LES ZONES À RISQUES !
Aux Philippines peu d’endroits échappent aux risques
inhérents aux tremblements de terre. Le pays se trouve sur la ceinture de feu
du Pacifique et de plus à une jonction de plusieurs plaques tectoniques.
Cela va de la petite secousse à la catastrophe majeure, mais aucun endroit de l’archipel, sauf l’île de Palawan, n’est à l’abri de ce genre de catastrophe naturelle qui, je le rappelle, à ce jour n’est toujours pas prévisible.
Cela va de la petite secousse à la catastrophe majeure, mais aucun endroit de l’archipel, sauf l’île de Palawan, n’est à l’abri de ce genre de catastrophe naturelle qui, je le rappelle, à ce jour n’est toujours pas prévisible.
Le phénomène qui de loin m’effraie le plus.
Imprévisible, violent, la force de la nature à l’état brut, un déchainement de
forces colossales, un combat de titans entre les plaques de la croûte terrestre,
le frissonnement de la planète Terre.
Le récent tremblement de terre qui a touché Bohol et
cette région des Visayas a fait de nombreuses victimes. Des églises, souvent
vieilles de plusieurs siècles, ont également souffertes, des dégâts parfois
irrémédiables.
Experts warn that many parts of the Philippines—including the nation's densely-populated capital—are long overdue for major earthquakes, and we can't entirely be sure where the next big one will strike.
But one thing
is for certain: it's only a matter of time.
Mario
Aurelio, Laboratory Head of the Structural Geology and Tectonics of the UP
National Institute of Geological Sciences (NIGS) laments the lack of
comprehensive knowledge about the country's numerous geologic faults.
The 7.2
magnitude earthquake that shook Central Visayas on October 15 was a relatively
rare event, Aurelio notes, but other parts of the country are also due for
similar quakes.
Earthquake-prone
areas
“Bohol and
Cebu earthquakes have been relatively rare, considering that the entire Philippine
archipelago is earthquake-prone except for Palawan,” said Mario Aurelio,
Laboratory Head of the Structural Geology and Tectonics of the UP National
Institute of Geological Sciences (NIGS).
“('Yung Bohol
at Cebu) hindi naman kasing active ng mga considered na very active faults
tulad ng sa Siargao and Zambales,” said Ric Mangao, research specialist from
the Philippine Institute of Volcanology and Seismology (Phivolcs).
Hidden faults
On Wednesday,
Phivolcs said that a newly-discovered fault might be the source of the Visayas
earthquake.
Phivolcs
identified the quake's real epicenter as being located between the municipality
of Catigbian and Sagbayan in Bohol, and not in the town of Carmen, as was
previously thought.
However,
Aurelio said that immediately associating the recent earthquake in Bohol with
an underlying fault is still a tentative hypothesis. He said that there are
many unidentified faults in the Bohol region and elsewhere, which makes the
identification of the origin of the earthquake “a little bit tricky”.
As a parallel
example, he cited the 7.7-magnitude earthquake in Northern Luzon in 1990. There
were no recorded faults in the area when this quake hit, killing 1,621 people
across the region.
Moreover,
Phivolcs' reassessment of the quake's epicenter coincides with initial data
from the US Geological Survey (USGS): in its summary page for the Bohol quake,
the agency located the epicenter at 2km northeast of Catigbian.
“'Yung mga
aftershock lumalabas sa East Bohol Fault,” said Mangao.
Fate of old
churches, other buildings
Old churches
and shrines in Bohol were not designed to be earthquake-proof.
“Assuming
that churches in Bohol were done through sound construction practices, the
damage were done not because of material but because (of the) design,” Aurelio
said.
Old churches
don't have rebars, the metal skeletons that serve as the foundation of a
structure and hold it together. Instead, they were built by piling blocks of
limestone, one on top of another.
Restoring the
churches in Bohol will take years, according to heritage documentation
specialist Joel Aldor in a GMA News TV report.
Earlier this
year, Phivolcs director Renato Solidum warned that many buildings, particularly
in the nation's densely-populated capital, remain unassessed for physical
integrity in the event of strong earthquakes.
“The issue
though is some of the buildlings are non-engineered and most likely walang
permit so they have to focus on that also,” he said.
Major
lifelines like water and power supply, and communication means, should be
strengthened to withstand fires and earthquakes.
Active fault
line under Metro Manila
Meanwhile,
hidden under Metro Manila is the West Valley fault line, which experts also
believe is long overdue for a large quake.
"Ripe na
gumalaw ang fault. Napakataas ng probability na gumalaw ito in the future,
hindi lang natin masabi ang exact date and time," Phivolcs deputy director
Bartolome Bautista said during a Senate inquiry on the country's disaster
preparedness on Wednesday.
The
earthquake fault runs from the Sierra Madre mountain range to Tagaytay, and
moves every 200 to 400 years. The last time this fault moved was 200 years ago.
Phivolcs
presented the prediction in July this year, warning Metro Manila that this
quake is due to happen within our lifetimes.
Solidum said
that preparations for the next large quake are of paramount importance.
Unlike storms
and typhoons, earthquakes cannot be “forecast” and can only be predicted by
looking at how often it happens in history. To date, there are no scientific
instruments that can predict when an earthquake will occur.
A
7.2-magnitude earthquake, as was seen in Bohol, can shake the ground even a
hundred kilometers away, meaning a tremor in Metro Manila can affect
surrounding provinces.
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