Articles | Volume 14, issue 6
https://doi.org/10.5194/tc-14-1989-2020
https://doi.org/10.5194/tc-14-1989-2020
Research article
 | 
18 Jun 2020
Research article |  | 18 Jun 2020

A quasi-annual record of time-transgressive esker formation: implications for ice-sheet reconstruction and subglacial hydrology

Stephen J. Livingstone, Emma L. M. Lewington, Chris D. Clark, Robert D. Storrar, Andrew J. Sole, Isabelle McMartin, Nico Dewald, and Felix Ng

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ED: Publish subject to minor revisions (review by editor) (16 Apr 2020) by Kerim Nisancioglu
AR by Stephen Livingstone on behalf of the Authors (17 Apr 2020)  Author's response   Manuscript 
ED: Publish subject to minor revisions (review by editor) (12 May 2020) by Kerim Nisancioglu
ED: Publish as is (15 May 2020) by Kerim Nisancioglu
AR by Stephen Livingstone on behalf of the Authors (15 May 2020)
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Short summary
We map series of aligned mounds (esker beads) across central Nunavut, Canada. Mounds are interpreted to have formed roughly annually as sediment carried by subglacial rivers is deposited at the ice margin. Chains of mounds are formed as the ice retreats. This high-resolution (annual) record allows us to constrain the pace of ice retreat, sediment fluxes, and the style of drainage through time. In particular, we suggest that eskers in general record a composite signature of ice-marginal drainage.