Click here to move to this Topic
Click here to move to this Topic
Click here to move to this Topic
Click here to move to this Topic
Click here to move to this Topic
Click here to move to this Topic
Click here to move to this Topic
Click here to move to this Topic

Fordhead Farm Click here to return to the Top of the Page

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.

After the Ice Age Click here to return to the Top of the Page
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.
The Flanders Moss Click here to return to the Top of the Page

Arial view
of
Flanders Moss

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'

The Early Inhabitants Click here to return to the Top of the Page

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.

The Fords of Frew Click here to return to the Top of the Page

'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.


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.

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.

Historical Crossings Click here to return to the Top of the Page

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.

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.

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.

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.

Clearing the Moss Click here to return to the Top of the Page
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.
Recent Times Click here to return to the Top of the Page

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.


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.

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.


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.

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.

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.