Results 21 to 30 of about 1,200 (173)
The last glaciation of Shetland : local ice cap or invasive ice sheet? [PDF]
Issue ISBN: 978-82-92-39488-5 This work is supported by the Carnegie Trust for the Universities of ScotlandThe question of whether the Shetland Islands were covered by an ice cap or by an ice sheet during the last glacial cycle (40–10 ka) remains ...
Hall, A. M.
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Glacier sliding, seismicity and sediment entrainment
The evolution of glaciers and ice sheets depends on processes in the subglacial environment. Shear seismicity along the ice–bed interface provides a window into these processes. Such seismicity requires a rapid loss of strength that is typically ascribed
Bradley Paul Lipovsky +6 more
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Surface digital elevation models (DEMs) and slope-related estimates of glacier thickness enable modelling of glacier-bed topographies over large ice-covered areas.
A. Linsbauer +5 more
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Northwestern Nunavik (Quebec, Canada) is characterized by specific landforms and poorly documented examples of emerging coastal landscapes. In this study, we identified the different types of coasts and examined how they were morphologically reworked and
Antoine Boisson, Michel Allard
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In a period of high rates of glacier retreat, increasing meltwater discharge from tidewater glaciers can influence marine fjord ecosystems due to increase sediment delivery and accumulation rates in the proglacial environment.
Cristián Rodrigo +8 more
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Exposed schlottenkarren karst terrains developed on gypsum-anhydrite evaporites in the Canadian Maritime provinces might be post-Glacial landscape features (formed on glacially-denuded rocks after they are uncovered by progressive erosion of overlying ...
Max Moseley
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Stratigraphische Begriffe für das Quartär des süddeutschen Alpenvorlandes [PDF]
This description of the Quaternary of the south German Alpine Foreland focuses on the classic morphostratigraphical terminology sensu PENCK & BRÜCKNER, with a methodological introduction by K.A. HABBE. These definitions correspond to the nomenclature
K.A. Habbe +2 more
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Glacial erosion and bedrock properties in NW Scotland : abrasion and plucking, hardness and joint spacing [PDF]
Subglacial erosion beneath glaciers occurs predominantly by abrasion and plucking, producing distinct erosional forms. The controls on the relative importance of abrasion vs. plucking are poorly understood.
Maarten Krabbendam +3 more
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Experimental constraints on subglacial rock friction
Subglacial rock friction is an important control on the sliding dynamics and erosive potential of hard-bedded glaciers, yet it remains largely unconstrained.
Dougal D. Hansen, Lucas K. Zoet
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Assessment of the tourist attractiveness of global geoparks in Europe
The article provides an inventory of geoparks from the list of the UNESCO Global Geoparks Network. It is noted that geoparks as important tourist attractions have been the subject of scientific attention of many authors, but the data presented in these ...
M. Lushchyk +3 more
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