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Monte Scenery

Saba

Estratovolcán · Netherlands · 887 m

Mt. Scenery, the summit lava dome of Saba volcano, is seen from the airport on the NE side of the island.  The sun-dappled slopes in the foreground are the surface of a large andesitic lava flow that descends the NE flank of the volcano and forms the Flat Point Peninsula, on which the airport was constructed.  A steep switch-backed road extends from the airport to the village of Lower Hells Gate (center).  Saba is the northernmost active volcano of the West Indies.
Mt. Scenery, the summit lava dome of Saba volcano, is seen from the airport on the NE side of the island. The sun-dappled slopes in the foreground are the surface of a large andesitic lava flow that descends the NE flank of the volcano and forms the Flat Point Peninsula, on which the airport was constructed. A steep switch-backed road extends from the airport to the village of Lower Hells Gate (center). Saba is the northernmost active volcano of the West Indies. · Foto: Photo by John Shepherd, 2000 (Seismic Research Unit, University of West Indies). · Wikimedia Commons
Tipo
Estratovolcán
País
Netherlands
Región
Middle America-Caribbean Volcanic Regions / Lesser Antilles Volcanic Arc
Altitud
887 m
Coordenadas
17.630, -63.230
Última erupción
1640
Contexto tectónico
Subduction zone / Oceanic crust (< 15 km)
Forma volcánica
Composite
Roca principal
Andesite / Basaltic Andesite
Resumen geológico

Saba, the northernmost active volcano of the West Indies, is a 5-km-diameter island forming the upper half of a large stratovolcano that rises 1,500 m above the sea floor. Its eruptive history is characterized by the emplacement of lava domes and associated pyroclastic flows. The summit, known as Mount Scenery (or The Mountain), is a Holocene lava dome that overtops a major collapse scarp that formed about 100,000 years ago. Flank domes were constructed on the SW, SE, E, and NE sides of the island near the coast. A large andesitic lava flow entered the sea on the NE flank, forming the Flat Point Peninsula. The village of The Bottom overlies pyroclastic-surge deposits that contain European pottery fragments and were radiocarbon dated at 280 +/- 80 years before present. The village was settled in 1640 CE on grassy meadows on the volcano's flanks reflecting initial vegetation recovery following destruction of tropical rainforests by pyroclastic flows and surges. Lava dome growth may also have occurred during this SW-flank eruption.

Resumen de Wikipedia

El monte Scenery es un volcán potencialmente activo en el Caribe de los Países Bajos. Su cúpula de lava forma la cumbre de la isla estratovolcán de Saba, un municipio especial neerlandés. Con una altura de 887 m, es el punto más alto, tanto en el Reino de los Países Bajos, como, desde la disolución de las Antillas Neerlandesas el 10 de octubre de 2010, el punto más alto en los Países Bajos propiamente dicho.

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Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
1640~1640 · 1 erupciones · VEI máx. ?16401640164116411641

Línea de tiempo detallada

  1. 1640VEI ?Observado
    1640 – En curso
    SW flank

Enlaces externos

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