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?

Peter Wilson; Angel Rodes; Alan Smith

doi:10.1002/jqs.3030

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?

Peter Wilson
, Angel Rodes
, Alan Smith

Research output: Contribution to journal › Article › peer-review

16 Citations (Scopus)

1294 Downloads (Pure)

Original language	English
Pages (from-to)	518-526
Journal	Journal of Quaternary Science
Volume	33
Early online date	15 Apr 2018
DOIs	https://doi.org/10.1002/jqs.3030
Publication status	Published (in print/issue) - 2018

Keywords

Heinrich event 1
Lake District
terrestrial cosmogenic nuclide surface exposure dating
valley glaciers

Access to Document

10.1002/jqs.3030

TextAuthor Accepted Manuscript, 144 KB
Wilson et al-2018-Journal of Quaternary ScienceFinal published version, 2.32 MB

Cite this

@article{40ef23f4f7984c70b212288ffd8ec85d,

title = "Valley glaciers persisted in the Lake District, north-west England, until \textasciitilde{}16-15 ka as revealed by terrestrial cosmogenic nuclide (10Be) dating: a response to Heinrich event 1?",

keywords = "Heinrich event 1, Lake District, terrestrial cosmogenic nuclide surface exposure dating, valley glaciers",

author = "Peter Wilson and Angel Rodes and Alan Smith",

year = "2018",

doi = "10.1002/jqs.3030",

language = "English",

volume = "33",

pages = "518--526",

journal = "Journal of Quaternary Science",