Old Park Stables is a Grade II listed building in the Forest of Dean local planning authority area, England. First listed on 7 August 1954. Stables.

Old Park Stables

WRENN ID
deep-keep-dew
Grade
II
Local Planning Authority
Forest of Dean
Constituency
Forest of Dean MP: Matt Bishop (Lab)
Country
England
Date first listed
7 August 1954
Type
Stables
Address
Old Park Stables, Lydney
OS grid reference
SO 621 021
Coordinates
51.71701, -2.54891
Source
Historic England listing

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

Description

Old Park Stables is a building that served as stables and grooms' accommodation, dating from the early 18th century. It is constructed of sandstone rubble and features stone slate roofs. The structure consists of a central block with two hipped ends that slope into a central pedimented section of the roof, which is topped by a square wooden bell turret with a lead cupola. This central block is flanked by low wings on either side. The steep pediment has a dentilled cornice, and the modillion cornice returns to the ridge of the lower wings.

The central block displays a clock in the pediment above a two-storey front with three windows. It has two-light 19th-century casements with wooden lintels above two multi-paned pseudo-sashes. The entrance features a central six-panel fielded door within a moulded surround and pediment. Inside, there are remains of three stalls. The single-storey wings are designed differently; the left wing has two windows, a door, and one window with multi-panes, while the right wing is rendered and includes a small single casement and three segmental-headed garage doors. This building is the major remnant of the former Manor house, which has since been rebuilt further up the hill at Lydney Park.

Local climate

Old Park Stables receives an average of 800 mm of rain a year. This makes it drier than 55% of listed buildings in the UK. Its exposure to wind-driven rain is greater than that of 52% of listed buildings.

It experiences an average of 36 freeze-thaw cycles a year, more than 64% of listed buildings. Of these, 15 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.

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  8. Cross Inn Grade II 572 m
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