The Old Man of Hoy is a sea stack on Hoy, part of the Orkney archipelago off the north coast of Scotland. Formed from Old Red Sandstone, it is one of the tallest stacks in the United Kingdom. The Old Man is popular with climbers, and was first climbed in 1966. Created by the erosion of a cliff through hydraulic action some time after 1750, the stack is not more than a few hundred years old, but may soon collapse into the sea. Geography The Old Man stands close to Rackwick Bay on the west coast of Hoy, in Orkney, Scotland, and can be seen from the Scrabster to Stromness ferry. From certain angles it is said to resemble a human figure. Winds are faster than for nearly a third of the time, and gales occur on average for 29 days a year. Combined with the depth of the sea, which quickly falls to , high-energy waves on the western side of Hoy lead to rapid erosion of the coast. Geology The Old Man of Hoy is a red sandstone stack, perched on a plinth of basalt rock, and one of the tallest sea stacks in the UK. It is separated from the mainland by a 60-metre (200 ft) chasm strewn with debris, and has nearly vertical sides with a top just a few metres wide. The rock is composed of layers of soft, sandy and pebbly sandstone and harder flagstones of Old Red Sandstone, giving the sides a notched and slab-like profile. History The Old Man is probably less than 250 years old and may be in danger of collapsing. The stack is not mentioned in the Orkneyinga saga, written 1230, and on the Blaeu map of 1600, a headland exists at the point where the Old Man is now. The McKenzie map of Hoy of 1750 similarly shows a headland but no stack, but by 1819 the Old Man had been separated from the mainland. William Daniell sketched the sea stack at this time as a wider column with a smaller top section and an arch at the base, from which it derived its name. Sometime in the early nineteenth century, a storm washed away one of the legs leaving it much as it is today, although erosion continues. By 1992 a 40-metre (130 ft) crack had appeared in the top of the south face, leaving a large