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16th of August 2004. | 0:00:11 | 0:00:14 | |
A freak storm strikes the village of Boscastle in Cornwall. | 0:00:15 | 0:00:19 | |
Without warning, a wall of water tears through the village, | 0:00:19 | 0:00:24 | |
destroying houses and sweeping 80 cars into the sea. | 0:00:24 | 0:00:28 | |
The damage will run into millions. | 0:00:30 | 0:00:33 | |
Nearly 100 people are airlifted from their flooded homes, | 0:00:36 | 0:00:39 | |
their lives saved by 21st-century technology. | 0:00:39 | 0:00:43 | |
400 years earlier, the peoples of the Bristol Channel were less fortunate. | 0:00:51 | 0:00:56 | |
On the 20th January 1607, another freak wave swept across the lowlands of the south-west. | 0:00:57 | 0:01:04 | |
It too came without warning and left 2,000 dead in its wake. | 0:01:10 | 0:01:15 | |
Yet for centuries this apocalyptic flood has been forgotten | 0:01:16 | 0:01:21 | |
and only now are scientists piecing together the evidence left behind. | 0:01:21 | 0:01:26 | |
Was it just a huge storm? | 0:01:26 | 0:01:28 | |
Or was the killer wave of 1607 in fact a British tsunami? | 0:01:28 | 0:01:33 | |
It is the winter of 1607. | 0:02:01 | 0:02:04 | |
The Stuart dynasty is not yet four years old and Britain is at last a united kingdom under James I. | 0:02:04 | 0:02:11 | |
This year will see the premiere of Shakespeare's Anthony and Cleopatra. | 0:02:17 | 0:02:22 | |
In the new North American colonies, Pocahontas will save John Smith's life. | 0:02:22 | 0:02:27 | |
In London, the Thames will freeze over. | 0:02:29 | 0:02:32 | |
The most remarkable event, however, will be forgotten - | 0:02:33 | 0:02:38 | |
the greatest flood in Britain's history. | 0:02:38 | 0:02:41 | |
On Tuesday 20th of January, as dawn breaks over the villages and hamlets of Somerset, Gwent and Monmouthshire, | 0:02:43 | 0:02:52 | |
there is no sign of an impending tragedy. | 0:02:52 | 0:02:54 | |
In these backwaters of the Bristol Channel, life is dominated by the steady rhythms of agriculture. | 0:02:55 | 0:03:02 | |
Sheep and cattle farming are the lifeblood of the local economy. | 0:03:03 | 0:03:07 | |
The people are relatively prosperous, hardworking and God-fearing. | 0:03:12 | 0:03:17 | |
Around nine o'clock in the morning, this simple, ordered life will be thrown into chaos. | 0:03:20 | 0:03:27 | |
In Llanwern, Monmouthshire, four miles from the sea, the servants of Mistress Van prepare her lunch. | 0:03:36 | 0:03:44 | |
In Goldcliff, of Gwent, William Tapp, church warden, makes ready for morning service. | 0:03:48 | 0:03:55 | |
In Berrow, Somerset, a milkmaid heads for work. | 0:03:58 | 0:04:01 | |
In the same village, John Stoles, | 0:04:03 | 0:04:07 | |
father of five, wakes late, unaware he will not survive the day. | 0:04:07 | 0:04:12 | |
No-one has any warning. | 0:04:14 | 0:04:16 | |
In an age when few people knew how to swim, | 0:05:07 | 0:05:10 | |
any caught in the freezing waters will be lucky to survive. | 0:05:10 | 0:05:14 | |
One Mistress Van, a gentlewoman of good sort, her house being four miles from the sea, | 0:05:23 | 0:05:30 | |
having seen the approaching waters, was surprised by them and destroyed | 0:05:30 | 0:05:34 | |
even before she could get into the higher rooms of her house, | 0:05:34 | 0:05:38 | |
such was the speed of the waters. | 0:05:38 | 0:05:40 | |
There was a maid that went to milk her cows in the morning | 0:05:51 | 0:05:54 | |
but before she had fully ended her business, the vehemence of the waters increased | 0:05:54 | 0:05:58 | |
and so suddenly environed her, she could not escape thence | 0:05:58 | 0:06:02 | |
but was forced to make shift up to the top of a high bank to save herself. | 0:06:02 | 0:06:07 | |
John Stoles was thrown down by the water. | 0:06:19 | 0:06:22 | |
He himself, with three or four of his children, drowned. | 0:06:22 | 0:06:26 | |
His wife and one of her sons were found the next day and survived. | 0:06:28 | 0:06:32 | |
According to eyewitness accounts, the dead perished in a mountainous wall of water | 0:06:36 | 0:06:42 | |
and that after the wave came a torrent that swept across the fields, | 0:06:42 | 0:06:47 | |
creating an inland sea of over 200 square miles. | 0:06:47 | 0:06:52 | |
The waters have washed many onto the rocks of poverty and misery. | 0:06:55 | 0:06:59 | |
But so have they brought some profit, | 0:06:59 | 0:07:03 | |
for seafaring men, I might call them thieves, come daily now in boats | 0:07:03 | 0:07:08 | |
and get richly laden with goods which they find swimming in the waters. | 0:07:08 | 0:07:12 | |
Many dead persons are sadly found floating | 0:07:14 | 0:07:17 | |
and as yet cannot be known who they are. | 0:07:17 | 0:07:20 | |
When the waters receded ten days later, they left behind a scene of devastation. | 0:07:21 | 0:07:27 | |
2,000 dead. | 0:07:27 | 0:07:30 | |
Hundreds of thousands of sheep and cattle drowned. | 0:07:30 | 0:07:33 | |
The local economy destroyed. | 0:07:33 | 0:07:37 | |
Men that were rich in the morning when they rose from their beds | 0:07:39 | 0:07:43 | |
were made poor before noon of the same day. | 0:07:43 | 0:07:46 | |
To this day, 20th of January 1607 remains the largest and most destructive flood in British history. | 0:07:48 | 0:07:56 | |
But until now, a full explanation for the disaster has not been scientifically researched. | 0:08:04 | 0:08:10 | |
Just why so many lost their lives remained a mystery. | 0:08:10 | 0:08:15 | |
When I was young I remember seeing in some books in a library some woodcuts of the flood - | 0:08:15 | 0:08:22 | |
pictures of people stranded up on top of high trees, on top of roofs, | 0:08:22 | 0:08:27 | |
rabbits even clinging to the back of sheep as they were floating along. | 0:08:27 | 0:08:32 | |
Very dramatic scenes which I've shown in my lectures to students for, well, getting on for ten years, | 0:08:32 | 0:08:40 | |
as a good example of what a storm can do. | 0:08:40 | 0:08:43 | |
Simon Haslett is a professor of geography from Bath Spa University College. | 0:08:43 | 0:08:48 | |
He grew up with the folklore of the flood. | 0:08:48 | 0:08:51 | |
You can't really imagine what it must have been like, other than the human tragedy of it. | 0:08:51 | 0:08:57 | |
Quite catastrophic and how people actually dealt with that is amazing. | 0:08:57 | 0:09:02 | |
For most of his life, Simon has accepted the conventional explanation of 1607. | 0:09:02 | 0:09:08 | |
A lot of the commentators on the 1607 flood have put it down to a storm coming in | 0:09:08 | 0:09:15 | |
and as a child you just accept what you're being told by the scientists and the historians | 0:09:15 | 0:09:21 | |
and you don't really question it. | 0:09:21 | 0:09:23 | |
Attributing the flooding of 1607 to a storm makes sense. | 0:09:26 | 0:09:30 | |
The area is famous for them. | 0:09:30 | 0:09:32 | |
-NEWS REPORTER: -The sea defences have been breached | 0:09:33 | 0:09:36 | |
at more than a dozen points along the coast | 0:09:36 | 0:09:39 | |
and there's now concern about tonight's high tide. | 0:09:39 | 0:09:42 | |
On December the 13th 1981, | 0:09:42 | 0:09:44 | |
the sea defences along the Somerset coast were breached by a storm-driven tidal surge | 0:09:44 | 0:09:49 | |
and the lowlands behind them were inundated, as they had been in 1607. | 0:09:49 | 0:09:54 | |
As the waves swept through seaside villages during the night, | 0:09:54 | 0:09:57 | |
they carried away cars and parts of houses. | 0:09:57 | 0:10:00 | |
Officials say it was a miracle no-one was killed or seriously injured. | 0:10:00 | 0:10:04 | |
The lowlands of the Bristol Channel have always been prone to flooding. | 0:10:04 | 0:10:08 | |
Much of the area is below high-tide mark and has been protected by sea walls for 600 years. | 0:10:08 | 0:10:15 | |
This weakness is exposed when heavy storms coincide with high tides. | 0:10:15 | 0:10:20 | |
It's exactly what happened in 1981. | 0:10:20 | 0:10:24 | |
Low pressure over the Irish Sea | 0:10:24 | 0:10:26 | |
drew a huge volume of water to the mouth of the Bristol Channel. | 0:10:26 | 0:10:29 | |
A combination of high tide and strong winds | 0:10:29 | 0:10:32 | |
then forced the swollen waters back against the Somerset coast. | 0:10:32 | 0:10:37 | |
What should have been just a high seasonal tide | 0:10:37 | 0:10:40 | |
became a storm surge. | 0:10:40 | 0:10:43 | |
As a local man, Simon is well aware of the dangers. | 0:10:44 | 0:10:47 | |
If you live on the Levels, you're always aware of the vulnerability. | 0:10:47 | 0:10:52 | |
Although it looks tranquil, it actually has a record of disaster | 0:10:52 | 0:10:56 | |
and if a big event comes in, a big flood comes in, | 0:10:56 | 0:11:00 | |
then it can actually tragically lead to a huge loss of life. | 0:11:00 | 0:11:05 | |
Fascinated by the scale of the 1607 disaster, | 0:11:08 | 0:11:11 | |
Simon decides to meet with witnesses of the 1981 flood - | 0:11:11 | 0:11:15 | |
the biggest in living memory. | 0:11:15 | 0:11:17 | |
Ken Burrell lives in the same house he did 23 years ago. | 0:11:21 | 0:11:25 | |
In those days there was a bathroom down there and that's about a foot lower than this room. | 0:11:25 | 0:11:30 | |
My daughter was going to take a bath and water was actually coming through the bath panel. | 0:11:30 | 0:11:35 | |
I thought it was a burst pipe, so we said forget about that. | 0:11:35 | 0:11:38 | |
Came in and maybe... | 0:11:38 | 0:11:40 | |
20 minutes, half an hour later, that's when I started looking out through here. | 0:11:40 | 0:11:45 | |
Coming dusk and the first thing I saw was a row of black things coming towards me. | 0:11:45 | 0:11:50 | |
And that was actually the leaves being picked up by the water, | 0:11:50 | 0:11:53 | |
not that fast, maybe a fast walking pace. | 0:11:53 | 0:11:57 | |
Stood here and saw the water deepening and then getting a little bit deeper | 0:11:57 | 0:12:02 | |
and then it started to come up to the window. | 0:12:02 | 0:12:04 | |
That's when I said to my wife and kids, "Time to get upstairs." | 0:12:04 | 0:12:07 | |
And what damage did it do to your property? | 0:12:07 | 0:12:10 | |
Apart from knocking furniture about, | 0:12:10 | 0:12:13 | |
it just brought in a slow, steady flood level. | 0:12:13 | 0:12:16 | |
A flood level I marked on the doorjamb the day after. | 0:12:16 | 0:12:18 | |
I carved that mark in the doorjamb which was the height of the water throughout this room. | 0:12:18 | 0:12:24 | |
Further up the coast, Simon meets Thelma Blake, a farmer at the front line of the storm. | 0:12:24 | 0:12:30 | |
Much of Thelma's land is below high-tide level and is only protected by the sea defences. | 0:12:32 | 0:12:37 | |
It just come cascading down the bank and on through, like. | 0:12:37 | 0:12:44 | |
I mean you just had to make sure all the cattle run was all right, you know. | 0:12:44 | 0:12:49 | |
-So just hoping it wasn't going to get any deeper. -Right. | 0:12:49 | 0:12:54 | |
Thelma lost just six sheep in the flood that night. | 0:12:54 | 0:12:57 | |
1981 was the worst tidal surge flooding in 100 years. | 0:12:59 | 0:13:04 | |
Yet the church in Kingston Seymour reveals how little damage it actually did. | 0:13:04 | 0:13:09 | |
In the 1981 flood, the church here wasn't flooded. It was dry. | 0:13:10 | 0:13:16 | |
In 1607, the water was five feet high here in the church | 0:13:16 | 0:13:21 | |
and most of that water actually was here on the ground for about ten days afterwards. | 0:13:21 | 0:13:27 | |
The level of the 1607 flood is recorded in five other churches on both sides of the Bristol Channel - | 0:13:29 | 0:13:36 | |
all record flood levels that make 1981 pale in comparison. | 0:13:36 | 0:13:41 | |
1607 was a local disaster unlike any other before or since. | 0:13:41 | 0:13:47 | |
News of the catastrophe spread fast. | 0:13:48 | 0:13:51 | |
As the waters retreated, the media of the day arrived to report on the event. | 0:13:51 | 0:13:57 | |
The waters as they did come down on their first entry. | 0:13:57 | 0:14:01 | |
So much did happen. So much terrible devastation. | 0:14:01 | 0:14:04 | |
They recorded the graphic accounts of destruction and lives lost | 0:14:04 | 0:14:08 | |
that appear in six different pamphlets written and published at the time. | 0:14:08 | 0:14:13 | |
It is from these eyewitness accounts that the full horror of the 1607 flood unfolds. | 0:14:13 | 0:14:20 | |
Upon Tuesday, being the 20th of January last past, | 0:14:21 | 0:14:26 | |
there happened an overflowing of waters and forcible breaches made into the firm land, | 0:14:26 | 0:14:31 | |
the sudden terror whereof struck such an amazed fear into the hearts of all the inhabitants | 0:14:31 | 0:14:37 | |
that everyone prepared himself ready to entertain the last period of his life's destruction. | 0:14:37 | 0:14:43 | |
The pamphlets revel in the details of death and destruction. | 0:14:43 | 0:14:48 | |
Then, as now, disaster sells. | 0:14:52 | 0:14:57 | |
It may be the case that the pamphleteers exaggerate in order to profit, | 0:14:57 | 0:15:02 | |
although I don't think we really know enough about the 17th-century book trade | 0:15:02 | 0:15:07 | |
to be certain that the bigger the lie you told, | 0:15:07 | 0:15:09 | |
the more copies you would sell. | 0:15:09 | 0:15:11 | |
That might be an attitude we're importing from the 21st century | 0:15:11 | 0:15:14 | |
back into the 17th century. | 0:15:14 | 0:15:16 | |
The quantity of detail about local geography for example, suggests that this just isn't made up. | 0:15:16 | 0:15:22 | |
One pamphlet is clearly written by a local as a pamphlet. | 0:15:22 | 0:15:26 | |
He has written it to present a local testimony about the flood and the damage done. | 0:15:26 | 0:15:32 | |
This is a direct communication | 0:15:36 | 0:15:38 | |
from an author who was, if not an eyewitness, at least close to eyewitnesses. | 0:15:38 | 0:15:43 | |
These pamphlets are published upon occasion | 0:15:43 | 0:15:46 | |
and they're published because something sensational has happened. | 0:15:46 | 0:15:50 | |
Usually what we find reported is based upon fact. | 0:15:50 | 0:15:55 | |
Page by page, they set out a chilling roll call of the villages | 0:16:02 | 0:16:06 | |
struck by the wave and of the lives lost. | 0:16:06 | 0:16:10 | |
In Brean Down stood nine houses and of those seven were consumed | 0:16:13 | 0:16:18 | |
and with them 21 persons lost their lives. | 0:16:18 | 0:16:21 | |
All the counties along on both sides of the River Severn, | 0:16:21 | 0:16:25 | |
from Gloucester to Bristol, which is about some 20 miles, were all overflown. | 0:16:25 | 0:16:30 | |
In some places six miles over. In some places more, in some less. | 0:16:32 | 0:16:38 | |
26 parishes in Monmouthshire were inundated | 0:16:41 | 0:16:45 | |
and in these cruel waters many men, women and children lost their lives. | 0:16:45 | 0:16:49 | |
There happened such an overflowing of waters into the boroughs of Monmouth, Glamorgan, Carmarthen | 0:16:51 | 0:16:56 | |
and diverse and sundry other places in South Wales. | 0:16:56 | 0:17:00 | |
In Bristol, all the houses standing upon the quay near the waterside were all overflown with water. | 0:17:00 | 0:17:07 | |
Everything lies melted and soaked in grime and salt water. | 0:17:07 | 0:17:11 | |
Taken in their entirety, | 0:17:16 | 0:17:18 | |
the pamphlets reveal an unparalleled chronicle of disaster | 0:17:18 | 0:17:22 | |
and the full extent of the flood. | 0:17:22 | 0:17:25 | |
Over 200 square miles of land lost to the sea. | 0:17:25 | 0:17:29 | |
With this information, scientists at the Proudman Oceanographic Laboratory in Liverpool | 0:17:32 | 0:17:38 | |
can model the precise storm conditions needed to produce the 1607 flood. | 0:17:38 | 0:17:43 | |
1607 is a fascinating event. | 0:17:43 | 0:17:44 | |
Although we've observed surges in the Bristol Channel before, | 0:17:44 | 0:17:48 | |
we've never seen one of that magnitude. | 0:17:48 | 0:17:50 | |
The data is excellent because it allows us to piece together the extent of the flooding | 0:17:50 | 0:17:55 | |
and also the depth of the flooding at many locations. | 0:17:55 | 0:17:58 | |
Critical to interpreting the 17th-century measurements is the height of the tide that day. | 0:17:58 | 0:18:05 | |
The morning of the event, we have a very big tide. It's almost eight metres above ordnance datum. | 0:18:06 | 0:18:12 | |
That's one of the biggest tides you can get in the Bristol Channel. | 0:18:12 | 0:18:15 | |
So we know that there was a massive tide on that particular morning. | 0:18:15 | 0:18:20 | |
Kevin can transform this tide into a storm surge by adding hurricane winds of 80 miles an hour. | 0:18:20 | 0:18:28 | |
Only then do the flood waters of 1607 become a computer reality. | 0:18:28 | 0:18:33 | |
The warm colours, the reds and the oranges, | 0:18:33 | 0:18:35 | |
represent a metre and a half to two metres of extra water due to the surge. | 0:18:35 | 0:18:40 | |
You can see how that amplifies into the Bristol Channel. | 0:18:40 | 0:18:43 | |
Ten metres of water above normal sea level. Two billion tons of water were probably involved in the flood. | 0:18:43 | 0:18:51 | |
Was it this cruel coincidence of high tide and hurricane winds that made 1607 the most deadly of storm surges? | 0:18:53 | 0:19:01 | |
It seems to be proof positive of the assumptions that for years Simon Haslett took as fact. | 0:19:15 | 0:19:22 | |
But in 2002, Simon made his own discovery | 0:19:23 | 0:19:27 | |
and it has forced him to consider a more shocking explanation for the 1607 flood. | 0:19:27 | 0:19:33 | |
Today, Simon is meeting again with the Australian geologist Ted Bryant, with whom he made that discovery. | 0:19:35 | 0:19:42 | |
-Hey, hi, Ted. How are you? -Not bad. | 0:19:42 | 0:19:45 | |
-Easy journey? -Yeah, oh, till we got to Bangkok. | 0:19:45 | 0:19:47 | |
Yeah? Oh. | 0:19:47 | 0:19:48 | |
Over the next two weeks they intend to collect evidence from around the Bristol Channel | 0:19:49 | 0:19:54 | |
that will substantiate their revolutionary theory - | 0:19:54 | 0:19:57 | |
a theory sparked by a chance discovery in a country church. | 0:19:57 | 0:20:00 | |
There it is, what we saw two years ago, "The great flood, AD1606". | 0:20:04 | 0:20:10 | |
Yeah, that's still as impressive as the first time I saw it. | 0:20:10 | 0:20:13 | |
The date reads 1606 because at the time, the new year did not begin until March. | 0:20:15 | 0:20:21 | |
Above the inscription, over five foot off the ground, | 0:20:21 | 0:20:25 | |
is a mark showing the level of the floodwaters. | 0:20:25 | 0:20:28 | |
But it was what they found inside that really stunned them. | 0:20:28 | 0:20:32 | |
As they thumbed through a history of the church, | 0:20:32 | 0:20:35 | |
they came across an extract from one eyewitness account recorded in the pamphlets. | 0:20:35 | 0:20:41 | |
They describe these waves as mountainous and the line was, | 0:20:41 | 0:20:44 | |
"Such a smoke as if mountains were on fire | 0:20:44 | 0:20:47 | |
"and to the view of some it seemed as if myriads of thousands of arrows | 0:20:47 | 0:20:51 | |
"had been shot forth all at one time." | 0:20:51 | 0:20:53 | |
So there's obviously sparks coming off this wave. | 0:20:53 | 0:20:57 | |
After we read this, we looked at each other and said, "That's not a storm." | 0:20:57 | 0:21:01 | |
That's a description of a tsunami. | 0:21:01 | 0:21:03 | |
Suddenly, the pamphlets had new significance. | 0:21:12 | 0:21:15 | |
They may be the only eyewitness accounts | 0:21:15 | 0:21:17 | |
of one of the world's most destructive natural phenomena striking Britain - | 0:21:17 | 0:21:22 | |
a tsunami. | 0:21:22 | 0:21:23 | |
It would explain why the victims of the killer wave of 1607 never stood a chance. | 0:21:23 | 0:21:28 | |
The terrifying reality of a tsunami stunned the whole world on Boxing Day 2004. | 0:21:30 | 0:21:36 | |
The Asian tsunami, known to have killed 300,000, was triggered by a submarine earthquake. | 0:21:49 | 0:21:56 | |
Giant underwater landslides and collapsing volcanoes can also unleash similar disasters. | 0:22:02 | 0:22:09 | |
For the last 15 years, | 0:22:11 | 0:22:12 | |
Professor Ted Bryant has been defining the unique character of tsunamis across the globe. | 0:22:12 | 0:22:18 | |
A tsunami surges over the land, | 0:22:18 | 0:22:20 | |
so there's an enormous volume of water brought onto the land | 0:22:20 | 0:22:23 | |
and you don't see that under storm waves. | 0:22:23 | 0:22:26 | |
Even thousands of miles away from its source, a tsunami can have terrifying destructive power. | 0:22:26 | 0:22:33 | |
In 1960, a massive earthquake off Chile generated a tsunami ten metres high. | 0:22:33 | 0:22:40 | |
It travelled across the Pacific Ocean at the speed of a Boeing 707. | 0:22:40 | 0:22:44 | |
600km an hour. | 0:22:44 | 0:22:45 | |
And when it got to the other side of the ocean - Japan - that's half a hemisphere away, | 0:22:53 | 0:22:58 | |
it had enough force to wreck buildings, to drive ships onto the shore | 0:22:58 | 0:23:03 | |
and there was massive damage right around the whole rim of the Pacific Ocean in 1960 | 0:23:03 | 0:23:08 | |
because of that earthquake-generated tsunami back on the coastline of Chile. | 0:23:08 | 0:23:13 | |
The eyewitnesses of some tsunamis have observed a strange and distinctive phenomenon. | 0:23:16 | 0:23:22 | |
They describe the crest of the waves as sparkling with strange lights. | 0:23:22 | 0:23:27 | |
The last such account was from survivors of the Papua New Guinea tsunami in 1998. | 0:23:27 | 0:23:34 | |
In Papua New Guinea, the tsunami came at twilight, | 0:23:34 | 0:23:37 | |
and again there were reports of flames. There were sparks coming off the top of the wave. | 0:23:37 | 0:23:43 | |
For Ted, the echoes of 1607 are uncanny. | 0:23:43 | 0:23:45 | |
The Redwick church one is about nine in the morning, it would have been daylight | 0:23:45 | 0:23:51 | |
and still there's this description of sparks. | 0:23:51 | 0:23:53 | |
We don't know what causes the sparks | 0:23:53 | 0:23:56 | |
but it is a characteristic of tsunami waves | 0:23:56 | 0:23:59 | |
and for Redwick people to see sparks on the top of the wave in broad daylight, | 0:23:59 | 0:24:04 | |
they were looking at some incredible phenomena coming towards them. | 0:24:04 | 0:24:08 | |
To Ted Bryant, the pamphlets are clearly describing a tsunami. | 0:24:12 | 0:24:16 | |
The size, speed and strange sparkling of the wave all fit. | 0:24:16 | 0:24:20 | |
It seemed as if millions of thousands of arrows had been shot forth all at once... | 0:24:22 | 0:24:26 | |
Those who saw the mighty torrent approaching say that the waters afar off | 0:24:26 | 0:24:30 | |
looked to be many yards above the earth and with such smoke as if all the mountains were on fire. | 0:24:30 | 0:24:36 | |
The like have never, ever been seen or heard of in the memory of man. | 0:24:36 | 0:24:41 | |
The pamphlets provide a foundation case for a tsunami | 0:24:44 | 0:24:48 | |
but Simon and Ted need physical proof to back up these chilling voices from the past. | 0:24:48 | 0:24:53 | |
They set out to scour the coast of the Bristol Channel for evidence. | 0:24:55 | 0:24:59 | |
At Dunraven Bay in South Wales, hundreds of boulders lie at the foot of the cliffs. | 0:25:01 | 0:25:06 | |
Some have obviously just dropped off the face but others are less easy to explain. | 0:25:06 | 0:25:12 | |
Which ones have we done? We've done that one over there, that one over there. | 0:25:12 | 0:25:16 | |
Have we done that one? All right? | 0:25:16 | 0:25:19 | |
To the untrained eye, all boulders look the same | 0:25:19 | 0:25:22 | |
but to Simon, each rock gives up clues to the events of the past. | 0:25:22 | 0:25:27 | |
This particular boulder has, I'm pretty sure, been moved off the beach. | 0:25:27 | 0:25:31 | |
It's got some fossils in it, which you don't normally associate with the older limestones | 0:25:31 | 0:25:36 | |
which you find on the cliffs here, | 0:25:36 | 0:25:38 | |
so it looks like this quite big boulder has come from over there on the beach. | 0:25:38 | 0:25:42 | |
The force of water needed to move seven-ton boulders could easily be produced by a tsunami. | 0:25:42 | 0:25:50 | |
The way the boulders are lying gives Simon and Ted another clue. | 0:25:50 | 0:25:54 | |
OK, that's 270 degrees west. | 0:25:56 | 0:25:59 | |
We're finding a lot of these boulders are actually sloping back | 0:25:59 | 0:26:03 | |
because they come to rest in an orientation | 0:26:03 | 0:26:07 | |
that offers least resistance to the flow going over the top of them | 0:26:07 | 0:26:10 | |
and we've got a lot of these boulders over here | 0:26:10 | 0:26:13 | |
which all point back in the same or similar direction. | 0:26:13 | 0:26:16 | |
A storm operates in splashes. | 0:26:16 | 0:26:19 | |
You've got a wave breaking and storms can move the odd boulder | 0:26:19 | 0:26:23 | |
and can fling boulders up onto the top of cliffs | 0:26:23 | 0:26:25 | |
but given that we've got so many boulders in a train - what we call a boulder train - | 0:26:25 | 0:26:30 | |
and they're all pointing back in the same direction. That suggests to us a constant flow over time. | 0:26:30 | 0:26:37 | |
By measuring the size and shape of the boulders, | 0:26:39 | 0:26:42 | |
Ted can estimate what height of tsunami would have been required to move them. | 0:26:42 | 0:26:46 | |
The equation we have is one that says, "This boulder is sitting at the edge of the beach. | 0:26:46 | 0:26:51 | |
"About water level. | 0:26:51 | 0:26:53 | |
"What force is required to lift it up and move it?" | 0:26:53 | 0:26:56 | |
And we have equations that relate that to the depth of the water and the height of the tsunami. | 0:26:56 | 0:27:02 | |
Ted reckons it would only have taken a five-metre tsunami wave to shift these boulders. | 0:27:02 | 0:27:08 | |
For a storm to do the same thing, they calculate it would have taken a wave at least 20 metres high. | 0:27:08 | 0:27:14 | |
Over 60 feet. | 0:27:14 | 0:27:16 | |
Yet the very idea of a tsunami laying waste to the Bristol Channel | 0:27:16 | 0:27:21 | |
goes against every assumption we have about Britain being geologically safe. | 0:27:21 | 0:27:26 | |
The widely held view is that storms batter us all the time but tsunamis never come anywhere near Britain. | 0:27:26 | 0:27:34 | |
But in fact, they do. | 0:27:34 | 0:27:37 | |
7,000 years ago, the entire east coast of Scotland was battered by a mega tsunami. | 0:27:41 | 0:27:47 | |
It was triggered by a gigantic landslide off Norway. | 0:27:47 | 0:27:50 | |
On an area of the continental shelf called Storegga, | 0:27:50 | 0:27:54 | |
billions of tons of sediment plunged from the shallows into the deep. | 0:27:54 | 0:27:59 | |
The scar of the landslide is still visible in sonar surveys | 0:27:59 | 0:28:03 | |
and from this evidence Norwegian scientists have calculated the size of the tsunami created by Storegga. | 0:28:03 | 0:28:09 | |
The wave that hit Scotland 7,000 years ago was 70 foot high. | 0:28:11 | 0:28:16 | |
Nor are British tsunamis confined to prehistory. | 0:28:20 | 0:28:24 | |
In 1755, an earthquake off the coast from Lisbon sent a series of tsunamis out into the Atlantic. | 0:28:26 | 0:28:33 | |
The south-west tip of Cornwall was hit by a three-metre wave. | 0:28:33 | 0:28:37 | |
If a third tsunami did hit the Bristol Channel in 1607, | 0:28:37 | 0:28:42 | |
the evidence should be extensive and not just on the shoreline. | 0:28:42 | 0:28:46 | |
Ted and Simon decide to investigate Rumney Wharf. | 0:28:47 | 0:28:51 | |
20 years ago, a survey of the marshes by a local archaeologist | 0:28:53 | 0:28:56 | |
revealed a strange anomaly in the sediment deposits. | 0:28:56 | 0:28:59 | |
Simon and Ted are hoping it might offer more evidence for a tsunami. | 0:29:02 | 0:29:07 | |
Well, the marshes here are very muddy and they've been like that for centuries | 0:29:10 | 0:29:14 | |
but back in the 1980s there was a survey done | 0:29:14 | 0:29:18 | |
that actually documented a sand layer within the mud deposits. | 0:29:18 | 0:29:23 | |
If the old survey is correct, the layer of sand should be visible on exposed sections of the marshes. | 0:29:25 | 0:29:31 | |
The same survey also proposed that the sand layer was left behind | 0:29:31 | 0:29:36 | |
by a massive surge of water from the sea around 400 years ago. | 0:29:36 | 0:29:41 | |
20 years on, is the sand layer still there? | 0:29:41 | 0:29:43 | |
And if so, what clues will it yield to Ted and Simon? | 0:29:43 | 0:29:47 | |
OK, Ted, I think I've got a dark layer here. | 0:29:47 | 0:29:51 | |
It's got... | 0:29:51 | 0:29:52 | |
It's coarse. It's quite sandy. | 0:29:54 | 0:29:57 | |
It's quite thin, here. It's coming to about ten centimetres. | 0:29:58 | 0:30:02 | |
Is there any pebbles in it at all? Can we see here? | 0:30:02 | 0:30:06 | |
No. No. No, but let's follow it round and see if it thickens. | 0:30:06 | 0:30:11 | |
Just around the corner, they find what they're looking for. | 0:30:14 | 0:30:17 | |
Gosh, it's got lots of pebbles in it. | 0:30:17 | 0:30:19 | |
And bits of shell. | 0:30:19 | 0:30:22 | |
This is heaps thick. | 0:30:22 | 0:30:24 | |
Not only is it sand but within it you have... | 0:30:24 | 0:30:27 | |
Well, just here small pebbles and also the little white flecks that you can see in here, | 0:30:27 | 0:30:33 | |
that's broken-up shell. Shell that's been smashed up and brought in here with the sand and been deposited. | 0:30:33 | 0:30:39 | |
Whatever force brought the sand here was an event of enormous power. | 0:30:49 | 0:30:55 | |
And for Ted, the sea shells rule out a storm. | 0:30:55 | 0:30:58 | |
Yeah, it's a good one. | 0:30:58 | 0:31:00 | |
It's a pipi, I think. | 0:31:00 | 0:31:03 | |
In these type of deposits you get them. You might be able to track it back to a source. | 0:31:03 | 0:31:08 | |
You look around you and there's no beach for miles, | 0:31:08 | 0:31:10 | |
so that's an indication that this stuff has been transported considerable distance. | 0:31:10 | 0:31:15 | |
The way some of the flow behaves, it will not abrade the material, so to find something very fragile | 0:31:15 | 0:31:21 | |
like this in this type of deposit is an indication that we're dealing with tsunami flow. | 0:31:21 | 0:31:26 | |
Microscopic analysis will provide more evidence of where the sand comes from | 0:31:27 | 0:31:32 | |
and how it got dumped onto the marshes. | 0:31:32 | 0:31:34 | |
To calculate the volume of sand deposited, Simon and Ted check how far the layer extends inland. | 0:31:37 | 0:31:44 | |
That's it. Right. | 0:31:44 | 0:31:46 | |
-Let's take this up really slow. -Yeah. | 0:31:52 | 0:31:55 | |
OK, let's see what we've got. | 0:32:02 | 0:32:04 | |
Sand. | 0:32:06 | 0:32:08 | |
More sand. | 0:32:08 | 0:32:10 | |
And then clay. | 0:32:10 | 0:32:11 | |
So it was about 20cm thick here. | 0:32:11 | 0:32:15 | |
So it's tapering from whatever that was there, about 40, 45cm thick to about 20 here | 0:32:15 | 0:32:22 | |
and we peter out inland across the marshes. | 0:32:22 | 0:32:26 | |
For me, that layer - that layer of sand - | 0:32:27 | 0:32:30 | |
is such a stark difference to the rest of the estuary. | 0:32:30 | 0:32:34 | |
The waters of the estuary are full of mud. | 0:32:34 | 0:32:36 | |
The Severn is one of the muddiest estuaries in Europe and we have marshes. | 0:32:36 | 0:32:40 | |
That sand layer is out of place. It couldn't have got here unless we had this high-energy event. | 0:32:40 | 0:32:45 | |
If I came here and we couldn't find our sand layer than I'd have doubts that the tsunami didn't exist. | 0:32:45 | 0:32:51 | |
It was probably a storm surge. | 0:32:51 | 0:32:52 | |
But having seen those sand layers, the tsunami's sitting in the back of my mind well and truly. | 0:32:52 | 0:32:57 | |
At another site, 20 miles away, they find similar evidence. | 0:33:00 | 0:33:03 | |
Have a look at that. | 0:33:03 | 0:33:06 | |
And that's sitting right on that land surface. | 0:33:06 | 0:33:09 | |
We've got to explain how that got there. | 0:33:09 | 0:33:12 | |
-Well, you wouldn't get that just by floating in. -No. | 0:33:12 | 0:33:15 | |
In total, Simon and Ted take samples from five separate locations around the Bristol Channel. | 0:33:15 | 0:33:22 | |
At all five sites, they find sand or gravel deposits and all in a single layer. | 0:33:22 | 0:33:28 | |
If the occurrence of sand layers in these marshes is due to storms, | 0:33:28 | 0:33:32 | |
you might expect to find more than one, | 0:33:32 | 0:33:34 | |
given that we do experience storms quite frequently. | 0:33:34 | 0:33:37 | |
But we have only got the one layer, which is interesting. | 0:33:37 | 0:33:41 | |
Back in his lab, Simon can examine the samples in more detail. | 0:33:43 | 0:33:47 | |
He is looking for microscopic evidence of where the sand originated. | 0:33:47 | 0:33:52 | |
Meanwhile, Ted heads out to Sully Island, a small outcrop of rock just off Cardiff. | 0:33:54 | 0:34:00 | |
It would have taken the full brunt of a tsunami moving up the Bristol Channel. | 0:34:00 | 0:34:06 | |
That's a major erosion. | 0:34:06 | 0:34:09 | |
Look at the big block over there that's collapsed in and the other rocks straight ahead. | 0:34:09 | 0:34:15 | |
Once again, big boulders seem to have been picked up and shoved against one another | 0:34:18 | 0:34:23 | |
by a massive movement of the water and on the headland, the top layer of rock has been eroded away - | 0:34:23 | 0:34:29 | |
exactly the sort of thing a tsunami could do. | 0:34:29 | 0:34:33 | |
So the tsunami will bash into this cliff, full force | 0:34:35 | 0:34:38 | |
and it could carve through the hardest rock. | 0:34:38 | 0:34:42 | |
It will carve through granites and salicified sandstones - | 0:34:42 | 0:34:46 | |
very resistant rock. | 0:34:46 | 0:34:48 | |
It just means nothing to it. | 0:34:48 | 0:34:49 | |
It just erodes them and it erodes it very quickly. | 0:34:49 | 0:34:52 | |
And this is as good as any evidence I've seen in New South Wales. | 0:34:52 | 0:34:55 | |
It's incredibly exciting. | 0:34:55 | 0:34:58 | |
However, dating the erosion on Sully Island back to 1607 is impossible. | 0:34:58 | 0:35:03 | |
Dramatic as this big-scale evidence is, it's far from conclusive. | 0:35:03 | 0:35:08 | |
But at a microscopic level, Simon has made a breakthrough. | 0:35:10 | 0:35:14 | |
These tiny spiral shells | 0:35:15 | 0:35:17 | |
are typical of the species that grow in the shallow waters inside the Bristol Channel. | 0:35:17 | 0:35:22 | |
But these shells are only found at much greater depths - | 0:35:24 | 0:35:28 | |
out in the open ocean, over 50 miles away from where they were deposited. | 0:35:28 | 0:35:33 | |
One of the sand layers that we're looking at here is from North Devon | 0:35:33 | 0:35:37 | |
and it's full of species of microfossils that have come from the Continental Shelf, | 0:35:37 | 0:35:43 | |
so this sand layer has been transported from out on the open ocean. | 0:35:43 | 0:35:47 | |
All of Simon and Ted's evidence - | 0:35:48 | 0:35:50 | |
the boulder movements, the sand deposits and the erosion of headlands - | 0:35:50 | 0:35:54 | |
reveals the 1607 flood in greater detail than ever. | 0:35:54 | 0:35:58 | |
Yet they have a problem. | 0:35:58 | 0:36:00 | |
None of it is unique to a tsunami. | 0:36:00 | 0:36:04 | |
At the Proudman Laboratory, the same evidence fits their explanation for 1607. | 0:36:04 | 0:36:09 | |
A storm surge is going to provide some billion tons of water | 0:36:09 | 0:36:13 | |
rushing across the flood plain | 0:36:13 | 0:36:15 | |
that's more than capable of picking up enormous rocks | 0:36:15 | 0:36:18 | |
and large amounts of sediment | 0:36:18 | 0:36:20 | |
and depositing them a long way from their origin | 0:36:20 | 0:36:22 | |
and as far as rocks and sediments are concerned, | 0:36:22 | 0:36:25 | |
they can't distinguish between one large, rushing volume of water and another. | 0:36:25 | 0:36:29 | |
And whilst the storm surge modelled at the Proudman Laboratory is of record proportions, | 0:36:29 | 0:36:35 | |
history and the pamphlets themselves do not rule out such a freak event. | 0:36:35 | 0:36:40 | |
The morning of January the 20th 1607 would indeed have been one of the highest tides on record. | 0:36:44 | 0:36:51 | |
Furthermore, three of the pamphlets begin their story of the flood by describing stormy weather. | 0:36:51 | 0:36:58 | |
In the month of January last past, upon a Tuesday, the sea being very tempestuously moved by the winds, | 0:36:58 | 0:37:06 | |
overflowed his ordinary banks and did drown 26 parishes... | 0:37:06 | 0:37:10 | |
And upon the highest of the spring, the wind blowing very hard at south-west, | 0:37:10 | 0:37:15 | |
there was such a flood of tide as the like was never seen in this town. | 0:37:15 | 0:37:21 | |
But not all of the pamphlets describe the weather of that day as being stormy. | 0:37:21 | 0:37:26 | |
One of the most detailed reports actually states it was a sunny morning. | 0:37:26 | 0:37:30 | |
About nine of the clock in the morning, the sun being most fairly and brightly spread, | 0:37:32 | 0:37:37 | |
the farmers overseeing their grounds and looking to their cattle perceived far off | 0:37:37 | 0:37:43 | |
huge and mighty hills of water tumbling one over the other. | 0:37:43 | 0:37:47 | |
Simon has been through the pamphlets time and time again | 0:37:49 | 0:37:52 | |
and believes the very brevity of their weather descriptions is significant. | 0:37:52 | 0:37:57 | |
In the pamphlets the weather only gets one or two lines, | 0:37:57 | 0:38:01 | |
so it seems to me that it wasn't of spectacular proportions. | 0:38:01 | 0:38:05 | |
There doesn't seem to be an overall impression of a huge storm, | 0:38:05 | 0:38:09 | |
one that would be necessary to actually cause the flooding that we have recorded. | 0:38:09 | 0:38:14 | |
Instead, the thing that really stands out for Simon is the detail with which they describe the wave. | 0:38:14 | 0:38:21 | |
There is an overall theme running through all the pamphlets | 0:38:21 | 0:38:25 | |
of a destructive event, very violent, disastrous, on a scale that is unprecedented. | 0:38:25 | 0:38:32 | |
The waters ran with a swiftness so incredible that no greyhound could have escaped by running before them. | 0:38:33 | 0:38:40 | |
Whole houses were removed from the ground where they stood | 0:38:40 | 0:38:43 | |
and were floating up and down like ships half sunk, | 0:38:43 | 0:38:46 | |
which came in such swiftness that the fowls of the air could scarcely fly so fast. | 0:38:46 | 0:38:53 | |
In contrast, observers of the 1981 storm surge | 0:38:53 | 0:38:56 | |
remember the flood waters advancing at only a fast walking pace. | 0:38:56 | 0:39:00 | |
It's a different character altogether. | 0:39:02 | 0:39:04 | |
Much more violent in 1607, with waters rushing inland at a velocity... | 0:39:04 | 0:39:10 | |
You know, some of the accounts say faster than a greyhound can run. | 0:39:10 | 0:39:14 | |
Nowhere is the comparison between the storm surge of 1981 and possible tsunami of 1607 | 0:39:14 | 0:39:21 | |
starker than at the village of Uphill. | 0:39:21 | 0:39:24 | |
In 1981, the biggest storm floods of the last 100 years barely broke a window. | 0:39:24 | 0:39:31 | |
In 1607, the same village caught the full force of the wave, | 0:39:31 | 0:39:35 | |
as recorded in the fate of local landowner, John Good. | 0:39:35 | 0:39:39 | |
The gentleman with his wife and children got up to the highest room of the house. | 0:39:42 | 0:39:47 | |
There they sat comforting each other in their misery, hoping they might but go away with their lives. | 0:39:47 | 0:39:53 | |
Yet even that very desire for life put the gentleman | 0:39:53 | 0:39:57 | |
in mind to preserve something by which afterwards they might live | 0:39:57 | 0:40:02 | |
and that was a box of writing, wherein were certain bonds and all the evidence of his lands. | 0:40:02 | 0:40:08 | |
This box he got with much danger | 0:40:08 | 0:40:11 | |
and tied it with cords fast to a rafter, hoping there it would be safe. | 0:40:11 | 0:40:15 | |
But alas, in the midst of his gladness, the sea fell with such violence upon the house | 0:40:21 | 0:40:29 | |
that it bore away the whole building, rent it in the middle from top to bottom. | 0:40:29 | 0:40:35 | |
The gentleman in this whirlwind of waves got to a beam | 0:40:35 | 0:40:38 | |
and clinging to that was carried against his will for some three or four miles. | 0:40:38 | 0:40:43 | |
There he crept up and sat pouring out his tears | 0:40:45 | 0:40:48 | |
and to make him desperate in his sorrows | 0:40:48 | 0:40:51 | |
the tyrannous stream presented him with the tragedy of his dear wife and dearest children, | 0:40:51 | 0:40:58 | |
wrenched to their deaths by the torrent. | 0:40:58 | 0:41:01 | |
To the 17th-century mindset, such tragedy was evidence of nothing less than an apocalypse. | 0:41:04 | 0:41:11 | |
The readers of these pamphlets are not asking themselves, | 0:41:11 | 0:41:14 | |
"Was this a tidal wave? Was this the consequence of global warming?" | 0:41:14 | 0:41:18 | |
because the cause for the authors and for the readers is the same. | 0:41:18 | 0:41:24 | |
This is God. God has sent this. God sends weather. God sends waves. | 0:41:24 | 0:41:27 | |
So the root cause is the same and that's what's significant. | 0:41:27 | 0:41:30 | |
SHE SOBS | 0:41:30 | 0:41:34 | |
A BELL TOLLS | 0:41:36 | 0:41:40 | |
What is true for them is that this happened | 0:41:43 | 0:41:49 | |
and that this is a visitation by God. A warning of some kind. | 0:41:49 | 0:41:54 | |
In these cruel waters, many men, women and children lost their lives. | 0:41:58 | 0:42:04 | |
Dead bodies float hourly to the surface and are continually taken up. | 0:42:04 | 0:42:09 | |
Countless flocks of sheep are utterly destroyed. | 0:42:10 | 0:42:13 | |
The whole country shall feel the smart. | 0:42:15 | 0:42:19 | |
For Simon and Ted, the apocalyptic character of a tsunami | 0:42:22 | 0:42:26 | |
matches the testimony of 1607 far more convincingly than a storm surge. | 0:42:26 | 0:42:31 | |
But without a credible explanation for what triggered the tsunami in the first place, | 0:42:31 | 0:42:36 | |
Simon and Ted will struggle to persuade others. | 0:42:36 | 0:42:39 | |
They had assumed that their tsunami was triggered by a submarine landslide | 0:42:45 | 0:42:50 | |
but they are out of luck. | 0:42:50 | 0:42:52 | |
Detailed surveys of the continental shelf around Great Britain reveal no evidence of a landslide. | 0:42:52 | 0:42:58 | |
Their next best hope | 0:42:58 | 0:43:01 | |
is the possibility that an earthquake on its own could have triggered the tsunami. | 0:43:01 | 0:43:06 | |
At the British Geological Survey, Dr Roger Musson, head of seismic hazards, assesses that likelihood. | 0:43:06 | 0:43:13 | |
We're really driven to the conclusion | 0:43:13 | 0:43:15 | |
that it must have been an earthquake that was quite large | 0:43:15 | 0:43:19 | |
and produced a tsunami by actually breaking through the sea floor | 0:43:19 | 0:43:23 | |
and causing a vertical displacement. | 0:43:23 | 0:43:25 | |
The big surprise is that the sea bed off the south-west tip of Ireland | 0:43:25 | 0:43:29 | |
is far less stable than commonly imagined | 0:43:29 | 0:43:32 | |
and is the location of an ancient but massive fault line. | 0:43:32 | 0:43:38 | |
We still have this old weakness in the crust here | 0:43:38 | 0:43:41 | |
and it's been suggested that this is exactly the sort of place | 0:43:41 | 0:43:45 | |
where you could get an anomalously large earthquake happening. | 0:43:45 | 0:43:49 | |
It's not just an idle theory. | 0:43:49 | 0:43:52 | |
On the 8th of February 1980, sensors recorded an earthquake from exactly this area. | 0:43:52 | 0:43:58 | |
It was 4.5 on the Richter Scale - | 0:43:58 | 0:44:01 | |
not enough to lift the sea floor but violent enough to give fresh impetus to the tsunami theory. | 0:44:01 | 0:44:06 | |
So we know from geological grounds that this is a probable likely place | 0:44:06 | 0:44:12 | |
for getting an extra-large earthquake if we're going to get one anywhere around Britain | 0:44:12 | 0:44:17 | |
and we know from seismological evidence that we've actually had an earthquake here, | 0:44:17 | 0:44:22 | |
so there is a fault which is moving. It's active. | 0:44:22 | 0:44:25 | |
So putting a hypothetical large historical earthquake in this spot is not so fanciful. | 0:44:25 | 0:44:33 | |
To the oral history of the pamphlets, and the geological evidence they've discovered, | 0:44:33 | 0:44:38 | |
Simon and Ted can finally add a possible cause. | 0:44:38 | 0:44:42 | |
The final piece of their tsunami theory is in place. | 0:44:42 | 0:44:46 | |
This, now, is how they believe the killer wave may have struck 400 years ago. | 0:44:46 | 0:44:51 | |
On the morning of the 20th of January 1607, | 0:44:52 | 0:44:55 | |
an ancient fault line off the coast of Ireland shifted violently, | 0:44:55 | 0:44:59 | |
displacing enough water to generate a tsunami. | 0:44:59 | 0:45:04 | |
Moving at close to 100 miles per hour, the tsunami rushed up the Bristol Channel, | 0:45:14 | 0:45:19 | |
its force magnified by the high tide and the funnelling effect of the geography. | 0:45:19 | 0:45:24 | |
As it roared towards its unsuspecting victims, | 0:45:24 | 0:45:27 | |
it eroded headlands and pushed boulders aside like pebbles. | 0:45:27 | 0:45:33 | |
A wall of water up to ten metres high rushed over the low-lying sea defences either side of the Channel. | 0:45:39 | 0:45:46 | |
Now travelling at 30 miles an hour, | 0:45:57 | 0:45:59 | |
the killer wave bore down on the villages of Somerset and Monmouthshire. | 0:45:59 | 0:46:03 | |
In one giant slab of water, billions of gallons kept coming with terrible violence. | 0:46:23 | 0:46:31 | |
The people caught in its path had next to no warning. | 0:46:36 | 0:46:40 | |
And the force of the waters was such that even those who thought they were safe in their houses, | 0:46:42 | 0:46:48 | |
they were swept away also and the numbers and numbers of... | 0:46:48 | 0:46:52 | |
I'm doubly excited now about what we've found. | 0:47:02 | 0:47:05 | |
We've managed to go right round the estuary | 0:47:05 | 0:47:07 | |
and we've seen the physical evidence that supports the historical accounts. | 0:47:07 | 0:47:13 | |
There's nothing at odds there at all and everything is very consistent. | 0:47:13 | 0:47:17 | |
Whether it's sand on the salt marsh or it's pebbles in the clay | 0:47:20 | 0:47:23 | |
or it's erosion on the headlands or boulders piled up in key spots, you go for the simplest explanation | 0:47:23 | 0:47:29 | |
and I can put down most of the signatures we've seen in the past week very easily by one way, | 0:47:29 | 0:47:35 | |
one process, one point in time, and that's the simplest explanation. | 0:47:35 | 0:47:39 | |
I think it's a colossal event. | 0:47:39 | 0:47:41 | |
If it is a storm, it's a big one but if it's a tsunami, | 0:47:41 | 0:47:45 | |
it could be well within what we've experienced elsewhere in the world. | 0:47:45 | 0:47:49 | |
We're just not used to it here. | 0:47:49 | 0:47:51 | |
For the people struck down by the killer wave, | 0:47:54 | 0:47:56 | |
there is still no definitive answer as to why they died. | 0:47:56 | 0:48:00 | |
But their fate is not just a historical curiosity, | 0:48:00 | 0:48:04 | |
for what is not in doubt is the vulnerability of the Bristol Channel lowlands. | 0:48:04 | 0:48:08 | |
Where once there were only farms and hamlets are now modern towns and many thousands of people. | 0:48:08 | 0:48:15 | |
Tsunami or storm surge - | 0:48:15 | 0:48:17 | |
both could happen again. | 0:48:17 | 0:48:19 | |
Another freak storm would give us some warning. | 0:48:19 | 0:48:22 | |
A tsunami would not. | 0:48:22 | 0:48:24 | |
Subtitles by BBC Broadcast 2005 | 0:48:24 | 0:48:27 | |
E-mail us at [email protected] | 0:48:27 | 0:48:30 |