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Qualibou, also known as the Soufrière Volcanic Center, is a 3.5 X 5 km-wide caldera on the island of Saint Lucia that formed between 32,000 and 39,000 years ago. This eruption also formed the Choiseul Tuff which covers the southeastern portion of the island.

Qualibou
View from Gros Piton over the Qualibou caldera
Highest point
Elevation777 m (2,549 ft)[1]
Coordinates13.838°N 61.046°W / 13.838; -61.046
Geography
Qualibou
Saint Lucia, Caribbean
Geology
Age of rock32-39,000 years
Mountain typeCaldera[2]
Last eruption1766

The Pitons are two large lava domes that formed 200 to 300,000 years ago, before the formation of the caldera; ever since then, other domes have filled the caldera floor. There was a phreatic eruption in 1766 that deposited ash over a wide area.

Sulfur Springs is an active geothermal area located roughly in the center of the caldera.

In 1990, 1999 and 2000 there were shallow volcanic earthquakes located 6 km ESE of the caldera.[3]




References


  1. This elevation is for Gros Piton, however Morne Gimie on the edge of the caldera has an elevation of 950 m.
  2. Global Volcanism Program, 1990. Report on Qualibou (Saint Lucia) (McClelland, L., ed.). Bulletin of the Global Volcanism Network, 15:5. Smithsonian Institution. DOI: 10.5479/si.GVP.BGVN199005-360140
  3. The University of the West Indies Seismic Research Centre (www.uwiseismic.com). "St Lucia".



На других языках


[de] Qualibou

Qualibou (auch: Soufrière Volcanic Centre) ist eine 3.5 × 5 km große Caldera auf der Insel Saint Lucia, die vor ca. 32–39.000 Jahren entstanden ist. Durch diese Eruption entstanden die Choiseul-Tuffe, die den Südosten der Insel bedecken.
- [en] Qualibou

[fr] Qualibou

Le Qualibou, aussi appelé Soufrière ou Soufrière de Sainte-Lucie[1], est un volcan de l'île de Sainte-Lucie constitué d'une caldeira en partie submergée par la mer des Caraïbes[2].



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