Could We Survive a Mega-Tsunami?


Could We Survive a Mega-Tsunami?

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For all our technological wonders,

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mankind is vulnerable to a far greater power.

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The wrath and fury that only our planet can unleash.

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Volcanoes...

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earthquakes...

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and silent assassins, unseen until it's too late.

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Tsunamis that bring death and devastation from the sea.

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On Boxing Day 2004,

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nearly a quarter of a million people were killed in southern Asia.

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On March 11, 2011, Japan

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and destruction that came within a whisker of nuclear catastrophe.

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But scientists believe

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that something even more destructive lies in wait.

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Something that will one day strike us in the West.

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A wave so many times bigger than any conventional tsunami,

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it's been dubbed a mega-tsunami.

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Now, using the very latest science, powerful computer models

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and the terrible evidence of all to recent events,

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this is the story of how some experts believe the greatest

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natural disaster in human history might one day unfold.

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The biggest wave ever seen...

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threatening cataclysmic destruction

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of some of the world's greatest cities...

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..death and devastation on an unprecedented scale

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and economic fallout that could reshape the future

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of the entire world.

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It will all begin on one of Britain's most popular

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tourist resorts...

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the Canary Islands,

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with an event that last occurred in 1971

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and, before that, in 1949.

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A volcanic eruption.

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'The Canary Islands' volcano of La Palma

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'erupted for the first time in two centuries.

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'Menacing the population

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'and is turning night into day with blazing rivers of molten lava.'

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People think of volcanoes of being, sort of, cone shaped

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with a little hole in the top

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and those are what we called stratovolcanoes,

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they are the traditional volcano shape,

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but this is very different, this is an elongate structure.

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La Palma is one of a chain of volcanic islands,

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lying off the coast of West Africa,

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that includes Gran Canaria and Tenerife.

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Its most active region is a high mountain ridge

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called La Cumbre Vieja.

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The Cumbre Vieja occupies the southernmost part of the island

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and it forms this north-south lined ridge.

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The whole ridge is, sort of, pockmarked craters and holes,

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and then you have lava flows heading off in both directions,

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to the west and east, from these particular craters.

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In 1949, quite a small eruption, in terms of volume of lava,

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the volume of magma, erupted but during the eruption

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there had been a series of very strong earthquakes

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and a fault line had developed along the crest of the volcano.

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A giant gash had opened up along the island's ridge,

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four kilometres long and up to four metres wide.

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Part of the west flank dropped a couple of metres towards the sea

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and then stopped, and that's really what tells us that something

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other than just magma coming up was going on during that eruption.

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That geological rift is the reason why this volcano

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could one day trigger a mega-tsunami.

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Because ever since 1949,

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the peaceful island of La Palma has been a time bomb...

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and some scientists believe that today another eruption

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could send 500 cubic kilometres of it crashing into the sea.

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A colossal landslide with enough energy

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to generate the biggest wave humanity will have ever seen.

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Unleashed not upon the Pacific but the Atlantic and heading for us...

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..the first mega-tsunami in recorded history.

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The terrible human cost of the recent Pacific tsunamis

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came from underwater earthquakes.

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But recent history has already shown that the collapse of a volcano

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could unleash even greater devastation.

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Most people think of volcanoes as these are unchanging sentinels

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of solid rock that persists for many millions of years

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and, really, just go on getting bigger,

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but they are better viewed, really, as unstable piles of rubble.

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It was the Mount St Helens eruption in 1980 that really provided us

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with that first visual proof that volcanoes did collapse.

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'This is the CBS Evening News with Dan Rather.'

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It is an event that defies superlatives.

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One geologist said today, "There is no record today, in geology,

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"in the last 4,000 years, of anything like this happening before.

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"The tremendous lateral blast is unprecedented."

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This is the only photographic evidence that we have

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for a volcano lateral collapse actually happening.

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'This sequence of photos was taken during the first 60 seconds

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'of the mountain's eruption,

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'beginning shortly after 8.30 on Sunday morning.'

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It was really an iconic moment, which taught us that volcanoes

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did things that we didn't think they did before, and that is that

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instead of just erupting upwards they can also erupt sideways.

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You can see the bulge dislodging,

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forming this landslide which heads off northwards.

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And then this massive column of ash, which heads up into the atmosphere,

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and ultimately covers the entire region.

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The question we all asked ourselves at the time was,

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"What would've happened if that collapse had occurred into water?"

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What would happen would be the conversion

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of a vast amount of energy into an ocean-going wave...

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..starting off up to one kilometre high

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and with the power to cross oceans at the speed of a jet aircraft...

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..ready to make landfall with potentially apocalyptic results.

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Startlingly, it wouldn't be the first time that a landslide

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has called a tsunami on the Canary Islands.

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One marine geologist thinks he's found evidence of a past event...

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..not on La Palma but nearby on Gran Canaria

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at a site called Agaete.

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What we have here are tiny pieces of shell - that's about two centimetres.

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That's a mollusc, it comes from the sea.

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What is strange about finding them here

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is that they are 50 metres above...

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the level in the sea at which they usually live.

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Shells like these can be found three kilometres inland

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and 200 metres above the sea -

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too far to have been carried there by any storm.

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And, without evidence of changes in sea level,

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there can be only one explanation.

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If they weren't laid down by a high sea level,

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if they weren't laid down by a storm, then what was the source?

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We need something to have created a wave 200 metres high.

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Dave Tappin's wave on Gran Canaria was far too big

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to have been made by an earthquake.

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The only answer, in my estimation, is the collapse of a volcano.

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It's unlikely to have been Gran Canaria but the nearest island,

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100 kilometres away, just over there, where I'm pointing, is Tenerife.

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On the coastline, facing Gran Canaria, there is a major collapse

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and that collapse is called Guimar.

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The area where we are now, in the Guimar Valley, in Tenerife,

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it's around about ten kilometres wide along the coast,

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extends several kilometres inland, so it's a big feature.

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Where now there is this broad, flat-floored valley,

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there would have originally been a steep sided volcanic cone.

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So, the area that collapsed is over to our right

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and on the left we can see the lavas that formed the old volcano.

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And between the two we have this enormous cliff.

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But originally that would have been the sidewall of the landslide.

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Over in the distance, from here,

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we can see the tops of the mountains of Gran Canaria,

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round about 100 kilometres away, so it's very easy to imagine

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that the Guimar landside, as it went down into the ocean,

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would have generated a tsunami that spread across the ocean

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to Gran Canaria and produced the tsunami deposits at Agaete.

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This tsunami would drive across the ocean,

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between Tenerife and Gran Canaria,

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and strike in this particular location,

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could easily build up after it hit the coastline,

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travel inland to heights above sea level of hundreds of metres.

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But even Tappin's tsunami would pale alongside the wave

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that would be created by a collapse of the entire mountain flank

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of La Cumbre Vieja.

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Not everyone agrees, but many experts think that such an event

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would have consequences of global proportions.

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It's not surprising that this tiny volcano has become

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so intensely studied.

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This is the story of a scientific model

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of a volcanic collapse of La Palma projected into the near future.

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By using reconstructions...

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Tens of thousands of people are feared dead and hundreds of thousands

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are still missing following the worst natural disaster in history.

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..real archive footage from previous natural disasters

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and graphical representations of what such a wave would do...

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..we can plot out the possible unfolding of events

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that one day could really happen.

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Our scenario begins

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one ordinary day on the island of La Palma itself.

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No-one knows it yet,

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but it's just five days before disaster will strike.

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Seismic monitoring will register a sudden increase in activity.

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Higher! Let's go, come up.

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But, since earthquakes here are common,

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no-one will take too much notice...

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..but then local wildlife will begin to die,

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succumbing to carbon monoxide fumes emanating from the ground.

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A harbinger that something more dangerous is afoot.

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An event that no-one can ignore.

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La Palma's La Cumbre Vieja is erupting once more.

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In one instant, a whole section of the island is dislodged.

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Breaking up as it falls, an entire mountainside plunges into the sea...

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at the speed of an express train.

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We see the landslide first generating an enormous wave.

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Within seconds, the surrounding ocean is distorted.

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At first it forms a huge dome of water...

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..and then a giant wall...

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..on a scale that is almost unimaginable.

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A mega-tsunami.

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That wave could be as much as a kilometre high.

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In terms of the height, you're talking about

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more than two Empire State Buildings on top of one another

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or three of London's Shard piled on top of one another.

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This is an immense mass of water.

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Not just fast, but fast.

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Travelling at up to 800 miles an hour,

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the giant wave surges out in all directions.

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Immediately in its path, the highly populated island of Tenerife,

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less than 100 miles away.

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In less than ten minutes the wave makes landfall.

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Locals and holidaymakers alike do all they can to outrun it.

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Within minutes, the wave has claimed its first victims.

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I don't think there's any doubt that,

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however big the collapse of the west flank of Cumbre Vieja,

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the initial wave will be very catastrophic

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for the islands themselves.

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So, you're talking about thousands of people dead and destruction

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on a scale that we've never seen in this part of the world before.

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With less than ten minutes to react,

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it's hard to see many of the two and a half million locals

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and visitors to the Canary Islands escaping with their lives.

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But even as the wave devastates neighbouring islands,

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La Palma continues to erupt.

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The mountain of La Cumbre Vieja is still collapsing...

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..releasing yet more energy into the sea.

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Our mega-tsunami's journey of destruction has only just begun.

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Within 20 or 30 minutes, all of the waves have spread out from La Palma

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and they've started this long journey out across the Atlantic Ocean.

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There's been no time to raise the alarm.

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Within 60 minutes, 90 metre waves will strike

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the coast of West Africa.

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Over the following hours, these waves will devastate

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the coastlines of Europe.

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While across the Atlantic Ocean, millions of Americans lie sleeping.

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Nothing can stop a wave this size.

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Only landfall and the coastal cities that lie in its path.

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It could be the costliest natural catastrophe

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in the history of our planet.

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While geologists have studied how a landslide tsunami could be caused,

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wave experts like Nils Kerpin are working out

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just how a mega-tsunami would travel once unleashed.

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A miniature Cumbre Vieja

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reveals exactly how fast waves would radiate out from La Palma.

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See that the wave that occurs due to the landslide will propagate

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and encircle around the island.

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Using physical modelling,

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Nils can analyse the very anatomy of the giant wave.

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Here we see the beginning of some landslides

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and we can see air bubbles that are rushing back

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and running up the slope of the remaining island.

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From the very moment it's first formed

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to its height and its speed as it spreads.

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The faster this landslides occurs,

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the more energy will be induced into the water body.

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Fluid science can model not only the wave itself

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but exactly how its journey progresses.

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Northwards towards Europe

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and unchecked across the open Atlantic.

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That science can help us to chart what will happen in our scenario

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in the hours to come.

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It's 80 minutes after the initial landslide

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and, to the east, the wave, still up to 60 metres high,

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is minutes from its first major cities...

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..Casablanca, in Morocco, and its capital Rabat.

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A combined population of six million.

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It is estimated that two thirds of them

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will not survive the wave's impact.

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Only now are the first reports of the unfolding disaster

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beginning to emerge.

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It's likely that, before any news agencies begin to report,

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Twitter, Facebook and mobile calls will carry the first images

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of unfolding disaster to the world.

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In London, the Prime Minister becomes aware of events.

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When a disaster happens that dominates everything,

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the whole diary's cleared.

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The PM summons the relevant government departments

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and representatives of the emergency services

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to the Cobra response room.

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Cobra's that kind of high-tech room with lots of links to police,

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the fire services, etc, round the country.

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But they have little time to plan.

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Just 30 minutes after Casablanca, the wave reaches Europe.

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It is still the height of a two-storey house.

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The coastal capital of Lisbon is devastated.

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Back in Westminster, the Cobra meeting room

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is now a centre of intense activity.

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So, the first thing we want to know

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is, "Just how big is this? What's actually happening?"

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Often, if you've got a TV screen on,

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you'll know as much as the person in the centre of Whitehall.

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As likely as not they'll have Sky and BBC 24-hour,

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and they'd be following Twitter and social media.

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There is always, always a period where there is a kind of fog of uncertainty.

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I think the key point is to alert the emergency services,

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so that they are prepared for it to happen.

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After hitting Lisbon, the emergency services have just three hours

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before the wave strikes Britain.

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The Environment Agency issues flood warnings to the south coast.

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Fire, ambulance and rescue units are put on standby.

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Police clear the streets of southern coastal towns,

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evacuating schools and vulnerable communities.

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Back in Whitehall, the Government has two work out what to say

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and how to deal with increasing public panic

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as awareness of the scale of unfolding events spreads.

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A giant tsunami is spreading throughout the Atlantic basin.

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Waves of up to 40 metres high have already devastated

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the coasts of Portugal, North Africa and Spain.

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Scientists estimate that the wave is travelling at approximately 500mph.

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It's expected to move across the Atlantic...

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You're still building up information as well as trying to move people.

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That'll be the time that the media are saying,

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"What are you doing about it? What's happening?"

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The key test of the Government will be to show they're responding,

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to outline the measures they're taking.

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But the measures they're taking

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are in the time when they really don't know how serious it is.

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Just three hours after the first UK warnings,

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a wave up to 25 metres high makes its first landfall in Britain...

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..on Cornwall.

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In the immediate aftermath, say two or three hours after it's hit,

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they'll still be confusion.

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I mean, we're probably talking about a very, very wide area of hundreds of miles.

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So, finding out what's happening in a cove in Devon or Cornwall,

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I mean, you know, how is that going to get back?

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I mean, you could well have communities wiped out.

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We can get some idea of the impact of a seven to ten metre wave,

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on the UK south coast,

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by looking at what happened in the Indian Ocean in 2004,

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in places like Sri Lanka and Thailand.

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The level of destruction was immense

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and the death toll was in the tens of thousands.

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You could say that the population of the south coast of the UK

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is probably quite a bit higher,

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so that sort of wave would be immensely destructive in the UK.

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From Cornwall, the wave surges through into the Irish Sea

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and through the English Channel,

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engulfing much of Britain's south coast.

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The aspect that makes a tsunami so devastating is its wavelength

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and how long it is.

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A storm wave might be ten, 20, 30 metres long, 40 metres long,

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50 metres long.

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In the case of a tsunami,

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we have a wave that is 200 or 300 kilometres long.

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Unlike a storm wave, a tsunami just keeps on coming -

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mile after mile of it.

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Seawater floods our southern cities

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and penetrates low-lying farmland for miles inland.

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It not only runs up the coastline and inundates the land,

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but it continues to flow inland, as if it's a river flowing over

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the land and scouring out, and removing things in its path.

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So, it's the inundation, it's the wavelength,

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that actually makes these events so dangerous.

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Models differ on what the wave might do to our southern cities

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as it works its way east.

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Towns such as Brighton would probably survive,

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but would suffer serious disruption.

0:31:080:31:10

In our scenario, London, our capital,

0:31:290:31:33

tucked in from the North Sea, is safely sheltered.

0:31:330:31:36

Britain, it seems, will survive the worst calamities seen elsewhere.

0:31:400:31:46

The wave, however, as well as travelling east to Africa

0:31:510:31:56

and north to Europe is also heading west, across the Atlantic.

0:31:560:32:01

And there is a whole new nation is waking up - America.

0:32:040:32:09

'Good morning, New York. It's a beautiful day out there in the city

0:32:090:32:13

'but here's a word of advice, enjoy it while you can.

0:32:130:32:16

'The weathermen says there's going to be some rain this afternoon

0:32:160:32:19

'and temperatures could drop dramatically by the end of the day.'

0:32:190:32:23

It's 7am. As the tsunami is devastating southern Britain,

0:32:230:32:28

it's three hours away from New York.

0:32:280:32:31

1,500 miles off the coast, the wave hurtles west at incredible speed.

0:32:390:32:47

The deeper the water, the faster the wave moves.

0:32:500:32:53

So, in five kilometres of water

0:32:530:32:55

the wave will move at 800 kilometres an hour.

0:32:550:32:58

It's travelling at the speed of a jet plane.

0:32:580:33:01

Bear in mind, it's not the water that is moving.

0:33:010:33:05

So, you can't imagine water moving at 800 kilometres an hour,

0:33:050:33:08

it's the energy of the wave.

0:33:080:33:10

The particles of water are pushing against each other

0:33:100:33:13

and so, if you like, each is knocking against the next

0:33:130:33:16

and it's moving the energy across the oceans.

0:33:160:33:19

For evidence of how tsunami waves can travel between continents,

0:33:230:33:27

scientists, once again, only need to look to the past.

0:33:270:33:31

In particular, evidence of

0:33:320:33:35

an earthquake generated tsunami that began in Chile in 1960.

0:33:350:33:40

'Devastation untold, a death toll close on 5,000,

0:33:420:33:46

'is part of the reckoning that staggers Chile. In Concepcion, city of...'

0:33:460:33:50

The earthquake itself caused lots of damage, significant damage

0:33:500:33:53

but it also created a very large tsunami.

0:33:530:33:57

That tsunami did cause damage in Chile itself,

0:33:570:34:00

but what was interesting about that one was that the damage it caused

0:34:000:34:03

further afield was also significant.

0:34:030:34:06

'Incredibly, Hawaii, 6,000 miles away in mid-Pacific,

0:34:060:34:09

'was struck by four gigantic tidal waves.

0:34:090:34:12

'On surged the terrifying walls of water as far as the Japanese coast

0:34:120:34:16

'9,000 miles from Chile.'

0:34:160:34:17

And that really brought home the fact that a tsunami happening

0:34:200:34:24

one side of the ocean can have a dramatic impact

0:34:240:34:27

the other side of the ocean.

0:34:270:34:28

The wrath of volcanoes and earthquakes is all too evident,

0:34:310:34:35

but often their violence is geographically limited.

0:34:350:34:38

But tsunamis are different.

0:34:390:34:43

Fluid dynamics means that the ocean itself can carry the energy

0:34:440:34:49

of a tsunami over thousands of miles and in all directions.

0:34:490:34:55

30 minutes after the northern face of the wave first struck Cornwall,

0:35:030:35:08

its western edge is just 1,200 miles from a whole new nation.

0:35:080:35:13

In the US, 40 million people

0:35:150:35:18

live within 40 kilometres of the coastline.

0:35:180:35:20

And of those 40 million people,

0:35:200:35:23

something like 30 million of them

0:35:230:35:25

live within ten metres, vertically, of the shoreline.

0:35:250:35:30

If you're looking at these extreme events, like a tsunami,

0:35:320:35:35

that can put ten, 20, 30 metre waves at the shoreline,

0:35:350:35:39

that's an incredibly vulnerable population.

0:35:390:35:43

Atlantic City, Washington, Boston...

0:35:430:35:49

and New York.

0:35:490:35:51

Major cities along the coast all lie directly in its path.

0:35:550:35:59

-ALARM BEEPING

-'Short period alarm.'

0:36:030:36:07

'Short period alarm.'

0:36:070:36:09

America is equipped with systems

0:36:090:36:12

capable of detecting an inbound tsunami.

0:36:120:36:15

The first is a network of seismometers,

0:36:150:36:18

located around the world,

0:36:180:36:20

which feed real-time data to a monitoring station in Alaska.

0:36:200:36:25

This shows the signal from all the different seismometers

0:36:250:36:28

that come in to the centre. Coming in in what we call real-time.

0:36:280:36:32

If there's anything that significant, it will trigger an alarm

0:36:320:36:35

and that will bring the guys in to take a look at the event.

0:36:350:36:38

But this system is designed to detect tsunamis generated by earthquakes.

0:36:390:36:45

Not a distant landslide

0:36:450:36:47

like the collapse of La Cumbre Vieja on La Palma.

0:36:470:36:51

Landslide generated tsunamis are very hard for us to respond to.

0:36:510:36:54

They do not show up on our seismic networks in the same way that earthquakes do.

0:36:540:36:58

Much, much more challenging.

0:36:580:37:00

A second line of defence is a network of deep ocean sensors

0:37:020:37:06

called DARTs, designed to detect changes in water pressure

0:37:060:37:11

caused by passing waves.

0:37:110:37:13

If there was a tsunami generated in the Canary Islands,

0:37:130:37:16

we would see impacts on our DART in the central Atlantic Ocean.

0:37:160:37:21

The DART system would raise the alarm,

0:37:230:37:26

but just three to four hours before the waves hit the coast.

0:37:260:37:30

The likelihood, though, is that, for all their sophistication,

0:37:430:37:48

these technological detection measures would do well

0:37:480:37:51

to beat the speed of reports coming through social media.

0:37:510:37:55

For America, news of the mega-tsunami's impact in Africa and Europe

0:37:580:38:04

would throw their own fate into sharp relief.

0:38:040:38:07

New York City is 8.4 million people who live on 302 square miles.

0:38:120:38:19

That is three islands and a peninsula,

0:38:190:38:21

mostly about 50 feet above the waterline.

0:38:210:38:24

It is a world-class city with enormous strengths

0:38:260:38:29

and also significant vulnerabilities.

0:38:290:38:32

An example is the island of Manhattan,

0:38:340:38:36

which has a population of about 1.5 million.

0:38:360:38:40

That population doubles every business day

0:38:400:38:42

to about three million people.

0:38:420:38:44

For the city authorities, it's a question of how many people

0:38:470:38:51

you might be able to save.

0:38:510:38:53

New York's Office of Emergency Management is responsible

0:38:570:39:01

for coordinating the response to any natural disaster.

0:39:010:39:04

We have spent the last ten years analysing the roadway network

0:39:060:39:13

and the mass transit network, and the population,

0:39:130:39:18

and determining how long it would take to evacuate.

0:39:180:39:24

The city's rail network would be the primary means of escape.

0:39:270:39:31

And yet, for all the evacuation plans in place,

0:39:360:39:40

there's a terrible irony.

0:39:400:39:41

Even in the apparent knowledge that disaster is imminent,

0:39:430:39:47

studies have shown that whole populations can go into denial.

0:39:470:39:52

Refusing to accept that the danger is real.

0:39:520:39:56

So, if we can get people to think, "This IS going to happen to me,

0:39:590:40:04

"I AM at risk, my family is at risk,"

0:40:040:40:06

then we can get them to move. But the reality is that up to half

0:40:060:40:10

the people won't move, no matter what we say to them.

0:40:100:40:13

They don't believe that it's going to happen.

0:40:130:40:16

For many typical New Yorkers,

0:40:240:40:26

with the wave heading straight towards them,

0:40:260:40:29

this is just another day in the Big Apple.

0:40:290:40:33

Meanwhile, as American city dwellers try to decide whether to go or stay,

0:40:540:41:00

the wave is about to hit the islands of the Caribbean.

0:41:000:41:03

Here, it's another ordinary day of perfect sun and sea.

0:41:060:41:11

But, across all the islands,

0:41:110:41:13

40 million people live predominantly in coastal towns.

0:41:130:41:18

The Caribbean would be absolutely devastated by this kind of wave.

0:41:280:41:32

We would have ten to 20 metre waves sweeping across many of the islands.

0:41:320:41:37

Bermuda, the wave would probably sweep entirely over the island.

0:41:380:41:42

There would be nothing left.

0:41:420:41:44

It would actually be stripped to the foundations.

0:41:440:41:47

A lot of the islands are volcanic, so they have very steep shorelines.

0:41:470:41:51

If you could go half a mile inland you would be out of the way

0:41:510:41:53

but how do you get half a mile inland?

0:41:530:41:56

The road infrastructure parallels the coastline,

0:41:560:41:58

so you would literally have to run on foot

0:41:580:42:00

to get out of the wave in many areas.

0:42:000:42:02

So it's an extremely dangerous event for the Caribbean.

0:42:020:42:06

With the wave now just minutes away from both the financial

0:42:110:42:14

and political centres of the world's greatest superpower,

0:42:140:42:19

most experts believe that the major eastern cities

0:42:190:42:22

would still be packed.

0:42:220:42:24

But now even hardened New Yorkers have to take notice.

0:42:280:42:32

Evacuation plans have been activated, but it's chaos.

0:42:340:42:39

You either go up high and risk becoming marooned

0:42:390:42:42

or take underground road and rail tunnels out of Manhattan,

0:42:420:42:46

and face the possibility of a gridlocked tomb.

0:42:460:42:50

By the time the warning network's been up, it's here.

0:42:500:42:54

So, we might have two or three hours notice at best.

0:42:540:42:58

The question is, what can you do in two or three hours?

0:42:590:43:02

And the answer is not much.

0:43:020:43:04

The ocean wave is now only 12 metres high,

0:43:040:43:08

but, as it approaches New York, it rears up again, becoming a monster.

0:43:080:43:14

The back of the wave is still moving at, say, 500 miles an hour.

0:43:160:43:20

The front of the wave is moving at, maybe, 40 miles an hour.

0:43:200:43:23

And so the wave piles up,

0:43:230:43:25

and that's where we go from a wave that is maybe a foot,

0:43:250:43:28

30 centimetres high, to a wave that can suddenly become 50 metres high.

0:43:280:43:32

And that's where the destruction occurs.

0:43:320:43:35

No-one knows exactly how great a mega-tsunami's impact would be,

0:43:380:43:44

but science points to one of mankind's greatest cities

0:43:440:43:48

being humbled by the power of nature.

0:43:480:43:52

What's worse is that studies have revealed that the landslide

0:43:550:43:59

will result in not one wave but several.

0:43:590:44:03

And the first will not be the biggest.

0:44:060:44:09

People think of it as being one tsunami.

0:44:110:44:13

There would be as many as ten waves sweeping across the coast.

0:44:130:44:16

The first wave would be maybe eight to ten metres.

0:44:180:44:21

The second wave would be as much as 25.

0:44:270:44:30

Only 12 hours earlier, it was just another normal day.

0:45:280:45:32

Now a geological collapse of a small volcano on a tiny island

0:45:330:45:38

has changed tens of millions of lives on three separate continents.

0:45:380:45:44

Tens of thousands of people are feared dead

0:45:460:45:48

and hundreds of thousands are still missing,

0:45:480:45:51

following the worst natural disaster in history.

0:45:510:45:53

By the time our tsunami strikes New York,

0:45:570:46:01

in Britain a nation is already coming to terms

0:46:010:46:05

with widespread loss.

0:46:050:46:07

The authorities say they are doing everything they can

0:46:070:46:10

and have appealed for calm.

0:46:100:46:12

A state of emergency has been declared.

0:46:120:46:15

But this tsunami itself would only be the beginning

0:46:200:46:24

of a whole new chain of events.

0:46:240:46:27

Disaster planners know that, following any catastrophe,

0:46:310:46:35

the biggest dangers come in the aftermath.

0:46:350:46:38

Rescuing the injured and identifying the dead...

0:46:390:46:42

..caring for a traumatised population and preventing disease...

0:46:450:46:49

..retaining law and order and the reins of civilisation.

0:46:510:46:56

In America, where our mega-tsunami has struck at the very heart

0:47:060:47:11

of the world's political and economic capitals,

0:47:110:47:14

the challenges are greatest of all.

0:47:140:47:17

When you talk about Manhattan,

0:47:200:47:22

virtually the entirety of Manhattan is below ten metres above sea level.

0:47:220:47:27

So, if you were in the New York City area, hopefully,

0:47:270:47:30

you evacuated up and didn't try to go out...

0:47:300:47:34

and you'd be trapped, basically, while the water receded.

0:47:340:47:37

You have this initial impact of the water, which is heavy,

0:47:400:47:44

but as it recedes you've got the same amount of water going back

0:47:440:47:47

into the ocean, taking with it a lot of debris.

0:47:470:47:50

It's taking trees, it's taking buildings, it's taking cars

0:47:500:47:54

and, so, all of a sudden, you have this water with a load

0:47:540:47:59

of battering rams going back through the population that it's just hit.

0:47:590:48:05

And as much damage is caused by the receding wave

0:48:050:48:08

as is often caused by that initial wave.

0:48:080:48:11

Taking the wave's progress to its final conclusion

0:48:130:48:16

and, with the help of experts in disaster planning,

0:48:160:48:20

we are able to continue our own scenario.

0:48:200:48:23

It takes days before calm finally returns to the sea.

0:48:270:48:31

Only now is the true scale of destruction becoming clear.

0:48:330:48:38

New York, Boston, Washington, Miami -

0:48:420:48:47

entire cities have been destroyed.

0:48:470:48:52

The number of casualties is really hard to get at

0:48:520:48:55

in something like this.

0:48:550:48:57

For the 25 metre scenario, with maybe three to four hours of warning,

0:48:570:49:02

we came up with roughly 4.5 million casualties.

0:49:020:49:05

After the wave, those living, like in Japan,

0:49:130:49:17

face a devastated homeland.

0:49:170:49:20

You'd be left with an unimaginable landscape.

0:49:200:49:23

Smaller structures would be destroyed and scattered,

0:49:230:49:26

so the debris would be piled probably five, six metres high in the streets.

0:49:260:49:30

Debris sits like a blanket across the city

0:49:350:49:39

and it prevents us from getting ambulances to people who need them,

0:49:390:49:43

and getting fire trucks to fires, and getting people to grocery stores

0:49:430:49:48

to get food, and so, debris is our biggest and worst problem.

0:49:480:49:52

The doctors, physicians, emergency responders,

0:49:540:49:57

they're going to have enough trouble dealing with things

0:49:570:50:00

they can see within 100 yards of their facility,

0:50:000:50:03

much less being able to actually go on emergency calls.

0:50:030:50:06

So, you can pretty much expect anyone that is injured

0:50:060:50:09

is going to be on their own for at least a week.

0:50:090:50:12

If it's any kind of a serious injury, without medical attention,

0:50:120:50:15

they are likely to expire.

0:50:150:50:16

Dealing with death on such a scale becomes a massive priority.

0:50:210:50:27

Kenyon International Emergency Services is a private company

0:50:270:50:30

that responds to disasters.

0:50:300:50:32

Disasters that typically involve the loss of human life.

0:50:320:50:36

We deal with mass fatalities that are catastrophic -

0:50:370:50:42

a quarter of a million dead.

0:50:420:50:44

This is a refrigeration unit, a portable refrigeration cabinet,

0:50:500:50:54

of which we have several that we use to hold the deceased.

0:50:540:50:58

The purpose of the morgue is where we examine the bodies

0:51:010:51:04

and collect that picture that we're going to use to identify them.

0:51:040:51:08

So, it's where the personal effects are collected...

0:51:080:51:12

where we take the fingerprints, get the dental x-ray,

0:51:120:51:16

make measurements of the body, record tattoos and scars.

0:51:160:51:20

In the case of a natural disaster,

0:51:200:51:23

where it's going to be some time before we can return the body,

0:51:230:51:25

doing the embalming, the restoration, and the preservation of the body.

0:51:250:51:30

So that it can be returned in a sanitary condition to the families.

0:51:300:51:35

But even if emergency facilities like these could be set up,

0:51:400:51:43

they would soon be overwhelmed.

0:51:430:51:46

It's possible that millions of dead

0:51:460:51:49

would be left to decay where they died

0:51:490:51:53

and that brings with it yet another threat.

0:51:530:51:56

It would be a horrific mix of debris and, unfortunately,

0:51:590:52:04

human remains, animal remains.

0:52:040:52:06

So, you can imagine, after a few hours,

0:52:080:52:10

you would have a biological nightmare.

0:52:100:52:13

Lack of shelter, food, water,

0:52:160:52:21

and diseases like dysentery all become killers.

0:52:210:52:25

We have identified 500 different locations

0:52:300:52:36

that we could activate as emergency shelters.

0:52:360:52:41

Those are primarily public schools

0:52:420:52:44

and some of our city university buildings and facilities.

0:52:440:52:48

The capacity of the system is 600,000 people.

0:52:480:52:52

We don't look forward to a job

0:52:520:52:56

where we would have to shelter 600,000 people,

0:52:560:53:00

but that is the capacity of the system today.

0:53:000:53:04

It's simply impossible to plan for such a scale of disaster.

0:53:080:53:13

All these provisions will feed only 70,000 people for seven days.

0:53:130:53:19

Just a tiny fraction of the possible numbers of displaced survivors

0:53:190:53:23

in Manhattan alone.

0:53:230:53:26

Our mega-tsunami has triggered not only death and destruction

0:53:300:53:34

in the American East,

0:53:340:53:36

but a humanitarian crisis that could affect the entire nation.

0:53:360:53:41

Think of losing every single east coast shipping port.

0:53:420:53:47

That's essentially what we're talking about with a mega-tsunami.

0:53:470:53:51

If you lose those ports, you have a huge problem,

0:53:530:53:56

believe it or not, into the Midwest of the US.

0:53:560:53:58

All the way to the Mississippi River because a lot of that infrastructure, those rail hubs,

0:53:580:54:03

come right to the coast.

0:54:030:54:06

So, even if people weren't directly impacted by the tsunami itself,

0:54:060:54:12

they wouldn't have food coming to their supermarkets.

0:54:120:54:16

Far inland, many hundreds of miles

0:54:160:54:18

from the direct effects of the mega-tsunami,

0:54:180:54:21

there could be mass food shortages.

0:54:210:54:23

Most cities only have a two or three day supply of food,

0:54:250:54:29

so you think about cities like Atlanta,

0:54:290:54:31

you think about Memphis, you think about those inland areas

0:54:310:54:34

that get a lot of their material coming from ports on the east coast

0:54:340:54:38

and that's suddenly gone for years, perhaps, to recover -

0:54:380:54:42

that's an enormous problem.

0:54:420:54:44

And, ultimately, the scale of disaster

0:54:450:54:48

won't just be measured in lives lost.

0:54:480:54:51

No-one can be sure,

0:54:530:54:54

but a mega-tsunami could deliver a financial shock so great

0:54:540:55:00

that it's impact could change the global economy,

0:55:000:55:03

politics and the balance of East-West power, perhaps forever.

0:55:030:55:08

You think about how much disruption was caused

0:55:080:55:10

by September 11, 2001, attacks

0:55:100:55:13

and how much that disrupted the world economy.

0:55:130:55:16

Well, they were back up and running four days later.

0:55:160:55:18

Imagine if they weren't able to be back up and running in 40 days or 40 months.

0:55:180:55:23

It could be that the world's economy would recover,

0:55:260:55:29

as capitalists moved electronic money to safer havens.

0:55:290:55:33

There is some evidence,

0:55:350:55:37

as was the case with the Kobe earthquake of 1995,

0:55:370:55:41

that's natural disasters can even trigger investment and renewal.

0:55:410:55:45

But it's hard to imagine the fragile global economy bouncing back

0:55:470:55:52

from such devastation as this.

0:55:520:55:55

The truth is, no-one really knows...

0:55:550:55:58

..and, hopefully, given that landslide events

0:55:590:56:03

are, fortunately, rare,

0:56:030:56:05

no-one soon will get the chance to find out.

0:56:050:56:08

In the long-term, we know these ocean island collapses occur.

0:56:150:56:19

Around the world, there may be one of these enormous events

0:56:190:56:23

maybe once every 20,000 years, maybe only once every 50,000 years.

0:56:230:56:27

We can't say when the collapse is going to occur...

0:56:290:56:31

..but the problem with the Cumbre Vieja

0:56:340:56:36

is that it seems to already be close to failure.

0:56:360:56:40

So, the crucial question is not a matter of "if" but of "when".

0:56:430:56:48

We aren't prepared in the UK, for a tsunami.

0:57:020:57:06

No measures have been put in place to mitigate tsunamis.

0:57:060:57:10

Now, I think we need to learn from events, like Japan,

0:57:100:57:13

that that really isn't the best policy.

0:57:130:57:15

I think the question, "Are you prepared for a tsunami?"

0:57:170:57:21

is almost the wrong question because, to an extent,

0:57:210:57:23

you can't prepare for them, as Japan very clearly illustrated.

0:57:230:57:27

The Japanese were ready,

0:57:270:57:29

they prepared themselves for the potential impact of a tsunami wave.

0:57:290:57:34

Those defences were still inadequate.

0:57:340:57:37

The consequences were 15,000 dead

0:57:390:57:41

and the costliest natural catastrophe in the history of our planet.

0:57:410:57:44

Can we prevent the same thing that happened in Japan happening in Britain?

0:57:510:57:55

No. Japan is probably one of the best equipped countries in the world

0:57:550:58:00

in defending itself against tsunamis.

0:58:000:58:03

If they can't get it right...we can't.

0:58:030:58:07

And it's not a question of them getting it wrong,

0:58:070:58:10

it's a question of there's a limit of what we can do

0:58:100:58:12

against the forces of nature.

0:58:120:58:14

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0:58:420:58:45

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