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De Lank River
The De Lank River ( kw, Dowr Dinlonk, meaning ''ravine fort river'') is a small river in north Cornwall, England. It is a tributary of the River Camel and is approximately nine miles (14.5 km) long from its source on Bodmin Moor to its confluence with the Camel two miles (3 km) south of St Breward. The De Lank River springs from Rough Tor Marsh between the two highest peaks on Bodmin Moor, Rough Tor and Brown Willy. Initially, its course is south between the peaks before turning southwest, past the southern foot of Garrow Tor, heading for the Camel. The De Lank's course is within the civil parish of St Breward. The river flows through an isolated area with few riverside settlements. Its upper reaches cross a bare moorland plateau and its lower reaches are characterised by ancient deciduous woodland. At Lank, near the confluence with the River Camel, the river flows through De Lank Quarries (the site of a Geological SSSI). The De Lank River is an important wildlife h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Civil Parish
In England, a civil parish is a type of administrative parish used for local government. It is a territorial designation which is the lowest tier of local government below districts and counties, or their combined form, the unitary authority. Civil parishes can trace their origin to the ancient system of ecclesiastical parishes, which historically played a role in both secular and religious administration. Civil and religious parishes were formally differentiated in the 19th century and are now entirely separate. Civil parishes in their modern form came into being through the Local Government Act 1894, which established elected parish councils to take on the secular functions of the parish vestry. A civil parish can range in size from a sparsely populated rural area with fewer than a hundred inhabitants, to a large town with a population in the tens of thousands. This scope is similar to that of municipalities in Continental Europe, such as the communes of France. However, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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". Selection and conservation Sites notified for their biological interest are known as Biological SSSIs (or ASSIs), and those notified for geological or physiographic interest are Geological SSSIs (or ASSIs). Sites may be divided into management units, with some areas including units that are noted for both biological and geological interest. Biological Biological SSSI/ASSIs may b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Special Area Of Conservation
A Special Area of Conservation (SAC) is defined in the European Union's Habitats Directive (92/43/EEC), also known as the ''Directive on the Conservation of Natural Habitats and of Wild Fauna and Flora''. They are to protect the 220 habitats and approximately 1,000 species listed in annex I and II of the directive which are considered to be of European interest following criteria given in the directive. They must be chosen from the Sites of Community Importance by the member states and designated SAC by an act assuring the conservation measures of the natural habitat. SACs complement Special Protection Areas and together form a network of protected sites across the European Union called Natura 2000. This, in turn, is part of the Emerald network of Areas of Special Conservation Interest (ASCIs) under the Berne Convention. Assessment methodology in the United Kingdom Prior to being designated as a Special Area of Conservation (SAC), sites have been assessed under a two-stage process ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Otter
Otters are carnivorous mammals in the subfamily Lutrinae. The 13 extant otter species are all semiaquatic, aquatic, or marine, with diets based on fish and invertebrates. Lutrinae is a branch of the Mustelidae family, which also includes weasels, badgers, mink, and wolverines, among other animals. Etymology The word ''otter'' derives from the Old English word or . This, and cognate words in other Indo-European languages, ultimately stem from the Proto-Indo-European language root , which also gave rise to the English word "water". Terminology An otter's den is called a holt or couch. Male otters are called dogs or boars, females are called bitches or sows, and their offspring are called pups or cubs. The collective nouns for otters are bevy, family, lodge, romp (being descriptive of their often playful nature) or, when in water, raft. The feces of otters are typically identified by their distinctive aroma, the smell of which has been described as ranging from freshly ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geological Site Of Special Scientific Interest
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". Selection and conservation Sites notified for their biological interest are known as Biological SSSIs (or ASSIs), and those notified for geological or physiographic interest are Geological SSSIs (or ASSIs). Sites may be divided into management units, with some areas including units that are noted for both biological and geological interest. Biological Biological SSSI/ASSIs may b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
De Lank Quarries
De Lank Quarries () is an active quarry and a 54-acre geological Site of Special Scientific Interest in St Breward parish, north Cornwall, England, UK. The quarry, which received its SSSI notification in 1994, takes its name from the nearby De Lank river. The quarry produces typical biotite granites and are of such quality that a slab now forms the base section of the reception desk at the Geological Society of London. Other notable structures built of De Lank granite are the fourth Eddystone Lighthouse, 1882; the Royal Opera House in Covent Garden, London and the New Parliamentary Building in Whitehall, London Geology De Lank quarry is located on the edge of the igneous rocks that form the majority of Bodmin moor, with the change to slate formations occurring less than to the west. The bedrock in the quarry is granite, predominantly biotite-bearing granites and aplogranite with some felsite intrusions. History In the 1950s the quarry was owned by T W Ward & Son Ltd. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lank, Cornwall
Lank (formerly also "Lanke") is a settlement in Cornwall, England, United Kingdom. It is situated approximately one mile (1.6 km) south of St Breward and six miles (10 km) east-northeast of Wadebridge in St Breward civil parish. It is in the civil parish of Blisland. The settlement consists of two hamlets, Higher Lank (to the north) and Lower Lank (to the south), situated on high ground between the valleys of the River Camel and De Lank River from which the settlements take their name. The De Lank granite quarry is half-a-mile east of Lower Lank. The quarry is still operational and is currently owned by Ennstone plc, a multinational asphalt and aggregates business. Wenfordbridge is half-a-mile to the west and was the terminus of a branch of the Bodmin and Wadebridge railway. A siding from Wenfordbridge ran between Higher Lank and Lower Lank and served the quarry via a rope-worked incline. The siding shut in 1940 but rail services to Wenfordbridge continued until 1 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Garrow Tor
Garrow Tor is a bare, tor-crowned hill, high, located on Garrow Downs in the northwest of Bodmin Moor in the county of Cornwall, England, UK.Ordnance Survey 1:25,000 ''Explorer'' map series, No. 109 At the summit of Garrow Tor are granite rock outcrops and the hill also bears extensive evidence of early settlement, including a massive stone hedge, Bronze Age settlements and hut circles and Medieval settlements. Panoramic views from the summit include Caradon Hill to the south, Rough Tor and Brown Willy to the north, Butter's Tor to the east, clay country to the west and the Atlantic Ocean The Atlantic Ocean is the second-largest of the world's five oceans, with an area of about . It covers approximately 20% of Earth's surface and about 29% of its water surface area. It is known to separate the " Old World" of Africa, Europe ... to the northwest. . [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stream Below Garrow Tor - Geograph
A stream is a continuous body of surface water flowing within the bed and banks of a channel. Depending on its location or certain characteristics, a stream may be referred to by a variety of local or regional names. Long large streams are usually called rivers, while smaller, less voluminous and more intermittent streams are known as streamlets, brooks or creeks. The flow of a stream is controlled by three inputs – surface runoff (from precipitation or meltwater), daylighted subterranean water, and surfaced groundwater ( spring water). The surface and subterranean water are highly variable between periods of rainfall. Groundwater, on the other hand, has a relatively constant input and is controlled more by long-term patterns of precipitation. The stream encompasses surface, subsurface and groundwater fluxes that respond to geological, geomorphological, hydrological and biotic controls. Streams are important as conduits in the water cycle, instruments in groundwater re ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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