Results 91 to 100 of about 708,716 (215)
Insights into glacial processes from micromorphology of silt-sized sediment [PDF]
Silt-rich meltwater plume deposits (MPDs) analyzed from marine sediment cores have elucidated relationships that are clearly connected, yet difficult to constrain, between subglacial hydrology, ice-marginal landforms, and grounding-zone retreat patterns ...
A. P. Lepp +9 more
doaj +1 more source
ABSTRACT This study examines the impact of geological, marine and anthropogenic sources on metal and metalloid concentrations in the forefields of four glaciers (Ecology, Sphinx, Tower and Windy) on King George Island, Antarctic. Water samples were collected at the beginning and end of the hydrological season (austral summer, December 2021 to February ...
Joanna Potapowicz +8 more
wiley +1 more source
Glaciers expel large amounts of water and sediments, and the discharge of both is influenced by glacier retreat. Because the majority of sediment originates subglacially, as opposed to proglacially, focus must be given to subglacial sediment discharge ...
Ian Delaney +4 more
doaj +1 more source
<p>Sediment core descriptions, Kruskal-Wallis summary statistics, and mineral phase content from X-ray diffraction data tables.</p>
et al., Timothy D. Campbell
openaire +1 more source
Deformation of Subglacial Sediments and its Implications (Abstract only) [PDF]
Field experiments have shown that unlithified sediments beneath a glacier may undergo strong shear deformation in response to the movement of the overlying glacier, and that much of the forward movement of the glacier may be contributed by this mechanism.
openaire +1 more source
Ice-shelf channels are long curvilinear tracts of thin ice found on Antarctic ice shelves. Many of them originate near the grounding line, but their formation mechanisms remain poorly understood.
R. Drews +11 more
semanticscholar +1 more source
Wet subglacial bedforms of the NE Greenland Ice Stream shear margins
We describe elongate, wet, subglacial bedforms in the shear margins of the NE Greenland Ice Stream and place some constraints on their formation. Lateral shear margin moraines have been observed across the previously glaciated landscape, but little is ...
Kiya L. Riverman +8 more
doaj +1 more source
Subglacial water and sediment samplers [PDF]
Erik W. Blake, Garry K.C. Clarke
openaire +1 more source
Topographic and geologic controls on the Northeast Greenland Ice Stream
The Northeast Greenland Ice Stream (NEGIS) is an elongated feature extending ∼600 km into the interior of the Greenland Ice Sheet. Here, we investigate detailed subglacial topography along the length of the NEGIS to ascertain the characteristics of the ...
Charlotte M. Carter +7 more
doaj +1 more source
Byrd Ice Core Debris Constrains the Sediment Provenance Signature of Central West Antarctica
Provenance records from sediments deposited offshore of the West Antarctic Ice Sheet (WAIS) can help identify past major ice retreat, thus constraining ice‐sheet models projecting future sea‐level rise.
J. W. Marschalek +14 more
doaj +1 more source

