Cuillin range. Cracks and fissures in the rock provided pathways for later magma intrusions, leading to dykes of basalt which are commonly seen across Skye. The Red Cuillin also have volcanic origins, being formed from a later intrusion of acidic, granitic rock. This granite was more uniformly eroded by wind and water than the gabbro and basalt, causing the red hills to have smoother outlines. The Cuillin provide classic examples of glacial topography and were the subject of an early published account by James Forbes in 1846 (who had become a fellow of the Royal Society of Edinburgh aged only nineteen).
Cuillin in 1611. In 2000 the Cuillin were put on sale for £10 million by the clan chief, John MacLeod of MacLeod, in a scheme of land in exchange for repairs to Dunvegan Castle, however there was a dispute over ownership, as opponents of the sale argued that the charter referred to the MacLeod’s Tables which stand across the loch from Dunvegan Castle and not to the Cuillin themselves. A deal was cut for the property to be gifted in return for repairs to the clan castle, although it later fell through, with opponents arguing that the cost was out of