00:00In the spring of 1902, the island of Martinique ceased to exist as it had been known,
00:07not from a slow geological process, not from centuries of incremental change,
00:14but in under two minutes on the morning of May 8th,
00:18when Mount Pellee discharged a superheated avalanche of gas and fragmented,
00:24rock traveling at roughly 670 kilometers per hour directly into the city of St. Pierre.
00:32The temperature at the floe's interior exceeded 700 degrees Celsius.
00:38Of the 30,000 people in the city that morning, fewer than a handful survived.
00:44The harbor, full of ships, was incinerated.
00:47The event was over before anyone on the outer islands understood what had happened.
00:54That was not the only eruption in 1902.
00:58That same year, Santa Maria in Guatemala exploded in one of the largest Plinian eruptions of the 20th century,
01:08driving ash to an altitude of 28 kilometers and burying agricultural land under meters of tefra.
01:15Sufriri on St. Vincent erupted the day before Pellee, killing over a thousand people.
01:24Three catastrophic eruptions on three separate volcanoes.
01:28In a single calendar year, a 2022 paper published in the Journal of Applied Volcanology
01:36attempted something ambitious, a systematic ranking of volcanic disaster years going back four centuries.
01:43Using standardized fatality records, eruption magnitude classifications,
01:50and secondary hazard data, including tsunami events and post-eruptive famine.
01:56The methodology is careful.
01:58The authors acknowledge the data degrades significantly before the 19th century.
02:04But the patterns that emerge are sobering and, in some respects, counterintuitive.
02:121902 ranks among the worst by direct mortality, somewhere between 35,000 and 40,000 dead, depending on the source.
02:22But raw fatalities alone do not define a catastrophic volcanic year.
02:28The ranking considers cascading effects, disease, crop failure, displacement, and the collapse of regional infrastructure.
02:37By that metric, several years in the analysis outrank, 1902 in total human consequence.
02:48The single most destructive volcanic year in recorded history, by most composite measures,
02:55is likely 1815, anchored by the eruption of Tambora on the island of Sumbawa in the Dutch East Indies.
03:04A Plinian eruption that ejected approximately 150 cubic kilometers of material,
03:11collapsed a caldera roughly 6 kilometers across,
03:15and drove a stratospheric aerosol veil that cooled the northern Hennesphere by 0.5 to 1 degree Celsius over the
03:26following year.
03:281816 became known as the year without a sun volcanic material into the Bismarck Sea.
03:35The resulting tsunami reached heights of 15 meters on nearby coastlines and killed somewhere between
03:432,000 and 3,000 people.
03:47The event predates instrumental monitoring.
03:51What volcanologists now understand is that Ritter Island was the preserved scar of a sector collapse,
03:58the same process, on a smaller scale.
04:02That has been modeled at Cumberville, at Etna.
04:06At Mauna Loa, volcanic tsunamis are the hazard most consistently underestimated in public,
04:12risk communication dot in 1979.
04:16Ding Plateau in central Java produced a phreatic eruption,
04:21driven not by fresh magma,
04:23but by superheated groundwater flashing to steam,
04:27that released a pulse of carbon dioxide and hydrogen sulfide gas.
04:32The gas cloud traveled downslope and asphyxiated 149 people,
04:38who were attempting to evacuate.
04:40No lava, no pyroclastic flow,
04:44no ash column reaching the stratosphere,
04:48a gas release from a hydrothermal system,
04:51and 149 people dead.
04:55That is what the data from the worst volcanic years actually shows,
05:00stripped of spectacle.
05:01The most dangerous eruptions are not always the largest.
05:06They are the unexpected ones,
05:08the ones from systems assumed to be stable,
05:11the ones where the hazard arrives in a form no one was watching for.
05:16The Earth does not issue warnings in forms we always recognize.
05:21It issues them in forms it always has
05:24pressure, gas, deformation, heat,
05:28and whether those signals are read in time is,
05:31historically, the only variable that has ever made a difference.
05:35it is going to be a number of
05:35we are going to stop.
05:35We are going to express our members
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