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The Berkshire Downs are a range of chalk downland hills in southern England, part of the North Wessex Downs Area of Outstanding Natural Beauty. The Berkshire Downs are wholly within the traditional county of Berkshire, although split between the current ceremonial counties of Berkshire and Oxfordshire. The western parts of the downs are also known as the Lambourn Downs.
The Berkshire Downs run east–west, with their scarp slope facing north into the Vale of White Horse and their dip slope bounded by the course of the River Kennet. Geologically they are continuous with the Marlborough Downs to the west and the Chilterns to the east. In the east they are divided from the Chilterns by Goring Gap on the River Thames. In the west their boundary is generally taken to be the border between Berkshire and Wiltshire, although the downs in Wiltshire between the Berkshire border and the valley of the River Og are sometimes considered to be part of the Berkshire Downs.
English downland has attracted human habitation since prehistoric times. The ancient track known as the Ridgeway runs along the Berkshire Downs. Prehistoric sites in the Downs include Wayland's Smithy (Neolithic), numerous tumuli (Neolithic or Bronze Age), Uffington White Horse (Bronze Age), Liddington Castle and Uffington Castle (Bronze Age and Iron Age), and Segsbury Camp and Grim's Ditch (Iron Age).
It is generally thought that in Anglo-Saxon times the downs were known as Æscesdūn or Ashdown, and that it was here that the Battle of Ashdown was fought in 871. [1]
In 1915, after a brief stint as a hospital orderly at the British hospital for French soldiers in Haute-Marne, John Masefield moved to his country retreat at Lollingdon Farm. The setting at the foot of the Downs - Masefield's "Lollingdon Downs" would inspire a number of poems and sonnets.
Downland pasture is firm and well drained, suited to grazing sheep and grazing and training horses. Horse racing is a major business in the area, with much of the downs covered with training areas, and stables centred on the village of Lambourn.
The Berkshire Downs can be accessed from various cities via the Great Western Main Line and its current single operator runs localised stopping trains as well as the high-speed trains along the Vale of White Horse calling at major stops Swindon and Didcot Parkway. From Reading to Newbury trains run along the Reading to Taunton Line in the River Kennet Valley to reach Devon on the quickest route from London. From Reading there are the scenic Thames Valley stations of Pangbourne, Goring & Streatley and Cholsey (linked to the Cholsey and Wallingford Railway).
The Ridgeway is a ridgeway or ancient trackway described as Britain's oldest road. The section clearly identified as an ancient trackway extends from Wiltshire along the chalk ridge of the Berkshire Downs to the River Thames at the Goring Gap, part of the Icknield Way which ran, not always on the ridge, from Salisbury Plain to East Anglia. The route was adapted and extended as a National Trail, created in 1972. The Ridgeway National Trail follows the ancient Ridgeway from Overton Hill, near Avebury, to Streatley, then follows footpaths and parts of the ancient Icknield Way through the Chiltern Hills to Ivinghoe Beacon in Buckinghamshire. The National Trail is 87 miles (140 km) long.
Wiltshire is a ceremonial county in South West England. It borders Gloucestershire to the north, Oxfordshire to the north-east, Berkshire to the east, Hampshire to the south-east, Dorset to the south, and Somerset to the west. The largest settlement is Swindon, and Trowbridge is the county town.
Oxfordshire is a ceremonial county in South East England. The county is bordered by Northamptonshire and Warwickshire to the north, Buckinghamshire to the east, Berkshire to the south, and Wiltshire and Gloucestershire to the west. The city of Oxford is the largest settlement and county town.
The Royal County of Berkshire, commonly known as simply Berkshire, is a ceremonial county in South East England. It is bordered by Oxfordshire to the north, Buckinghamshire to the north-east, Greater London to the east, Surrey to the south-east, Hampshire to the south, and Wiltshire to the west. Reading is the largest settlement and the county town.
The Uffington White Horse is a prehistoric hill figure, 110 m (360 ft) long, formed from deep trenches filled with crushed white chalk. The figure is situated on the upper slopes of Whitehorse Hill in the English civil parish of Uffington in Oxfordshire, some 16 km (10 mi) east of Swindon, 8 km (5.0 mi) south of the town of Faringdon and a similar distance west of the town of Wantage; or 2.5 km (1.6 mi) south of Uffington. The hill forms a part of the scarp of the Berkshire Downs and overlooks the Vale of White Horse to the north. The best views of the figure are obtained from the air, or from directly across the Vale, particularly around the villages of Great Coxwell, Longcot, and Fernham.
Downland, chalkland, chalk downs or just downs are areas of open chalk hills, such as the North Downs. This term is used to describe the characteristic landscape in southern England where chalk is exposed at the surface. The name "downs" is derived from the Old English word dun, meaning "hill".
The Kennet is a tributary of the River Thames in Southern England. Most of the river is straddled by the North Wessex Downs AONB. The lower reaches have been made navigable as the Kennet Navigation, which – together with the Avon Navigation, the Kennet and Avon Canal and the Thames – links the cities of Bristol and London.
The Icknield Way is an ancient trackway in southern and eastern England that runs from Norfolk to Wiltshire. It follows the chalk escarpment that includes the Berkshire Downs and Chiltern Hills.
The Chiltern Hills are a chalk escarpment in southern England, northwest of London, covering 660 square miles (1,700 km2) across Oxfordshire, Buckinghamshire, Hertfordshire, and Bedfordshire, stretching 45 miles (72 km) from Goring-on-Thames in the southwest to Hitchin in the northeast. The hills are 12 miles (19 km) at their widest.
West Berkshire is a unitary authority area in the ceremonial county of Berkshire, England. It is administered from Newbury by West Berkshire Council.
The South Downs are a range of chalk hills in the south-eastern coastal counties of England that extends for about 260 sq mi (670 km2) across the south-eastern coastal counties of England from the Itchen valley of Hampshire in the west to Beachy Head, in the Eastbourne Downland Estate, East Sussex, in the east. The Downs are bounded on the northern side by a steep escarpment, from whose crest there are extensive views northwards across the Weald. The South Downs National Park forms a much larger area than the chalk range of the South Downs, and includes large parts of the Weald.
The Vale of White Horse is a local government district of Oxfordshire in England. It was historically part of Berkshire. The area is commonly referred to as the 'Vale of the White Horse'. It is crossed by the Ridgeway National Trail in its far south, across the North Wessex Downs AONB at the junction of four counties. The northern boundary is defined by the River Thames. The name refers to Uffington White Horse, a prehistoric hill figure.
The Vale of Pewsey or Pewsey Vale is an area of Wiltshire, England to the east of Devizes and south of Marlborough, centred on the village of Pewsey.
The River Lambourn is a chalk stream in the English county of Berkshire. It rises in the Berkshire Downs near its namesake village of Lambourn and is a tributary of the River Kennet, which is itself a tributary of the River Thames.
Lambourn is a village and civil parish in Berkshire, England. It lies just north of the M4 Motorway between Swindon and Newbury, and borders Wiltshire to the west and Oxfordshire to the north. After Newmarket it is the largest centre of racehorse training in England, and is home to a rehabilitation centre for injured jockeys, an equine hospital, and several leading jockeys and trainers. To the north of the village are the prehistoric Seven Barrows and the nearby long barrow. In 2004 the Crow Down Hoard was found close to the village.
The North Wessex Downs National Landscape is located in the English counties of Berkshire, Hampshire, Oxfordshire and Wiltshire. The name North Wessex Downs is not a traditional one, the area covered being better known by various overlapping local names, including the Berkshire Downs, the North Hampshire Downs, the White Horse Hills, the Lambourn Downs, the Marlborough Downs, the Vale of Pewsey and Savernake Forest.
Uffington is a village and civil parish in Oxfordshire, about 4 miles (6.4 km) south of Faringdon and 6 miles (10 km) west of Wantage. The 2011 Census recorded the parish's population as 783. Lying within the historic county boundaries of Berkshire, in 1974 it was transferred for local government purposes to Oxfordshire under the Local Government Act 1972. Uffington is most commonly known for the Uffington White Horse hill figure on the Berkshire Downs in the south of the parish.
Lardon Chase, the Holies and Lough Down is a National Trust countryside property in the English county of Berkshire. It is situated on the edge of the Berkshire Downs above the village of Streatley and overlooking the Goring Gap. The property comprises an outstanding area of 27 hectares of downland and woodland with many attractive walks and views. Lardon Chase, and a part of the Holies known as Holies Down, are also designated as Sites of Special Scientific Interest. The property lies within the North Wessex Downs Area of Outstanding Natural Beauty, and in an area known for the presence of several Neolithic and Iron Age forts.
Cholsey is a village and civil parish 2 miles (3 km) south of Wallingford in South Oxfordshire. In 1974 it was transferred from Berkshire to Oxfordshire, and from Wallingford Rural District to the district of South Oxfordshire. The 2011 Census recorded Cholsey's parish population as 3,457. Cholsey's parish boundaries, some 17 miles (27 km) long, reach from the edge of Wallingford into the Berkshire Downs. The village green is called "The Forty" and has a substantial and ancient walnut tree.
The London Basin is an elongated, roughly triangular sedimentary basin approximately 250 kilometres (160 mi) long which underlies London and a large area of south east England, south eastern East Anglia and the adjacent North Sea. The basin formed as a result of compressional tectonics related to the Alpine orogeny during the Palaeogene period and was mainly active between 40 and 60 million years ago.
