World Library  
Flag as Inappropriate
Email this Article

Northern Fells

Article Id: WHEBN0013331421
Reproduction Date:

Title: Northern Fells  
Author: World Heritage Encyclopedia
Language: English
Subject: Lake District, Skiddaw, Blencathra, Skiddaw Little Man, Esk Pike, Binsey, Knott, Carl Side, Mungrisdale Common, Latrigg
Collection:
Publisher: World Heritage Encyclopedia
Publication
Date:
 

Northern Fells

The Northern Fells are a mountain range in the English Lake District. Including Skiddaw, they occupy a wide area to the north of Keswick. Smooth sweeping slopes predominate with a minimum of tarns or crags. Blencathra in the south east of the group is the principal exception to this trend.

Partition of the Lakeland Fells

The Lake District is a National Park in the north west of the country which, in addition to its lakes, contains a complex range of hills. These are known locally as fells and range from low hills to the highest ground in England. Hundreds of tops exist and many writers have attempted to draw up definitive lists. In doing so the compilers frequently divide the range into smaller areas to aid their description.

The most influential of all such authors was Alfred Wainwright whose Pictorial Guide to the Lakeland Fells series has sold in excess of 2 million copies,[1] being in print continuously since the first volume was published in 1952. Wainwright divided the fells into seven geographical areas, each surrounded by valleys and low passes. While any such division must be arbitrary- and later writers have deviated to a greater or lesser extent from this blueprint-[2][3] Wainwright's sevenfold division remains the best known partitioning of the fells into 'sub ranges', each with its own characteristics. The Northern Fells are one of these divisions, covered by volume 5 of Wainwright's work.[4]

Boundaries

The Northern Fells form a self-contained unit, quite remote from the other ranges. The western boundary is formed by the course of the River Derwent north of Keswick and the southern perimeter by the River Greta, one of its principal feeders. The River Caldew bounds the eastern edge of the group, flowing away toward Carlisle. At Caldbeck the Calder is joined by the Whelpo Beck which drains many of the northern slopes. Only on the east, between the headwaters of the Greta and Caldew, does a bridge of higher ground strike out to connect with the rest of Lakeland, a long ridge curving southward to connect with Great Mell Fell in the Eastern Fells. This ridge, whilst significant topographically, is in many places unnoticed on the ground. The deep trough of Bassenthwaite wards off the North Western Fells, while the Central Fells rise beyond Keswick and the Greta.

North of the area defined by Wainwright the countryside takes on a moorland character, gradually declining toward the Solway Firth. Some of the minor tops in this area were covered by Wainwright in his later Outlying Fells volume, published in 1974.

Topography

The Northern Fells occupy a circular area about 10 miles in diameter. The centre is slightly lower, an area of upland grazing and marshland known as Skiddaw Forest. This name may be misleading since the only trees form the windbreak of Skiddaw House. This isolated building, 3 miles from roads or other habitation, was once a shepherd's bothy. It currently serves as a youth hostel. Skiddaw Forest stands at the head of the three major rivers of the Northern Fells. The Caldew begins eastward, Dash Beck flows north west and the Glenderaterra to the south. These streams divide the circular area into three distinct sections.

The highest ground is in the south west, between the Glenderaterra and Dash Beck. This is the Skiddaw group, well known in views down Borrowdale and Derwentwater. The steep but sweeping slopes, deep folds and smooth texture can best be described as resembling a heavy sheet of velvet laid over a supporting frame. Skiddaw stands in the centre of the group, surrounded by its many satellites. Above Bassenthwaite are Ullock Pike, Long Side, Carl Side and the sometimes wooded Dodd. Eastward are Skiddaw Little Man, Lonscale Fell and the diminutive Latrigg, a pleasant short climb from Keswick.


The south eastern sector is formed around Blencathra with its blasted crags and knife-edge ridges overlooking the Keswick to Penrith road. The northern ridges lead to Souther Fell (of 'Spectral Army' fame), Bannerdale Crags, Bowscale Fell and Mungrisdale Common, the most inexplicable of Wainwight's choice of fells with a barely discernible summit.

The northern section is known commonly as 'Back o'Skiddaw' and contains many lower fells of a gentler nature, although the paths to climb them can be long. In these hills are many evidences of historic mining activity, a testament to the mineral wealth beneath. The group has a central apex at Knott with Great Calva standing to the south above Skiddaw Forest. High Pike (Caldbeck) and Carrock Fell rise to the east, marching along the Caldew valley. The western ridges are more complex and include Great Sca Fell, Meal Fell, Great Cockup, Brae Fell and Longlands Fell. Alone to the extreme west across the tarn of Over Water stands Binsey.

Access for walkers

The Northern Fells are entirely surrounded by roads, but traversed by none. Keswick and Threlkeld provide good access to the south from the A66 road for the Skiddaw and Blencathra groups respectively. The minor road along the eastern boundary connects the hamlets of Mosedale and Mungrisdale and gives equally good access to the Caldew and other eastern valleys. Further minor roads circuit the northern perimeter for operations Back o'Skiddaw, connecting finally to the Keswick - Carlisle road along the shore of Bassenthwaite. From here the Dash Valley and Longside Edge can be gained. A service track follows Dash Beck past its major fall (Whitewater Dash) to Skiddaw House, the easiest entrance to Skiddaw Forest.

The tourist route up Skiddaw will generally be busy, but solitude can easily be found on the northern fells.

See also

Cumbria portal

References

This article was sourced from Creative Commons Attribution-ShareAlike License; additional terms may apply. World Heritage Encyclopedia content is assembled from numerous content providers, Open Access Publishing, and in compliance with The Fair Access to Science and Technology Research Act (FASTR), Wikimedia Foundation, Inc., Public Library of Science, The Encyclopedia of Life, Open Book Publishers (OBP), PubMed, U.S. National Library of Medicine, National Center for Biotechnology Information, U.S. National Library of Medicine, National Institutes of Health (NIH), U.S. Department of Health & Human Services, and USA.gov, which sources content from all federal, state, local, tribal, and territorial government publication portals (.gov, .mil, .edu). Funding for USA.gov and content contributors is made possible from the U.S. Congress, E-Government Act of 2002.
 
Crowd sourced content that is contributed to World Heritage Encyclopedia is peer reviewed and edited by our editorial staff to ensure quality scholarly research articles.
 
By using this site, you agree to the Terms of Use and Privacy Policy. World Heritage Encyclopedia™ is a registered trademark of the World Public Library Association, a non-profit organization.
 


Copyright © World Library Foundation. All rights reserved. eBooks from Project Gutenberg are sponsored by the World Library Foundation,
a 501c(4) Member's Support Non-Profit Organization, and is NOT affiliated with any governmental agency or department.