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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...)

The ruined keep at Brough Castle

Brough Castle is a ruined castle in the village of Brough, Cumbria, England. The castle was built by William Rufus around 1092 within the old Roman fort of Verterae to protect a key route through the Pennine Mountains. The initial motte and bailey castle was attacked and destroyed by the Scots in 1174 during the Great Revolt against Henry II. Rebuilt after the war, a square keep was constructed and the rest of the castle converted to stone.

The Clifford family took possession of Brough after the Second Barons' War in the 1260s; they built Clifford's Tower and undertook a sequence of renovations to the castle, creating a fortification in a typical northern English style. In 1521, however, Henry Clifford held a Christmas feast at the castle, after which a major fire broke out, destroying the property. The castle remained abandoned until Lady Anne Clifford restored the property between 1659 and 1661, using it as one of her northern country homes. In 1666 another fire broke out, once again rendering the castle uninhabitable. Brough Castle went into sharp decline and was stripped first of its fittings and then its stonework. The castle's masonry began to collapse around 1800. (Full article...)

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Featured articles

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

Featured pictures

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 360 degree view from the summit of Catbells near Keswick on Derwent Water in the Lake District.
A 360 degree view from the summit of Catbells near Keswick on Derwent Water in the Lake District.
Credit: Diliff
A 360 degree view from the summit of Catbells near Keswick on Derwent Water in the Lake District.

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