Kamis, 16 Juni 2011

DEFINITION OF LAHAR

Volcanic mudflows are known as lahars, some of

which have killed tens of thousands of people in single

events. When pyroclastic flows and nuée ardentes move into

large rivers, they quickly cool and mix with water, becoming

fast-moving mudflows. Lahars may also result from the

extremely rapid melting of icecaps on volcanoes. A type of

lahar in which ash, blocks of rock, trees, and other material

is chaotically mixed together is known as a debris flow. Such

lahars and mudflows were responsible for much of the burial

of buildings and deaths from the trapping of automobiles

during the 1980 eruption of Mount Saint Helens. Big river

valleys were also filled by lahars and mudflows during the

1991 eruption of Mount Pinatubo in the Philippines, resulting

in extensive property damage and loss of life. One of the

greatest volcanic disasters of the 20th century resulted from

the generation of a huge lahar when the icecap on the volcano

Nevado del Ruiz in Colombia catastrophically melted

during the 1985 eruption. Nevado del Ruiz entered an active

phase in November 1984 and began to show harmonic

tremors on November 10, 1985. At 9:37 P.M. that night, a

large Plinian eruption sent an ash cloud several miles into the

atmosphere, and this ash settled onto the ice cap on top of

the mountain. This ash, together with volcanic steam, quickly

melted large amounts of the ice, which mixed with the ash

and formed giant lahars down the east side of the mountain

into the village of Chinchina, killing 1,800 people. The eruption

continued and melted more ice that mixed with more ash

and sent additional larger lahars westward. Some of these

lahars moved nearly 30 miles (48 km) at nearly 30 miles per

hour (48 km/hr) and buried the town of Armero under 26

feet (8 m) of mud, killing 23,000 people in Armero and surrounding

communities.

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