Edinburgh
Edinburgh (/ˈɛdɪnbərə/ ⓘ[11][12][13] Scots: [ˈɛdɪnbʌrə]; Scottish Gaelic: Dùn Èideann [ˌt̪un ˈeːtʲən̪ˠ]) is the capital city of Scotland and one of its 32 council areas. The city is located in south-east Scotland, and is bounded to the north by the Firth of Forth estuary and to the south by the Pentland Hills. Edinburgh had a population of 506,520 in mid-2020,[7] making it the second-most populous city in Scotland and the seventh-most populous in the United Kingdom. The wider metropolitan area has a population of 912,490[14]
This article is about the capital of Scotland. For other uses, see Edinburgh (disambiguation).
Edinburgh
Dùn Èideann
City of Edinburgh
Edinburgh
Before 7th century AD
1125
1633
Robert Aldridge
-
Ash Regan (Alba)
-
Angus Robertson (SNP)
-
Daniel Johnson (Lab)
-
Gordon MacDonald (SNP)
- Ben Macpherson (SNP)
-
Alex Cole-Hamilton (LD)
- Joanna Cherry (SNP)
-
Tommy Sheppard (SNP)
-
Ian Murray (Lab)
-
Deidre Brock (SNP)
-
Christine Jardine (LD)
46 sq mi (119 km2)
49 sq mi (126 km2)
101.7 sq mi (263.4 km2)
154 ft (47 m)
506,520
11,000/sq mi (4,300/km2)
530,990
11,000/sq mi (4,200/km2)
901,455
526,470
5,180/sq mi (1,999/km2)
£25.419 billion (2021)
0131
GB-EDH
S12000036
UKM25
Old and New Towns of Edinburgh
Cultural: ii, iv
1995 (19th Session)
The Forth Bridge
Cultural: i, iv
2015 (39th Session)
Recognised as the capital of Scotland since at least the 15th century, Edinburgh is the seat of the Scottish Government, the Scottish Parliament, the highest courts in Scotland, and the Palace of Holyroodhouse, the official residence of the British monarch in Scotland. It is also the annual venue of the General Assembly of the Church of Scotland. The city has long been a centre of education, particularly in the fields of medicine, Scottish law, literature, philosophy, the sciences and engineering. The University of Edinburgh, founded in 1582 and now one of three in the city, is considered one of the best research institutions in the world. It is the second-largest financial centre in the United Kingdom, the fourth largest in Europe, and the thirteenth largest internationally.[15]
The city is a cultural centre, and is the home of institutions including the National Museum of Scotland, the National Library of Scotland and the Scottish National Gallery.[16] The city is also known for the Edinburgh International Festival and the Fringe, the latter being the world's largest annual international arts festival. Historic sites in Edinburgh include Edinburgh Castle, the Palace of Holyroodhouse, the churches of St. Giles, Greyfriars and the Canongate, and the extensive Georgian New Town built in the 18th/19th centuries. Edinburgh's Old Town and New Town together are listed as a UNESCO World Heritage Site,[17] which has been managed by Edinburgh World Heritage since 1999. The city's historical and cultural attractions have made it the UK's second-most visited tourist destination, attracting 4.9 million visits, including 2.4 million from overseas in 2018.[18][19]
Edinburgh is governed by the City of Edinburgh Council, a unitary authority. The City of Edinburgh council area had an estimated population of 526,470 in mid-2021,[8] and includes outlying towns and villages which are not part of Edinburgh proper. The city is in the Lothian region and was historically part of the shire of Midlothian (also called Edinburghshire).
Geography[edit]
Cityscape[edit]
Situated in Scotland's Central Belt, Edinburgh lies on the southern shore of the Firth of Forth. The city centre is 2+1⁄2 mi (4.0 km) southwest of the shoreline of Leith and 26 mi (42 km) inland, as the crow flies, from the east coast of Scotland and the North Sea at Dunbar.[98] While the early burgh grew up near the prominent Castle Rock, the modern city is often said to be built on seven hills, namely Calton Hill, Corstorphine Hill, Craiglockhart Hill, Braid Hill, Blackford Hill, Arthur's Seat and the Castle Rock,[99] giving rise to allusions to the seven hills of Rome.[100]
Occupying a narrow gap between the Firth of Forth to the north and the Pentland Hills and their outrunners to the south, the city sprawls over a landscape which is the product of early volcanic activity and later periods of intensive glaciation.
[101]: 64–65 Igneous activity between 350 and 400 million years ago, coupled with faulting, led to the creation of tough basalt volcanic plugs, which predominate over much of the area.[101]: 64–65 One such example is the Castle Rock which forced the advancing ice sheet to divide, sheltering the softer rock and forming a 1 mi-long (1.6 km) tail of material to the east, thus creating a distinctive crag and tail formation.[101]: 64–65 Glacial erosion on the north side of the crag gouged a deep valley later filled by the now drained Nor Loch. These features, along with another hollow on the rock's south side, formed an ideal natural strongpoint upon which Edinburgh Castle was built.[101]: 64–65 Similarly, Arthur's Seat is the remains of a volcano dating from the Carboniferous period, which was eroded by a glacier moving west to east during the ice age.[101]: 64–65 Erosive action such as plucking and abrasion exposed the rocky crags to the west before leaving a tail of deposited glacial material swept to the east.[102] This process formed the distinctive Salisbury Crags, a series of teschenite cliffs between Arthur's Seat and the location of the early burgh.[103] The residential areas of Marchmont and Bruntsfield are built along a series of drumlin ridges south of the city centre, which were deposited as the glacier receded.[101]: 64–65
Other prominent landforms such as Calton Hill and Corstorphine Hill are also products of glacial erosion.[101]: 64–65 The Braid Hills and Blackford Hill are a series of small summits to the south of the city centre that command expansive views looking northwards over the urban area to the Firth of Forth.[101]: 64–65