Dartmoor is an upland area in southern Devon, South West England. The moorland and surrounding land has been protected by National Park status since 1951. Dartmoor National Park covers 954 km2 (368 sq mi).
Princetown is a village located within Dartmoor national park in the English county of Devon. It is the principal settlement of the civil parish of Dartmoor Forest.
Moretonhampstead is a market town, parish and ancient manor in Devon, situated on the north-eastern edge of Dartmoor, within the Dartmoor National Park. The parish now includes the hamlet of Doccombe, and it is surrounded clockwise from the north by the parishes of Drewsteignton, Dunsford, Bridford, Bovey Tracey, Lustleigh, North Bovey and Chagford.
The River Teign 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.
Chagford is a market town and civil parish on the north-east edge of Dartmoor, in Devon, England, close to the River Teign and the A382, 4 miles (6 km) west of Moretonhampstead. The name is derived from chag, meaning gorse or broom, and the ford suffix indicates its importance as a crossing place. At the 2011 Census, it had a population of 1,449.
Teignbridge is a local government district in Devon, England. Its council is based in the town of Newton Abbot. The district also includes the towns of Ashburton, Buckfastleigh, Dawlish, Kingsteignton and Teignmouth, along with numerous villages and surrounding rural areas. Teignbridge contains part of the south Devon coastline, including the Dawlish Warren National Nature Reserve. Some of the inland western parts of the district lie within the Dartmoor National Park. It is named after the old Teignbridge hundred.
A packhorse bridge is a bridge intended to carry packhorses across a river or stream. Typically a packhorse bridge consists of one or more narrow masonry arches, and has low parapets so as not to interfere with the panniers borne by the horses. Multi-arched examples sometimes have triangular cutwaters that are extended upward to form pedestrian refuges.
Bridford is a village and civil parish in south west England, located in the Teign Valley, Devon on the edge of Dartmoor. The parish is surrounded by the parishes of Dunsford, Doddiscombsleigh, Christow, and Moretonhampstead. At the 2011 census the population of the parish was 503, compared with 404 in 1901.
The Two Moors Way is a long-distance trail mostly in Devon, UK, first established in 1976. It links Dartmoor and Exmoor and has been extended to become a Devon Coast-to-Coast trail.
Bovey Tracey is a town and civil parish in Devon, England. It is located on the edge of Dartmoor, 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. About 10 miles (16 km) south-west of Exeter, it 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 the ward was 7,721.
Haytor, also known as Haytor Rocks, Hay Tor, or occasionally Hey Tor, is a granite tor on the eastern edge of Dartmoor in the English county of Devon.
The Cann Quarry canal was a canal in Devon, England which ran for just under 2 miles (3.2 km) from Cann Quarry to the River Plym at Marsh Mills. It opened in 1829, and a short tramway connected it to the Plymouth and Dartmoor Railway at Crabtree Junction. It had been replaced by a tramway within ten years, but continued to be used as a mill leat to supply Marsh Mills corn mill, and most of it is still visible.
The Hackney Canal was a short canal in Devon, England, that linked the Hackney Clay Cellars to the River Teign. It was privately built by Lord Clifford in 1843, and throughout its life carried ball clay for use in the production of pottery. It closed in 1928, when its function was replaced by road vehicles.
The A382 is a road in South West England, connecting Newton Abbot to the A38, then to Bovey Tracey and on through Moretonhampstead to the A30.
The Dartmoor crosses are a series of stone crosses found in Dartmoor National Park in the centre of Devon, England. Many of them are old navigational aids, needed because of the remoteness of the moorland and its typically bad weather. Some mark medieval routes between abbeys. Other crosses were erected as memorials, for prayer, as town or market crosses, in churchyards, and as boundary markers. The crosses were erected over a long period of time, some as recently as 100 years ago, the earliest probably almost 1,000 years ago.
The Gallox Bridge in Dunster, Somerset, England dates from the 15th century. It has been designated as a Grade I listed building and scheduled monument. The bridge is in the guardianship of English Heritage.
The River Avill is a small river on Exmoor in Somerset, England.
North Bovey is a village and civil parish situated on the south-eastern side of Dartmoor National Park, Teignbridge, Devon, England, about 11 miles WSW of the city of Exeter and 1.5 miles SSW of Moretonhampstead. The village lies above the eastern bank of the River Bovey from which it takes its name. In 2001 the population of the parish was 274, compared to 418 in 1901 and 519 in 1801.
Sharp Tor is a common name given to tors (outcrops), particularly on Dartmoor and Bodmin Moor. All the "Sharp Tors" are listed below with their location and height:
This article describes the geology of Dartmoor National Park in Devon, in south-west England. Dartmoor gained national park status in 1951 but the designated area of 954 km2 (368 sq mi) extends beyond the upland of Dartmoor itself to include much of the surrounding land, particularly in the northeast. The geology of the national park consists of a 625 km2 (241 sq mi) core of granite intruded during the early Permian period into a sequence of sedimentary rocks originating in the Devonian and Carboniferous periods. These rocks were faulted and folded, sometimes, intensely, during the Variscan orogeny. Thermal metamorphism has also taken place around the margins of the granite pluton altering the character of the sedimentary rocks whilst mineral veins were emplaced within the granite. A small outlier of Palaeogene sediments occurs on the eastern boundary of the national park.
