During the last glaciation, most of the British Isles and the surrounding continental shelf were covered by the British–Irish Ice Sheet (BIIS). An earlier compilation from the existing literature (BRITICE version 1) assembled the relevant glacial geomorphological evidence into a freely available GIS geodatabase and map (Clark et al. 2004: Boreas 33, 359). New high-resolution digital elevation models, of the land and seabed, have become available casting the glacial landform record of the British Isles in a new light and highlighting the shortcomings of the V.1 BRITICE compilation. Here we present a wholesale revision of the evidence, onshore and offshore, to produce BRITICE version 2, which now also includes Ireland. All publishe...
Digital elevation models of the area around the Solway Lowlands reveal complex subglacial bedform im...
An inversion of the glacial geomorphological record provides an effective means to reconstruct forme...
The Loch Lomond Stadial (LLS) was an abrupt period of renewed cooling between 12.9 and 11.7 ka and h...
During the last glaciation, most of the British Isles and the surrounding continental shelf were cov...
During the last glaciation, most of the British Isles and the surrounding continental shelf were cov...
During the last glaciation, most of the British Isles and the surrounding continental shelf were cov...
A review of the academic literature and British Geological Survey mapping is employed to produce a ‘...
We here present a glacial geomorphological map covering 11,800 km2, at a scale of 1:550,000, of the ...
The last British Ice Sheet has been a focus of research for over a century, and yet we have only a g...
An inversion of the glacial geomorphological record provides an effective means to reconstruct form...
This paper reviews the evidence presently available (as at December 2003) for the compilation of the...
A review of the academic literature and British Geological Survey mapping is employed to produce a '...
The use of digital terrain mapping in determining the anatomy of the Late Devensian British–Irish Ic...
The Gaick is an enigmatic glaciated landscape in the Central Grampians, Scotland, dominated by an ex...
The BRITICE Glacial Mapping Project: version two release (2017) is a map and GIS database of glacia...
Digital elevation models of the area around the Solway Lowlands reveal complex subglacial bedform im...
An inversion of the glacial geomorphological record provides an effective means to reconstruct forme...
The Loch Lomond Stadial (LLS) was an abrupt period of renewed cooling between 12.9 and 11.7 ka and h...
During the last glaciation, most of the British Isles and the surrounding continental shelf were cov...
During the last glaciation, most of the British Isles and the surrounding continental shelf were cov...
During the last glaciation, most of the British Isles and the surrounding continental shelf were cov...
A review of the academic literature and British Geological Survey mapping is employed to produce a ‘...
We here present a glacial geomorphological map covering 11,800 km2, at a scale of 1:550,000, of the ...
The last British Ice Sheet has been a focus of research for over a century, and yet we have only a g...
An inversion of the glacial geomorphological record provides an effective means to reconstruct form...
This paper reviews the evidence presently available (as at December 2003) for the compilation of the...
A review of the academic literature and British Geological Survey mapping is employed to produce a '...
The use of digital terrain mapping in determining the anatomy of the Late Devensian British–Irish Ic...
The Gaick is an enigmatic glaciated landscape in the Central Grampians, Scotland, dominated by an ex...
The BRITICE Glacial Mapping Project: version two release (2017) is a map and GIS database of glacia...
Digital elevation models of the area around the Solway Lowlands reveal complex subglacial bedform im...
An inversion of the glacial geomorphological record provides an effective means to reconstruct forme...
The Loch Lomond Stadial (LLS) was an abrupt period of renewed cooling between 12.9 and 11.7 ka and h...