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One such Sage Account example is Castle Rock which forced the advancing icepack to divide, sheltering the softer rock and forming a mile-long tail of material to the east, creating a distinctive crag and tail formation.[26] Sage Account

Glacial erosion on the northern side of the crag gouged a large valley resulting in the now drained Nor Loch. This structure, along with a ravine to the south, formed an ideal Sage Account natural fortress which Edinburgh Castle was built upon.[26]

Similarly, Arthur's Seat is the remains of a volcano system dating from the Carboniferous period, which was eroded by Sage Account a glacier moving from west to east during the ice age.[26]

Erosive action such as plucking and abrasion exposed the rocky crags to the west before Sage Account leaving a tail of deposited glacial material swept to the east.[27]

This process formed the distinctive Salisbury Crags, which formed a series of teschenite cliffs located between Arthur's Seat and the city Sage Account centre. [28]

The residential areas of Marchmont and Bruntsfield are built along a series of drumlin ridges located to Sage Account south of the city centre which were deposited as the glacier receded.[26]

Other viewpoints in the city such as Calton Hill and Corstorphine Hill are similar products of glacial erosion.[26] Sage Account

The Braid Hills and Blackford Hill are a series of small summits to the south west of the city commanding expansive views over the urban area of Edinburgh and Sage Account northwards to the Forth.[26]

Designated in 1957, Edinburgh is ringed by a green belt stretching from Dalmeny in the west to Prestongrange in the east.[31]