Results 21 to 30 of about 708,716 (215)

A thermomechanical model for frost heave and subglacial frozen fringe [PDF]

open access: yesJournal of Fluid Mechanics, 2021
Ice-infiltrated sediment, or frozen fringe, is responsible for phenomena such as frost heave, ice lenses and metres of debris-rich ice under glaciers. Understanding frozen fringes is important as frost heave is responsible for damaging infrastructure at ...
C. Meyer, C. Schoof, A. Rempel
semanticscholar   +1 more source

Assessing the Environmental Consequences of the Generation and Alteration of Mafic Volcaniclastic Deposits During Large Igneous Province Emplacement

open access: yesGeophysical Monograph Series, Page 117-131., 2021

Exploring the links between Large Igneous Provinces and dramatic environmental impact

An emerging consensus suggests that Large Igneous Provinces (LIPs) and Silicic LIPs (SLIPs) are a significant driver of dramatic global environmental and biological changes, including mass extinctions.
Benjamin Black   +4 more
wiley  

+1 more source

Debris-bed friction during glacier sliding with ice–bed separation

open access: yesAnnals of Glaciology, 2019
Theory and experiments indicate that ice–bed separation during glacier slip over 2-D hard beds causes basal shear stress to reach a maximum at a particular slip velocity and decrease at higher velocities.
Neal R. Iverson   +2 more
doaj   +1 more source

Subglacial landforms beneath Rutford Ice Stream, Antarctica: detailed bed topography from ice-penetrating radar [PDF]

open access: yesEarth System Science Data, 2016
We present a digital elevation model of the bed of Rutford Ice Stream, Antarctica, derived from radio-echo sounding data. The data cover an 18  ×  40 km area immediately upstream of the grounding line of the ice stream.
E. C. King, H. D. Pritchard, A. M. Smith
doaj   +1 more source

Prospects of obtaining samples of bottom sediments from subglacial lake Vostok

open access: yesЗаписки Горного института, 2017
The paper proves the timeliness of obtaining and examining bottom sediments from subglacial Lake Vostok. Predictive geological section of Lake Vostok and information value of bottom sediments have been examined.
N. I. Vasil'ev   +2 more
doaj   +1 more source

The life and death of a subglacial lake in West Antarctica

open access: yesGeology, 2023
Over the past 50 years, the discovery and initial investigation of subglacial lakes in Antarctica have highlighted the paleoglaciological information that may be recorded in sediments at their beds.
M. Siegfried   +22 more
semanticscholar   +1 more source

Prokaryotic assemblages in suspended and subglacial sediments within a glacierized catchment on Qeqertarsuaq (Disko Island), west Greenland

open access: yesFEMS Microbiology Ecology, 2018
Microbes transported by glacial meltwater streams are thought to be a product of passive dispersal from both supra‐ and subglacial sources, though studies investigating the origins of these assemblages are scarce.
J. Žárský   +7 more
semanticscholar   +1 more source

Bed-type variability and till (dis)continuity beneath Thwaites Glacier, West Antarctica

open access: yesAnnals of Glaciology, 2019
Recent seismic measurements from upper Thwaites Glacier indicate that the bed-type variability is closely related to the along-flow basal topography. In high-relief subglacial highlands, stoss sides of topographic highs have a relatively higher acoustic ...
Atsuhiro Muto   +3 more
doaj   +1 more source

Water blister geomorphology and subglacial drainage sediments: an example from the bed of the Fennoscandian Ice Sheet in SW Finland

open access: yesJournal of Glaciology, 2023
This study presents the first light detection and ranging (LiDAR)-based morphometric description of a water blister from a past ice-sheet bed caused by rapid supraglacial drainage.
Joni Mäkinen   +6 more
doaj   +1 more source

Effects of basal topography and ice-sheet surface slope in a subglacial glaciofluvial deposition model

open access: yesJournal of Glaciology, 2023
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

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