Portal:Cumbria

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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.

The county 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 large upland areas. The south-west contains the Lake District, a national park and UNESCO world heritage site which includes Scafell Pike, England's highest mountain, and Windermere, its longest and largest lake. The Border Moors and North Pennines lie along the county's eastern border. The south-east contains the Orton Fells, Howgill Fells and part of the Yorkshire Dales, which are all within the Yorkshire Dales national park. The Vale of Eden, the valley of the River Eden, runs south-east to north-west between these upland areas, and broadens into the Solway Plain near Carlisle. 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 to the south are the Cartmel and Furness peninsulas. East of the peninsulas, the county contains part of Arnside and Silverdale, also a national landscape. (Full article...)

Carlisle (/kɑːrˈll/ kar-LYLE, locally /ˈkɑːrll/ KAR-lyle; from Cumbric: Caer Luel) is a cathedral city in the ceremonial county of Cumbria in England. It is the administrative centre of Cumberland Council which covers an area similar to the historic county of Cumberland.

Carlisle's early history is marked by the establishment of a Human settlement to serve castles along Hadrian's Wall in Britain. Due to its proximity to Scotland (being located 8 mi (13 km) south of the current Anglo-Scottish border), Carlisle Castle and the city became an important military stronghold in the Middle Ages. The castle served as a prison for Mary, Queen of Scots in 1568 and currently hosts the Duke of Lancaster's Regiment and the Border Regiment Museum. In the early 12th century, a priory was built and gained cathedral status with a diocese in 1133 (city status at the time meant the settlement became a city) while the county of Cumberland was created and later renamed Cumbria. (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

Good articles

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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Geological map of the Lake District showing the main structures and areas of mineralisation
The geology of England's Lake District is dominated by sedimentary and volcanic rocks of mainly Ordovician age underpinned by large granitic intrusions. Younger sedimentary sequences outcrop on the edges of the Lake District area, with Silurian to the south, Carboniferous to the north, east, and west and Permo-Triassic to the west and east. The entire area was covered by a Mesozoic sequence that was eroded off during the Paleogene uplift related to the opening of the North Atlantic. During the Quaternary the area was affected by repeated glaciations, which sculpted the current mountainous landscape. (Full article...)

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A panoramic view of Derwent Water, one of the principal bodies of water in the Lake District National Park, as seen from the northern shore of Keswick.
A panoramic view of Derwent Water, one of the principal bodies of water in the Lake District National Park, as seen from the northern shore of Keswick.
Credit: Diliff
A panoramic view of Derwent Water, one of the principal bodies of water in the Lake District National Park, as seen from the northern shore of Keswick.

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