The Quantock Hills west of Bridgwater in Somerset, England, consist of heathland, oak woodlands, ancient parklands and agricultural land. They were England's first Area of Outstanding Natural Beauty, designated in 1956.[1]
Archaeological landscape features include Bronze Ageround barrows, extensive ancient field systems and Iron Age hill forts. Romansilver coins have been discovered in West Bagborough. The hills are popular with walkers, mountain bikers, horse riders and tourists who explore paths such as the Coleridge Way.
Etymology
The name first appears in Saxon charters in around AD 880 as Cantuctun and two centuries later in the Domesday Book as Cantoctona and Cantetone. The name means settlement by a rim or circle of hills;[5]Cantuc is Celtic for a rim or circle, and -ton or -tun is Old English for a settlement. The highest point of the hills is called Will's Neck meaning ridge of the Welshman, probably referring to a time when the hills marked the boundary between the expanding Saxon kingdom of Wessex and the lands of the Britons or 'Welsh' to the West. A battle was fought locally at that time.[3]
Geology
Beach at Quantock's Head. The wave cut platform is visible at low tide below the short "cliff" exposing the rock strata.
The Quantock Hills are largely formed by rocks of the Devonian period, which consist of sediments originally laid down under a shallow sea and slowly compressed into solid rock. In the higher north-western areas older Early Devonian rocks known as Hangman Grits (or, more formally, the Hangman Sandstone Formation) predominate[5] and can be seen in the exposed rock at West Quantoxhead quarry, which was worked for road building.[6] The Hangman Grits are described in three divisions: the lowest are the Little Quantock Beds, which are located near Crowcombe, and made up of siltstones and slates. Between Triscombe and West Quantoxhead is a layer of the Triscombe Beds which is around 500 metres (1,600 ft) thick and is made up of green sandstone and mudstones. The uppermost division is the Hodders Combe Beds of sandstone and conglomerate and is approximately 300 metres (980 ft) thick.[7]
Further south there are newer Middle and Late Devonian rocks, known as Ilfracombe beds and Morte Slates.[6] These include sandstone and limestone, which have been quarried near Aisholt. At Great Holwell, south of Aisholt, is the only limestone cave in the Devonian limestone of North Devon and West Somerset.[6] The lower fringes around the hills are composed of younger New Red Sandstone rocks of the Triassic period.[8] These rocks were laid down in a shallow sea and often contain irregular masses or veins of gypsum, which was mined on the foreshore at Watchet.[6]
Kilve has the remains of a red-brick retort built in 1924 after the shale in the cliffs was found to be rich in oil. Along this coast, the cliffs are layered with compressed strata of oil-bearing shale and blue, yellow and brown Lias embedded with fossils. The Shaline Company was founded in 1924 to exploit these strata but was unable to raise sufficient capital. The company's retort house is thought to be the first structure erected here for the conversion of shale to oil and is all that remains of the anticipated Somerset oil boom.[9]
At Blue Anchor the coloured alabaster found in the cliffs gave rise to the name of the colour "Watchet Blue".[3] The village has the only updraught brick kiln known to have survived in Somerset. It was built around 1830 and was supplied by small vessels carrying limestone to the small landing jetty.[10] Now used as a garage, the kiln is thought to have operated until the 1870s, when the large-scale production of bricks in Bridgwater rendered small brickyards uneconomic.[11]
Cockercombe tuff is a greenish-grey, hard pyroclastic rock formed by the compression of volcanic ash and is found almost exclusively in the south-eastern end of the Quantock Hills.
Climate
Aerial view of the Quantock Hills
Along with the rest of South West England, the Quantock Hills has a temperate climate that is generally wetter and milder than the rest of England. The mean temperature is approximately 10 °C (50 °F) and shows a seasonal and a diurnal variation, but because of the modifying effect of the sea the range is less than in most other parts of the United Kingdom. January is the coldest month with mean minimum temperatures between 1 °C (34 °F) and 2 °C (36 °F). July and August are the warmest months, with mean daily maxima around 21 °C (70 °F). December is normally the most cloudy month and June the sunniest. High pressure over the Azores often brings clear skies to south-west England, particularly in summer.
Cloud often forms inland especially near hills, and acts to reduce sunshine. The average annual sunshine totals around 1,600 hours. Rainfall tends to be associated with Atlantic depressions or with convection. In summer, convection caused by solar surface heating sometimes forms shower clouds, and a large proportion of rain falls from showers and thunderstorms at this time of year. Average rainfall is around 31 to 35 inches (790 to 890 mm). About 8 to 15 days of snowfall is typical. From November to March, mean wind speeds are highest; winds are lightest from June to August. The predominant wind direction is from the south-west.[12]
The Northern Flank of Beacon Hill (Quantocks). In late summer the northern Quantocks are ablaze with heather and gorse. Minehead can be seen in the distance.
The hilltops are covered in heathland of gorse, heather, bracken and thorn with plantations of conifer. The western side of the Quantocks are steep scarp slopes of pasture, woods and parkland. Deep stream-cut combes to the north-east contain extensive oak-woods with small flower-rich bogs above them. The areas where there is limited drainage are dominated by heather (Calluna vulgaris), with significant populations of cross-leaved heath (Erica tetralix), purple moor-grass (Molinia caerulea), bilberry (Vaccinium myrtillus) and wavy hair-grass (Deschampsia flexuosa). Drier areas are covered with bell heather (Erica cinerea), western gorse (Ulex gallii) and bristle bent (Agrostis curtisii), while bracken (Pteridium aquilinum) is common on well-drained deeper soils. The springs and streams provide a specialist environment that supports bog pimpernel (Anagallis tenella). The woodland is generally birch/sessile oak woodland, valley alder woodland and ash/wych elm woodland, which support a rich lichen flora. Alfoxton Wood is one of only three British locations where the lichen Tomasellia lectea is present.[4]
Fauna
The various habitats, together with the wide range of slopes and aspects, provide ideal conditions
for a rich fauna. Amphibians including the palmate newt (Triturus helveticus), common frog (Rana temporaris), and common toad (Bufo bufo) are represented in the damper environments. Reptiles
present include adder (Vipera berus), grass snake (Natrix natrix), slowworm (Anguis fragilis) and common lizard (Lacerta vivipara). Many bird species breed on the Quantocks, including the grasshopper warbler (Locustella naevia), nightjar (Caprimulgus europaeus), raven (Corvus corax) and the European pied flycatcher (Ficedula hypoleuca). The Quantocks are also an important site for red deer (Cervus elaphus). Invertebrates of note include the silver-washed fritillary butterfly (Argynnis paphia), and three nationally rare dead-wood beetles: Thymalus limbatus, Orchesia undulata and Rhinosimus ruficollis.[4]
Iron Age sites in the Quantocks include major hill forts at Dowsborough and Ruborough, as well as several smaller earthwork enclosures, such as Trendle Ring and Plainsfield Camp. Ruborough near Broomfield is on an easterly spur from the main Quantock ridge, with steep natural slopes to the north and south east. The fort is triangular in shape, with a single rampart and ditch (univallate), enclosing 4 acres (1.6 ha). A linear outer work about 131 yards (120 m) away, parallel to the westerly rampart, encloses another 4 acres (16,000 m2). The name Ruborough comes from Rugan beorh or Ruwan-beorge meaning Rough Hill.[14] The Dowsborough fort has an oval shape, with a single rampart and ditch (univallate) following the contours of the hill top, enclosing an area of 7 acres (2.8 ha). The main entrance is to the east, towards Nether Stowey, with a simpler opening to the north west, aligned with a ridgeway leading down to Holford. A col to the south connects the hill to the main Stowey ridge, where a linear earthwork known as Dead Woman's Ditch cuts across the spur.[15]
Little evidence exists of Roman influence on the Quantock region beyond isolated finds and hints of transient forts. A Roman port was at Combwich, and it is possible that a Roman road ran from there to the Quantocks, because the names Nether Stowey and Over Stowey come from the Old English stan wey, meaning stone way.[3] In October 2001 the West Bagborough Hoard of 4th-century Romansilver was discovered in West Bagborough. The 681 coins included two denarii from the early 2nd century, and eight miliarense and 671 siliqua dating to 337–367 AD. The majority were struck in the reigns of emperors Constantius II and Julian and derive from a range of mints including Arles and Lyons in France, Trier in Germany and Rome.[16]
Dark Ages and Anglo-Saxon
The area remained under Romano-British Celtic control until 681–685 AD, when Centwine of Wessex pushed west from the River Parrett, conquered the Welsh King Cadwaladr, and occupied the rest of Somerset north to the Bristol Channel.[17]
Saxon rule was later consolidated under King Ine, who established a fort at Taunton in about 700 AD.[18]
The first documentary evidence of the village of Crowcombe is by Æthelwulf of Wessex in 854, where it was spelt 'Cerawicombe'.[19] At that time the manor belonged to Glastonbury Abbey.[20] In the later Saxon period, King Alfred led the resistance to Viking invasion from Athelney, south-east of the Quantocks.[6] According to the Anglo-Saxon Chronicle, the early port at Watchet was plundered by Danes in 987 and 997.[21] Alfred established a series of forts and lookout posts linked by a military road, or herepath, so his army could cover Viking movements at sea. The herepath has a characteristic form that is familiar on the Quantocks: a regulation 66-foot (20 m) wide track between avenues of trees growing from hedge laying embankments. The herepath ran from the ford on the River Parrett at Combwich, past Cannington hill fort to Over Stowey, where it climbed the Quantocks along the line of the current Stowey road, to Crowcombe Park Gate. Then it went south along the ridge, to Triscombe Stone. One branch may have led past Lydeard Hill and Buncombe Hill, back to Alfred's base at Athelney. The main branch descended the hills at Triscombe, then along the avenue to Red Post Cross, and west to the Brendon Hills and Exmoor.[22] There is some evidence that an area of the hills known as Quantock Common may have been a Saxon Royal Forest.[23]
Stowey Castle at Nether Stowey was built in the 11th century. The castle is sited on a small isolated knoll, about 390 ft (119 m) high. It consisted of a square keep (which may have been stone, or a wooden superstructure on stone foundations) and its defences and an outer and an inner bailey.[24] The mount is 29 ft (9 m) above the 6 ft (2 m) wide ditch which itself is 7 ft (2 m) deep. The motte has a flat top with two large and two small mounds, which may be sites of towers, at the edge.[25] The Blue Lias rubble walling is the only visible structural remains of the castle, which stand on a conical earthwork with a ditch approximately 820 ft (250 m) in circumference.[26] The castle was destroyed in the 15th century, which may have been as a penalty for the local Lord Audley's involvement in the Second Cornish Uprising of 1497 led by Perkin Warbeck against the taxes of Henry VII.[27] Some of the stone was used in the building of Stowey Court in the village.[6]
At the end of the Monmouth Rebellion of 1685, (also known as the Pitchfork Rebellion), many participants were executed in the Quantocks. The rebellion was an attempt to overthrow the King of England, James II, who became king when his elder brother, Charles II, died on 6 February 1685. James II was unpopular because he was Roman Catholic, and many people were opposed to a "papist" king. James Scott, 1st Duke of Monmouth, claimed to be rightful heir to the throne and attempted to displace James II.[29] The rebellion ended with the defeat of Monmouth's forces at the Battle of Sedgemoor on 6 July 1685. Monmouth was executed for treason on 15 July,[29] and many of his supporters were executed, including some by hanging at Nether Stowey and Cothelstone,[6] or transported in the Bloody Assizes of Judge Jeffreys.
Dodington was the site of the Buckingham Mine where copper was extracted.[30] The mine was established before 1725 and followed earlier exploration at Perry Hill, East Quantoxhead. It was financed by the Marquis of Buckingham until 1801 when it was closed, until various attempts were made to reopen it during the 19th century.[31]
In 1724 the 14th century spire of the Church of the Holy Ghost in Crowcombe was damaged by a lightning strike. The top section of the spire was removed and is now planted in the churchyard,[32] and stone from the spire was used in the flooring of the church. Inside the church, carved bench-ends dating from 1534[33] depict such pagan subjects as the Green Man and the legend of the men of Crowcombe fighting a two-headed dragon.[34]
Norton Fitzwarren was the site of a boat lift on the now unused section of the Grand Western Canal from 1839 to 1867. A 300-person prisoner of war camp built here during World War II housed Italian prisoners from the Western Desert Campaign and German prisoners from the Battle of Normandy.
Walking routes
Poet Samuel Taylor Coleridge lived in Nether Stowey in the Quantocks from 1797 to 1799. In his memory a footpath, The Coleridge Way, was set up by the Exmoor park authorities. The 36-mile (58 km) route begins in Nether Stowey and crosses the Quantocks, the Brendon Hills and Exmoor before finishing in Porlock.[35]
The Quantock Greenway is a footpath that opened in 2001. The route of the path follows a figure of eight centred on Triscombe. The northern loop, taking in Crowcombe and Holford, is 19 miles (31 km) long, and the southern loop to Broomfield extends for 18 miles (29 km). The path travels through many types of landscape, including deciduous and coniferous woodland, private parkland, grazed pasture and cropped fields.[36]
The film Pandaemonium (2000), based on the lives of Wordsworth and Coleridge, much of it filmed on the hills.[39]
Literature
The poet Samuel Taylor Coleridge lived here for three years from 1797, while he wrote The Rime of the Ancient Mariner (written in 1797–98 and published in 1798), part of Christabel (the first part was reputedly written in 1797, and the second in 1800), Frost at Midnight, and Kubla Khan (completed in 1797 and published in 1816).[40]
Virginia and Leonard Woolf spent a few days of their honeymoon at The Plough Inn, Holford, before continuing to the continent in 1912. They returned about a year later to try to help Virginia recover from one of her recurring nervous breakdowns.[45]
In the 1980s and 1990s, English novelist Ruth Elwin Harris wrote her Quantock Quartet, a set of novels centred on four sisters growing up around the Quantock Hills during the early 20th century.
The Doctor Who serial Shada (1980) makes a sidelong reference to this region – the Fourth Doctor (played by Tom Baker) claims that walking through the Time Vortex "is a little trick I learned from a space-time mystic in the Quantocks".[50]
The Quantocks are the setting for the final episodes of the third and eighth series (2005 and 2012) of Peep Show, which are titled "Quantocking" and "Quantocking II"[51][52]
Cultural attractions and places of interest
A series of concerts called Music on the Quantocks takes place each year in Quantock villages. Headlining acts have included Sir James Galway, guitarist John Williams and choral groups The Sixteen, The Tallis Scholars and the Gabrieli Consort. The concerts are run by volunteers.
One of the most popular Coleridge Cottage is a cottage situated in Nether Stowey. It was constructed in the 17th century as a building containing a parlour, kitchen and service room on the ground floor and three corresponding bed chambers above.[53] It has been designated by English Heritage as a grade II* listed building.[54] Having served for many years as Moore's Coleridge Cottage Inn, the building was acquired for the nation in 1908, and the following year it was handed over to the National Trust.[55] On 23 May 1998, following a £25,000 appeal by the Friends of Coleridge and the National Trust, two further rooms on the first floor were opened.[56]
At Aley is Quantock Lodge, a green-grey 19th-century mansion built from cockercombe tuff. It was the family home of Henry Labouchere, 1st Baron Taunton, until the 1960s when it was converted into a school. In 2000, it became a centre for recreation and banqueting and summer camps for youths.
Broomfield is home to Fyne Court. Once the home of pioneer 19th century electrician, Andrew Crosse. Since 1972 it has been owned by the National Trust. The Quantock Hills National Landscape Service have their headquarters at Fyne Court.
The Church of St Mary in Kingston St Mary dates from the 13th century, but the tower is from the early 16th century and was re-roofed in 1952, with further restoration from 1976 to 1978. It is a three-stage crenellated tower, with crocketed pinnacles, bracketed pinnacles set at angles, decorative pierced merlons, and set-back buttresses crowned with pinnacles.[57] The decorative "hunky-punks" are perched high on the corners. These may be so named because the carvings are hunkering (squatting) and are "punch" (short and thick). They serve no function, unlike gargoyles that carry off water.[58] The churchyard includes tombs of the Warre family who owned nearby Hestercombe House,[6] a historic country house in Cheddon Fitzpaine visited by about 70,000 people per year. The site includes a 0.2-acre (810 m2) biological Site of Special Scientific Interest notified in 2000. The site is used for roosting by Lesser horseshoe bats,[59] and has been designated as a Special Area of Conservation (SAC).[60] The house was used as the headquarters of the British 8th Corps[61] during the Second World War, and has been owned by Somerset County Council since 1951. It is used as an administrative centre and a base for the Somerset Fire and Rescue Service.
Bishops Lydeard station. The locomotive is Great Western 2-8-0T tank no. 5224.
The West Somerset Railway (WSR) is a heritage railway that runs along the edge of the Quantock Hills between Bishops Lydeard and Watchet. The line then turns inland to Washford, and returns to the coast for the run to Minehead. At 23 miles (37 km), it is the longest privately owned passenger rail line in the UK.[63]
Halsway Manor in Halsway, is now used as England's National Centre for Traditional Music, Dance and Song. It is the only residential folk centre in the UK. The eastern end of the building dates from the 15th century and the western end was a 19th-century addition.[64] The manor, which is mentioned in the Domesday Book, was at one time used by Cardinal Beaufort as a hunting lodge and thereafter as a family home until the mid-1960s[65] when it became the folk music centre. It has been designated by English Heritage as a grade II* listed building.[66]
Halswell House in Goathurst has Tudor origins but was purchased by the Tynte family and rebuilt in 1689.[6] The surrounding park and 17 acres (6.9 ha) pleasure garden was developed between 1745 and 1785. The grounds contain many fish ponds, cascades, bridges and fanciful buildings,[67] including the Temple of Harmony, which stands in Mill Wood[68] and has now been fully restored.
^A P Baggs and M C Siraut, 'Aisholt', in A History of the County of Somerset: Volume 6, andersfield, Cannington, and North Petherton Hundreds (Bridgwater and Neighbouring Parishes), ed. R W Dunning and C R Elrington (London, 1992), pp. 68-69 http://www.british-history.ac.uk/vch/som/vol6/pp68-69 [accessed 17 May 2015].
