The role of landslides in the evolution of a small mountain river valley (Polish Carpathians)

2021
journal article
article
1
dc.abstract.enIn this work we describe the role of landslide processes in shaping river channels and the development of valley floors in $3^{rd}$ and $4^{th}$ order catchments in the Polish Flysch Carpathians. The main focus of the study was on the contact zone between the landslide system and the river channel, where it has been shown that 30.2% of the length of the river network are affected by landslides. Research shows that 93% of landslides have some form of contact with the river system. Research further shows that the most common contact types in the study are point and area types according to the Korup classification. The most common impacts of landslides on the river channel are riparian and partial occlusion types. Landslides very often cause complete or partial displacement of the river channel, which frequently leads to the blockage of flow, which in turn creates landslide lakes, followed by accumulation zones. The effect of such events is the transformation of the longitudinal profile of the river and the intensification of erosive processes in the contact zone and downstream. Increased activity of erosive processes can lead to the activation of landslide processes, including on the opposite slope.pl
dc.affiliationWydział Geografii i Geologii : Instytut Geografii i Gospodarki Przestrzennejpl
dc.affiliationSzkoła Doktorska Nauk Ścisłych i Przyrodniczychpl
dc.contributor.authorCaputa, Joanna - 243910 pl
dc.contributor.authorGorczyca, Elżbieta - 128116 pl
dc.date.accession2021-09-08pl
dc.date.accessioned2021-09-29T08:01:45Z
dc.date.available2021-09-29T08:01:45Z
dc.date.issued2021pl
dc.date.openaccess0
dc.description.accesstimew momencie opublikowania
dc.description.additionalBibliogr. s. 238-239pl
dc.description.number3pl
dc.description.physical227-239pl
dc.description.versionostateczna wersja wydawcy
dc.description.volume44pl
dc.identifier.doi10.18814/epiiugs/2020/020078pl
dc.identifier.eissn2586-1298pl
dc.identifier.issn0705-3797pl
dc.identifier.projectROD UJ / Opl
dc.identifier.urihttps://ruj.uj.edu.pl/xmlui/handle/item/279236
dc.identifier.weblinkhttps://www.episodes.org/journal/view.html?doi=10.18814/epiiugs/2020/020078pl
dc.languageengpl
dc.language.containerengpl
dc.pbn.affiliationDziedzina nauk ścisłych i przyrodniczych : nauki o Ziemi i środowiskupl
dc.rightsUdzielam licencji. Uznanie autorstwa - Użycie niekomercyjne 4.0 Międzynarodowa*
dc.rights.licenceCC-BY-NC
dc.rights.urihttp://creativecommons.org/licenses/by-nc/4.0/legalcode.pl*
dc.share.typeotwarte czasopismo
dc.subtypeArticlepl
dc.titleThe role of landslides in the evolution of a small mountain river valley (Polish Carpathians)pl
dc.title.journalEpisodespl
dc.typeJournalArticlepl
dspace.entity.typePublication
dc.abstract.enpl
In this work we describe the role of landslide processes in shaping river channels and the development of valley floors in $3^{rd}$ and $4^{th}$ order catchments in the Polish Flysch Carpathians. The main focus of the study was on the contact zone between the landslide system and the river channel, where it has been shown that 30.2% of the length of the river network are affected by landslides. Research shows that 93% of landslides have some form of contact with the river system. Research further shows that the most common contact types in the study are point and area types according to the Korup classification. The most common impacts of landslides on the river channel are riparian and partial occlusion types. Landslides very often cause complete or partial displacement of the river channel, which frequently leads to the blockage of flow, which in turn creates landslide lakes, followed by accumulation zones. The effect of such events is the transformation of the longitudinal profile of the river and the intensification of erosive processes in the contact zone and downstream. Increased activity of erosive processes can lead to the activation of landslide processes, including on the opposite slope.
dc.affiliationpl
Wydział Geografii i Geologii : Instytut Geografii i Gospodarki Przestrzennej
dc.affiliationpl
Szkoła Doktorska Nauk Ścisłych i Przyrodniczych
dc.contributor.authorpl
Caputa, Joanna - 243910
dc.contributor.authorpl
Gorczyca, Elżbieta - 128116
dc.date.accessionpl
2021-09-08
dc.date.accessioned
2021-09-29T08:01:45Z
dc.date.available
2021-09-29T08:01:45Z
dc.date.issuedpl
2021
dc.date.openaccess
0
dc.description.accesstime
w momencie opublikowania
dc.description.additionalpl
Bibliogr. s. 238-239
dc.description.numberpl
3
dc.description.physicalpl
227-239
dc.description.version
ostateczna wersja wydawcy
dc.description.volumepl
44
dc.identifier.doipl
10.18814/epiiugs/2020/020078
dc.identifier.eissnpl
2586-1298
dc.identifier.issnpl
0705-3797
dc.identifier.projectpl
ROD UJ / O
dc.identifier.uri
https://ruj.uj.edu.pl/xmlui/handle/item/279236
dc.identifier.weblinkpl
https://www.episodes.org/journal/view.html?doi=10.18814/epiiugs/2020/020078
dc.languagepl
eng
dc.language.containerpl
eng
dc.pbn.affiliationpl
Dziedzina nauk ścisłych i przyrodniczych : nauki o Ziemi i środowisku
dc.rights*
Udzielam licencji. Uznanie autorstwa - Użycie niekomercyjne 4.0 Międzynarodowa
dc.rights.licence
CC-BY-NC
dc.rights.uri*
http://creativecommons.org/licenses/by-nc/4.0/legalcode.pl
dc.share.type
otwarte czasopismo
dc.subtypepl
Article
dc.titlepl
The role of landslides in the evolution of a small mountain river valley (Polish Carpathians)
dc.title.journalpl
Episodes
dc.typepl
JournalArticle
dspace.entity.type
Publication
Affiliations

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