Castle Rock (Edinburgh) in the context of "Edinburgh Castle"

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⭐ Core Definition: Castle Rock (Edinburgh)

Castle Rock (Scottish Gaelic: Creag a' Chaisteil, Scottish Gaelic pronunciation: [ˈkʰʲɾʲekˈaˈxaʃtʰʲɪl]) is a volcanic plug in the middle of Edinburgh upon which Edinburgh Castle sits. The rock is estimated to have formed some 350 million years ago during the early Carboniferous period. It is the remains of a volcanic pipe which cut through the surrounding sedimentary rock, before cooling to form very hard dolerite, a coarser-grained equivalent of basalt. Subsequent glacial erosion was resisted more by the dolerite, which protected the softer rock to the east, leaving a crag and tail formation.

The summit of the castle rock is 130 m (430 ft) above sea level, with rocky cliffs to the south, west and north, rearing up to 80 m (260 ft) from the surrounding landscape. This means that the only readily accessible route to the castle lies to the east, where the ridge slopes more gently. The defensive advantage of such a site is clear, but the geology of the rock also presents difficulties, since basalt is an extremely poor aquifer. Providing water to the Upper Ward of the castle was problematic, and despite the sinking of a 28 m (92 ft) deep well, the water supply often ran out during drought or siege, for example during the Lang Siege of 1573.

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👉 Castle Rock (Edinburgh) in the context of Edinburgh Castle

Edinburgh Castle (Scottish Gaelic: Caisteal Dhùn Èideann) is a historic castle in Edinburgh, Scotland. It stands on Castle Rock, which has been occupied by humans since at least the Iron Age. There has been a royal castle on the rock since the reign of Malcolm III in the 11th century, and the castle continued to be a royal residence until 1633. From the 15th century, the castle's residential role declined, and by the 17th century it was principally used as a military garrison. Its importance as a part of Scotland's national heritage was recognised increasingly from the early 19th century onwards, and various restoration programmes have been carried out over the past century and a half.

Edinburgh Castle has played a prominent role in Scottish history, and has served variously as a royal residence, an arsenal, a treasury, a national archive, a mint, a prison, a military fortress, and the home of the Honours of Scotland – the Scottish regalia. As one of the most important strongholds in the Kingdom of Scotland, the castle was involved in many historical conflicts from the Wars of Scottish Independence in the 14th century to the Jacobite rising of 1745. Research undertaken in 2014 identified 26 sieges in its 1,100-year history, giving it a claim to having been "the most besieged place in Great Britain and one of the most attacked in the world". Few of the present buildings pre-date the Lang Siege of 1573, when the medieval defences were largely destroyed by artillery bombardment. The most notable exceptions are St Margaret's Chapel from the early 12th century, which is regarded as the oldest building in Edinburgh, the Royal Palace, and the early 16th-century Great Hall. The castle is the site of the Scottish National War Memorial and the National War Museum. The British Army is still responsible for some parts of the castle, although its presence is now largely ceremonial and administrative. The castle is the regimental headquarters of the Royal Regiment of Scotland and the Royal Scots Dragoon Guards and houses their regimental museums, along with that of the Royal Scots.

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Castle Rock (Edinburgh) in the context of St Cuthbert's Church, Edinburgh

The Parish Church of St Cuthbert is a parish church of the Church of Scotland in central Edinburgh. Probably founded in the 7th century, the church once covered an extensive parish around the burgh of Edinburgh. The church's current building was designed by Hippolyte Blanc and completed in 1894.

St Cuthbert's is situated within a large churchyard that bounds Princes Street Gardens and Lothian Road. A church was probably founded on this site during or shortly after the life of Cuthbert. The church is first recorded in 1128, when David I granted it to Holyrood Abbey. At that time, the church covered an extensive parish, which was gradually reduced until the 20th century by the erection and expansion of other parishes, many of which were founded as chapels of ease of St Cuthbert's. St Cuthbert's became a Protestant church at the Scottish Reformation in 1560: from after the Reformation until the 19th century, the church was usually called the West Kirk. After the Restoration in 1660, the congregation remained loyal to the Covenanters. The church's position at the foot of Castle Rock saw it damaged or destroyed at least four times between the 14th and 17th centuries.

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Castle Rock (Edinburgh) in the context of Eidyn

Eidyn was the region around modern Edinburgh in sub-Roman and early medieval Britain, approximately during the 5th–7th centuries. It centred on the stronghold of Din Eidyn, thought to have been at Castle Rock, now the site of Edinburgh Castle, and apparently included much of the area below the Firth of Forth. It was the most important district of the Brittonic kingdom of Gododdin, and a significant power in the Hen Ogledd, or Old North, the Brittonic-speaking area of what is now southern Scotland and northern England.

The site of Din Eidyn has been nearly continuously occupied since the Bronze Age, serving as a stronghold of the Votadini during the Roman era and later the principal centre of their successors, the Gododdin kingdom. Eidyn's importance to the Hen Ogledd is reflected in the medieval poem Y Gododdin, which concerns a war band that gathered there for a raid around AD 600. After years of decline, Eidyn was conquered by the Angles in 638.

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