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Fordhead
Farm 
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Fordhead Farm
overlooks the Fords of Frew on the River Forth, some 9 miles west
of Stirling in Central Scotland. This region, known as the Carse
of Stirling is one of the most fertile areas in Scotland.
The Carse is regarded as 'Scotlands Hay Basket' and at Fordhead,
one of the main crops is Timothy Hay, a high quality variety that
is particularly suited to the area. Grain crops in the form of
Wheat, Barley and Oats are grown here with yields of up to 4 tons
per acre in an exceptional year. Cattle and Sheep thrive on the
lush pastures and Fordhead has its own small Aberdeen Angus Herd.
Fordhead offers two self-catering cottages for superb holidays
in the midst of the finest scenery in Scotland.
This page gives a brief history of the Fordhead area and the activities
of its inhabitants.
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After
the Ice Age 
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Evidence of huge changes
in the land and water of the Forth Valley and its surroundings are preserved
in the layers of peat that make up the ancient Flanders Moss.
More than 11,000 years ago, the Menteith Glacier dumped ridges and mounds
of sand, gravel and clay as it melted here.
As a result of the retreating ice, the sea level rose, and about 9,600 years
ago fell again, stranding a beach that was later smothered in the great
Forth Valley peat bog.
Some 8,500 years ago, the sea returned in force. It almost cut the country
in two, leaving only an 8 kilometer wide neck of land linking northern and
southern Scotland. Buried seashells and the clay-rich 'Carse' deposits of
the valley floor provide evidence of that time. As a testament to this marine
phase, the complete skeleton of a whale was found only 4 miles from Fordhead
towards Stirling.
Around 7,000 years ago, an underwater landslide off the Norwegian coast
propelled a huge tidal wave or 'Tsunami' across the North Sea to Scotland.
When it hit the Forth Valley, it was still 15 meters high. Fine sand within
the strata of the remaining bogland marks the fall-out from this event.
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The
Flanders Moss 
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Arial
view
of
Flanders Moss
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Fordhead is located on the eastern margins of the Flanders Moss.
This large expanse of ancient bog is all that remains of the huge
marshlands that covered the Forth Valley in former times.
'Raised Bogs' like Flanders Moss - so called because they grow
above the surrounding landscape - form immense domes of peat,
with a living skin of plants. These domes began to form in the
valley after the sea levels dropped.
'Sphagnum' mosses power the upward growth of a raised bog, slowly
adding layer upon layer and forming the bulk of the plant material
in the peat. Several sphagnum species grow on Flanders Moss, creating
a colourful patchwork of emerald, amber, tawny and claret.
Amazingly, water can form up to 98% of the bog! The mosses soak
up water like a sponge and grow upwards from their tips, leaving
the lower, shaded parts to die. Gradually, this material forms
peat, adding less than a needle-width 1mm per year to the bog
height. Over the thousands of years, this tiny growth has resulted
in peat that is piled over 7m in depth on Flanders.
Raised bogs form when they no longer rely on incoming groundwater
and are fed purely by rainwater. Flanders Moss reached that lofty
position thousands of years ago and its rare size and quality
have led it to being nominated as one of the European Union's
'Special Areas of Conservation'
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The
Early Inhabitants 
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Ancient remains
of Broch's, a Bronze Age bucket (right), swords and Britains oldest
wheel show that this part of the Forth Valley has been used by
people for thousands of years.
The boglands were a treacherous natural barrier that thwarted
the efforts of many invasions from north or south. When the Romans
arrived in Scotland, they swiftly moved up the eastern side of
the valley through Stirling, but, like many armies before them,
were halted by the great bog to the west.
Local inhabitants and defenders from the northern side of the
valley knew the bog-lands well. They harried and attacked the
Romans from the relative safety of the marshes and the wooded
areas. The Roman response to this annoyance is seen in the thousands
of preserved oak and birch trees - all found in a layer that corresponds
to Roman times. The tree trunks show clear signs of axe blows
and their associated stumps are nearby. By felling the trees,
all the cover was gone and advance warning of any attack was possible.
As an irony to their solution, the water that was drawn up by
all those trees was now available to enhance the raised bog.
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The
Fords of Frew 
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'Frew'
is the name of the area to the west, north and east of Fordhead.
Many of the farms in the area bear the legacy of this old name
as seen in Wester Frew, North-mid-Frew, Easter Frew and Bridge
of Frew. In other words, their geographical relationship to the
area is in their name. Similarly, Fordhead is situated at the
Head of this Ford.
The Fords of Frew are mentioned in a number of historical documents
and events. Their importance as a crossing place over the Forth
is easy to understand when you consider that, at the time, there
was no other place until you reached Stirling. This fact made
Stirling an obvious place to settle and fortify as it also has
good access to the east via the river.
Over the years, various fortifications were constructed to protect
the Fords, although long gone, their existance lives on in the
form of place names to this day.
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The actual Fords constitute a mile long stretch of the
river to the east of the present day bridge.
The old Drover Road that leads through the Ford is marked
by a mile stone on the southern bank of the river. (Photo
to follow soon). The stone informs the traveller of the
distance to Burnfoot - 6 miles south, high in the hills.
The Boquhan Burn joins the Forth just west of the Ford.
The normal sandy/muddy bottom is replaced by smooth stones
and gravel from this point on.
It seems highly probable that stones and gravel from the
burn (washed downstream during periods of flood) is responsible
for the riverbed at this section.
During the summer months - especially during a long dry
period, it is possible to make your way across the river
(with a pair of ordinary wellington boots) at this spot.
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Outwith
the summer months, the water level is never low enough to repeat
this easy crossing. In fact, the speed of the river at the Fords
is somewhat intimidating (as well as a lot colder). Suffice to
say, if the Fords were used on a regular basis throughout the
year, our forefathers were made of stronger stuff than their decendants
of today.
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Historical
Crossings 
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It cant be
stressed enough how treacherous the bog lands were for travellers,
(and in fact, they still are today).
This photograph shows the top surface of the moss and the abundance
of water. Considering its height above the surrounding land, the
amazing ability of the bog to retain water should be apparent.
This high water content makes travel on unfamiliar moss a very
dangerous practice indeed. Solid-looking ground could well be
a layer of moss over a spongy pit of rotting vegetation and could
be several metres deep - a death trap for a fully clothed or armoured
man.
Drovers knew of safe routes through the moss and used them to
drive their cattle to market in Stirling and Falkirk. Knowledge
of these routes was passed down from generation to generation.
Today, many of the main Drove Roads still survive as paths and
tracks (where they have not been incorporated in tarred roads),
and are popular with walkers and hikers.
One expert in the lore of the region was the famous Rob Roy MacGregor.
Tales abound of his exploits in and around the small parishes
that fringed the moss.
Sir Walter Scott's novel 'Rob Roy' has many references to the
activities of Rob Roy and the MacGregors in the Fordhead area.
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Cattle were very important to the people of his time and were a measure
of wealth.
The countryside to the south of the moss was fertile and lush with grass
compared to the northern side. These southern lands were used by highland
cattlemen to feed their herds, moving from north to south and back again
through the moss and over the Fords of Frew. This practice was common,
and the southern landowners were paid for the use of their land in this
way. Cattle Rustling was common however, and herds of animals entrusted
to the stewardship of these lowland lairds often caused friction between
the two sides when things went wrong.
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The following account is just one of many events that revolved
around the theft of cattle.
Rob Roy and his men had devised a plan to seize a herd of valuable
cattle that were being driven from Menteith to Stirling. Their
ambush would take place at Buchlyvie, (5 miles from present day
Fordhead). Unfortunately, the locals from Buchlyvie thought they
were the target of the imminent raid and quickly summoned help
from the neighbouring village of Kippen. As the herd approached
Buchlyvie, Rob Roy and his men swooped down from Kippen Muir -
to find a hostile reception from the men of Buchlyvie and Kippen.
After a bloody fight, the MacGregors were victorious and whisked
the cattle away via the Fords.
Later, after assessing the cost of the raid in dead and wounded,
Rob Roy returned to wreak a swift and violent revenge on his opponents,
emptying every byre in Kippen for good measure and driving their
cattle north beyond their reach.
This photograph shows the statue of Rob Roy in Stirling. What
is most striking about the figure is the length of the arms. This
was no mistake on the part of the sculptor as Rob Roy was reputed
to have arms so long that from a standing position, he could tie
the garters at the top of his socks without bending his back!
Whether this feature is accurate or not, he certainly did inspire
awe - and in some cases dread - among the populations of the western
end of the great moss.
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The Fords have played
their part in military action. In
1645, Montrose used the Fords to bring his army south and win the Battle
of Kilsyth. Kilsyth is on the southern side of the hills that run along
the southern edge of the moss. This unexpected (and speedy) deployment took
the defeated army by surprise and won the day.
Scotland saw two Jacobite 'Risings' or rebellions and the Fords were used
for various troop movements in both.
In the first rising of 1715, Rob Roy proposed to the Earl of Mar that he
should lead part of the Jacobite army across the Forth at the Fords of Frew
and get behind and outflank the army of the Duke of Argyle and the Government
forces holding the bridge at Stirling. This manouver may well have altered
the course of Scottish history as Argyle was very weakly supported and was
thought to have been ready to switch sides. Unfortunately for the Jacobites,
'Bobbing John' (as Mar was nicknamed), hesitated as he was ever apt to do,
and did not support the MacGregors. This delay was why the MacGregors were
late for the Battle of Sheriffmuir the next day - a conflict that ended
in complete disaster for the Jacobites.
In the second rising of 1745, Prince Charles (Bonnie Prince Charlie), used
the Ford to march south after Stirling Bridge had been breached against
him by the Government troops.
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Clearing
the Moss 
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The greatest human
impact on the Great Bog came on the 18th and 19th centuries through the
work of 'Agricultural Improvers'.
Henry Home, or Lord Kames, was one such man. When his wife inherited her
brother's Blairdrummond Estate, Kames looked at the Kincardine moss, just
west of Stirling, and saw potential farmland in the clay-rich layers beneath
the peat. The Kincardine moss was just one of the many moss areas that constituted
the great Forth Valley bog.
In the mid 1760's he began to turn his vision into a reality by renting
out 8-acre portions of the bog on long leases. This was the start of a massive
project - greatly expanded after Lord Kames's death by his son, George Home
Drummond - which continued until 1840.
Most of Home Drummonds tenants were families evicted from their lands in
Balquidder and Glen Lyon during the notorious Highland Clearances. These
Gaelic-speaking newcomers were mockingly called 'The Moss Lairds' by local
people. They cut the walls of their homes out of the Moss and topped them
with a roof of timbers and turf. By 1811, some 764 men, women and children,
plus their livestock, were living on the Moss.
Bit by bit, the moss dwellers dug away the deep peat, throwing sods of it
into specially cut channels. Water then washed the peat into the River Forth
which carried it away down stream. All this peat had to end up somewhere
and the Forth Estuary still has a substantial layer at its bottom to this
day. Hundreds of hectares of the Moss were cleared in this fashion, leaving
the rich fertile clays and soils exposed. This cleared land was quickly
put to good use as farmland.
Those who followed Home Drummonds example cleared the bog from thousands
more hectares in the carse of Stirling. The remaining Flanders Moss is where
the clearance stopped.
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Recent
Times 
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There
have been marked changes to the Fordhead area over the last century.
In the late 1800's, there was a thriving Tile Works at Kippen
Station.
The clay from the carse was perfect for making all manner of bricks.
They also made tiles for use in roofing and drainage.
The Tile Works closed in 1895. The actual site was on an area
of land on the north side of the station. This area is largely
untouched to this day and may well have remnants of the tileworks
under the thick covering of vegetation.
A more dramatic sign of its existance is in the large field that
runs from the Station to the Forth. This field (a part of Fordhead)
is where the clay was dug out, and as a consequence is at least
a metre lower than the surrounding area at the station end.
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The railway ran all the way from Stirling to Glasgow via Balloch and was
actually the main Stirling-Glasgow line. The locomotives that operated on
the carse line were steam powered and must have looked impressive as they
made their way through the valley.
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At the height
of its day, the railway provided a vital link for farmers to move
their produce to Stirling and beyond. It also allowed the transport
of freight and was used to deliver fertiliser to Kippen Station
where the local farmers could pick it up by horse and cart.
The trains also catered for passengers and a horse-drawn bus transferred
passengers up and down the hill (known as the Station Brae) from
Kippen Village to the Station.
This is a photograph of Kippen Station around 1920.
With the onset of WW2, the role of the trains changed to the movement
of freight and munitions. A special siding was built into the
near-by electricity sub-station building to protect any trains
and their cargo from air attack. The building was reinforced with
massive amounts of concrete and over the years, the extra weight
has actually pressed the whole structure into the clay by a considerable
amount.
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The Stirling-Glasgow
track cut an almost straight line from Stirling to Kippen and
beyond.
Many roads ran across the line throughout its length.
Although the line was built on a solid base that was usually elevated
above the surrounding area, it was often too low to bridge the
carse roads. The choice was either to raise the track (and bridge
the road) or use a level-crossing. Rivers also posed problems
and the only course of action was to raise the line and bridge
them.
Where crossings were used, they were controlled by a Gatekeeper.
It was his job to man the gates, day and night, giving the right
of way to the trains when they were due. Small two-roomed Gatehouses
were built at each of the crossings for the Gatekeeper and his
family. The picture shows the Gatehouse only half a mile from
Fordhead (now a ruin).
Many Gatehouses (most of them modernised) can be seen from the
A811 as the railway ran parallel to most of the road.
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In 1959 the last train
ran through the carse. The main reason for the demise of the railway was
the increase in road traffic, in particular, the introduction of a bus service
to all the villages throughout the length of the line. Bus routes ran straight
into the heart of each village. This was far more convenient than the added
journey to and from the train stations.
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The increase
in road traffic also affected the rural road systems - especially
the bridges.
This is the old 'Bridge of Frew', a graceful three-arched structure
built with local red sandstone from a quarry near Kippen. It was
completed in 1783. Perfect for horse-drawn traffic, the bridge
was wide enough to allow easy passage for a fully loaded horse
and cart.
In the early 1960's, the bridge was replaced by the present day
one which is wide enough to allow two-way traffic and strong enough
to support the increased weight of haulage vehicles. All that
remains of the old bridge are the approach roads on either side
that terminate where the bridge stonework started.
The photograph was taken downstream of the bridge looking west,
very close to where the Boquhan Burn joins the Forth at the Ford.
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