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Morne Watt

Watt, Morne

Estratovolcán · Dominica · 1224 m

Fumarolic clouds mark the Valley of Desolation and Boiling Lake thermal areas, NE of Morne Watt (Watt Mountain) volcano in SE Dominica.  The Valley of Desolation and the Boiling Lake are major tourist attractions within the national park east of Roseau.  A major eruption from Morne Watt produced pyroclastic flows about 930 years ago.  The only historical eruptions on the island of Dominica were a moderately large phreatic explosion at the Valley of Desolation thermal area in 1880 and a smaller phreatic explosion in July 1997.
Fumarolic clouds mark the Valley of Desolation and Boiling Lake thermal areas, NE of Morne Watt (Watt Mountain) volcano in SE Dominica. The Valley of Desolation and the Boiling Lake are major tourist attractions within the national park east of Roseau. A major eruption from Morne Watt produced pyroclastic flows about 930 years ago. The only historical eruptions on the island of Dominica were a moderately large phreatic explosion at the Valley of Desolation thermal area in 1880 and a smaller phreatic explosion in July 1997. · Foto: Photo by Paul Jackson, 1998 (Seismic Research Unit, University of West Indies). · Wikimedia Commons
Tipo
Estratovolcán
País
Dominica
Región
Middle America-Caribbean Volcanic Regions / Lesser Antilles Volcanic Arc
Altitud
1224 m
Coordenadas
15.307, -61.305
Última erupción
1997
Contexto tectónico
Subduction zone / Oceanic crust (< 15 km)
Forma volcánica
Composite
Roca principal
Andesite / Basaltic Andesite
Resumen geológico

Morne Watt (Watt Mountain) volcano lies SE of the Trois Piton/Micotrin lava-dome complex in SE Dominica, E of the capital city of Roseau. The two best-known volcanic features on Dominica, the Valley of Desolation and the Boiling Lake thermal areas, lie on the flank; both are major tourist attractions within the national park. Morne Anglais stratovolcano lies 4 km SW of Morne Watt. Soufrière Hills volcano, with dated pyroclastic-flow producing eruptions ~10,000 years ago, lies 3 km E. A major eruption from Morne Watt producing pyroclastic flows occurred ~1300 years ago. A moderately large phreatic explosion took place at the Valley of Desolation thermal area NE of Morne Watt in 1880, when ash fell over a 4-km-wide sector at the coast, 10 km from the vent. A smaller phreatic explosion occurred in July 1997, when ashfall was confined to the Valley of Desolation area. These mark the only known historical eruptions on the island.

Resumen de Wikipedia

Morne Watt es un estratovolcán en el sur de la isla de Dominica. Se eleva a una altitud de 1.224 m y es el tercer pico más alto en Dominica. Una gran erupción del Morne Watt que produjo flujos piroclásticos tuvo lugar hace unos 1300 años. Una erupción freática moderadamente grande tuvo lugar en el Valle de la Desolación en la zona termal al NE de Morne Watt en 1880, cuando la ceniza volcánica cayó sobre un sector de 4 km de ancho en la costa, a 10 km de la rejilla de ventilación.

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Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
1800 BCE~1600 BCE · 1 erupciones · VEI máx. ?1001 BCE~801 BCE · 1 erupciones · VEI máx. ?598~798 · 1 erupciones · VEI máx. ?1797~1997 · 2 erupciones · VEI máx. 21800 BCE801 BCE1 BCE9981797

Línea de tiempo detallada

  1. 1997VEI 1Observado
    1997-07-15 – 1997-07-15
    NE of Watt Mtn (Valley of Desolation)
  2. 1880VEI 2Observado
    1880-01-04 – 1880-01-04
    NE of Watt Mtn (Valley of Desolation)
  3. 640 (±150 años)VEI ?Estimación geológica
    640 – En curso
    West flank of Morne Watt
  4. 950 a. C. (±300 años)VEI ?Estimación geológica
    BCE 950 – En curso
    NE of Watt Mtn (Valley of Desolation)
  5. 1800 a. C. (±100 años)VEI ?Estimación geológica
    BCE 1800 – En curso
    NE of Watt Mtn (Valley of Desolation)

Enlaces externos

⚠ Solo como referencia. No apto para respuesta ante emergencias.