The Lyd is a river rising at Lyd Head [1] (Corn Ridge in NW Dartmoor) in the Dartmoor national park in Devon in South West England and flowing into the River Tamar beyond Lifton. [2] It runs through Lydford Gorge, the deepest gorge in South West England.
Lydford Gorge (National Trust) is a dramatic feature of the river at Lydford on the edge of the Dartmoor National Park; it is a 1.5-mile (2.4 km) gorge near Lydford on the River Lyd, which is the deepest in South West England. It was formed by the process of river capture, where the start of a nearby river eroded backwards until its origin met the Lyd, diverting its course into the second channel. [3]
Owned and maintained by the National Trust since 1947, the gorge features the 100-foot (30 m) tall White Lady Waterfall and a series of whirlpools known as the Devil's Cauldron. [4]
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).
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.
The Tamar is a river in south west England that forms most of the border between Devon and Cornwall. A part of the Tamar Valley is a World Heritage Site due to its historic mining activities.
West Devon is a local government district with borough status in Devon, England. Its council is based in Tavistock, the borough's largest town. The borough also includes the towns of Hatherleigh, North Tawton and Okehampton, along with numerous villages and surrounding rural areas.
Lydford, sometimes spelled Lidford, is a village, once an important town, in Devon, seven miles (11 km) north of Tavistock on the western fringe of Dartmoor in the West Devon district. There is an electoral ward with the same name which includes Princetown. The population of this ward at the 2011 census was 2,047.
The Erme is a river in south Devon, England. From its source on Dartmoor it flows in a generally southerly direction past some of the best-preserved archaeological remains on the moor. It leaves the moor at the town of Ivybridge and continues southward, passing the settlements of Ermington, Modbury and Holbeton. Near Holbeton it becomes a ria and empties into the English Channel in Bigbury Bay, between the rivers Yealm and Avon.
Bridgetown occupies the left bank of the Dart in the town of Totnes, Devon, England.
Penstone is a hamlet of some 21 houses in Devon, England, about 1 mile (2 km) from the villages of Colebrooke and Coleford, close to the point where the Exeter-Barnstaple and former Exeter-Okehampton rail lines diverge; the latter is now a freight line but there has recently been talk of reopening it to passenger traffic and extending it to Plymouth in order to avoid the shoreline track at Dawlish Warren which has recently been washed away several times by winter storms. The nearest stations are Yeoford and Copplestone.
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.
The East Webburn is a stream in the Dartmoor moors in Devon in south-west England. It rises on the western side of the moors flowing off the west side of Hameldown ridge. Its source is less than 1 kilometre south west of Grimspound Bronze Age settlement. It flows south past Widecombe-in-the-Moor and joins the West Webburn River. These combined streams then join the River Dart close to the village of Holne.
The River Meavy is a river in the southwest part of Dartmoor in Devon in south-west England. It runs entirely in the national park and connects Burrator Reservoir to the River Plym.
The West Dart River is one of the two main tributaries of the River Dart in Devon, England.
Dartmoor Forest is a civil parish in Devon, England. It was formed in 1987 by the splitting of the former parish of Lydford. It covers about 56,000 acres (230 km2) entirely within Dartmoor National Park, and is the largest parish in Devon. Despite its size its population in 2001 was only 1,619. Due to its large size it is surrounded by many other parishes: these are, clockwise from the north, Belstone, South Tawton, Throwleigh, Gidleigh, Chagford, North Bovey, Manaton, Widecombe in the Moor, Holne, West Buckfastleigh, Dean Prior, South Brent, Ugborough, Harford, Cornwood, Shaugh Prior, Sheepstor, Walkhampton, Whitchurch, Peter Tavy, Lydford, land common to the parishes of Bridestowe and Sourton, and Okehampton Hamlets.
The River Ottery is a small river in northeast Cornwall, England, United Kingdom. The river is about twenty miles (32 km) long from its source southeast of Otterham to its confluence with the River Tamar at Nether Bridge, two miles (3.2 km) northeast of Launceston.
Colliford Lake is a reservoir on Bodmin Moor, Cornwall, England, United Kingdom. Covering more than 900 acres (3.6 km2), it is the largest lake in Cornwall. It is situated south of the A30 trunk road near the village of Bolventor, the approximate centre of the lake being at OS grid reference SX179730. Dozmary Pool outfalls into the lake and the lake's own outfall forms one of the tributaries of the River Fowey.
The Walla Brook is the name of four different streams on Dartmoor, England:
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.
Bridestowe and Sourton Common, also known as Common to Bridestowe and Sourton and Lands common to the Parishes of Bridestowe and Sourton, is a civil parish in the district of West Devon, Devon, England. It is surrounded by the parishes of Okehampton Hamlets, Dartmoor Forest, Lydford, Bridestowe and Sourton.
50°37′59″N4°17′59″W / 50.633°N 4.2996°W
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