Results 41 to 50 of about 2,018 (207)
We use a mathematical model to investigate the effect of basal topography and ice surface slope on transport and deposition of sediment within a water-filled subglacial channel. In our model, three zones of different behaviour occur. In the zone furthest
David Stevens +5 more
doaj +1 more source
Subglacial sediment deformation in the Ross Sea, Antarctica
Abstract:: The Ross Sea embayment is the outlet for one-third of all Antarctic ice flow, receiving input from both East and West Antarctica. Marine-based ice streams, whose stability is susceptible to global sea-level changes, expand and contract across the Ross Sea continental shelf, eroding and deforming the substrate and transporting sediment ...
Delaney E. Robinson +3 more
openaire +2 more sources
Surface-wave analysis for identifying unfrozen zones in subglacial sediments [PDF]
To reveal the extent of freezing in subglacial sediments, we estimated S-wave velocity along a glacier using surface-wave analysis. Because the S-wave velocity varies significantly with the degree of freezing of the pore fluid in the sediments, this ...
Toshifumi Matsuoka +8 more
core +1 more source
Stable isotopes of water (δ18O and δ2H) were measured in the debris-laden ice underlying an Antarctic blue ice moraine, and in adjoining Law Glacier in the central Transantarctic Mountains.
JOSEPH A. GRALY +4 more
doaj +1 more source
Viable cold-tolerant iron-reducing microorganisms in geographically diverse subglacial environments [PDF]
Subglacial environments are known to harbour metabolically diverse microbial communities. These microbial communities drive chemical weathering of underlying bedrock and influence the geochemistry of glacial meltwater.
S. L. Nixon +3 more
doaj +1 more source
Reconstruction of ice-sheet changes in the Antarctic Peninsula since the Last Glacial Maximum [PDF]
This paper compiles and reviews marine and terrestrial data constraining the dimensions and configuration of the Antarctic Peninsula Ice Sheet (APIS) from the Last Glacial Maximum (LGM) through deglaciation to the present day.
Glasser, N.F. +66 more
core +1 more source
ANTASed – An Updated Sediment Model for Antarctica
We compile existing seismic, gravity, radar and magnetic data, together with the subglacial bedrock relief from the BEDMACHINE project, to build the most detailed sediment model for Antarctica.
A. Baranov, A. Morelli, A. Chuvaev
doaj +1 more source
Fast ice flow is associated with the deformation of subglacial sediment. Seismic shear velocities, Vs, increase with the rigidity of material and hence can be used to distinguish soft sediment from hard bedrock substrates.
Siobhan F. Killingbeck +5 more
doaj +1 more source
Sediment behavior controls equilibrium width of subglacial channels
Flow-frictional resistance at the base of glaciers and ice sheets is strongly linked to subglacial water pressure. Understanding the physical mechanisms that govern meltwater fluxes in subglacial channels is hence critical for constraining variations in ...
ANDERS DAMSGAARD +5 more
doaj +1 more source
Advances in understanding subglacial meltwater drainage from past ice sheets
Meltwater drainage beneath ice sheets is a fundamental consideration for understanding ice–bed conditions and bed-modulated ice flow, with potential impacts on terminus behavior and ice-shelf mass balance.
Lauren M. Simkins +4 more
doaj +1 more source

