Lyell Collection

Geological Society, London, Special Publications

Lyell Centre  |   Lyell Collection  |   Subscriptions   |   Geological Society  |   Email alerts  |   Online bookshop  |   Help


Keywords:
Author:
Advanced search>>
This Article
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow Request Permissions
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Gaigalas, A.
Right arrow Articles by Urban, H.
Right arrow Search for Related Content
Geological Society, London, Special Publications; 2008; v. 301; p. 141-147;
DOI: 10.1144/SP301.9
© 2008 Geological Society of London

Articles

Ceslovas Pakuckas (or Czeslaw Pachucki): pioneer of modern glaciomorphology in Lithuania and Poland

Algirdas Gaigalas1, Marek Graniczny2, Jonas Satkunas3 & Halina Urban2

1 Department of Geology and Mineralogy, Vilnius University, Vilnius, Lithuania (e-mail: Algirdas.Gaigalas{at}gf.vu.lt)
2 Polish Geological Institute, Warsaw, Poland
3 Geological Survey of Lithuania, Vilnius, Lithuania

The contributions of the Lithuanian geologist Ceslovas Pakuckas (1898–1956) (in Poland – Czeslaw Pachucki) to Pleistocene geology are of major significance, and he is regarded as the pioneer of modern glaciomorphological investigations of the Baltic marginal highlands in Lithuania and Poland. Pakuckas published his first paper on the glacial morphology of south Lithuania in 1934, followed in 1936 with one on the orientation marginal moraines in the east Lithuanian highlands and their origin, and in 1938 with another on the glacial morphology of south Lithuania. His ideas on glacial morphology were presented at the First Conference of Lithuanian and Latvian geologists held in Kaunas in 1940. Working in Poland after World War II, Pakuckas continued his glaciomorphological research and compiled data on the correlation of end moraines of NE Poland and south Lithuania with those in west Belarus as well as the Peribalticum. He concluded that during the Last Glaciation, the continental glacier was not a single ice sheet but consisted of a number of flows, each dependent on topography and each with its specific glacial centre. In Lithuania, Pakuckas defined one large field of lateral moraines, the so-called Baltic Highland consisting of the Suduva, Dzukija and Aukstaitija highlands. He traced this formation SW as the Mazurian arc of lateral moraines (in NE Poland) and found that the Svencionys–Naroch or north Belarus field of lateral moraines extend to the NE of the Baltic Highland.