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Bilberry Hill | |
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Highest point | |
Elevation | 260 m (850 ft) [1] |
Prominence | 116 m (381 ft) [2] |
Geography | |
Location | Worcestershire, UK |
Parent range | Lickey Hills |
Bilberry Hill is one of the Lickey Hills in northern Worcestershire, England, 10.3 miles (16.6 kilometres) southwest of Birmingham and 24 miles (39 kilometres) northeast of Worcester. It stands above and to the west of the village of Cofton Hackett, and is part of the Lickey Hills Country Park.
The three hilltops comprising The Lickeys—Bilberry Hill, Rednal Hill and Cofton Hill—form the northern extremity of the Lickey Ridge, a formation of hard quartzite. Views over Birmingham and the surrounding countryside can be seen from the top of these hills.
The hill is named after the tracts of Bilberry (Vaccinium myrtillus) bushes that cover the hill, between the pathways. Local people have been cropping the bushes of their fruit each autumn for hundreds of years to make jams, preserves or apple and bilberry pies.
In 1888, the Birmingham Society for the Preservation of Open Spaces purchased Rednal Hill and handed it to the City in trust. In 1913, they also arranged for Bilberry Hill and Pinfold Wood to be leased to the city on a nominal peppercorn rent in perpetuity. Birmingham City Council finally purchased Cofton Hill, Lickey Warren and Pinfield Wood outright in 1920. With the eventual purchase of the Rose Hill Estate from the Cadbury family in 1923, free public access was finally restored to the entire hills with what would become the Lickey Hills Country Park in 1971.
The Bilberry Hill Centre was a hostel and sports facility run by Birmingham Clubs for Young People and nestling at the base of Bilberry Hill. The building was donated to the people of Birmingham by Mr. and Mrs. Barrow Cadbury in 1904 as the Lickey Tea Rooms and remained in use as a restaurant until the early 1960s. The hostel can accommodate up to 65 persons. [3] In the winter of 2008, the Centre was under threat of imminent closure over funding issues, and there was an internet campaign to save the facility for future use by young people. [4] It remained in operation until 2019, when the Birmingham Federation of Clubs for Young People went into administration. The Birmingham City Council has owned the site since, which is currently derelict. In 2022, the Cofton Hackett Parish Council held two public meetings to decide the future of the site. [5]
The Lickey Hills area is of significant geological interest due to the range and age of the rocks. The darker quartzite making up Bilberry Hill shows signs of having been deposited as sand at the bottom of a shallow sea. The stratigraphic sequence, which is the basis for the area's diversity of landscape and habitat, comprises: [6]
The soil is marl and the subsoil gravel, sand and clay. There is a small quarry where Wenlock limestone was worked at the time of the making of the Worcester and Birmingham Canal, and there are some gravel-pits.
Barnt Green is a village and civil parish in the Bromsgrove District of Worcestershire, England, situated 10 miles (16 km) south of Birmingham city centre, with a population at the 2011 census of 1,794.
Rednal is a residential suburb on the south western edge of metropolitan Birmingham, West Midlands, England, 9 miles southwest of Birmingham city centre and forming part of Longbridge parish and electoral ward. Historically it was part of Worcestershire.
West Heath is a residential area of Birmingham, England on the boundary with Worcestershire. Forming the larger part of the ward of Longbridge And West Heath it is situated between Kings Norton, Northfield, Longbridge and Cofton Hackett and lies on traditional heathland formed in the 13th century as part of the Kings Norton manorial lands, and was historically in Worcestershire.
Lickey Hills Country Park is a country park in England. It is 10 miles south west of Birmingham and 24 miles north east of Worcester. The 524 acres (212 ha) park is situated just south of Rednal and close to Barnt Green. It is half a mile west of Cofton Hackett. It is one of the oldest parks managed by Birmingham City Council. The hills rise to 298 m (978 ft) above sea level at Beacon Hill.
The Clent Hills lie 10 miles (16 km) south-west of Birmingham city centre in Clent, Worcestershire, England. The closest towns are Stourbridge and Halesowen, both in the West Midlands conurbation. The Clent Hills range consists of, in order from north-west to south-east: Wychbury Hill, Clent Hill, and Walton Hill. The north Worcestershire range of hills continues eastwards to include Romsley Hill, Waseley Hills and the Lickey Hills.
Lickey is a "linear development" in the north of Worcestershire, England approximately 10 miles (16 km) south west from the centre of Birmingham. It lies in Bromsgrove District and is situated on the Lickey Ridge, amongst the Lickey Hills, its proximity to countryside and the city makes it a popular commuter area. The civil parish of Lickey and Blackwell has a population of 4,140.
Cofton Hackett is a village and civil parish in the Bromsgrove District of north east Worcestershire, England. It is 10+1⁄4 miles southwest of the city centre of Birmingham and 16 miles (26 km) northeast of Worcester. In 2011, the village had a population of 1,893 but with housing development on the former Austin Rover site, this is expected to double over the five years to 2023. The village is served by two main bus services, these being the 20 and 145/145A operated by National Express and Diamond Bus respectively.
The Lickey Hills are a range of hills in Worcestershire, England, 11 miles (18 km) to the south-west of the centre of Birmingham near the villages of Lickey, Cofton Hackett and Barnt Green. The hills are a popular country park area and they afford panoramic views over much of the surrounding countryside.
Barnt Green railway station serves the village of Barnt Green, North Worcestershire, England. It is situated 9+1⁄2 miles (15.3 km) south west of Birmingham New Street. The station, and all trains serving it, are operated by West Midlands Trains.
For the Skiddaw group of hills, see Skiddaw Group
The Drefach Group is an Ordovician lithostratigraphic group in west Wales. The name is derived from the village of Drefach near Meidrim in Carmarthenshire. The Group comprises the Mydrim Shales Formation, the Mydrim Limestone Formation, the Hendre Shales Formation, Asaphus Ash Formation and at its base, the underlying Felin-wen Formation.
The Llanbedrog Volcanic Group is an Ordovician lithostratigraphic group in northwest Wales. The name is derived from the village of Llanbedrog on the Llyn Peninsula where the strata are exposed.
The Snowdon Volcanic Group is an Ordovician lithostratigraphic group in Snowdonia, north-west Wales. The name is derived from Snowdon, the highest peak in Wales where it outcrops. This assemblage of rocks has also been referred to as the Snowdon Volcanic Series.
Haffield Breccia, or Clent Breccia, consist of a texturally immature compacted gravel, rich in volcanic clasts with some sedimentary rocks, in a sandy or muddy matrix, which outcrops in the English Midlands, in South Staffordshire, Birmingham and the Malverns. It is thought to have been deposited by during flash floods in rivers that were flowing through a desert, somewhere between 200 and 280 million years ago during the Permian period. The gravel consists of angular fragments, showing that they have not been transported over long distances.
The Dent Group is a group of Upper Ordovician sedimentary and volcanic rocks in north-west England. It is the lowermost part of the Windermere Supergroup, which was deposited in the foreland basin formed during the collision between Laurentia and Avalonia. It lies unconformably on the Borrowdale Volcanic Group. This unit was previously known as the Coniston Limestone Group or Coniston Limestone Formation and should not be confused with the significantly younger Coniston Group.
The Ceiswyn Formation is an Ordovician lithostratigraphic group in Mid Wales. The rock of the formation is made up of interleaved beds of silty mudstones and siltstones with some sandstones and tuffs also present in small amounts. The formation runs diagonally across Mid Wales from close by Bala Lake to Cardigan Bay near Tywyn.
The geology of Loch Lomond and The Trossachs National Park in the southwestern part of the Scottish Highlands consists largely of Neoproterozoic and Palaeozoic bedrock faulted and folded and subjected to low grade metamorphism during the Caledonian orogeny. These older rocks, assigned to the Dalradian Supergroup, lie to the northwest of the northeast – southwest aligned Highland Boundary Fault which defines the southern edge of the Highlands. A part of this mountainous park extends south of this major geological divide into an area characterised by younger Devonian rocks which are assigned to the Old Red Sandstone.
The geology of Exmoor National Park in south-west England contributes significantly to the character of Exmoor, a landscape which was designated as a national park in 1954. The bedrock of the area consists almost wholly of a suite of sedimentary rocks deposited during the Devonian, a period named for the English county of Devon in which the western half of the park sits. The eastern part lies within Somerset and it is within this part of the park that limited outcrops of Triassic and Jurassic age rocks are to be found.
The Ogwen Group is an Ordovician lithostratigraphic group in Gwynedd, north-west Wales. The name is derived from Ogwen Valley, a locality in Snowdonia where it outcrops.
The geology of Staffordshire in the West Midlands region of England is largely characterised by sedimentary bedrock of late Palaeozoic to early Mesozoic age overlain by a suite of superficial materials deposited during the Quaternary period. The extraction of coal, limestone and clay have been significant industries within the county.