Search results for "Crevasse"

showing 2 items of 2 documents

The thermal structure, subglacial topography and surface structures of the NE outlet of Eyjabakkajökull, east Iceland

2020

Abstract This study presents the detailed surveys of the NE outlet of Eyjabakkajokull glacier, East Iceland, from the combination of low-frequency ground penetrating radar (GPR), unmanned aerial vehicle (UAV) and GNSS measurements. Data analyses reveal the complex subglacial topography with a prominent, up to 45-m-deep longitudinal trough in the central part of the outlet that serves as the main trunk for the fast ice flow during the glacier surges. During the last decade (2010–2018), the studied part of the glacier has thinned by 4.37 m/yr on average and the ice margin has retreated ~750 m. We detect a boundary between scatter-free zone and zone of intense scattering near the ice margin an…

0106 biological sciencesgeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesEcology010604 marine biology & hydrobiologyCrevassesFlow (psychology)Trough (geology)Piezometric surfaceGlacierUnmanned aerial vehicleAquatic Science01 natural sciencesGround penetrating radarFast iceThermalGround-penetrating radarGeneral Earth and Planetary SciencesDrainage networkTemperate iceGeomorphologyEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesPolar Science
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Two-dimensional numerical modeling of fracturing and shear band development in glacier fronts

2014

In this contribution we present a two-dimensional numerical model of a deforming glacier front. The model is based on a hybrid lattice spring network approach where particles in the model can deform in a volume conservative visco-elastic manner but at the same time they can be compressed elastically and fracture by discrete failure. We restrict ourselves to a simple setting where the glacier sits on a frictionless slope that dips with 5–10°, the ice block is fixed on one side and has a free surface on the other. The glacier varies in viscosity and can flow at the base, whereas it is brittle at the top. Results show that the head of the glacier is unstable. Failure happens as a combination o…

Glacier ice accumulationPluckinggeographyCrevassegeography.geographical_feature_categoryShear (geology)IcefallIce streamAccumulation zoneGeologyGlacierGeomorphologyGeologyJournal of Structural Geology
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