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Timing of terminal Pleistocene deglaciation at high elevations in southern and central British Columbia constrained by 10Be exposure dating

Margold, Martin, Stroeven, Arjen P., Clague, John J., Heyman, Jakob·2014·Quaternary Science Reviews
DOI 10.1016/j.quascirev.2014.06.027
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  • This finding is consistent with a trend of ice sheet thinning by around 14.0 ka, during which the Cordilleran Ice Sheet contributed 2.5-3.0 m to eustatic sea-level rise.

    “This finding is consistent with a trend of ice sheet thinning by around 14.0 ka, during which the Cordilleran Ice Sheet contributed 2.5-3.0 m to eustatic sea-level rise (Lambeck et al., 2014;Margold et al., 2014;Menounos et al., 2017), potentially contributing to meltwater pulses at this time (Gomez et al., 2015;Gregoire et al., 2016Gregoire et al., , 2012;;Ivanovic et al., 2017).”

    From Retreat of the Western Cordilleran Ice Sheet Margin During the Last Deglaciation (2018) · cites this paper as Margold et al., 2014

  • The Cordilleran Ice Sheet contributed 2.5-3.0 m to eustatic sea-level rise during ice sheet thinning by around 14.0 ka.

    “This finding is consistent with a trend of ice sheet thinning by around 14.0 ka, during which the Cordilleran Ice Sheet contributed 2.5-3.0 m to eustatic sea-level rise (Lambeck et al., 2014;Margold et al., 2014;Menounos et al., 2017), potentially contributing to meltwater pulses at this time (Gomez et al., 2015;Gregoire et al., 2016Gregoire et al., , 2012;;Ivanovic et al., 2017).”

    From Retreat of the Western Cordilleran Ice Sheet Margin During the Last Deglaciation (2018) · cites this paper as Margold et al., 2014

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Authors
Margold, M., Stroeven, A. P., Clague, J. J., & Heyman, J.
Venue
Quaternary Science Reviews
Publisher
Elsevier BV
Published
2014-09
Volume
99
Pages
193-202
ISSN
0277-3791
DOI
10.1016/j.quascirev.2014.06.027
Cited by
23
References
0
Language
en
Licence
www.elsevier.com/tdm/userlicense/1.0/ (tdm)

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