[HTML][HTML] Deglaciation of the Eurasian ice sheet complex
The Eurasian ice sheet complex (EISC) was the third largest ice mass during the Last
Glacial Maximum with a span of over 4500 km and responsible for around 20 m of eustatic …
Glacial Maximum with a span of over 4500 km and responsible for around 20 m of eustatic …
Glacial geomorphological map**: A review of approaches and frameworks for best practice
Geomorphological map** is a well-established method for examining earth surface
processes and landscape evolution in a range of environmental contexts. In glacial …
processes and landscape evolution in a range of environmental contexts. In glacial …
[КНИГА][B] Glaciers and glaciation
Glaciers and Glaciation is the classic textbook for all students of glaciation. Stimulating and
accessible, it has established a reputation as a comprehensive and essential resource. In …
accessible, it has established a reputation as a comprehensive and essential resource. In …
[КНИГА][B] Glacial geology: ice sheets and landforms
MM Bennett, NF Glasser - 2011 - books.google.com
The new Second Edition of Glacial Geology provides a modern, comprehensive summary of
glacial geology and geomorphology. It is has been thoroughly revised and updated from the …
glacial geology and geomorphology. It is has been thoroughly revised and updated from the …
[HTML][HTML] Arctic Ocean glacial history
While there are numerous hypotheses concerning glacial–interglacial environmental and
climatic regime shifts in the Arctic Ocean, a holistic view on the Northern Hemisphere's late …
climatic regime shifts in the Arctic Ocean, a holistic view on the Northern Hemisphere's late …
[HTML][HTML] Reconciling records of ice streaming and ice margin retreat to produce a palaeogeographic reconstruction of the deglaciation of the Laurentide Ice Sheet
This paper reconstructs the deglaciation of the Laurentide Ice Sheet (LIS; including the
Innuitian Ice Sheet) from the Last Glacial Maximum (LGM), with a particular focus on the …
Innuitian Ice Sheet) from the Last Glacial Maximum (LGM), with a particular focus on the …
[HTML][HTML] The build-up, configuration, and dynamical sensitivity of the Eurasian ice-sheet complex to Late Weichselian climatic and oceanic forcing
The Eurasian ice-sheet complex (EISC) was the third largest ice mass during the Last
Glacial Maximum (LGM), after the Antarctic and North American ice sheets. Despite its …
Glacial Maximum (LGM), after the Antarctic and North American ice sheets. Despite its …
Timescales of methane seepage on the Norwegian margin following collapse of the Scandinavian Ice Sheet
Gas hydrates stored on continental shelves are susceptible to dissociation triggered by
environmental changes. Knowledge of the timescales of gas hydrate dissociation and …
environmental changes. Knowledge of the timescales of gas hydrate dissociation and …
Ice-sheet grounding-zone wedges (GZWs) on high-latitude continental margins
Grounding-zone wedges (GZWs) are asymmetric sedimentary depocentres which form
through the rapid accumulation of glacigenic debris along a line-source at the grounding …
through the rapid accumulation of glacigenic debris along a line-source at the grounding …
On the reconstruction of palaeo-ice sheets: recent advances and future challenges
Reconstructing the growth and decay of palaeo-ice sheets is critical to understanding
mechanisms of global climate change and associated sea-level fluctuations in the past …
mechanisms of global climate change and associated sea-level fluctuations in the past …