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DRRM
reporting 5.1-6.2
5.5
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Lahars
Wet cement-like mixture of volcanic material and
water
that flows down the slopes of a
volcano
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Lahar in Javanese
(an Indonesian dialect)
Lava or lava flow
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Lahars can form during
eruptive
episodes or during periods of
dormancy
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How
lahars
are generated
1. Intense
rainfall
during an eruption
2. Occurrence favors
stratovolcanoes
, tall and steep volcanoes, and those with weak or easily
erodible volcano
rock layer
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Types of lahar processes and deposits
Dilute
Streamflow (20 to >~60% vol, 40-80% wt.)
Hyperconcentrated
Streamflow (<20% vol., <40% wt.)
Debris
Flow (>~60% vol., >80% wt.)
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Lahars
Move as
fluid
masses with the general consistency of wet
concrete
Can cause serious
economic
and environmental damage to large floodplain areas, and to those affected by the severed
lifelines
Can destroy through direct impact of the
debris
,
logs
, and the flow itself
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Hazard
maps play an important role in identifying the location, magnitude and countermeasures to be undertaken during
volcanic
crises
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Taming lahars
1. Assess and designate
at-risk
areas
2. Investigate past history of lahars to form the bases of
predicting
the
size
and frequency of future lahars
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Lahar
Lava
or
lava
flow
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Lahar
Wet
cement-like mixture of volcanic material and water flowing down the slopes of a
volcano
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Lahars can travel at
high
speeds
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Lahars
can have a significant impact on the surrounding environment
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Effective dissemination of lahar hazard information
Educating
the local residents, local authorities, and local and national civil defense organizations
Coordination
between the lahar experts and emergency management agencies
Good monitoring and warning system should be in place to
alert
people early enough for them to
evacuate
to safe places
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Role of
water
in lahar
formation
Water
acts as a lubricant, allowing
volcanic
materials to flow more easily downhill
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Lahars
typically move quickly and pose significant
danger
to nearby communities
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