Gales, J.A. 
ORCID: https://orcid.org/0000-0003-4402-5800; Larter, R.D. ORCID: https://orcid.org/0000-0002-8414-7389; Leat, P.T..
2016
Submarine gullies on the southern Weddell Sea slope, Antarctica.
In: Dowdeswell, J.A., (ed.)
Atlas of submarine glacial landforms : modern, Quaternary and ancient.
London, UK, Geological Society of London, 383-384.
(Geological Society Memoir, 46, 46).
Abstract
Submarine gullies are small-scale, confined channels on the order of tens of metres depth that form one of the most common morphological features of high-latitude continental slopes. Gully morphology varies in width, incision depth, length, sinuosity, branching order, shelf-incision, cross-sectional shape and gully spacing, with six distinct gully signatures recognized on high-latitude continental slopes (Gales et al. 2013a, b). Here we analyse the morphology of slope gullies off Halley and Filchner troughs in the southern Weddell Sea (Fig. 1a–f).
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Programmes:
BGS Programmes 2013 > Geology & Regional Geophysics
BAS Programmes 2015 > Palaeo-Environments, Ice Sheets and Climate Change
BAS Programmes 2015 > Palaeo-Environments, Ice Sheets and Climate Change
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