There are two hills in Hampshire called Beacon Hill; the other one is near Burghclere
Beacon Hill, Warnford
Site of Special Scientific Interest
LocationHampshire
Grid referenceSU 603 227[1]
InterestBiological
Area46.4 hectares (115 acres)[1]
Notification1984[1]
Location mapMagic 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]

Location

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]

Site of Special Scientific Interest

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]

Geology

Structure

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]

Geomorphology

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.

References

  1. 1 2 3 4 5 "Designated Sites View: Beacon Hill, Warnford". Sites of Special Scientific Interest. Natural England. Retrieved 3 May 2020.
  2. ↑ "Map of Beacon Hill, Warnford". Sites of Special Scientific Interest. Natural England. Retrieved 3 May 2020.
  3. ↑ "Designated Sites View: Beacon Hill". National Nature Reserves. Natural England. Retrieved 21 April 2020.
  4. ↑ "Round barrow cemetery and hollow ways on Beacon Hill". Historic England. Retrieved 21 April 2020.
  5. ↑ "South Downs Way Public Inquiry 2004". Countryside Agency. Archived from the original on 7 January 2009. Retrieved 1 April 2008.
  6. ↑ "South Downs Way - Latest news on the route across the Meon Valley". Natural England. Archived from the original on 21 October 2007. Retrieved 1 April 2008.
  7. ↑ English Nature SSSI citation sheet for this site Archived September 26, 2007, at the Wayback Machine
  8. ↑ British Geological Survey (1998), England and Wales Sheet 316 Fareham, Solid and drift edition, 1:50,000 scale geological map, Keyworth, Nottingham: British Geological Survey, ISBN 0-7518-3168-9
  9. ↑ British Geological Survey (1999), England and Wales Sheet 300 Alresford, Solid and drift edition, 1:50,000 scale geological map, Keyworth, Nottingham: British Geological Survey, ISBN 0-7518-3340-1
  10. ↑ British Geological Survey (2002), England and Wales Sheet 299 Winchester, Solid and drift edition, 1:50,000 scale geological map, Keyworth, Nottingham: British Geological Survey, ISBN 0-7518-3250-2
  11. ↑ Small, R.J. (1980),The Tertiary geomorphological evolution of south-east England:an alternative interpretation,in Jones D.K.C (ed), The Shaping of Southern England, Institute of British Geographers Special Publication 11, Academic Press, 1980, ISBN 0-12-388950-2

51°00′02″N 1°08′23″W / 51.000431°N 1.139844°W / 51.000431; -1.139844

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