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Teesdale District Council
Teesdale is a dale, or valley, in Northern England. The dale is in the River Tees’s drainage basin, most water flows stem from or converge into said river, including the Skerne and Leven. Upper Teesdale, more commonly just Teesdale, falls between the Durham and Yorkshire Dales. Large parts of Upper Teesdale are in the North Pennines AONB (Area of Outstanding Natural Beauty) - the second largest AONB in England and Wales. The River Tees rises below Cross Fell, the highest hill in the Pennines at , and its uppermost valley is remote and high. The local climate was scientifically classified as "Sub-Arctic" and snow has sometimes lain on Cross Fell into June (there is an alpine ski area Yad Moss). Lower Teesdale has mixed urban (Tees Valley or Teesside) and rural (Cleveland) parts. Roseberry Topping is a notable hill on the south eastern side, of which this and other adjoining hills form the northern end of the North York Moors. Newer terms have gained stronger associations w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tees Valley
Tees Valley is a mayoral combined authority and Local enterprise partnership area in northern England, around the River Tees. The area is not a geographical valley. The LEP was established in 2011 and the combined authority was established in 2016, the latter after public consultation in 2015. The area covers five council areas: Darlington, Hartlepool, Middlesbrough, Redcar and Cleveland and Stockton-on-Tees. Administrating the area is the Tees Valley Combined Authority, consisting of a mayor and six selected chairs; local enterprise partnership chair and a chair for each unitary authority. The town of Middlesbrough is the largest population centre in the area. The borough of Middlesbrough is the smallest of the five at only and a population of : the Stockton-on-Tees borough (including multiple towns) is the largest with and a population of , as of Before the region, from 1968 until 1974, parts of the area had been under the County Borough of Teesside council area. This ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dale (landform)
A dale is an open valley. ''Dale'' is a synonym of the word ''valley''. The name is used when describing the physical geography of an area. It is used most frequently in the Lowlands of Scotland and in the North of England; the term "fell" commonly refers to the mountains or hills that flank the dale. Etymology The word ''dale'' comes from the Old English word ''dæl'', from which the word " dell" is also derived. It is also related to Old Norse word ''dalr'' (and the modern Icelandic word ''dalur''), which may perhaps have influenced its survival in northern England. The Germanic origin is assumed to be *''dala-''. ''Dal-'' in various combinations is common in placenames in Norway. Modern English valley and French vallée are presumably not related to dale. A distant relative of ''dale'' is currency unit dollar, stemming from German ''thaler'' or ''daler'', short for joachimsthaler coins manufactured in the town of Joachimsthal in Bohemia.Falk, Hjalmar (1991). ''Etymologi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Igneous
Igneous rock (derived from the Latin word ''ignis'' meaning fire), or magmatic rock, is one of the three main rock types, the others being sedimentary and metamorphic. Igneous rock is formed through the cooling and solidification of magma or lava. The magma can be derived from partial melts of existing rocks in either a planet's mantle or crust. Typically, the melting is caused by one or more of three processes: an increase in temperature, a decrease in pressure, or a change in composition. Solidification into rock occurs either below the surface as intrusive rocks or on the surface as extrusive rocks. Igneous rock may form with crystallization to form granular, crystalline rocks, or without crystallization to form natural glasses. Igneous rocks occur in a wide range of geological settings: shields, platforms, orogens, basins, large igneous provinces, extended crust and oceanic crust. Geological significance Igneous and metamorphic rocks make up 90–95% of the top ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North York Moors
The North York Moors is an upland area in north-eastern Yorkshire, England. It contains one of the largest expanses of Calluna, heather moorland in the United Kingdom. The area was designated as a national parks of England and Wales, National Park in 1952, through the National Parks and Access to the Countryside Act 1949. Covering an area of , the National Park has a population of 23,380. It is administered by the North York Moors National Park Authority, whose head office is based in Helmsley. Location and transport To the east the area is clearly defined by the impressive cliffs of the North Sea coast. The northern and western boundaries are defined by the steep scarp slopes of the Cleveland Hills edging the Tees lowlands and the Hambleton Hills above the Vale of Mowbray. To the south lies the broken line of the Tabular Hills and the Vale of Pickering. Four roads cross the North York Moors from north to south. In the east the A171 road, A171 joins Whitby and Scarborough, Nor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cleveland Hills
The Cleveland Hills are a range of hills on the north-west edge of the North York Moors in North Yorkshire, England, overlooking Cleveland and Teesside. They lie entirely within the boundaries of the North York Moors National Park. Part of the long Cleveland Way National Trail runs along the hills, and they are also crossed by a section of Wainwright's Coast to Coast Walk. The hills, which rise abruptly from the flat Tees Valley to the north, include distinctive landmarks such as the cone-shaped peak of Roseberry Topping, near the village of Great Ayton – childhood home of Captain James Cook. Geology The hills are formed by multiple stacked layers of Jurassic age sedimentary rocks. The scarp rises above the low ground to the north and west formed by the mudstones of the Redcar Mudstone Formation, though largely buried beneath glacial till from the last ice age. The same formation also provides the lowermost slopes of the scarp. The full sequence, presented in stratigraph ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Roseberry Topping
Roseberry Topping is a distinctive hill in North Yorkshire, England. It is situated near Great Ayton and Newton under Roseberry. Its summit has a distinctive half-cone shape with a jagged cliff, which has led to many comparisons with the much higher Matterhorn in the Swiss-Italian Alps.Howard Peach, ''Curious Tales of Old North Yorkshire'', p. 39 (Sigma Leisure, 2004) It forms a symbolic image of the area and features in the logo for the nearby Teesside International Airport. At , Roseberry Topping was traditionally thought to be the highest hill on the North York Moors; however, there are 15 higher peaks with the nearby Urra Moor being the highest, at . Roseberry Topping offers views of Captain Cook's Monument at Easby Moor and the monument at Eston Nab, previously a beacon. Geology The hill is an outlier of the North York Moors uplands. It is formed from sandstone laid down in the Middle and Lower Jurassic periods, between 208 and 165 million years ago, which constitutes th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cross Fell
Cross Fell is the highest mountain in the Pennines of Northern England and the highest point in England outside the Lake District. It is located in the North Pennines Area of Outstanding Natural Beauty. It lies within the county of Cumbria and the historic county boundaries of Cumberland. The summit, at , is a stony plateau, part of a ridge running north-west to south-east, which also incorporates Little Dun Fell at and Great Dun Fell at . The three adjoining fells form an escarpment that rises steeply above the Eden Valley on its south-western side and drops off more gently on its north-eastern side towards the South Tyne and Tees Valleys. Cross Fell summit is crowned by a cross-shaped dry-stone shelter. On a clear day there are excellent views from the summit across the Eden Valley to the mountains of the Lake District. On the northern side of Cross Fell there are also fine views across the Solway Firth to the Southern Uplands of Scotland. The fell is prone to dense hil ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
AONB
An Area of Outstanding Natural Beauty (AONB; , AHNE) is an area of countryside in England, Wales, and Northern Ireland, that has been designated for conservation due to its significant landscape value. 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. In place of 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 unlike national parks the responsible bodies do not have their own planning powers. They also differ from national parks in their more limited opportunities for extensive outdoor recreation. History The idea for what would eventually become the AONB designation was first put forward by John Dower in his 1945 ''Report to the Government on National Parks in England and Wales''. Dower ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Pennines
The North Pennines is the northernmost section of the Pennine range of hills which runs north–south through northern England. It lies between Carlisle to the west and Darlington to the east. It is bounded to the north by the Tyne Valley and to the south by the Stainmore Gap. Overview The North Pennines was designated as an Area of Outstanding Natural Beauty (AONB) in 1988 for its moorland scenery, the product of centuries of farming and lead-mining, and is also a UNESCO Global Geopark. At almost , it is the second largest of the 49 AONBs in the United Kingdom. The landscape of the North Pennines AONB is one of open heather moors between deep dales, upland rivers, hay meadows and stone-built villages, some of which contain the legacies of a mining and industrial past. The area has previously been mined and quarried for minerals such as barytes, coal fluorspar, iron, lead, witherite and zinc. Natural England maps Maps for North Pennines – Area of Outstanding Natural Beauty, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yorkshire Dales
The Yorkshire Dales is an upland area of the Pennines in the Historic counties of England, historic county of Yorkshire, England, most of it in the Yorkshire Dales National Park created in 1954. The Dales comprise river valleys and the hills rising from the Vale of York westwards to the hilltops of the Pennine Drainage divide, watershed. In Ribblesdale, Dentdale and Garsdale, the area extends westwards across the watershed, but most of the valleys drain eastwards to the Vale of York, into the River Ouse, Yorkshire, Ouse and the Humber. The extensive limestone cave systems are a major area for caving in the UK and numerous walking trails run through the hills and dales. Etymology The word ''Dale (landform), dale'', like ''dell'', is derived from the Old English word ''dæl''. It has cognates in the North Germanic languages, Nordic/Germanic languages, Germanic words for valley (''dal'', ''tal''), and occurs in valley names across Yorkshire and Northern England. Usage here may have ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Durham Dales
The Durham Dales is the name given to a large area of landscape in the west of County Durham, consisting primarily of the Durham portion of the North Pennines, in England. Geography The Durham Dales consist primarily of a series of high exposed moorlands, hills and mountains, a number exceeding a height of 2,000 ft above sea level, along with the valleys or dales, from which the area gets its name. These valleys include Teesdale and Weardale. The area covers roughly one third of County Durham and is its least populous area. Settlements There are just a few market towns within the area—Barnard Castle, Consett, Middleton-in-Teesdale, Stanhope, Tow Law, and Wolsingham,—though some also consider the Durham Dales to extend as far east as Bishop Auckland and Crook. There are a number of small villages in the area, which in general tend to be sparsely populated and spread out, in great contrast to much of the rest of County Durham. Geology Like much of the North Pe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Upper Teesdale
Upper Teesdale is a Site of Special Scientific Interest (SSSI) in the west County Durham, England. It encompasses an extensive upland area that includes the headwaters of the River Tees and the surrounding catchment area upstream of the village of Langdon Beck. The site has a diverse mix of habitats, mainly dry heath, with wet heath and blanket bog, blanket mire in areas that are poorly drained. The Upper Teesdale SSSI is one of the most important botanical sites in Britain; the flora is exceptionally rich in species that are nationally rare, including some that are Relict (biology), relicts of the arctic-alpine environment of the last glacial period. The area supports internationally important populations of some wader, wading birds and is home to several rare invertebrates. Within the SSSI are several locations that are of national importance geologically, including one of only two known outcrops of 'sugar' limestone in Britain. The southern part of the SSSI largely coinc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
