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The Little Ice Age in the Alps : its record in glacial deposits and rock glacier formation

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The Little Ice Age in the Alps : its record in glacial deposits and rock glacier formation

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dc.contributor.author Zasadni, Jerzy [USOS58307] pl
dc.date.accessioned 2019-01-08T08:27:10Z
dc.date.available 2019-01-08T08:27:10Z
dc.date.issued 2007 pl
dc.identifier.isbn 83-88549-56-1 pl
dc.identifier.isbn 978-83-88549-56-4 pl
dc.identifier.issn 0081-6434 pl
dc.identifier.uri https://ruj.uj.edu.pl/xmlui/handle/item/65070
dc.language eng pl
dc.rights Udzielam licencji. Uznanie autorstwa - Użycie niekomercyjne - Na tych samych warunkach 4.0 Międzynarodowa *
dc.rights.uri http://creativecommons.org/licenses/by-nc-sa/4.0/pl/legalcode *
dc.title The Little Ice Age in the Alps : its record in glacial deposits and rock glacier formation pl
dc.title.alternative Mała Epoka Lodowa w Alpach : jej zapis w osadach glacjalnych i formowaniu lodowców gruzowych pl
dc.type JournalArticle pl
dc.description.physical 117-137 pl
dc.description.additional Bibliogr. s. 133-136 pl
dc.identifier.weblink https://www.igipz.pan.pl/tl_files/igipz/ZGiHGiW/sgcb/sgcb_41/sgcb_41_07.pdf pl
dc.abstract.en Climatic fluctuations of glaciers of the Little Ice Age (LIA)-rank used to show comparable magnitudes during the Holocene. That is why the extent of maximal LIA moraines in the Alps attains similar position as those of the previous LIA-type Holocene advances. Consequently, the LIA moraines represent a massive and frequently multi-ridge depositional system. Certain differences in reaction to climatic changes and in moraine development result from the glacier size, percentage of debris-covered ice surfaces, and topography of alimentary areas. Such differences are particularly spectacular regarding "pure ice" and debris-covered glaciers. Another system represent rock glaciers which, however, frequently accompany regular glaciers. Some rock glaciers originated due to one-time transformation of a "glacial" glacier during its recession, while others formed owing to long-term accumulation of rock debris within glacial cirques during successive oscillations of small cirque glaciers in the Holocene, given suitable topographic and topoclimatic conditions. The relationship between the ELA and altitude of cirque bottom and/or debris supply from surrounding walls is of key importance in this case. pl
dc.subject.en Little Ice Age pl
dc.subject.en moraines pl
dc.subject.en rock glaciers pl
dc.subject.en ELA pl
dc.subject.en climatic change pl
dc.subject.en Alps pl
dc.description.volume 41 pl
dc.identifier.eissn 2199-6180 pl
dc.title.journal Studia Geomorphologica Carpatho-Balcanica pl
dc.language.container eng pl
dc.date.accession 2018-12-10 pl
dc.affiliation Wydział Biologii i Nauk o Ziemi : Instytut Nauk Geologicznych pl
dc.subtype Article pl
dc.rights.original OTHER; otwarte czasopismo; ostateczna wersja wydawcy; w momencie opublikowania; 0 pl
dc.identifier.project ROD UJ / OP pl


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Udzielam licencji. Uznanie autorstwa - Użycie niekomercyjne - Na tych samych warunkach 4.0 Międzynarodowa Except where otherwise noted, this item's license is described as Udzielam licencji. Uznanie autorstwa - Użycie niekomercyjne - Na tych samych warunkach 4.0 Międzynarodowa