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63-582: These rocks are found in northwest England as far north as Carlisle (and extending just into Scotland around Annan and Gretna ) and in the Vale of Eden and then extending down the Cumbrian coast into Lancashire and Cheshire . They are mostly obscured by superficial deposits but the highest coastal cliffs in northwest England at St Bees Head are formed in the St Bees Sandstone, the lowermost formation within

126-554: A large rural area with many villages and towns including Dalston , Brampton , Longtown , Wetheral , Bewcastle and Scotby . Cumberland Council , the local authority for Cumberland , is a unitary authority , having the powers of a non-metropolitan county and district council combined. It operated as a shadow authority until taking up its powers on 1 April 2023. Cumberland Council replaced Cumbria County Council, Allerdale Borough Council , Carlisle City Council and Copeland Borough Council . The first election to Cumberland Council

189-460: A single civil parish of Carlisle in 1904. The civil parish was abolished on 1 April 1974, although parts of the urban fringe are in the parishes of Stanwix Rural , Kingmoor and St Cuthbert Without . Carlisle unsuccessfully applied to become a Lord Mayoralty in 2002. Carlisle City Council had its headquarters at the 1960s Civic Centre in Rickergate, the tallest building in the city. At the time of

252-526: 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 eight miles or thirteen kilometres south of

315-772: Is of Induan/Olenekian age. Also encountered as the Hopwas or Moira Breccia. The Lenton Sandstone Formation (named from the Nottingham suburb of Lenton ) is of Induan/Olenekian age. The Stafford Basin includes the Kibbleston Formation (named from the Staffordshire locality of Kibbleston) which is underlain by the Wildmoor Formation which is in turn underlain by the Kidderminster Formation. The rock succession in

378-518: Is often divided into an upper Frodsham Member and a lower Delamere Member . Faulted blocks of these rocks are largely responsible for the prominent west facing escarpment of the Mid Cheshire Ridge and the Helsby Sandstone is exposed in numerous localities here, southwards from Runcorn through Frodsham to Utkinton , spectacularly at the outlier of Beeston Castle hill and lastly within

441-447: Is operational and used by railfreight companies. The Strand Road drill hall opened in 1874. At the start of the 20th century, the population had grown to over 45,000. Transport was improved by the City of Carlisle Electric Tramways from 1900 until 1931, and the first cinema was built in 1906. In 1912, the boundaries of Carlisle were extended to include Botcherby in the east and Stanwix in

504-537: The Ala Gallorum Petriana , the sole regiment of this size along the wall. Hadrian's successor Antoninus Pius abandoned the frontier and attempted to move further north; he built the Antonine Wall between the firths of Forth and Clyde . It was not a success and, after 20 years, the garrisons returned to Hadrian's Wall. At one time, Carlisle broke off from Rome when Marcus Carausius assumed power over

567-670: The 2001 census , the population of Carlisle was 71,773, with 100,734 living in the district. In the 2011 census, the city's population had risen to 75,306, with 107,524 in the district. On 1 April 2023 the City of Carlisle local government district was abolished, and the boundaries of the City of Carlisle were redefined to cover the following wards: Belah and Kingmoor, Botcherby and Harraby North, Cathedral and Castle, Currock and Upperby, Denton Holme and Morton South, Harraby South and Parklands, Newtown and Morton North, Sandsfield and Morton West and Stanwix and Houghton. Charter trustees were formed from

630-606: The Anglian kingdom of Northumbria . In 685, St Cuthbert , visiting the Queen of Northumbria in her sister's monastery at Carlisle, was taken to see the city walls and a marvellously constructed Roman fountain. By the time of the Norman Conquest of England in 1066, Carlisle was in the possession of the Scots. It was not recorded in the 1086 Domesday Book . This changed in 1092, when William

693-576: The Archbishop of Glasgow Gavin Dunbar cursed all the reivers of the borderlands. The curse was detailed in 1,069 words, beginning: "I curse their head and all the hairs of their head; I curse their face, their brain (innermost thoughts), their mouth, their nose, their tongue, their teeth, their forehead, their shoulders, their breast, their heart, their stomach, their back, their womb, their arms, their leggs, their hands, their feet and every part of their body, from

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756-649: The Cheshire Basin , which also extends into north Shropshire. It comprises the following formations: The Helsby Sandstone Formation (named from the Cheshire village of Helsby where the type section is exposed at Helsby Hill ) comprises around 250m thickness of sandstone with conglomerate and siltstone which occurs across the Cheshire Basin. Older literature includes it as part of the Lower Keuper Sandstone. It

819-557: The Guildhall and Tithe Barn . The Citadel towers , which until 2016 also served as offices for Cumbria County Council, were designed by Thomas Telford , with the eastern tower incorporating part of the 16th-century building. The first Citadel building was a Tudor fortification replacing the medieval Englishgate, designed by the Moravian military engineer Stefan von Haschenperg in 1541. Next to

882-612: The Peckforton Hills . The Wilmslow Sandstone Formation (named from the town of Wilmslow in Cheshire) comprises up to 900m thickness of early Triassic sandstones with occasional siltstones. It was earlier known as the Upper Mottled Sandstone. In Wirral , the 60m thick Thurstaston Sandstone Member and the 2m thick Thurstaston Hard Sandstone Bed are distinguished at the top of the sequence. The Chester Formation (named from

945-448: The cathedral's nave to obtain the stone to rebuild the castle. Carlisle continued to remain a barracks thereafter. In 1698 travel writer Celia Fiennes wrote of Carlisle as having most of the trappings of a military town and that it was rife with alcohol and prostitutes. In 1707 an act of union was passed between England and Scotland, creating Great Britain , but Carlisle remained a garrison town. The tenth, and most recent siege in

1008-624: The 'Great Border City', Carlisle today is a main cultural, commercial and industrial centre within the British borders. The ancient history of Carlisle is derived mainly from archaeological evidence and the works of the Roman historian Tacitus . The earliest recorded inhabitants in the area were the Carvetii tribe of Britons who made up the main population of ancient Cumbria and North Lancashire . According to Boethius and John of Fordun , writing in

1071-582: The 18th and 19th centuries, Carlisle existed before the arrival of the Romans in Britain and was one of the strongest British towns at the time. In the time of the emperor Nero , it was said to have burned down. The Roman settlement was named Luguvalium , based on a native name that has been reconstructed as Brittonic * Luguwaljon , "[city] of Luguwalos", a masculine Celtic given name meaning "strength of Lugus ". Excavations undertaken along Annetwell Street in

1134-514: The 1970s dated the Roman timber fort constructed at the site of present Carlisle Castle to the winter of AD 73. It protected a strategic location on the Roman road to the north and overlooking the confluence of the Caldew and Eden rivers. The fort at Carlisle was reconstructed in 83 using oak timbers from further afield, rather than local alder as a possible result of the increased Roman control of

1197-926: The Calder Sandstone Formation in the Carlisle and Vale of Eden basins of north and east Cumbria. A sandstone which underlies Sellafield and Drigg is known as the Sellafield Member and is assigned to the Helsby Sandstone Formation. The group is represented in Somerset and east Devon by the Otterton Sandstone and the underlying Budleigh Salterton Pebble Beds formations,. Carlisle, Cumbria Carlisle ( / k ɑːr ˈ l aɪ l / kar- LYLE , locally / ˈ k ɑːr l aɪ l / KAR -lyle ; from Cumbric : Caer Luel )

1260-531: The Carlisle Board of Control, and subsequently the Carlisle & District State Management Scheme , it lasted until 1971. During the Second World War, Carlisle hosted over 5,000 evacuees, many of whom arrived from Newcastle upon Tyne and the surrounding towns. A shopping centre (including a new central library) was built to the east and north-east of the market cross and opened in 1986. The area east of

1323-503: The Citadel is Carlisle railway station , designed by William Tite in the neo-Tudor style, considered by Historic England to be among the most important early railway stations in England. Carlisle has held city status since the Middle Ages and a borough constituency or parliamentary borough for centuries, at one time returning two MPs. In 1835 it became a municipal borough which

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1386-570: The Conqueror 's son William Rufus invaded the region and incorporated Carlisle into England. The construction of Carlisle Castle began in 1093 on the site of the Roman fort, south of the River Eden . The castle was rebuilt in stone in 1112, with a keep and the city walls . The walls enclosed the city south of the castle and included three gates to the east, south, and north called the Irish or Caldew Gate,

1449-589: The Cumbrian coast the Group comprises the Calder Sandstone Formation and the underlying St Bees Sandstone Formation. The former is around 500m thick and includes sandstones of both aeolian and fluviatile origin. The latter is between 400 and 600m thick and includes some siltstone and claystone beds. It overlies the varied lithologies of the Permian age Cumbrian Coastal Group . The Kirklinton Sandstone Formation in places overlies

1512-612: The Durranhill Industrial Estate. Adjoining Harraby to the south but outside the former borough boundary is the hamlet of Carleton . Carlisle is linked to the rest of England via the M6 motorway to the south, and to Scotland via the M74/A74 towards Glasgow and the north. Many trunk roads begin or terminate in Carlisle, including the A6 to Penrith and Luton (historically the main road to

1575-778: The England/Wales border west of Chester) is a sequence which ranges from 0m to over 150m thickness of largely aeolian sandstones of early Triassic age. It was formerly known as the Lower Mottled Sandstone. Once known locally as the Bromsgrove Sandstone Formation (from the town of Bromsgrove in Worcestershire), the Helsby Sandstone Formation is early Triassic to Anisian in age and comprises variously coloured sandstones whose bases are frequently conglomeratic, together with mudstones and siltstones. The thickness of

1638-557: The English or Botcher Gate, and the Scotch or Ricker Gate respectively. The names of the gates exist in road names in Carlisle today. Carlisle Cathedral was founded as an Augustinian priory and became a cathedral in 1133. In 1157, Carlisle became the seat of the new county of Carliol (a name that was originally an abbreviation of Latin Carlioliensis , meaning "[Bishop] of Carlisle"); in 1177

1701-698: The Needwood Basin includes the Hollington Formation (named from the Staffordshire locality of Hollington ) which is underlain by the Hawksmoor Formation (named from the Staffordshire locality of Hawksmoor) which includes the Hulme Member , a conglomerate and which is in turn underlain by the Huntley Formation (named from the Staffordshire locality of Huntley ). They are all of Scythian age. On

1764-554: The Sands Centre (and the nearby Shell petrol station and Bitts Park), marooned from the rest of the city. As several other areas of Cumbria were also badly affected (particularly Appleby and Wigton), all trains to Scotland were postponed indefinitely, with trains on the West Coast Mainline going no further than Preston, as nearby Lancaster suffered flooding and problems with electricity supply. Prime Minister David Cameron visited

1827-866: The Worcestershire town of Kidderminster ) is a 0 - 200m thick sequence of conglomerates and sandstones previously known as either the Bunter Pebble Beds or the Kidderminster Conglomerate Formation. Formerly known locally as the Polesworth Formation (from the Warwickshire village of Polesworth ), the Chester Formation here is of ?Olenekian to Anisian age. The Moira Formation (named from the Leicestershire village of Moira )

1890-533: The area. At this time the Roman fort was garrisoned by a 500-strong cavalry regiment, the Ala Gallorum Sebosiana . By the early 2nd century, Carlisle was established as a prominent stronghold. The 'Stanegate' frontier, which consisted of Luguvalium and several other forts in a line east to Corbridge , was proving a more stable frontier against the Picts than those established deeper into Caledonia . In 122,

1953-561: The castle was garrisoned for the king. It endured a long siege from October 1644 until June 1645 when the Royalist forces surrendered after the Battle of Naseby . The city was occupied by a parliamentary garrison, and subsequently by their Scots allies. In 1646, the Scots, now holding Carlisle pending payment of monies owed them by the English Parliament, improved its fortifications, destroying

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2016-516: The city of Chester ) comprises sandstones with some conglomerates and siltstones of early Triassic age. It ranges from less than 90m to over 220m in thickness. It has been known in the past as the Bunter Pebble Beds and the Chester Pebble Beds Formation. There are a couple of reference sections for this sequence in the vicinity of Chester. The Kinnerton Sandstone Formation (named from the twin villages of Higher and Lower Kinnerton on

2079-458: The city on 7 December 2015 to assess the damage, having earlier called an emergency Cobra meeting. In the north of Carlisle are the suburbs of Kingstown, Lowry Hill and Moorville, formerly part of the parish of Kingmoor. To the south of them are Stanwix , Edentown, Etterby, St Ann's Hill and Belah which were added to Carlisle in 1912. The parish of Stanwix Rural exists but only includes a small part of Carlisle's urban area, Whiteclosegate . To

2142-569: The city's history took place after Charles Edward Stuart took Carlisle in the Jacobite Rising of 1745 . When the Jacobites retreated across the border to Scotland they left a garrison of 400 men in Carlisle Castle. Ten days later Prince William, Duke of Cumberland took the castle and executed 31 Jacobites on the streets of Carlisle. Although Carlisle continued to garrison soldiers, becoming

2205-474: The city's modern Welsh name Caerliwelydd . Rheged came under Northumbrian control before 730, probably by inheritance after Rienmelth, daughter of Royth and great-granddaughter of Urien, married Oswy , King of Northumbria . For the rest of the first millennium, Carlisle was an important stronghold contested by several entities who warred over the area, including the Brythonic Kingdom of Strathclyde and

2268-577: The coast of East Devon . There are further occurrences in Northern Ireland north and east of Limavady , east of Cookstown , between Dungannon and Armagh and along the Lagan Valley beneath Belfast and Newtownards and on the Antrim coast. The Group comprises different sequences in each of the various basins in which it is developed as described below. The sequence is most thickly developed in

2331-636: The councillors that cover the said areas. They act as appropriate bodies in which historic rights and privileges of Carlisle, including the mayoralty will continue until a governance review will determine the need of a city council . The current member of Parliament is Julie Minns , representing the Labour Party . Carlisle used to be within the North West England constituency of the European Parliament . Carlisle elected 18 county councillors to

2394-459: The county was renamed Cumberland . The conquest of Cumberland was the beginning of a war between Scotland and England which saw the region centred around Carlisle change hands a number of times. It was a major stronghold after the construction of the castle. During the wars, the livelihood of the people on the borders was devastated by armies from both sides. Even when the countries were not at war, tension remained high, and royal authority in one or

2457-513: 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

2520-403: The end of the 19th century when mass housing was built west of the city walls. In 1823 a canal was built to Fisher's Cross ( Port Carlisle ) to transport goods produced in the city. This enabled other industrial centres such as Liverpool to link with Carlisle via the Solway . This was short-lived and when the canal operators ran into financial difficulty the waterway was filled in. A railway

2583-507: The formation is variable but reaches around 500m in the Worcester area. It is often encountered in older literature as the Lower Keuper Sandstone. The formation includes the Shepshed Sandstone Member. The Wildmoor Sandstone Formation (named from the Worcestershire locality of Wildmoor, north of Bromsgrove) is a 0 - 284m thick sequence of sandstones formerly known as the Upper Mottled Sandstone or Wildmoor Beds. It also includes some mudstones and siltstones. The Kidderminster Formation (named from

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2646-403: The former Cumbria County Council. Its headquarters were located at Cumbria House on Botchergate. Until April 2023 Carlisle was governed by a district council , Carlisle City Council and a County Council, Cumbria County Council. After the 2019 elections the Conservative Party ran a minority administration on the district council with the support of the Independents. The district council covered

2709-468: The group. In the northeast they extend from Hartlepool south through the Vale of Mowbray and the Vale of York , then south through Nottinghamshire into the English Midlands, though are very largely concealed by superficial sediments. They occur widely through the Midlands (though usually concealed) and notably in an outlier at Leek, Staffordshire . They extend south to the Severn Estuary and beyond there through Somerset to Budleigh Salterton on

2772-540: The headquarters of the Border Regiment , the city's importance as a military town decreased as the industrial age took over. The post of Governor of Carlisle as garrison commander was abolished in 1838. In the early 19th century textile mills, engineering works and food manufacturers built factories in the city mostly in the Denton Holme , Caldewgate and Wapping suburbs in the Caldew Valley. These included Carr's of Carlisle , Kangol , Metal Box and Cowans Sheldon. Shaddon Mill , in Denton Holme, became famous for having

2835-498: The immediate south of Stanwix is the River Eden. On the opposite bank is the city centre bounded on the west by the West Coast Main Railway line and the River Caldew. In the past industry flourished on the banks of the River Caldew, especially Denton Holme and Caldewgate on the west bank and Wapping, around the former Metal Box works, on the east. West of Caldewgate and north of Denton Holme the suburbs of Newtown, Morton, Sandsfield Park, Longsowerby, Raffles and Belle Vue developed in

2898-442: The kingdom took its name from a major stronghold within it; this has been suggested to have been broadly coterminous with the Civitas Carvetiorum , Carlisle. King Urien and his son and successor Owain became the subjects of a great deal of Arthurian legend . Their capital has been identified as the Cair Ligualid listed by Nennius among the 28 cities of Britain, which later developed into Caer -luel , whence

2961-535: The late 19th and 20th centuries. The eastern side of the city centre developed in the 19th century into a more affluent area along the main A69 road . It links with the former village of Botcherby to which a large council estate was added in the mid-20th century and later still Durranhill Housing Estate. South of the city centre is the Botchergate/St Nicholas area of late Victorian terraced housing similar to that found in Denton Holme and Caldewgate. The Botchergate East area until recently had older slum dwellings. To

3024-430: The latter as far as Morecambe . At the time of the flood, emergency services also had to respond to cases of car-related arson in the city. Carlisle is the only city in Cumbria. The city centre is largely pedestrianised and the Lanes shopping centre is home to around 75 shops. Carlisle has a compact historic centre with a castle , cathedral and semi-intact city walls , as well as other medieval buildings including

3087-609: The market cross had formerly been occupied by narrow alleyways of housing and small shops (on a layout which had not changed much since medieval times) and referred to locally as The Lanes . Carlisle city centre was pedestrianised in 1989. On the evening of Friday, 7 January 2005, the rivers Eden, Caldew and Petteril burst their banks due to as much as 180 mm rainfall upstream that day. 2,700 homes were flooded and three people died. The city's police and fire stations were flooded along with Brunton Park football stadium. The police, fire service and Carlisle United F.C. were mobilised,

3150-506: The north end the castle towers were converted to artillery platforms, at the south the medieval Bochard gate was converted into the Citadel , an artillery fortification with two massive artillery towers. The death of Queen Elizabeth I in 1603 and her succession by James VI of Scotland as King James I of England allowed more determined and coordinated efforts to suppress reiving. The borderers were not quick to change their ways and many were hanged and whole families were exiled to Ireland. It

3213-409: The north. Carlisle was subject to the decline in the textile industry experienced throughout Britain as new machinery made labour unnecessary. In 1916, during the First World War , the government took over the public houses and breweries in Carlisle because of drunkenness among construction and munitions workers from the munitions factory at Gretna . This experiment nationalised brewing. As

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3276-444: The other kingdom was often weak. The uncertainty of existence meant that communities or peoples kindred to each other sought security through their own strength and cunning, and they improved their livelihoods at their enemies' expense. These peoples were known as the Border Reivers and Carlisle was the major city within their territories. The Reivers became so much of a nuisance to the Scottish and English governments that, in 1525,

3339-400: The province was visited by Hadrian , who approved a plan to build a wall the length of the frontier. A new fort, Petriana , was therefore built in the Stanwix area of the city north of the river on Hadrian's Wall . It was the largest fort along the wall and was completed in stone by around 130. Like Luguvalium, which lay within sight, Petriana housed a nominal 1,000-strong cavalry regiment,

3402-477: The south west of Botchergate and St Nicholas are the former villages now suburbs of Upperby and Currock . The urban area spills over the former county borough boundary into Blackwell and Durdar in the civil parish of St Cuthbert Without . Between Upperby and Botcherby is Harraby, a former village once part of St Cuthbert Without and the largest suburb of Carlisle. Harraby is subdivided into Harraby East, New Harraby, Harraby Green, Old Harraby, Petteril Bank and

3465-405: The territory. He was assassinated and suffered damnatio memoriae , but a surviving reference to him has been uncovered in Carlisle. Coins excavated in the area suggest that Romans remained in Carlisle until the reign of Emperor Valentinian II , from 375 to 392. The period of late antiquity after Roman rule saw Cumbria organised as the native British kingdom of Rheged . It is likely that

3528-520: The time meant the settlement became a city) while the county of Cumberland was created and later renamed Cumbria. In the 19th century, the introduction of textile manufacture during the Industrial Revolution began a process of socioeconomic transformation in Carlisle, which developed into a densely populated mill town . This, combined with its strategic position, allowed for the development of Carlisle as an important railway town , with seven railway companies sharing Carlisle railway station . Nicknamed

3591-404: The top of their head to the soles of their feet, before and behind, within and without." After the Pilgrimage of Grace , Henry VIII , concerned at the weakness of his hold on the North, employed (1539) the engineer Stefan von Haschenperg to modernise the defences of Carlisle. von Haschenperg was sacked in 1543 for having "spent great treasures to no purpose"; but (by him and his successors) at

3654-558: The world's 8th tallest chimney and was the largest cotton mill in England. The expanding industries brought about an increase in population as jobs shifted from rural farms towards the cities. This produced a housing shortage where at one point 25,000 people in the city only had 5,000 houses to live in. People were said to be herded together with animal houses, slaughter houses and communal lavatories with open drains running between them. Living conditions were so bad that riots were common and some people emigrated. The problem wasn't solved until

3717-436: Was built in place of the canal. Carlisle became a major railway centre on the West Coast Main Line with connections to the east. At one time seven companies used Carlisle Citadel railway station . Before the building of the Citadel railway station the city had several other railway stations, including London Road railway station . Carlisle had the largest railway marshalling yard in Europe, Kingmoor, which, reduced in size,

3780-1012: Was held on 5 May 2022. All 46 seats were up for election. Labour won a majority of 30 seats. Conservatives have 7 seats, Liberal Democrats 4 seats, Independents 3 seats and Green Party 2 seats. Turnout was 36.1%. Carlisle is situated on a slight rise, in the Cumberland Ward , at the confluence of the rivers Eden , Caldew and Petteril . An important centre for trade, it is located 56 mi (90 km) west of Newcastle upon Tyne , 71 mi (114 km) north of Lancaster , 90 mi (140 km) south-east of Glasgow , 93 mi (150 km) south of Edinburgh , 120 mi (190 km) north-west of York , and 300 mi (480 km) north-north-west of London . Nearby towns and villages include Longtown (north), Penrith (south), Brampton (east), Wigton (west), Haggbeck, Harker , Carwinley, Blackford , Houghton, Scotby , Wreay and Rockcliffe . Carlisle experiences an oceanic climate ( Köppen climate classification Cfb ). In January 2005 Carlisle

3843-449: Was hit by strong gales and heavy rain, and on Saturday 8 January 2005 all roads into Carlisle were closed owing to severe flooding , the worst since 1822, which caused three deaths. Even worse flooding than in 2005 affected Carlisle between 4 and 6 December 2015. During this time, nearly 36 hours of incessant rainfall breached flood defences and left several areas submerged – including Bitts Park, Hardwicke Circus and Warwick Road. This left

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3906-423: Was not until 1681 that the problem of the reivers was acknowledged as no longer an issue. Following the personal union of the crowns Carlisle Castle should have become obsolete as a frontier fortress, but the two kingdoms continued as separate states. In 1639, with war between the two kingdoms looming, the castle was refortified using stone from the cathedral cloisters. In 1642 the English Civil War broke out and

3969-506: Was promoted to county borough status in 1914. The city's boundaries have changed several times since 1835, most notably between 1974 and 2023, when under the Local Government Act 1972 the city and county borough and the Border Rural District were abolished and new enlarged City of Carlisle non-metropolitan district was created within the newly formed administrative county of Cumbria . The municipal borough contained several civil parishes or parts of parishes but these were merged into

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