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The Durham Dales are a series of valleys in the west of County Durham, North East England. They are the Durham portion of the North Pennines, the northernmost part of the Pennine uplands. The principal valleys are Teesdale in the south and Weardale in the north, each of which has several side valleys, including Baldersdale, Lunedale, and Rook Hope. The part of Teesdale south of the Tees was historically in Yorkshire.
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.
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.
Like much of the North Pennines, the Durham Dales form an anticline, with carboniferous limestone exposed at the surface. The Durham Dales, like much of the Pennines, have long been exploited for their rich mineralogical resources, notably lead and ironstone.
Many of the high hills are occupied by moors with peat-mosses, the higher ground being uncultivable and barely fit for pastures. As with much of the landscape of the Pennines, they are generally upland areas of high moorland indented by the more fertile valleys of various rivers and streams.
The Durham Dales constitute the principal watershed for the county of Durham, as well as contributing to those of the neighbouring counties of Cumbria, Northumberland and North Yorkshire. The rivers Wear, Tees and Derwent all rise in the Durham Dales and flow eastward towards the North Sea. The Derwent helps to form County Durham's northerly border, and the Tees traditionally its southern border.
Along the course of the Tees are the three attractions of the High Force, Low Force and Cauldron Snout waterfalls.
North Yorkshire is a ceremonial county in the Yorkshire and the Humber and North East regions of 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. Northallerton is the county town.
The North York Moors is an upland area in north-eastern Yorkshire, England. It contains one of the largest expanses of heather moorland in the United Kingdom. The area was designated as a National Park in 1952, through the National Parks and Access to the Countryside Act 1949. Covering an area of 554 sq mi (1,430 km2), the National Park has a population of 23,380. It is administered by the North York Moors National Park Authority, which is based in Helmsley.
The River Tees, in England, rises on the eastern slope of Cross Fell in the North Pennines and flows eastwards for 85 miles (137 km) 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.
The Pennines, also known as the Pennine Chain or Pennine Hills, are a range of uplands mainly located in Northern England. Commonly described as the "backbone of England" because of its length and position, the range runs from Derbyshire and Staffordshire in the North Midlands to Northumberland in North East England, near the Anglo-Scottish border. The range starts near the valley of the River Trent to the south and extends northwards across the Peak District, South Pennines, Yorkshire Dales, and North Pennines, ending at the Tyne Gap. Beyond the gap are the Border Moors and Cheviot Hills, which are included in some definitions of the range.
The Pennine Way is a National Trail in England, with a small section in Scotland. The trail stretches for 268 miles (431 km) from Edale, in the northern Derbyshire Peak District, north through the Yorkshire Dales and Northumberland National Park and ends at Kirk Yetholm, just inside the Scottish border. The path runs along the Pennine hills, sometimes described as the "backbone of England". Although not the United Kingdom's longest National Trail, it is according to The Ramblers, "one of Britain's best known and toughest".
County Durham, officially simply Durham (/ˈdʌrəm/), is a ceremonial county in North East England. The county borders Northumberland and Tyne and Wear to the north, the North Sea to the east, North Yorkshire to the south, and Cumbria to the west. The largest settlement is Darlington.
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.
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.
Holwick is a small village in Teesdale, County Durham (district), England. Located in the Pennine hills, it consists of a few houses spread along a road in the pattern of a linear settlement. As the population taken at the 2011 Census was less than 100, details are maintained in the parish of Lunedale.
Weardale is a dale, or valley, on the east side of the Pennines in County Durham, England. Large parts of Weardale fall within the North Pennines Area of Outstanding Natural Beauty (AONB) – the second-largest AONB in England and Wales. The upper dale is surrounded by high fells and heather grouse moors. The River Wear flows through Weardale before reaching Bishop Auckland and then Durham, meeting the sea at Sunderland.
Mickle Fell is a mountain in the Pennines, the range of hills and moors running down the middle of Northern England. It has a maximum elevation of 788 m (2,585 ft). It lies slightly off the main watershed of the Pennines, about 10 miles south of Cross Fell. After Cross Fell, Mickle Fell is the highest Marilyn within the North Pennines designated Area of Outstanding Natural Beauty (AONB).
England comprises most of the central and southern two-thirds of the island of Great Britain, in addition to a number of small islands of which the largest is the Isle of Wight. England is bordered to the north by Scotland and to the west by Wales. It is closer to continental Europe than any other part of mainland Britain, divided from France only by a 33 km (21 mi) sea gap, the English Channel. The 50 km (31 mi) Channel Tunnel, near Folkestone, directly links England to mainland Europe. The English/French border is halfway along the tunnel.
Burnhope Seat is a high moorland fell in the North Pennines Area of Outstanding Natural Beauty (AONB) in northern England. It lies between the heads of the Rivers Tees, South Tyne and Wear. The summit is crossed by the boundary between County Durham and Cumbria. The trig point is the highest point in historic County Durham. However, this is not quite the summit of the mountain. Mickle Fell, south of Teesdale is higher than Burnhope Seat and is sometimes quoted as being the highest top of County Durham, but this is historically not correct. Mickle Fell, although it lies within the unitary council area of Durham County Council for administrative purposes, is historically a part of the North Riding of Yorkshire, and is the highest point in that county.
The mountains and hills of England comprise very different kinds of terrain, from a mountain range which reaches almost 1,000 metres high, to several smaller areas of lower mountains, foothills and sea cliffs. Most of the major upland areas have been designated as Areas of Outstanding Natural Beauty (AONB) or national parks. The highest and most extensive areas are in the north and west, while the midlands, south-east and east of the country tend to be low-lying.
In Yorkshire there is a very close relationship between the major topographical areas and the geological period in which they were formed. The Pennine chain of Hills in the west is of Carboniferous origin. The central vale is Permo-Triassic. The North York Moors in the north-east of the county are Jurassic in age while the Yorkshire Wolds to the south east are Cretaceous chalk uplands. The plain of Holderness and the Humberhead levels both owe their present form to the Quaternary ice ages.
The Geology of Yorkshire in northern England shows a very close relationship between the major topographical areas and the geological period in which their rocks were formed. The rocks of the Pennine chain of hills in the west are of Carboniferous origin whilst those of the central vale are Permo-Triassic. The North York Moors in the north-east of the county are Jurassic in age while the Yorkshire Wolds to the south east are Cretaceous chalk uplands. The plain of Holderness and the Humberhead levels both owe their present form to the Quaternary ice ages. The strata become gradually younger from west to east.
The River Wear in Northern England rises in the Pennines and flows eastwards, mostly through County Durham, to the North Sea in the City of Sunderland. At 60 mi (97 km) long, it is one of the region's longest rivers. The Wear wends in a steep valley through the cathedral city of Durham and gives its name to Weardale in its upper reach and Wearside by its mouth.
The geology of County Durham in northeast England consists of a basement of Lower Palaeozoic rocks overlain by a varying thickness of Carboniferous and Permo-Triassic sedimentary rocks which dip generally eastwards towards the North Sea. These have been intruded by a pluton, sills and dykes at various times from the Devonian Period to the Palaeogene. The whole is overlain by a suite of unconsolidated deposits of Quaternary age arising from glaciation and from other processes operating during the post-glacial period to the present. The geological interest of the west of the county was recognised by the designation in 2003 of the North Pennines Area of Outstanding Natural Beauty as a European Geopark.