Table of Contents
What type of plate boundary is Mt 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.
Where is Mt Pelee found?
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 continent is Mount Pelee in?
Caribbean
Mount Pelée, French Montagne Pelée, active volcanic mountain on the Caribbean island of Martinique. Situated 15 miles (24 km) northwest of Fort-de-France, it reaches an elevation of 4,583 feet (1,397 metres).
Is Mount Pelee on a plate boundary?
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. The boundary near Mount Pelee is an oceanic:oceanic convergent plate boundary. These boundaries form island arcs, much like the island arc Lesser Antilles.
Is Mount Pelée acting up?
Current status. The volcano is currently active. A few volcano tectonic earthquakes occur on Martinique every year, and Mount Pelée is under continuous watch by geophysicists and volcanologists (IPGP).
How long did the 1902 Mount Pelee eruption last?
Heavy ash fall at times caused 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….
| 1902 eruption of Mount Pelée | |
|---|---|
| Start date | April 23, 1902 |
| End date | October 5, 1905 |
| Type | Phreatic, Peléan |
What type of eruption does Mount Pelee have?
Stratovolcano
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….
| Mount Pelée | |
|---|---|
| Mountain type | Stratovolcano |
| Volcanic arc/belt | Lesser Antilles Volcanic Arc |
| Last eruption | 1929–1932 |
| Climbing |
Why was Mount Pelee formed in a subduction zone?
Tectonic Plates• Mount Pelee was formed in a subduction zone.That is when an oceanic crust (in this case theCocos plate) collides with continental crust (Caribbean plate), the continental crust is pushedover the oceanic crust, since it is lighter.
Where is Mount Pelee located in the Caribbean?
Mount Pelée is on the northernend of the French Caribbeanisland Martinique.• Mount Pelée is the result of asubduction zone. Thesubduction formed the LesserAntilles island arc, a curvedchain of volcanoesapproximately 850 kilometres (530 miles) in length, betweenPuerto Rico and Venezuela.Tuesday, June 11, 2013
What are the different phases of Mount Pelee?
Geological history. Volcanologists have identified three different phases in the evolution of Mount Pelée volcano: initial, intermediate, and modern. In an initial phase, called the “Paléo-Pelée” stage, Mount Pelee was a common stratovolcano.
How big is the Tower of Pelee volcano?
In October 1902 (post eruption) a pillar ofcooled lava arose, which was pushed up bythe pressure in the volcano. This lavadome, called the tower of Pelée, was 100to 150 metres wide. At the top the domewas approximately 300 metres above theedge of the crater. The tower was notstable enough and in september 1903 itcollapsed.Tuesday, June 11, 2013 3.