What plate boundaries is Mount Pelee on?

What plate boundaries is Mount Pelee on?

Mount Pelee is the result of a subduction zone. It lies in Martinique where the Caribbean Plate and the South American Plate form a convergent boundary. This is the result of compression. The boundary near Mount Pelee is an oceanic:oceanic convergent plate boundary.

Is Mt Pelee on a subduction zone?

Mount Pelée is the result of a typical subduction zone. The subduction formed the Lesser Antilles island arc, a curved chain of volcanoes approximately 850 kilometres (530 mi) in length, between Puerto Rico and Venezuela, where the Caribbean Plate meets Atlantic oceanic crust belonging to the South American Plate.

Where was Mount Pelee located?

island of Martinique
Mount Pelée is a stratovolcano that forms the north end of the French island of Martinique, along the Lesser Antilles subduction zone.

What plate is Cotopaxi on?

Formed by the subduction of the Nazca plate underneath the South American plate, Cotopaxi has risen 19,000 ft tall, making it one of the tallest and most dangerous volcanoes around the world.

What type of plate boundary is Mount Vesuvius?

convergent boundary
Vesuvius is at a convergent boundary where the African plate is being subducted meaning one tectonic plate is moving under another.

What is the width of Mount Pelee?

about 100 to 150 m
To date, this was the last fatal eruption of Mount Pelée. Beginning in October 1902, a large volcanic spine grew from the crater floor in the Étang Sec crater, reaching a maximum width of about 100 to 150 m (300 to 500 ft) and a height of about 300 m (1,000 ft).

What type of lava comes out of Mount Pelee?

Mount Pelée The lava is a pasty one, because really rich in silica. It cannot flow out of the crater and piles up there , often forming a dome spiked with needles.

What specific plate boundary is Cotopaxi sitting on?

Cotopaxi is part of the Cordillera’s Northern Volcanic Zone, the volcanism a product of the subduction of the Nazca Plate underneath the South American Plate.

How did Mount Pelee form in the Caribbean?

Mount Pelée is on the boundary of the North America Plate and the Caribbean Plate. The North America Plate subducted under the Caribbean Plate, and the magma produced when the crust subducted rises to the surface and forms a chain of volcanic islands. Martinique, and subsequently, Mount Pelée, were formed this way.

What kind of subduction zone is Mount Pelee?

Mount Pelée is the result of a typical subduction zone. The subduction formed the Lesser Antilles island arc, a curved chain of volcanoes approximately 850 kilometres (530 mi) in length, between Puerto Rico and Venezuela, where the Caribbean Plate meets Atlantic oceanic crust belonging to the South American Plate.

What kind of volcano is Mt Pelee in Martinique?

Mt. Pelee, a stratovolcano made mostly of pyroclastic rocks, is on the north end of the island of Martinique. Martinique is part of the Lesser Antilles volcanic arc. The arc is formed by the subduction of the North American Plate under the Caribbean Plate.

Where is Mount Pelee in the Lesser Antilles?

Mount Pelée ( /pəˈleɪ/ pə-LAY; French: Montagne Pelée [mɔ̃taɲ pəle], meaning “bald mountain” or “peeled mountain”) is a volcano at the northern end of Martinique, an island and French overseas department in the Lesser Antilles island arc of the Caribbean. Its volcanic cone is composed of stratified layers…