[HTML][HTML] Ice streams in the Laurentide Ice Sheet: Identification, characteristics and comparison to modern ice sheets
This paper presents a comprehensive review and synthesis of ice streams in the Laurentide
Ice Sheet (LIS) based on a new mapping inventory that includes previously hypothesised ice …
Ice Sheet (LIS) based on a new mapping inventory that includes previously hypothesised ice …
[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 …
Ice-sheet grounding-zone wedges (GZWs) on high-latitude continental margins
CL Batchelor, JA Dowdeswell - Marine Geology, 2015 - Elsevier
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 …
Ice streams in the Laurentide Ice Sheet: a new mapping inventory
Rapidly flowing ice streams dominate the drainage of continental ice sheets and are a key
component of their mass balance. Due to their potential impact on sea level, their activity in …
component of their mass balance. Due to their potential impact on sea level, their activity in …
Reconstructing the last Irish Ice Sheet 1: changing flow geometries and ice flow dynamics deciphered from the glacial landform record
SL Greenwood, CD Clark - Quaternary Science Reviews, 2009 - Elsevier
The glacial geomorphological record provides an effective means to reconstruct former ice
sheets at ice sheet scale. In this paper we document our approach and methods for …
sheets at ice sheet scale. In this paper we document our approach and methods for …
Deglaciation of the Laurentide ice sheet from the last glacial maximum
CR Stokes - Cuadernos de investigación …, 2017 - durham-repository.worktribe.com
The last deglaciation of the Laurentide Ice Sheet (LIS) was associated with major
reorganisations in the ocean-climate system and its retreat also represents a valuable …
reorganisations in the ocean-climate system and its retreat also represents a valuable …
Diagnosing ice sheet grounding line stability from landform morphology
The resilience of a marine-based ice sheet is strongly governed by the stability of its
grounding lines, which are in turn sensitive to ocean-induced melting, calving, and flotation …
grounding lines, which are in turn sensitive to ocean-induced melting, calving, and flotation …
Seabed corrugations beneath an Antarctic ice shelf revealed by autonomous underwater vehicle survey: origin and implications for the history of Pine Island Glacier
Ice shelves are critical features in the debate about West Antarctic ice sheet change and sea
level rise, both because they limit ice discharge and because they are sensitive to change in …
level rise, both because they limit ice discharge and because they are sensitive to change in …
Major advance of South Georgia glaciers during the Antarctic Cold Reversal following extensive sub-Antarctic glaciation
AGC Graham, G Kuhn, O Meisel… - Nature …, 2017 - nature.com
The history of glaciations on Southern Hemisphere sub-polar islands is unclear. Debate
surrounds the extent and timing of the last glacial advance and termination on sub-Antarctic …
surrounds the extent and timing of the last glacial advance and termination on sub-Antarctic …
Sedimentary imprints of former ice-sheet margins: Insights from an end-Ordovician archive (SW Libya)
F Girard, JF Ghienne, X Du-Bernard, JL Rubino - Earth-Science Reviews, 2015 - Elsevier
From the Proterozoic to the Quaternary, the evolution of the Earth was characterised by
recurrent periods of glaciation. However, the margins of many ancient ice-sheets are poorly …
recurrent periods of glaciation. However, the margins of many ancient ice-sheets are poorly …