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Bilberry Hill is one of the
Lickey Hills The Lickey Hills (known locally as simply ''The Lickeys'') are a range of hills in Worcestershire, England, to the south-west of the centre of Birmingham near the villages of Lickey, Cofton Hackett and Barnt Green. The hills are a popular coun ...
in northern
Worcestershire Worcestershire ( , ; written abbreviation: Worcs) is a Ceremonial counties of England, ceremonial county in the West Midlands (region), West Midlands of England. It is bordered by Shropshire, Staffordshire, and the West Midlands (county), West ...
, England, southwest of
Birmingham Birmingham ( ) is a City status in the United Kingdom, city and metropolitan borough in the metropolitan county of West Midlands (county), West Midlands, within the wider West Midlands (region), West Midlands region, in England. It is the Lis ...
and northeast of
Worcester Worcester may refer to: Places United Kingdom * Worcester, England, a city and the county town of Worcestershire in England ** Worcester (UK Parliament constituency), an area represented by a Member of Parliament * Worcester Park, London, Engl ...
. It stands above and to the west of the
village A village is a human settlement or community, larger than a hamlet but smaller than a town with a population typically ranging from a few hundred to a few thousand. Although villages are often located in rural areas, the term urban v ...
of
Cofton Hackett Cofton Hackett is a village and civil parish in the Bromsgrove (district), Bromsgrove District of Worcestershire, north east Worcestershire, England. It is southwest of the city centre of Birmingham and northeast of Worcester, England, Worcest ...
, and is part of the
Lickey Hills Country Park Lickey Hills Country Park is a country park in England. It is south-west of Birmingham and north-east of Worcester. The 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 three
hill A hill is a landform that extends above the surrounding terrain. It often has a distinct summit, and is usually applied to peaks which are above elevation compared to the relative landmass, though not as prominent as Mountain, mountains. Hills ...
tops comprising The Lickeys—Bilberry Hill, Rednal Hill and Cofton Hill—form the northern extremity of the Lickey Ridge, a formation of hard
quartzite Quartzite is a hard, non- foliated metamorphic rock that was originally pure quartz sandstone.Essentials of Geology, 3rd Edition, Stephen Marshak, p 182 Sandstone is converted into quartzite through heating and pressure usually related to tecton ...
. Views over
Birmingham Birmingham ( ) is a City status in the United Kingdom, city and metropolitan borough in the metropolitan county of West Midlands (county), West Midlands, within the wider West Midlands (region), West Midlands region, in England. It is the Lis ...
and the surrounding countryside can be seen from the top of these hills. The hill is named after the tracts of
Bilberry Bilberries () are Eurasian low-growing shrubs in the genus ''Vaccinium'' in the flowering plant family Ericaceae that bear edible, dark blue berries. They resemble but are distinct from North American blueberries. The species most often referre ...
(''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.


History

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 The Cadbury family is a British family of wealthy Quaker industrialists descending from Richard Tapper Cadbury. * Richard Tapper Cadbury (1768–1860), draper and abolitionist, who financed his sons' start-up business; married Elizabeth Head **J ...
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. 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. 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.


Geology

The Lickey Hills area is of significant
geological Geology (). is a branch of natural science concerned with the Earth and other astronomical objects, the rocks of which they are composed, and the processes by which they change over time. Modern geology significantly overlaps all other Earth s ...
interest due to the range and age of the
rocks In geology, rock (or stone) is any naturally occurring solid mass or aggregate of minerals or mineraloid matter. It is categorized by the minerals included, its chemical composition, and the way in which it is formed. Rocks form the Earth's ...
. The darker quartzite making up Bilberry Hill shows signs of having been deposited as sand at the bottom of a shallow sea. The
stratigraphic Stratigraphy is a branch of geology concerned with the study of rock layers (strata) and layering (stratification). It is primarily used in the study of sedimentary and layered volcanic rocks. Stratigraphy has three related subfields: lithost ...
sequence, which is the basis for the area's diversity of
landscape A landscape is the visible features of an area of land, its landforms, and how they integrate with natural or human-made features, often considered in terms of their aesthetic appeal.''New Oxford American Dictionary''. A landscape includes th ...
and
habitat In ecology, habitat refers to the array of resources, biotic factors that are present in an area, such as to support the survival and reproduction of a particular species. A species' habitat can be seen as the physical manifestation of its ...
, comprises: *Barnt Green rocks -
tuff Tuff is a type of rock made of volcanic ash ejected from a vent during a volcanic eruption. Following ejection and deposition, the ash is lithified into a solid rock. Rock that contains greater than 75% ash is considered tuff, while rock co ...
s and
volcanic A volcano is commonly defined as a vent or fissure in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often fo ...
grits Grits (stylized as GRITS) is an American Christian hip hop group from Nashville, Tennessee. Their name is an acronym, which stands for "Grammatical Revolution In the Spirit". GRITS is made up of Stacey "Coffee" Jones and Teron "Bonafide" Carter ...
siltstone Siltstone, also known as aleurolite, is a clastic sedimentary rock that is composed mostly of silt. It is a form of mudrock with a low clay mineral content, which can be distinguished from shale by its lack of fissility. Although its permeabil ...
s and
mudstone Mudstone, a type of mudrock, is a fine-grained sedimentary rock whose original constituents were clays or muds. Mudstone is distinguished from ''shale'' by its lack of fissility.Blatt, H., and R.J. Tracy, 1996, ''Petrology.'' New York, New York, ...
s from the Tremadocian stage of the
Ordovician The Ordovician ( ) is a geologic period and System (geology), system, the second of six periods of the Paleozoic Era (geology), Era, and the second of twelve periods of the Phanerozoic Eon (geology), Eon. The Ordovician spans 41.6 million years f ...
*Lickey Quartzite - an
Ordovician The Ordovician ( ) is a geologic period and System (geology), system, the second of six periods of the Paleozoic Era (geology), Era, and the second of twelve periods of the Phanerozoic Eon (geology), Eon. The Ordovician spans 41.6 million years f ...
quartzite Quartzite is a hard, non- foliated metamorphic rock that was originally pure quartz sandstone.Essentials of Geology, 3rd Edition, Stephen Marshak, p 182 Sandstone is converted into quartzite through heating and pressure usually related to tecton ...
with thin beds of mudstone and possibly tuff *Halesowen Formation - a
Carboniferous The Carboniferous ( ) is a Geologic time scale, geologic period and System (stratigraphy), system of the Paleozoic era (geology), era that spans 60 million years, from the end of the Devonian Period Ma (million years ago) to the beginning of the ...
mudstone Mudstone, a type of mudrock, is a fine-grained sedimentary rock whose original constituents were clays or muds. Mudstone is distinguished from ''shale'' by its lack of fissility.Blatt, H., and R.J. Tracy, 1996, ''Petrology.'' New York, New York, ...
of Westphalian D age * Clent Formation - a
breccia Breccia ( , ; ) is a rock composed of large angular broken fragments of minerals or Rock (geology), rocks cementation (geology), cemented together by a fine-grained matrix (geology), matrix. The word has its origins in the Italian language ...
of lower
Permian The Permian ( ) is a geologic period and System (stratigraphy), stratigraphic system which spans 47 million years, from the end of the Carboniferous Period million years ago (Mya), to the beginning of the Triassic Period 251.902 Mya. It is the s ...
age * Bunter Pebble Beds -
bed A bed is a piece of furniture that is used as a place to sleep, rest, and relax. Most modern beds consist of a soft, cushioned mattress on a bed frame. The mattress rests either on a solid base, often wood slats, or a sprung base. Many beds ...
s of
Triassic The Triassic ( ; sometimes symbolized 🝈) is a geologic period and system which spans 50.5 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.4 Mya. The Triassic is t ...
water-worn
pebble A pebble is a clastic rocks, clast of rock (geology), rock with a grain size, particle size of based on the Particle size (grain size), Udden-Wentworth scale of sedimentology. Pebbles are generally considered larger than Granule (geology), gra ...
s The quary that was on Bilberry Hill cut into rocks dating from the Ordovician period of geological time, around 488 million years ago; the rocks are known to geologists as the Lickey Quartzite Formation. 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 The Worcester and Birmingham Canal is a canal linking Birmingham and Worcester in England. It starts in Worcester, as an 'offshoot' of the River Severn (just after the river lock) and ends in Gas Street Basin in Birmingham. It is long. There ...
, and there are some gravel-pits.


See also

*
Lickey Incline The Lickey Incline, south of Birmingham, is the steepest sustained main-line railway incline in Great Britain. The climb is a gradient of 1 in 37.7 (2.65% or 26.5‰ or 1.52°) for a continuous distance of two miles (3.2 km). Constructed o ...
*Margaret Mabey, ''A Little History of the Lickey Hills'', The Lickey Hills Society, 1993, *Around Rubery and The Lickey Hills compiled by Martin Hampson. From the Images of England Series published by Tempus Publishing Limited 2000.


References


External links


Country park website
{{Authority control Country parks in Worcestershire Hills of Worcestershire