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| Kinder Reservoir | |
|---|---|
| Name | Kinder Reservoir |
| Location | Peak District, Derbyshire, England |
| Coordinates | 53.347°N 1.892°W |
| Type | reservoir |
| Basin countries | United Kingdom |
| Area | 0.18 km² |
| Volume | 1,700,000 m³ |
| Dam length | 410 m |
| Dam height | 24 m |
| Inaugurated | 1912 |
Kinder Reservoir is an upland water body in the Peak District National Park supplying drinking water and regulating flows for downstream communities in Derbyshire and the Greater Manchester area. Located on the western side of Kinder Scout, it forms part of a network of reservoirs and waterworks developed by municipal authorities and private companies in the late 19th and early 20th centuries. The site intersects conservation designations, outdoor recreation routes, and historic transport corridors tied to industrial-era urban expansion.
The reservoir's genesis is tied to the water supply demands of Manchester, Bolton, and Stockport during the Industrial Revolution. Early proposals invoked engineering firms and municipal bodies including the Manchester Corporation and the Waterworks Committee (Manchester). Parliamentary approval followed precedents set by schemes such as the Thirlmere Reservoir and reservoirs serving Leeds. Construction commenced in the Edwardian era, contemporaneous with projects like the Longdendale Chain and the expansion of the Manchester Ship Canal hinterland. The reservoir was completed under the auspices of regional water authorities that later amalgamated into entities such as the North West Water Authority and ultimately successor companies after the Water Act 1973. Wartime and interwar resource constraints affected maintenance schedules similarly to impacts felt at Glen Affric and Loch Katrine. Postwar nationalisation trends and later privatisation influenced operational control alongside environmental legislation including measures inspired by the Rivers (Prevention of Pollution) Act 1951 and subsequent UK statutes.
Situated in the western moorlands of the Peak District, the reservoir occupies a glacially influenced valley below the northern escarpments of Kinder Scout and adjacent to features like Shipley Bridge and the River Kinder headwaters. The catchment drains peat moorlands and gritstone outcrops characteristic of the Dark Peak geology, comparable to hydrological settings at Ladybower Reservoir and the Derwent Reservoir (Derbyshire). Hydrological inputs are driven by orographic rainfall from prevailing westerlies originating over the Irish Sea and the Cumbrian Mountains, affecting runoff regimes similar to those recorded at Mallerstang and Todmorden monitoring stations. Outflow routes connect to the River Kinder and thence to the River Sett and ultimately the River Goyt, integrating the reservoir into the Mersey catchment. Water quality is influenced by moorland peat leachates, atmospheric deposition observed in studies across the Pennines, and land management practices mirrored in Moors for the Future initiatives.
The dam is an earth embankment with a puddle clay core, reflecting construction techniques used in contemporaneous projects such as Rivington Reservoirs and civil works overseen by firms that worked on the Thirlmere Aqueduct. Structural elements include spillways, sluices, and masonry headworks built with local stone comparable to masonry at Torside Reservoir. Engineering surveys addressed permeable substrates and slope stability common to peat-rich moors found at Kinder Scout and Bleaklow. Access tracks and temporary railways used during construction paralleled logistics at remote sites including Howden Reservoir and Derwent Reservoir (Derbyshire). Maintenance regimes have incorporated inspections guided by standards similar to those promulgated by the Institution of Civil Engineers and the Water Industry Act 1991 regulatory environment, with asset management coordinated by regional water companies and trusts.
The reservoir and surrounding moorland support assemblages typical of Dark Peak habitats: heather-dominated heath, peat bogs, and upland grasses that provide habitat for species found in Peak District conservation assessments such as red grouse, curlew, and ring ouzel. Aquatic communities include invertebrates and fish fauna comparable to populations in Ladybower and Fernilee Reservoir, with management interventions to control non-native species reflecting wider policies exemplified by initiatives at River Don catchment sites. The area is affected by habitat fragmentation, acid deposition, and peat erosion issues addressed by partnerships such as Moors for the Future Partnership and conservation bodies like Natural England and the Peak District National Park Authority. Archaeological features and industrial heritage near the site connect to the same landscape narratives that include Derbyshire lead mining and upland trackways catalogued by the Ordnance Survey and heritage organizations like Historic England.
The reservoir lies within popular walking and climbing territory frequented by visitors to Kinder Scout, linked to routes from Hayfield, Glossop, and Ringinglow that form part of long-distance trails related to the Pennine Way and regional footpath networks administered by the Ramblers and local parish councils. Recreation management balances public access with water protection obligations enforced by water companies and overseen in partnership with agencies such as Peak District National Park Authority and Natural England. Activities include hiking, birdwatching, and photography; constraints on boating and angling echo restrictions applied at supply reservoirs across the United Kingdom, including those at Thirlmere and Derwent Reservoir (Derbyshire). Visitor education draws on interpretation from organizations like the National Trust and volunteer groups including local branches of the Royal Society for the Protection of Birds.
Access to the reservoir is via moorland tracks and public rights of way connected to local road networks such as the A6187 and lanes serving Hayfield and Edale. Public transport links include regional bus services operating between Manchester and the High Peak towns, with rail connections at stations on lines serving Glossop and Manchester Piccadilly. Historic packhorse routes and industrial tramways in the vicinity reflect transport histories shared with the Derwent Valley Mills and upland supply chains documented by the Peak District National Park Authority. Visitor parking and signage are managed in coordination with district councils like High Peak Borough Council and parish authorities to mitigate erosion and congestion in sensitive upland corridors.
Category:Reservoirs in Derbyshire Category:Reservoirs in the Peak District Category:Water supply reservoirs in England