Details

Long-term post-event processes and major reactivation of a complex landslide : 2000–2023 evolution of the Ciprnik landslide, Julian Alps, Slovenia
ID Novak, Andrej (Author), ID Vrabec, Marko (Author), ID Šmuc, Andrej (Author)

.pdfPDF - Presentation file, Download (9,86 MB)
MD5: 8C6FB2DCD70CF9524CA7CCE6C984DE28
URLURL - Source URL, Visit https://link.springer.com/article/10.1007/s10346-025-02598-5 This link opens in a new window

Abstract
The Ciprnik complex landslide in the Planica valley (NW Slovenia) happened on 19. 11. 2000 as a translation slip-debris flow-hyperconcentrated flow event. It was triggered by a combination of the local geological structure (highly fractured beds dipping parallel to the surface), lithology (alternation of thin bedded carbonates and fine-grained clastics), and record-breaking monthly rainfall (613.6 mm in the month of the event). Twenty-three years later, on the night from 24. to 25. 10. 2023, large parts of the landslide reactivated during intense short-duration rainfall, which has a relatively common occurrence (104.2 mm in 24 h). We use 2006–2023 time series of photogrammetrically derived digital elevation models generated from aerial photographs and unmanned aerial vehicle surveys, sedimentological analysis, and meteorological data to (1) analyze decade-scale post-event processes on the Ciprnik landslide following the initial sliding event in November 2000 and (2) to study the October 2023 event and compare it to the November 2000 event. We find that after the initial November 2000 event, the area of the Ciprnik landslide remained unstable with an average annual erosion rate of 1000 to 3500 m$^3$ of sediment. The 2023 event measured 26,000 m$^3$ and, despite a different triggering rainfall, again occurred as a translation slip-debris flow-hyperconcentrated flow event exhibiting a strong fining down of sediment (from muddy-sandy-gravel to sandy-silt). This study demonstrates the complexity of triggering thresholds in the aftermath of the main mass movement event. Even in the later events, which have the same transport mechanisms as the original event, the triggering precipitation can differ considerably in duration and magnitude.

Language:English
Keywords:complex landslide, translational slip, debris flow, hyperconcentrated flow, UAV, granulometry
Work type:Article
Typology:1.01 - Original Scientific Article
Organization:NTF - Faculty of Natural Sciences and Engineering
Publication status:Published
Publication version:Version of Record
Year:2025
Number of pages:Str. 4013-4027
Numbering:Vol. 22, iss. 12
PID:20.500.12556/RUL-178847 This link opens in a new window
UDC:55
ISSN on article:1612-510X
DOI:10.1007/s10346-025-02598-5 This link opens in a new window
COBISS.SI-ID:246472963 This link opens in a new window
Publication date in RUL:30.01.2026
Views:478
Downloads:219
Metadata:XML DC-XML DC-RDF
:
Copy citation
Share:Bookmark and Share

Record is a part of a journal

Title:Landslides : journal of the International Consortium on Landslides
Publisher:Springer Nature, International Consortium on Landslides
ISSN:1612-510X
COBISS.SI-ID:2274913 This link opens in a new window

Licences

License:CC BY 4.0, Creative Commons Attribution 4.0 International
Link:http://creativecommons.org/licenses/by/4.0/
Description:This is the standard Creative Commons license that gives others maximum freedom to do what they want with the work as long as they credit the author.

Projects

Funder:ARIS - Slovenian Research and Innovation Agency
Project number:P1-0419
Name:Dinamična Zemlja

Funder:ARIS - Slovenian Research and Innovation Agency
Project number:P1-0195
Name:Geookolje in geomateriali

Funder:ARIS - Slovenian Research and Innovation Agency
Project number:J7-60124
Name:Celostni pristop k preučevanju vplivov ekstremnih vremenskih dogodkov na procese na Zemljinem površju (ExtremEarth)

Similar documents

Similar works from RUL:
Similar works from other Slovenian collections:

Back