Search results for "subglacial deformation"

showing 4 items of 4 documents

STOP 14: Morphology and internal structure of the Lāči drumlin at Tērvete village, Zemgale Drumlin Field

2014

geographygeography.geographical_feature_categoryDrumliniDrumlin:NATURAL SCIENCES::Earth sciences::Exogenous earth sciences::Sedimentology [Research Subject Categories]Morphology (biology):NATURAL SCIENCES::Earth sciences::Exogenous earth sciences::Quaternary geology [Research Subject Categories]Field (geography)Kvartāra ģeoloģijasubglacial deformationWeichselian glaciationGeomorphologyWeichselian glaciationtill macrofabricLate Quaternary Terrestrial Processes, Sediments and History: From Glacial to Postglacial Environments
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STOP 15: Morphology and internal structure of a ribbed moraine and drumlin remnant in the environs of Baldone, Central Latvian Lowland

2014

geographyCentrāllatvijas zemienegeography.geographical_feature_categoryDrumlin:NATURAL SCIENCES::Earth sciences::Exogenous earth sciences::Sedimentology [Research Subject Categories]LatvianMorphology (biology):NATURAL SCIENCES::Earth sciences::Exogenous earth sciences::Quaternary geology [Research Subject Categories]language.human_languagePaleontologyMoraineKvartāra ģeoloģijasubglacial deformationlanguageWeichselian glaciationGeomorphologyWeichselian glaciationtill macrofabricGeologyLate Quaternary Terrestrial Processes, Sediments and History: From Glacial to Postglacial Environments
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Fluid-pressure controlled soft-bed deformation sequence beneath the surging Breiðamerkurjökull (Iceland, Little Ice Age).

2009

16 pages; International audience; The general subject of this paper is subglacial deformation beneath Breiðamerkurjökull, a surging Icelandic glacier. More specifically it discusses the evolution and the role of fluid pressure on the behaviour of subglacial sediments during deformation. During Little Ice Age maximum, the two outcrops studied, North Jökulsarlon (N-Jk) and Brennhola-Alda (BA), were located at 2550 m and 550 m respectively from the front of the Breiðamerkurjökull. Sedimentological analysis at the forefield of the glacier shows thick, coarse glaciofluvial deposits interbedded with thin, fine-grained shallow lacustrine/swamp deposits, overlain by a deformed till unit at N-Jk. BA…

geographygeography.geographical_feature_categoryFluid pressureOutcropStratigraphyBreiðamerkurjökullIceland[ SDU.STU.GL ] Sciences of the Universe [physics]/Earth Sciences/GlaciologySedimentGeologyGlacier[ SDU.STU.TE ] Sciences of the Universe [physics]/Earth Sciences/TectonicsDeformation (meteorology)[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/StratigraphyClast-fabric analysisSimple shear[ SDE.MCG ] Environmental Sciences/Global ChangesClastic rockSubglacial eruptionSedimentary rockPetrologyGeomorphologyGeologySubglacial deformation
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Two-dimensional apparent microfabric of the basal Late Weichselian till and associated shear zone: case study from western Latvia

2008

The examination of glacial sediments in thin sections has become a common procedure in recent years. Apparent sand grain orientation (microfabric) in thin sections is one of the key elements marking certain microstructures. In an attempt to make till micromorphology studies less subjective and investigate the orientation of sand-sized particles in tills, we have developed an image analysis procedure to measure and analyse the spatial distribution of the till microfabric. We studied 13 thin sections of the Weichselian subglacial till and basal shear zone outcropping in the Baltic Sea bluffs at the Ziemupe site in western Latvia. The results were visualized as a two-dimensional grid of rose d…

OutcropThin sectionlcsh:QE1-996.5shear zonemicromorphologySpatial distributionlcsh:GeologyPaleontologyBaltic seaGlacial sedimentsimage analysistillsubglacial deformationGeneral Earth and Planetary SciencesmicrofabricShear zoneGeomorphologythin sectionsGrain orientationGeologyWater Science and TechnologyEstonian Journal of Earth Sciences
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