Valley glaciers persisted in the Lake District, north‐west England, until ∼16–15 ka as revealed by terrestrial cosmogenic nuclide (10Be) dating: a response to Heinrich event 1?
The Lake District of north‐west England acted as an independent centre of ice dispersal within the more extensive British–Irish Ice Sheet (BIIS) during the Last Glacial Maximum, but relatively little is known about the pattern and timing of glacier retreat. Four new terrestrial cosmogenic nuclide (1...
| Published in: | Journal of Quaternary Science |
|---|---|
| Main Authors: | , , |
| Format: | Article in Journal/Newspaper |
| Language: | unknown |
| Published: |
Wiley on behalf of Quaternary Research Association
2018
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| Subjects: | |
| Online Access: | http://eprints.gla.ac.uk/196804/ |