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The aim of the study is to determine the scale of differentiation and variability of ice phenomena on the lakes in the south-eastern part of the Baltic Sea catchment area. The analysis was performed based on data from the period 1961–2020 from 15 lakes located in Poland (10) and Belarus (5). The characteristics of ice phenomena were characterized, i.e.,
Rajmund Skowron, Adam Choiński
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The Baltic Ice Lake-Yoldia Sea transition
Quaternary International, 1995Abstract The Baltic Ice Lake, the Yoldia Sea, the Ancylus Lake and the Littorina Sea are the four classical stages in the postglacial evolution of the Baltic basin. The picture is complicated by what concerns the details of each of these stages. Between the Baltic Ice Lake and the Yoldia Sea it is necessary to introduce a separate lake stage; an ...
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Boreas, 1989
The deglaciation pattern at Mt. Billingen, within the Middle Swedish end moraine zone, and its relationship with dramatic water level changes in the Baltic Ice Lake is a classic topic of Swedish Quaternary Geology. Based on data west of Mt. Billingen, the authors (in two earlier papers) presented a stratigraphic model associated with this subject. This
Svante Björck, Gunnar Digerfeldt
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The deglaciation pattern at Mt. Billingen, within the Middle Swedish end moraine zone, and its relationship with dramatic water level changes in the Baltic Ice Lake is a classic topic of Swedish Quaternary Geology. Based on data west of Mt. Billingen, the authors (in two earlier papers) presented a stratigraphic model associated with this subject. This
Svante Björck, Gunnar Digerfeldt
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Boreas, 1982
Book reviewed in this article:A stratigraphic study of Late Weichselian de‐glaciation, shore displacement and vegetation history in southeastern Sweden.
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Book reviewed in this article:A stratigraphic study of Late Weichselian de‐glaciation, shore displacement and vegetation history in southeastern Sweden.
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Boreas, 2002
A clay‐varve chronology based on 14 cross‐correlated varve graphs from the Baltic Sea and a mean varve thickness curve has been constructed. This chronology is correlated with the Swedish Time Scale and covers the time span 11 530 to 10250 varve years BP.
Thomas Andrén +2 more
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A clay‐varve chronology based on 14 cross‐correlated varve graphs from the Baltic Sea and a mean varve thickness curve has been constructed. This chronology is correlated with the Swedish Time Scale and covers the time span 11 530 to 10250 varve years BP.
Thomas Andrén +2 more
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First direct age determination for the Baltic Ice Lake/Yoldia Sea transition in Finland
GFF, 2013The drainage of the Baltic Ice Lake (BIL) to the Yoldia Sea level occurred at around 11 600 years ago and can be considered as one of the most important events in the Late-Glacial Baltic Basin history. Distinctive sandy deposits were formed as a result of the water-level fall.
Kaakinen Anu +3 more
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A Baltic Ice Lake transgression in the southwestern Baltic: Evidence from Fakse Bugt, Denmark
Quaternary International, 1995Abstract Marine geological investigations including shallow seismic surveys and corings have been carried out in the shallow waters of Fakse Bugt (Bay) and Hjelm Bugt near to the island of Mon, Denmark. A combined sequence- and lithostratigraphy has been established and supplemented with biostratigraphic data and 14 C datings.
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Quaternary Research, 1998
Diatom data from the Skagerrak–Kattegat show that large amounts of meltwater were discharged into the Kattegat–Skagerrak from the Baltic Ice Lake during the Younger Dryas interval. Strong meltwater discharge greatly freshened surface-water salinity in the Kattegat and areas along the Swedish west coast and possibly changed the directions of sea-surface
Hui Jiang +2 more
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Diatom data from the Skagerrak–Kattegat show that large amounts of meltwater were discharged into the Kattegat–Skagerrak from the Baltic Ice Lake during the Younger Dryas interval. Strong meltwater discharge greatly freshened surface-water salinity in the Kattegat and areas along the Swedish west coast and possibly changed the directions of sea-surface
Hui Jiang +2 more
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Estuarine, Coastal and Shelf Science, 2017
Abstract Besides providing high resolution chronological information, varved sediments also are excellent environmental archives. We examined the grain size distribution of varved glaciolacustrine sediments as a proxy for estimation of the water depth and the duration of winter – a period with diminished sediment input from the melting glacier and ...
Andis Kalvāns, Tiit Hang, Marko Kohv
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Abstract Besides providing high resolution chronological information, varved sediments also are excellent environmental archives. We examined the grain size distribution of varved glaciolacustrine sediments as a proxy for estimation of the water depth and the duration of winter – a period with diminished sediment input from the melting glacier and ...
Andis Kalvāns, Tiit Hang, Marko Kohv
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Boreas, 1991
Mt. Kroppefjall is situated just south of the Middle Swedish (Younger Dryas) ice‐marginal zone. Its abundance of lake basins makes it very suitable for detailed shore displacement studies close to the Younger Dryas ice margin. Altogether 12 lakes at altitudes between 157 and 78 m were studied and all but one situated above the marine limit contained ...
SVANTE BJÖRCK, GUNNAR DIGERFELDT
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Mt. Kroppefjall is situated just south of the Middle Swedish (Younger Dryas) ice‐marginal zone. Its abundance of lake basins makes it very suitable for detailed shore displacement studies close to the Younger Dryas ice margin. Altogether 12 lakes at altitudes between 157 and 78 m were studied and all but one situated above the marine limit contained ...
SVANTE BJÖRCK, GUNNAR DIGERFELDT
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