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Open AccessJournal ArticleDOI

Subglacial bedforms of the last British Ice Sheet

TLDR
In this article, the authors presented the first consistent and countrywide map of subglacial bedforms for Britain produced from systematic mapping, where individual landforms were mapped from relief-shaded renditions of high-resolution elevation data and Landsat TM imagery.
Abstract
Please click here to download the map associated with this article. Subglacial bedforms are a characteristic feature of formerly glaciated landscapes. Formed parallel (e.g. drumlins) or transverse (ribbed moraine) to ice flow their preserved distribution is a valuable record of ice sheet configuration. To date these landforms have been underused in Britain such that we have only a simple static view of the flow patterns of the last British Ice Sheet, with glimpses of complexity recorded in just a few locations. Arguably, this is because of the lack of a suitable, ice-sheet scale, map of subglacial bedform distribution. We present the first consistent and countrywide map of subglacial bedforms for Britain produced from systematic mapping. Individual landforms were mapped from relief-shaded renditions of high-resolution elevation data and Landsat TM imagery. The outline or crest-line of each bedform was manually captured by onscreen digitisation directly into a Geographic Information System (GIS) d...

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Citations
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The last Eurasian ice sheets - a chronological database and time-slice reconstruction, DATED-1

TL;DR: In this paper, the authors present a new time-slice reconstruction of the Eurasian ice sheets (British-Irish, Svalbard-Barents-Kara Seas and Scandinavian) documenting the spatial evolution of these interconnected ice sheets every 1000 years from 25 to 10 years and at four selected time periods back to 40 years.
Journal ArticleDOI

Flow-pattern evolution of the last British Ice Sheet

TL;DR: In this paper, a 10-stage reconstruction of the evolution in ice-flow patterns of the last British Ice Sheet from build-up to demise derived from geomorphological evidence is presented.
Journal ArticleDOI

Do subglacial bedforms comprise a size and shape continuum

TL;DR: In this paper, the authors analyzed the largest data set of subglacial bedform size and shape measurements and found that flutes form a distinct population of narrow bedforms and a continuum of sub-glacial ribs also exists, with no clear size or shape distinctions indicating separate populations.
References
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Journal ArticleDOI

Late Wisconsinan and Holocene History of the Laurentide Ice Sheet

TL;DR: The history of advance, retreat, and readvances of the Laurentide Ice Sheet along with associated changes in proglacial drainage and relative sea level oscillations for Late Wisconsinan and Holocene times is described in this paper.
Journal ArticleDOI

Fennoscandian palaeoglaciology reconstructed using a glacial geological inversion model

TL;DR: In this article, the evolution of ice-sheet configuration and flow pattern in Fennoscandia through the last glacial cycle was reconstructed using a glacial geological inversion model, i.e. a theoretical model that formalises the procedure of using the landform record to reconstruct ice sheets.
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Methods for the visualization of digital elevation models for landform mapping

TL;DR: A variety of techniques that can visualize a DEM are described and curvature visualization is recommended for initial mapping as this provides a non-illuminated (and therefore unbiased) image and no single visualization method provides complete and unbiased mapping.
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A highly mobile Laurentide ice sheet revealed by satellite images of glacial lineations

TL;DR: Satellite images of the North American continent reveal previously unrecognized patterns of crossing drift lineations reflecting unexpected shifts of centres of mass of the Laurentide ice sheet throughout the last glacial cycle.
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