Downland
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A downland is an area of open chalk upland. This term is especially used to describe the chalk countryside in southern England. Areas of downland are often referred to as Downs.
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Formation of downland
Downland is formed when chalk formations are raised above the surrounding rocks. The chalk slowly erodes to form characteristic rolling hills and valleys. Chalk downland formations typically have a marked scarp slope on one side, which is very steep, and a dip slope on the other, which is much shallower. Where the downs meet the sea, characteristic white chalk cliffs can be formed, such as the White cliffs of Dover.
Hydrology
Chalk deposits are very porous, so the height of the water table in chalk hills rises in winter and falls in summer. This leads to characteristic chalk downland features such as dry valleys or coombes, and seasonally-flowing streams or winterbournes. In the valleys below the downs there is typically a clay soil, and at the interface between the two a springline can occur where water emerges from the porous chalk. Along this line settlements and farms were often built, as on the higher land no water was available. In many chalk downland areas there is no surface water at all other than artificially created dewponds.
Downland soil
The soil profile of chalk downland in England is a thin soil overlaying the parent chalk. Weathering of the chalk has created a characteristic soil known as rendzina. Unlike many soils in which there are easily distinguished layers or horizons, a chalk rendzina soil consists of only a shallow dark humus rich surface layer which grades through a lighter brown hillwash containing small pellets of chalk, to the white of the chalk itself. This is largely because of the purity of the chalk which is here about 98% calcium carbonate and the consequent absence of soil-building clay minerals which are abundant, for example, in valley floors.
Steep slopes on chalk downland develop a ribbed pattern of grass covered horizontal steps a foot or two high. Although subsequently emphasised by cattle and sheep walking along them, these terracettes (commonly known as sheep tracks) were formed by the movement of soil downhill, a process known as soil creep.
Downland habitat
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Examples of downland
The Southern England Chalk Formation
- Berkshire Downs
- Chiltern Hills (Dunstable Downs)
- Cranborne Chase
- Dorset Downs (Hambledon Hill, Hodd Hill, Maiden Castle, Cerne Abbas Giant)
- Isle of Wight (The Needles, Culver Down)
- North Downs (White cliffs of Dover)
- Purbeck Hills (Ballard Down, Lulworth Cove, Old Harry Rocks, White Nothe)
- Salisbury Plain
- South Downs (Beachy Head, Eastbourne, Seven Sisters, Watership Down)
United States
- Austin Chalk formation, which underlies much of central Texas
External links
- Seven Sisters cliffs (http://www.sevensisters.org.uk/)
- Seven Sisters (http://www.roger.beckwith.btinternet.co.uk/Sussex/SevenSisters.htm)
- South Downs Virtual Information Centre (http://www.vic.org.uk)
References
- UK Lowland calcereous grassland habitat action plan (http://www.ukbap.org.uk/UKPlans.aspx?ID=12#1)