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Mount Scenery

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Mount Scenery is a dormant volcano in the Caribbean Netherlands. Its lava dome forms the summit of the Saba island stratovolcano. At an elevation of 870 m (2,854 ft), it is the highest point in both the Kingdom of the Netherlands, and, since the dissolution of the Netherlands Antilles on 10 October 2010, the highest point in the Netherlands proper. The Saba volcano is potentially dangerous.

Saba (island)Saba (island)Saba is a Caribbean island and the smallest special municipality (officially "public body") of the Netherlands. It consists largely of the dormant volcano Mount Scenery, which at 870 meters (2,854.3 ft) is the highest point of the entire Kingdom of the Netherlands. The island lies in the northern Leeward Islands portion of the West Indies, southeast of the Virgin Islands.Cloud forestCloud forestA cloud forest, also called a water forest, primas forest, or tropical montane cloud forest, is a generally tropical or subtropical, evergreen, montane, moist forest characterized by a persistent, frequent or seasonal low-level cloud cover, usually at the canopy level, formally described in the International Cloud Atlas (2017) as silvagenitus.Kingdom of the NetherlandsKingdom of the NetherlandsThe Kingdom of the Netherlands, commonly known simply as the Netherlands, is a sovereign state consisting of a collection of constituent territories united under the monarch of the Netherlands, who functions as head of state. The realm is a unitary monarchy with its largest subdivision, the eponymous Netherlands, predominantly located in Northwestern Europe and with three smaller island territories located in the Caribbean.List of volcanoes in the CaribbeanList of volcanoes in the CaribbeanThis is a list of active and extinct volcanoes in the Caribbean, listed by country or territory.StratovolcanoStratovolcanoA stratovolcano, also known as a composite volcano, is a typically conicalvolcano built up by many alternating layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a summit crater and explosive eruptions. Some have collapsed summit craters called calderas. The lava flowing from stratovolcanoes typically cools and solidifies before spreading far, due to high viscosity.NetherlandsNetherlandsThe Netherlands, also informally known as Holland, is a country in Northwestern Europe, with overseas territories in the Caribbean. It is the largest of the four constituent countries of the Kingdom of the Netherlands. The Netherlands consists of twelve provinces and three overseas special municipalities. European Netherlands has land borders with Germany to the east and with Belgium to the south, and a coastline to the north and west.Caribbean NetherlandsCaribbean NetherlandsThe Caribbean Netherlands (Dutch: Caribisch Nederland, pronounced) is a geographic region of the Netherlands located outside Europe, in the Caribbean, consisting of three special municipalities. These are the islands of Bonaire, Sint Eustatius, and Saba, as they are also known in legislation, or the BES islands for short.Dissolution of the Netherlands AntillesDissolution of the Netherlands AntillesThe Netherlands Antilles was an autonomous Caribbean country within the Kingdom of the Netherlands. It was dissolved on 10 October 2010. After dissolution, the "BES islands" of the Dutch Caribbean—Bonaire, Sint Eustatius, and Saba—became the Caribbean Netherlands, "special municipalities" of the Netherlands proper—a structure that only exists in the Caribbean.Lava domeLava domeIn volcanology, a lava dome is a circular, mound-shaped protrusion resulting from the slow extrusion of viscouslava from a volcano. Dome-building eruptions are common, particularly in convergent plate boundary settings. Around 6% of eruptions on Earth form lava domes. The geochemistry of lava domes can vary from basalt (e.g. Semeru, 1946) to rhyolite (e.g. Chaiten, 2010) although the majority are of intermediate composition (such as Santiaguito, dacite-andesite, present day).VolcanoVolcanoRupture in a planet's crust where material escapesAugustine Volcano (Alaska) during its eruptive phase on January 24, 2006A volcano is a vent or fissure in the crust of a planetary-mass object that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and because most of Earth's plate boundaries are underwater, most volcanoes are found underwater.Global Volcanism ProgramGlobal Volcanism ProgramThe Smithsonian Institution's Global Volcanism Program (GVP) documents Earth's volcanoes and their eruptive history during the Quaternary Period of Earth's geologic history, with particular emphasis on volcanic activity during the Holocene Epoch (the last 11,700 years). The mission of the GVP is to document, understand, and disseminate information about global volcanic activity.Pyroclastic flowPyroclastic flowA pyroclastic flow, more broadly known as a pyroclastic density current, is a fast-moving current of hot gas and volcanic matter (collectively known as tephra) that flows along the ground away from a volcano. Pyroclastic currents travel at extremely high speeds and have extremely high temperatures. Pyroclastic flows are the deadliest of all volcanic hazards and are produced as a result of certain explosive eruptions.

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