A review of the academic literature and British Geological Survey mapping is employed to produce a 'Glacial Map', and accompanying geographic information system (GIS) database, of features related to the last (Devensian) British Ice Sheet. The map (1:625 000) is included in a folder and GIS data are freely available by web download (http://www.shef.ac.uk/geography/staff/clark_chris/britice.html). Emphasis is on information that constrains the last ice sheet. The following are included: moraines, eskers, drumlins, meltwater channels, tunnel valleys, trimlines, limit of key glacigenic deposits, glaciolacustrine deposits, ice-dammed lakes, erratic dispersal patterns, shelf-edge fans and the Loch Lomond Readvance limit of the main ice cap. The ...
Subglacial bedforms are a characteristic feature of formerly glaciated landscapes. Formed parallel (...
The Loch Lomond Stadial (LLS) was an abrupt period of renewed cooling between 12.9 and 11.7 ka and h...
An inversion of the glacial geomorphological record provides an effective means to reconstruct forme...
A review of the academic literature and British Geological Survey mapping is employed to produce a '...
This paper reviews the evidence presently available (as at December 2003) for the compilation of the...
The last British Ice Sheet has been a focus of research for over a century, and yet we have only a g...
This paper reviews the evidence presently available (as at December 2003) for the compilation of the...
<p>This paper presents a detailed glacial Main Map of the Great Glen region of Scotland, UK, coverin...
During the last glaciation, most of the British Isles and the surrounding continental shelf were cov...
The Gaick is an enigmatic glaciated landscape in the Central Grampians, Scotland, dominated by an ex...
We here present a glacial geomorphological map covering 11,800 km2, at a scale of 1:550,000, of the ...
During the last glacial the ice sheet that subsumed most of Britain, Ireland and the North Sea attai...
During the last glaciation, most of the British Isles and the surrounding continental shelf were cov...
In 2006 the British Geological Survey initiated a new cross-thematic project specifically to examine...
During the last glaciation, most of the British Isles and the surrounding continental shelf were cov...
Subglacial bedforms are a characteristic feature of formerly glaciated landscapes. Formed parallel (...
The Loch Lomond Stadial (LLS) was an abrupt period of renewed cooling between 12.9 and 11.7 ka and h...
An inversion of the glacial geomorphological record provides an effective means to reconstruct forme...
A review of the academic literature and British Geological Survey mapping is employed to produce a '...
This paper reviews the evidence presently available (as at December 2003) for the compilation of the...
The last British Ice Sheet has been a focus of research for over a century, and yet we have only a g...
This paper reviews the evidence presently available (as at December 2003) for the compilation of the...
<p>This paper presents a detailed glacial Main Map of the Great Glen region of Scotland, UK, coverin...
During the last glaciation, most of the British Isles and the surrounding continental shelf were cov...
The Gaick is an enigmatic glaciated landscape in the Central Grampians, Scotland, dominated by an ex...
We here present a glacial geomorphological map covering 11,800 km2, at a scale of 1:550,000, of the ...
During the last glacial the ice sheet that subsumed most of Britain, Ireland and the North Sea attai...
During the last glaciation, most of the British Isles and the surrounding continental shelf were cov...
In 2006 the British Geological Survey initiated a new cross-thematic project specifically to examine...
During the last glaciation, most of the British Isles and the surrounding continental shelf were cov...
Subglacial bedforms are a characteristic feature of formerly glaciated landscapes. Formed parallel (...
The Loch Lomond Stadial (LLS) was an abrupt period of renewed cooling between 12.9 and 11.7 ka and h...
An inversion of the glacial geomorphological record provides an effective means to reconstruct forme...