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The North Downs are a ridge of chalk hills in south east Englandmarker that stretch for 120 miles (190 km) from Farnhammarker in Surreymarker to the White Cliffs of Dovermarker in Kentmarker. The North Downs lie within two Areas of Outstanding Natural Beauty (AONBs), the Surrey Hillsmarker and the Kent Downsmarker. The North Downs Waymarker National Trail runs along the North Downs from Farnhammarker to Dovermarker.

Geography

Geology of the South East, Chalk is light green (6)
The narrow spine of the Hog's Backmarker between Farnham and Guildfordmarker forms the western extremity of the North Downs whilst the cliffs between Folkestonemarker and Deal terminate the ridge in the east. There are two distinct aspects, the steep south facing escarpment and the gentle north facing dip slope. The southern boundary is defined by the foot of the escarpment which gives way to the flat, broad clay lands between the Downs and Greensand Ridgemarker known as the Vale of Holmesdalemarker. The northern boundary is less apparent but occurs where the chalk submerges below the more recent Paleocene deposits.

The Downs are highest near the Kent-Surrey border, often reaching heights in excess of 200 metres above sea level at the crest of the escarpment. The highest point is Botley Hillmarker in Surrey at 267 metres (876 ft). The highest point in London, Westerham Heights, is located on the North Downs. East of the Medway Valley the Downs become broader and flatter, extending as far as the Isle of Thanetmarker.

The ridge is intersected by the valleys of a series of rivers: the Weymarker, Mole, Darentmarker, Medway and Stour rivers. These drain much of the Wealdmarker to the south, the western ones are tributaries of the Thames; they carve steep valleys through the chalk and provide natural corridor routes. In addition to existing rivers, the Downs are crossed by a number of wind gap – fossil river valleys no longer occupied by rivers, including those at Farnhammarker, Betchworthmarker, Caterhammarker, Lymingemarker and Hawkingemarker. Except for the river valleys and wind gaps, the crest of the escarpment is almost continuous along its length. The dip slope is dissected by many small dry valleys, and in the broad eastern part in Kent, by further river valleys such as that of the Little Stourmarker. Leith Hillmarker is sometimes incorrectly referred to as part of the North Downs but is located on the parallel Greensand Ridgemarker and does not consist of chalk.

Geology

A cross-section, showing the Wealden Dome, and relating it to the towns of Kent
The Downland of the North Downs consists of distinct lithostratigraphic features (the types of strata, the names of which are always capitalized):

  • The more level tops of the downs are often covered by acidic strata, usually including a layer of Clay-with-Flints, a sandy clay with many flints, or various sands and gravels (note: these are not shown on the geological map and section in this article).


  • The Chalk Formation, composed mostly of chalk (the rock type), a kind of soft fine-grained limestone. It is formed of three parts, the Upper Chalk, which has many flints, the Middle Chalk, with fewer flints, and the Lower Chalk or Coombe Rock, greyish, with few flints. The chalk is most commonly exposed on slopes or as cliffs, where the overlying acidic strata have been quarried or washed away. The buried upper surface of the chalk beneath the acidic strata is often eroded into pipes, gulleys and pinnacles, sometimes visible in road cuttings and quarries.


  • The Upper Greensand Formation, a whitish, limy sandstone, often used for building, for which it has been mined from beneath the chalk (for example from the Godstone Baby Mines). The Upper Greensand of the North Downs is a thin bed of one or two metres thickness, and it is rarely visible at the surface (it is much thicker elsewhere).


The Upper Greensand marks the southern edge of the Downs, being underlain by:

  • The Gault Formation of stiff blue clay.


  • The Lower Greensand Formation of Lower Cretaceous age, containing greensand, a glauconite sand or sandstone, as well as a certain amount of silts, clays, ironstone and limestone.


The topography of the North Downs mainly consists of the Chalk Formation, the rock strata of the Upper Cretaceous period which in certain areas is overlain by superficial deposits of gravels or clay-with-flints.

Citing Dr D. T. Aldiss of the British Geological Survey:

Ecology

The North Downs support several important habitats. The most distinctive of these is chalk grassland which is largely limited to steep escarpment and valley slopes. This semi-natural habitat is maintained through sheep, cattle and rabbit grazing which prevents scrub encroachment. It has been noted that chalk grassland to the west of the Medway Valley is dominated by Upright Brome (Bromus erectus) and Fescue (Festuca) whilst grassland to the east is dominated by Tor-grass (Brachypodium pinnatum). Because of the close proximity of the North Downs to the continent, the warm climate and the south facing escarpment several plant species survive on the chalk grassland which are scarce or not found elsewhere in the British Isles.

The nationally rare Late Spider Orchid (Ophrys fuciflora) is limited within the British Isles to chalk grassland between Folkestonemarker and Wyemarker. One of the two native British sites for the nationally rare Monkey Orchid (Orchis simia) is on the North Downs. The nationally scarce Man Orchid (Orchis anthropophora) is not uncommon on chalk grassland on the downs in Surrey and Kent. Other scarce plant species such as Early Gentian (Gentiana anglica ), Dwarf Milkwort (Polygala amarella) and Bedstraw Broomrape (Orobanche caryophyllacea) also occur on chalk grassland in the North Downs.

Chalk grassland also supports a rich fauna, particularly of insects. Notable butterfly species include Adonis Blue (Lysandra bellargus) and Silver-spotted Skipper (Hesperia comma) which may be found on warm, sheltered, south facing slopes. The chalk downland above the Stour Valley is the only British site for the Black-veined Moth (Siona lineata). Other notable moth species that occur on the North Downs include the Fiery Clearwing Moth (Bembecia chrysidiformis) and Straw Belle Moth (Aspitates gilvaria).

Woodland was far more extensive on the North Downs prior to human clearance 4000 to 5000 years ago. Fragments still remain particularly where the layer of clay with flints overlying the chalk has inhibited clearance. Where this is the case species such as Pedunculate Oak (Quercus robur) predominate although much woodland has been replanted with conifer and Sweet Chestnut (Castanea sativa). In Surrey, there are localised areas of chalk heath where heathland and chalkland plants grow alongside each other.

woodland occurs on thin soils where chalk is close to the surface. These conditions are most often found on the escarpment of the North Downs and on valley slopes but may also occur on the plataeu of the dip slope. Calcaerous woodland is typically dominated by Beech (Fagus), Hornbeam (Carpinus betulus), Yew (Taxus baccata) and Ash (Fraxinus excelsior). Box Hillmarker comprises one of the largest areas of native Box (Buxus sempervirens) woodland in England. One notable species characteristic of calcaerous woodland is the nationally scarce Lady Orchid (Orchis purpurea) which is found in more than 100 sites on the Kent stretch of the North Downs although it is confined to just two sites elsewhere in the UK.

On the summit of the cliffs between Deal and Folkestone the Early Spider Orchid (Ophrys Sphegodes) occurs in large numbers as well as the rare Oxtongue Broomrape (Orobanche artemisae campestris). Naturally exposed chalk is rare inland with the exception of the river cliffs formed by the Mole on the west face of Box Hill and at Ham Bank in Norbury Parkmarker. However, quarry lakes within chalk pits provide habitat for Great Crested Newt (Triturus cristatus). The scarce Musk Orchid (Herminium monorchis) has colonised disused chalk pits near Hollingbournemarker in Kent.

History

The discovery of worked flints and human and animal remains dating from the Lower Paleolithic, approximately 400,000 years ago at Barnfield Pitmarker near Swanscombemarker provides the earliest evidence of human occupation in the North Downs. It is suggested that human activity at this time coincided with intermittent warm phases during the last glacial period and that continuous occupation of the Downs did not occur until warming after the glaciation. Flint axes have also been found on river terraces at Farnham, on Walton and Banstead Heaths and on the crest of the escarpment above Folkestone. There is considerable evidence of Mesolithic activity in the Surrey Downs through the discovery of pit-dwellings at Weston Woods near Alburymarker and the quantity of discarded tools, microliths and other implements discovered .

At about 3000 BC the emergence of Neolithic culture saw the lifestyle of the Mesolithic hunter-gatherer shift to a more sedentary and communal lifestyle that relied upon the keeping of livestock and the growing of crops. There is substantial evidence of Neolithic activity within the North Downs, notably the long barrows concentrated in the Medway and Stour valleys. The Medway long barrowsmarker, which include Kit's Coty Housemarker and Coldrum Stones are constructed of sarsen stone, locally found on Blue Bell Hillmarker and the valleys of the dip slope, whilst the Stour Valley long barrows are constructed of earth.

Agriculture and industry

The landscape of the North Downs has been greatly shaped by man. Deforestation has been an important activity that has taken place on the downs for centuries. Today, the woodland that remains largely exists where deforestation has been inhibited by steep slopes or the layer of clay with flints which is difficult to plough. Because of the many small farms that have survived on the downs, a network of narrow lanes and minor roads has developed. This has resulted in a landscape similar to that found in Normandy known as bocage. The predominant type of farming on the Downs is arable farming and this increased greatly during the twentieth century. Pastoral farming also occurs but to a lesser extent. Human settlements within the downs have generally formed in sheltered valleys and at the foot of scarp slope (known as spring line settlements).

There is plenty of evidence of chalk extraction on the North Downs particularly along the scarp slope. Oil drilling at the foot of the downs occurs in several locations in Surrey. The Kent coalfieldmarker was established in the late 19th century after coal was found in 1890. Four collieries produced a successful output and lasted throughout the 20th century - Betteshanger, Snowdown, Tilmanstonemarker and Chisletmarker. The east to west ridge of the downs has provided a natural transport route for centuries. Much of the historic Pilgrims' Waymarker still survives at the foot of the scarp slope and this has been joined much more recently by the M20 motorway. The scarp slope has also been used for fortification and many examples of this still exist such as Thurnham Castlemarker and on Castle Hill near Folkestonemarker.

Places of interest

Many beauty spots on the North Downs are owned by the National Trust such as Box Hillmarker and Langdon Cliffsmarker. Other areas of interest are Newland's Cornermarker, Wye Downsmarker and the Hog's Backmarker. Much chalk grassland and ancient woodland on the downs is open-access and there are also many historic sites on the downs such as Kit's Coty Housemarker near Maidstone and Dover Castlemarker.

Photo gallery



Image:Wye Downs 1.jpg|The North Downs at the Wye Downsmarker National Nature Reserve.Image:Hollingbourne Downs 1.jpg|The North Downs above Hollingbournemarker.Image:NorthDownsWayStoneSign9948.JPG|A marker on the North Downs Waymarker, Ranscombe Farmmarker, Cuxtonmarker, Medway.Image:BluebellWood9923Ranscombe.JPG| Bluebell at Ranscombe Farmmarker, Cuxtonmarker, Medway.Image:Downs with Cloud 0177.JPG| Looking East, typical downland scenery in the Medway Gap,Ranscombe Farmmarker, Cuxtonmarker, Medway.Image:DownsPoppyCloud.JPG|Looking East, typical downland scenery in the Medway Gap,Ranscombe Farmmarker, Cuxtonmarker, Medway.Image:Dry Valley, Hucking 1.jpg|A dry valley on the dip slope of the North Downs near Huckingmarker.Image:North Downs woodland at Hucking.JPG|Woodland on the North Downs at the Huckingmarker Estate.Image:NorthDownsWayTrail.jpg|Typical chalk downland trail near Hollingbournemarker.Image:North Downs Way.jpg|A modern metal trail marker near Harrietshammarker.Image:WealdfromDowns.JPG|A view South across the Kent Weald from the North Downs Way near Detlingmarker.


See also



References

  1. Gallois RW and Edmunds FH (1965) British Regional Geology: The Wealden District (4th Ed.) published by the Natural Environment Research Council: Institute of Geological Sciences


External links




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