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North Devon's Biosphere Reserve
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North Devon's Biosphere Reserve
North Devon's Biosphere Reserve is a UNESCO biosphere reserve in North Devon. It covers 5,262 square kilometres (2,032 sq mi) and is centred on Braunton Burrows, the largest sand dune system (psammosere) in England. The boundaries of the reserve follow the edges of the conjoined catchment basin of the Rivers Taw and the Torridge and stretch out to sea to include the island of Lundy. The biosphere reserve is primarily lowland farmland, and includes many protected sites including 63 Sites of Special Scientific Interest which protect habitats such as culm grassland and broadleaved woodlands. The most populous settlements in its buffer area are Barnstaple, Bideford, Northam, Ilfracombe, and Okehampton.
The reserve was the first of the "new style" of UNESCO biosphere reserves in the United Kingdom when it was expanded from its previous area in 2002. The new guidelines encourage its management to strike a balance between people and conservation of the environment they live in through sustainability, income generation, and a reduction in poverty. It is managed by the Biosphere Reserve Partnership, which includes a number of interested parties such as the Environment Agency, Natural England, Devon Wildlife Trust, and the National Trust. The partnership organises landscape projects and works closely with the inhabitants of the reserve.
Within the reserve's core area are the sand dune system and culm grassland. To the west in Bideford Bay (visible from the beach element of the dunes, Saunton Sands which is a due-west facing surfing beach) is a coral reef with a diversity of coral and marine life seen nowhere else in Britain. The sand dunes have a rich habitat of hundreds of flowering plants while the Taw-Torridge estuary is an important feeding area for long-journey migratory birds.
The economy of North Devon is largely supported by tourism. Four million people per year visit the area, and visitor numbers can rise as high as 60,000 per day in August. Most of these people come because of the environment.
North Devon's Biosphere Reserve is in northern Devon in South West England. Although mainly in the districts of North Devon and Torridge, the reserve also extends into West and Mid Devon. It covers a large area of sea up to 160 feet (49 m) in depth off the North Devon coast and includes Lundy island 12 miles (19 km) from the shore. The core area is centred on Braunton Burrows, a large sand dune system, which consists of 19 sq mi (49 km2) of sand dunes, slacks (troughs between the dunes), grassland, scrub habitat, and a part of the Taw-Torridge Estuary. The reserve's boundary follows the edges of several river catchment areas, mainly of the River Taw and the River Torridge, but also those of smaller rivers running into the sea between Hartland and Lynton. The North Devon Coast Area of Outstanding Natural Beauty lies at the heart of the reserve, while parts of the national parks of Dartmoor and Exmoor fringe the boundaries.
There are no cities within the reserve. Barnstaple, Bideford, Ilfracombe, Braunton, Northam and Great Torrington contain many of the 155,000 people living in the wider buffer area of the Biosphere. The surrounding towns and villages are also included in reserve projects and policy decisions.
There is evidence of humans in North Devon from Mesolithic times onward. Worked pieces of flint or stone, known as flint scatters, that date to this era have been found around Baggy Point in an area where flint does not occur naturally. In the clays beneath the sand of Westward Ho! beach there is a Mesolithic midden, a prehistoric dump for domestic waste, composed of mussels, cockles, peppery furrow shells (Scrobicularia plana), and carpet shells (Venerupis spp.). On Exmoor the remains of small flint tools called microliths, used by hunter-gatherers to hunt and prepare animals, have been found and date to the late Mesolithic. In the Neolithic period, people started to manage animals and grow crops on farms, and started to cut down the woodlands of Exmoor, rather than act purely as hunters and gatherers. These Neolithic people created stone monuments and by the Bronze Age were creating barrows (burial mounds) and roundhouses. Evidence shows that extraction and smelting of mineral ores to make metal tools, weapons, containers and ornaments had started by the Iron Age. Bronze Age barrows have also been found on elevated parts of Bursdon Moor, near Hartland and on Berry Down, near Berrynarbor. Iron Age hill forts were built on prominent parts of the coastline and hinterland. Examples can be found at Hillsborough near Ilfracombe, Embury Beacon and Clovelly Dykes in the Hartland area, with numerous other examples along the coast.
Biosphere reserves are designed to deal with one of the most important
questions the World faces today: How can we reconcile conservation of
biodiversity and biological resources with their sustainable use?
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North Devon's Biosphere Reserve AI simulator
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North Devon's Biosphere Reserve
North Devon's Biosphere Reserve is a UNESCO biosphere reserve in North Devon. It covers 5,262 square kilometres (2,032 sq mi) and is centred on Braunton Burrows, the largest sand dune system (psammosere) in England. The boundaries of the reserve follow the edges of the conjoined catchment basin of the Rivers Taw and the Torridge and stretch out to sea to include the island of Lundy. The biosphere reserve is primarily lowland farmland, and includes many protected sites including 63 Sites of Special Scientific Interest which protect habitats such as culm grassland and broadleaved woodlands. The most populous settlements in its buffer area are Barnstaple, Bideford, Northam, Ilfracombe, and Okehampton.
The reserve was the first of the "new style" of UNESCO biosphere reserves in the United Kingdom when it was expanded from its previous area in 2002. The new guidelines encourage its management to strike a balance between people and conservation of the environment they live in through sustainability, income generation, and a reduction in poverty. It is managed by the Biosphere Reserve Partnership, which includes a number of interested parties such as the Environment Agency, Natural England, Devon Wildlife Trust, and the National Trust. The partnership organises landscape projects and works closely with the inhabitants of the reserve.
Within the reserve's core area are the sand dune system and culm grassland. To the west in Bideford Bay (visible from the beach element of the dunes, Saunton Sands which is a due-west facing surfing beach) is a coral reef with a diversity of coral and marine life seen nowhere else in Britain. The sand dunes have a rich habitat of hundreds of flowering plants while the Taw-Torridge estuary is an important feeding area for long-journey migratory birds.
The economy of North Devon is largely supported by tourism. Four million people per year visit the area, and visitor numbers can rise as high as 60,000 per day in August. Most of these people come because of the environment.
North Devon's Biosphere Reserve is in northern Devon in South West England. Although mainly in the districts of North Devon and Torridge, the reserve also extends into West and Mid Devon. It covers a large area of sea up to 160 feet (49 m) in depth off the North Devon coast and includes Lundy island 12 miles (19 km) from the shore. The core area is centred on Braunton Burrows, a large sand dune system, which consists of 19 sq mi (49 km2) of sand dunes, slacks (troughs between the dunes), grassland, scrub habitat, and a part of the Taw-Torridge Estuary. The reserve's boundary follows the edges of several river catchment areas, mainly of the River Taw and the River Torridge, but also those of smaller rivers running into the sea between Hartland and Lynton. The North Devon Coast Area of Outstanding Natural Beauty lies at the heart of the reserve, while parts of the national parks of Dartmoor and Exmoor fringe the boundaries.
There are no cities within the reserve. Barnstaple, Bideford, Ilfracombe, Braunton, Northam and Great Torrington contain many of the 155,000 people living in the wider buffer area of the Biosphere. The surrounding towns and villages are also included in reserve projects and policy decisions.
There is evidence of humans in North Devon from Mesolithic times onward. Worked pieces of flint or stone, known as flint scatters, that date to this era have been found around Baggy Point in an area where flint does not occur naturally. In the clays beneath the sand of Westward Ho! beach there is a Mesolithic midden, a prehistoric dump for domestic waste, composed of mussels, cockles, peppery furrow shells (Scrobicularia plana), and carpet shells (Venerupis spp.). On Exmoor the remains of small flint tools called microliths, used by hunter-gatherers to hunt and prepare animals, have been found and date to the late Mesolithic. In the Neolithic period, people started to manage animals and grow crops on farms, and started to cut down the woodlands of Exmoor, rather than act purely as hunters and gatherers. These Neolithic people created stone monuments and by the Bronze Age were creating barrows (burial mounds) and roundhouses. Evidence shows that extraction and smelting of mineral ores to make metal tools, weapons, containers and ornaments had started by the Iron Age. Bronze Age barrows have also been found on elevated parts of Bursdon Moor, near Hartland and on Berry Down, near Berrynarbor. Iron Age hill forts were built on prominent parts of the coastline and hinterland. Examples can be found at Hillsborough near Ilfracombe, Embury Beacon and Clovelly Dykes in the Hartland area, with numerous other examples along the coast.
Biosphere reserves are designed to deal with one of the most important
questions the World faces today: How can we reconcile conservation of
biodiversity and biological resources with their sustainable use?
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