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Physical Process

Lahar

Tectonics and Volcanism

A destructive flow of volcanic debris, ash and water that rushes down a volcano's slopes and valleys with the speed and consistency of wet concrete, triggered when an eruption rapidly melts snow and ice, or when heavy rain mobilizes loose volcanic ash. Lahars can travel far beyond the volcano itself and have caused some of the deadliest volcanic disasters in history, including the 1985 Armero tragedy in Colombia.

Facts
Process Type
Geomorphological 1
Timescale
flows several tens of metres per second and can exceed 200 kilometres per hour on steep slopes 1
First Proposed Year
1922 1
Connections

Associated With

Caused By

Sources
1. Lahar - Wikipedia
  • Description section, opening definition
    a violent type of mudflow or debris flow composed of a slurry of pyroclastic material, rocky debris and water.
  • Description section, speed paragraph
    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. On steep slopes, lahar speeds can exceed 200 kilometres per hour (120 mph).
  • Etymology section
    Berend George Escher introduced it as a geological term in 1922.
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