Results 21 to 30 of about 2,967 (157)
Bulletin of the Geological Society of Denmark, 1987 Deglaciation sequences comprising glaciolacustrine sediments overlain by till deposited in a subaqueous environment around the Danish coast of 0resund and in central Northeast Sjrelland are grouped into five facies (a, b, c, d and e ). Facies a and facies bare clays deposited from suspension fall out in ice dammed lakes.
Houmark-Nielsen, Michael, Lagerlund, E.
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Glacial dynamics in pre-Alpine narrow valleys during the Last Glacial Maximum inferred by lowland fluvial records (northeast Italy) [PDF]
, 2018 During the Last Glacial Maximum (LGM), most of the major glaciated basins of the European Southern Alps had piedmont lobes with large outwash plains; only a few glaciers remained within the valley.
Carraro, Anna +4 more
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A Facies Approach to the Stratigraphic Analysis of Late Wisconsinan Sediments in the Portal Creek Area, Jasper National Park, Alberta [PDF]
, 1986 Glacial diamictons described and sampled during regional stratigraphie studies in Jasper National Park, Alberta, Canada, are categorized using a facies approach.
Levson, Victor, Rutter, Nathaniel W.
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Polish Polar Research, 2015 The Ebbabreen ice−cored moraine area is covered with a sediment layer of up to 2.5 m thick, which mostly consists of massive diamicton. Due to undercutting by lateral streams, debris flow processes have been induced in marginal parts of this moraine.
Pleskot Krzysztof
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Depositional dynamics in the El'gygytgyn Crater margin: implications for the 3.6 Ma old sediment archive [PDF]
Climate of the Past, 2012 The combination of permafrost history and dynamics, lake level changes and the tectonical framework is considered to play a crucial role for sediment delivery to El'gygytgyn Crater Lake, NE Russian Arctic.
G. Schwamborn +5 more
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Grain textural analysis across a range of glacial facies [PDF]
, 1999 A technique proposed by Hooke and Iverson (1995) to identify deformed subglacial sediments is reviewed and tested, based on two main objectives. First, an investigation of whether the fractal dimension can distinguish between non-deformed and deformed ...
Hart, JK, Khatwa, A, Payne, AJ
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Open Geosciences, 2020 Glacial sediments in the eastern part of the Głubczyce Plateau, at the Krowiarki site, were studied. Two units were distinguished within the sedimentary succession.
Salamon Tomasz
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Diamicton facies in the vicinity of Duhlata cave, Bosnek karst region, Southwestern Bulgaria
Review of the Bulgarian Geological Society, 2021 Karst caverns in the Upper Triassic dolostones of the Rusinovdel Formation are filled with allochthonous clastics (brecciaconglomerates with maximum boulder size) and locally with speleothems (flowstones). Deposition of the former (diamicton facies) by debris flows resulted from extreme flood events along the upper reaches of Struma river. The polymict
Athanas Chatalov, Dilyana Hristova
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International Journal of Speleology, 2017 Las Karmidas Cave (Puebla State, Mexico) is an unusual type of pseudokarstic cavity generated by piping and erosive processes within the contact of a diamicton and an overlying Quaternary ignimbrite.
María del Pilar Aliaga-Campuzano +5 more
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Quaternary Stratigraphy and History, Quesnel, British Columbia [PDF]
, 1988 Thick Quaternary sediments at Quesnel, British Columbia, provide a record of the late Quaternary history of an area near the centre of the former Cordilieran Ice Sheet.
Clague, John J.
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