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I set out to understand some of the great landscapes of Britain, | 0:00:04 | 0:00:09 | |
to piece together the history that shaped them. | 0:00:09 | 0:00:13 | |
This is one of the most perplexing - the Fens. | 0:00:13 | 0:00:17 | |
A million acres of flat farmland, much of it below sea level. | 0:00:17 | 0:00:22 | |
Without thousands of canals, rivers and drains, it would disappear completely into marsh and mudflat. | 0:00:22 | 0:00:30 | |
It looks like an entirely man-made landscape. | 0:00:31 | 0:00:36 | |
The puzzle is - when was it made? | 0:00:36 | 0:00:39 | |
In one great feat of engineering? Or over thousands of years? | 0:00:39 | 0:00:44 | |
There's reclaimed and drained land throughout Britain, but nothing on the scale of the Fens. | 0:01:05 | 0:01:12 | |
They're in a great arc around the Wash. | 0:01:12 | 0:01:17 | |
It's a landscape as flat as the eye can see. | 0:01:17 | 0:01:21 | |
It's full of geometric patterns - straight lines of drainage ditches, right angles of fields. | 0:01:21 | 0:01:28 | |
It's like something off a drawing board. My first question is - | 0:01:28 | 0:01:33 | |
did this just grow up piecemeal through the centuries? Or was there ever a grand plan? | 0:01:33 | 0:01:40 | |
I went to Wisbech, to the museum. | 0:01:41 | 0:01:44 | |
I met Tom Williamson, a landscape historian working in East Anglia. | 0:01:44 | 0:01:50 | |
We looked out one of the earliest maps of the area, dating from 1631. | 0:01:50 | 0:01:56 | |
It shows that the Fens had not yet been drained. | 0:01:56 | 0:02:00 | |
This was a great, huge area of bog? | 0:02:00 | 0:02:04 | |
Yes, it's peat fen. Much of it would be flooded, certainly in winter - | 0:02:04 | 0:02:10 | |
reed beds, sedge beds, some grazing, a huge great common, really, teeming with life. | 0:02:10 | 0:02:16 | |
There's the Wash. This is this great area of peat fen, into which you have a series of rivers, | 0:02:16 | 0:02:23 | |
feeding from the Midlands and East Anglia - Cam, here, | 0:02:23 | 0:02:28 | |
-the Ouse and the Nene. -At what point did they start to drain? | 0:02:28 | 0:02:33 | |
There were sporadic attempts in medieval times, but the big drainage was in the 17th century. | 0:02:33 | 0:02:39 | |
How did they do it? Did they get in a great drainage expert? | 0:02:39 | 0:02:44 | |
Yes, a bloke called Vermuyden. Francis, the 4th Duke of Bedford, | 0:02:44 | 0:02:50 | |
and some financial backers called "adventurers" because they ventured their capital on the enterprise, | 0:02:50 | 0:02:57 | |
they employed a Dutch engineer called Vermuyden - people pronounce it different ways. | 0:02:57 | 0:03:04 | |
But his view was quite simple really. | 0:03:04 | 0:03:07 | |
The rivers all feed into here. They're sluggish and meander around | 0:03:07 | 0:03:12 | |
with silt deposits in their beds. | 0:03:12 | 0:03:14 | |
Their outfalls get choked. They're too sluggish and if you don't speed them up, they'll take the water | 0:03:14 | 0:03:21 | |
-across this peat fen quickly and out through to the North Sea into the Wash. -And carry the silt. | 0:03:21 | 0:03:28 | |
They'll be self-clearing channels. | 0:03:28 | 0:03:31 | |
So there really was a great plan. | 0:03:31 | 0:03:34 | |
In the 1630s, they think they can drain and develop the whole lot. | 0:03:34 | 0:03:39 | |
The great plan was to straighten out the silty rivers and then drain the land into them, | 0:03:40 | 0:03:47 | |
dividing it up into rectangular blocks for the adventurers. | 0:03:47 | 0:03:51 | |
The centre of the whole system was Vermuyden's new cut for the Ouse, named the Bedford River, | 0:03:51 | 0:03:58 | |
after the Fourth Duke, chief of the adventurers. | 0:03:58 | 0:04:02 | |
-Is this it? -That's right. 1637 that was completed. -God! | 0:04:02 | 0:04:07 | |
20 miles long. | 0:04:07 | 0:04:09 | |
20 miles dead straight. It'd be a major engineering achievement today. | 0:04:09 | 0:04:14 | |
Yeah. This was done with guys with spades and pickaxes and wheelbarrows. | 0:04:14 | 0:04:20 | |
It's a phenomenal thing. It takes a lot of the water of the Ouse so that it doesn't go meandering around. | 0:04:20 | 0:04:27 | |
It comes straight, speeding up the flow and preventing inundation, particularly in winter. | 0:04:27 | 0:04:34 | |
But the adventurers' grand plan ran into trouble. This had been common land | 0:04:34 | 0:04:40 | |
and local Fensmen resented the way it was being privatised by outside speculators. | 0:04:40 | 0:04:47 | |
And it wasn't long before the land started to flood again. | 0:04:47 | 0:04:51 | |
Once Vermuyden's cut was running, the Fens were drained, were they? | 0:04:54 | 0:05:00 | |
They were declared drained, but that's not the same thing. Flooding continued in many parts. | 0:05:00 | 0:05:07 | |
There wasn't enough capacity in these drains to get the water through and there was opposition, sabotage | 0:05:07 | 0:05:14 | |
and vandalism of the drainage works by the local commoners. | 0:05:14 | 0:05:18 | |
Then everything stopped for a while because of the Civil War. Then, in 1650-51, Vermuyden's back | 0:05:18 | 0:05:25 | |
-and they dig this, the new river bed. -Good heavens! -It's even bigger. -Monstrous! 20 miles again? | 0:05:25 | 0:05:32 | |
Yeah, parallel with the other. Doesn't silt up. Thousands of gallons pouring through it. | 0:05:32 | 0:05:38 | |
-And this IS still working? -Yes, it's the main arterial drainage channel for the peat fens. | 0:05:38 | 0:05:45 | |
-350 years and it's working. -Yeah. -So this was the Fens finally drained? | 0:05:45 | 0:05:50 | |
That's what they thought. But they were wrong. Come on, I'll show you. | 0:05:50 | 0:05:54 | |
What Vermuyden and the others hadn't realised was, as they drained the peat, it gradually shrinks. | 0:06:00 | 0:06:06 | |
It shrinks cos the water's removed and as it's ploughed, the peat surface desiccates and blows off. | 0:06:06 | 0:06:13 | |
-It falls and falls and falls. -How did they get the water up? | 0:06:13 | 0:06:18 | |
-The land must be ten metres below... -That's the most striking thing about the Fenland landscape. | 0:06:18 | 0:06:25 | |
All the rivers stand up above the farmland. | 0:06:25 | 0:06:28 | |
When you get to the late-17th, early-18th century, they have to pump the water from these lower levels | 0:06:28 | 0:06:35 | |
over this bank into the drain. | 0:06:35 | 0:06:38 | |
Where that house stands is the site of one of the wind pumps. | 0:06:38 | 0:06:43 | |
-There were two, one after the other, in steps. -To bring it up in stages? | 0:06:43 | 0:06:47 | |
Yes, sometimes there were three. All this area, you'd have seen hundreds, particularly on these main banks. | 0:06:47 | 0:06:54 | |
Absolutely full of them. | 0:06:54 | 0:06:57 | |
Then, in the 19th century, those are replaced by these - | 0:06:57 | 0:07:02 | |
by steam pumps. | 0:07:02 | 0:07:04 | |
And did the land go on shrinking? | 0:07:06 | 0:07:09 | |
The land goes on shrinking, but the steam pumps are gradually replaced by more modern technology, | 0:07:09 | 0:07:17 | |
-which we have here. -Great diesel. | 0:07:17 | 0:07:20 | |
The adventurers' investment straightened out and speeded up the rivers | 0:07:27 | 0:07:33 | |
so that the land could be drained into them and shared out. | 0:07:33 | 0:07:37 | |
But for 300 years, the peat's been drying, decaying and disappearing. | 0:07:37 | 0:07:42 | |
In some places, it's ten metres below its original level. | 0:07:42 | 0:07:46 | |
It was too much for the wind and steam pumps. What about modern ones? | 0:07:46 | 0:07:51 | |
You really have got a demonstration of the levels, haven't you? | 0:07:54 | 0:07:58 | |
There's the windmill up there, then the steam pump, then the diesel, | 0:07:58 | 0:08:03 | |
-and the latest - the electric pump at the bottom. -Yes. -How much longer can this go on? -Not much longer. | 0:08:03 | 0:08:11 | |
Down here, we've got the peat soil. | 0:08:11 | 0:08:14 | |
As you rummage around, you find, in places, they're ploughing through into the clay. | 0:08:14 | 0:08:20 | |
-Down to the bedrock. -Effectively, that's right. | 0:08:20 | 0:08:25 | |
Whereas peat is wonderfully fertile - as anyone buying it from the garden centre knows - this stuff is not. | 0:08:25 | 0:08:32 | |
So the amount of effort and money put in to keep this dry is not going to be viable eventually. | 0:08:32 | 0:08:39 | |
If you turn that thing off, within a few months, this will be under water. | 0:08:39 | 0:08:45 | |
-The Fens come back. -The Fens come back. | 0:08:45 | 0:08:49 | |
The adventurers' grand design may be near the end of its life. | 0:09:00 | 0:09:04 | |
I tried to imagine what the Fens would be like if they came back. | 0:09:04 | 0:09:09 | |
I remembered how the Fensmen sabotaged the original drainage. | 0:09:09 | 0:09:15 | |
What had been so attractive about a bog? | 0:09:15 | 0:09:18 | |
I asked archeologist Ben Robinson and he took me to Wood Walton, | 0:09:18 | 0:09:23 | |
a few acres that have amazingly survived. | 0:09:23 | 0:09:28 | |
It looks to us a very beautiful, restful place, but presumably they thought it was wasted ground. | 0:09:28 | 0:09:35 | |
Not at all. It's got everything you need to sustain life. | 0:09:35 | 0:09:39 | |
These meres would have been shallow. The medieval fen would be stuffed full of fish and eels. | 0:09:39 | 0:09:46 | |
The reeds were harvested for building materials, the peat was cut for fuel. Woodland fringes this area, | 0:09:46 | 0:09:53 | |
which again was used for fuel and building, so it's full of resources. | 0:09:53 | 0:09:58 | |
We talk about biodiversity and rainforest, but fenland had it all. | 0:09:58 | 0:10:02 | |
-You make it sound as if they lived rather well. -Yeah. | 0:10:02 | 0:10:06 | |
The monasteries carved up the whole fenland region among themselves... | 0:10:06 | 0:10:11 | |
-And grow rich on it. -Yes, Ely ended up amongst the richest monasteries. | 0:10:11 | 0:10:16 | |
I could see now why the Fensmen sabotaged the great drainage. | 0:10:18 | 0:10:23 | |
In the Middle Ages, these were among the richest lands in England. | 0:10:23 | 0:10:28 | |
But wherever did they live? | 0:10:28 | 0:10:31 | |
Ben, who turned out to be a man of many parts, took me to see. Medieval Fensmen lived on islands. | 0:10:31 | 0:10:38 | |
There's a small fen island down there sticking up from the fen floor. | 0:10:38 | 0:10:44 | |
-It's surrounded by a drain. -It does look like an island. -That's right. | 0:10:44 | 0:10:49 | |
Exactly. An entirely different sort of field on top of the island there. | 0:10:49 | 0:10:54 | |
You can see most of the houses on the ridge on the firm ground, | 0:10:54 | 0:10:59 | |
surrounded by rectangular reclamation fields. | 0:10:59 | 0:11:02 | |
-It would flood on each side. There'd be reed beds. -The fringes would be surrounded by seasonally flooded land | 0:11:02 | 0:11:09 | |
which might have been taken in for summer pasture. | 0:11:09 | 0:11:13 | |
There'd be reed bed further out and then a few meres. It would have stuck out as somewhere quite different. | 0:11:13 | 0:11:21 | |
There'd be orchards on some of these medieval islands, even vineyards. | 0:11:23 | 0:11:28 | |
-Really? -On ones owned by monasteries. They really looked different. | 0:11:28 | 0:11:33 | |
It's very clear down there. | 0:11:33 | 0:11:36 | |
Before the great drainage of the 17th century, the Fen was a vast expanse of waterways and bog, | 0:11:40 | 0:11:47 | |
rich in reeds, rushes, summer grass and wildlife. | 0:11:47 | 0:11:51 | |
Its people lived on islands which they ploughed and cultivated - | 0:11:51 | 0:11:56 | |
a rare and rich way of life. | 0:11:56 | 0:11:59 | |
So the Fens aren't just a 17th-century landscape. | 0:11:59 | 0:12:03 | |
Medieval villages and fields survive if you know how to see them. | 0:12:03 | 0:12:09 | |
I drove north looking for other old fenland landscapes. | 0:12:09 | 0:12:13 | |
I'd almost reached the Wash when I hit a string of villages, each with a fine medieval church. | 0:12:13 | 0:12:19 | |
Whaplode, Fleet, Holbeach - old names. | 0:12:19 | 0:12:25 | |
And the landscape looks rather different - the fields are smaller, the soil is paler. | 0:12:25 | 0:12:32 | |
Is it possible this is another ancient landscape surviving in the Fens? | 0:12:32 | 0:12:39 | |
Along both sides of this narrow strip of old villages, | 0:12:39 | 0:12:44 | |
I noticed a succession of high banks snaking through the landscape, | 0:12:44 | 0:12:49 | |
most of them topped with roads. | 0:12:49 | 0:12:51 | |
It looked like these villages had built banks to keep the water back. | 0:12:51 | 0:12:56 | |
I asked Tom Lane, a fenland archaeologist. | 0:12:56 | 0:13:01 | |
When these villages were built, they must have been on quite a narrow strip of land. | 0:13:01 | 0:13:07 | |
It couldn't have been more than a mile and a half across. | 0:13:07 | 0:13:11 | |
It's almost like existing on a sandbank really. | 0:13:11 | 0:13:16 | |
They were really on the edge of the sea, I suppose. | 0:13:16 | 0:13:20 | |
They were in danger of going UNDER the sea. That's why these banks were so important. | 0:13:20 | 0:13:26 | |
At one time, the Wash continually flooded this area, reaching far inland. | 0:13:26 | 0:13:32 | |
That's why the soil is light and silty. The villagers built banks to keep the water away from their land. | 0:13:32 | 0:13:40 | |
From the air, you can see the banks, because now they have roads on top. | 0:13:40 | 0:13:45 | |
Tom said the oldest were to landward, built out into the Fen. | 0:13:45 | 0:13:50 | |
The first bank was built by Domesday - by 1086. | 0:13:53 | 0:13:59 | |
It's the one down there that's so wiggly. | 0:13:59 | 0:14:02 | |
That's because it was built in small lengths - | 0:14:02 | 0:14:07 | |
the Whaplode people, the Holbeach people, the Gedney people - | 0:14:07 | 0:14:11 | |
each doing their contribution - a fantastic community effort. | 0:14:11 | 0:14:16 | |
-That's good soil, isn't it? -Silt soil is the most fertile in Britain. | 0:14:16 | 0:14:22 | |
That's why they were so successful when they made the banks. Initially, it was for protection, | 0:14:22 | 0:14:28 | |
but it worked as reclamation. They ploughed it because it was fertile. | 0:14:28 | 0:14:33 | |
We're also quickly coming up to the third one, which is called Hassock Dyke, 1180 this one. | 0:14:33 | 0:14:40 | |
It's just a straight line. There's actually one more, a common dyke, | 0:14:40 | 0:14:45 | |
which is built round about 1215 | 0:14:45 | 0:14:49 | |
or into the mid-13th century. | 0:14:49 | 0:14:52 | |
Brilliant little system. | 0:14:52 | 0:14:55 | |
As the silty soil behind the banks dried, it turned out to be even more valuable than the Fen. | 0:14:57 | 0:15:04 | |
So between about 1050 and 1250, these villages built more and more banks and reclaimed 90 square miles. | 0:15:04 | 0:15:11 | |
They crossed their new land with drove roads for cattle to graze the peaty fen beyond. | 0:15:11 | 0:15:18 | |
It's another surviving medieval landscape. | 0:15:18 | 0:15:21 | |
So successful were the banks, that from the 13th or 14th century, | 0:15:21 | 0:15:26 | |
the villagers built them on the other side, out towards the sea. | 0:15:26 | 0:15:31 | |
And here they've been building them ever since. | 0:15:31 | 0:15:36 | |
We threaded between the banks along the River Nene, towards the Wash. | 0:15:36 | 0:15:41 | |
Once, it was just an open landscape, miles and miles of salt marsh. | 0:15:41 | 0:15:46 | |
-They made salt here. -Sea salt was a huge industry in the Wash area in medieval times and before. | 0:15:46 | 0:15:54 | |
So the sea banks changed it all. | 0:15:54 | 0:15:57 | |
What happened was that people were able to reclaim land further and further out. | 0:15:57 | 0:16:04 | |
-When this lighthouse was built, this was the end of the land. -On the sea? | 0:16:04 | 0:16:09 | |
-Right on the sea. -So people have been winning back the land through the ages. | 0:16:09 | 0:16:16 | |
"Winning back the land" is the right phrase - over a very long period. | 0:16:16 | 0:16:22 | |
This medieval landscape of dykes and drove roads stretches almost all around the edge of the Wash. | 0:16:23 | 0:16:31 | |
Fensmen had after all been reclaiming little sections of land | 0:16:31 | 0:16:37 | |
before the great 17th-century plan. | 0:16:37 | 0:16:40 | |
I began to wonder how far back in time this piecemeal fen drainage went. | 0:16:40 | 0:16:46 | |
It's an astonishing thought that that's an ancient drove road | 0:16:48 | 0:16:53 | |
and some of these banks and ditches date back more than 1,000 years. | 0:16:53 | 0:16:58 | |
But people here will tell you the Romans started all this off. | 0:16:58 | 0:17:03 | |
So the next question is - | 0:17:03 | 0:17:06 | |
was it the Romans who first drained the Fens? | 0:17:06 | 0:17:10 | |
Everyone told me that the person to ask about Romans is Rog Palmer. | 0:17:15 | 0:17:21 | |
He's a photographer in Cambridge, using aerial photographs to map out faint traces of Roman remains. | 0:17:21 | 0:17:28 | |
What I'm doing is drawing out the archeological features I can see. | 0:17:28 | 0:17:35 | |
We can see some of the enclosures here, which would have been settlement enclosures or for stock. | 0:17:35 | 0:17:42 | |
A linear feature there which doesn't look like a track, but might be. | 0:17:42 | 0:17:47 | |
Most of what I'm seeing here are the ditches from former settlements and occupation. | 0:17:49 | 0:17:55 | |
So these are actually Roman? We've got Romans living in the Fens? | 0:17:55 | 0:18:01 | |
What we see on the Fens is Iron-Age peasants carrying on being peasants, | 0:18:01 | 0:18:07 | |
but under Roman government, if you like. These aren't Romans in togas. | 0:18:07 | 0:18:12 | |
Roger's photographs are oblique views from the side of a plane. | 0:18:14 | 0:18:19 | |
He straightens his tracings up by computer, then plots them on a map. | 0:18:19 | 0:18:24 | |
Piece by piece, he's been building a complete picture of Roman settlements in the Fens. | 0:18:24 | 0:18:31 | |
One thing that strikes the eye is this great string here. | 0:18:32 | 0:18:38 | |
They're all the way along in this line. Was it a main road they built? | 0:18:38 | 0:18:44 | |
No, these settlements were on the high and dry ground, | 0:18:44 | 0:18:48 | |
which were the silted beds of old rivers which we call "roddens" now. | 0:18:48 | 0:18:53 | |
-So this was a pattern of high ground at the time? -Yes. | 0:18:53 | 0:18:57 | |
The rodden was a river in Neolithic times, | 0:18:57 | 0:19:01 | |
which has silted up since then and the silt is hard and compact | 0:19:01 | 0:19:07 | |
and doesn't compress as much as the peat does. | 0:19:07 | 0:19:11 | |
So the rodden stands in places two metres above the ground surface. | 0:19:11 | 0:19:16 | |
-This is the pattern of settlements here? -Yes, they were on the roddens. | 0:19:16 | 0:19:21 | |
It's amazingly precise, isn't it? | 0:19:21 | 0:19:24 | |
-Well... -It's astonishing. | 0:19:24 | 0:19:26 | |
So the Romans didn't drain the Fens. They didn't need to do so. | 0:19:26 | 0:19:32 | |
They used the high ground, yes, with no drainage. | 0:19:32 | 0:19:36 | |
The Romans didn't drain the Fens - they lived on the dry roddens. | 0:19:36 | 0:19:40 | |
But as the Roman Empire fell, the water table rose and the roddens and settlements disappeared. | 0:19:40 | 0:19:47 | |
Now the peat has shrunk, the roddens are back - strange humps in the landscape. | 0:19:47 | 0:19:53 | |
But the rest of the Roman world is gone. | 0:19:53 | 0:19:57 | |
Makes you wonder whether that is the end of the story. | 0:19:58 | 0:20:02 | |
Well, it's an amazing thing that Francis Pryor, at Flag Fen, | 0:20:02 | 0:20:08 | |
has discovered not only earlier settlements, but a whole earlier landscape. | 0:20:08 | 0:20:15 | |
Francis took me to a drove road, one reconstructed from his archeological evidence. | 0:20:22 | 0:20:28 | |
It dates back to long before the Romans. | 0:20:28 | 0:20:32 | |
At about two and a half thousand years BC, there were huge flocks of animals around here... | 0:20:32 | 0:20:39 | |
-So we're talking 4,000-5,000 years ago? -Yes, the early Bronze Age. | 0:20:39 | 0:20:44 | |
-This was a pastoral economy. -Yes, a very specialised pastoral economy. | 0:20:44 | 0:20:49 | |
As you can see by this. This is a specialised land-management feature, this Bronze-Age road. | 0:20:49 | 0:20:56 | |
It's on a grand scale, this great roadway here. | 0:20:56 | 0:21:01 | |
There were loads of these roadways, where people took their animals. | 0:21:01 | 0:21:06 | |
-This extends over a large area of the Fens here. -Yeah. | 0:21:06 | 0:21:11 | |
Absolutely soaking wet. What did they do? Did they drain the land? | 0:21:11 | 0:21:17 | |
No, it wasn't soaking wet. It was dry. | 0:21:17 | 0:21:21 | |
-This was dry land? -In the Bronze Age. | 0:21:21 | 0:21:25 | |
The fens around here STARTED to form about 2000 BC. | 0:21:25 | 0:21:29 | |
-So the Fens were dry? -There WERE wet patches, but not the huge expanses of peat that formed later. | 0:21:29 | 0:21:36 | |
I wanted to know how Francis could be so sure this landscape was first flooded during the Bronze Age. | 0:21:39 | 0:21:46 | |
He took me to the remains of a timber platform he'd discovered. | 0:21:46 | 0:21:51 | |
It was built about 1300 BC, late in the Bronze Age. | 0:21:51 | 0:21:56 | |
Francis's theory is that it stood right through the years when this land passed from bone dry to fen. | 0:21:56 | 0:22:03 | |
In the early Bronze Age, this would have been just getting a bit boggy. | 0:22:03 | 0:22:09 | |
Then the water slowly crept up, inch by inch. Every winter, the flooding got worse and worse. | 0:22:09 | 0:22:16 | |
And that's why those posts have survived as high as they do. | 0:22:16 | 0:22:20 | |
If they hadn't been wet to the top of the post, none of that wood would have survived. | 0:22:20 | 0:22:27 | |
-This was a platform, a walkway? -And much more than that. | 0:22:27 | 0:22:31 | |
I imagine this line of posts was a sort of symbolic wall against the incoming waters - | 0:22:31 | 0:22:38 | |
a King Canute effect. So they come to the posts to make their offerings | 0:22:38 | 0:22:43 | |
-at the posts. -What sort of offerings? -Valuable offerings - bronze swords, | 0:22:43 | 0:22:49 | |
daggers, spearheads. They're actually sending a message to the ancestors, | 0:22:49 | 0:22:55 | |
saying, "Keep back, water." | 0:22:55 | 0:22:58 | |
Because it's the ancestors who they believed controlled the elements like flooding and storms. | 0:22:58 | 0:23:05 | |
-Then we have a picture of this landscape changing over time... -Slow change was from about 2000-3000 BC, | 0:23:05 | 0:23:13 | |
as the land slowly began to get flooded. | 0:23:13 | 0:23:16 | |
Then the flooding got worse and worse and about 1000 BC, it was really serious. | 0:23:16 | 0:23:23 | |
So that when the Romans came here in 43 AD, this part of the Fen was just water. | 0:23:23 | 0:23:29 | |
It's all very well as theory, but could I dig up any evidence | 0:23:31 | 0:23:36 | |
to show exactly how dry fields had been transformed into a bog of peat and silt? | 0:23:36 | 0:23:42 | |
Charlie French is a soil specialist. He's studied a prehistoric land surface, uncovered during quarrying | 0:23:42 | 0:23:50 | |
near the River Ouse, on the western edge of the Fens. | 0:23:50 | 0:23:54 | |
How far back in time does this cut take us? | 0:23:54 | 0:23:57 | |
What we're looking at is an old ground surface that was used until about the last 3,000 years. | 0:23:57 | 0:24:04 | |
So from here to here, if I clean this off, | 0:24:04 | 0:24:08 | |
we've actually got a buried soil, | 0:24:08 | 0:24:11 | |
so where you see this mottled grey and orange sitting on top of terraced sands and gravels. | 0:24:11 | 0:24:18 | |
-It was dry at this time. -Yeah, very much a dry-land situation with woodland and trees. | 0:24:18 | 0:24:25 | |
Eventually it becomes subsumed. You see these darker deposits here - a mixture of freshwater peat, | 0:24:25 | 0:24:32 | |
which is coming in from the Fens with rising water tables, | 0:24:32 | 0:24:37 | |
mixed with freshwater silts and clays, this blocky material here, | 0:24:37 | 0:24:42 | |
which comes inland from Bedfordshire and so on, spreading out over this | 0:24:42 | 0:24:46 | |
and getting that combination of two flows - one from inland, one from the Fens to the east. | 0:24:46 | 0:24:53 | |
So when the Fens were first flooded, water came from two directions. | 0:24:53 | 0:24:58 | |
It's a story Charlie has pieced together by examining fenland soils under the microscope. | 0:24:58 | 0:25:04 | |
Water was coming from one direction because, 5,000 years ago, | 0:25:04 | 0:25:09 | |
melting ice from the last ice age was raising the sea level, flooding the area around the Wash. | 0:25:09 | 0:25:16 | |
As the land became boggier, the first peat began to form. | 0:25:16 | 0:25:20 | |
By the later Bronze Age, we have a great swathe of peat, | 0:25:20 | 0:25:25 | |
3,000 years ago, running up these major channel systems like the Ouse, | 0:25:25 | 0:25:32 | |
where we actually get peat formation or the build-up of organic remains. | 0:25:32 | 0:25:38 | |
The whole slide, as you might expect, dominated by organic matter. | 0:25:38 | 0:25:44 | |
'But then something else began to happen, which clogged up and spread out the rivers coming from inland.' | 0:25:44 | 0:25:51 | |
At the same time, in Bedfordshire, Leicestershire and Hertfordshire, | 0:25:51 | 0:25:56 | |
-we get clearance on thick, heavy soil for the first time. -Felling? -Yes, ploughing for the first time. | 0:25:56 | 0:26:03 | |
New sediment - clay and silt - gets into the water system, as we've seen on these slides. | 0:26:03 | 0:26:10 | |
Here, where we get fantastic silt and clay through the whole system. | 0:26:10 | 0:26:17 | |
-Masses of silt coming down those rivers. -And, of course, it can't get out to the sea. | 0:26:17 | 0:26:23 | |
It spreads out, ponds back against that peat. | 0:26:23 | 0:26:28 | |
The material finally settles out of suspension in still-water conditions | 0:26:28 | 0:26:33 | |
And the water is locked in that great basin. There's an irony here. | 0:26:33 | 0:26:39 | |
We think of human action destroying the Fens, but your work shows that 5,000 years ago, | 0:26:39 | 0:26:45 | |
human activity helped create the Fens. | 0:26:45 | 0:26:49 | |
It was human exploitation of a wide catchment area around the system | 0:26:49 | 0:26:54 | |
which contributes to the formations we see today. | 0:26:54 | 0:26:58 | |
So water flooded this land from two directions - it came from the sea | 0:26:59 | 0:27:04 | |
and also from the slow, silty rivers clogged by the first farmers ploughing heavy soils in the west, | 0:27:04 | 0:27:11 | |
the same rivers the great drainage engineers would struggle to speed up 4,000 years later. | 0:27:11 | 0:27:18 | |
Before I left, I went back to that steam pump on the Bedford River. | 0:27:18 | 0:27:23 | |
I saw that this drained landscape is just a short episode in the history | 0:27:23 | 0:27:29 | |
of the way we've moulded these vast, flat acres. | 0:27:29 | 0:27:34 | |
I first saw the Fens as a man-made landscape, with its straight ditches and right-angled fields, | 0:27:34 | 0:27:40 | |
and it's true - it IS a man-made landscape, but in a way totally unexpected to me. | 0:27:40 | 0:27:47 | |
People thousands of years ago in middle England felled and cultivated and brought the silt down. | 0:27:47 | 0:27:53 | |
They created the Fens. | 0:27:53 | 0:27:56 | |
But the Fens are coming to another turning point in their history | 0:27:56 | 0:28:01 | |
because, after three centuries of drainage and cultivation, the peat's almost all gone | 0:28:01 | 0:28:08 | |
The bedrock clay is coming out. | 0:28:08 | 0:28:11 | |
It may not be economic to continue pumping. | 0:28:11 | 0:28:15 | |
It's an extraordinary thought that perhaps the waters will come back | 0:28:15 | 0:28:20 | |
and the reed beds, the willow, the alder and wildfowl will return, | 0:28:20 | 0:28:25 | |
just like in the Middle Ages. | 0:28:25 | 0:28:28 | |
Subtitles by Roger Young BBC Scotland - 2000 | 0:28:44 | 0:28:48 | |
E-mail us at [email protected] | 0:28:48 | 0:28:52 |