Low Force is an 18-foot (5.5m) high set of falls on the River Tees, England, UK. Further upstream is the High Force waterfall. Low Force is also the site of the Wynch Bridge, completed in 1830. It is suggested by signs at each end that only one person at a time should cross the bridge as it may be unstable.
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 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".
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, 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.
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.
Newbiggin is a village and civil parish in County Durham, England. At the 2011 census the parish had a population of 146. It is situated on the north side of Teesdale, opposite Holwick. An influx of Derbyshire lead miners into the area in the late 18th century may have brought the name from Biggin. The village is within the North Pennines Area of Outstanding Natural Beauty (AONB).
Middleton-in-Teesdale is a market town and civil parish in County Durham, England. It is in Teesdale, on the River Tees's north banks, and surrounded by the North Pennines. The town is between Eggleston and Newbiggin, a few miles to the north-west of Barnard Castle.
Hardraw Force is a waterfall on Hardraw Beck in Hardraw Scar, a wooded ravine just outside the hamlet of Hardraw, 0.9 miles (1.5 km) north of the town of Hawes, Wensleydale, in the Yorkshire Dales. The Pennine Way long distance footpath passes close by.
The Whin Sill or Great Whin Sill is a tabular layer of the igneous rock dolerite in County Durham, Northumberland and Cumbria in the northeast of England. It lies partly in the North Pennines Area of Outstanding Natural Beauty and partly in Northumberland National Park and stretches from Teesdale northwards towards Berwick.
Cauldron Snout is a cascade on the upper reaches of the River Tees in Northern England, immediately below the dam of the Cow Green Reservoir. It is well upstream of the High Force waterfall, and is on the boundary between County Durham and Cumbria, England. The waterfall lies within the North Pennines Area of Outstanding Natural Beauty (AONB) and European Geopark.
The geology of England is mainly sedimentary. The youngest rocks are in the south east around London, progressing in age in a north westerly direction. The Tees–Exe line marks the division between younger, softer and low-lying rocks in the south east and the generally older and harder rocks of the north and west which give rise to higher relief in those regions. The geology of England is recognisable in the landscape of its counties, the building materials of its towns and its regional extractive industries.
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.
Middleton Quarry is a Site of Special Scientific Interest in the Teesdale district of west County Durham, England. It is a disused quarry, from which Whin Sill stone was formerly excavated. It lies just south of the River Tees, opposite the village of Middleton-in-Teesdale on the river's northern bank.
Park End Wood is a Site of Special Scientific Interest in the Teesdale district of west County Durham, England. The site occupies a low hill of Whin Sill on the southern edge of the River Tees floodplain just over 2 km upstream from the village of Middleton-in-Teesdale. It adjoins the Upper Teesdale SSSI to the south, and the Middle Crossthwaite and Stonygill Meadows SSSIs are nearby.
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.
The geology of Northumberland in northeast England includes a mix of sedimentary, intrusive and extrusive igneous rocks from the Palaeozoic and Cenozoic eras. Devonian age volcanic rocks and a granite pluton form the Cheviot massif. The geology of the rest of the county is characterised largely by a thick sequence of sedimentary rocks of Carboniferous age. These are intruded by both Permian and Palaeogene dykes and sills and the whole is overlain by unconsolidated sediments from the last ice age and the post-glacial period. The Whin Sill makes a significant impact on Northumberland's character and the former working of the Northumberland Coalfield significantly influenced the development of the county's economy. The county's geology contributes to a series of significant landscape features around which the Northumberland National Park was designated.
High Cup Gill, almost a geometrically perfect U-shaped chasm, is a valley deeply incised into the Pennine scarp to the northeast of Appleby-in-Westmorland in Cumbria and within the North Pennines AONB in northern England. It is considered to be glacial in origin, ice having over-ridden the area during successive ice ages. To its southeast is Murton Fell and Dufton Fell is to the north.
The geology of Northumberland National Park in northeast England includes a mix of sedimentary, intrusive and extrusive igneous rocks from the Palaeozoic and Cenozoic eras. Devonian age volcanic rocks and a granite pluton form the Cheviot massif. The geology of the rest of the national park is characterised largely by a thick sequence of sedimentary rocks of Carboniferous age. These are intruded by Permian dykes and sills, of which the Whin Sill makes a significant impact in the south of the park. Further dykes were intruded during the Palaeogene period. The whole is overlain by unconsolidated sediments from the last ice age and the post-glacial period.
The Great Flood of 1771 affected several rivers, including the Tyne, Tees, Wear and Eden and settlements across northern England from 16 and 17 November 1771. Its cause was a sudden thaw of the ice in upper Teesdale, a cloud burst over the Pennines and a continuous period of rain.
