09.06.2013 Views

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

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

<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.

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!