— — Scotland, folded small and set in the sea.
“The Highland Boundary Fault runs straight through Arran, so the north half is granite mountain and the south half is rolling lowland. Locals call it Scotland in miniature. The Machrie Moor standing stones have held the western shore since before the Bronze Age. The ferry from Ardrossan takes about 55 minutes; on a clear morning Goatfell is visible the whole way across.
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Arran sits in the Firth of Clyde off Scotland's Ayrshire coast, roughly 432 square kilometres, the seventh-largest Scottish island. The Highland Boundary Fault crosses it on a diagonal from Lochranza in the north to Dippin Head in the south, dividing the island geologically between Highland granite and Lowland sedimentary rock. Brodick, the main town, sits on the eastern shore opposite the fourteenth-century Brodick Castle. The CalMac ferry from Ardrossan on the mainland makes the crossing in about 55 minutes through the year.
The Machrie Moor standing stones on the west coast are a complex of six Neolithic and Bronze Age stone circles dating roughly from 3500 to 1500 BCE. The tallest stone still standing rises 5.5 metres; several fell or were buried in the peat and were re-erected during nineteenth-century excavation. Goatfell, the granite peak that crowns the north of the island at 874 metres, was raised by the same Caledonian orogeny that built the Highlands. The exposed pink-grey granite catches the late light over the Firth.
Arran's weather comes off the Atlantic and the Firth. The west coast at Machrie sits in a relative rain-shadow; the north and east hold the cloud against Goatfell and the Cir Mhòr ridge. Spring brings primrose and bluebell to the glens; summer is the walking season on the Goatfell path, a 12-kilometre return from Brodick. The Arran Coastal Way circles the island in 105 kilometres, generally walked over seven days. Mid-September is when the heather on the lower slopes turns purple.