Glen More, on the Isle of Mull, Scotland, is a classic locality for studying glacial landforms and sediments. Here, two prominent ice-transported boulders stand guard at the head of the valley, left behind after the Loch Lomond Readvance (Younger Dryas stade), the final pulse of Quaternary glaciation in Scotland. Behind them in the characteristic U-shaped valley, hummocky morraines are littered wi ...[Read More]
Imaggeo on Mondays: When boulders hitch a ride from glaciers
Glacially transported boulders, Glen More. Credit: Ian Watkinson (distributed via imaggeo.egu.eu)