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Burbage Info Sheet.pdf

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13/10/2009 Peak District National Park: Study Area<br />

Geology<br />

Prehistoric Settlement<br />

Carl Wark<br />

The landscape in the burbage valley<br />

Routeways<br />

Land Use In The Valley<br />

Land Use Today<br />

Map of the <strong>Burbage</strong> Valley area<br />

The <strong>Burbage</strong> Valley lies in the eastern side of the Peak District National Park. It is close to Fox House Inn on<br />

the A625 road from Chapel-en-le-Frith to Sheffield and is approximately 3 miles east of Hathersage and 8<br />

miles west of the centre of Sheffield.<br />

As it is so near to Sheffield, the <strong>Burbage</strong> Valley is very popular both for recreation - walking, climbing,<br />

picnicking - and for school field trips. Parking is available at Upper <strong>Burbage</strong> Bridge and there is invalid parking<br />

at the southern end of the valley. Further parking is available at the Surprise car park by Millstone Edge,<br />

which can also accommodate buses and coaches.<br />

Geology<br />

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13/10/2009 Peak District National Park: Study Area<br />

The <strong>Burbage</strong> Valley is a basin partly surrounded by scarps or edges of gritstone: <strong>Burbage</strong> Rocks on the east<br />

and Higger Tor and Carl Wark on the west. The gritstone is resistant to erosion.<br />

The shale valley basin is partly filled with an overlying deposit known as head. This is a deposit which is a<br />

mixture of sands and clay and it is thought to have been brought by ice sheets during the Ice-Age.<br />

East of <strong>Burbage</strong> Rocks is <strong>Burbage</strong> Moor, an extensive plateau partly covered by peat. This consists of<br />

partially decomposed vegetation which accumulated in water-logged conditions during periods when the<br />

climate was cool and wet.<br />

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Prehistoric Settlement<br />

The first evidence of human activity comes from flints left behind by groups of hunter-gatherers who travelled<br />

through the area. Early evidence of occupation occurs south of Carl Wark and dates from the Bronze Age<br />

(circa 1500 BC). It is marked by small clearance cairns formed out of stones cleared from the area by the<br />

early farmers. These cairns are now covered by vegetation which makes them difficult to find.<br />

Carl Wark<br />

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Carl Wark<br />

The defended promontory fort of Carl Wark, which is a Scheduled Ancient Monument, probably dates from the<br />

Iron Age. It may have been used as a refuge when the local inhabitants were under threat. The earthen<br />

rampart and stone wall, built to defend the one acre site, can still be seen on the western side of the fort.<br />

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The landscape in the burbage valley<br />

<strong>Burbage</strong> Brook<br />

The <strong>Burbage</strong> Brook rises in the moorland north of the <strong>Burbage</strong> Valley and enters the valley under the Upper<br />

<strong>Burbage</strong> Bridge. From here the height of the stream quickly drops from just over 396m down to 335m in less<br />

than 1 km. The Brook therefore provides a good area for hydrological work. Hypotheses showing the different<br />

water velocities along the Brook and the differences in the size of contents of the stream bed, can easily be<br />

tested.<br />

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13/10/2009 Peak District National Park: Study Area<br />

Aerial view of Millstone Edge<br />

Forest Areas<br />

The 83 acre plantation was planted between 1968 and 1971. The trees are mainly Scots Pine, Japanese<br />

Larch and Lodgepole Pine. Some deciduous species were planted around the edges of the plantation to<br />

soften its outline.<br />

Bird species which are regularly seen in the plantation are jays, rooks and chaffinches.<br />

Ecology<br />

The Dark Peak moorland, such as that on <strong>Burbage</strong> Moor, is the nearest thing to wilderness in England. The<br />

moorland and blanket bog terrain found here are rare and valuable habitats which support a unique fauna.<br />

<strong>Burbage</strong> Moor lies around 400 metres above sea level and experiences low temperatures, high rainfall, is<br />

exposed and windy. Plants and animals need to be hardy and highly adapted to live on the moorland,<br />

because of the extreme climate and acid soils. High rainfall carries the few minerals downwards where many<br />

plants cannot reach them.<br />

Heather, cowberry, bilberry and moorland grasses, are found on the gritstone areas. The shale and head<br />

deposits in the valley are more fertile, enabling more vigorous grasses and bracken to grow. Because of the<br />

lack of competition from other plants, bracken has started to dominate the vegetation in these areas. Efforts<br />

have been made to limit this domination by cutting back and controlling the bracken.<br />

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13/10/2009 Peak District National Park: Study Area<br />

Moorland birds like wheatears and meadow pipits can be seen during spring to autumn. Skylarks can also be<br />

heard in spring. The elusive mountain hare and the red grouse are able to survive all winter on the moors.<br />

<strong>Burbage</strong> Brook is home to dippers and grey wagtails throughout the year<br />

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Routeways<br />

Packhorse Routes<br />

Routeways through the <strong>Burbage</strong> area may have been in existence for thousands of years. However, the hollow<br />

ways and the pack horse bridge, which can be seen below Carl Wark, are mostly from the Medieval Period.<br />

One pack horse route crossed Millstone Edge and forded the <strong>Burbage</strong> Brook to the south of the more recent<br />

A625.<br />

The pack horse trains could consist of up to 50 horses all carrying goods through the landscape.<br />

Turnpike Roads<br />

The roads which now surround <strong>Burbage</strong> Moor were first built as turnpike roads, though many of the routes<br />

may have followed existing trackways. The owners of these roads were able to charge a toll to people using<br />

the route. This funding enabled the roads to be maintained to a higher standard than the normal roads and<br />

therefore movement of goods and people along them was quicker.<br />

The Houndkirk road was built in 1758 and was never surfaced with modern materials. It is therefore an exellent<br />

example of a turnpike road. Another road built at this time crosses over the Upper <strong>Burbage</strong> Bridge and<br />

continues into Ringinglow. Part of the main A625 road, which crosses the bottom of the valley area was built<br />

in 1781.<br />

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Land Use In The Valley<br />

Quarrying and the Millstone Industry<br />

Quarrying in the <strong>Burbage</strong> area probably started over 2000 years ago when millstone grit was used to make<br />

rotary querns. These were the hand-held equivalents of the later millstones.<br />

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13/10/2009 Peak District National Park: Study Area<br />

Millstones<br />

During the 18th and 19th centuries Wild Moorstones Edge Quarry manufactured millstones, grindstones (for<br />

the Sheffield edge-tool industry) and other stone products. The sizes and shapes of the millstones varied<br />

through time. The earlier were dome-shaped on top whilst the later ones were flat on both sides. The average<br />

size was approximately 5 feet in diameter and over a ton in weight.<br />

The millstones were made at the quarry site and transported all over Britain and even abroad. Discarded<br />

millstones can still be seen at the quarry sites in the <strong>Burbage</strong> Valley and also at other quarries in the Peak<br />

District.<br />

Land Ownership<br />

Since 1928 the <strong>Burbage</strong> Valley has been owned by Sheffield City Council, who bought it from the Duke of<br />

Rutland, with the idea of building a reservoir in the area. Due to local opposition to this proposed reservoir, the<br />

project was cancelled but Sheffield Council continued to manage the land, which is now tenanted out to a<br />

local sheep farmer.<br />

The rights to use the valley for grouse shooting and other sporting activities were leased out by the council<br />

until 1936. This limited public access to the land. After 1936 new paths were gradually opened up and public<br />

access was extended in to the valley. A new access agreement has recently been completed.<br />

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Land Use Today<br />

Farming<br />

Higger Tor<br />

The area is classed by the Ministry of Agriculture as Grade 5 land which means the land is very poor farming<br />

land. Grants are available from the Government to help the farming community. Only a small number of sheep<br />

can be kept on the moors, as overgrazing has a serious effect on the vegetation, which cannot regenerate<br />

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13/10/2009 Peak District National Park: Study Area<br />

quickly due to the difficult growing conditions. Overgrazing also allows invasive species like bracken to<br />

encroach onto the moors.<br />

It is likely that much of the area was once covered with trees. Bronze Age and Iron Age farmers cleared the<br />

trees to grow crops and centuries of sheep grazing have prevented their regrowth. The natural moorland is in<br />

fact a man-made environment.<br />

Recreation<br />

The closeness of the <strong>Burbage</strong> Valley to major towns has led to its popularity with a wide range of people. The<br />

many tracks and paths through the valley have encouraged walkers into the area and rock climbers can be<br />

seen on many days throughout the year taking advantage of the climbing routes available on <strong>Burbage</strong> Edge.<br />

Another sport popular with many youth groups is that of weaseling and this involves scrambling around some<br />

of the large gritstone blocks on Higger Tor.<br />

Management of the Moors<br />

When the moors had shooting rights let out on them, they were specifically managed to encourage the<br />

grouse. This involved the burning of small patches of heather in rotation during the winter to encourage new<br />

growth. Recently, controlled burning has taken place to encourage regrowth of heather, creating habitats for<br />

wildlife and food for sheep. Uncontrolled summer fires can cause a lot of damage to vegetation and to<br />

creatures. An area devastated by fire in 1976 is still mainly bare peat and (where the peat has burnt away)<br />

bare gritstone.<br />

Further management problems come from the erosion of footpaths by walkers and increasingly by mountain<br />

bikes. Footpaths around Higger Tor are being repaired and re-surfaced by the Peak District Rangers to keep<br />

erosion to a minimum.<br />

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