River Manifold

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Manifold valley (from Thors Cave).jpg
Manifold Valley from Thor's Cave
Physical characteristics
 • locationSouth of Buxton near Axe Edge
 • location
Confluence with the Dove
 • coordinates
53°3′0″N 1°47′5″W / 53.05000°N 1.78472°W / 53.05000; -1.78472Coordinates: 53°3′0″N 1°47′5″W / 53.05000°N 1.78472°W / 53.05000; -1.78472
Length12 miles (19 km)
Basin size9,111 hectares (22,510 acres)[1]
Basin features
ProgressionDoveTrentHumberNorth Sea
 • rightOakenclough Brook, Warslow Brook, Hoo Brook, River Hamps
A bridge over a dry River Manifold, near Grindon

The River Manifold is a river in Staffordshire, England. It is a tributary of the River Dove (which also flows through the Peak District, forming the boundary between Derbyshire and Staffordshire).

The Manifold rises at Flash Head[2] just south of Buxton near Axe Edge,[3] at the northern edge of the White Peak, known for its limestone beds. It continues for 12 miles (19 km)[4] before it joins the Dove. For part of its course, it runs underground (except when in spate), from Wetton Mill to Ilam.[2] During this section it is joined by its major tributary, the River Hamps.

Villages on the river include Longnor, Hulme End and Ilam.

Its name may come from Anglo-Saxon manig-fald = "many folds", referring to its meanders.

Manifold Way[edit]

The Manifold Way is an 8-mile (13 km) long-distance footpath from Hulme End to Waterhouses, along the former route of the narrow-gauge (2' 6") Leek and Manifold Valley Light Railway which operated between 1904 and 1934.[5] Opened in July 1937 after the LMS handed over the trackbed to Staffordshire County Council, it is tarmacked throughout.

The Manifold Valley Visitor Centre is housed in Hulme End Station, which also has a model of the railway.[6]

Limestone crags and caves[edit]

[citations needed]The limestone cliffs that fringe the valley contain several rock-climbing areas, and named rock features, including Thor's Cave (grid reference SK098549) and Beeston Tor (grid reference SK105540), which overlooks the confluence with the River Hamps.

Mining in the Manifold valley[edit]

The Manifold valley was famous for the mining of copper and lead, and the mines at Ecton were some of the richest in the country. The discovery of Stone Age implements in some of the caves imply that minerals were mined around the Manifold valley thousands of years ago. Nowadays there is little trace of the industry that made many people (mainly the Duke of Devonshire who at one time owned the Ecton mines) very rich.[3] The main areas of interest are around Ecton where the old spoil banks and the old engine house still remain.


The river has been noted as being important for European bullhead and lamprey. In the underground section of the river where it resurfaces at Ilam, the bullhead have no pigmentation. It was previously a stronghold for white-clawed crayfish, but most of the river's population were wiped out by crayfish plague in 2008.[7] Crayfish have been noted in the tributaries of the Manifold and it is hoped that re-colonisation can be achieved by the surviving upstream crayfish.

See also[edit]


  1. ^ "Manifold - Source to conf R Dove". Environment Agency. Retrieved 1 August 2016.
  2. ^ a b Jacklin, Tim (June 2008). "Advisory visit to the River Manifold, Derbyshire" (PDF). The Wild Trout Trust. p. 2. Retrieved 31 July 2016.
  3. ^ a b "River Manifold". Peak District online. Retrieved 31 July 2016.
  4. ^ Bridgland, David; Howard, Andy; White, Mark; White, Tom (2014). "6 Synthesis: the Pleistocene evolution and human occupation of the Trent catchment". Quaternary of the Trent. Oxford: Oxbow Books. p. 362. ISBN 978-1-78297-026-2.
  5. ^ "River Manifold". Peak District Information. Retrieved 31 July 2016.
  6. ^ "The Manifold Valley & Manifold Trail". Hulmeend.co.uk. Retrieved 31 July 2016.
  7. ^ "Rare crayfish wiped out in River Manifold". Stoke Sentinel. 4 August 2008. Retrieved 31 July 2016.

External links[edit]