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Lahar

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Encyclopedia of Natural Hazards

Part of the book series: Encyclopedia of Earth Sciences Series ((EESS))

Synonyms

Volcanic mudflow; Debris flow

Definition

A lahar is a flowing slurry of rock debris and water originating on the slopes of a volcano. The term may also mean the deposit of such a flow.

Discussion

Characteristics: Lahars contain grains from clay to large boulders. The flowing material is water-lubricated sand or mud, but the whole mixture maybe more than half of incorporated cobbles and boulders. Volumes can reach 109 m3 and peak discharge may exceed 107 m3/s. Depending on proportions of freshly erupted volcanic debris and snow or water, temperatures range from nearly 100°C to 0°C but are typically below 50°C. Flowing lahars peak swiftly and wane more slowly, passing any one place within minutes to a couple hours but sometimes lasting several hours.

Origin: Lahars can originate by eruption of hot fragmental debris onto snow or ice. A melting mass then flows swiftly downslope, incorporating more and more ash and rock from the volcano’s slopes. Some large lahars initiate from...

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Bibliography

  • Major, J. J., and Newhall, C. G., 1989. Snow and ice perturbation during historical volcanic eruptions and the formation of lahars and floods. Bulletin of Volcanology, 52, 1–27.

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  • Pierson, T. C., and Scott, K. M., 1985. Downstream dilution of a lahar – transition from debris flow to hyperconcentrated streamflow. Water Resources Research, 21, 1511–1524.

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  • Vallance, J. W., 2005. Volcanic debris flows. In Jakob, M., and Hungr, O. (eds.), Debris-Flow Hazards and Related Phenomena. Berlin: Springer, pp. 247–274.

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Correspondence to Richard B. Waitt .

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© 2013 Springer-Verlag Berlin Heidelberg

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Waitt, R.B. (2013). Lahar. In: Bobrowsky, P.T. (eds) Encyclopedia of Natural Hazards. Encyclopedia of Earth Sciences Series. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-4399-4_206

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