Results 131 to 140 of about 1,074 (174)
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Ice recession and depositional environment in the Blekinge archipelago of the Baltic Ice Lake
GFF, 1994The Swedish varved clays, deposited in the former Baltic Ice Lake during the deglaciation, constitute an excellent tool to decipher the ice recession with annual precision. New clay varve diagrams from Blekinge, southern Sweden, enable to place the deglaciation of sites situated in northern Blekinge between the local varve years ‐39 to +77, which ...
Wohlfarth, Barbara +4 more
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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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Palaeoreconstruction of the Baltic Ice Lake in the Eastern Baltic
2011A GIS-based palaeogeographic reconstruction of the development of the Baltic Ice Lake (BIL) in the eastern Baltic during the deglaciation of the Scandinavian Ice Sheet is presented. A Late Glacial shoreline database containing sites from Finland, NW Russia, Estonia, Latvia and modern digital terrain models was used for palaeoreconstructions.
Jüri Vassiljev +2 more
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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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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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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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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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Reconstructing the Younger Dryas ice dammed lake in the Baltic Basin: Bathymetry, area and volume
Global and Planetary Change, 2007A digital 3D-reconstruction of the Baltic Ice Lake’s (BIL) configuration during the termination of the Younger Dryas cold phase (ca. 11700 cal.
Martin Jakobsson +5 more
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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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Quaternary Science Reviews, 2018
Abstract The rapid retreat of the Baltic Ice Stream and the development of the Baltic Ice Lake is assessed using data from sediment cores retrieved from three sub-basins in the southern Baltic Sea. Hydraulic piston coring by the International Ocean Discovery Program (IODP) recovered for the first time intact glacial lake sequences overlying ...
April L. Kelly, Sandra Passchier
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Abstract The rapid retreat of the Baltic Ice Stream and the development of the Baltic Ice Lake is assessed using data from sediment cores retrieved from three sub-basins in the southern Baltic Sea. Hydraulic piston coring by the International Ocean Discovery Program (IODP) recovered for the first time intact glacial lake sequences overlying ...
April L. Kelly, Sandra Passchier
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