Total meltwater volume since the Last Glacial Maximum and viscosity structure of Earth's mantle inferred from relative sea level changes at Barbados and Bonaparte Gulf and GIA-inducedJ̇2

2015 ◽  
Vol 204 (2) ◽  
pp. 1237-1253 ◽  
Author(s):  
Masao Nakada ◽  
Jun'ichi Okuno ◽  
Yusuke Yokoyama
Keyword(s):  
Sea Level ◽  
Last Glacial Maximum ◽  
Glacial Maximum ◽  
Sea Level Changes ◽  
Relative Sea Level ◽  
Last Glacial ◽  
Earth’S Mantle ◽  
The Last Glacial Maximum ◽  
The Last Glacial

Relative sea-level changes, glacial isostatic modelling and ice-sheet reconstructions from the British Isles since the Last Glacial Maximum

2006 ◽  
Vol 21 (6) ◽  
pp. 585-599 ◽  
Author(s):  
Ian Shennan ◽  
Sarah Bradley ◽  
Glenn Milne ◽  
Anthony Brooks ◽  
Sophie Bassett ◽  
...  
Keyword(s):  
Sea Level ◽  
Last Glacial Maximum ◽  
Ice Sheet ◽  
Glacial Maximum ◽  
British Isles ◽  
Sea Level Changes ◽  
Relative Sea Level ◽  
Last Glacial ◽  
The Last Glacial Maximum ◽  
The Last Glacial

scholarly journals Shoreface migrations at the shelf edge and sea-level changes around the Last Glacial Maximum (Gulf of Lions, NW Mediterranean)

2006 ◽  
Vol 234 (1-4) ◽  
pp. 21-42 ◽  
Author(s):  
G. Jouet ◽  
S. Berné ◽  
M. Rabineau ◽  
M.A. Bassetti ◽  
P. Bernier ◽  
...  
Keyword(s):  
Sea Level ◽  
Last Glacial Maximum ◽  
Glacial Maximum ◽  
Shelf Edge ◽  
Sea Level Changes ◽  
Gulf Of Lions ◽  
Last Glacial ◽  
Nw Mediterranean ◽  
The Last Glacial Maximum ◽  
The Last Glacial

scholarly journals Submarine Geomorphology of the Southwestern Sardinian Continental Shelf (Mediterranean Sea): Insights into the Last Glacial Maximum Sea-Level Changes and Related Environments

Water ◽  
2021 ◽  
Vol 13 (2) ◽  
pp. 155
Author(s):  
Giacomo Deiana ◽  
Luciano Lecca ◽  
Rita Teresa Melis ◽  
Mauro Soldati ◽  
Valentino Demurtas ◽  
...  
Keyword(s):  
Continental Shelf ◽  
Sea Level ◽  
Last Glacial Maximum ◽  
Glacial Maximum ◽  
Sea Level Changes ◽  
Side Scan Sonar ◽  
Last Glacial ◽  
Depositional Processes ◽  
The Last Glacial Maximum ◽  
The Last Glacial

During the lowstand sea-level phase of the Last Glacial Maximum (LGM), a large part of the current Mediterranean continental shelf emerged. Erosional and depositional processes shaped the coastal strips, while inland areas were affected by aeolian and fluvial processes. Evidence of both the lowstand phase and the subsequent phases of eustatic sea level rise can be observed on the continental shelf of Sardinia (Italy), including submerged palaeo-shorelines and landforms, and indicators of relict coastal palaeo-environments. This paper shows the results of a high-resolution survey on the continental shelf off San Pietro Island (southwestern Sardinia). Multisensor and multiscale data—obtained by means of seismic sparker, sub-bottom profiler chirp, multibeam, side scan sonar, diving, and uncrewed aerial vehicles—made it possible to reconstruct the morphological features shaped during the LGM at depths between 125 and 135 m. In particular, tectonic controlled palaeo-cliffs affected by landslides, the mouth of a deep palaeo-valley fossilized by marine sediments and a palaeo-lagoon containing a peri-littoral thanatocenosis (18,983 ± 268 cal BP) were detected. The Younger Dryas palaeo-shorelines were reconstructed, highlighted by a very well preserved beachrock. The coastal paleo-landscape with lagoon-barrier systems and retro-littoral dunes frequented by the Mesolithic populations was reconstructed.

Relative sea-level observations in western Scotland since the Last Glacial Maximum for testing models of glacial isostatic land movements and ice-sheet reconstructions

2006 ◽  
Vol 21 (6) ◽  
pp. 601-613 ◽  
Author(s):  
Ian Shennan ◽  
Sarah Hamilton ◽  
Caroline Hillier ◽  
Amanda Hunter ◽  
Ruth Woodall ◽  
...  
Keyword(s):  
Sea Level ◽  
Last Glacial Maximum ◽  
Ice Sheet ◽  
Glacial Maximum ◽  
Relative Sea Level ◽  
Last Glacial ◽  
The Last Glacial Maximum ◽  
The Last Glacial
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