Results 161 to 170 of about 1,423,161 (175)
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Quaternary International, 1995
Abstract This paper is the first attempt to summarize the results of diatom analyses from sediments of Late Glacial and Preboreal age in the central, south-eastern and eastern Baltic. The Baltic Ice Lake deposits are poor in diatoms and amongst those present planktonic freshwater species dominate.
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Abstract This paper is the first attempt to summarize the results of diatom analyses from sediments of Late Glacial and Preboreal age in the central, south-eastern and eastern Baltic. The Baltic Ice Lake deposits are poor in diatoms and amongst those present planktonic freshwater species dominate.
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2014 IEEE/OES Baltic International Symposium (BALTIC), 2014
Thy work aims to development of a simple method for distinction between open water and ice cover on the base of geophysical data record (GDR) of altimetry satellite Jason-2 for large and middle-sized freshwater inland water bodies. The method is applied to the lakes of Baltic and White Seas basins: Ladoga, Onega, Vygozero and Segosero.
null Rybushkina +2 more
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Thy work aims to development of a simple method for distinction between open water and ice cover on the base of geophysical data record (GDR) of altimetry satellite Jason-2 for large and middle-sized freshwater inland water bodies. The method is applied to the lakes of Baltic and White Seas basins: Ladoga, Onega, Vygozero and Segosero.
null Rybushkina +2 more
exaly +2 more sources
Geologiska Föreningen i Stockholm Förhandlingar, 1977
Abstract Short-distance varve correlations across the Sodertorn area have extended the continuous Swedish Time Scale back to about varve -1500 (about 10,400 B.P.). Varve -1073 (= 9,965 varves B.P.) is represented by a distinct drainage varve and a change from diatact to symict varves, recording the “drainage” of the Baltic Ice Lake at Billingen and the
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Abstract Short-distance varve correlations across the Sodertorn area have extended the continuous Swedish Time Scale back to about varve -1500 (about 10,400 B.P.). Varve -1073 (= 9,965 varves B.P.) is represented by a distinct drainage varve and a change from diatact to symict varves, recording the “drainage” of the Baltic Ice Lake at Billingen and the
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Palaeogeographic reconstruction of the Baltic Ice Lake in the eastern Baltic
Quaternary International, 2012openaire +1 more source