Mount Pelée in the context of Ludger Sylbaris


Mount Pelée in the context of Ludger Sylbaris

⭐ Core Definition: Mount Pelée

Mount Pelée or Mont Pelée (/pəˈl/ pə-LAY; French: la montagne Pelée [la mɔ̃taɲ pəle], lit.'bald mountain' or 'peeled mountain'; Antillean Creole: Montann Pèlé) is an active volcano at the northern end of Martinique, an island and French overseas department in the Lesser Antilles Volcanic Arc of the Caribbean. Its volcanic cone is composed of stratified layers of hardened ash and solidified lava. Its most recent eruption was in 1932.

The stratovolcano's 1902 eruption destroyed the town of Saint-Pierre, killing 29,000 to 30,000 people in the space of a few minutes, in the worst volcanic disaster of the 20th century. The main eruption, on 8 May 1902, left only three known survivors. Ludger Sylbaris survived because he was in a poorly ventilated, dungeon-like jail cell. Léon Compère-Léandre, living on the edge of the city, escaped with severe burns. The third was a young girl named Havivra Da Ifrile, who fled to a nearby sea cave in a boat, enduring burns from falling ash.

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Mount Pelée in the context of Martinique

Martinique (/ˌmɑːrtɪˈnk/ MAR-tin-EEK [maʁtinik] ; Martinican Creole: Matinik or Matnik; Kalinago: Madinina or Madiana) is an island in the Lesser Antilles of the West Indies, in the eastern Caribbean Sea. It was previously known as Iguanacaera which translates to 'Iguana Island' in Kari'nja. A part of the French West Indies (Antilles), Martinique is an overseas department and region and a single territorial collectivity of France.

It is a part of the European Union as an outermost region within the special territories of members of the European Economic Area, and an associate member of the CARICOM, the Organization of Eastern Caribbean States (OECS), the Association of Caribbean States (ACS), and the Economic Commission for Latin America and the Caribbean (ECLAC) but is not part of the Schengen Area or the European Union Customs Union. The currency in use is the euro. It has been a UNESCO Biosphere Reserve since 2021 for its entire land and sea territory. In September 2023, the volcanoes and forests of Mount Pelée and the peaks of northern Martinique, in particular the Pitons du Carbet, were listed as UNESCO World Heritage Sites.

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Mount Pelée in the context of Lateral eruption

A lateral eruption or lateral blast is a volcanic eruption which is directed laterally from a volcano rather than upwards from the summit. Lateral eruptions are caused by the outward expansion of flanks due to rising magma. Breaking occurs at the flanks of volcanoes making it easier for magma to flow outward. As magma is pushed upward towards the volcano it diverges towards the flanks before it has a chance to erupt from the crater. When the expanding flank finally gives it releases a flow of magma. More explosive lateral eruptions are referred to as lateral blasts. Some of the most notable examples of a lateral eruption include Mount St. Helens, Mount Pelée, and Mount Etna.

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Mount Pelée in the context of Lesser Antilles Volcanic Arc

The Lesser Antilles Volcanic Arc is a volcanic arc that forms the eastern boundary of the Caribbean Plate. It is part of a subduction zone, also known as the Lesser Antilles subduction zone, where the oceanic crust of the North American Plate is being subducted under the Caribbean Plate. This subduction process formed a number of volcanic islands, from the Virgin Islands in the north to the islands off the coast of Venezuela in the south. The Lesser Antilles Volcanic Arc includes 21 'active' volcanoes, notably Soufriere Hills on Montserrat; Mount Pelée on Martinique; La Grande Soufrière on Guadeloupe; Soufrière Saint Vincent on Saint Vincent; Mount Scenery on Saba; and the submarine volcano Kick 'em Jenny which lies about 10 kilometres (5.4 nmi) north of Grenada.

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Mount Pelée in the context of 1902 eruption of Mount Pelée

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.

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Mount Pelée in the context of Léon Compère-Léandre

Léon Compère-Léandre (1874?–1936) was a Martiniquais shoemaker in Saint-Pierre on the French Caribbean island of Martinique when Mount Pelée erupted on May 8, 1902, and destroyed the town. He was one of only two (arguably three) known survivors.

His own description of the morning of May 8, 1902, follows.

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