Geomorphological map** is a well-established method for examining earth surface
processes and landscape evolution in a range of environmental contexts. In glacial …

Icelandic glaciers are sensitive to climate variability on short-term timescales owing to their
North Atlantic maritime setting, and have been undergoing ice-marginal retreat since the mid …

Considerable research has been conducted in Scotland to reconstruct Younger Dryas
glaciers and palaeoclimatic conditions, but our understanding remains incomplete. In this …

This paper systematically reviews the glacial geomorphological evidence of the Loch
Lomond Stadial (LLS; Younger Dryas) glaciation in Britain (12.9–11.7 ka). The …

Glacial geomorphology relating to the Loch Lomond Stadial (Younger Dryas) in Britain is
used to construct five glacial landsystem models. These landsystems lie on a continuum of …

Small-scale recessional push moraines are a characteristic signature of the active temperate
glacial landsystem, and are often clearly linked to annual re-advances. These recessional …

A record of Younger Dryas glaciation in Scotland is well established. However, the role of
the Monadhliath, a significant plateau area extending over 840 km 2 in central Scotland, has …

ABSTRACT A 1: 4000 scale map of the terrestrial margins of the foreland of
Nordenskiöldbreen depicts a polythermal glacial landsystem containing a record of the …

Plateau icefields are a common form of mountain ice mass, frequently found in mid‐latitude
to high‐arctic regions and increasingly recognized in the Quaternary record. Their top …

This paper presents the results of an investigation of early Holocene cryptotephra layers
recovered from sediments in two kettle-hole basins at Inverlair (Glen Spean) and Loch …