stagnant water. Smilla recognizes Chiang Rai as an example of a place where drought can make conditions favorable, while rainfall and flowing, cooler water impede the parasite. Tørk’s point is that host and parasite have developed in relation to one another: a successful parasite usually does not kill its host. The stone’s site becomes more alarming when research suggests that the Arctic worm may escape familiar ecological limits. Tørk reports that its larva has adapted to the human immune system, disguising itself with proteins from the person’s own body, and that its development in humans can accelerate from the much slower process observed in sea mammals.

Experiments further suggest that the worm can adapt to different fish, whether saltwater or freshwater, and across varying temperatures. Tørk interprets this as the absence of a key restriction on the parasite’s dispersal: a narrow range of transmitting hosts. Yet he also describes a remaining bottleneck. The parasite’s development in sea mammals is slow, and worms washed from lakes into the sea would have to survive until seals carried them farther. In his explanation, human beings could change that timescale, making the prospect of human infection central to the danger surrounding the stone.

Evidence, Interpretation, and Value

Tørk distinguishes the stone’s measurable properties from the story likely to be made about them. He argues that the stone need not actually be alive for people to believe that it is: ideas about life arising from inorganic matter have prepared an audience to interpret it as evidence, and belief and anticipation could make the stone seem alive regardless of its true nature. He expects the Arctic worm to be drawn into speculative accounts connecting the stone, inorganic life, and more complex organisms. The importance of that account, in his view, lies less in whether it is scientifically correct than in the forces of fear and hope it will unleash.

He also states his own material interest plainly: money and fame. The stone is valuable because of its size, its heat, and its association with the worm, and because it can be touched, cut, sold, photographed, and filmed. Its physical presence can be converted into a public spectacle and a marketable scientific discovery in a way that abstract findings cannot. Smilla consequently reads it as a symbol of Western science’s impulse to measure and possess the world, with the desire for money overriding empathy for living things. The danger is not only interpretive: transporting the worm to a densely populated region before its nature is understood could provoke a catastrophe if its numbers were previously held in check by the destruction of its hosts.

Significance

The Stone of Gela Alta remains materially specific and scientifically unresolved. Its fragments have an identified mineral mixture; its heat and its effect on the surrounding ice are reported; and organisms found in the glacial environment provide evidence for an unusual parasite. None of those facts proves that the stone itself is alive. The uncertainty is part of its power: it draws researchers into successive expeditions, furnishes a setting for claims about life and adaptation, and offers Tørk a prospect of wealth and renown.

The stone also concentrates the novel’s conflict over how knowledge is made and used. Laboratory instruments, observations, and samples can support particular claims, but those claims are then shaped by expectations, professional ambition, and commercial value. Tørk openly treats belief as a force that can make the stone real to the public, while Smilla sees in that process an attempt to turn an enigmatic natural object—and the organisms connected to it—into something that can be measured, owned, and sold. Its decisive significance therefore rests not on a confirmed revelation that it is alive, but on the consequences of acting as though it might be.