Soesoo); in 2010, issue 2--'The INQUA Peribaltic Working Group Symposium' (the Weichselian
glaciation, guest editor V.
The soil is terminal morainic deposits from the Weichselian
glaciation (Nielsen and Moberg 1984) and classified as an Aric Haplic Luvisol (1USS Working Group WRB 2015) and Ultic Hapludalf (Soil Survey Staff 2014).
Hieronymus, "Stress evolution and fault instability during the Weichselian
glacial cycle," Tech.
(2000): Variability of fluvial sediment supply to the Laptev Sea continental margin during Late Weichselian
to Holocene times: implications from clay-mineral records.
Impact of bedrock surface topography on spatial distribution of Quaternary sediments and on the flow pattern of late Weichselian
glaciers on the East European Craton (Russian Plain).
Glaciofluvial sandur sediments deposited by proglacial melt water occur as wide belts in front of the ice marginal zones of the Weichselian
glaciation (Katzung & Muller 2004).
The presence of Picea abies and Larix sibirica within the interval 8500-7300 cal yr BP contributes to a growing recognition and insight that these species were regular components of the high-mountain flora within the entire extent of the Scandes, from south to north, during the early Holocene and late Weichselian
(Kullman, 2002, 2008; Paus, 2010, 2013; Oberg and Kullman, 2011b; Paus et al., 2011; Carcaillet et al., 2012).
Quaternary stratigraphic scheme of Lithuania Division Subdivision Step formation Pleistocene Upper Nemunas (Weichselian
), glacial Merkine (Eemian), interglacial Middle Medininkai (Warthe), glacial Snaigupele (Karlich), interglacial Zemaitija (Drenthe), glacial Butenai (Holsteinian), interglacial Dainava (Elsterian 2), glacial Turgeliai (Voigstedt), interglacial Dzukija (Elsterian 1), glacial Vindziunai (Bavelian), interglacial Kalviai (Nidanian), glacial Lower Daumantai complex (preglacial) Please Note: Illustration(s) are not available due to copyright restrictions.
The "Lower Loess" is from the early to middle Lower Weichselian
(MIS 5c-d), and after Semmel , a product of the first part of the glaciation (early Late Pleistocene, Figure 2), where, in this mountainous region, loess was deposited in a mammoth steppe environment.
Smaller-scale tectonic mobility was also noted in the Eemian Interglacial, Weichselian
Late Glacial and at the beginning of the Holocene.
The researchers, who evaluated geochemical and pollen analyses of lake sediments in Saxony-Anhalt, Brandenburg and Russia, determined that in Central and Eastern Europe, the slow ransition from the Eemian Interglacial to the Weichselian
Glacial was marked by a growing instability in vegetation trends with possibly at least two warming events.
Geological processes caused by the Weichselian
glaciation and the changes in continental, lacustrine and marine environments over last 14 500 years have played an important role in relief formation and sediment distribution .