Eisspeedway

Lahar: Difference between revisions

Content deleted Content added
No edit summary
No edit summary
Line 4: Line 4:
[[Image:MSH82 lahar from march 82 eruption 03-21-82.jpg|thumb|220px|Lahar from a March 1982 eruption of [[Mount St. Helens]].]]
[[Image:MSH82 lahar from march 82 eruption 03-21-82.jpg|thumb|220px|Lahar from a March 1982 eruption of [[Mount St. Helens]].]]
[[Image:Volcanoevacuationroute.jpg|thumb|An evacuation Route sign in case of volcanic eruption or lahar.]]
[[Image:Volcanoevacuationroute.jpg|thumb|An evacuation Route sign in case of volcanic eruption or lahar.]]
A '''lahar''' is a type of [[mudflow]] composed of [[pyroclastic]] material and [[water]] that flows down from a [[volcano]], typically along a [[river]] [[valley]]. The term 'lahar' originated in [[Indonesia]].
A '''lahar''' is a type of [[mudflow]] composed of [[pyroclastic]] material and [[water]] that flows down from a [[volcano]], typically along a [[river]] [[valley]]. The term 'lahar' originated in the [[Javanese language]] of [[Indonesia]].


Lahars have the consistency of [[concrete]]: fluid when moving, then solid when stopped. Lahars can be huge: the Osceola lahar produced 5,600 years ago by [[Mount Rainier]] in [[Washington]] produced a wall of mud 180 m (600 feet) deep in the [[White River (Washington)|White River]] canyon and extends over an area of over 320 km².
Lahars have the consistency of [[concrete]]: fluid when moving, then solid when stopped. Lahars can be huge: the Osceola lahar produced 5,600 years ago by [[Mount Rainier]] in [[Washington]] produced a wall of mud 180 m (600 feet) deep in the [[White River (Washington)|White River]] canyon and extends over an area of over 320 km².

Revision as of 01:59, 31 July 2007

Lahar from a March 1982 eruption of Mount St. Helens.
File:Volcanoevacuationroute.jpg
An evacuation Route sign in case of volcanic eruption or lahar.

A lahar is a type of mudflow composed of pyroclastic material and water that flows down from a volcano, typically along a river valley. The term 'lahar' originated in the Javanese language of Indonesia.

Lahars have the consistency of concrete: fluid when moving, then solid when stopped. Lahars can be huge: the Osceola lahar produced 5,600 years ago by Mount Rainier in Washington produced a wall of mud 180 m (600 feet) deep in the White River canyon and extends over an area of over 320 km².

Lahars can be extremely dangerous, because of their energy and speed. Large lahars can flow several dozen meters per second and can flow for many kilometres, causing catastrophic destruction in their path. The lahars from the Nevado del Ruiz eruption in Colombia in 1985 killed an estimated 21,000 in the city of Armero, buried under 8 m (26 ft) of mud and debris. The 1953 Tangiwai disaster in New Zealand was caused by a lahar.

Lahars have several possible causes:

In particular, although lahars are typically associated with the effects of volcanic activity, lahars can occur even without any current volcanic activity, as long as the conditions are right to cause the collapse and movement of mud originating from existing volcanic ash deposits.

Several mountains in the world, including Mount Rainier in the USA, Mount Ruapehu in New Zealand, and Galunggung in Indonesia, are considered particularly dangerous due to the risk of lahars. Several towns in the Puyallup River valley in Washington state, including Orting, the closest to Mount Rainier, are built on top of lahar deposits that are only about 500 years old. Lahars are predicted to flow through the valley every 500-1,000 years, so Orting, Sumner, Puyallup, Fife, and the Port of Tacoma face considerable risk. The USGS has set up lahar warning sirens in Pierce County, so that people can flee an approaching debris flow.

A lahar warning system has been set up at Mount Ruapehu by the New Zealand Department of Conservation and hailed a success after it successfully alerted officials to an impending lahar on 18 March 2007.

The 1991 Mount Pinatubo eruption caused lahar as well, but it was due to the passing of a major typhoon over the Philippines which resulted in a torrent of volcanic ash and water down to the rivers surrounding the volcano. The Lahar was caused by the mixing of settled ash and water from the monsoon which occurred the day after the volcano finished erupting. Although the eruption only killed 6 people, 1500 were killed in the resulting lahar, showing the destructive nature of lahars.

See also