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Complex kame belt morphology, stratigraphy and architecture

Research output: Contribution to journal › Article

The development of glacier karst at the margins of melting ice sheets produces
complex glaciofluvial sediment-landform assemblages that provide information on icesheet downwasting processes. We present the first combined geomorphological, sedimentological and geophysical investigation of the Brampton Kame Belt, an important glaciofluvial depositional zone at the centre of the last British-Irish Ice Sheet. Ground-penetrating radar (GPR) data allow the broad scale internal architecture of ridges (eskers) and flat-topped hills (ice-walled lake plains) to be determined at four sites. In combination with sediment exposures, these provide information on lateral and vertical variations in accretion styles, depositional boundaries, and grain size changes. Building on existing work on the subject, we propose a refined model for the formation of ice-walled lake plains resulting from the evolution and collapse of major
drainage axes into lakes as stable glacier karst develops during deglaciation. The
internal structure of esker ridges demonstrates variations in sedimentation that can be linked to differences in ridge morphologies across the kame belt. This includes low energy flow conditions and multiple accretion phases identified within large S-N oriented esker ridges; and fluctuating water pressures, hyperconcentrated flows, and significant deformation within a fragmented SW-NE oriented esker ridge. In combination with updated geomorphological mapping, this work allows us to identify two main styles of drainage within the kame belt: (1) major drainage axes aligned broadly S-N that extend through the entire kame belt and collapsed into a chain of icewalled lakes; and (2) a series of smaller, fragmented SW-NE aligned esker ridges that represent ice-marginal drainage as the ice sheet receded south-eastwards up the Vale of Eden. Our study demonstrates the importance of integrated geomorphological, sedimentological and geophysical investigations in order to understand complex and polyphase glaciofluvial sediment-landform assemblages.
Original languageEnglish
JournalEarth Surface Processes and Landforms
Early online date30 Jun 2019
DOIs
Publication statusEarly online - 30 Jun 2019

Documents

  • Lovell et al. (2019) (accepted manuscript)

    Rights statement: This is the peer reviewed version of the following article: Lovell, H., Livingstone, S. J., Boston, C. M., Booth, A. D., Storrar, R. D., and Barr, I. D. ( 2019) Complex kame belt morphology, stratigraphy and architecture. Earth Surf. Process. Landforms, , which has been published in final form at https://doi.org/10.1002/esp.4696. This article may be used for non-commercial purposes in accordance with Wiley Terms and Conditions for Use of Self-Archived Versions.

    Accepted author manuscript (Post-print), 2.31 MB, PDF document

    Due to publisher’s copyright restrictions, this document is not freely available to download from this website until: 30/06/20

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