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Dufton Fell
Dufton is a village and civil parish in Cumbria, England. Historically part of Westmorland, it lies in the Eden Valley and below Great Dun Fell. It is mostly around 180m above sea level. At the 2001 census the parish had a population of 169, increasing to 204 at the 2011 Census The centre of the village is built around a green, on the north side of which is the Stag Inn. The village green is oblong in shape and is bisected by an avenue of lime trees that crosses it diagonally. Houses in the village were built from the 17th century onwards and the village has changed little over the last 100 years. History Dufton is an ancient settlement and some of the earliest written records of the village are from the 1320s. The place-name ''Dufton'' is first attested in 1289 and means 'dove town or farmstead'. The Rolls of Appointment report the "living" of the parish of Dufton in 1323. St Cuthbert's Church just outside the village mainly dates from the 19th century. Dufton was a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eden, Cumbria
Eden is a Non-metropolitan district, local government district in Cumbria, England, based at Penrith Town Hall in Penrith, Cumbria, Penrith. It is named after the River Eden, Cumbria, River Eden, which flows north through the district toward Carlisle, Cumbria, Carlisle. Its population of 49,777 at the United Kingdom Census 2001, 2001 census, increased to 52,564 at the 2011 Census. A 2019 estimate was 53,253. In July 2021 it was announced that in April 2023, Cumbria will divide into two Unitary authorities of England, unitary authorities. Eden District Council will cease and its functions pass to a new authority, Westmorland and Furness, covering the current districts of Borough of Barrow-in-Furness, Barrow-in-Furness, Eden and South Lakeland. Extent The Eden District area of 2,156 sq. km (832 square miles) makes it, since 2009, the eighth largest in England and the largest non-unitary authority, unitary district. It also has the lowest population density of any district in Engla ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pennine Way
The Pennine Way is a National Trail in England, with a small section in Scotland. The trail stretches for 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 Anglo-Scottish border, Scottish border. The path runs along the Pennines, Pennine hills, sometimes described as the "backbone of England". Although not the United Kingdom's longest National Trail (this distinction belongs to the South West Coast Path), it is according to The Ramblers "one of Britain's best known and toughest". History The path was the idea of the journalist and rambler Tom Stephenson (activist), Tom Stephenson, inspired by similar trails in the United States of America, particularly the Appalachian Trail. Stephenson proposed the concept in an article for the ''Daily Herald (UK newspaper), Daily Herald'' in 1935, and lobbied Parliament for the creation of an official trail. The walk was planned ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Villages In Cumbria
A village is a clustered human settlement or community, larger than a hamlet but smaller than a town (although the word is often used to describe both hamlets and smaller towns), with a population typically ranging from a few hundred to a few thousand. Though villages are often located in rural areas, the term urban village is also applied to certain urban neighborhoods. Villages are normally permanent, with fixed dwellings; however, transient villages can occur. Further, the dwellings of a village are fairly close to one another, not scattered broadly over the landscape, as a dispersed settlement. In the past, villages were a usual form of community for societies that practice subsistence agriculture, and also for some non-agricultural societies. In Great Britain, a hamlet earned the right to be called a village when it built a church. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dufton
Dufton is a village and civil parish in Cumbria, England. Historically part of Westmorland, it lies in the Eden Valley and below Great Dun Fell. It is mostly around 180m above sea level. At the 2001 census the parish had a population of 169, increasing to 204 at the 2011 Census The centre of the village is built around a green, on the north side of which is the Stag Inn. The village green is oblong in shape and is bisected by an avenue of lime trees that crosses it diagonally. Houses in the village were built from the 17th century onwards and the village has changed little over the last 100 years. History Dufton is an ancient settlement and some of the earliest written records of the village are from the 1320s. The place-name ''Dufton'' is first attested in 1289 and means 'dove town or farmstead'. The Rolls of Appointment report the "living" of the parish of Dufton in 1323. St Cuthbert's Church just outside the village mainly dates from the 19th century. Dufton was a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Listed Buildings In Dufton
Dufton is a civil parish in the Eden District, Cumbria, England. It contains eleven listed buildings that are recorded in the National Heritage List for England The National Heritage List for England (NHLE) is England's official database of protected heritage assets. It includes details of all English listed buildings, scheduled monuments, register of historic parks and gardens, protected shipwrecks, a .... All the listed buildings are designated at Grade II, the lowest of the three grades, which is applied to "buildings of national importance and special interest". The parish contains the village of Dufton and the surrounding countryside. Most of the listed buildings are houses and associated structures, farmhouses and farm buildings in the village centre. Also in the village is a listed pump. Away from the centre of the village, and listed, are a church, its rectory and structures in the rectory garden. __NOTOC__ Buildings References Citations Sources * ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Helm Wind
The Helm Wind is a named wind in Cumbria, England, a strong north-easterly wind which blows down the south-west slope of the Cross Fell escarpment. It is the only named wind in the British Isles, although many other mountain regions in Britain exhibit the same phenomenon when the weather conditions are favourable. It may take its name from the helmet or cap of cloud which forms above Cross Fell, known as the Helm Bar, since a line of clouds over the fells can predict and accompany a Helm. Research into the helm wind was carried out by Gordon Manley in the 1930s. He interpreted the phenomenon in hydrodynamic terms as a " standing wave" and "rotor", a model confirmed in 1939 by glider flights. The dale at the head of the Eden Valley has its own Helm Wind, which sweeps over Mallerstang Mallerstang is a civil parish in the extreme east of Cumbria, and, geographically, a dale at the head of the upper Eden Valley. Originally part of Westmorland, it lies about south of the neares ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
High Cup
High Cup Gill (or High Cup Nick or just High Cup), almost a geometrically perfect U-shaped chasm, is a valley deeply incised into the Pennines, 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 U-shaped valley, glacial in origin, ice having over-ridden the area during successive ice ages. To its southeast is Murton, Cumbria, Murton Fell whilst Dufton Fell is to the north. The Ordnance Survey name the valley as High Cup Gill but it is often referred to by the name High Cup Nick, a name which properly refers in a more limited sense to the point at its northeastern limit where the headwaters of Highcup Gill Beck pass from the relatively flat terrain of High Cup Plain over the lip of High Cup Scar into the valley. 'Gill' is a word of Norse origin meaning narrow valley or ravine whilst 'beck' signifies a stream; both occur widely in the hills of northern England. As seen in the classic view ... [...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] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ancient Woodland
In the United Kingdom, an ancient woodland is a woodland that has existed continuously since 1600 or before in England, Wales and Northern Ireland (or 1750 in Scotland). Planting of woodland was uncommon before those dates, so a wood present in 1600 is likely to have developed naturally. In most ancient woods, the trees and shrubs have been cut down periodically as part of the management cycle. Provided that the area has remained as woodland, the stand is still considered ancient. Since it may have been cut over many times in the past, ancient woodland does not necessarily contain very old trees. For many species of animal and plant, ancient woodland sites provide the sole habitat, and for many others, conditions on these sites are much more suitable than those on other sites. Ancient woodland in the UK, like rainforest in the tropics, is home to rare and threatened species. For these reasons ancient woodland is often described as an irreplaceable resource, or 'critical natural ca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gill (stream)
A gill or ghyll is a ravine or narrow valley in the North of England and other parts of the United Kingdom. The word originates from the Old Norse . Examples include Dufton Ghyll Wood, Dungeon Ghyll, Troller's Gill and Trow Ghyll. As a related usage, Gaping Gill is the name of a cave, not the associated stream, and Cowgill, Masongill and Halton Gill are derived names of villages. The stream flowing through a gill is often referred to as a beck: for example in Swaledale, Gunnerside Beck flows through Gunnerside Ghyll. ''Beck ''is also used as a more general term for streams in the north of England – examples include Ais Gill Beck, Arkle Beck and Peasey Beck. In the North Pennines, the word sike or syke is found in similar circumstances. This is particularly common in the Appleby Fells area where sikes significantly outnumber the becks and gills; it can also be seen in the name of Eden Sike Cave in Mallerstang. In the High Weald gills are deeply cut ravines, usually with a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Knock, Cumbria
Knock is a small village in the Eden district of Cumbria, England, and 1.9 km northwest of the larger village of Dufton and 3.1 km south of the village of Milburn. It lies midway between Cross Fell to the north and the town of Appleby-in-Westmorland to the south. Knock is situated 1 km east of the small hamlet and farm, Knock Cross. History, geography and etymology The place-name 'Knock' is first attested in a Yorkshire charter from between 1150 and 1162, where it appears as ''Chonoc-salchild''. It appears as ''Knok'' in an '' Inquisition post mortem'' of 1323. The name means 'hillock', from the Brittonic ''*cnuc'', Old Irish ''cnocc'' or Irish ''cnoc''; an apparent reference to the nearby Knock Pike, which is 1,306 feet high, and can be seen in the photo to the right. Circa 1870, it had a population of 197 as recorded in the Imperial Gazetteer of England and Wales. Knock is also shown on Thomas Jefferys's 1770 map of Westmorland. Knock once had a Methodist ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saunders_Quarry-1.jpg "Click for more on -> Sandstone")
