Inside the Last Glaciation Limit

Ice-smoothed slabs on the northern face of Carningli. This sort of feature is difficult to date, except maybe with the aid of cosmogenic dating, but here the surface appears fresh, so I would hazard a guess that the smoothing was done by Devensian (Last Glaciation) ice -- thus matching this feature with the Pont Ceunant moraine described in the last couple of days.