Lahar

A hot lahar rushes down a river valley in Guatemala near the Santa Maria volcano, 1989.

A lahar ( /ˈlɑːhɑːr/) is a type of mudflow or debris flow composed of a slurry of pyroclastic material, rocky debris, and water. The material flows down from a volcano, typically along a river valley.[1]

Lahars are extremely destructive: they can flow tens of metres per second (22 mph or more), be 140 metres (460 ft) deep, and destroy any structures in their path. Notable lahars include those at Mount Pinatubo and Nevado del Ruiz, the latter of which killed thousands of people.

The word lahar is the Javanese term for "flowing lava".

Description

A lahar is a volcanic mudflow or debris flow.[2] Lahars have the consistency, viscosity and approximate density of wet concrete: fluid when moving, solid at rest.[3] Lahars can be huge. The Osceola lahar produced by Mount Rainier (Washington) some 5,600 years ago resulted in a wall of mud 140 metres (460 ft) deep in the White River canyon, which covered an area of over 330 square kilometres (130 sq mi), for a total volume of 2.3 cubic kilometres (0.55 cu mi).[4]

A lahar of sufficient size and intensity can erase virtually any structure in its path, and is capable of carving its own pathway, making the prediction of its course difficult. Conversely, a lahar quickly loses force when it leaves the channel of its flow: even frail huts may remain standing, while at the same time being buried to the roof line in mud. A lahar's viscosity decreases with time, and can be further thinned by rain, but it nevertheless solidifies quickly when coming to a stop.

Lahars vary in size and speed. Small lahars less than a few metres wide and several centimetres deep may flow a few metres per second. Large lahars hundreds of metres wide and tens of metres deep can flow several tens of metres per second (22 mph or more): much too fast for people to outrun.[3] With the potential to flow at speeds up to 100 kilometres per hour (60 mph), and flow distances of more than 300 kilometres (190 mi), a lahar can cause catastrophic destruction in its path.[5]

Lahars from the 1985 Nevado del Ruiz eruption in Colombia caused the Armero tragedy, which killed an estimated 23,000 people, when the city of Armero was buried under 5 metres (16 ft) of mud and debris.[6] A lahar caused New Zealand's Tangiwai disaster,[7] where 151 people died after a Christmas Eve express train fell into the Whangaehu River in 1953. Lahars have been responsible for 17% of volcano-related deaths between 1783 and 1997.[8] A lahar can cause fatalities years after its precipitating eruption. For example, the Cabalantian tragedy occurred four years subsequent to the 1991 eruption of Mount Pinatubo.

The word lahar is of Indonesian origin.[9]

Causes

This mudline left behind on the trees on the banks of the Muddy River after the 1980 eruption of Mount St. Helens shows how high the lahars reached here.

Lahars have several possible causes:[3]

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.

Places at risk

The aftermath of a lahar from the 1982 eruption of Galunggung, Indonesia.

Several mountains in the world, including Mount Rainier in the United States, 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, are built on top of lahar deposits that are only about 500 years old. Lahars are predicted to flow through the valley every 500 to 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, Washington, so that people can flee an approaching debris flow in the event of a Mount Rainier eruption.

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

Since mid-June 1991, when violent eruptions triggered Mount Pinatubo's first lahars in 500 years, a system to monitor and warn of lahars has been in operation. Radio-telemetered rain gauges provide data on rainfall in lahar source regions, acoustic flow monitors on stream banks detect ground vibration as lahars pass, and manned watchpoints further confirm that lahars are rushing down Pinatubo's slopes. This system has enabled warnings to be sounded for most but not all major lahars at Pinatubo, saving hundreds of lives.[10] Physical preventative measures by the Philippine government were not adequate to stop over 20 feet (6.1 m) of mud from flooding many villages around Mount Pinatubo from 1992 through 1998.

Scientists and governments try to identify areas with a high risk of lahars based on historical events and computer models. Volcano scientists play a critical role in effective hazard education by informing officials and the public about realistic hazard probabilities and scenarios (including potential magnitude, timing, and impacts); by helping evaluate the effectiveness of proposed risk-reduction strategies; by helping promote acceptance of (and confidence in) hazards information through participatory engagement with officials and vulnerable communities as partners in risk reduction efforts; and by communicating with emergency managers during extreme events. [11]An example of such a model is TITAN2D. These models are directed towards future planning: identifying low-risk regions to place community buildings, discovering how to mitigate lahars with dams, and constructing evacuation plans.

Examples

Nevado del Ruiz

The lahar from the 1985 eruption of Nevado del Ruiz that wiped out the town of Armero in Colombia.

In 1985, the volcano Nevado del Ruiz erupted in central Colombia. As pyroclastic flows erupted from the volcano's crater, they melted the mountain's glaciers, sending four enormous lahars down its slopes at 60 kilometers per hour (40 miles per hour). The lahars picked up speed in gullies and coursed into the six major rivers at the base of the volcano; they engulfed the town of Armero, killing more than 20,000 of its almost 29,000 inhabitants.[12]

Casualties in other towns, particularly Chinchiná, brought the overall death toll to 23,000. Footage and photographs of Omayra Sánchez, a young victim of the tragedy, were published around the world. Other photographs of the lahars and the impact of the disaster captured attention worldwide and led to controversy over the degree to which the Colombian government was responsible for the disaster.

Mount Pinatubo

A before and after photograph of a river valley filled in by lahars from Mount Pinatubo.
Lahar flow on Mount Pinatubo

The 1991 eruption of Mount Pinatubo caused lahar flows: the first eruption itself killed six people, but the lahar flows killed more than 1500. The eye of Typhoon Yunya passed over the volcano during its eruption on June 15, 1991. The rain from the typhoon triggered the flow of volcanic ash, boulders, and water down the rivers surrounding the volcano. Angeles City was damaged by the volcano's sticky mud when Sapang Balen Creek and the Abacan River became the channel for the lahar and carried it to the heart of the city.

Over 6 metres (20 ft) of mud destroyed or damaged Castillejos, San Marcelino, Botolan, Porac, Mabalacat, Tarlac City, Capas, Concepcion, and Bamban. The mud flow down the Sacobia Bamban River scoured all structures in its path, including the bridges and dikes by the Parua river in Concepcion. The Tarlac River in Tarlac City was inundated by over 6 metres (20 ft) of lahar, causing the river to lose the ability to hold water.

On the morning of October 1, 1995, pyroclastic material which clung to the slopes of Pinatubo and surrounding mountains rushed down because of heavy rain, and turned into a 8-metre (25 ft) lahar. The mudflow killed hundreds of people in Barangay Cabalantian in Bacolor. The Philippine government under President Fidel V. Ramos ordered the construction of the FVR Mega Dike in an attempt to protect people from further mudflows.

Another typhoon-volcano lahar hit the Philippines in 2006; see Typhoon Reming.

See also

References

  1. ↑ "Lahar". USGS Photo Glossary. Retrieved 2009-04-19.
  2. ↑ Gerrard, John (1990). Mountain Environments: An Examination of the Physical Geography of Mountains. MIT Press. p. 209. ISBN 978-0262071284.
  3. 1 2 3  This article incorporates public domain material from the United States Geological Survey document: "Lahars and Their Effects". Retrieved 2012-08-23.
  4. ↑ Crandall, D.R. (1971). "Post glacial lahars From Mount Rainier Volcano, Washington". U.S. Geological Survey Professional Paper. 677.
  5. ↑ Hoblitt, R.P.; Miller, C.D.; Scott, W.E. "Volcanic Hazards with Regard to Siting Nuclear-Power Plants in the Pacific Northwest". U.S. Geological Survey Open-File Report. 87–297.
  6. ↑ "Deadly Lahars from Nevado del Ruiz, Colombia". USGS Volcano Hazards Program. Archived from the original on 2007-08-24. Retrieved 2007-09-02.
  7. ↑ "Lahars from Mt Ruapehu" (PDF). Department of Conservation (New Zealand). 2006. Retrieved 5 November 2016.
  8. ↑ Tanguy, J.; et al. (1998). "Victims from volcanic eruptions: a revised database". Bulletin of Volcanology. 60 (2): 140. doi:10.1007/s004450050222.
  9. ↑ Vallance, James W.; Iverson, Richard M. (2015-01-01). Sigurdsson, Haraldur, ed. Chapter 37 – Lahars and Their Deposits. Amsterdam: Academic Press. pp. 649–664. ISBN 978-0-12-385938-9.
  10. ↑  This article incorporates public domain material from the United States Geological Survey document: Chris Newhall, Peter H. Stauffer, and James W. Hendley II. "Lahars of Mount Pinatubo, Philippines".
  11. ↑ Pierson, Thomas C; Wood, Nathan J; Driedger, Carolyn L (2014-11-06). "Reducing risk from lahar hazards: concepts, case studies, and roles for scientists". Journal of Applied Volcanology. 3 (1). ISSN 2191-5040. doi:10.1186/s13617-014-0016-4.
  12. ↑ Schuster, Robert L.; Highland, Lynn M. (2001). "Socioeconomic and Environmental Impacts of Landslides in the Western Hemisphere". U.S. Geological Survey. Open-File Report 01-0276. Retrieved June 11, 2010.
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