The Cumbria Portal

The County Flag of Cumbria

Cumbria (/ˈkʌmbriə/ KUM-bree-ə) is a ceremonial county in North West England. It borders the Scottish council areas of Dumfries and Galloway and Scottish Borders to the north, Northumberland and County Durham to the east, North Yorkshire to the south-east, Lancashire to the south, and the Irish Sea to the west. Its largest settlement is the city of Carlisle.

Cumbria is predominantly rural, with an area of 6,769 km2 (2,614 sq mi) and a population of 500,012; this makes it the third largest ceremonial county in England by area but the eighth-smallest by population. After Carlisle (74,281), the largest settlements are Barrow-in-Furness (56,745), Kendal (29,593), and Whitehaven (23,986). For local government purposes the county comprises two unitary authority areas, Westmorland and Furness and Cumberland. Cumbria was created in 1974 from the historic counties of Cumberland and Westmorland, the Furness area of Lancashire, and a small part of Yorkshire.

The interior of Cumbria contains several upland areas which together fringe the Vale of Eden, the wide valley of the River Eden which runs south-east to north-west across the county and broadens into the Solway Plain near Carlisle. To the north-east are part of the Border Moors and to the east part of the North Pennines; the latter have been designated a national landscape. South of the vale are the Orton Fells, Howgill Fells, and part of the Yorkshire Dales, which are all within the Yorkshire Dales national park. The south-west contains the Lake District, a large upland area which has been designated a national park and UNESCO world heritage site. It includes Scafell Pike, England's highest mountain, and Windermere, its longest and largest lake. The county has long coast to the west, which is bordered by a plain for most of its length. In the north-west it borders the Solway Firth, a national landscape, and the southern coast includes the Cartmel and Furness peninsulas. East of the peninsulas, the county contains part of Arnside and Silverdale another national landscape (Full article...)

Nethermost Pike from Grisedale

Nethermost Pike is a fell in Cumbria, England, and a part of the Lake District. At 891 metres (2,923 ft) it is the second highest Wainwright in the Helvellyn range, the highest of which is Helvellyn itself. It is located close to the southern end of the ridge, with Helvellyn to the north, and High Crag and Dollywaggon Pike to the south. Nethermost Pike, along with many of the Eastern Fells, lies between Thirlmere in the west and the Ullswater catchment in the east. The closest villages are Glenridding and Patterdale on the shores of Ullswater, over 8 kilometres (5 mi) away.

Like most fells in the Helvellyn range, Nethermost Pike has grassy western slopes and rocky outcrops on the eastern side. Geologically, Nethermost Pike belongs to the Borrowdale Volcanic Group. Lead was once mined on its eastern slopes, resulting in open workings and underground mines. The eastern slopes are protected as part of a Site of Special Scientific Interest because of the Pike's geological and biological features, which include some of England's best arctic-alpine and tall-herb vegetation. (Full article...)

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Brougham CastleHMS Cardiff (D108)Norman Birkett, 1st Baron Birkett

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File:Derwent Water, Keswick - June 2009.jpgFile:Helvellyn Striding Edge 360 Panorama, Lake District - June 09.jpgFile:Keswick, Cumbria Panorama 1 - June 2009.jpgFile:Keswick Panorama - Oct 2009.jpgFile:Catbells Northern Ascent, Lake District - June 2009.jpgFile:Glenridding, Cumbria, England - June 2009.jpg

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Andrew Johnston (singer)Askam and IrelethBrough CastleGrayrigg derailmentHerdwickLady in the Lake trialNethermost PikeThe Story of a Fierce Bad RabbitThe Story of Miss MoppetThe Tale of Benjamin BunnyThe Tale of Jemima Puddle-DuckThe Tale of Mr. Jeremy FisherThe Tale of Mr. TodThe Tale of Mrs. Tiggy-WinkleThe Tale of Mrs. TittlemouseThe Tale of The Flopsy BunniesThe Tale of Timmy Tiptoes

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Lapilli-tuff of the Helvellyn Tuff Formation on High Crag

The Borrowdale Volcanic Group is a group of igneous rock formations named after the Borrowdale area of the Lake District, in England. They are Caradocian (late Ordovician) in age (roughly 450 million years old). It is thought that they represent the remains of a volcanic island arc, approximately similar to the island arcs of the west Pacific today. This developed as oceanic crust to the (present) north-west and was forced by crustal movement under a continental land-mass to the present south-east. Such forcing under, as two plates meet, is termed subduction. This land-mass has been named Avalonia by geologists. It is now incorporated into England and Wales and a sliver of North America. (Full article...)

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A panoramic view of Derwent Water as viewed from the summit of Catbells on the western side.
A panoramic view of Derwent Water as viewed from the summit of Catbells on the western side.
Credit: Diliff
A panoramic view of Derwent Water as viewed from the summit of Catbells on the western side.

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