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

2007
journal article
article
dc.abstract.enClimatic 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.affiliationWydział Biologii i Nauk o Ziemi : Instytut Nauk Geologicznychpl
dc.contributor.authorZasadni, Jerzy - 142902 pl
dc.date.accession2018-12-10pl
dc.date.accessioned2019-01-08T08:27:10Z
dc.date.available2019-01-08T08:27:10Z
dc.date.issued2007pl
dc.date.openaccess0
dc.description.accesstimew momencie opublikowania
dc.description.additionalBibliogr. s. 133-136pl
dc.description.physical117-137pl
dc.description.versionostateczna wersja wydawcy
dc.description.volume41pl
dc.identifier.eissn2199-6180pl
dc.identifier.isbn83-88549-56-1pl
dc.identifier.isbn978-83-88549-56-4pl
dc.identifier.issn0081-6434pl
dc.identifier.projectROD UJ / OPpl
dc.identifier.urihttps://ruj.uj.edu.pl/xmlui/handle/item/65070
dc.identifier.weblinkhttps://www.igipz.pan.pl/tl_files/igipz/ZGiHGiW/sgcb/sgcb_41/sgcb_41_07.pdfpl
dc.languageengpl
dc.language.containerengpl
dc.rightsUdzielam licencji. Uznanie autorstwa - Użycie niekomercyjne - Na tych samych warunkach 4.0 Międzynarodowa*
dc.rights.licenceInna otwarta licencja
dc.rights.urihttp://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.pl*
dc.share.typeotwarte czasopismo
dc.subject.enLittle Ice Agepl
dc.subject.enmorainespl
dc.subject.enrock glacierspl
dc.subject.enELApl
dc.subject.enclimatic changepl
dc.subject.enAlpspl
dc.subtypeArticlepl
dc.titleThe Little Ice Age in the Alps : its record in glacial deposits and rock glacier formationpl
dc.title.alternativeMała Epoka Lodowa w Alpach : jej zapis w osadach glacjalnych i formowaniu lodowców gruzowychpl
dc.title.journalStudia Geomorphologica Carpatho-Balcanicapl
dc.typeJournalArticlepl
dspace.entity.typePublication
dc.abstract.enpl
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.
dc.affiliationpl
Wydział Biologii i Nauk o Ziemi : Instytut Nauk Geologicznych
dc.contributor.authorpl
Zasadni, Jerzy - 142902
dc.date.accessionpl
2018-12-10
dc.date.accessioned
2019-01-08T08:27:10Z
dc.date.available
2019-01-08T08:27:10Z
dc.date.issuedpl
2007
dc.date.openaccess
0
dc.description.accesstime
w momencie opublikowania
dc.description.additionalpl
Bibliogr. s. 133-136
dc.description.physicalpl
117-137
dc.description.version
ostateczna wersja wydawcy
dc.description.volumepl
41
dc.identifier.eissnpl
2199-6180
dc.identifier.isbnpl
83-88549-56-1
dc.identifier.isbnpl
978-83-88549-56-4
dc.identifier.issnpl
0081-6434
dc.identifier.projectpl
ROD UJ / OP
dc.identifier.uri
https://ruj.uj.edu.pl/xmlui/handle/item/65070
dc.identifier.weblinkpl
https://www.igipz.pan.pl/tl_files/igipz/ZGiHGiW/sgcb/sgcb_41/sgcb_41_07.pdf
dc.languagepl
eng
dc.language.containerpl
eng
dc.rights*
Udzielam licencji. Uznanie autorstwa - Użycie niekomercyjne - Na tych samych warunkach 4.0 Międzynarodowa
dc.rights.licence
Inna otwarta licencja
dc.rights.uri*
http://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.pl
dc.share.type
otwarte czasopismo
dc.subject.enpl
Little Ice Age
dc.subject.enpl
moraines
dc.subject.enpl
rock glaciers
dc.subject.enpl
ELA
dc.subject.enpl
climatic change
dc.subject.enpl
Alps
dc.subtypepl
Article
dc.titlepl
The Little Ice Age in the Alps : its record in glacial deposits and rock glacier formation
dc.title.alternativepl
Mała Epoka Lodowa w Alpach : jej zapis w osadach glacjalnych i formowaniu lodowców gruzowych
dc.title.journalpl
Studia Geomorphologica Carpatho-Balcanica
dc.typepl
JournalArticle
dspace.entity.type
Publication
Affiliations

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