Using the size and position of drumlins to understand how they grow, interact and evolve

Jeremy C. Ely, Chris D. Clark, Matteo Spagnolo, Anna L. C. Hughes, Chris R. Stokes

Research output: Contribution to journalArticlepeer-review

22 Citations (Scopus)
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Drumlins are subglacial bedforms streamlined in the direction of ice flow. Common in deglaciated landscapes, they have been widely studied providing rich information on their internal geology, size, shape, and spacing. In contrast with bedform investigations elsewhere in geomorphology (aeolian and fluvial dunes and ripples for example) most drumlin studies derive observations from relict, and thus static features. This has made it difficult to gain information and insights about their evolution over time, which likely hampers our understanding of the process(es) of drumlin formation. Here we take a morphological approach, studying drumlin size and spacing metrics. Unlike previous studies which have focussed on databases derived from entire ice sheet beds, we adopt a space-for-time substitution approach using individual drumlin flow-sets distributed in space as proxies for different development times/periods. Framed and assisted by insights from aeolian and fluvial geomorphology, we use our metric data to explore possible scenarios of drumlin growth, evolution and interaction. We study the metrics of the size and spacing of 36,222 drumlins, distributed amongst 71 flow-sets, left behind by the former British-Irish Ice Sheet, and ask whether behaviour common to other bedform phenomena can be derived through statistical analysis. Through characterising and analysing the shape of the probability distribution functions of size and spacing metrics for each flow-set we argue that drumlins grow, and potentially migrate, as they evolve leading to pattern coarsening. Furthermore, our findings add support to the notion that no upper limit to drumlin size exists, and to the idea that perpetual coarsening could occur if given sufficient time. We propose that the framework of process and patterning commonly applied to non-glacial bedforms is potentially powerful for understanding drumlin formation and for deciphering glacial landscapes.
Original languageEnglish
Pages (from-to)1073-1087
Number of pages15
JournalEarth Surface Processes and Landforms
Issue number5
Early online date29 Sept 2017
Publication statusPublished - Apr 2018

Bibliographical note

JCE would like to thank Kathy and Chris Denison for supporting his PhD. This work was initiated and supported by NERC grant NE/D011175/1 led by CDC. A.L.C.H acknowledges BGS NERC PhD studentship (NE/S/A/2004/12102). Colm Ó Cofaigh and Andrew Sole are thanked for their comments during JCEs viva, and Andrew Fowler is thanked for useful discussions. John Hillier, an anonymous reviewer and the editorial team are thanked for their constructive comments.


  • drumlin
  • patterning
  • subglacial
  • bedform
  • glacial geomorphology


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