Great Hill

Black Brook in Lancashire has its source at Great Hill in the West Pennine Moors. The water is acidic due to a high level of peat in the uplands near to Round Loaf, giving the brook its brown colour. The young river was known as Warth Brook in olden Heapey. A feeder stream also known as Black Brook joins near Kittiwake Road - this short and weak water course commences at Eagle Tower. The jointed brook feeds Anglezarke Reservoir, and joins the River Yarrow in lowland Chorley at Yarrow Bridge. The entire course of Black Brook and the River Yarrow fall within Chorley and its villages.

Round Loaf is a late-Neolithic or Bronze Age tumulus on Anglezarke Moor in the West Pennine Moors near Chorley in Lancashire, England. The bowl barrow is a scheduled monument considered to be of national importance. It was first scheduled in March 1954. The structure is aligned between Great Hill and Pikestones.

Spitlers Edge is a ridge running along the eastern edge of Anglezarke Moor, Chorley, Lancashire, England from Standing Stones Hill to Hordern Stoops. The peak, complete with a cairn at 1,286 feet (392 m), is the high point of the moorland. Redmonds Edge links Spitlers Edge to Great Hill and is paved. As of 2017, there are plans to extend the paving along the length of Spitlers Edge - with funding secured from the Lancashire Environmental Fund and United Utilities.Along the length of the edge is a stone wall of some historical importance - the boundary was built in 1841 as a relief measure to provide respite from the Hungry Forties, and is the parliamentary division boundary between Chorley and Blackburn. The name is derived from the fact that in mediaeval times, the Knights Hospitallers of St. John of Jerusalem used this route when travelling to their holdings in this district. The ridge provides the peaks that supply the source water to the River Yarrow.

Roddlesworth is a hamlet in the parish of Withnell in Lancashire, England. It lies on the road connecting Preston with Bolton. The name is first encountered as Rodtholfeswrtha (1160), meaning "the homestead of Hrothwulf".

Hurst Hill is a location on Anglezarke Moor, within the West Pennine Moors of Lancashire, England. Despite a modest height of 317 metres (1040 feet), the summit provides excellent views towards the Irish Sea. Of more note, however, is its location between Round Loaf and Pikestones, both of which are Neolithic remnants. It is probable that Hurst Hill (and nearby Grain Pole Hill) were vantage points for the ancient communities. No excavation work has taken place.

Rake Brook Reservoir is a reservoir fed by two streams, including the eponymous Rake Brook, a tributary of the River Roddlesworth in Lancashire, England. The reservoir is adjacent to the two Roddlesworth Reservoirs. It was constructed in the 1850s by Thomas Hawksley for Liverpool Corporation Waterworks, and was designed to hold compensation water to maintain flows in the rivers, whereas the reservoirs at Lower Rivington, Upper Rivington and Anglezarke held water for the public water supply. Water from the reservoir was fed into Anglezarke reservoir by a 3.75-mile (6.04 km) channel called The Goit.Construction of the reservoir was authorised by an Act of Parliament obtained in 1847, and the engineer Thomas Hawksley designed an earth dam which was 85 feet (26 m) tall at its highest point and 1,490 feet (450 m) long. The reservoir was finished in 1857, and impounded 73 million imperial gallons (330 Ml) of water when full.

Hollinshead Hall was a manor house close to the village of Tockholes, Lancashire. It is unclear whether the hall was originally the manor house of Tockholes, or if Hollinshead was indeed a manor in its own right alongside Tockholes and Livesey. The ruins of the hall are situated approximately 2 miles (3.2 km) south of the village. The main features of the site consist of the ruins of the late 18th century hall and Gardens, and the associated barn and stables. To the south of here are the remains of the farmhouse and farm buildings, and at the south-east side of the enclosed garden is a well house, the only structure on the site which remains standing today.

Withnell is a village and civil parish in the Borough of Chorley, Lancashire, England. According to the census of 2001, it had a population of 3,631, reducing to 3,498 at the census of 2011. Withnell is about 5 miles (8 km) north-east of Chorley itself and about 5 miles (8 km) from Blackburn. It constituted an urban district from 1894 to 1974. It was originally called 'Withinhull' around 1160, later appearing as 'Withinhulle' in the 1332 Subsidy Rolls of Lancashire, meaning 'a hill where willow trees grow'. It borders the villages of Brinscall and Abbey Village which are part of the parish.

Lower Roddlesworth Reservoir is a reservoir on the River Roddlesworth close to Abbey Village in Lancashire, England. The reservoir is close to Upper Roddlesworth Reservoir and Rake Brook Reservoir, situated within thick forest. It was constructed in the 1850s by Thomas Hawksley for Liverpool Corporation Waterworks, and together with Rake Brook, was designed to hold compensation water to maintain flows in the rivers, whereas the reservoirs at Lower Rivington, Upper Rivington and Anglezarke held water for the public water supply. Water from the two compensation reservoirs was fed into Anglezarke reservoir by a 3.75-mile (6 km) channel called The Goit.An Act of Parliament to authorise its construction was obtained in 1847, and Hawksley designed an earth dam which was 82 feet (25 m) tall at its highest point and 590 feet (180 m) long. It impounded 91 million imperial gallons (414 Ml) of water when full. The reservoir was completed in 1857.

Abbey Village is a village in the English county of Lancashire and the constituency of Chorley. It is located on the A675 road, six miles (10 km) from Blackburn, eight miles from Chorley, nine miles (14 km) from Preston and ten miles from Bolton.

Upper Roddlesworth Reservoir is a reservoir on the River Roddlesworth near Abbey Village in Lancashire, England. The reservoir is close to Lower Roddlesworth Reservoir and Rake Brook Reservoir and sits within dense woodland.

Pikestones is the remains of a Neolithic Burial Cairn, located on Anglezarke moor in Lancashire, England. The site is approximately 150 feet (45 metres) long and 60 feet (18 metres) across at its widest point. It consisted of one burial chamber constructed of large upright slabs, capped by two lintel slabs, forming a chamber of 15 feet (4.5 metres) long, 3 feet (0.9 metres) wide and 3 feet (0.9 metres) high, covered by a huge mound of stones and turves. The cairn was aligned almost exactly North-South, with the burial chamber under the wider northern end. At the northern edge of the cairn, a double wall could be made out, curving inwards to form an entrance to a forecourt. Today the cairn has been badly robbed and the main features are the five large gritstone slabs, the remains of the burial chamber. Surprisingly, evidence suggests that the bodies were not interred directly in the tomb, but were left outside, perhaps at the entrance to the cairn, for birds and wild animals to consume the flesh and then, probably after elaborate ceremonies, the bones were placed inside the chamber. Pikestones is the earliest man-made structure in the area and only one other chambered tomb has been found in Lancashire. The monument must have taken an immense amount of labour to construct and like most long barrows was erected in a prominent position, located on a ridge at a height of just over 900 feet (276 metres). This gave the neolithic builders excellent views, and made the structure visible from a wide area of the Lancashire plain, perhaps warning other people that the land belonged to the builders.