Re-interpretation of ‘hummocky moraine’ in the Gaick, Scotland, as erosional remnants : Implications for palaeoglacier dynamics
Many glaciated valleys in Scotland contain distinctive, closely spaced ridges and mounds, which have been termed ‘hummocky moraine’. The ridges and mounds are widely interpreted as ice-marginal moraines, constructed during active retreat of mainly temperate glaciers. However, hummocky terrain can form by various processes in glacial environments, and it may relate to a range of contrasting glaciod
