The Temple of Flora is a Grade I listed building in the Wiltshire local planning authority area, England. First listed on 6 January 1966. A C18 Temple.
The Temple of Flora
- WRENN ID
- kindled-basalt-thunder
- Grade
- I
- Local Planning Authority
- Wiltshire
- Constituency
- South West Wiltshire MP: Dr Andrew Murrison (Con)
- Country
- England
- Date first listed
- 6 January 1966
- Type
- Temple
- Period
- C18
- Address
- The Temple of Flora, Stourton with Gasper
- OS grid reference
- ST 774 340
- Coordinates
- 51.10498, -2.32385
- Source
- Historic England listing
Description
The Temple of Flora is a Grade I listed temple located in Stourton with Gasper, built between 1744 and 1746 by Henry Flitcroft for Henry Hoare. It is constructed of limestone ashlar and stucco, topped with a hipped slate roof. The temple features a tetrastyle Doric portico with an entablature that includes triglyphs and bucrania, as well as a moulded pediment. The central double doors are made up of six fielded panels within a moulded architrave topped by a broken pediment, and there is a Latin inscription from the Aeneid above the door, flanked by large 12-pane sash windows. The side walls are blind and rendered.
Inside, the rectangular space has a semi-circular niche on the back wall that houses a Coade stone copy of the Borghese Vase, created by Daniel Pincot around 1772. Circular niches on the side walls contain marble female busts. The Temple also includes a significant contemporary group of altars and seats, or pulvinaria, which are copies of those found in Montfaucon's Supplement to Antiquity Explained from 1725. The Temple was one of the first features added to the gardens by Henry Hoare, predating the lake, and the mason responsible for its construction was William Privet of Chilmark. The Borghese Vase was originally located in the Venetian Seat but was dismantled in the 1790s by Colt Hoare.
Local climate
The Temple of Flora receives an average of 850 mm of rain a year. This makes it wetter than 58% of listed buildings in the UK. Its exposure to wind-driven rain is greater than that of 62% of listed buildings.
It experiences an average of 35 freeze-thaw cycles a year, more than 60% of listed buildings. Of these, 16 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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- Detailed attributes — period, style, materials, features
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