Willowyard is a Grade B listed building in the North Ayrshire local planning authority area, Scotland. First listed on 2 December 1980.

Willowyard

WRENN ID
iron-transept-grove
Grade
B
Local Planning Authority
North Ayrshire
Constituency
North Ayrshire and Arran MP: Irene Campbell (Lab)
Country
Scotland
Date first listed
2 December 1980
OS grid reference
NS 334 535
Coordinates
55.7467, -4.65451
Source
Historic Environment Scotland listing

Also on this page: flood risk · radon risk · weather exposure · detailed attributes ↓

Description

Willowyard is a former farmhouse dated 1727, with the date carved on the skewputt of the building. It is a substantial 3-bay, 2-storey structure with an attic storey, distinguished by steep crowstepped gables typical of early 18th-century Scottish vernacular architecture. The building is constructed of random yellow sandstone rubble with raised window margins and raised angle margins topped with corniced caps. A moulded eaves course runs beneath the roofline. The roof is covered with grey slates laid in diminishing courses, and the end stacks are of coped ashlar.

The principal (western) elevation features three bays with a later 20th-century piend-roofed porch to the centre right, flanked by single windows on the ground floor and three windows on the first floor. The eastern (rear) elevation also has three bays and includes a later window surround at ground floor level, where a door was subsequently converted to a window on the right side. The north gable contains a blocked opening at ground floor right, with a first-floor window above and a small blocked attic window.

The building originally had timber sash and case windows, now replaced with UPVC. The interior contains no surviving original features.

A large extension to the south and a porch to the west were added at a later date and are architecturally out-of-keeping with the original building. The rubble walls would originally have been harled, with the window and angle margins left exposed as dressed stone. The roof is likely to have been thatched originally.

William Simson is recorded as the owner around the mid-18th century. By the late 18th century, Willowyard was a thriving farmstead. An advertisement in the Edinburgh Advertiser of January 1786 described the property as consisting of approximately 175 English acres of arable land, subdivided into fifteen fields and let to three substantial tenants for £130 per annum. The estate included a good house with garden stocked with fruit trees, a malt mill, and newly erected farm offices. A valuable flag and stone quarry had been opened on the grounds, with believed deposits of coal and limestone. The property encompassed about ten acres of wood with thriving belts of planting surrounding most of the farm, and was offered for sale at £3000.

In the Heritors' Records of 1820–22, Robert Steele is recorded as the owner, with the lands assessed as the 14th most valuable in the parish. By 1839, according to the Statistical Account, Alexander Shedden was the proprietor. The first edition Ordnance Survey map of 1856 shows the house with adjacent U-plan outbuildings and a circular horse-engine house. These structures and the layout of gardens and woods remained visible on early 20th-century maps but no longer survive. Late 20th-century industrial development has encroached significantly, and Willowyard now forms part of Willowyard Industrial Estate.

Despite the loss of interior features and its surrounding context, the building remains an important reminder of a once prosperous estate and is one of Beith's few surviving fine early vernacular buildings of the 18th century.

Local climate

Willowyard sits in one of the wettest parts of the UK, with an average of 1,450 mm of rain a year. This makes it wetter than 98% of listed buildings in the UK. Its exposure to wind-driven rain is greater than that of 97% of listed buildings.

It experiences an average of 27 freeze-thaw cycles a year, fewer than 71% of listed buildings. Of these, 13 follow at least 1 mm of rain in the preceding 48 hours. Average temperatures at this location have risen by 0.2°C per decade since 1991.

Averages for 1991–2020; temperature trend 1991–2025. Figures describe the wider area (a grid cell of roughly 10 km), not the individual site. Contains modified Copernicus Climate Change Service information 2026.

More on this building

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