Zobrazeno 1 - 10
of 15
pro vyhledávání: '"Zbigniew Rdzany"'
Autor:
Małgorzata Frydrych, Zbigniew Rdzany
Publikováno v:
Acta Geobalcanica, Vol 2, Iss 2, Pp 77-84 (2016)
Tunnel valleys are among the largest erosional structures in the Pleistocene cover of the Polish Lowland and other areas around the Baltic Sea. They have been fairly well recognised within the extent of the Weichselian (Vistulian) Glaciation. Researc
Externí odkaz:
https://doaj.org/article/91d57852c78d4ebb8510ec57751350a5
Autor:
Zbigniew Rdzany, Małgorzata Frydrych
Publikováno v:
Quaternary International. 617:21-39
In this study, a glacial lake-outburst flood was documented in the immediate foreland of the maximum phase of the Wartanian (Warthian, Late Saalian, MIS 6) Glaciation at Adamow in south central Poland. The structural and textural analyses of the sedi
Publikováno v:
Przegląd Geologiczny. 68:584-600
Autor:
Zbigniew Rdzany
Publikováno v:
Acta Geographica Lodziensia. 112
Autor:
Zbigniew Rdzany
Publikováno v:
Acta Universitatis Lodziensis. Folia Geographica Physica. :79-90
Autor:
Małgorzata Frydrych, Zbigniew Rdzany
Publikováno v:
Sedimentary Geology. 374:85-97
The aim of the research conducted in an outcrop of late Saalian sediments in Siedlątkow (Central Poland) was to reconstruct extreme meltwater flows during a jokulhlaup on the basis of the geological record. A combination of field and laboratory lith
Autor:
Małgorzata Frydrych, Zbigniew Rdzany
Publikováno v:
ACTA UNIVERSITATIS LODZIENSIS. FOLIA GEOGRAPHICA PHYSICA. :33-40
In international literature, much attention has been paid to sedimentological and geomorphological evidence of extreme floods in the forelands of both contemporary and Pleistocene glaciers and ice sheets. Reports on this subject come from areas and p
Autor:
Zbigniew Rdzany, Małgorzata Frydrych
Publikováno v:
Acta Geobalcanica. 2:77-84
Autor:
Zbigniew Rdzany
Publikováno v:
Bulletin of Geography. Physical Geography Series. 8:33-45
The article comprises a justification for the need to distinguish the record of the paraglacial environments in the belt of relief formed as a result of the Warta Glaciation in Poland. The zone covers the foreland of the Weichselian Glaciation, occup