Walk 22 The Three Reservoirs and Turton Tower
Walk 23 Longworth Clough and Turton Heights
Walk 24 Cheetham Close
RAMSBOTTOM, HODDLESDEN AND HASLINGDEN GRANE
Walk 25 Calf Hey and Ogden Reservoirs
Walk 26 Haslingden Grane
Walk 27 Jumbles and Two Brooks Valley
Walk 28 Holcombe Moor and Peel Monument
Walk 29 Around Alden Brook
Walk 30 Irwell Valley
APPENDIX 1 Route Summary Table
APPENDIX 2 Further Reading
Above Anglezarke Reservoir (Walk 9)
INTRODUCTION
The West Pennine Moors, located between the towns of Chorley, Bolton, Horwich, Ramsbottom, Haslingden, Oswaldtwistle and Darwen, comprise 233km2 (90 square miles) of moorland and reservoir scenery. The area has been a place of recreation for many generations of Lancashire folk; indeed, long before the much-vaunted mass trespass on Kinder Scout, there were organised trespasses in the late 1800s (small and large: around 10,000 people in 1896) and court proceedings on both Winter Hill and Darwen Moor in an attempt to keep rights of way across the moors open. The West Pennine Moors were very much in the vanguard of the campaign for access to our countryside, not that you’ll find many so-called authoritative texts on the matter admitting as much. But the facts speak for themselves; it happened here first.
Dissected by wooded cloughs and characterised by skyline features like Rivington Pike, the Peel Monument on Holcombe Moor and Jubilee Tower (also known as Darwen Tower) on Darwen Moor, the moors are a highly valued and much-appreciated region for recreation and study. Almost the entire area is water catchment, and the successor to the North West Water Authority, United Utilities, owns around 40 per cent of the land, and operates four information centres – at Rivington, Jumbles Country Park, Roddlesworth and Clough Head, Haslingden Grane, which also offer refreshment facilities.
Darwen Tower (Walk 14)
The summit of Cheetham Close (Walk 24)
For the walker, the area has much to offer. This is gritstone country, and the landscape is often dark and sombre as a result. And there is a clue in its use as a water catchment area; in all but the driest of climatic periods, it is wet, boggy and invariably muddy. This might lead you to suppose that it is unappetising, unappealing and unattractive. But nothing could be further from the truth. This is a beautiful, semi-primeval landscape, a moorland theatre of considerable appeal and attraction, and a superb canvas for interests in flora, fauna, biology – even the modern leisure pursuit of geocaching. Come here at any time of year, and you will find others doing the same. The West Pennine Moors are a rich and varied playground for the walker, giving pleasure throughout the year.
Geography and Natural History
Rising to a peak on Winter Hill (456m/1496ft), the area is predominantly upland, with myriad well- trodden paths and areas of historical and geological significance. Although a large area of moorland became freely accessible under the right-to-roam legislation introduced by the Countryside and Rights of Way Act (2000) much of the terrain is marshy and difficult walking, and the footpaths – of which there are a great many – generally remain the most convenient means of access.
The moorland occurs in fairly well-defined blocks – at Withnell, Anglezarke and Rivington Moors; Darwen and Turton Moors; and Oswaldtwistle and Holcombe Moors, where the prevalent land use is sheep farming. Unlike other areas of moorland in the north of England, the West Pennine Moors are not managed for grouse shooting (not for want of trying), and are characterised by rough grassland and peat bog. This is one of the reasons why the moors never suffered the same degree of ‘access aggravation’ that occurred further south, in the Peak District.
Providing useful habitat areas for wildlife, the West Pennine Moors are bisected by a number of wooded valleys and cloughs, the largest being the Roddlesworth valley, near Tockholes. Although there are some small coniferous plantations, particularly around the reservoirs, the woodland cover overall is nominal, and it is a fine sense of openness that dominates here, and this, coupled with the intricate network of footpaths, makes the area an ideal place to begin a lifetime of recreational walking and to practice the necessary skills of map reading and navigation.
The main valleys are consumed by large reservoirs constructed in the mid- to late 19th century to supply water for Lancashire’s urban population. Evidence of this Victorian landscape is found in the form of mixed woodlands, styles of architecture and dressed stone walls. Along the valleys, the landscape is characterised by farmland pasture and meadows enclosed by drystone walls, built from the sombre gritstone that pervades great parts of the moorland area. Species-rich grassland is restricted in both area and distribution, mostly to steeper valleys or cloughs.
Approaching White Coppice (Walk 6)
It’s worth keeping your eyes open in the woodlands…
The valleys are very rural in character, with large areas of grazing land and broadleaved woodland and plantations, notably around Roddlesworth and the Turton and Entwistle reservoirs, which enable them to absorb high numbers of recreational visitors without feeling overcrowded. It is a curious paradox: you may always be able to see someone, or a farm or villages, but yet feel very isolated up on the moors. Although native broadleaved woodland is a habitat restricted almost entirely to valleys, there are fine examples of oak woodland, ash woodland, and wet woodland dominated by alder or willow, such as at Longworth Clough SSSI.
Plantlife
The West Pennine Moors area is recognised as a Core Biodiversity Resource at both regional and sub-regional levels, supporting a range of UK Priority Habitats and Species. The moors and farmland that surround and meld with the West Pennine Moors have a high level of biodiversity. Where the moors are unenclosed, there are widespread areas of blanket bog on deep peat soils.
Repeatedly modified by grazing, burning and attempts at drainage, the moors are in places dominated by purple moor-grass, along with distinctive species such as cotton-grass, heather, cross-leaved heath, cranberry and numerous species of sphagnum moss, as well as less prevalent plants like bog rosemary. Elsewhere there are rolling areas of upland heath, acidic grassland and upland flushes.
The extensive hill peat is of considerable importance for preserved plant and animal remains, and as a means of providing information about past climates and weather patterns. Most importantly, it
