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June
25, 2007 Engineers at MIT
have devised a simple yet
effective system for determining an area's landslide risk, a tool that
could
help planners improve building codes, determine zoning and strengthen
mitigation measures in mountainous tropical regions frequently hit by
typhoons. Devised originally
for "The system could
be applied directly to
any country with similar topography, geology and climate, which would
be much
of The two report in
the May 2007 issue of
Engineering Geology that the new landslide risk rating system is
especially
applicable to many areas of the developing world, where a detailed
landslide
risk analysis has not previously been performed, because the system is
based on
characteristics that can be assessed in the field or from available
records. "The fact that the
The area is
becoming increasingly more
populous and built-up, in part because it sits at a higher elevation
and has
cooler temperatures than most of the country, making it a popular
tourist destination.
The average annual rainfall for the city on the Landslides occur
when earthquakes or heavy
rains loosen layers of surface soil. Surface soils in tropical and
subtropical
areas tend to be residual--that is, they're created when the underlying
bedrock
deteriorates--rather than sedimentary, which is soil that has been laid
down by
flowing water or wind, said Einstein, whose research focuses on rock
mechanics,
engineering geology and risk analysis of tunnels and landslides. In the
To prepare their
hazard ratings, the
researchers mapped the seven types of underlying bedrock in the area,
overlaid
with data on slope inclination and vegetation growth. Some of their
findings
are a bit counterintuitive, Saldivar-Sali explained. For instance,
steeper
slopes don't necessarily indicate greater landslide risk. "What we found
didn't follow any kind of
predictable pattern," she said. "The conclusion we reached is that
the landslide hazard is determined by a combination of two factors: the
underlying bedrock and the slope." They found that landslides are less
common in areas with limestone bedrock, even though they may be
relatively
steep. "Limestone is a very hard rock that forms steep slopes
naturally.
So the steep slope is the stable condition for this rock," she said. While roughly half
of the 50-square-kilometer
area rests on bedrock from the Pliocene Baguio Formation, only 5.7
percent of
landslides occur in these areas, and more than half of those took place
on
moderate slopes. Broadleaf trees provided the least amount of
protection on
this type of bedrock. But in general, a mix of broadleaf trees or
bushes and
scrub provided the most protection. The highest
incidence of landslides in the
area (14.3 percent) occurs on bedrock from the oldest geologic era
represented,
the Cretaceous Pugo Formation of volcanic rock, which accounts for only
1.4
square kilometers of the total area. The researchers
assumed uniformity in heavy
rainfall associated with typhoons and underground faults, because these
are
common to the study area. But the system could be easily adapted to a
region
where that consistency does not hold. Saldivar-Sali, who is now working
toward
a Ph.D. in building technology at MIT, hopes that the system will be
applied in
the "Building codes as
they are now will
specify a maximum building height and certain structural requirements
that are
standard for the entire country," said Saldivar-Sali. "But in an area
with a 66 hazard rating, which is relatively high on a scale that goes
up to
99, should the building code be more stringent or be zoned for no
building at
all?" Saldivar-Sali
stresses the importance of
using the landslide risk rating system to prioritize mitigation
measures, as
well. For instance, streams and river channels could be stabilized,
buildings
could benefit from increased stabilization provided by installing piles
at
certain points on a slope, blasting could be more stringently
controlled during
road construction and mining, and reforestation could be hastened in
some
areas. "The uncertainty
of natural threats and
their consequences have to be--and can be--treated in a systematic
manner using
hazard and risk analysis, assessment and management," said Einstein.
"The problem of typhoon-induced landslides is a good example of the
sort
of natural threat we can address in this way." ##
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