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ranking hazardous volcanoes_internet lab
ranking hazardous volcanoes_internet lab

... mudflows are common volcanic hazards. An explosive volcano may not be a hazard to human life and property, however, if it is located in a remote area or erupts infrequently. A number of factors must be taken into account to determine if a particular volcano poses a risk. Problem: Which volcanoes on ...
File
File

... the surface of the earth. When pressure builds up, eruptions occur. Gases and rock shoot up through the opening and spill over or fill the air with lava fragments. Eruptions can cause lateral blasts, lava flows, hot ash flows, mudslides, avalanches, falling ash and floods. Volcano eruptions have bee ...
76 Volcanism and Igneous Processes I. Introduction A. Volcanism
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... Composite cones or Strato Volcano- Volcanos comprised of a mixture or alternating layers of lava and pyroclastic material, generally form large Volcanos, often associated with violent eruptions (e.g. MT. St. Helens) and andesitic magmas (sl. more siliceous than basalt). a. ...
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... • Fiery pyroclastic flow made of hot gases infused with ash and other debris • Move down the slopes of a volcano at speeds up to 200 km per hour – May produce a lahar, which is a volcanic mudflow ...
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... Cinder cone volcanoes are smaller than shield volcanoes and composite volcanoes. If the eruption contains thick magma, the gas pressure shatters the rock within the volcano into small pieces. In other cases, the lava in the air may harden and fall as fragments. These small pieces are called cinders. ...
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... Volcano: a weak spot in the _______________ where molten material or _______________ comes to the surface Magma: a molten mixture of ________ forming substances, ________ and H2O from the mantle Volcanic Belts: Form along the Earth’s _______________ boundaries o The boundaries _______________ or Div ...
Volcano Glossary III
Volcano Glossary III

... Light, porous volcanic rock formed during explosive eruptions as dissolved carbon dioxide is erupted with the magma. Pumice is composed of a network of bubbles and volcanic glass and minerals. Pumice can be formed from all types of magma. ...
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Nevado del Ruiz



The Nevado del Ruiz (Spanish pronunciation: [neβaðo ðel ˈrwis]), also known as La Mesa de Herveo (English: Mesa of Herveo (the nearby town)), or Kumanday in the language of the local pre-Columbian indigenous people, is a volcano located on the border of the departments of Caldas and Tolima in Colombia, about 129 kilometers (80 mi) west of the capital city Bogotá. It is a stratovolcano, composed of many layers of lava alternating with hardened volcanic ash and other pyroclastic rocks. Nevado del Ruiz has been active for about two million years, since the early Pleistocene or late Pliocene epoch, with three major eruptive periods. The current volcanic cone formed during the present eruptive period, which began 150 thousand years ago.The volcano usually generates Plinian eruptions, which produce swift-moving currents of hot gas and rock called pyroclastic flows. These eruptions often cause massive lahars (mud and debris flows), which pose a threat to human life and the environment. The impact of such an eruption is increased as the hot gas and lava melts the mountain's snowcap, adding large quantities of water to the flow. On November 13, 1985, a small eruption produced an enormous lahar that buried and destroyed the town of Armero in Tolima, causing an estimated 25,000 deaths. This event later became known as the Armero tragedy—the deadliest lahar in recorded history. Similar but less deadly incidents occurred in 1595 and 1845, consisting of a small explosive eruption followed by a large lahar.The volcano is part of Los Nevados National Natural Park, which also contains several other volcanoes. The summit of Nevado del Ruiz is covered by large glaciers, although these have retreated significantly since 1985 because of global warming. The volcano continues to pose a threat to the nearby towns and villages, and it is estimated that up to 500,000 people could be at risk from lahars from future eruptions.
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