Historia zlodowacenia archipelagu Svalbard od późnego vistulianu do współczesności

Joanna Ćwiąkała, Mateusz Moskalik, Jan Rodzik, Piotr Zagórski

Streszczenie w języku polskim


Svalbard jest obszarem, gdzie zachowały się w różnym stopniu „ślady” zdarzeń glacjalnych. Dowodami ich wystąpienia są między innymi osady oraz formy glacjalne i fluwioglacjalne (np. Boulton 1979; Boulton i in. 1982; Landvik i in. 1998; Mangerud i in. 1998; Pękala, Repelewska-Pękalowa 1990; Lindner, Marks 1993ab; Ingólfsson, Landvik 2013). Bliskość tego obszaru w stosunku do centrów zlodowaceń powodowała, że kolejne epizody glacjalne „zamazywały ślady” poprzednich, niszcząc je lub przekształcając (np. Landvik i in. 1992; Mangerud i in. 1998; Zagórski 2007). Po deglacjacji następował zazwyczaj okres intensyfikacji działania procesów nieglacjalnych (paraglacjalnych), np. morskich, peryglacjalnych (Mercier, Laffly 2005; Strzelecki 2011; Zagórski i in. 2012). Stąd najlepiej zachowały się pozostałości najmłodszych zdarzeń i epizodów glacjalnych, np. małej epoki lodowej (np. Baranowski 1977abc; Lindner Marks 1993b; Werner 1993; Wójcik, Ziaja 1999; Reder 1996ab;  Birkenmajer, Łuczkowska 1997; Svendsen Mangerud 1997; Zagórski i in. 2008, 2012; Rodzik i in. 2013).

Słowa kluczowe


stratygrafia późnego vistulianu i holocenu, zlodowacenia Svalbardu

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Bibliografia


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DOI: http://dx.doi.org/10.17951/b.2014.69.2.27
Data publikacji: 2015-05-25 18:43:09
Data złożenia artykułu: 2015-05-24 18:01:29

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Prawa autorskie (c) 2015 Joanna Ćwiąkała, Mateusz Moskalik, Jan Rodzik, Piotr Zagórski

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