89: Whittlesey Mere
Once it was southern England’s largest inland lake. Today, that water has long been drained for agriculture – but it may be about to make a partial comback.
Where is it?

The Holme Fen Post.
When
originally driven in in 1852 its
topmost point
was at the level
of the ground which has sunk
13ft in a century-and-a-half.
Whittlesey Mere is on the western edge
of the fens, south-east of Peterborough
near the villages of Yaxley, Farcet,
Holme and Stilton. It’s hard to believe
now that these neat rows of fields, with
long straight roads and equally straight
drainage ditches – ‘dykes’ – was once a
vast lake. It stretched about three miles
east to west and two-and-a-half miles
north to south in the summer, while
winter flooding could make it even
larger. Until the 19th century it was a
paradise for boaters and fishermen,
teeming with wildlife all year round and
used by skaters in the winter when
frozen.
Man-made or natural?
Unlike the Norfolk Broads, now believed
to be diggings which later flooded,
geologists say Whittlesey Mere was
created by nature. About 6,000 years
ago forest covered what is now the fens,
this large area in parts of Norfolk,
Cambridgeshire and Lincolnshire, and
prehistoric man hunted in forests of oak,
yew and pine. Rising sea levels held
back river flows, waterlogging the fen
basin and drowning trees. Reeds and
sedges thrived in wet conditions and
peat formed from the remains of dead
vegetation. In low-lying areas it led to
the creation of lakes or meres. The
skeleton of a killer whale has been
found on the bed of the mere. By
Victorian times it was seven metres
(about 21ft) deep in places. This
situation existed for centuries, and a
hardy breed of people – the legendary
Fen Tigers – lived by waterfowling in the
watery landscape. Monasteries were
built on islands, attracted by the
isolation of the place; after the mere
was drained, silver treasures from
nearby Ramsey Abbey were found at the
bottom. Although the Romans undertook
some small-scale drainage, continued in
medieval times, it was not until the 17th
century that people looked seriously at
changing the landscape with large-scale
projects.
Why would they want to?
Profit. The fertile peat soil would in time
be turned into the bread basket of
England, a huge agricultural area to
feed a growing population. But we are
getting ahead of ourselves. While
Dutchman Cornelius Vermuyden, backed
by wealthy cash ‘adventurers’, was busy
straightening rivers and draining vast
areas of fenland elsewhere, Whittlesey
Mere remained largely untouched. In
summer it was a playground for the rich.
George Walpole, third earl of Orford,
grandson of Britain’s first prime minister,
sailed a flotilla of nine boats to the mere
in 1774 for a month of nautical high
jinks, along with the Earl of Sandwich.
Humble folk made the best of the hard
winters of the period; from the 17th to
19th centuries the mere was regularly
frozen over. Skating championships were
held with big cash prizes offered. It is
said a top skater could cover a mile in
just three minutes over the ice.
Nineteenth century writer Charles
Kingsley claimed some expert skaters
even chased pike seen beneath the ice,
tracking the fish until they were
exhausted, then breaking the ice and
netting them. Wildlife such as the
bittern thrived, along with uncounted
numbers of geese, swans and heron
which hid in the reedbeds. The
swallowtail butterfly was common there
along with copper butterflies and many
other species of fauna and flora.
And then came the adventurers...
By the 1840s a group of businessmen
– called adventurers as they
‘adventured’ their money – had plans
for the mere. To these hard-headed
capitalists, the mere was wasted. It
was time this land was put to work. The
usual methods of drainage – digging
ditches – proved inadequate, but
modern science came to their aid. A
centrifugal pump demonstrated at the
Crystal Palace in 1851 could get rid of
70 tons of water in a minute. Holme
landowner William Wells bought one,
powered by a steam engine, and
installed it in a pumping station. Soon
the mere was dry. Fishermen, boaters,
skaters and, of course, the wildlife were
left high and dry. A pike said to weigh
52lb – the biggest found in Britain –
was among the casualties.
And the results?
A way of life came to an end. The
adventurers reaped the rewards. What
was once only useful as fen for cutting
reeds was now prime agricultural land.
Rents soared. But there was another
consequence. The peat shrank
dramatically once it dried out and was
exposed to bacteria and winds. Realising
this, Wells sank an iron post deep into
the ground near Holme in 1852. Within
10 years the top of the post stuck out
six feet above the ground and this
shrinkage continued until the end of the
century. It has slowed since, but now
the peat has shrunk 13ft in the centuryand-
a-half since installation. This is the
lowest point in the country, seven feet
below sea level.
What will happen if sea
levels rise, as predicted?
A second post
was sunk in 1957.
What’s the future?
Birch wood grew as the fen dried up.
Some fragments of the original fen and
bog remain; they are managed by
Natural England, which helps rare plants
survive. The Holme Fen Reserve posts
are surrounded by woodland; it is eerily
quiet despite being close to the A1 and
the railway line. Geese and swans still
have a haven in small lakes, ghosts of
what used to exist here. Commercial
peat-cutting in the reserve has led to
the creation of areas of open water that
support birds, dragonflies and marsh
plants such as golden dock. More
ambitious is the Great Fen Project, a
scheme to see 7,000 acres of farmland
in the area returned to natural fen.
Supported by local authorities and
conservationists, the plan is to gradually
buy back farmland, pump water back in
and create a wildlife reserve that could
even harbour the likes of the bittern and
copper butterfly. The Whittlesey Mere
that existed before 1851 might make a
partial comeback.