Pyroclastic flows in the context of "Plymouth, Montserrat"

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⭐ Core Definition: Pyroclastic flows

A pyroclastic flow (also known as a pyroclastic density current or a pyroclastic cloud) is a fast-moving current of hot gas and volcanic matter (collectively known as tephra) that flows along the ground away from a volcano at average speeds of 100 km/h (30 m/s; 60 mph; 90 ft/s) but is capable of reaching speeds up to 700 km/h (190 m/s; 430 mph; 640 ft/s). The gases and tephra can reach temperatures of about 1,000 °C (1,800 °F).

Pyroclastic flows are the deadliest of all volcanic hazards and are produced as a result of certain explosive eruptions; they normally touch the ground and hurtle downhill or spread laterally under gravity. Their speed depends upon the density of the current, the volcanic output rate, and the gradient of the slope.

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👉 Pyroclastic flows in the context of Plymouth, Montserrat

Plymouth is a ghost town and the de jure capital of the island of Montserrat, an overseas territory of the United Kingdom located in the Leeward Island chain of the Lesser Antilles, West Indies. It is the only ghost town that is the capital of a political territory.

Constructed during the Georgian era on historical lava deposits near the then long-inactive Soufrière Hills volcano, the town was evacuated in 1995 when the volcano resumed erupting. Plymouth was eventually abandoned permanently in 1997, after it was substantially buried by a series of pyroclastic flows and lahars.

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Pyroclastic flows in the context of Pyroclastic fall

A pyroclastic fall deposit is a uniform deposit of material which has been ejected from a volcanic eruption or plume such as an ash fall or tuff. Pyroclastic fallout deposits are a result of:

  1. Ballistic transport of ejecta such as volcanic blocks, volcanic bombs and lapilli from volcanic explosions
  2. Deposition of material from convective clouds associated with pyroclastic flows such as coignimbrite falls
  3. Ejecta carried in gas streaming from a vent. The material under the action of gravity will settle out from an eruption plume or eruption column
  4. Ejecta settling from an eruptive plume or eruption column that is displaced laterally by wind currents and is dispersed over great distances
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Pyroclastic flows in the context of Miravalles

The Miravalles Volcano is an andesitic stratovolcano in Costa Rica. The caldera was formed during several major explosive eruptions that produced voluminous dacitic-rhyolitic pyroclastic flows between about 1.5 and 0.6 million years ago. The only reported historical eruptive activity was a small steam explosion on the south-western flank in 1946. High heat flow remains, and Miravalles is the site of the largest developed geothermal field in Costa Rica.

The Miravalles Volcano reaches an elevation of 2,023 metres (6,637 ft) and is the highest mountain in the Guanacaste Mountains. The heat from the volcano also helps power a geothermal energy plant at Las Hornillas, which is run by the Institute of Electricity.

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Pyroclastic flows in the context of Mount Scenery

Mount Scenery (pronounced like the word '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. It is currently classified as "dormant", which means it is an active volcano that is not erupting now, but could erupt in the future. The last eruption was in or around the year 1640 and included explosions and pyroclastic flows. The most recent major eruption was at least 5,000 years ago. According to the U.S. Global Volcanism Program, Saba's volcano is the northernmost active volcano in the Caribbean.

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