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Lorsque la Colombie a été frappée par un violent tremblement de terre, le pays a été pris par surprise : des foules entières se sont ruées dehors et une vague de doutes s’est abattue sur le niveau réel de préparation face à une catastrophe d’une telle intensité. Ces secousses brutales ont mis en lumière les risques quotidiens dans une région située au contact de plaques tectoniques, où des séismes destructeurs peuvent survenir presque sans avertissement. Malgré les technologies modernes de surveillance sismique, la science est encore incapable d’indiquer avec précision le moment où un séisme se déclenchera, ce qui laisse aux habitants à peine quelques instants pour réagir. Entre la fragilité de nombreux bâtiments, la densité extrême de certaines villes et la peur constante des répliques, nous analyserons ce qui a rendu cet épisode particulièrement alarmant et en quoi le prochain grand séisme pourrait surprendre un nombre encore plus important de personnes. Reste une interrogation centrale : que se produit-il lorsque la terre commence à vibrer avant même que l’on ait le temps de réaliser ce qui est en train d’arriver ?

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Transcript
00:01It's a Sunday morning in Colombia.
00:03A taxi driver to Cali sees the city and suddenly,
00:06he sees the buildings start to evaporate.
00:10An enormous rainstorms in the air.
00:13For a moment,
00:14it looks like the ground itself has exploded.
00:18He doesn't let it yet,
00:19but he sees the most powerful disaster
00:21that has been known in Colombia for decades.
00:24We talk about a earthquake of magnitude 7.4
00:28which struck the west of Colombia in August 2026.
00:32It took the life to more than 300 people
00:34and destroyed thousands of buildings.
00:38Today, a new study reveals why this disaster was so devastating
00:42and why the same problem could happen elsewhere in the world.
00:47At the time, Cali has suffered the most violent effects.
00:51It's one of the biggest cities of Colombia
00:53with more 2,2 millions of inhabitants.
00:56The cities like Manizales and Perea
00:59have also been deeply touched.
01:02But the disaster started in fact
01:04at about 5 hours of route
01:06in a small town called San Jose del Palmar.
01:10About 4800 people live here
01:13and this day,
01:14they have traveled something terrifying.
01:16More than 580 houses have been damage
01:19and electricity has been cut in all the area.
01:22The community has been completely isolated
01:25from the exterior world
01:26and the aid has been bad at it.
01:28It's a very mountainous region
01:30of Colombia
01:31and the main road of the village
01:33is not goudronnée.
01:35The cliffs of terrain
01:36were blocked after the disaster,
01:38so that the first secours
01:39by the terrestrial
01:40were only a few days later.
01:43Some rural areas
01:45were still without electricity
01:46a week after the disaster.
01:48Unfortunately,
01:50no one has been badly affected.
01:51But some inhabitants
01:52have said
01:53that it looked like
01:54the end of the world.
01:56In the streets,
01:57people faced
01:58the roof,
01:59the roof roof,
01:59the roof roof
01:59and the canalizations
02:01broken.
02:02But the real pressure
02:04went deep
02:04down,
02:05down,
02:07It's true
02:08that this part
02:09of the Colombian
02:10is located along the
02:11ceiling of the Pacific Pacific
02:13a huge area
02:14around the Pacific Pacific
02:16where the disasters are very frequent.
02:18The scientists
02:19still don't know
02:20exactly what effect
02:21caused this disaster.
02:23But they know
02:24that it was produced
02:25along a
02:25caused by
02:26in general,
02:28two enormous pieces
02:29of the land
02:30of the terrestrial
02:30have suddenly fallen
02:31one against the other
02:32later,
02:34instead of moving
02:35from high to low.
02:38Localizing precisely
02:39this rupture
02:40is difficult
02:40because this
02:41was incredibly
02:43deep
02:43at about 107 km
02:46below the surface.
02:47And that's
02:48something important
02:49to scientists.
02:50The rupture
02:51is not produced
02:52directly
02:53to the border
02:53between the NASCA
02:55and the South American
02:56is produced
02:57in deep
02:58inside the
03:00plate
03:00of the NASCA.
03:01At this point,
03:03the plate
03:03had already been
03:04pushed down
03:04to the South America.
03:06The pressure
03:07has stopped
03:08and then
03:09BOOM!
03:10The roaster
03:10has ceded.
03:12In summary,
03:14a deep fracture
03:14in the
03:15plate
03:15of the NASCA
03:16has suddenly
03:17released
03:18two
03:19blocks
03:20terrestrial
03:21the one
03:22against the other
03:23of the sea.
03:26The problem,
03:27it's that the sea
03:28profond
03:29function a little
03:30differently.
03:31As they start
03:31very far
03:32far,
03:33the secouss
03:33can spread
03:34into a massive
03:35zone.
03:36In the meantime,
03:38a part of this energy
03:39has reduced
03:39to reach the surface.
03:41But the problem,
03:42it's the place
03:43where it started.
03:45The sea
03:45has hit
03:46under the region
03:47of Tioco,
03:48one of the most
03:49poor
03:49of the Columbia,
03:50surrounded by
03:50a heavy jungle
03:52and at some
03:53places,
03:54the land itself
03:55has amplified
03:56the secousses.
03:57The walls
03:58and the deep
03:59walls
04:00can intensify
04:01the vibrations.
04:03Then,
04:03the secousses
04:04have reached the
04:04big cities.
04:05For many,
04:07it seemed to happen
04:07by waves.
04:08At the beginning,
04:09it was a brief secousses.
04:12Many inhabitants
04:13have thought
04:14that a big truck
04:14was next.
04:16But then,
04:17the telephones
04:18had to vibrate
04:19with an alert
04:20announcing
04:20that another
04:21could hit
04:22in the 20 minutes.
04:23One big one.
04:26It must be
04:27to say that
04:28these alerts
04:28do not
04:29predicts
04:29what they did.
04:30They did
04:31detect the first
04:33and the most weak
04:34and send an alert
04:36before
04:36the most strong
04:38hit.
04:39And when
04:40the violent
04:40hit hit
04:41this day,
04:42the damage
04:43had been terrible.
04:44The force
04:45was incredible.
04:46At a moment,
04:47the current
04:48had been cut.
04:49Some have seen
04:50that
04:50in the surface
04:51on the mur
04:52with the paint
04:53and the
04:53paint
04:53platter
04:54they had seen
04:55the secousses.
04:57And by their windows,
05:00they saw the buildings
05:01oscillate
05:02from one side
05:02to the other.
05:03But believe me,
05:05they had a chance.
05:06D'autres
05:07have experienced
05:07something worse.
05:09The
05:10videos of this day
05:11show the whole
05:12buildings
05:13evaporate.
05:14The enormous
05:15clouds
05:16envahi
05:16and people
05:18running out
05:18to find a
05:19place.
05:21And in the days
05:22that followed,
05:23the damage
05:24were everywhere.
05:25The schools
05:26were suspended
05:27in schools
05:27and universities.
05:29And five
05:30airports
05:31in Colombia
05:31were closed after
05:32the crisis.
05:34The secousses
05:36were also made
05:36feel beyond
05:37the region
05:38of Chioco.
05:39We saw them
05:40in the parts
05:40of the Valley
05:41del Cauca,
05:42the Risaralda,
05:44the Antioquia
05:45and the Tolima.
05:46Hundreds of thousands
05:47of thousands
05:48have been touched
05:49and 743
05:50buildings
05:50were flooded.
05:52It's difficult
05:53to represent
05:54such an
05:55amount of destruction.
05:57A recent study
05:58helps
05:59understand
05:59why
06:00the damage
06:00of the Americas
06:00have been so serious.
06:01Because yes,
06:03a magnitude
06:04of 7.4
06:06is extremely
06:07powerful.
06:08But the
06:09only number
06:09doesn't tell
06:10how much
06:11a tsunami
06:11will be destructive.
06:14In countries
06:15such as
06:16Mexico
06:16or Turkey
06:17are not
06:19very rare.
06:21The same
06:22for Japan.
06:23In April
06:242026,
06:26a tsunami
06:26of 7.4
06:28hit
06:28the
06:28large
06:29of the
06:29Sandriku
06:30on
06:31Honshu
06:31to
06:34Tohoku
06:34and Hokkaido.
06:36But the
06:37damage
06:37there was nothing
06:38to do with what
06:39we saw in Colombia.
06:40Only
06:40230 structures
06:42have been
06:42damaged.
06:44The researchers
06:45wanted to know
06:47why
06:47the damage
06:48in Colombia
06:48were more
06:49serious.
06:50And
06:51one
06:51part
06:51of the
06:52part
06:52of
06:52of
07:19the
07:20of
07:20the
07:20of
07:21the
07:21the
07:21of
07:21the
07:21of
07:21the
07:22of
07:49the
07:50in
07:50in the
07:50least.
07:51The
07:52the
07:53the
08:03the
08:04of
08:04the
08:05three
08:08of
08:09the
08:09that
08:09the
08:14of
08:18the
08:19small fissures, only big fissures could appear.
08:23It concentrates all the contraintes in one point.
08:27The inside of the wall casts and the wall cede.
08:31The researchers have also discovered another problem.
08:35The walls were so fins that even in adding more steel,
08:38it could not suffice. Their tests show that these walls
08:42simply don't have the necessary resistance to face
08:45and the most important thing is that this type of construction
08:50is also used in other regions of Latin America.
08:54The experts fear that the same tragedy can be reproduced ailleurs.
08:58And remember, six weeks ago,
09:01two powerful explosions had hit the Venezuela,
09:05almost 50,000 buildings according to the estimation.
09:10And as in Colombia, the ancient buildings were not ready
09:13for such violent secourses,
09:16what has aggravated the destruction.
09:20After two major explosions so close,
09:23the countries of South America have begun to examine
09:26the prevention of close close.
09:29There are more strict standards
09:30and a better planification of emergency.
09:33The hope is that during the next big crash,
09:36these buildings,
09:37these buildings more solid and clear evacuation plans
09:40allow them to save more lives.
09:43This is the end of the day.
09:44The end of the day.
09:45The end of the day.
09:46The end of the day.
09:46Bye!話
09:46.
09:46.
09:46You
09:46.
09:47.
09:47.
09:47.
09:48.

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