stylistic:style_transfer, structural:scholar_edition
The 1902 eruption of Mount Pelée was a volcanic eruption on the island of Martinique in the Lesser Antilles Volcanic Arc of the eastern Caribbean, which was one of the deadliest eruptions in recorded history. Eruptive activity began on 23 April as a series of phreatic eruptions from the summit of Mount Pelée. Within days, the vigor of these eruptions exceeded anything witnessed since the island was settled by Europeans. The intensity then subsided for a few days until early May, when the phreatic eruptions increased again. Lightning laced the eruption clouds and trade winds dumped ash on villages to the west. Heavy ash fell, sometimes causing total darkness. Some of the afflicted residents panicked and headed for the perceived safety of larger settlements, especially Saint-Pierre, about 10 km (6.2 mi) south of Pelée's summit. Saint-Pierre received its first ash fall on 3 May. Mount Pelée remained relatively quiet until the afternoon of 5 May when a mudflow swept down a river on the southwest flank of the volcano, destroying a sugar mill. The massive flow buried about 150 people and generated a series of three tsunamis as it hit the sea. The tsunamis swept along the coast, damaging buildings and boats. The explosions resumed the night of 5 May. The following morning, parts of the eruption plume became incandescent, signifying that the character of the eruption had changed. The phreatic eruptions had finally given way to magmatic eruptions as magma reached the surface. These eruptions continued through the next day and night. A brief lull was shattered by a tremendous eruption at about 8:00 a.m. on 8 May. A ground-hugging cloud of incandescent lava particles suspended by searing turbulent gases called a pyroclastic surge moved at hurricane speed down the southwest flank of the volcano, reaching Saint-Pierre at 8:02 a.m. Escape from the city was virtually impossible. Almost everyone within the city proper—about 28,000 people—died, burned or buried by falling masonry. The hot ash ignited a firestorm, fueled by smashed buildings and countless casks of rum. One survivor within the city was a clueless prisoner who was locked in a windowless underground jail cell, later being discovered by rescue workers. The only other survivors were a few tens of people caught within the margins of the cloud, who were all badly burned. Explosive activity on 20 May resulted in another 2,000 deaths as rescuers, engineers and mariners brought supplies to the island. A powerful eruption on 30 August generated a pyroclastic flow that resulted in over 800 people killed. The eruption continued until 5th October 1905.