Hollow Meadows

Moscar Cross is the name of a standing stone (or "guide stoop") and surrounding area in the Peak District on the border between Derbyshire and Sheffield, England. Moscar moor is located south of the cross, and contains a stone circle, Hordron Edge stone circle.

Sugworth Hall is an English country house on Sugworth Road in Bradfield Dale, near Sheffield, England. It is situated approximately 8 miles (13 km) west from Sheffield City Centre. The hall is a Grade II listed building which stands within the Peak District National Park at a height of 984 feet (300 m) above sea level.

Long Causeway or Long Causey was a medieval packhorse route in England, which ran between Sheffield in South Yorkshire and Hathersage in Derbyshire. In the past the route has been marked on maps as a Roman Road as it was believed it followed part of the route of Batham Gate between Templeborough and Buxton, although in recent years some scholars have cast doubt on this.

Strines Reservoir is a water storage reservoir situated at 53.4099°N 1.6557°W / 53.4099; -1.6557 (Strines_Reservoir), 8 miles (13 km) west of the centre of Sheffield in South Yorkshire, England.

Stanedge Pole also known as Stanage Pole (grid reference SK2468784429) is a landmark on Hallam Moors close to Stanage Edge in South Yorkshire, England. Standing at a height of 438 metres (1,437 feet), it marks the border between Derbyshire and South Yorkshire and can be seen for several miles around. A pole has stood on the site since at least 1550. Many initials have been carved into the rock that supports it, and five can be identified as initials of the parish road surveyors who renewed the pole when needed. "T.C. 1550", "H.W. 1581", "T.M. 1631", "H.H. 1697" and "F.N. 1740" are the marks of the parish surveyors and the date the pole was renewed. The pole is a way marker on a medieval packhorse road known as the Long Causeway or Long Causey which runs west from Sheffield. It was used for centuries as a boundary marker between the parishes of Sheffield, Hathersage and Ecclesfield. Although it is widely believed the Long Causeway follows the line of a Roman road that ran from Templeborough Roman fort to the fort at Navio (Brough-on-Noe), archaeologists have cast doubt on this. There is some suggestion that the pole also marks the old boundary between Mercia and Northumberland. The top part of the pole was removed on Friday, 27 February 2015. A spokesperson for the Peak District National Park explained that "the wood on the top half of the pole was rotten and therefore a health and safety risk to the public. We had no choice but to make the pole safe by cutting off the top part.” On 17 April 2016 a group of people with an interest in the pole and surrounding environment, including the Peak District National Park Authority and the British Mountaineering Council, erected a new pole at the site to mark the 65th anniversary of the creation of the Peak District National Park. Support for the renewal also came from the Hope Cement Works, The Durham Foundry (Sheffield) Ltd, The Cutler's Company, Sheffield Clarion Ramblers and some public subscriptions. The new pole is formed from a locally felled larch tree, with a frame made by Hope Cement Works, and a base cast in Sheffield. The base is cast from ductile iron and has information cast into it (see photograph).

Bradfield Dale is a rural valley 12 kilometres (7.5 mi) west-northwest of the City of Sheffield in England. The valley stands within the north-eastern boundary of the Peak District National Park just west of the village of Low Bradfield. The dale is drained by the Strines Dike which becomes the Dale Dike lower down the valley, these being the headwaters of the River Loxley. The dale contains two reservoirs, Strines and Dale Dike, and a third, Agden Reservoir, stands in a side valley just above Low Bradfield. The dale is characterised by agricultural land interspersed with farming and residential buildings. It is approximately 5 kilometres (3.1 mi) long from its foot at Low Bradfield to its head on Strines Moor.

Dale Dike Reservoir or Dale Dyke Reservoir (grid reference SK240913) is a reservoir in the north-east Peak District, in the City of Sheffield, South Yorkshire, England, a mile (1.6 km) west of Bradfield and eight miles (13 km) from the centre of Sheffield, on the Dale Dike, a tributary of the River Loxley. Along with three other reservoirs around the village of Bradfield – Agden, Damflask and Strines – it was constructed between 1859 and 1864 by the Sheffield Waterworks Company to guarantee a supply of water to power the mills downstream and to supply drinking water to the growing population of Sheffield. The architect was John Gunson.

Hallfield House is a Grade II listed building situated in Bradfield Dale, 1.7 miles (2.74 km) west of the village of Low Bradfield, near Sheffield in England.

The Redmires Reservoirs are a group of three reservoirs in Fulwood, Sheffield, South Yorkshire, England. They are fed from the Hallam Moors by various small streams including Fairthorn Clough. The three reservoirs are named Upper, Middle and Lower and were built between 1833 and 1854 to provide clean drinking water via an open water course which led to the Hadfield Dam situated in Crookes, following the devastating Sheffield cholera epidemic of 1832. The dams were built as part of the Sheffield Water Works continuing expansion to meet the ever growing population of Sheffield. The area is popular with walkers and bird watchers. Adjacent to the Middle Reservoir is Hammond's Field Nature Reserve, which is managed by The Wildlife Trust for Sheffield and Rotherham. The nature reserve forms part of the South Pennine Moors Special Protected Area. A path, the Long Causeway leads from the Upper reservoir, onto the moors to Stanedge Pole and then onto Stanage Edge. This route was once thought to be a Roman road but is now thought to be a Medieval packhorse saltway, used to convey salt from Cheshire to Yorkshire.

Ughill is a small, rural hamlet within the City of Sheffield in Bradfield Parish in England. It is 5 mi (8 km) west-northwest of the city centre. It stands in a lofty position at 918 ft (280 m) above sea level, on a ridge between Bradfield Dale and the valley of the Ughill Brook. It has traditionally been a farming community, but there was some mining in the area in the late 19th and 20th century. Ughill Hall was the scene of an infamous murder in September 1986. The hamlet falls within the Stannington ward of the City.

Stanage Edge, or simply Stanage (from "stone edge") is a gritstone escarpment in the Peak District, England, famous as a location for climbing. It lies a couple of miles to the north of Hathersage, and the northern part of the edge forms the border between the High Peak of Derbyshire and Sheffield in South Yorkshire. Its highest point is High Neb at 458 metres (1,503 ft) above sea level. Areas of Stanage were quarried in the past to produce grindstones, and some can still be seen on the hillside—carved, but never removed.

Hordron Edge stone circle, also known as 'The Seven Stones of Hordron' is a Bronze Age stone circle (grid reference SK2152486851) in Derbyshire, England. It is on the edge of Moscar Moor. Ladybower reservoir is to the west, and Moscar Cross is to the northeast. Seven stones are presently (2017) visible with a further three stones, now recumbent and hidden discovered in 1992. Some authorities believe that the circle might have once comprised 26 stones.The stone circle is approximately 15 to 16 m (49 to 52 ft) in diameter, with eleven stones between 45 cm and 95 cm high extant upright.