The granite which forms the uplands dates from the Carboniferous Period of geological history. The landscape consists of moorland capped with many exposed granite hilltops known as tors, providing habitats for Dartmoor wildlife. The highest point is High Willhays, 621 m (2,037 ft) above sea level. The entire area is rich in antiquities and archaeology.
Parts of Dartmoor have been used as military firing ranges for over 200 years. The public is granted extensive land access rights on Dartmoor (including restricted access to the firing ranges) and it is a popular tourist destination.
IUCN category V (protected landscape/seascape)
View down the River Meavy towards Leather Tor and Sharpitor
|Location||Devon, England, United Kingdom|
|Area||954 km2 (368 sq mi)|
|Governing body||Dartmoor National Park Authority|
Dartmoor includes the largest area of granite in Britain, with about 625 km2 (241 sq mi) at the surface, though most of it is under superficial peat deposits. The granite (or more specifically adamellite) was intruded at depth as a pluton into the surrounding sedimentary rocks during the Carboniferous period, probably about 309 million years ago. It is generally accepted that the present surface is not far below the original top of the pluton; evidence for this includes partly digested shale xenoliths, contamination of the granite and the existence of two patches of altered sedimentary rock on top of the granite. A considerable gravity anomaly is associated with the Dartmoor pluton as with other such plutons. Measurement of the anomaly has helped to determine the likely shape and extent of the rock mass at depth.
Dartmoor is known for its tors – hills topped with outcrops of bedrock, which in granite country such as this are usually rounded boulder-like formations. More than 160 of the hills of Dartmoor have the word tor in their name but quite a number do not. However, this does not appear to relate to whether or not there is an outcrop of rock on their summit. The tors are the focus of an annual event known as the Ten Tors Challenge, when around 2400 people aged between 14 and 19 walk for distances of 56, 72 or 88 km (35, 45 or 55 mi) between ten tors on many differing routes.
The highest points on Dartmoor are on the northern moor: High Willhays, 621 m (2,037 ft), (grid reference ) and Yes Tor, 619 m (2,031 ft), (grid reference ) The highest points on the southern moor are Ryder's Hill, 515 m (1,690 ft), (grid reference ), Snowdon 495 m (1,624 ft), (grid reference ), and an unnamed point, 493 m (1,617 ft) at (grid reference ), between Langcombe Hill and Shell Top. The best-known tor on Dartmoor is Haytor (called Hey Tor by William Crossing), 457 m (1,499 ft), (grid reference ). For a more complete list see List of Dartmoor tors and hills.
The high ground of Dartmoor forms the catchment area for many of Devon's rivers. As well as shaping the landscape, these have traditionally provided a source of power for moor industries such as tin mining and quarrying.
The moor takes its name from the River Dart, which starts as the East Dart and West Dart and then becomes a single river at Dartmeet. It leaves the moor at Buckfastleigh, flowing through Totnes below where it opens up into a long ria, reaching the sea at Dartmouth.
For a full list, expand the Rivers of Dartmoor navigational box at the bottom of this page.
Much more rain falls on Dartmoor than in the surrounding lowlands. As much of the national park is covered in thick layers of peat (decaying vegetation), the rain is usually absorbed quickly and distributed slowly, so the moor is rarely dry. In areas where water accumulates, dangerous bogs or mires can result. Some of these, topped with bright green moss, are known to locals as "feather beds" or "quakers", because they can shift (or 'quake') beneath a person's feet. Quakers result from sphagnum moss growing over the water that accumulates in the hollows in the granite.
The vegetation of the bogs depends on the type and location. Blanket bog, which forms on the highest land where the rainfall exceeds 2,000 millimetres (79 in) a year, consists mainly of cotton-grass (Eriophorum species), sedges (Carex and Rhynchospora), Bog Asphodel and Common Tormentil, with Sphagnum thriving in the wettest patches. The valley bogs have lush growth of rushes, with sphagnum, cross-leaved heath, sundews and several other species.
Some of the bogs on Dartmoor have achieved notoriety. Fox Tor Mires was supposedly the inspiration for Great Grimpen Mire in Conan Doyle's novel The Hound of the Baskervilles, although there is a waymarked footpath across it. Sabine Baring-Gould, in his Book of Dartmoor (1900) related the story of a man who was making his way through Aune Mire at the head of the River Avon when he came upon a top-hat brim down on the surface of the mire. He kicked it, whereupon a voice called out: "What be you a-doin' to my 'at?" The man replied, "Be there now a chap under'n?" "Ees, I reckon," was the reply, "and a hoss under me likewise."
Along with the rest of South West England, Dartmoor has a temperate climate which is generally wetter and milder than locations at similar height in the rest of England. At Princetown, near the centre of the moor at a height of 453 metres (1,486 ft), January and February are the coldest months with mean minimum temperatures around 1 °C (34 °F). July and August are the warmest months with mean daily maxima not reaching 18 °C (64 °F). Compared with Teignmouth, which is on the coast about 22 miles (35 km) to the east, the average maximum and minimum temperatures are 3.0 °C (5.4 °F) and 2.6 °C (4.7 °F) lower respectively, and frost is at least five times as frequent. On the highest ground, in the north of the moor, the growing season is less than 175 days – this contrasts with some 300 days along most of the south coast of the county.
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 rainfall falls from showers and thunderstorms at this time of year. The wettest months are November and December and on the highest parts of the moor the average annual total rainfall is over 2,000 millimetres (79 in). This compares with less than 800 millimetres (31 in) in the lower land to the east around the Exe Estuary, which is in the rain shadow of the moor. Due to the influence of the Gulf Stream snowfall is not common, though due to its high altitude it is more vulnerable to snowfall than surrounding regions.
Between 1961 and 1990 Met Office data shows that there was an average of 20 days when snow fell on the moor, and over 40 days a year with hail, which is as high as anywhere else in the country. This results when cold polar maritime air that has travelled over a large expanse of warmer ocean is forced to rise over high country.
When average temperatures at Princetown between 1961 and 2000 are compared, the average annual temperature in the decade 1990–2000 was up by 0.2 °C (0.4 °F) and the late winter temperature increased by 0.5 °C (0.9 °F).
Because of Dartmoor's height and granite geology, it experiences strong winds and has acidic soils. In consequence it has been subject to very little intensive farming, and all these factors combine to form the basis of the important ecosystems found here. The landscape is one of granite with peat bogs overlying it. While the moors topped with granite tors are the most iconic part of Dartmoor's landscape, only about half of Dartmoor is actually moorland. Equally important for wildlife are the blanket bogs, upland heaths and the oak woodlands which are all of global importance. Dartmoor is a Special Area of Conservation (SAC) with four habitats (Northern Atlantic wet heaths with Erica tetralix; European dry heaths; Blanket bogs and Old sessile oak woods with Ilex and Blechnum in the British Isles) being listed as primary reasons for the selection of Dartmoor as a SAC. In addition the area has a population of the Southern damselfly which is also a primary reason for its selection along with populations of Atlantic salmon and Otter being qualifying reasons.
Wistman's Wood is one of the old sessile oak woods which contribute to the listing of Dartmoor as a SAC and is possibly a surviving fragment from the earliest Neolithic woodland clearances. It is home to exceptional epiphytic mosses, liverworts and lichens. Nearly 50 species of moss and liverwort are found in the wood along with 120 types of lichen, including Smith's horsehair lichen, speckled sea-storm lichen and pendulous wing-moss. Over 60 species of lichens grow on the exposed surfaces of the granite tors, including granite-speck rim-lichen, purple rock lichen, brown cobblestone lichen and goldspot lichen and many rare lichen grow on rocks exposed by mining which are rich in heavy metals. On the upland heaths heather (ling) and bell heather are common along with western gorse. In dry grassy areas tormentil, heath bedstraw and heath milkwort are all common. Cross-leaved heath and purple moor grass grow in wetter spots and in the boggy areas many different species of sphagnum and other mosses can be found along with liverworts, Hare's-tail Cotton-grass, round-leaved sundew and bog asphodel and in the valley bottoms, many different sedges, bogbean and pale butterwort all grow.
A large variety of bird species can be found on Dartmoor including ones that have declined elsewhere in the UK, such as skylark and snipe, or are even rare nationally, such as the ring ouzel and the cuckoo. There are internationally important populations of meadow pipit and stonechat. Woodland birds include a number of migrant species, like the pied flycatcher, the wood warbler or the common redstart. Mammals found here include otters, hazel dormice and nearly all of the UK's 16 bat species. Three rare species, the barbastelle, and the greater and lesser horseshoe bats are of particular importance. The upper reaches of the rivers, are spawning grounds for Salmon and trout and Palmate newts, frogs and toads breed in the numerous small pools. Two shrimp species can be found on Dartmoor: fairy shrimp that can be found in temporary pools and in underground streams very rare cave shrimp. The world's largest land slug, the Ash black, is also found. Reptiles include common lizards and adders. The farmland in the wet valleys around the edge of the moors is the most important habitat for insects including the marsh fritillary butterfly, southern damselfly, narrow-bordered bee hawkmoth and bog hoverfly. Areas of bracken are home to the high brown fritillary and pearl-bordered fritillary. Insects found in the heathlands include the emperor moth, green hairstreak and the bilberry bumblebee. The old oak woodlands have a distinctive group of insects including the blue ground beetle and Heckford's pygmy moth, a species found nowhere else in the world.
The majority of the prehistoric remains on Dartmoor date back to the late Neolithic and early Bronze Age. Indeed, Dartmoor contains the largest concentration of Bronze Age remains in the United Kingdom, which suggests that this was when a larger population moved onto the hills of Dartmoor. The large systems of Bronze Age fields, divided by reaves, cover an area of over 10,000 hectares (39 sq mi) of the lower moors.
The climate at the time was warmer than today, and much of today's moorland was covered with trees. The prehistoric settlers began clearing the forest, and established the first farming communities. Fire was the main method of clearing land, creating pasture and swidden types of fire-fallow farmland. Areas less suited for farming tended to be burned for livestock grazing. Over the centuries these Neolithic practices greatly expanded the upland moors, and contributed to the acidification of the soil and the accumulation of peat and bogs.
After a few thousand years the mild climate deteriorated leaving these areas uninhabited and consequently relatively undisturbed to the present day. The highly acidic soil has ensured that no organic remains have survived, but the durability of the granite has meant that the remains of buildings, enclosures and monuments have survived well, as have flint tools. A number of remains were "restored" by enthusiastic Victorians and that, in some cases, they have placed their own interpretation on how an area may have looked.
Numerous prehistoric menhirs (more usually referred to locally as standing stones or longstones), stone circles, kistvaens, cairns and stone rows are to be found on the moor. The most significant sites include:
There are also an estimated 5,000 hut circles still surviving although many have been raided over the centuries by the builders of the traditional dry stone walls. These are the remnants of Bronze Age houses. The smallest are around 1.8 m (6 ft) in diameter, and the largest may be up to five times this size.
Some have L-shaped porches to protect against wind and rain; some particularly good examples are to be found at Grimspound. It is believed that they would have had a conical roof, supported by timbers and covered in turf or thatch.
There are also numerous kistvaens, Neolithic stone box-like tombs.
The climate became wetter and cooler over the course of a thousand years from around 1000 BC, resulting in much of high Dartmoor being largely abandoned by its early inhabitants.
It was not until the early Mediaeval period that the weather again became warmer, and settlers moved back onto the moors. Like their ancient forebears, they also used the natural granite to build their homes, preferring a style known as the longhouse — some of which are still inhabited today, although they have been clearly adapted over the centuries. Many are now being used as farm buildings, while others were abandoned and fell into ruin.
The earliest surviving farms, still in operation today, are known as the Ancient Tenements. Most of these date back to the 14th century and sometimes earlier.
Some way into the moor stands the town of Princetown, the site of Dartmoor Prison, which was originally built by Isbell Rowe & Company, Plymouth, for prisoners of war from the Napoleonic Wars and the War of 1812. The prison has an incorrect reputation for being escape-proof, due to both the buildings themselves and its physical location.
The Dartmoor landscape is scattered with the marks left by the many generations who have lived and worked there over the centuries – such as the remains of the Dartmoor tin-mining industry, and farmhouses long since abandoned. Indeed, the industrial archaeology of Dartmoor is a subject in its own right.
Dartmoor is known for its myths and legends. It is reputedly the haunt of pixies, a headless horseman, a mysterious pack of "spectral hounds", and a large black dog, among others. During the Great Thunderstorm of 1638, the moorland village of Widecombe-in-the-Moor was even said to have been visited by the Devil.
Many landmarks have ancient legends and ghost stories associated with them, such as the allegedly haunted Jay's Grave, the ancient burial site of Childe's Tomb, the rock pile called Bowerman's Nose, and the stone crosses that mark former mediaeval routes across the moor.
Dartmoor has inspired a number of artists and writers, such as Sir Arthur Conan Doyle in The Hound of the Baskervilles and The Adventure of Silver Blaze, R. D. Blackmore, Eden Phillpotts, Beatrice Chase, Agatha Christie, Rosamunde Pilcher, and the Reverend Sabine Baring-Gould. In Harry Potter and the Goblet of Fire, the fictional 1994 Quidditch World Cup final between Ireland and Bulgaria was hosted on the moor. In 1820, the newly formed Royal Society of Literature offered a prize for a poem on the subject of Dartmoor, this being won by Felicia Hemans.
Over half of Dartmoor National Park (57.3%) is private land; the Forest of Dartmoor being the major part of this, owned by the Duke of Cornwall. The Ministry of Defence owns 14% (see below), 3.8% is owned by water companies (see Dartmoor reservoirs), 3.7% by the National Trust, 1.8% by the Forestry Commission and 1.4% by Dartmoor's national park authority. About 37% of Dartmoor is common land.
Dartmoor differs from some other National Parks in England and Wales, in that since the Dartmoor Commons Act 1985 much of it has been designated as 'Access Land', which, although it remains privately owned, has no restrictions on where walkers can roam. In addition to this Access Land, there are about 730 km (450 mi) of public rights of way on Dartmoor, and many kilometres of permitted footpaths and bridleways where the owner allows access.
Because of the 1985 Act, Dartmoor was largely unaffected by the Countryside and Rights of Way Act 2000, which established similar rights in other rural parts of the country, but in 2006, this Act opened up much of the remaining restricted land to walkers.
There is a tradition of military usage of Dartmoor dating back to the Napoleonic Wars. Today, a large British Army training camp remains at Okehampton — also the site of an airbase during the Second World War.
The Ministry of Defence (MoD) uses three areas of the northern moor for manoeuvres and live-firing exercises, totalling 108.71 km2 (41.97 sq mi), or just over 11% of the National Park. Red and white posts mark the boundaries of these military areas (shown on Ordnance Survey 1:25,000 scale maps). Flagpoles on many tors in and around the ranges fly red flags when firing is taking place. At other times, members of the public are allowed access. Blank rounds may also be used, but the MoD does not notify the public of this in advance.
Dartmoor's fictional use as an MoD centre for animal testing called Baskerville was referenced in the BBC drama Sherlock episode "The Hounds of Baskerville".
Throughout human history, the landscape has been exploited for industrial purposes. In recent years, controversy has surrounded the work of industrial conglomerates Imerys and Sibelco (formerly Watts Blake Bearne), who have used parts of the moor for china clay mining. Licences were granted by the British Government but were recently renounced after sustained public pressure from bodies such as the Dartmoor Preservation Association.
The British government has made promises to protect the integrity of the moor; however, the cost of compensating companies for these licences, which may not have been granted in today's political climate, could prove prohibitive.
The military use of the moor has been another source of controversy, such as when training was extended in January 2003. The national park authority received 1,700 objections before making the decision. Objectors claimed that Dartmoor should be an area for recreation, and that the training disturbs the peace.
Those who objected included the Open Spaces Society and the Dartmoor Preservation Association. During her lifetime, Lady Sayer was another outspoken critic of the damage which she perceived that the army was doing to the moor.
Dartmoor has a resident population of about 33,000, which swells considerably during holiday periods with incoming tourists. The largest settlements within the National Park are Ashburton (the largest with a population of about 3,500), Buckfastleigh, Moretonhampstead, Princetown, Yelverton, Horrabridge, South Brent, Christow, and Chagford.
For a full list, expand the Settlements of Dartmoor navigational box at the bottom of this page.
Until the early 19th century Dartmoor was not considered to be a place worth visiting: in the 1540s John Leland wrote in his Itinerary that "Dartmore is muche a wilde Morish and forest Ground", and even by 1789 Richard Gough's opinion was that it is a "dreary mountainous tract". At the turn of the 19th century John Swete was one of the first people to visit Dartmoor for pleasure and his journals and watercolour paintings now provide a valuable historical resource.
The oldest leisure pursuit on the moor is hill walking. William Crossing's definitive Guide to Dartmoor was published in 1909, and in 1938 a plaque and letterbox in his memory were placed at Duck's Pool on the southern moor. Parts of the Abbots Way, Two Moors Way and the Templer Way are on Dartmoor.
Letterboxing originated on Dartmoor in the 19th century and has become increasingly popular in recent decades. Watertight containers, or 'letterboxes', are hidden throughout the moor, each containing a visitor's book and a rubber stamp. Visitors take an impression of the letterbox's rubber stamp as proof of finding the box and record their visit by stamping their own personal stamp in the letterbox's logbook. A recent related development is geocaching. Geocache clues make use of GPS coordinates, whereas letterboxing clues tend to consist of grid references and compass bearings.
Whitewater kayaking and canoeing are popular on the rivers due to the high rainfall and their high quality, though for environmental reasons access is restricted to the winter months. The River Dart is the most prominent meeting place, the section known as the Loop being particularly popular. Other white water rivers are the Erme, Tavy, Plym and Meavy.
Other activities are rock climbing on the granite tors and outcrops, some of the well-known venues being Haytor, Hound Tor and The Dewerstone; horse riding, which can be undertaken on any of the common land; cycling (but not on open moorland); and angling for wild brown trout, sea trout and salmon—although much of the river fishing on Dartmoor is privately owned, permits are available for some stretches.
The park's main visitor centre is located in Princetown and features exhibits about Dartmoor's history, culture and wildlife, as well as changing displays of local art. The visitor centres located in Postbridge and Haytor feature information, maps, guidebooks and items for exploring the area.
Belstone is a small village and civil parish in the West Devon District of Devon, England. Lying on the northern side of Dartmoor, the western boundary of the parish is mostly formed by the East Okement River and the eastern by the River Taw; its highest point is Belstone Tor in the south, at 1,508 feet. The parish is surrounded, clockwise from the north, by the parishes of Sticklepath, South Tawton, Dartmoor Forest and Okehampton Hamlets. In 2001 its population was 257, relatively unchanged from the 1901 figure of 236.The village, recorded in the Domesday Book as Bellestam, is central in its parish and lies at around 990 feet above sea level. It is only accessible by minor roads from the A30 road, east of the town of Okehampton, which is about three miles to the north-west. The parish church, dedicated to St. Mary, dates from the 13th century and has priests recorded from 1260.There are a number of Bronze Age remains within the parish, including the Nine Maidens stone circle, the remains of the outer wall of a burial chamber.In the 19th century, copper was worked on the moor at Taw River mine which closed in 1892, and at Greenhill in the north-east.
It is possible that Fatherford, in the north west of Belstone parish, was one stage in a Roman extension of the Fosse Way road from Exeter to Launceston.Bovey Tracey
Bovey Tracey () is a small town and civil parish in Devon, England, on the edge of Dartmoor, its proximity to which gives rise to the "slogan" used on the town's boundary signs, "The Gateway to the Moor". It is often known locally as "Bovey". It is about 10 miles south-west of Exeter and lies on the A382 road, about halfway between Newton Abbot and Moretonhampstead. The village is at the centre of the electoral ward of Bovey. At the 2011 census the population of this ward was 7,721.Dartmoor Railway
The Dartmoor Railway is a 15 1⁄2-mile (24.9 km) long railway line in Devon, England. From Crediton the line parallels the Tarka Line to the site of the former Coleford Junction. Heading west, it then serves Sampford Courtenay, Okehampton and Meldon Quarry. The section from Crediton to Coleford Junction is owned by Network Rail and from there to Meldon is owned by Aggregate Industries. In the past freight trains served the ballast quarry at Meldon. The line is leased to and maintained by the Dartmoor Railway CIC, who operate some services and facilitate access to the line by other operators.
Great Western Railway run a public service between Exeter and Okehampton on summer Sundays. Ballast and stone trains were formerly operated by one of the national freight operating companies. In 2011 the quarry was mothballed, leading to the suspension of ballast and stone trains. The line is also used occasionally by other operators for training purposes,and is visited from time to time by main line charter services via the connection to the national network at Crediton.
The route was originally part of the London and South Western Railway's West of England Main Line (route from Exeter to Plymouth), which opened between 1865 and 1879. In 1968, British Rail closed the line beyond Meldon as part of the Beeching cuts. The Exeter to Okehampton passenger service was withdrawn by British Rail in 1972.
Between 1972 and 1997 the line was used for railway ballast traffic from Meldon Quarry and occasional freight traffic to the remaining goods yard at Okehampton before its closure. Occasional charter and special trains were operated to Okehampton and Meldon Quarry during the passenger closure period. The railway reopened to regular passenger services in 1997 with the formation of Dartmoor Railway. A summer Sunday passenger service was introduced from Exeter to Okehampton as part of the Dartmoor Rover network.British American Railway Services Ltd, a company created by Iowa Pacific Holdings of Chicago, became the new owner of the Dartmoor Railway CIC on 4 September 2008. The company announced its intention to develop freight, passenger and tourist services on the railway.Volunteer support for the railway is provided by the Dartmoor Railway Supporters Association (DRSA). Volunteers assist the railway operation in many of its activities.A proposal was made in 2009 to restore and reopen the disused down platform at Yeoford and extend Dartmoor Railway services to terminate there. At the time it was not possible to agree arrangements with Network Rail, who own Yeoford Station and the section of line from near the site of the former Coleford Junction towards Yeoford and Crediton. If this proposal were eventually achieved it could allow the extension of Dartmoor Railway passenger services and make interchange with Exeter–Barnstaple "Tarka Line" trains possible.Dartmoor Zoological Park
Dartmoor Zoological Park (originally Dartmoor Wildlife Park) is a 30-acre (12 ha) zoo near the village of Sparkwell, on the south-west edge of Dartmoor, in the county of Devon in the South West of England. It was opened in 1968 by Ellis Daw who ran it until its licence was revoked and it was forced to close in 2006. The zoo was bought in August 2006 by Benjamin Mee who moved in with his two children Milo and Ella and reopened the zoo in July 2007, later writing a book about his experiences called We Bought a Zoo (2008). A 2011 film of the same title was loosely based on the book.Dartmoor kistvaens
Dartmoor kistvaens are burial tombs or cists from the late Neolithic and early Bronze Age, i.e. from c 2500 BC to c 1500 BC. Kistvaens have been found in many places, including Dartmoor, a 954 km2 (368 square miles) area of moorland in south Devon, England. The box-like stone tombs were created when the ancient people of the area lived in hut circles. Cists are often to be found in the centre of a cairn circle although some appear solitary which could be the result of the loss of an original slight mound. There are over 180 known cists on Dartmoor although there could be up to 100 that remain buried underneath unexplored cairns. In the South West there are no cists to be found on the Quantock Hills, only 2 to be found on Exmoor and 58 to be found on Bodmin Moor. The Dartmoor cists are unique in that about 94% have the longer axis of the tomb oriented in a NW/SE direction It appears that Dartmoor cists were positioned in such a way that the deceased were facing the sun.In August 2011 an untouched cist, on Whitehorse Hill, near Chagford, was the first to be excavated on the moor for over 100 years. This burial yielded some rare Bronze Age artefacts made of organic materials.Drizzlecombe
Drizzlecombe or Thrushelcombe is an area of Dartmoor in the county of Devon, England, containing a number of Bronze Age stone rows, cairns and menhirs.
There are three principal stone rows each with an associated barrow and terminal menhir. Most of the artifacts are on the southwest slope of Hartor Hill. The tallest menhir, which at 14 ft (4.3 m) high is the largest on Dartmoor, was re-erected by Sabine Baring-Gould, R. Hansford Worth and others in 1893.Drizzlecombe is located on the western side of Dartmoor, about 4 miles (6.4 km) east of the village of Yelverton, to the west of the upper reaches of the River Plym.
Nearby is the large but damaged cairn known as Giant's Basin; many of its stones were removed by warreners to build their rabbit-warrens at Ditsworthy, lower down the river. Higher up the slope and overlooking these monuments is a village of stone hut circles, akin to the one at Grimspound. To the north-east lie the extensive remains of Eylesbarrow tin mine and north-west is the concentric Yellowmead stone circle. The area also includes the Neolithic Dartmoor kistvaens, or tombs.East Okement River
East Okement is a river in the Dartmoor moors in Devon in south-west England. It joins the West Okement at Okehampton to form the Okement.HM Prison Dartmoor
HM Prison Dartmoor is a Category C men's prison, located in Princetown, high on Dartmoor in the English county of Devon. Its high granite walls dominate this area of the moor. The prison is owned by the Duchy of Cornwall, and is operated by Her Majesty's Prison Service.Okehampton
Okehampton ( also ) is a town and civil parish in West Devon in the English county of Devon. It is situated at the northern edge of Dartmoor, and had a population of 5,922 at the 2011 census. Two electoral wards are based in the town (east and west). Their joint population at the same census is 7,500.Okehampton is 21 miles (33 km) west of Exeter, 26 miles (42 km) north of Plymouth and 24 miles (38 km) south of Barnstaple.River Dart
The River Dart is a river in Devon, England which rises high on Dartmoor, and releases to the sea at Dartmouth.River Lemon
The River Lemon is a 9.9 mile (16 kilometre) river in the county of Devon in southwest England. It is a tributary of the River Teign, starting on Dartmoor by Haytor, and ending in Newton Abbot. It rises on the south-east side of Dartmoor near Haytor, joins with the River Sig and the Langworthy Brook at Sigford, then passes the village of Bickington. Lower down, it is joined by the Kestor Brook and it then flows through the woods in Bradley Valley, past the manor house of Bradley, and through the town of Newton Abbot where it flows through a 440-yard-long tunnel below the town centre. Just below the town, the river joins the River Teign at 50.517°N 3.607°W / 50.517; -3.607, near the head of its estuary.
The name Lemon is a derivative of a Celtic word meaning elm.River Lyd, Devon
The Lyd is a river rising at Lyd Head (Corn Ridge in NW Dartmoor) in the Dartmoor national park in Devon in south-west England and flowing into the River Tamar beyond Lifton. This is the deepest gorge in the South West of England.River Plym
The River Plym is a river in Devon, England. It runs from Dartmoor in the centre of the county southwest to meet the River Meavy, then south towards Plymouth Sound. The river is popular with canoeists, and the Plym Valley Railway runs alongside a section of the river.River Swincombe
The River Swincombe is a tributary of the West Dart River that flows through
Dartmoor national park in Devon, south-west England. It rises south-east of Princetown, and flows 2 km south-east to Foxtor Mires, where it turns north-east to meet the West Dart near Hexworthy. The first 2 km are known as the Strane River. Some maps show that the source starts north of Nakers Hill and heads north west to the east of Foxtor Mires where it meets the Strane River which (on some maps) is its own river.River Teign
The River Teign or is a river in the county of Devon, England. It is 31 mi (50 km) long and rises on Dartmoor, becomes an estuary just below Newton Abbot and reaches the English Channel at Teignmouth.Scorhill
Scorhill (pronounced Scorill) Stone Circle is now the commonly known name for Gidleigh Stone Circle or Steep Hill Stone Circle, one of Devon's biggest and most intact stone circles, situated on Gidleigh Common near the village of Gidleigh in the north east of Dartmoor, in the United Kingdom. It is an English Heritage scheduled monument and has been described as Devon's finest stone circle.Sticklepath
Sticklepath is a village on Dartmoor, in the county of Devon, England.Tor (rock formation)
A tor, which is also known by geomorphologists as either a castle koppie or kopje, is a large, free-standing rock outcrop that rises abruptly from the surrounding smooth and gentle slopes of a rounded hill summit or ridge crest. In the South West of England, the term is commonly also used for the hills themselves – particularly the high points of Dartmoor in Devon and Bodmin Moor in Cornwall.West Dart River
The West Dart River is one of the two main tributaries of the River Dart in Devon, England.
Its source is about 2 km north of Rough Tor on north Dartmoor. It flows south to Two Bridges, then south east past Hexworthy to meet the East Dart River at Dartmeet.
On the left bank of the river about a mile above Two Bridges is the broadleaved Wistman's Wood, "fascinating high-level woods that are quite unlike anywhere else".Tributaries include the Cowsic River which rises near Devils Tor and flows south below Lydford Tor, to join the West Dart at Two Bridges. Other right bank tributaries include the Blackbrook River, River Swincombe and the O Brook. The Cherry Brook joins the West Dart on the left bank near Sherberton.
|Boroughs or districts|
Parentheses denote year of establishment as a National Park. An area with ‡ has similar status to a UK National Park. Areas marked † are proposed.
Rivers of Dartmoor, Devon, England