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Geological Survey of Finland, Special Paper 46 - arkisto.gsf.fi

Geological Survey of Finland, Special Paper 46 - arkisto.gsf.fi

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The thin (up to 30-40 m) Pleistocene bed in the<br />

North Lithuanian region is subdivided into three<br />

lithostratigraphic complexes. These are: the lower<br />

glacial complex <strong>of</strong> the Middle Pleistocene (Medininkai<br />

sub-formation) or Upper Pleistocene (Lower<br />

Nemunas sub-formation), the overlying intertill<br />

sediments aged 86-81 thousand years and the upper<br />

till complex <strong>of</strong> the Baltic Stage <strong>of</strong> the last Ice Age.<br />

The lower (older) glacial complex in the pre-<br />

Quaternary declensions was formed in the interface<br />

between a glacier advancing from the north and a<br />

The authors are thankful to Dr. A. Molodkov, Head<br />

<strong>of</strong> the Laboratory <strong>of</strong> Quaternary Research, Institute<br />

<strong>of</strong> Geology <strong>of</strong> Tallinn Technical University, and<br />

palynologist A. Grigien from the Lithuanian Geo-<br />

Baltr0nas, V., Karmaza, B. & Karmazien, D. 2005. Pleistoceno<br />

nuogul< sandaros ir formavimosi ypatybs Šiaurs<br />

Lietuvoje. Geologija 52, 22–33. (in Lithuanian with English<br />

and Russian summary)<br />

Bucevic v<br />

i0t, S., Dobkevic v<br />

ius, M. & Marcinkevic v<br />

ius, V. 1992.<br />

Rajono geologins ir hidrogeologins s_lygos. Karstinio<br />

rajono gamtin ir technogenin situacija. Geologija 13, 30–<br />

49. (in Lithuanian with English and Russian summary)<br />

Gaigalas, A. 1971. Texture, structure and the genetic varieties<br />

<strong>of</strong> the ground-moraines (in Russian). In: Gudelis, V.<br />

& Gaigalas, A. (eds.) Structure and morphogenesis <strong>of</strong> the<br />

Middle Lithuanian morainic plain. Mintis, 28–87.<br />

<strong>Geological</strong> <strong>Survey</strong> <strong>of</strong> <strong>Finland</strong>, <strong>Special</strong> <strong>Paper</strong> <strong>46</strong><br />

Structural characteristics <strong>of</strong> Pleistocene deposits in North Lithuania<br />

CONCLUSIONS<br />

ACKNOWLEDGEMENTS<br />

REFERENCES<br />

pre-Quaternary surface inclined to the north and the<br />

east.<br />

The Upper Pleistocene glacial complex <strong>of</strong> the<br />

Baltic Stage <strong>of</strong> the last Ice Age is composed <strong>of</strong><br />

strata accumulated during two recessions <strong>of</strong> the glacier<br />

that advanced from the north. The strata differ<br />

from the older tills in a lower content <strong>of</strong> imported<br />

clastic material and a higher content <strong>of</strong> local excavated<br />

material. The strata differ among themselves<br />

in granulometric composition and sorting.<br />

logical <strong>Survey</strong> for assistance in analysing the sections<br />

<strong>of</strong> the North Lithuanian Pleistocene deposits<br />

and summarizing the research data.<br />

Lietuvos kvartero stratigra<strong>fi</strong> jos schema. 1994. Valstybini<<br />

geologini tyrim< taisykls ir metodins rekomendacijos.<br />

Lietuvos geologijos tarnyba. 17 p. (in Lithuanian)<br />

Satk0nas, J. 1999. The Upper Pleistocene stratigraphy and<br />

geochronology in Lithuania. Litosfera 3, 43–57.<br />

Šliaupa, A. 1997. The sub-Quaternary reljef <strong>of</strong> Lithuania and<br />

<strong>of</strong> adjacent territories. Litosfera 1, <strong>46</strong>–57.<br />

Šliaupa, A. 2004. Prekvartero uolien< paviršius. Lietuvos<br />

˘ems gelmi< raida ir ištekliai (ats. red. Baltr0nas, V.).<br />

˘urnalo “Litosfera” leidinys, 254–260. (in Lithuanian with<br />

English summary)<br />

37

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