[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 …
Pattern and timing of retreat of the last British-Irish Ice Sheet
During the last glacial the ice sheet that subsumed most of Britain, Ireland and the North Sea
attained its maximum extent by 27 ka BP and with an ice volume sufficient to raise global …
attained its maximum extent by 27 ka BP and with an ice volume sufficient to raise global …
The last Eurasian ice sheets–a chronological database and time‐slice reconstruction, DATED‐1
We 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 …
Svalbard–Barents–Kara Seas and Scandinavian) documenting the spatial evolution of these …
Growth and retreat of the last British–Irish Ice Sheet, 31 000 to 15 000 years ago: the BRITICE‐CHRONO reconstruction
The BRITICE‐CHRONO consortium of researchers undertook a dating programme to
constrain the timing of advance, maximum extent and retreat of the British–Irish Ice Sheet …
constrain the timing of advance, maximum extent and retreat of the British–Irish Ice Sheet …
Glacial geomorphological mapping: A review of approaches and frameworks for best practice
Geomorphological mapping 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 …
BRITICE Glacial Map, version 2: a map and GIS database of glacial landforms of the last British–Irish Ice Sheet
During the last glaciation, most of the British Isles and the surrounding continental shelf were
covered by the British–Irish Ice Sheet (BIIS). An earlier compilation from the existing …
covered by the British–Irish Ice Sheet (BIIS). An earlier compilation from the existing …
[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 …
Gas hydrate dissociation off Svalbard induced by isostatic rebound rather than global warming
Methane seepage from the upper continental slopes of Western Svalbard has previously
been attributed to gas hydrate dissociation induced by anthropogenic warming of ambient …
been attributed to gas hydrate dissociation induced by anthropogenic warming of ambient …
[HTML][HTML] Rock-slope failure following Late Pleistocene deglaciation on tectonically stable mountainous terrain
CK Ballantyne, GF Sandeman, JO Stone… - Quaternary Science …, 2014 - Elsevier
The ages of 31 postglacial rock-slope failures (RSFs) in Scotland and NW Ireland, derived
from 89 cosmogenic isotope exposure ages, are employed to analyse the temporal pattern …
from 89 cosmogenic isotope exposure ages, are employed to analyse the temporal pattern …
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 …