Smardale Hall and Adjoining Buildings is a Grade II* listed building in the Yorkshire Dales National Park local planning authority area, England. First listed on 6 February 1968. A Medieval Hall.

Smardale Hall and Adjoining Buildings

WRENN ID
solitary-keep-merlin
Grade
II*
Local Planning Authority
Yorkshire Dales National Park
Constituency
Westmorland and Lonsdale MP: Tim Farron (LD)
Country
England
Date first listed
6 February 1968
Type
Hall
Period
Medieval
OS grid reference
NY 739 080
Coordinates
54.46757, -2.40389
Source
Historic England listing

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

Description

Smardale Hall and the adjoining buildings date from the 15th and 16th centuries. The Hall is constructed of coursed rubble and features a tower at each corner, banded just below the top. It has a graduated slate roof with stone chimneys and ball finials on the conical tower roofs. The building is two storeys high and has six bays. Most windows on both side elevations have two, three, or four lights in stucco surrounds, while a two-light window in the apex of the south gable is the only surviving example with a stone mullion. All doors are 19th and 20th century insertions.

Inside, a large segmental arch leads to the kitchen fireplace. An attached range of farm buildings once formed the south range of the Hall's original courtyard plan. These buildings have slobbered rubble walls and a graduated slate roof, and are also two storeys high. Blocked doors and windows can be seen on both side elevations. Internally, the hay loft was once the Great Hall, and some decorative plasterwork remains on the eastern wall. The thickness of the walls suggests that the south-east tower predates the other three, which may have been added for symmetry. A plan from around 1670 indicates a 14th-century tower-house in the east wing, built by the Smerdales (before 1388), while the rest of the house was constructed by the Warcops (before 1580).

Local climate

Smardale Hall and Adjoining Buildings sits in one of the wettest parts of the UK, with an average of 1,230 mm of rain a year. This makes it wetter than 92% of listed buildings in the UK. Its exposure to wind-driven rain is greater than that of 85% of listed buildings.

It experiences an average of 59 freeze-thaw cycles a year, more than 98% of listed buildings. Of these, 37 follow at least 1 mm of rain in the preceding 48 hours. Average temperatures at this location have risen by 0.3°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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