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 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 whilst Dufton Fell is to the north.
| Attributes | Values |
|---|
| rdf:type
| |
| rdfs:label
| |
| rdfs:comment
| - 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 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 whilst Dufton Fell is to the north. (en)
|
| geo:lat
| |
| geo:long
| |
| foaf:depiction
| |
| dcterms:subject
| |
| Wikipage page ID
| |
| Wikipage revision ID
| |
| Link from a Wikipage to another Wikipage
| |
| sameAs
| |
| dbp:wikiPageUsesTemplate
| |
| thumbnail
| |
| georss:point
| |
| has abstract
| - 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 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 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 southwest over the valley into the Vale of Eden from its head at High Cup Nick, it is considered one of the finest natural features in northern England. High Cup Scar is formed by a near-horizontal outcrop of the Whin Sill, a dolerite intrusion of late Carboniferous age which underlies much of the North Pennines and northeast England. Tumbled blocks of this rock are scattered down the scree slopes beneath the scar. A notable pinnacle of this rock on the northern side of the valley is known as Nichol or Nichol's Chair after a local cobbler who, for a bet, practised his craft perched on its summit. The country rock into which the sill is intruded is the Alston Formation, a part of the Yoredale Group of multiple layers of limestones, sandstones, siltstones and mudstones. At the base of the gill, though largely obscured by the dolerite blocks, are older rocks: the sedimentary rocks of the Ravenstonedale Group and, beneath them, the metamorphosed slates and sandstones of the Skiddaw Group which date from the Ordovician period. The Pennine Way skirts the valley on its northern side by a traditional route known as 'Narrow Gate' as it runs from Dufton east via Maize Beck and Cauldron Snout to Forest in Teesdale. This national trail briefly splits into two separate routes running on either bank of Maize Beck; it is the southerly of the two which leads via High Cup Nick. Listed in the 100 best Pathfinder walks in Britain, High Cup Nick has been described as a difficult walk of 8 miles, with an elevation of 1,445 feet. The famous fellwalker Alfred Wainwright describes High Cup as "a great moment on the journey" in his book Pennine Way Companion. The village of Dufton lies between two of the most challenging sections of the Pennine Way. There are precipitous drops along the higher sections of the walk and the Helm Wind blowing through the valley can be very strong. The whole of the valley is within an area mapped as open country under the Countryside and Rights of Way Act 2000, hence there is a general right for walkers to roam at will. This section of the Pennine Way is a bridleway, and is therefore legally available to cyclists and horseriders too. (en)
|
| prov:wasDerivedFrom
| |
| page length (characters) of wiki page
| |
| foaf:isPrimaryTopicOf
| |
| geo:geometry
| - POINT(-2.4070000648499 54.623001098633)
|
| is Link from a Wikipage to another Wikipage
of | |
| is Wikipage redirect
of | |
| is foaf:primaryTopic
of | |
![[RDF Data]](/fct/images/sw-rdf-blue.png)
![[cxml]](/fct/images/cxml_doc.png)
![[csv]](/fct/images/csv_doc.png)
![[text]](/fct/images/ntriples_doc.png)
![[turtle]](/fct/images/n3turtle_doc.png)
![[ld+json]](/fct/images/jsonld_doc.png)
![[rdf+json]](/fct/images/json_doc.png)
![[rdf+xml]](/fct/images/xml_doc.png)
![[atom+xml]](/fct/images/atom_doc.png)
![[html]](/fct/images/html_doc.png)
