Wszystkie pola: kames - Katalog OPAC zbiorów

Skocz do pozycji: 1.

Tytuł:: Eemian Interglacial deposits at Haćki near Bielsk Podlaski: implications for the limit of the last glaciation in northeastern Poland
Autorzy:: Brud, S.
Kupryjanowicz, M.
Powiązania:: https://bibliotekanauki.pl/articles/2059922.pdf
Data publikacji:: 2002
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: NE Poland
Wartanian glaciation
Eemian Interglacial
Vistulian
kames
pollen analysis
Opis:: Pollen analysis was conducted on organic deposits on a kame ridge at Haćki in northeastern Poland. The deposits are referred to the Eemian Interglacial. Slope sediments only covered these biogenic deposits. The glacigenic landforms therefore relate to the Wartanian Glaciation, and so this area has not been occupied by an ice sheet of the Vistulian Glaciation.
Źródło:: Geological Quarterly; 2002, 46, 1; 75-80
1641-7291
Pojawia się w:: Geological Quarterly
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 2.

Tytuł:: Osady deglacjacyjne zlodowacenia Warty we wschodniej części regionu łódzkiego
Sediments of the Warta ice-sheet deglaciation in the eastern part of the Łódź region.
Autorzy:: Rdzany, Z.
Powiązania:: https://bibliotekanauki.pl/articles/2074439.pdf
Data publikacji:: 2006
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: lądolód warty
analiza facjalna
osad glacjalny
proces deglacjacji
Warta glaciation
Łódź Region
facial analysis
palaeogeographic reconstruction
areal deglaciation, kames
Opis:: The author attempts at formulating a synthetic description of geological and geomorphological effects of theWartanian ice-sheet deglaciation in the eastern part of the Łódź region, taking their spatial variability into consideration. Characteristic features of Wartanian Glaciation sediments occur in this area, and their lithofacial diversity and spatial distribution needed interpretation. The deposits document the complex processes of deglaciation, which developed here across an unusually broad area in the scale of the Polish Lowland. The best developed deglaciation sediments occur in the eastern part of the Łódź Heights, between the Mroga and Rawka rivers, as structural components of different types of kames and glaciofluvial covers. In locations where glacial till is elevated they include mainly sediments of braided rivers and alluvial cones, whereas in areas of wide depressions of till and, thus, of the ice-sheet bedrock — glaciolimnic sediments prevail. The highest and most diverse western part of the Łódź Heights is characterised by the occurrence of thin and discontinuous deglaciation sediments, because this area was shaped mainly during the ice-sheet transgression. During deglaciation, ablation waters left mainly traces of erosion, whereas the glaciofluvial accumulation series are not well developed. In the Rawa Interfluve, deglaciation sediments accumulated predominantly at the early deglaciation stage in sparesely distributed broad basins of kame sedimentation. In the Piotrków Plain, deglaciation deposits are thin; ice-sheet disintegration proceeded without major blockages of ablation waters, resulting in a less diverse interfluvial landscape.
Źródło:: Przegląd Geologiczny; 2006, 54, 4; 343-351
0033-2151
Pojawia się w:: Przegląd Geologiczny
Dostawca treści:: Biblioteka Nauki

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