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River Tees
The River Tees (), in England, rises on the eastern slope of Cross Fell in the North Pennines and flows eastwards for to reach the North Sea in the North East of England. The modern-day history of the river has been tied with the industries on Teesside in its lower reaches, where it has provided the means of import and export of goods to and from the North East England. The need for water further downstream also meant that reservoirs were built in the extreme upper reaches, such as Cow Green. Etymology The name ''Tees'' is possibly of Brittonic origin. The element ''*tēs'', meaning "warmth" with connotations of "boiling, excitement" ( Welsh ''tes''), may underlie the name. ''*Teihx-s'', a root possibly derived from Brittonic ''*ti'' (Welsh ''tail'', "dung, manure"), has also been used to explain the name ''Tees'' (compare River Tyne). Geography The river drains and has a number of tributaries including the River Greta, River Lune, River Balder, River Leven and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
High Force
High Force is a waterfall on the River Tees, near Middleton-in-Teesdale, Teesdale, England. The waterfall is within the North Pennines Area of Outstanding Natural Beauty (AONB) and the European Geopark. The whole of the River Tees plunges over a precipice (an almost vertical cliff edge) in two stages. After heavy rainfall the river will also flow over the usually dry right-hand side channel, creating two falls. Very occasionally the river level will be high enough to flow over the central section of rock; the last recorded time this happened was in December 2015 after Storm Desmond. In harsh winters the falls have been known to freeze, creating cathedral-like ice formations. Access to the northern bank is via a private footpath on the Raby Castle, Raby estate for which a fee is charged. The southern bank can be reached free of charge via the Pennine Way public footpath which crosses the Moor House-Upper Teesdale National Nature Reserve. Geology High Force was formed where th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cow Green Reservoir
Cow Green Reservoir is a long water reservoir forming part of the border between the historic counties of Westmorland and County Durham in northern England, built by Mitchell Construction between 1967 and 1971 to supply the industries of Teesside. The reservoir acts as a river regulation reservoir releasing water into the River Tees during dry conditions so that it can be abstracted further downstream. These regulated flows allow six further reservoir levels to be maintained and these in turn provide water for industry and domestic use. Environmentally, this part of Upper Teesdale is of national importance and the plan to construct this reservoir had been strongly opposed by local conservationists, professional botanists and geologists, including botanist Margaret E. Bradshaw. Their main concern was the protection of the rich flora and fauna of the district and especially rare alpine plants like the unique Teesdale violet. In the end, about a tenth of this plant's habitat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone is a type of carbonate rock, carbonate sedimentary rock which is the main source of the material Lime (material), lime. It is composed mostly of the minerals calcite and aragonite, which are different Polymorphism (materials science), crystal forms of calcium carbonate . Limestone forms when these minerals Precipitation (chemistry), precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly Dolomite (rock), dolomite, a closely related rock, which contains a high percentage of the mineral Dolomite (mine ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shake Holes
A sinkhole is a depression or hole in the ground caused by some form of collapse of the surface layer. The term is sometimes used to refer to doline, enclosed depressions that are also known as shakeholes, and to openings where surface water enters into underground passages known as ''ponor'', swallow hole or swallet. A ''cenote'' is a type of sinkhole that exposes groundwater underneath. ''Sink'', and ''stream sink'' are more general terms for sites that drain surface water, possibly by infiltration into sediment or crumbled rock. Most sinkholes are caused by karst processes – the chemical dissolution of carbonate rocks, collapse or suffosion processes. Sinkholes are usually circular and vary in size from tens to hundreds of meters both in diameter and depth, and vary in form from soil-lined bowls to bedrock-edged chasms. Sinkholes may form gradually or suddenly, and are found worldwide. Formation Natural processes Sinkholes may capture surface drainage from runnin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Area Of Outstanding Natural Beauty
An Area of Outstanding Natural Beauty (AONB; , AHNE) is one of 46 areas of countryside in England, Wales, or Northern Ireland that has been designated for conservation due to its significant landscape value. Since 2023, the areas in England and Wales have also adopted the name National Landscape (). Areas are designated in recognition of their national importance by the relevant public body: Natural England, Natural Resources Wales, and the Northern Ireland Environment Agency respectively. On 22 November 2023, following a review, the AONBs in England and Wales adopted the National Landscapes name, and are in the process of rebranding. AONBs in Northern Ireland did not rename. The name "area of outstanding natural beauty" is still the designated legal term. In place of the term AONB, Scotland uses the similar national scenic area (NSA) designation. Areas of Outstanding Natural Beauty enjoy levels of protection from development similar to those of UK national parks, but unli ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moorland
Moorland or moor is a type of Habitat (ecology), habitat found in upland (geology), upland areas in temperate grasslands, savannas, and shrublands and the biomes of montane grasslands and shrublands, characterised by low-growing vegetation on Soil pH, acidic soils. Moorland today generally means uncultivated hill land (such as Dartmoor in South West England), but also includes low-lying wetlands (such as Sedgemoor, also South West England). It is closely related to heath, although experts disagree on the exact distinction between these types of vegetation. Generally, moor refers to Highland (geography), highland and high rainfall areas, while heath refers to lowland zones which are more likely to be the result of human activity. Moorland habitats are found mainly in Tropics, tropical Africa, Northern Europe, northern and western Europe, and South America. Most of the world's moorlands are diverse ecosystems. In the extensive moorlands of the tropics, biodiversity can be extremely ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Teesdale
Teesdale is a dale, or valley, located principally in County Durham, North East England. It is one of the Durham Dales, which are themselves part of the North Pennines, the northernmost part of the Pennine uplands. The dale is named after its principal river, the Tees, which has its source below Cross Fell () in Cumbria. The upper dale is remote and high, but becomes gentler after it enters County Durham shortly downstream. The dale follows the river's south-easterly course to Barnard Castle, at which point the landscape begins to flatten into the Tees Lowlands. The Cumbrian part of Teesdale was historically divided between Cumberland and Westmorland, and the County Durham area between the former and Yorkshire. Large parts of Teesdale are within the North Pennines national landscape, and Upper Teesdale has been designated a Site of Special Scientific Interest. Parts of the local climate have been scientifically classified as "Sub-Arctic", and snow has sometimes lain ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Westmorland
Westmorland (, formerly also spelt ''Westmoreland''R. Wilkinson The British Isles, Sheet The British IslesVision of Britain/ref>) is an area of North West England which was Historic counties of England, historically a county. People of the area are known as Westmerians. The area includes part of the Lake District and the southern Vale of Eden. The county had an administrative function from the 12th century until 1974, when it was subsumed into Cumbria together with Cumberland, the Sedbergh Rural District, Sedbergh area of Yorkshire, and the Furness area of Lancashire. It gives its name to the Westmorland and Furness unitary authority area, which covers a larger area than the historic county. Early history Background At the beginning of the 10th century in England, 10th century a large part of modern day Cumbria was part of the Kingdom of Strathclyde, and was known as ''"Scottish Cumberland"''. The Rey Cross, Rere Cross was ordered by Edmund I (r.939–946) to serve as a boun ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Yorkshire
North Yorkshire is a Ceremonial counties of England, ceremonial county in Northern England.The Unitary authorities of England, unitary authority areas of City of York, York and North Yorkshire (district), North Yorkshire are in Yorkshire and the Humber, and Borough of Middlesbrough, Middlesbrough, Redcar and Cleveland, and Stockton-on-Tees Borough Council, Stockton-on-Tees are in North East England. It borders County Durham to the north, the North Sea to the east, the East Riding of Yorkshire to the south-east, South Yorkshire to the south, West Yorkshire to the south-west, and Cumbria and Lancashire to the west. The county is the largest in England by land area, at , and had a population of 1,158,816 in 2021. The largest settlements are Middlesbrough (148,215) in the north-east and the city of York (141,685) in the south. Middlesbrough is part of the Teesside built-up area, which extends into County Durham and had a total population of 376,663 in 2011. The remainder of the cou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ceremonial Counties Of England
Ceremonial counties, formally known as ''counties for the purposes of the lieutenancies'', are areas of England to which lord-lieutenant, lord-lieutenants are appointed. A lord-lieutenant is the Monarchy of the United Kingdom, monarch's representative in an area. Shrieval counties have the same boundaries and serve a similar purpose, being the areas to which High sheriff#England, Wales, and Northern Ireland, high sheriffs are appointed. High sheriffs are the monarch's judicial representative in an area. The ceremonial counties are defined in the Lieutenancies Act 1997, and the shrieval counties in the Sheriffs Act 1887. Both are defined as groups of Local government in England, counties used for local government. History The historic counties of England were originally used as areas for administering justice and organising the militia, overseen by a High sheriff, sheriff. From Tudor period, Tudor times onwards a lord-lieutenant was appointed to oversee the militia, taki ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Historic Counties Of England
The historic counties of England are areas that were established for administration by the Normans, in many cases based on earlier Heptarchy, kingdoms and shires created by the Angles (tribe), Angles, Saxons, Jutes, Celts and the Danes (tribe), Danes and Norsemen, Norse in the North. They are alternatively known as ''ancient counties'', ''traditional counties'', ''former counties'' or simply as ''counties''. In the centuries that followed their establishment, as well as their administrative function, the counties also helped define local culture and identity. This role continued even after the counties ceased to be used for administration after the creation of Administrative counties of England, administrative counties in 1889, which were themselves amended by further local government reforms in the years following. Unlike the partly self-governing Ancient borough, boroughs that covered urban areas, the counties of medieval England existed primarily as a means of enforcing cent ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Tyne
The River Tyne is a river in North East England. Its length (excluding tributaries) is . It is formed by the North Tyne and the South Tyne, which converge at Warden, Northumberland, Warden near Hexham in Northumberland at a place dubbed 'The Meeting of the Waters'. The Tyne Rivers Trust measure the whole Tyne Drainage basin, catchment as , containing of waterways. Course North Tyne The Ordnance Survey records 'the source of the North Tyne river' at grid reference NY 605974 at Deadwater, a few tens of metres short of the Scottish border. It flows southeast through the village of Kielder before entering first Bakethin Reservoir and then Kielder Water, both set within Kielder Forest. It then passes by the village of Bellingham, Northumberland, Bellingham before the River Rede enters as a left-bank tributary at Redesmouth. It passes Hadrian's Wall near Chollerford before joining the South Tyne near Warden to the northwest of Hexham. South Tyne The South Tyne rises at Tyne ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
