
Browse content similar to Could We Survive a Mega-Tsunami?. Check below for episodes and series from the same categories and more!
| Line | From | To | |
|---|---|---|---|
For all our technological wonders, | 0:00:05 | 0:00:07 | |
mankind is vulnerable to a far greater power. | 0:00:07 | 0:00:12 | |
The wrath and fury that only our planet can unleash. | 0:00:15 | 0:00:20 | |
Volcanoes... | 0:00:25 | 0:00:28 | |
earthquakes... | 0:00:28 | 0:00:30 | |
and silent assassins, unseen until it's too late. | 0:00:30 | 0:00:35 | |
Tsunamis that bring death and devastation from the sea. | 0:00:43 | 0:00:48 | |
On Boxing Day 2004, | 0:00:53 | 0:00:56 | |
nearly a quarter of a million people were killed in southern Asia. | 0:00:56 | 0:01:00 | |
On March 11, 2011, Japan | 0:01:02 | 0:01:06 | |
and destruction that came within a whisker of nuclear catastrophe. | 0:01:06 | 0:01:11 | |
But scientists believe | 0:01:13 | 0:01:15 | |
that something even more destructive lies in wait. | 0:01:15 | 0:01:19 | |
Something that will one day strike us in the West. | 0:01:19 | 0:01:23 | |
A wave so many times bigger than any conventional tsunami, | 0:01:25 | 0:01:30 | |
it's been dubbed a mega-tsunami. | 0:01:30 | 0:01:34 | |
Now, using the very latest science, powerful computer models | 0:01:46 | 0:01:54 | |
and the terrible evidence of all to recent events, | 0:01:54 | 0:01:58 | |
this is the story of how some experts believe the greatest | 0:01:58 | 0:02:01 | |
natural disaster in human history might one day unfold. | 0:02:01 | 0:02:06 | |
The biggest wave ever seen... | 0:02:10 | 0:02:13 | |
threatening cataclysmic destruction | 0:02:13 | 0:02:16 | |
of some of the world's greatest cities... | 0:02:16 | 0:02:19 | |
..death and devastation on an unprecedented scale | 0:02:22 | 0:02:27 | |
and economic fallout that could reshape the future | 0:02:27 | 0:02:31 | |
of the entire world. | 0:02:31 | 0:02:33 | |
It will all begin on one of Britain's most popular | 0:02:52 | 0:02:55 | |
tourist resorts... | 0:02:55 | 0:02:58 | |
the Canary Islands, | 0:02:58 | 0:03:00 | |
with an event that last occurred in 1971 | 0:03:00 | 0:03:04 | |
and, before that, in 1949. | 0:03:04 | 0:03:07 | |
A volcanic eruption. | 0:03:11 | 0:03:13 | |
'The Canary Islands' volcano of La Palma | 0:03:13 | 0:03:16 | |
'erupted for the first time in two centuries. | 0:03:16 | 0:03:18 | |
'Menacing the population | 0:03:18 | 0:03:20 | |
'and is turning night into day with blazing rivers of molten lava.' | 0:03:20 | 0:03:23 | |
People think of volcanoes of being, sort of, cone shaped | 0:03:30 | 0:03:33 | |
with a little hole in the top | 0:03:33 | 0:03:35 | |
and those are what we called stratovolcanoes, | 0:03:35 | 0:03:37 | |
they are the traditional volcano shape, | 0:03:37 | 0:03:39 | |
but this is very different, this is an elongate structure. | 0:03:39 | 0:03:43 | |
La Palma is one of a chain of volcanic islands, | 0:03:48 | 0:03:51 | |
lying off the coast of West Africa, | 0:03:51 | 0:03:53 | |
that includes Gran Canaria and Tenerife. | 0:03:53 | 0:03:56 | |
Its most active region is a high mountain ridge | 0:04:01 | 0:04:04 | |
called La Cumbre Vieja. | 0:04:04 | 0:04:06 | |
The Cumbre Vieja occupies the southernmost part of the island | 0:04:08 | 0:04:12 | |
and it forms this north-south lined ridge. | 0:04:12 | 0:04:16 | |
The whole ridge is, sort of, pockmarked craters and holes, | 0:04:16 | 0:04:19 | |
and then you have lava flows heading off in both directions, | 0:04:19 | 0:04:22 | |
to the west and east, from these particular craters. | 0:04:22 | 0:04:25 | |
In 1949, quite a small eruption, in terms of volume of lava, | 0:04:30 | 0:04:36 | |
the volume of magma, erupted but during the eruption | 0:04:36 | 0:04:39 | |
there had been a series of very strong earthquakes | 0:04:39 | 0:04:42 | |
and a fault line had developed along the crest of the volcano. | 0:04:42 | 0:04:46 | |
A giant gash had opened up along the island's ridge, | 0:04:51 | 0:04:55 | |
four kilometres long and up to four metres wide. | 0:04:55 | 0:04:59 | |
Part of the west flank dropped a couple of metres towards the sea | 0:05:02 | 0:05:07 | |
and then stopped, and that's really what tells us that something | 0:05:07 | 0:05:10 | |
other than just magma coming up was going on during that eruption. | 0:05:10 | 0:05:13 | |
That geological rift is the reason why this volcano | 0:05:19 | 0:05:23 | |
could one day trigger a mega-tsunami. | 0:05:23 | 0:05:27 | |
Because ever since 1949, | 0:05:32 | 0:05:35 | |
the peaceful island of La Palma has been a time bomb... | 0:05:35 | 0:05:41 | |
and some scientists believe that today another eruption | 0:05:41 | 0:05:45 | |
could send 500 cubic kilometres of it crashing into the sea. | 0:05:45 | 0:05:50 | |
A colossal landslide with enough energy | 0:05:53 | 0:05:56 | |
to generate the biggest wave humanity will have ever seen. | 0:05:56 | 0:06:00 | |
Unleashed not upon the Pacific but the Atlantic and heading for us... | 0:06:02 | 0:06:08 | |
..the first mega-tsunami in recorded history. | 0:06:10 | 0:06:14 | |
The terrible human cost of the recent Pacific tsunamis | 0:06:30 | 0:06:33 | |
came from underwater earthquakes. | 0:06:33 | 0:06:36 | |
But recent history has already shown that the collapse of a volcano | 0:06:44 | 0:06:49 | |
could unleash even greater devastation. | 0:06:49 | 0:06:52 | |
Most people think of volcanoes as these are unchanging sentinels | 0:06:54 | 0:06:58 | |
of solid rock that persists for many millions of years | 0:06:58 | 0:07:00 | |
and, really, just go on getting bigger, | 0:07:00 | 0:07:03 | |
but they are better viewed, really, as unstable piles of rubble. | 0:07:03 | 0:07:07 | |
It was the Mount St Helens eruption in 1980 that really provided us | 0:07:08 | 0:07:12 | |
with that first visual proof that volcanoes did collapse. | 0:07:12 | 0:07:16 | |
'This is the CBS Evening News with Dan Rather.' | 0:07:16 | 0:07:20 | |
It is an event that defies superlatives. | 0:07:20 | 0:07:23 | |
One geologist said today, "There is no record today, in geology, | 0:07:23 | 0:07:27 | |
"in the last 4,000 years, of anything like this happening before. | 0:07:27 | 0:07:31 | |
"The tremendous lateral blast is unprecedented." | 0:07:31 | 0:07:34 | |
This is the only photographic evidence that we have | 0:07:35 | 0:07:38 | |
for a volcano lateral collapse actually happening. | 0:07:38 | 0:07:42 | |
'This sequence of photos was taken during the first 60 seconds | 0:07:42 | 0:07:45 | |
'of the mountain's eruption, | 0:07:45 | 0:07:47 | |
'beginning shortly after 8.30 on Sunday morning.' | 0:07:47 | 0:07:50 | |
It was really an iconic moment, which taught us that volcanoes | 0:07:51 | 0:07:54 | |
did things that we didn't think they did before, and that is that | 0:07:54 | 0:07:57 | |
instead of just erupting upwards they can also erupt sideways. | 0:07:57 | 0:08:01 | |
You can see the bulge dislodging, | 0:08:05 | 0:08:08 | |
forming this landslide which heads off northwards. | 0:08:08 | 0:08:11 | |
And then this massive column of ash, which heads up into the atmosphere, | 0:08:14 | 0:08:18 | |
and ultimately covers the entire region. | 0:08:18 | 0:08:20 | |
The question we all asked ourselves at the time was, | 0:08:22 | 0:08:25 | |
"What would've happened if that collapse had occurred into water?" | 0:08:25 | 0:08:28 | |
What would happen would be the conversion | 0:08:31 | 0:08:34 | |
of a vast amount of energy into an ocean-going wave... | 0:08:34 | 0:08:37 | |
..starting off up to one kilometre high | 0:08:39 | 0:08:42 | |
and with the power to cross oceans at the speed of a jet aircraft... | 0:08:42 | 0:08:47 | |
..ready to make landfall with potentially apocalyptic results. | 0:08:48 | 0:08:52 | |
Startlingly, it wouldn't be the first time that a landslide | 0:09:08 | 0:09:11 | |
has called a tsunami on the Canary Islands. | 0:09:11 | 0:09:15 | |
One marine geologist thinks he's found evidence of a past event... | 0:09:15 | 0:09:20 | |
..not on La Palma but nearby on Gran Canaria | 0:09:25 | 0:09:31 | |
at a site called Agaete. | 0:09:31 | 0:09:33 | |
What we have here are tiny pieces of shell - that's about two centimetres. | 0:09:36 | 0:09:43 | |
That's a mollusc, it comes from the sea. | 0:09:43 | 0:09:46 | |
What is strange about finding them here | 0:09:46 | 0:09:50 | |
is that they are 50 metres above... | 0:09:50 | 0:09:55 | |
the level in the sea at which they usually live. | 0:09:55 | 0:09:59 | |
Shells like these can be found three kilometres inland | 0:10:00 | 0:10:04 | |
and 200 metres above the sea - | 0:10:04 | 0:10:07 | |
too far to have been carried there by any storm. | 0:10:07 | 0:10:11 | |
And, without evidence of changes in sea level, | 0:10:11 | 0:10:14 | |
there can be only one explanation. | 0:10:14 | 0:10:17 | |
If they weren't laid down by a high sea level, | 0:10:17 | 0:10:20 | |
if they weren't laid down by a storm, then what was the source? | 0:10:20 | 0:10:24 | |
We need something to have created a wave 200 metres high. | 0:10:25 | 0:10:30 | |
Dave Tappin's wave on Gran Canaria was far too big | 0:10:35 | 0:10:39 | |
to have been made by an earthquake. | 0:10:39 | 0:10:41 | |
The only answer, in my estimation, is the collapse of a volcano. | 0:10:42 | 0:10:48 | |
It's unlikely to have been Gran Canaria but the nearest island, | 0:10:48 | 0:10:54 | |
100 kilometres away, just over there, where I'm pointing, is Tenerife. | 0:10:54 | 0:10:58 | |
On the coastline, facing Gran Canaria, there is a major collapse | 0:11:00 | 0:11:05 | |
and that collapse is called Guimar. | 0:11:05 | 0:11:08 | |
The area where we are now, in the Guimar Valley, in Tenerife, | 0:11:22 | 0:11:26 | |
it's around about ten kilometres wide along the coast, | 0:11:26 | 0:11:31 | |
extends several kilometres inland, so it's a big feature. | 0:11:31 | 0:11:36 | |
Where now there is this broad, flat-floored valley, | 0:11:37 | 0:11:42 | |
there would have originally been a steep sided volcanic cone. | 0:11:42 | 0:11:47 | |
So, the area that collapsed is over to our right | 0:11:49 | 0:11:53 | |
and on the left we can see the lavas that formed the old volcano. | 0:11:53 | 0:11:59 | |
And between the two we have this enormous cliff. | 0:12:01 | 0:12:04 | |
But originally that would have been the sidewall of the landslide. | 0:12:05 | 0:12:10 | |
Over in the distance, from here, | 0:12:13 | 0:12:15 | |
we can see the tops of the mountains of Gran Canaria, | 0:12:15 | 0:12:19 | |
round about 100 kilometres away, so it's very easy to imagine | 0:12:19 | 0:12:23 | |
that the Guimar landside, as it went down into the ocean, | 0:12:23 | 0:12:28 | |
would have generated a tsunami that spread across the ocean | 0:12:28 | 0:12:32 | |
to Gran Canaria and produced the tsunami deposits at Agaete. | 0:12:32 | 0:12:36 | |
This tsunami would drive across the ocean, | 0:12:40 | 0:12:43 | |
between Tenerife and Gran Canaria, | 0:12:43 | 0:12:46 | |
and strike in this particular location, | 0:12:46 | 0:12:49 | |
could easily build up after it hit the coastline, | 0:12:49 | 0:12:52 | |
travel inland to heights above sea level of hundreds of metres. | 0:12:52 | 0:12:56 | |
But even Tappin's tsunami would pale alongside the wave | 0:12:59 | 0:13:03 | |
that would be created by a collapse of the entire mountain flank | 0:13:03 | 0:13:07 | |
of La Cumbre Vieja. | 0:13:07 | 0:13:09 | |
Not everyone agrees, but many experts think that such an event | 0:13:11 | 0:13:16 | |
would have consequences of global proportions. | 0:13:16 | 0:13:18 | |
It's not surprising that this tiny volcano has become | 0:13:21 | 0:13:24 | |
so intensely studied. | 0:13:24 | 0:13:26 | |
This is the story of a scientific model | 0:13:31 | 0:13:34 | |
of a volcanic collapse of La Palma projected into the near future. | 0:13:34 | 0:13:40 | |
By using reconstructions... | 0:13:42 | 0:13:44 | |
Tens of thousands of people are feared dead and hundreds of thousands | 0:13:45 | 0:13:49 | |
are still missing following the worst natural disaster in history. | 0:13:49 | 0:13:53 | |
..real archive footage from previous natural disasters | 0:13:53 | 0:13:58 | |
and graphical representations of what such a wave would do... | 0:13:58 | 0:14:02 | |
..we can plot out the possible unfolding of events | 0:14:04 | 0:14:08 | |
that one day could really happen. | 0:14:08 | 0:14:10 | |
Our scenario begins | 0:14:21 | 0:14:23 | |
one ordinary day on the island of La Palma itself. | 0:14:23 | 0:14:26 | |
No-one knows it yet, | 0:14:28 | 0:14:30 | |
but it's just five days before disaster will strike. | 0:14:30 | 0:14:34 | |
Seismic monitoring will register a sudden increase in activity. | 0:14:40 | 0:14:44 | |
Higher! Let's go, come up. | 0:14:44 | 0:14:47 | |
But, since earthquakes here are common, | 0:14:47 | 0:14:50 | |
no-one will take too much notice... | 0:14:50 | 0:14:52 | |
..but then local wildlife will begin to die, | 0:15:03 | 0:15:06 | |
succumbing to carbon monoxide fumes emanating from the ground. | 0:15:06 | 0:15:12 | |
A harbinger that something more dangerous is afoot. | 0:15:12 | 0:15:15 | |
An event that no-one can ignore. | 0:15:23 | 0:15:26 | |
La Palma's La Cumbre Vieja is erupting once more. | 0:15:55 | 0:15:59 | |
In one instant, a whole section of the island is dislodged. | 0:16:13 | 0:16:18 | |
Breaking up as it falls, an entire mountainside plunges into the sea... | 0:16:26 | 0:16:33 | |
at the speed of an express train. | 0:16:33 | 0:16:36 | |
We see the landslide first generating an enormous wave. | 0:16:46 | 0:16:50 | |
Within seconds, the surrounding ocean is distorted. | 0:16:59 | 0:17:02 | |
At first it forms a huge dome of water... | 0:17:06 | 0:17:09 | |
..and then a giant wall... | 0:17:11 | 0:17:13 | |
..on a scale that is almost unimaginable. | 0:17:15 | 0:17:20 | |
A mega-tsunami. | 0:17:20 | 0:17:21 | |
That wave could be as much as a kilometre high. | 0:17:24 | 0:17:28 | |
In terms of the height, you're talking about | 0:17:30 | 0:17:32 | |
more than two Empire State Buildings on top of one another | 0:17:32 | 0:17:35 | |
or three of London's Shard piled on top of one another. | 0:17:35 | 0:17:38 | |
This is an immense mass of water. | 0:17:40 | 0:17:42 | |
Not just fast, but fast. | 0:17:44 | 0:17:48 | |
Travelling at up to 800 miles an hour, | 0:17:48 | 0:17:51 | |
the giant wave surges out in all directions. | 0:17:51 | 0:17:54 | |
Immediately in its path, the highly populated island of Tenerife, | 0:17:56 | 0:18:01 | |
less than 100 miles away. | 0:18:01 | 0:18:03 | |
In less than ten minutes the wave makes landfall. | 0:18:09 | 0:18:13 | |
Locals and holidaymakers alike do all they can to outrun it. | 0:18:17 | 0:18:21 | |
Within minutes, the wave has claimed its first victims. | 0:18:51 | 0:18:55 | |
I don't think there's any doubt that, | 0:18:57 | 0:18:59 | |
however big the collapse of the west flank of Cumbre Vieja, | 0:18:59 | 0:19:03 | |
the initial wave will be very catastrophic | 0:19:03 | 0:19:06 | |
for the islands themselves. | 0:19:06 | 0:19:07 | |
So, you're talking about thousands of people dead and destruction | 0:19:11 | 0:19:14 | |
on a scale that we've never seen in this part of the world before. | 0:19:14 | 0:19:17 | |
With less than ten minutes to react, | 0:19:22 | 0:19:25 | |
it's hard to see many of the two and a half million locals | 0:19:25 | 0:19:29 | |
and visitors to the Canary Islands escaping with their lives. | 0:19:29 | 0:19:33 | |
But even as the wave devastates neighbouring islands, | 0:19:36 | 0:19:40 | |
La Palma continues to erupt. | 0:19:40 | 0:19:42 | |
The mountain of La Cumbre Vieja is still collapsing... | 0:19:45 | 0:19:48 | |
..releasing yet more energy into the sea. | 0:19:51 | 0:19:55 | |
Our mega-tsunami's journey of destruction has only just begun. | 0:20:04 | 0:20:09 | |
Within 20 or 30 minutes, all of the waves have spread out from La Palma | 0:20:10 | 0:20:17 | |
and they've started this long journey out across the Atlantic Ocean. | 0:20:17 | 0:20:23 | |
There's been no time to raise the alarm. | 0:20:27 | 0:20:31 | |
Within 60 minutes, 90 metre waves will strike | 0:20:31 | 0:20:35 | |
the coast of West Africa. | 0:20:35 | 0:20:36 | |
Over the following hours, these waves will devastate | 0:20:38 | 0:20:41 | |
the coastlines of Europe. | 0:20:41 | 0:20:43 | |
While across the Atlantic Ocean, millions of Americans lie sleeping. | 0:20:50 | 0:20:54 | |
Nothing can stop a wave this size. | 0:20:56 | 0:20:59 | |
Only landfall and the coastal cities that lie in its path. | 0:20:59 | 0:21:05 | |
It could be the costliest natural catastrophe | 0:21:05 | 0:21:07 | |
in the history of our planet. | 0:21:07 | 0:21:09 | |
While geologists have studied how a landslide tsunami could be caused, | 0:21:22 | 0:21:27 | |
wave experts like Nils Kerpin are working out | 0:21:27 | 0:21:30 | |
just how a mega-tsunami would travel once unleashed. | 0:21:30 | 0:21:35 | |
A miniature Cumbre Vieja | 0:21:40 | 0:21:44 | |
reveals exactly how fast waves would radiate out from La Palma. | 0:21:44 | 0:21:48 | |
See that the wave that occurs due to the landslide will propagate | 0:21:49 | 0:21:54 | |
and encircle around the island. | 0:21:54 | 0:21:56 | |
Using physical modelling, | 0:22:05 | 0:22:07 | |
Nils can analyse the very anatomy of the giant wave. | 0:22:07 | 0:22:11 | |
Here we see the beginning of some landslides | 0:22:17 | 0:22:20 | |
and we can see air bubbles that are rushing back | 0:22:20 | 0:22:25 | |
and running up the slope of the remaining island. | 0:22:25 | 0:22:28 | |
From the very moment it's first formed | 0:22:30 | 0:22:33 | |
to its height and its speed as it spreads. | 0:22:33 | 0:22:37 | |
The faster this landslides occurs, | 0:22:37 | 0:22:40 | |
the more energy will be induced into the water body. | 0:22:40 | 0:22:44 | |
Fluid science can model not only the wave itself | 0:22:48 | 0:22:53 | |
but exactly how its journey progresses. | 0:22:53 | 0:22:56 | |
Northwards towards Europe | 0:22:57 | 0:23:00 | |
and unchecked across the open Atlantic. | 0:23:00 | 0:23:03 | |
That science can help us to chart what will happen in our scenario | 0:23:06 | 0:23:12 | |
in the hours to come. | 0:23:12 | 0:23:13 | |
It's 80 minutes after the initial landslide | 0:23:25 | 0:23:29 | |
and, to the east, the wave, still up to 60 metres high, | 0:23:29 | 0:23:34 | |
is minutes from its first major cities... | 0:23:34 | 0:23:36 | |
..Casablanca, in Morocco, and its capital Rabat. | 0:23:39 | 0:23:43 | |
A combined population of six million. | 0:23:45 | 0:23:47 | |
It is estimated that two thirds of them | 0:23:50 | 0:23:52 | |
will not survive the wave's impact. | 0:23:52 | 0:23:55 | |
Only now are the first reports of the unfolding disaster | 0:24:10 | 0:24:14 | |
beginning to emerge. | 0:24:14 | 0:24:16 | |
It's likely that, before any news agencies begin to report, | 0:24:22 | 0:24:27 | |
Twitter, Facebook and mobile calls will carry the first images | 0:24:27 | 0:24:32 | |
of unfolding disaster to the world. | 0:24:32 | 0:24:34 | |
In London, the Prime Minister becomes aware of events. | 0:24:39 | 0:24:42 | |
When a disaster happens that dominates everything, | 0:24:43 | 0:24:47 | |
the whole diary's cleared. | 0:24:47 | 0:24:49 | |
The PM summons the relevant government departments | 0:24:51 | 0:24:55 | |
and representatives of the emergency services | 0:24:55 | 0:24:58 | |
to the Cobra response room. | 0:24:58 | 0:25:00 | |
Cobra's that kind of high-tech room with lots of links to police, | 0:25:00 | 0:25:05 | |
the fire services, etc, round the country. | 0:25:05 | 0:25:08 | |
But they have little time to plan. | 0:25:10 | 0:25:13 | |
Just 30 minutes after Casablanca, the wave reaches Europe. | 0:25:19 | 0:25:24 | |
It is still the height of a two-storey house. | 0:25:32 | 0:25:35 | |
The coastal capital of Lisbon is devastated. | 0:25:37 | 0:25:41 | |
Back in Westminster, the Cobra meeting room | 0:25:55 | 0:25:58 | |
is now a centre of intense activity. | 0:25:58 | 0:26:01 | |
So, the first thing we want to know | 0:26:03 | 0:26:05 | |
is, "Just how big is this? What's actually happening?" | 0:26:05 | 0:26:08 | |
Often, if you've got a TV screen on, | 0:26:11 | 0:26:14 | |
you'll know as much as the person in the centre of Whitehall. | 0:26:14 | 0:26:18 | |
As likely as not they'll have Sky and BBC 24-hour, | 0:26:20 | 0:26:23 | |
and they'd be following Twitter and social media. | 0:26:23 | 0:26:26 | |
There is always, always a period where there is a kind of fog of uncertainty. | 0:26:27 | 0:26:31 | |
I think the key point is to alert the emergency services, | 0:26:31 | 0:26:36 | |
so that they are prepared for it to happen. | 0:26:36 | 0:26:39 | |
After hitting Lisbon, the emergency services have just three hours | 0:26:44 | 0:26:49 | |
before the wave strikes Britain. | 0:26:49 | 0:26:51 | |
The Environment Agency issues flood warnings to the south coast. | 0:26:53 | 0:26:58 | |
Fire, ambulance and rescue units are put on standby. | 0:27:00 | 0:27:05 | |
Police clear the streets of southern coastal towns, | 0:27:07 | 0:27:11 | |
evacuating schools and vulnerable communities. | 0:27:11 | 0:27:14 | |
Back in Whitehall, the Government has two work out what to say | 0:27:20 | 0:27:25 | |
and how to deal with increasing public panic | 0:27:25 | 0:27:29 | |
as awareness of the scale of unfolding events spreads. | 0:27:29 | 0:27:32 | |
A giant tsunami is spreading throughout the Atlantic basin. | 0:27:34 | 0:27:38 | |
Waves of up to 40 metres high have already devastated | 0:27:38 | 0:27:41 | |
the coasts of Portugal, North Africa and Spain. | 0:27:41 | 0:27:44 | |
Scientists estimate that the wave is travelling at approximately 500mph. | 0:27:44 | 0:27:49 | |
It's expected to move across the Atlantic... | 0:27:49 | 0:27:51 | |
You're still building up information as well as trying to move people. | 0:27:51 | 0:27:54 | |
That'll be the time that the media are saying, | 0:27:54 | 0:27:56 | |
"What are you doing about it? What's happening?" | 0:27:56 | 0:27:58 | |
The key test of the Government will be to show they're responding, | 0:27:58 | 0:28:01 | |
to outline the measures they're taking. | 0:28:01 | 0:28:03 | |
But the measures they're taking | 0:28:03 | 0:28:05 | |
are in the time when they really don't know how serious it is. | 0:28:05 | 0:28:07 | |
Just three hours after the first UK warnings, | 0:28:09 | 0:28:13 | |
a wave up to 25 metres high makes its first landfall in Britain... | 0:28:13 | 0:28:18 | |
..on Cornwall. | 0:28:20 | 0:28:22 | |
In the immediate aftermath, say two or three hours after it's hit, | 0:28:36 | 0:28:39 | |
they'll still be confusion. | 0:28:39 | 0:28:41 | |
I mean, we're probably talking about a very, very wide area of hundreds of miles. | 0:28:41 | 0:28:44 | |
So, finding out what's happening in a cove in Devon or Cornwall, | 0:28:44 | 0:28:48 | |
I mean, you know, how is that going to get back? | 0:28:48 | 0:28:50 | |
I mean, you could well have communities wiped out. | 0:28:50 | 0:28:52 | |
We can get some idea of the impact of a seven to ten metre wave, | 0:29:08 | 0:29:12 | |
on the UK south coast, | 0:29:12 | 0:29:13 | |
by looking at what happened in the Indian Ocean in 2004, | 0:29:13 | 0:29:17 | |
in places like Sri Lanka and Thailand. | 0:29:17 | 0:29:19 | |
The level of destruction was immense | 0:29:21 | 0:29:23 | |
and the death toll was in the tens of thousands. | 0:29:23 | 0:29:26 | |
You could say that the population of the south coast of the UK | 0:29:29 | 0:29:32 | |
is probably quite a bit higher, | 0:29:32 | 0:29:34 | |
so that sort of wave would be immensely destructive in the UK. | 0:29:34 | 0:29:38 | |
From Cornwall, the wave surges through into the Irish Sea | 0:29:40 | 0:29:45 | |
and through the English Channel, | 0:29:45 | 0:29:47 | |
engulfing much of Britain's south coast. | 0:29:47 | 0:29:50 | |
The aspect that makes a tsunami so devastating is its wavelength | 0:29:51 | 0:29:55 | |
and how long it is. | 0:29:55 | 0:29:56 | |
A storm wave might be ten, 20, 30 metres long, 40 metres long, | 0:30:02 | 0:30:05 | |
50 metres long. | 0:30:05 | 0:30:07 | |
In the case of a tsunami, | 0:30:07 | 0:30:09 | |
we have a wave that is 200 or 300 kilometres long. | 0:30:09 | 0:30:12 | |
Unlike a storm wave, a tsunami just keeps on coming - | 0:30:14 | 0:30:19 | |
mile after mile of it. | 0:30:19 | 0:30:21 | |
Seawater floods our southern cities | 0:30:24 | 0:30:27 | |
and penetrates low-lying farmland for miles inland. | 0:30:27 | 0:30:32 | |
It not only runs up the coastline and inundates the land, | 0:30:36 | 0:30:40 | |
but it continues to flow inland, as if it's a river flowing over | 0:30:40 | 0:30:44 | |
the land and scouring out, and removing things in its path. | 0:30:44 | 0:30:49 | |
So, it's the inundation, it's the wavelength, | 0:30:49 | 0:30:51 | |
that actually makes these events so dangerous. | 0:30:51 | 0:30:54 | |
Models differ on what the wave might do to our southern cities | 0:30:57 | 0:31:01 | |
as it works its way east. | 0:31:01 | 0:31:03 | |
Towns such as Brighton would probably survive, | 0:31:04 | 0:31:08 | |
but would suffer serious disruption. | 0:31:08 | 0:31:10 | |
In our scenario, London, our capital, | 0:31:29 | 0:31:33 | |
tucked in from the North Sea, is safely sheltered. | 0:31:33 | 0:31:36 | |
Britain, it seems, will survive the worst calamities seen elsewhere. | 0:31:40 | 0:31:46 | |
The wave, however, as well as travelling east to Africa | 0:31:51 | 0:31:56 | |
and north to Europe is also heading west, across the Atlantic. | 0:31:56 | 0:32:01 | |
And there is a whole new nation is waking up - America. | 0:32:04 | 0:32:09 | |
'Good morning, New York. It's a beautiful day out there in the city | 0:32:09 | 0:32:13 | |
'but here's a word of advice, enjoy it while you can. | 0:32:13 | 0:32:16 | |
'The weathermen says there's going to be some rain this afternoon | 0:32:16 | 0:32:19 | |
'and temperatures could drop dramatically by the end of the day.' | 0:32:19 | 0:32:23 | |
It's 7am. As the tsunami is devastating southern Britain, | 0:32:23 | 0:32:28 | |
it's three hours away from New York. | 0:32:28 | 0:32:31 | |
1,500 miles off the coast, the wave hurtles west at incredible speed. | 0:32:39 | 0:32:47 | |
The deeper the water, the faster the wave moves. | 0:32:50 | 0:32:53 | |
So, in five kilometres of water | 0:32:53 | 0:32:55 | |
the wave will move at 800 kilometres an hour. | 0:32:55 | 0:32:58 | |
It's travelling at the speed of a jet plane. | 0:32:58 | 0:33:01 | |
Bear in mind, it's not the water that is moving. | 0:33:01 | 0:33:05 | |
So, you can't imagine water moving at 800 kilometres an hour, | 0:33:05 | 0:33:08 | |
it's the energy of the wave. | 0:33:08 | 0:33:10 | |
The particles of water are pushing against each other | 0:33:10 | 0:33:13 | |
and so, if you like, each is knocking against the next | 0:33:13 | 0:33:16 | |
and it's moving the energy across the oceans. | 0:33:16 | 0:33:19 | |
For evidence of how tsunami waves can travel between continents, | 0:33:23 | 0:33:27 | |
scientists, once again, only need to look to the past. | 0:33:27 | 0:33:31 | |
In particular, evidence of | 0:33:32 | 0:33:35 | |
an earthquake generated tsunami that began in Chile in 1960. | 0:33:35 | 0:33:40 | |
'Devastation untold, a death toll close on 5,000, | 0:33:42 | 0:33:46 | |
'is part of the reckoning that staggers Chile. In Concepcion, city of...' | 0:33:46 | 0:33:50 | |
The earthquake itself caused lots of damage, significant damage | 0:33:50 | 0:33:53 | |
but it also created a very large tsunami. | 0:33:53 | 0:33:57 | |
That tsunami did cause damage in Chile itself, | 0:33:57 | 0:34:00 | |
but what was interesting about that one was that the damage it caused | 0:34:00 | 0:34:03 | |
further afield was also significant. | 0:34:03 | 0:34:06 | |
'Incredibly, Hawaii, 6,000 miles away in mid-Pacific, | 0:34:06 | 0:34:09 | |
'was struck by four gigantic tidal waves. | 0:34:09 | 0:34:12 | |
'On surged the terrifying walls of water as far as the Japanese coast | 0:34:12 | 0:34:16 | |
'9,000 miles from Chile.' | 0:34:16 | 0:34:17 | |
And that really brought home the fact that a tsunami happening | 0:34:20 | 0:34:24 | |
one side of the ocean can have a dramatic impact | 0:34:24 | 0:34:27 | |
the other side of the ocean. | 0:34:27 | 0:34:28 | |
The wrath of volcanoes and earthquakes is all too evident, | 0:34:31 | 0:34:35 | |
but often their violence is geographically limited. | 0:34:35 | 0:34:38 | |
But tsunamis are different. | 0:34:39 | 0:34:43 | |
Fluid dynamics means that the ocean itself can carry the energy | 0:34:44 | 0:34:49 | |
of a tsunami over thousands of miles and in all directions. | 0:34:49 | 0:34:55 | |
30 minutes after the northern face of the wave first struck Cornwall, | 0:35:03 | 0:35:08 | |
its western edge is just 1,200 miles from a whole new nation. | 0:35:08 | 0:35:13 | |
In the US, 40 million people | 0:35:15 | 0:35:18 | |
live within 40 kilometres of the coastline. | 0:35:18 | 0:35:20 | |
And of those 40 million people, | 0:35:20 | 0:35:23 | |
something like 30 million of them | 0:35:23 | 0:35:25 | |
live within ten metres, vertically, of the shoreline. | 0:35:25 | 0:35:30 | |
If you're looking at these extreme events, like a tsunami, | 0:35:32 | 0:35:35 | |
that can put ten, 20, 30 metre waves at the shoreline, | 0:35:35 | 0:35:39 | |
that's an incredibly vulnerable population. | 0:35:39 | 0:35:43 | |
Atlantic City, Washington, Boston... | 0:35:43 | 0:35:49 | |
and New York. | 0:35:49 | 0:35:51 | |
Major cities along the coast all lie directly in its path. | 0:35:55 | 0:35:59 | |
-ALARM BEEPING -'Short period alarm.' | 0:36:03 | 0:36:07 | |
'Short period alarm.' | 0:36:07 | 0:36:09 | |
America is equipped with systems | 0:36:09 | 0:36:12 | |
capable of detecting an inbound tsunami. | 0:36:12 | 0:36:15 | |
The first is a network of seismometers, | 0:36:15 | 0:36:18 | |
located around the world, | 0:36:18 | 0:36:20 | |
which feed real-time data to a monitoring station in Alaska. | 0:36:20 | 0:36:25 | |
This shows the signal from all the different seismometers | 0:36:25 | 0:36:28 | |
that come in to the centre. Coming in in what we call real-time. | 0:36:28 | 0:36:32 | |
If there's anything that significant, it will trigger an alarm | 0:36:32 | 0:36:35 | |
and that will bring the guys in to take a look at the event. | 0:36:35 | 0:36:38 | |
But this system is designed to detect tsunamis generated by earthquakes. | 0:36:39 | 0:36:45 | |
Not a distant landslide | 0:36:45 | 0:36:47 | |
like the collapse of La Cumbre Vieja on La Palma. | 0:36:47 | 0:36:51 | |
Landslide generated tsunamis are very hard for us to respond to. | 0:36:51 | 0:36:54 | |
They do not show up on our seismic networks in the same way that earthquakes do. | 0:36:54 | 0:36:58 | |
Much, much more challenging. | 0:36:58 | 0:37:00 | |
A second line of defence is a network of deep ocean sensors | 0:37:02 | 0:37:06 | |
called DARTs, designed to detect changes in water pressure | 0:37:06 | 0:37:11 | |
caused by passing waves. | 0:37:11 | 0:37:13 | |
If there was a tsunami generated in the Canary Islands, | 0:37:13 | 0:37:16 | |
we would see impacts on our DART in the central Atlantic Ocean. | 0:37:16 | 0:37:21 | |
The DART system would raise the alarm, | 0:37:23 | 0:37:26 | |
but just three to four hours before the waves hit the coast. | 0:37:26 | 0:37:30 | |
The likelihood, though, is that, for all their sophistication, | 0:37:43 | 0:37:48 | |
these technological detection measures would do well | 0:37:48 | 0:37:51 | |
to beat the speed of reports coming through social media. | 0:37:51 | 0:37:55 | |
For America, news of the mega-tsunami's impact in Africa and Europe | 0:37:58 | 0:38:04 | |
would throw their own fate into sharp relief. | 0:38:04 | 0:38:07 | |
New York City is 8.4 million people who live on 302 square miles. | 0:38:12 | 0:38:19 | |
That is three islands and a peninsula, | 0:38:19 | 0:38:21 | |
mostly about 50 feet above the waterline. | 0:38:21 | 0:38:24 | |
It is a world-class city with enormous strengths | 0:38:26 | 0:38:29 | |
and also significant vulnerabilities. | 0:38:29 | 0:38:32 | |
An example is the island of Manhattan, | 0:38:34 | 0:38:36 | |
which has a population of about 1.5 million. | 0:38:36 | 0:38:40 | |
That population doubles every business day | 0:38:40 | 0:38:42 | |
to about three million people. | 0:38:42 | 0:38:44 | |
For the city authorities, it's a question of how many people | 0:38:47 | 0:38:51 | |
you might be able to save. | 0:38:51 | 0:38:53 | |
New York's Office of Emergency Management is responsible | 0:38:57 | 0:39:01 | |
for coordinating the response to any natural disaster. | 0:39:01 | 0:39:04 | |
We have spent the last ten years analysing the roadway network | 0:39:06 | 0:39:13 | |
and the mass transit network, and the population, | 0:39:13 | 0:39:18 | |
and determining how long it would take to evacuate. | 0:39:18 | 0:39:24 | |
The city's rail network would be the primary means of escape. | 0:39:27 | 0:39:31 | |
And yet, for all the evacuation plans in place, | 0:39:36 | 0:39:40 | |
there's a terrible irony. | 0:39:40 | 0:39:41 | |
Even in the apparent knowledge that disaster is imminent, | 0:39:43 | 0:39:47 | |
studies have shown that whole populations can go into denial. | 0:39:47 | 0:39:52 | |
Refusing to accept that the danger is real. | 0:39:52 | 0:39:56 | |
So, if we can get people to think, "This IS going to happen to me, | 0:39:59 | 0:40:04 | |
"I AM at risk, my family is at risk," | 0:40:04 | 0:40:06 | |
then we can get them to move. But the reality is that up to half | 0:40:06 | 0:40:10 | |
the people won't move, no matter what we say to them. | 0:40:10 | 0:40:13 | |
They don't believe that it's going to happen. | 0:40:13 | 0:40:16 | |
For many typical New Yorkers, | 0:40:24 | 0:40:26 | |
with the wave heading straight towards them, | 0:40:26 | 0:40:29 | |
this is just another day in the Big Apple. | 0:40:29 | 0:40:33 | |
Meanwhile, as American city dwellers try to decide whether to go or stay, | 0:40:54 | 0:41:00 | |
the wave is about to hit the islands of the Caribbean. | 0:41:00 | 0:41:03 | |
Here, it's another ordinary day of perfect sun and sea. | 0:41:06 | 0:41:11 | |
But, across all the islands, | 0:41:11 | 0:41:13 | |
40 million people live predominantly in coastal towns. | 0:41:13 | 0:41:18 | |
The Caribbean would be absolutely devastated by this kind of wave. | 0:41:28 | 0:41:32 | |
We would have ten to 20 metre waves sweeping across many of the islands. | 0:41:32 | 0:41:37 | |
Bermuda, the wave would probably sweep entirely over the island. | 0:41:38 | 0:41:42 | |
There would be nothing left. | 0:41:42 | 0:41:44 | |
It would actually be stripped to the foundations. | 0:41:44 | 0:41:47 | |
A lot of the islands are volcanic, so they have very steep shorelines. | 0:41:47 | 0:41:51 | |
If you could go half a mile inland you would be out of the way | 0:41:51 | 0:41:53 | |
but how do you get half a mile inland? | 0:41:53 | 0:41:56 | |
The road infrastructure parallels the coastline, | 0:41:56 | 0:41:58 | |
so you would literally have to run on foot | 0:41:58 | 0:42:00 | |
to get out of the wave in many areas. | 0:42:00 | 0:42:02 | |
So it's an extremely dangerous event for the Caribbean. | 0:42:02 | 0:42:06 | |
With the wave now just minutes away from both the financial | 0:42:11 | 0:42:14 | |
and political centres of the world's greatest superpower, | 0:42:14 | 0:42:19 | |
most experts believe that the major eastern cities | 0:42:19 | 0:42:22 | |
would still be packed. | 0:42:22 | 0:42:24 | |
But now even hardened New Yorkers have to take notice. | 0:42:28 | 0:42:32 | |
Evacuation plans have been activated, but it's chaos. | 0:42:34 | 0:42:39 | |
You either go up high and risk becoming marooned | 0:42:39 | 0:42:42 | |
or take underground road and rail tunnels out of Manhattan, | 0:42:42 | 0:42:46 | |
and face the possibility of a gridlocked tomb. | 0:42:46 | 0:42:50 | |
By the time the warning network's been up, it's here. | 0:42:50 | 0:42:54 | |
So, we might have two or three hours notice at best. | 0:42:54 | 0:42:58 | |
The question is, what can you do in two or three hours? | 0:42:59 | 0:43:02 | |
And the answer is not much. | 0:43:02 | 0:43:04 | |
The ocean wave is now only 12 metres high, | 0:43:04 | 0:43:08 | |
but, as it approaches New York, it rears up again, becoming a monster. | 0:43:08 | 0:43:14 | |
The back of the wave is still moving at, say, 500 miles an hour. | 0:43:16 | 0:43:20 | |
The front of the wave is moving at, maybe, 40 miles an hour. | 0:43:20 | 0:43:23 | |
And so the wave piles up, | 0:43:23 | 0:43:25 | |
and that's where we go from a wave that is maybe a foot, | 0:43:25 | 0:43:28 | |
30 centimetres high, to a wave that can suddenly become 50 metres high. | 0:43:28 | 0:43:32 | |
And that's where the destruction occurs. | 0:43:32 | 0:43:35 | |
No-one knows exactly how great a mega-tsunami's impact would be, | 0:43:38 | 0:43:44 | |
but science points to one of mankind's greatest cities | 0:43:44 | 0:43:48 | |
being humbled by the power of nature. | 0:43:48 | 0:43:52 | |
What's worse is that studies have revealed that the landslide | 0:43:55 | 0:43:59 | |
will result in not one wave but several. | 0:43:59 | 0:44:03 | |
And the first will not be the biggest. | 0:44:06 | 0:44:09 | |
People think of it as being one tsunami. | 0:44:11 | 0:44:13 | |
There would be as many as ten waves sweeping across the coast. | 0:44:13 | 0:44:16 | |
The first wave would be maybe eight to ten metres. | 0:44:18 | 0:44:21 | |
The second wave would be as much as 25. | 0:44:27 | 0:44:30 | |
Only 12 hours earlier, it was just another normal day. | 0:45:28 | 0:45:32 | |
Now a geological collapse of a small volcano on a tiny island | 0:45:33 | 0:45:38 | |
has changed tens of millions of lives on three separate continents. | 0:45:38 | 0:45:44 | |
Tens of thousands of people are feared dead | 0:45:46 | 0:45:48 | |
and hundreds of thousands are still missing, | 0:45:48 | 0:45:51 | |
following the worst natural disaster in history. | 0:45:51 | 0:45:53 | |
By the time our tsunami strikes New York, | 0:45:57 | 0:46:01 | |
in Britain a nation is already coming to terms | 0:46:01 | 0:46:05 | |
with widespread loss. | 0:46:05 | 0:46:07 | |
The authorities say they are doing everything they can | 0:46:07 | 0:46:10 | |
and have appealed for calm. | 0:46:10 | 0:46:12 | |
A state of emergency has been declared. | 0:46:12 | 0:46:15 | |
But this tsunami itself would only be the beginning | 0:46:20 | 0:46:24 | |
of a whole new chain of events. | 0:46:24 | 0:46:27 | |
Disaster planners know that, following any catastrophe, | 0:46:31 | 0:46:35 | |
the biggest dangers come in the aftermath. | 0:46:35 | 0:46:38 | |
Rescuing the injured and identifying the dead... | 0:46:39 | 0:46:42 | |
..caring for a traumatised population and preventing disease... | 0:46:45 | 0:46:49 | |
..retaining law and order and the reins of civilisation. | 0:46:51 | 0:46:56 | |
In America, where our mega-tsunami has struck at the very heart | 0:47:06 | 0:47:11 | |
of the world's political and economic capitals, | 0:47:11 | 0:47:14 | |
the challenges are greatest of all. | 0:47:14 | 0:47:17 | |
When you talk about Manhattan, | 0:47:20 | 0:47:22 | |
virtually the entirety of Manhattan is below ten metres above sea level. | 0:47:22 | 0:47:27 | |
So, if you were in the New York City area, hopefully, | 0:47:27 | 0:47:30 | |
you evacuated up and didn't try to go out... | 0:47:30 | 0:47:34 | |
and you'd be trapped, basically, while the water receded. | 0:47:34 | 0:47:37 | |
You have this initial impact of the water, which is heavy, | 0:47:40 | 0:47:44 | |
but as it recedes you've got the same amount of water going back | 0:47:44 | 0:47:47 | |
into the ocean, taking with it a lot of debris. | 0:47:47 | 0:47:50 | |
It's taking trees, it's taking buildings, it's taking cars | 0:47:50 | 0:47:54 | |
and, so, all of a sudden, you have this water with a load | 0:47:54 | 0:47:59 | |
of battering rams going back through the population that it's just hit. | 0:47:59 | 0:48:05 | |
And as much damage is caused by the receding wave | 0:48:05 | 0:48:08 | |
as is often caused by that initial wave. | 0:48:08 | 0:48:11 | |
Taking the wave's progress to its final conclusion | 0:48:13 | 0:48:16 | |
and, with the help of experts in disaster planning, | 0:48:16 | 0:48:20 | |
we are able to continue our own scenario. | 0:48:20 | 0:48:23 | |
It takes days before calm finally returns to the sea. | 0:48:27 | 0:48:31 | |
Only now is the true scale of destruction becoming clear. | 0:48:33 | 0:48:38 | |
New York, Boston, Washington, Miami - | 0:48:42 | 0:48:47 | |
entire cities have been destroyed. | 0:48:47 | 0:48:52 | |
The number of casualties is really hard to get at | 0:48:52 | 0:48:55 | |
in something like this. | 0:48:55 | 0:48:57 | |
For the 25 metre scenario, with maybe three to four hours of warning, | 0:48:57 | 0:49:02 | |
we came up with roughly 4.5 million casualties. | 0:49:02 | 0:49:05 | |
After the wave, those living, like in Japan, | 0:49:13 | 0:49:17 | |
face a devastated homeland. | 0:49:17 | 0:49:20 | |
You'd be left with an unimaginable landscape. | 0:49:20 | 0:49:23 | |
Smaller structures would be destroyed and scattered, | 0:49:23 | 0:49:26 | |
so the debris would be piled probably five, six metres high in the streets. | 0:49:26 | 0:49:30 | |
Debris sits like a blanket across the city | 0:49:35 | 0:49:39 | |
and it prevents us from getting ambulances to people who need them, | 0:49:39 | 0:49:43 | |
and getting fire trucks to fires, and getting people to grocery stores | 0:49:43 | 0:49:48 | |
to get food, and so, debris is our biggest and worst problem. | 0:49:48 | 0:49:52 | |
The doctors, physicians, emergency responders, | 0:49:54 | 0:49:57 | |
they're going to have enough trouble dealing with things | 0:49:57 | 0:50:00 | |
they can see within 100 yards of their facility, | 0:50:00 | 0:50:03 | |
much less being able to actually go on emergency calls. | 0:50:03 | 0:50:06 | |
So, you can pretty much expect anyone that is injured | 0:50:06 | 0:50:09 | |
is going to be on their own for at least a week. | 0:50:09 | 0:50:12 | |
If it's any kind of a serious injury, without medical attention, | 0:50:12 | 0:50:15 | |
they are likely to expire. | 0:50:15 | 0:50:16 | |
Dealing with death on such a scale becomes a massive priority. | 0:50:21 | 0:50:27 | |
Kenyon International Emergency Services is a private company | 0:50:27 | 0:50:30 | |
that responds to disasters. | 0:50:30 | 0:50:32 | |
Disasters that typically involve the loss of human life. | 0:50:32 | 0:50:36 | |
We deal with mass fatalities that are catastrophic - | 0:50:37 | 0:50:42 | |
a quarter of a million dead. | 0:50:42 | 0:50:44 | |
This is a refrigeration unit, a portable refrigeration cabinet, | 0:50:50 | 0:50:54 | |
of which we have several that we use to hold the deceased. | 0:50:54 | 0:50:58 | |
The purpose of the morgue is where we examine the bodies | 0:51:01 | 0:51:04 | |
and collect that picture that we're going to use to identify them. | 0:51:04 | 0:51:08 | |
So, it's where the personal effects are collected... | 0:51:08 | 0:51:12 | |
where we take the fingerprints, get the dental x-ray, | 0:51:12 | 0:51:16 | |
make measurements of the body, record tattoos and scars. | 0:51:16 | 0:51:20 | |
In the case of a natural disaster, | 0:51:20 | 0:51:23 | |
where it's going to be some time before we can return the body, | 0:51:23 | 0:51:25 | |
doing the embalming, the restoration, and the preservation of the body. | 0:51:25 | 0:51:30 | |
So that it can be returned in a sanitary condition to the families. | 0:51:30 | 0:51:35 | |
But even if emergency facilities like these could be set up, | 0:51:40 | 0:51:43 | |
they would soon be overwhelmed. | 0:51:43 | 0:51:46 | |
It's possible that millions of dead | 0:51:46 | 0:51:49 | |
would be left to decay where they died | 0:51:49 | 0:51:53 | |
and that brings with it yet another threat. | 0:51:53 | 0:51:56 | |
It would be a horrific mix of debris and, unfortunately, | 0:51:59 | 0:52:04 | |
human remains, animal remains. | 0:52:04 | 0:52:06 | |
So, you can imagine, after a few hours, | 0:52:08 | 0:52:10 | |
you would have a biological nightmare. | 0:52:10 | 0:52:13 | |
Lack of shelter, food, water, | 0:52:16 | 0:52:21 | |
and diseases like dysentery all become killers. | 0:52:21 | 0:52:25 | |
We have identified 500 different locations | 0:52:30 | 0:52:36 | |
that we could activate as emergency shelters. | 0:52:36 | 0:52:41 | |
Those are primarily public schools | 0:52:42 | 0:52:44 | |
and some of our city university buildings and facilities. | 0:52:44 | 0:52:48 | |
The capacity of the system is 600,000 people. | 0:52:48 | 0:52:52 | |
We don't look forward to a job | 0:52:52 | 0:52:56 | |
where we would have to shelter 600,000 people, | 0:52:56 | 0:53:00 | |
but that is the capacity of the system today. | 0:53:00 | 0:53:04 | |
It's simply impossible to plan for such a scale of disaster. | 0:53:08 | 0:53:13 | |
All these provisions will feed only 70,000 people for seven days. | 0:53:13 | 0:53:19 | |
Just a tiny fraction of the possible numbers of displaced survivors | 0:53:19 | 0:53:23 | |
in Manhattan alone. | 0:53:23 | 0:53:26 | |
Our mega-tsunami has triggered not only death and destruction | 0:53:30 | 0:53:34 | |
in the American East, | 0:53:34 | 0:53:36 | |
but a humanitarian crisis that could affect the entire nation. | 0:53:36 | 0:53:41 | |
Think of losing every single east coast shipping port. | 0:53:42 | 0:53:47 | |
That's essentially what we're talking about with a mega-tsunami. | 0:53:47 | 0:53:51 | |
If you lose those ports, you have a huge problem, | 0:53:53 | 0:53:56 | |
believe it or not, into the Midwest of the US. | 0:53:56 | 0:53:58 | |
All the way to the Mississippi River because a lot of that infrastructure, those rail hubs, | 0:53:58 | 0:54:03 | |
come right to the coast. | 0:54:03 | 0:54:06 | |
So, even if people weren't directly impacted by the tsunami itself, | 0:54:06 | 0:54:12 | |
they wouldn't have food coming to their supermarkets. | 0:54:12 | 0:54:16 | |
Far inland, many hundreds of miles | 0:54:16 | 0:54:18 | |
from the direct effects of the mega-tsunami, | 0:54:18 | 0:54:21 | |
there could be mass food shortages. | 0:54:21 | 0:54:23 | |
Most cities only have a two or three day supply of food, | 0:54:25 | 0:54:29 | |
so you think about cities like Atlanta, | 0:54:29 | 0:54:31 | |
you think about Memphis, you think about those inland areas | 0:54:31 | 0:54:34 | |
that get a lot of their material coming from ports on the east coast | 0:54:34 | 0:54:38 | |
and that's suddenly gone for years, perhaps, to recover - | 0:54:38 | 0:54:42 | |
that's an enormous problem. | 0:54:42 | 0:54:44 | |
And, ultimately, the scale of disaster | 0:54:45 | 0:54:48 | |
won't just be measured in lives lost. | 0:54:48 | 0:54:51 | |
No-one can be sure, | 0:54:53 | 0:54:54 | |
but a mega-tsunami could deliver a financial shock so great | 0:54:54 | 0:55:00 | |
that it's impact could change the global economy, | 0:55:00 | 0:55:03 | |
politics and the balance of East-West power, perhaps forever. | 0:55:03 | 0:55:08 | |
You think about how much disruption was caused | 0:55:08 | 0:55:10 | |
by September 11, 2001, attacks | 0:55:10 | 0:55:13 | |
and how much that disrupted the world economy. | 0:55:13 | 0:55:16 | |
Well, they were back up and running four days later. | 0:55:16 | 0:55:18 | |
Imagine if they weren't able to be back up and running in 40 days or 40 months. | 0:55:18 | 0:55:23 | |
It could be that the world's economy would recover, | 0:55:26 | 0:55:29 | |
as capitalists moved electronic money to safer havens. | 0:55:29 | 0:55:33 | |
There is some evidence, | 0:55:35 | 0:55:37 | |
as was the case with the Kobe earthquake of 1995, | 0:55:37 | 0:55:41 | |
that's natural disasters can even trigger investment and renewal. | 0:55:41 | 0:55:45 | |
But it's hard to imagine the fragile global economy bouncing back | 0:55:47 | 0:55:52 | |
from such devastation as this. | 0:55:52 | 0:55:55 | |
The truth is, no-one really knows... | 0:55:55 | 0:55:58 | |
..and, hopefully, given that landslide events | 0:55:59 | 0:56:03 | |
are, fortunately, rare, | 0:56:03 | 0:56:05 | |
no-one soon will get the chance to find out. | 0:56:05 | 0:56:08 | |
In the long-term, we know these ocean island collapses occur. | 0:56:15 | 0:56:19 | |
Around the world, there may be one of these enormous events | 0:56:19 | 0:56:23 | |
maybe once every 20,000 years, maybe only once every 50,000 years. | 0:56:23 | 0:56:27 | |
We can't say when the collapse is going to occur... | 0:56:29 | 0:56:31 | |
..but the problem with the Cumbre Vieja | 0:56:34 | 0:56:36 | |
is that it seems to already be close to failure. | 0:56:36 | 0:56:40 | |
So, the crucial question is not a matter of "if" but of "when". | 0:56:43 | 0:56:48 | |
We aren't prepared in the UK, for a tsunami. | 0:57:02 | 0:57:06 | |
No measures have been put in place to mitigate tsunamis. | 0:57:06 | 0:57:10 | |
Now, I think we need to learn from events, like Japan, | 0:57:10 | 0:57:13 | |
that that really isn't the best policy. | 0:57:13 | 0:57:15 | |
I think the question, "Are you prepared for a tsunami?" | 0:57:17 | 0:57:21 | |
is almost the wrong question because, to an extent, | 0:57:21 | 0:57:23 | |
you can't prepare for them, as Japan very clearly illustrated. | 0:57:23 | 0:57:27 | |
The Japanese were ready, | 0:57:27 | 0:57:29 | |
they prepared themselves for the potential impact of a tsunami wave. | 0:57:29 | 0:57:34 | |
Those defences were still inadequate. | 0:57:34 | 0:57:37 | |
The consequences were 15,000 dead | 0:57:39 | 0:57:41 | |
and the costliest natural catastrophe in the history of our planet. | 0:57:41 | 0:57:44 | |
Can we prevent the same thing that happened in Japan happening in Britain? | 0:57:51 | 0:57:55 | |
No. Japan is probably one of the best equipped countries in the world | 0:57:55 | 0:58:00 | |
in defending itself against tsunamis. | 0:58:00 | 0:58:03 | |
If they can't get it right...we can't. | 0:58:03 | 0:58:07 | |
And it's not a question of them getting it wrong, | 0:58:07 | 0:58:10 | |
it's a question of there's a limit of what we can do | 0:58:10 | 0:58:12 | |
against the forces of nature. | 0:58:12 | 0:58:14 | |
Subtitles by Red Bee Media Ltd | 0:58:42 | 0:58:45 |