I was going to post this on my textile blog wroot.blog but on reflection it’s as much about walking as textiles, and I’m certain there will be more non-textile history to write about as we explore the history of this area.
After 5 years in western Canada, where there are few if any rights of way across the landscape and landscape history is much more obscure, we’ve been walking the UK footpath network with enthusiasm and appreciation of its value. Last Saturday we continued our exploration of the landscape around three reservoirs (Swinsty, Fewston and Thruscross) constructed by damming the River Washburn in Nidderdale. Follow the A59 west from Harrogate (we drove it, you can Google Satellite it) to Blubberhouses (nothing to do with fat: the name may be derived from Anglo-Saxon bluberhūs ‘the house/s by the bubbling stream’, the stream being the River Washburn), or from the iron-smelting furnaces known as blowers or blauers known to have worked nearby in the 13th century. This Google Maps link https://goo.gl/maps/3pCcwHKpdroy7Ypj7 should show you the reservoir and access roads; zoom in for more detail.
Yorkshire Water now manages the water supply and the reservoirs and has created several car parks to serve the exceedingly popular footpaths around the reservoirs. We turned north at Blubberhouses for the Thruscross Reservoir car park, then walked widdershins around the reservoir. Cross the dam, up the hill (mind the traffic) and follow the path. It’s clearly visible on the north shore of the main reservoir, dives up onto the moor and fields around the northern arm, then back into the woods to emerge as the white track on the north shore of the western arm. This story starts where a footpath crosses Capelshaw Beck (now a small stream) below the road bridge. We looked west from the footpath bridge and saw a cascade of water running down a manmade structure.
The path ran uphill and continued east along a bank that clearly defined … something. The line of an old road, worn into the hill? Didn’t feel right. Ditch to prevent water from the uphill field flowing down into … something? No. Too much work for too little gain.
We walked on, amicably arguing explanations based on vague knowledge that there’s a village somewhere under the reservoir (there are villages under many of the reservoirs here). Then, through the trees, there was a structure by the shore.
The remains of two walls are visible from the path. I’ve produced information boards for things that look like this: there would have been a water-driven mill wheel between those walls.
I ran forward to check (see the next photo) and yes, an arch for the drive wheel and opening for the axle can be seen on the other side of the wall. A quick look back and up: that hollow way contoured along on the hillside above the mill, so it probably was the leat bringing water from a millpond… that cascade is flowing down the dam holding water back to (once upon a time) fill the leat and drive the overshot (water flowing down onto it) wheel.
SO EXCITING. The wheel under that arch would have been toothed to drive machinery that did things, processed stuff. What sort of mill was it? When was it demolished, when was the reservoir built. So many questions, no phone signal, SO FRUSTRATING.
Fortunately there was phone signal before I exploded from frustration.
This was once Little Mill, one of several flax mills associated with West End, once a village just south of the reservoir in what is now Thruscross Parish.
I’ve overlain an excerpt of the 1854 (surveyed in 1848) Ordnance Survey map
https://maps.nls.uk/view/102344725
on a Google satellite image of the reservoir (If you click on the image below WordPress should show you a larger version to see the detail). Little Mill is marked in red, one of four mills on Capelshaw Beck as this stream was known. High Mill is out of view to the left/west; below Little Mill is Patrick’s Mill and then Low Mill, both marked orange. The village of West End was a dispersed settlement, with most houses scattered south of the mills; there was a village school, a Wesleyan chapel higher on the hill while Holy Trinity Church and the Butchers Arms Public House stood together near the post office, across the beck from Patrick’s Mill and just above the point where Capelshaw Beck flowed into the River Washburn.
The rise and fall of West End Village
Archaeological surveys of the south-facing slope of the Washburn Valley around Thruscross (north of the reservoir) have found the remains of prehistoric settlements, field systems and possible burials dating from the Neolithic to Bronze Ages (c. 4000 BCE to 700 BCE. ‘BCE’ means ‘Before Common/Christian Era’). The name ‘Thruscross’ is thought to derive from Anglo-Scandinavian personal names, indicating that the settlement was recognised some time after AD1000, with the first text record dating from AD1142.
For centuries West End and its near neighbours were largely agricultural villages eating what they produced and selling any surplus for money to buy luxuries and pay tax. Wool from local sheep would have been spun by local women — and men, too, if times were hard. Some yarn went to local weavers to become cloth, and some would have been sold to travelling wool factors who eventually sold it on to the owners of ‘factories’ combining handlooms and finishing mills that wove and finished cloth even before the industrial revolution.
Sidebar: What did flax mills do?
The fibres that become linen are found in the stems of flax grown for fibre (different, shorter, varieties are grown for seed and oil). At the end of the growing season the flax plants are pulled up, dried, rippled to remove the seeds, retted in damp or wet conditions to break down the pectins that hold the fibres in the stems, dried, then scutched to remove waste material, hackled to separate the prized long line flax fibres from shorter waste tow, then spun into yarn and woven into the cloth known as linen.
The rise of the linen industry
Flax and linen processing became increasingly important in Yorkshire in the 1700s as the British government passed laws to support the industry and keep money spent on linen fabric in the UK instead of sending it abroad. Some flax was grown locally, especially in the Vale of York but it’s a difficult crop requiring fertile damp soil and skilled processing to produce the best quality fibre. Eastern Yorkshire had the climate and soil “At one time the flax grown in the East of Yorkshire was of as good quality as that grown in Belgium” (The Linen trade, ancient and modern, 1864) but the costs of processing the flax meant that by the 1700s most mills processed scutched flax imported from Russia and Holland. The American War of Independence (1775–1783) created huge demand for linen on both sides of the Atlantic, spurring a race to expand the flax industry in Yorkshire and elsewhere (although wool and worsted spinning remained the most important industry).
In 1797 the first West House flax mill was built on the River Washburn downstream of what is now Thruscross Reservoir. By 1854 the Ordnance Survey recorded four flax mills on Capelshaw Beck, each with a mill pond holding back the water needed to power that mill and then ran downstream in the Beck to power the next mill downstream. If you look closely at the 1854 map below you’ll see the mill leat supplying Little Mill (the mill we found) was covered, running under the road from the end of the mill pond to the mill. That hollow we found was the (empty) Mill Pond.
The water supplies for High Mill and Little Mill are clear in a LIDAR image. Harry’s Dam still holds water, but the flat areas marking the site of High Mill is obscured by scrub and trees on the ground. Capelshaw Beck is the meandering grey line incised into the valley; I’ve only added blue to show how water could move from one mill to the next.
These mills probably processed and spun linen yarn to be woven elsewhere, perhaps at West House Mill, which had added a weaving factory and bleaching yards in 1807.
The decline of the linen industry on the Washburn
Census returns for Thruscross, the settlement north of the reservoir, record the changing prosperity of the area. In 1801 Thruscross had a population of 467; 611 in 1837, 339 in 1851 of whom half worked in ‘industry’ (the mills) rather than agriculture. By 1871 the population was 301 of whom only 16 worked in the mills, and by 1891 there were 30 unoccupied houses and none of the 219 inhabitants worked in industry.
These small remote mills could not compete with the new, larger and more efficient mills in Nidderdale, especially those in Leeds itself, and further west: it was simply too costly to move the goods to and from Upper Washburndale. Worse, the demand for linen was declining. Linen had been the affordable fabric for ‘ordinary’ people until cotton arrived, first as calicoes and other prints from India and then as cotton fibre to be spun and woven in British mills. It was softer, whiter, cheaper, and took vivid printed colour more easily than linen.
Small flax mills closed. Larger mills struggled longer, sometimes moving to different fibres; West House Mill closed in 1844 to reopen as a silk mill in 1858. That venture failed, with the mill closing permanently in 1864.
Leeds needs more water
As the city of Leeds grew larger, fueled by the success of its industry (including mills) its need for water also grew. In 1871 the Leeds Waterworks Company began construction of Swinsty Reservoir, the lowest of the three reservoirs on the Washburn. Swinsty was completed in 1878; work on Fewston Reservoir, above Swinsty, began in 1874 and was completed in 1879. West House Mill was demolished as part of the Fewston works, with its stone incorporated into the wall around the reservoir.
In 1900 Leeds Corporation began to buy land in the expectation it would need a third reservoir, now Thruscross. Low Mill (see the overlay image) was purchased and demolished c. 1911. Thruscross Reservoir was eventually completed in 1966; in the late 1980s these and all the other water infrastructure of Yorkshire became the responsibility of Yorkshire Water. Much of the best farmland of the Upper Washburn and Capelshaw Beck now lies under the waters of Thruscross; Yorkshire Water refurbished the farmhouses on the slopes around the reservoir using stone from demolished buildings, then sold them to private owners most of whom work elsewhere.
Now I have to go back and view that landscape again in the light of what I’ve learned.