Pow Hill Bog | |
Site of Special Scientific Interest | |
Pow Hill Country Park and Derwent Reservoir | |
Country | England |
---|---|
Region | North East |
District | Wear Valley |
Location | NZ009518 |
- coordinates | 54°51′41″N1°59′12″W / 54.86139°N 1.98667°W Coordinates: 54°51′41″N1°59′12″W / 54.86139°N 1.98667°W |
Area | 6.7 ha (16.6 acres) |
Notification | 1986 |
Management | Natural England |
Area of Search | County Durham |
Interest | Biological |
Website: Map of site | |
Pow Hill Bog is a Site of Special Scientific Interest in the Wear Valley district of County Durham, England. It lies alongside Derwent Reservoir, approximately 2 km north-west of the village of Edmundbyers and adjacent to the Edmundbyers Common portion of the Muggleswick, Stanhope and Edmundbyers Commons and Blanchland Moor SSSI.
A Site of Special Scientific Interest (SSSI) in Great Britain or an Area of Special Scientific Interest (ASSI) in the Isle of Man and Northern Ireland is a conservation designation denoting a protected area in the United Kingdom and Isle of Man. SSSI/ASSIs are the basic building block of site-based nature conservation legislation and most other legal nature/geological conservation designations in the United Kingdom are based upon them, including national nature reserves, Ramsar sites, Special Protection Areas, and Special Areas of Conservation. The acronym "SSSI" is often pronounced "triple-S I".
Wear Valley was, from 1974 to 2009, a local government district in County Durham, England. Its council and district capital was Crook.
County Durham is a county in North East England. The county town is Durham, a cathedral city. The largest settlement is Darlington, closely followed by Hartlepool and Stockton-on-Tees. It borders Tyne and Wear to the north east, Northumberland to the north, Cumbria to the west and North Yorkshire to the south. The county's historic boundaries stretch between the rivers Tyne and Tees, thus including places such as Gateshead, Jarrow, South Shields and Sunderland.
The site contains two types of mire, a valley mire and a soligenous mire, the former a scarce habitat in County Durham. There are also areas of heathland and semi-improved grassland, as well as small plantations of larch and spruce. [1]
A bog or bogland is a wetland that accumulates peat, a deposit of dead plant material—often mosses, and in a majority of cases, sphagnum moss. It is one of the four main types of wetlands. Other names for bogs include mire, quagmire, and muskeg; alkaline mires are called fens. They are frequently covered in ericaceous shrubs rooted in the sphagnum moss and peat. The gradual accumulation of decayed plant material in a bog functions as a carbon sink.
Grasslands are areas where the vegetation is dominated by grasses (Poaceae); however, sedge (Cyperaceae) and rush (Juncaceae) families can also be found along with variable proportions of legumes, like clover, and other herbs. Grasslands occur naturally on all continents except Antarctica. Grasslands are found in most ecoregions of the Earth. For example, there are five terrestrial ecoregion classifications (subdivisions) of the temperate grasslands, savannas, and shrublands biome (ecosystem), which is one of eight terrestrial ecozones of the Earth's surface.
Larches are conifers in the genus Larix, of the family Pinaceae. Growing from 20 to 45 m tall, they are native to much of the cooler temperate northern hemisphere, on lowlands in the north and high on mountains further south. Larches are among the dominant plants in the boreal forests of Siberia and Canada. Although they are conifers, larches are deciduous trees that lose their needles in the autumn.
The wetter parts of the valley mire are characterised by an abundance of bog mosses, Sphagnum spp , in association with species such as common cottongrass, Eriophorum angustifolium , star sedge, Carex echinata , and bog asphodel, Narthecium ossifragum . The drier areas are heathland, with heather, Calluna vulgaris , hare's-tail cottongrass, Eriophorum vaginatum , cross-leaved heath, Erica tetralix , and common sedge, Carex nigra .
Sphagnum is a genus of approximately 380 accepted species of mosses, commonly known as "peat moss". Accumulations of Sphagnum can store water, since both living and dead plants can hold large quantities of water inside their cells; plants may hold 16–26 times as much water as their dry weight, depending on the species. The empty cells help retain water in drier conditions. Hence, as sphagnum moss grows, it can slowly spread into drier conditions, forming larger mires, both raised bogs and blanket bogs. Thus, Sphagnum can influence the composition of such habitats, with some describing Sphagnum as 'habitat manipulators'. These peat accumulations then provide habitat for a wide array of peatland plants, including sedges and ericaceous shrubs, as well as orchids and carnivorous plants. Sphagnum and the peat formed from it do not decay readily because of the phenolic compounds embedded in the moss's cell walls. In addition, bogs, like all wetlands, develop anaerobic soil conditions, which produces slower anaerobic decay rather than aerobic microbial action. Peat moss can also acidify its surroundings by taking up cations, such as calcium and magnesium, and releasing hydrogen ions. Under the right conditions, peat can accumulate to a depth of many meters. Different species of Sphagnum have different tolerance limits for flooding and pH, so any one peatland may have a number of different Sphagnum species.
Eriophorum angustifolium, commonly known as common cottongrass or common cottonsedge, is a species of flowering plant in the sedge family Cyperaceae. Native to North America, North Asia, and Northern Europe, it grows on peat or acidic soils, in open wetland, heath or moorland. It begins to flower in April or May and, after fertilisation in early summer, the small, unremarkable brown and green flowers develop distinctive white bristle-like seed-heads that resemble tufts of cotton; combined with its ecological suitability to bog, these characteristics give rise to the plant's alternative name, bog cotton.
Carex echinata is a species of sedge known by the common names star sedge and little prickly sedge.
The soligenous mire is characterised by sharp-flowered rush, Juncus acutiflorus , and purple moor-grass, Molinia caerulea . Several local species are also present, including narrow-leaved buckler-fern, Dryopteris carthusiana , lesser skullcap, Scutellaria minor , and grass of Parnassus, Parnassia palustris .
Juncus acutiflorus, also called sharp-flowered rush, is a rush or a grassy plant of the genus Juncus. As the name suggests, the plant has notable sharp-looking flowers, flowering between July and September.
Molinia caerulea, the purple moor-grass, is a species of grass that is native to Europe, west Asia, and north Africa. It grows in locations from the lowlands up to 2,300 m (7,546 ft) in the Alps. Like most grasses, it grows best in acid soils, ideally pH values of between 3.5 and 5, however, it can continue to live under more extreme conditions, sometimes to as low as 2. It is common on moist heathland, bogs and moorland throughout Britain. Introduced populations exist in northeastern and northwestern North America.
Dryopteris carthusiana is a species of fern native to damp forests throughout the Holarctic Kingdom. It is known as the narrow buckler-fern in the United Kingdom, and as the spinulose woodfern in North America.
The site is located within the Pow Hill Country Park, a recreational area managed by Durham County Council.
Durham County Council is the local authority of the non-metropolitan County Durham in North East England. Since 2009 it has been a unitary authority, having the powers of a non-metropolitan county and district council combined. From 1889 to 2009 it was a county council in a two-tier arrangement.
The Mer Bleue Conservation Area is a 33.43 km2 (12.91 sq mi) protected area east of Ottawa in Eastern Ontario, Canada. Its main feature is a sphagnum bog that is situated in an ancient channel of the Ottawa River and is a remarkable boreal-like ecosystem normally not found this far south. Stunted black spruce, tamarack, bog rosemary, blueberry, and cottongrass are some of the unusual species that have adapted to the acidic waters of the bog.
NVC community M2 is one of the mire communities in the British National Vegetation Classification system.
Yanal Bog is a 1.6 hectare biological Site of Special Scientific Interest on the southern edge of the North Somerset Levels, just north of the village of Sandford, North Somerset. It was notified as an SSSI in 1988.
Lambert's Castle is an Iron Age hill fort in the county of Dorset in southwest England. Since 1981 it has been designated as a Site of Special Scientific Interest (SSSI) on account of its geology, archaeology and ecology.
Cors Caron is a raised bog in Ceredigion, Wales. Cors is the Welsh word for "bog": the site is also known as Tregaron Bog, being near the small town of Tregaron. Cors Caron covers an area of approximately 862 acres (349 ha). Cors Caron represents the most intact surviving example of a raised bog landscape in the United Kingdom. About 44 different species groups inhabit the area including various land and aquatic plants, fish, insects, crustaceans, lichen, fungi, terrestrial mammals and birds.
A poor fen is a natural wetland habitat, supporting a dense carpet of mosses and sedges. It develops where the water is fairly acidic and has very few plant nutrients. Poor fen is intermediate between the taller vegetation of fen, which occurs where the water is much less acidic, and the short, mossy vegetation of bog, which is even more acidic.
Waldridge Fell is a Site of Special Scientific Interest located immediately south-west of Chester-le-Street in the northern part of County Durham, England. It is one of the largest areas of lowland heath in County Durham and contains the only lowland valley-mire in the county. The fell is home to a number of plants and insects that are scarce to rare elsewhere in the county.
Burnhope Burn is a Site of Special Scientific Interest in the Wear Valley district of north County Durham, England. It consists of a 12.6-acre (5.1 ha) area of woodland, carr, fen and mire in the valley of Burnhope Burn, just below the dam of the Derwent Reservoir, a mile (1.6 km) north-east of the village of Edmundbyers.
Frog Wood Bog is a Site of Special Scientific Interest in the Teesdale district of County Durham, England. It lies alongside Bedburn Beck, approximately 3.5 km west of the village of Bedburn.
Hexhamshire Moors is a Site of Special Scientific Interest covering an extensive area of moorland in the Wear Valley district of north-west County Durham and the Tynedale district of south-west Northumberland, England.
Hisehope Burn Valley is a Site of Special Scientific Interest in the Derwentside district of Durham, England. It consists of two separate parcels of land, one on the west bank of Hisehope Burn, the other a few hundred yards to the east, straddling the headwaters of another small burn. The site is some 3 km west of the village of Castleside and 1 km north of the Smiddy Shaw Reservoir. The larger area adjoins the Muggleswick, Stanhope and Edmundbyers Commons and Blanchland Moor SSSI.
Muggleswick, Stanhope and Edmundbyers Commons and Blanchland Moor is a Site of Special Scientific Interest in County Durham and Northumberland, England. It consists of two separate areas, the larger—encompassing the upland areas of Muggleswick, Stanhope and Edmundbyers Commons—in the Derwentside and Wear Valley districts of north Durham, the smaller—Blanchland Moor—in the Tynedale district of south-west Northumberland.
Pike Whin Bog is a Site of Special Scientific Interest in the Easington district of east County Durham, England. It is situated just east of Hurworth Burn Reservoir, about 8 km west of Hartlepool.
Cefn Blaenau is a 23-hectare Site of Special Scientific Interest in a small upland valley in Carmarthen & Dinefwr, Wales. It was designated an SSSI in 1989 primarily for its flush and spring vegetation as well as the diverse mosaic of unimproved pasture, ‘ffridd’ land, marshy grassland, wet heath, acid grassland, broadleaved woodland, streams, and small rock outcrops. These habitats, which are well represented at this site, have been greatly reduced in north Carmarthenshire due to land improvement, agricultural intensification, and afforestation. Only about 140 hectares of flush and spring vegetation remain in the county.
Rosenannon Downs is a nature reserve in mid Cornwall, England, UK, being designated Rosenannon Bog and Downs Site of Special Scientific Interest (SSSI), noted for its biological characteristics. The site supports a wide variety of flora and fauna and includes Bronze Age barrows. Conservation work is carried out on the site by the owners, the Cornwall Wildlife Trust.
Allendale Moors is a Site of Special Scientific Interest (SSSI) in Northumberland, England. The upland moorland ridge site is listed for its heath, flush and upland grassland which provide a habitat for a nationally important assemblage of moorland breeding birds.
Bewick and Beanley Moors is the name given to a Site of Special Scientific Interest (SSSI) in north Northumberland, in the north-east of England. The moors are asserted to be of national importance by Natural England for the extent, quality and diversity of upland types including heaths, fens, wet grassland, flushes, mires and blanket bogs, together creating an extensive mosaic habitat supporting an exceptional community of amphibians. The moors are important, too, for their relict juniper woodland and scrub.
Billsmoor Park and Grasslees Wood is the name given to a Site of Special Scientific Interest (SSSI) in Northumberland, North East England, designated in 1954. Billsmoor Park is an extensive alder woodland of a sort increasingly uncommon in the county; the much smaller Grasslees Wood is an oak woodland.
Fallowlees Flush is the name given to a Site of Special Scientific Interest (SSSI) in mid-Northumberland, England. The steeply sloping site has calcium-rich springs supporting vegetation rare in the county.