The Disaster ArchiveThe Disaster Archive
6 min readChapter 3Americas

Catastrophe

The eruption at Galeras came with the kind of violence that turns a summit into a killing ground. On the morning of 14 January 1993, the mountain’s danger was not abstract, nor distant, nor confined to a plume on the horizon. It struck the people already on top of the volcano, where the difference between warning and impact could be measured in steps and fractions of a second. In that instant, the normal logic of retreat failed. There was no long approach of smoke and no leisurely escalation that would have given the group time to reorganize. The eruption came as an explosive release from the vent area, sudden enough to overwhelm the field party before escape could be coordinated.

At the crater rim, the body of the event was ballistic. Hot blocks of rock were hurled outward with lethal force, and the blast carried ash, gases, and fractured debris into the narrow summit zone. This was the most unforgiving kind of volcanic violence: a pressure release that transformed the crater’s edge from an observation point into an impact zone. In a volcanic accident of this type, the mechanics are mercilessly simple. The vent opens, pressure drops, fragments accelerate, and those nearby have no real shelter. Helmets and field gear can protect against smaller hazards, but they do not stop high-velocity blocks or a sudden cloud of superheated material. The mountain’s geometry made the danger worse. The crater lip, which had served as a place to look inward and measure the volcano, became the place where visibility, mobility, and survival all collapsed at once.

Ground-level accounts from the disaster reconstruct a scene of confusion and instantaneous harm. Researchers and assistants who had been moving across the summit were forced to react in a landscape that offered almost no cover. The eruption did not arrive as a distant spectacle; it arrived in the middle of the work. That matters in the forensic reading of the event. Galeras was not a disaster that began far away and advanced toward a settled population. It was a close-range eruption, one that overtook a small scientific party already positioned in the most dangerous terrain on the volcano. Some survivors later described the problem not as a long tragedy but as a compressed one: a shift in the mountain, then the eruption itself, then injury, separation, and the struggle to get away.

The human cost was concentrated, and that concentration is part of what made the catastrophe so difficult to absorb. The eruption did not devastate a city or bury a broad region under ash. Instead, it focused death around a handful of people conducting fieldwork at the summit. The smaller statistical footprint should never be mistaken for a smaller moral one. Among the dead were internationally known volcanologists and local participants whose role had been to support the scientific mission. The fatal logic of the eruption did not distinguish between credentials and proximity. In this setting, the difference between expert and assistant mattered far less than the difference between being on the crater rim and being off it.

Official and later scientific reconstructions generally agreed on a crucial point: the 1993 eruption was not a massive caldera-forming event or a prolonged eruptive episode. It was a relatively small explosive outburst from an active summit. Yet the scale of the eruption did not determine the scale of the loss. What made Galeras so important in hazard discussions was exactly this mismatch. It demonstrated that an eruption need not be large to be deadly, and that summit exposure can shift from accepted risk to fatal exposure in the time it takes to hear the volcano change tone. The event became a warning not because it was unprecedented in volcanic physics, but because it exposed how fast field assumptions can fail when the volcano decides the terms.

The physical destruction at the summit was followed by the immediate consequences of trauma. Those struck by blocks or caught in the blast had little time for organized self-rescue. The summit terrain itself compounded the injury. Loose ash reduced footing, gas irritated lungs and eyes, and the descent became difficult precisely when speed mattered most. In volcanic disasters, the first blast is often followed by a second layer of danger created by the mountain’s altered surface. The same routes that had carried the team upward now had to be negotiated in shock, with damaged equipment, obscured vision, and injured bodies moving downhill under unstable conditions. The eruption therefore did not end at the crater rim. It continued in the struggle to leave.

The event is especially sobering because of the gap between the scale of the mountain and the scale of the killing. Galeras was, and remained, a volcano visible to people in Pasto, part of the region’s landscape and daily awareness. Yet on 14 January 1993 it became, for a small group at the summit, a site of concentrated loss. That contrast is central to the disaster’s historical meaning. It shows how a familiar volcano can become fatal without warning to those closest to it, and it shows how scientific familiarity is not the same as safety. The death of scientists under observation also struck the scientific community with unusual force, because it challenged a core assumption: that expertise, instrumentation, and planning could always keep fieldwork within acceptable danger.

The summit event was so abrupt that its aftermath had to be assembled from fragments: the condition of the crater area, the injuries sustained, the position of survivors, and the sequence by which the party tried to withdraw. The eruption did not last forever, but it lasted long enough to kill. Once the immediate blast had passed, the mountain had been altered, the expedition broken, and the survivors forced into descent under the pressure of shock and uncertainty. Below them, the volcano still loomed over the city, its dangers not erased by the explosion. The next phase of the disaster had already begun: the race to locate the missing, account for the injured and dead, and determine how a scientific ascent into an active crater had turned, in seconds, into a catastrophe at close range.