Site of Special Scientific Interest | |
Location | Hampshire |
---|---|
Grid reference | SU 603 227 [1] |
Interest | Biological |
Area | 46.4 hectares (115 acres) [1] |
Notification | 1984 [1] |
Location map | Magic Map |
Beacon Hill, Warnford is a 46.4-hectare (115-acre) biological Site of Special Scientific Interest west of Warnford in Hampshire. [1] [2] It is a Nature Conservation Review site, [1] and an area of 40.1 hectares (99 acres) is a national nature reserve. [3] There is a round barrow cemetery dating to the Late Neolithic or Bronze Age on the hill, and this is a scheduled monument. [4]
The hill lies to the west of the Meon Valley and opposite Old Winchester Hill. It gives a commanding view over the Hampshire Basin to the south, from the lower Itchen Valley and New Forest, the Solent and Isle of Wight and round to Portsdown Hill (over which the top of Portsmouth's Spinnaker Tower can be seen). On the eastern side the view takes in the Meon Valley including Meonstoke and West Meon, and the South Downs including Old Winchester Hill and Butser Hill. The spire of Privett church can be seen to the north.
The hill is crossed by two long-distance footpaths, the South Downs Way and the Monarch's Way. Due to the fragile nature of the thin chalk soils there has been much controversy over routing. At present there are temporary routes to the north of the main summit via Warnford, and to the south via Exton. [5] [6]
The site consists of the steep slopes of a chalk spur on the western side of the Meon valley, covered by chalk grassland, beech / ash / hazel woodland and chalk scrub. There are two separate parts, which are not joined to each other. The main section centred on grid reference SU603227 consists of two divisions: 16.2 hectares (40 acres) of Beaconhill Beeches (mixed broadleaved and yew woodland), and 23.54 hectares (58.2 acres) of chalk grassland. The smaller, separate northern section (centred on grid reference SU604234 ) is a strip of grassland on a north-facing slope of the northern of the hill's two eastern spurs.
The grassland at the site has sheep's fescue (Festuca ovina), salad burnet (Sanguisorba minor) and common rock-rose (Helianthemum nummularium) as its dominant species. Other species present are horseshoe vetch (Hippocrepis comosa), yellow-wort (Blackstonia perfoliata), fragrant orchid (Gymnadenia conopsea) and clustered bellflower (Campanula glomerata).
The grassland supports several rarer species - rampion (Phyteuma tenerum), field fleawort (Senecio integrifolius), hairy rock-cress (Arabis hirsuta) and man orchid (Aceras anthropophorum).
The site's butterfly fauna is mentioned in its citation sheet. Twenty-five species are known to breed, including colonies of silver-spotted skipper and Duke of Burgundy, together with comparatively large populations of brown argus, green hairstreak, chalkhill blue, marbled white and dingy skipper. [7]
The structural picture is similar to that at Winchester 15 kilometres (9.3 mi) to the west, with an east–west trending anticline in the upper chalk (the Winchester-East Meon Anticline) cut through by a south-flowing river to expose an inlier of middle and lower chalk. As with the Itchen, the upper Meon flows westwards along the fold trend, before swinging south to cut through the anticline. Beacon Hill at 201 metres (659 ft) to the west of the Meon and Old Winchester Hill at 212 metres (696 ft) to the east are remnants of the southward-dipping chalk on the southern side of the anticline. The anticline is somewhat domed, with the result that Old Winchester Hill is capped by older chalk than Beacon Hill despite being rather higher, whilst Wether Down and Butser Hill to the east are higher still. [8] [9] [10]
Beacon Hill is a section of east-facing Upper Chalk escarpment. Both Beacon Hill and Old Winchester Hill have a claim to being the point at which the main north-facing scarp of the South Downs turns northwards around the western end of the Weald; Beacon Hill is lower, but represents a higher level within the chalk, and Old Winchester Hill is cut to the north by the upper Meon valley. Small [11] suggests that the upper Meon (which like the upper Itchen flows east–west) was originally a headwater of the Itchen following the col to the north of Beacon Hill, before the south-flowing lower Meon cut back through the chalk.
The hill has been incised by a series of steep-sided semi-circular combes to the east, and deep dry valleys to the south and west. Between these several radiating spurs with minor roads and tracks meet near the summit.
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 visible geology of Hampshire in southern England broadly comprises a folded succession of sedimentary rocks dating from the Cretaceous and Palaeogene periods – mostly gentle folding in the north, more complex folding along the south coast. The lower (early) Cretaceous rocks are sandstones and mudstones whilst those of the upper (late) Cretaceous are the various formations that comprise the Chalk Group and give rise to the county's downlands. Overlying these rocks are the less consolidated Palaeogene clays, sands, gravels and silts of the Lambeth, Thames and Bracklesham Groups which characterise the Hampshire Basin.
The Monarch's Way is a 625-mile (1,006 km) long-distance footpath in England that approximates the escape route taken by King Charles II in 1651 after being defeated in the Battle of Worcester. It runs from Worcester via Bristol and Yeovil to Shoreham, West Sussex.
Beacon Hill is near the village of Burghclere and Watership Down, in north Hampshire. The hill's name is derived from the fact that it was one of many Beacon Hills in England and beyond. This hill was once the site of the most famous beacon in Hampshire. It is 261 metres high and has one of England's most well known hill forts on its slopes, visible from the main A34 road which passes close by. From there, outstanding views of the surrounding area and much of Hampshire may be obtained. The site is open to the public and managed by Hampshire County Council. It is an 80.7-hectare (199-acre) biological Site of Special Scientific Interest called Burghclere Beacon and a Nature Conservation Review site, Grade I.
Twyford is a village and civil parish in Hampshire, England, approximately three miles south of Winchester and near the M3 motorway and Twyford Down. In 2001, the population of the parish was 1,456. The village and parish are on the left bank of the Itchen, which passes through nearby watermeadows, and has been important economically for its residents.
Fair Oak is a large village to the east of the town of Eastleigh in Hampshire, England. Together with the village of Horton Heath, which lies to the south, it is part of the civil parish of Fair Oak and Horton Heath.
Compton and Shawford is a civil parish in the City of Winchester district, immediately southwest of the city, in Hampshire, England. Its main settlements are the villages of Compton and Shawford.
East Hampshire Area of Outstanding Natural Beauty (AONB) in England was designated in 1962. The designation was revoked in March 2010, together with the neighbouring Sussex Downs AONB, upon the establishment of the South Downs National Park. The southern part of the area is mainly rolling chalk downland used for farming that is a westward extension of the Sussex Downs. The north and east includes steep wooded hills and heathland.
Chilcomb is a small village and civil parish in the English county of Hampshire 3 miles (4.8 km) east of Winchester and includes the South Downs Way long-distance footpath.
Upham is a small village and civil parish in the south of England located in Hampshire approximately 7 miles south-east of Winchester.
Warnford is a village and civil parish in the City of Winchester district of Hampshire, England. The parish covers 1283 hectares. The village lies on the A32 in the upper valley of the River Meon between West Meon and Exton. The population in 2019 was estimated at 220. The village is rural in character, with most of the buildings along River Lane, Lippen Lane and Hayden Lane.
St. Catherine's Hill is a chalk downland hill and 43-hectare (110-acre) biological Site of Special Scientific Interest on the outskirts of Winchester in Hampshire, England. It is owned by Winchester College but open to the public. It is managed by Hampshire and Isle of Wight Wildlife Trust, and topped by an Iron Age hillfort, a scheduled monument. In the Black Death, plague pits were dug in the dry valley on the south side of the hill. In the Early modern period, a mizmaze was cut on the hilltop. Winchester College football used to be played on the hill; in an old custom, members of the college assemble on the hill every year, early in the morning.
The Hampshire Basin is a geological basin of Palaeogene age in southern England, underlying parts of Hampshire, the Isle of Wight, Dorset, and Sussex. Like the London Basin to the northeast, it is filled with sands and clays of Paleocene and younger ages and it is surrounded by a broken rim of chalk hills of Cretaceous age.
Henwood Down is one of the highest points in the county of Hampshire, England, and in the South Downs, reaching a height of 201 metres (659 ft) above sea level. Its prominence of 64 metres qualifies it as a Tump.
The Winchester-East Meon Anticline is one of a series of parallel east–west trending folds in the Cretaceous chalk of Hampshire. It lies at the western end of the South Downs, immediately to the north of the Hampshire Basin and south-east of Salisbury Plain.
The Winchester-King's Somborne Syncline is one of a series of parallel east-west trending folds in the Cretaceous chalk of Hampshire. It lies at the western end of the South Downs, immediately to the north of the Winchester-East Meon Anticline and east of Salisbury Plain.
The Stockbridge Anticline is one of a series of parallel east-west trending folds in the Cretaceous chalk of Hampshire. It lies at the western end of the South Downs, immediately to the north of the Winchester-King's Somborne Syncline and east of Salisbury Plain.
The geology of West Sussex in southeast England comprises a succession of sedimentary rocks of Cretaceous age overlain in the south by sediments of Palaeogene age. The sequence of strata from both periods consists of a variety of sandstones, mudstones, siltstones and limestones. These sediments were deposited within the Hampshire and Weald basins. Erosion subsequent to large scale but gentle folding associated with the Alpine Orogeny has resulted in the present outcrop pattern across the county, dominated by the north facing chalk scarp of the South Downs. The bedrock is overlain by a suite of Quaternary deposits of varied origin. Parts of both the bedrock and these superficial deposits have been worked for a variety of minerals for use in construction, industry and agriculture.
The Exmoor Group is a late Devonian to early Carboniferous lithostratigraphic group in southwest England whose outcrop extends from Croyde in north Devon east across Exmoor to Minehead in west Somerset. The group comprises the following formations :
The geology of the South Downs National Park in South East England comprises a gently folded succession of sedimentary rocks from the Cretaceous and early Palaeogene periods overlain in places by a range of superficial deposits from the last 2.6 million years. Whereas the South Downs are formed from the Late Cretaceous age chalk, the South Downs National Park extends into the Weald to the north of the range and thereby includes older rock strata dating from the Early Cretaceous including sandstones and mudstones. The youngest solid rocks are found on the southern fringes of the National Park in the eastern extension of the Hampshire Basin and include sand, silt and clay deposited during the Palaeocene and Eocene epochs.
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