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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 (Avtor), ID Vrabec, Marko (Avtor), ID Šmuc, Andrej (Avtor)

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Izvleček
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.

Jezik:Angleški jezik
Ključne besede:complex landslide, translational slip, debris flow, hyperconcentrated flow, UAV, granulometry
Vrsta gradiva:Članek v reviji
Tipologija:1.01 - Izvirni znanstveni članek
Organizacija:NTF - Naravoslovnotehniška fakulteta
Status publikacije:Objavljeno
Različica publikacije:Objavljena publikacija
Leto izida:2025
Št. strani:Str. 4013-4027
Številčenje:Vol. 22, iss. 12
PID:20.500.12556/RUL-178847 Povezava se odpre v novem oknu
UDK:55
ISSN pri članku:1612-510X
DOI:10.1007/s10346-025-02598-5 Povezava se odpre v novem oknu
COBISS.SI-ID:246472963 Povezava se odpre v novem oknu
Datum objave v RUL:30.01.2026
Število ogledov:41
Število prenosov:14
Metapodatki:XML DC-XML DC-RDF
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Gradivo je del revije

Naslov:Landslides : journal of the International Consortium on Landslides
Založnik:Springer Nature, International Consortium on Landslides
ISSN:1612-510X
COBISS.SI-ID:2274913 Povezava se odpre v novem oknu

Licence

Licenca:CC BY 4.0, Creative Commons Priznanje avtorstva 4.0 Mednarodna
Povezava:http://creativecommons.org/licenses/by/4.0/deed.sl
Opis:To je standardna licenca Creative Commons, ki daje uporabnikom največ možnosti za nadaljnjo uporabo dela, pri čemer morajo navesti avtorja.

Projekti

Financer:ARIS - Javna agencija za znanstvenoraziskovalno in inovacijsko dejavnost Republike Slovenije
Številka projekta:P1-0419
Naslov:Dinamična Zemlja

Financer:ARIS - Javna agencija za znanstvenoraziskovalno in inovacijsko dejavnost Republike Slovenije
Številka projekta:P1-0195
Naslov:Geookolje in geomateriali

Financer:ARIS - Javna agencija za znanstvenoraziskovalno in inovacijsko dejavnost Republike Slovenije
Številka projekta:J7-60124
Naslov:Celostni pristop k preučevanju vplivov ekstremnih vremenskih dogodkov na procese na Zemljinem površju (ExtremEarth)

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