Results 81 to 90 of about 2,982 (205)
The conditions under which ice fractures and calves icebergs from Antarctic ice shelves are poorly understood due largely to a lack of relevant observations. Though previous studies have estimated the stresses at which ice fractures in the laboratory and
Sarah Wells-Moran +2 more
doaj +1 more source
Automated detection of basal icequakes and discrimination from surface crevassing
Icequakes at or near the bed of a glacier have the potential to allow us to investigate the interaction of ice with the underlying till or bedrock. Understanding this interaction is important for studying basal sliding of glaciers and ice streams, a ...
Thomas S. Hudson +3 more
doaj +1 more source
The aim of this paper is to characterise the internal structures and ice-flow history of representative valley glaciers in Svalbard and infer from them dynamic changes over centennial timescales.
Stephen J.A. Jennings +5 more
doaj +1 more source
Seasonal lake Gornersee forms at the confluence of Gornergletscher and Grenzgletscher, Switzerland, and experiences outburst floods annually in midsummer.
Louis Garcia +3 more
doaj +1 more source
Fourth District Map Showing Crevasses and Area Overflow Flood of 1893
Fourth District Map Showing Crevasses and Area Overflow Flood of 1893 Mississippi River Commission drawn by B.J. Olivera. 20.5 x 16.
core +1 more source
Assessment of landslide hazards often depends on the ability to track possible changes in natural slopes. To that end, historical air photos can be useful, particularly when slope stability is compromised by visible cracking.
Yaniv Darvasi +5 more
doaj +1 more source
Abstract. Crevasse depth calculations with the zero stress approximation or linear elastic fracture mechanics are used in many applications, including calving laws, determination of stable cliff heights, shelf vulnerability to collapse via hydrofracture, and damage evolution in ice.
Benjamin Reynolds +2 more
openaire +1 more source
Vertical Extension of the Subglacial Drainage System into Basal Crevasses
Water plays a first-order role in basal sliding of glaciers and ice sheets and is often a key constituent of accelerated glacier motion1, 2, 3, 4. Subglacial water is known to occupy systems of cavities and conduits at the interface between ice and the ...
Joel T. Harper +7 more
core +1 more source
Crevasses on the Priestley Glacier
This record was harvested from a previous catalogue system and will be withdrawn in 2025. Information in this record may be superseded or incomplete.
University Of Melbourne. Department Of Geology
core
Progression of the surge in the Negribreen Glacier System from two years of ICESat-2 measurements
The state-of-the-art measurement capabilities of ICESat-2 allow high spatiotemporal resolution of complex ice-dynamic processes that occur during a surge.
Thomas Trantow, Ute Christina Herzfeld
doaj +1 more source

