Temple of Fame on Cliff Top at South Side of Moon Pond is a Grade II listed building in the North Yorkshire local planning authority area, England. First listed on 6 March 1967. A C18 Temple.
Temple of Fame on Cliff Top at South Side of Moon Pond
- WRENN ID
- carved-lancet-wax
- Grade
- II
- Local Planning Authority
- North Yorkshire
- Constituency
- Skipton and Ripon MP: Sir Julian Smith (Con)
- Country
- England
- Date first listed
- 6 March 1967
- Type
- Temple
- Address
- Temple of Fame on Cliff Top at South Side of Moon Pond, Lindrick with Studley Royal and Fountains
- OS grid reference
- SE 281 686
- Coordinates
- 54.11305, -1.57137
- Source
- Historic England listing
Description
The Temple of Fame is a rotunda located on a cliff top at the south side of Moon Pond, built in 1729 by Thomas Buck and Robert Doe for John Aislabie. It was moved from its original site and rebuilt, likely between 1780 and 1781, by William Aislabie, and has undergone restorations in the 19th century and late 20th century. The structure features a gritstone podium and pillar bases, wooden pillars, and a lead-covered dome. Access to the platform, which is approximately 4 meters in diameter, is via three steps with slabs laid in radiating circles. The rotunda is supported by eight Roman Doric columns, and the fluted entablature includes paterae and a modillioned cornice, topped with a parapet and dome. Originally, the rotunda had Ionic columns and was situated near the Banqueting House, but it has since been relocated to provide a viewpoint towards that structure across the Moon Pond. During restorations, three different styles of capital were discovered, and two stone column drums now stand at the gateway to Fountains Hall. The design from 1781, which influenced the 1970 restoration, may have been created by Robert Adam, who worked for William Aislabie at his properties in Grosvenor Square and Hendon.
Local climate
Temple of Fame on Cliff Top at South Side of Moon Pond receives an average of 860 mm of rain a year. This makes it wetter than 62% of listed buildings in the UK. Its exposure to wind-driven rain is lower than that of 59% of listed buildings.
It experiences an average of 46 freeze-thaw cycles a year, more than 87% of listed buildings. Of these, 25 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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- Flood risk assessment
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