Geological Survey of Finland, Special Paper 46 - arkisto.gsf.fi
Geological Survey of Finland, Special Paper 46 - arkisto.gsf.fi
Geological Survey of Finland, Special Paper 46 - arkisto.gsf.fi
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<strong>Geological</strong> <strong>Survey</strong> <strong>of</strong> <strong>Finland</strong>, <strong>Special</strong> <strong>Paper</strong> <strong>46</strong><br />
Valentinas Baltrünas, K´stutis Švedas and Violeta Pukelyt<br />
Many publications have been dedicated to issues <strong>of</strong><br />
the Late Pleistocene palaeogeography in Lithuania.<br />
Some <strong>of</strong> them are theoretical in nature and are con<strong>fi</strong><br />
ned to general and schematic palaeogeographical<br />
characteristics <strong>of</strong> the region. The publications served<br />
both as a theoretical and methodological basis for<br />
more recent investigations (Basalykas 1965, Dvareckas<br />
1993). Some other studies were more speci<strong>fi</strong> c<br />
with a special method used for analyzing diverse<br />
geologic and geomorphologic objects and with fundamental<br />
conclusions substantially contributing to<br />
the knowledge <strong>of</strong> the history <strong>of</strong> palaeogeographic<br />
conditions <strong>of</strong> the time (Basalykas et al. 1984, Dvareckas<br />
& Diceviπien 1987, Kabailien 1990, Kon-<br />
40<br />
INTRODUCTION<br />
dratien 1996, Komarovsky 1996, Satk0nas 1999,<br />
Gaigalas 2001, Švedas 2001, Švedas et al. 2004).<br />
Furthermore, it should be recognized that a composite<br />
evaluation and more accurate cartographic depiction<br />
<strong>of</strong> the palaeogeographical conditions were<br />
not fully realized, and the correlation <strong>of</strong> Pleistocene<br />
stratigraphical events in Lithuania was not associated<br />
with changes in the periglacial conditions.<br />
The purpose <strong>of</strong> this article is to summarise previous<br />
investigations on the geology and palaeogeography<br />
<strong>of</strong> the last glaciation and soil permafrost<br />
structures in periglacial areas in southern Lithuania<br />
to obtain a comprehensive model <strong>of</strong> the evolution <strong>of</strong><br />
the area (Fig. 1).<br />
Fig. 1a) Location map <strong>of</strong> the studied area, b) Deglaciation <strong>of</strong> the Last (Weichselian, Nemunas) Glaciation in the<br />
South Lithuania (after Gaigalas (2001)): G – Gr0da (Brandenburg) stage, ˘ – ˘iogeliai (Frankfurt) phase, B (EL)<br />
– Baltija (Pomeranian) stage (East-Lithuanian phase), SL – South-Lithuanian phase, ML – Middle-Lithuanian<br />
phase, NL – North-Lithuanian phase; c) Geomorphological regions (compiled according to Atlas <strong>of</strong> Lithuania<br />
(Drobnys 1981): 1 – Middle Nemunas Plateau, 2 – South Lithuania Upland, 3 – Dainava Plain, 4 – Eišišks<br />
Plateau, 5 – Medininkai Upland.