Saddleworth Moor
From Wikipedia, the free encyclopedia
| Saddleworth Moor | |
|---|---|
Saddleworth Moor towards Dovestone Reservoir | |
| Highest point | |
| Coordinates | 53°32′36″N 1°57′21″W / 53.54333°N 1.95583°W |
| Geography | |
Location of Saddleworth Moor in Greater Manchester | |
| Location | Northern England |
| Parent range | Peak District |
| Geology | |
| Mountain type | Moorland |
| Climbing | |
| Easiest route | Pennine Way |
Saddleworth Moor is a moorland in North West England. Reaching more than 1,312 feet (400 m) above sea level, it is in the Dark Peak area of the Peak District National Park. It is crossed by the A635 road and the Pennine Way passes to its eastern side.[1][2]
Vegetation
The moor takes its name from the parish of Saddleworth to the west, historically in the West Riding of Yorkshire, although it is on the western side of the Pennines and so has been administrated by Oldham and part of Greater Manchester since 1974. The moor, an elevated plateau with gritstone escarpments or edges and, around its margins, deeply incised v-shaped valleys or cloughs[a] with fast-flowing streams, straddles the metropolitan boroughs of Oldham in Greater Manchester and Kirklees in West Yorkshire. Moorland east of the county boundary with West Yorkshire is known as Wessenden Moor and Wessenden Head Moor. The moor is crossed by the A635 between the Greater Manchester and West Yorkshire Urban Areas. The A635 is known locally as the Isle of Skye road, taking the name from a former public house at Wessenden Head, Upperthong that was demolished after a fire.[4][5] The Pennine Way arrives from the Wessenden Valley to the north and crosses the moor on its ascent to Black Hill on Holme Moss to the south. The high moorland is sparsely inhabited. Scattered farmsteads, built of gritstone, and fields demarcated by dry stone walls are on the lower land and in the valleys where there is some coniferous woodland. The overlying peat is cut by drainage channels or groughs. Much of the area is open access land.[2]
Blanket bog covers much of the moor. Cottongrass is the most dominant feature but sphagnum mosses are scarce. Heather, crowberry, bilberry and the rare cloudberry are also found. The peat formation is 9,000 years old but extensive areas contain bare peat from which the surface has eroded.[6]
Reservoirs
Dovestone, Yeoman Hey, Greenfield and Chew Reservoirs east of Oldham, are accessed from the A635 road. They supply water to the surrounding area. The valley is surrounded by rocky outcrops and moorland. Spruce and pine plantations are found in the valley and broad-leaved trees have been introduced to provide a more diverse habitat.[7]
Yeoman Hey was built in 1880 and Chew Reservoir in 1914, and when built, was the highest reservoir in the British Isles at 1,601 feet (488 m) above sea level. The bed of a tramway, built to aid its construction, remains visible. The area around the reservoir is used for recreation.[7]

