Lodgement Till is a type of glacial till that is deposited subglacially through the direct, cohesive emplacement of sediment beneath a glacier or ice sheet as a result of the melting of basal ice or the loss of shear strength at the ice-bed interface, distinguished from other tills by its formation mechanism involving frictional freezing to the glacier sole and typically exhibiting a dense, compacted fabric with evidence of deformation in place.
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3.9K
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114
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78
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2017–2026
3
Variants
Lodgment Till
Publications
72
Till fabric associated with deformable beds
Jane Hart · Earth Surface Processes and Landforms · 1994 · 161 citations
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114
- JK
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- MS
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1–5 of 114
Institutions
78
University of Copenhagen
Copenhagen, Denmark
11 h-index
11 publications
600 citations
Geocenter Denmark
Copenhagen, Denmark
5 h-index
5 publications
305 citations
University of Cambridge
Cambridge, United Kingdom
3 h-index
4 publications
662 citations
Queen's University Belfast
Belfast, United Kingdom
2 h-index
6 publications
174 citations
University of the Fraser Valley
Abbotsford, Canada
2 h-index
3 publications
131 citations
Trinity College Dublin
Dublin, Ireland
2 h-index
3 publications
63 citations
British Geological Survey
Nottingham, United Kingdom
2 h-index
3 publications
89 citations
University of Oxford
Oxford, United Kingdom
2 h-index
2 publications
162 citations
1–8 of 78
Venues
- Boreas
11 publications · 647 citations
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- Journal of Glaciology
10 publications · 522 citations
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- Journal of Quaternary Science
JQS · 4 publications · 217 citations
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- Canadian Journal of Earth Sciences
4 publications · 228 citations
4
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- Canadian Geotechnical Journal
4 publications · 144 citations
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