Drumlin formation within the Bustarfell drumlin field, northeast Iceland: integrating sedimentological and ground‐penetrating radar data

Aradóttir, Nína; Benediktsson, Ívar Örn; Ingólfsson, Ólafur; Sturkell, Erik; Brynjólfsson, Skafti; Farnsworth, Wesley R.; Phillips, Emrys. 2023 Drumlin formation within the Bustarfell drumlin field, northeast Iceland: integrating sedimentological and ground‐penetrating radar data. Journal of Quaternary Science, 38 (3). 386-402. https://doi.org/10.1002/jqs.3481

Before downloading, please read NORA policies.

Preview

Text Aradóttir et al._2023_Bustarfell.pdf - Accepted Version Available under License Creative Commons Attribution Non-commercial No Derivatives 4.0. Download (885kB) | Preview

Abstract/Summary

Drumlins are important bedforms of former glaciated landscapes as they demonstrate past ice-flow directions and elucidate processes that operated at the ice/bed interface. Recently mapped drumlins and other streamlined subglacial bedforms in northeast Iceland reveal the flow-sets of cross-cutting palaeo-ice streams that were active within the Iceland Ice Sheet (IIS) during and following the Last Glacial Maximum. Here we study the Bustarfell drumlin field within the Vopnafjörður–Jökuldalsheiði flow-set. The internal architecture of two drumlins was investigated using sedimentological analysis and ground-penetrating radar (GPR, 50 and 100 MHz) to illuminate subglacial processes that contributed to drumlin formation, as well as the history and dynamics of the IIS. On the stoss side of one of the drumlins, two subglacial traction till units were identified, separated by a thick unit of deformed glaciofluvial sand and gravel. The core of glaciofluvial material suggests that the drumlin formed around well-drained patches (sticky spots) in the subglacial bed that retarded the ice flow locally through increased basal drag and encouraged till deposition. Furthermore, our GPR data indicate a combination of erosional and depositional processes. We suggest that the glaciofluvial sediments were deposited as small ice-marginal fans on the Bustarfell plateau, possibly during the Bølling–Allerød interstadial, and that the drumlins were formed around these fans during a subsequent readvance during the Younger Dryas.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	https://doi.org/10.1002/jqs.3481
ISSN:	0267-8179
Date made live:	09 May 2023 13:41 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/534482

Actions (login required)

View Item

Document Downloads

More statistics for this item...