Gladhouse Reservoir is a Grade B listed building in the Midlothian local planning authority area, Scotland. First listed on 18 November 1998. Reservoir. 1 related planning application.
Gladhouse Reservoir
- WRENN ID
- unlit-outpost-wind
- Grade
- B
- Local Planning Authority
- Midlothian
- Constituency
- Midlothian MP: Kirsty McNeill (Lab)
- Country
- Scotland
- Date first listed
- 18 November 1998
- Type
- Reservoir
- OS grid reference
- NT 300 535
- Coordinates
- 55.77017, -3.11665
- Source
- Historic Environment Scotland listing
Description
Gladhouse Reservoir was built in 1879 by James and Alexander Leslie to supply water to Edinburgh, Leith, Portobello, and Dalkeith.
The dam features squared and snecked pink sandstone with a slightly battered retaining wall topped with semi-circular coping. To the south of the dam, there is a platform with an ironwork whipple gangway leading to an ashlar upstand shaft. A curved weir is located to the east of the dam, crossed by a plate girder bridge, while a pier and slipway are situated to the west. There is also a sharply curved weir at the foot of the embankment to the north.
Adjacent to the weir at the foot of the embankment is the measuring house, which is a single-storey structure with stugged walls and droved dressings. It has raised margins and strip quoins. The east elevation has three bays, with a central doorway featuring a simple pediment and a boarded timber door, flanked by windows. The north elevation has a central opening with a boarded timber shutter and a louvred bull's eye opening in the gable head. The west elevation has three bays with regular fenestration, while the south elevation features a central window and a louvred bull's eye opening in the gable head. The building has three-pane lying pane windows, a grey slate roof with a lead ridge, coped stone skew, and cast iron rainwater goods. The interior was not seen in 1998.
The Tweedaleburn Aqueduct emerges from a tall semi-circular arched opening to the southwest of the reservoir. It is constructed of coursed bull-faced pink sandstone with a stugged rusticated arch ring and keystone, and features stugged bull-faced coping. The aqueduct has a coursed, steep-sided channel that enters the reservoir on the west side and passes under a flat segmental arched bull-faced bridge with stugged rusticated coping and arch ring, and slightly splayed wing walls.
Additionally, there is a small round-arched bridge over Crosslee Burn, made of bull-faced sandstone on the outer walls, squared and snecked below the parapet, and stugged on the inner walls. It has semi-circular stugged coping and splayed wing walls.
Local climate
Gladhouse Reservoir sits in a wetter-than-average part of the UK, with an average of 980 mm of rain a year. This makes it wetter than 78% of listed buildings in the UK. Its exposure to wind-driven rain is lower than that of 53% of listed buildings.
It experiences an average of 55 freeze-thaw cycles a year, more than 95% of listed buildings. Of these, 34 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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- No EPC on record for this property
- No sale records on file
- Related listed building consents — 1 application
- Detailed attributes — period, style, materials, features
- Flood risk assessment
- Radon risk assessment
- Weather exposure and heating demand — rain and frost month by month and year by year, wind direction, solar and humidity
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