izpis_h1_title_alt

Using a lidar-based height variability method for recognizing and analyzing fault displacement and related fossil mass movement in the Vipava Valley, SW Slovenia
ID Popit, Tomislav (Author), ID Rožič, Boštjan (Author), ID Šmuc, Andrej (Author), ID Novak, Andrej (Author), ID Verbovšek, Timotej (Author)

.pdfPDF - Presentation file, Download (8,84 MB)
MD5: E58FA2BB2B7D46ABAE4828AE7743A941
URLURL - Source URL, Visit https://www.mdpi.com/2072-4292/14/9/2016 This link opens in a new window

Abstract
The northern slopes of the Vipava Valley are defined by a thrust front of Mesozoic carbonates over Tertiary flysch deposits. These slopes are characterized by a variety of different surface forms, among which recent and fossil polygenetic landslides are the most prominent mass movements. We used the height variability method as a morphometric indicator, which proved to be the most useful among the various methods for quantifying and visualizing fossil landslides. Height variability is based on the difference in elevations derived from a high-resolution lidar-derived DEM. Based on geologic field mapping and geomorphometric analysis, we distinguished two main types of movements: structurally induced movement along the fault zone and movements caused by complex Quaternary gravitational slope processes. The most pronounced element is the sliding of the huge rotational carbonate massif, which was displaced partly along older fault structures in the hinterland of fossil rock avalanches and carbonate blocks. In addition to the material properties of the lithology, the level of surface roughness also depends on the depositional processes of the individual sedimentary bodies. These were formed by complex sedimentary events and are intertwined in the geological past. The sedimentary bodies indicate two large fossil rock avalanches, while the smaller gravity blocks indicate translational–rotational slides of carbonate and carbonate breccia.

Language:English
Keywords:slope process, surface roughness, rock avalanche, geomorphometric analysis, geological setting, deep-seated rotational and translational slides
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:2022
Number of pages:16 str.
Numbering:Vol. 14, iss. 9, art. 2016
PID:20.500.12556/RUL-145254 This link opens in a new window
UDC:55
ISSN on article:2072-4292
DOI:10.3390/rs14092016 This link opens in a new window
COBISS.SI-ID:105725699 This link opens in a new window
Publication date in RUL:14.04.2023
Views:333
Downloads:54
Metadata:XML RDF-CHPDL DC-XML DC-RDF
:
Copy citation
Share:Bookmark and Share

Record is a part of a journal

Title:Remote sensing
Shortened title:Remote sens.
Publisher:MDPI
ISSN:2072-4292
COBISS.SI-ID:32345133 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:ARRS - Slovenian Research Agency
Project number:P1-0195
Name:Geookolje in geomateriali

Funder:Other - Other funder or multiple funders
Funding programme:International Consortium on Landslides
Project number:IPL-216
Name:Diversity and Hydrogeology of Mass Movements in the Vipava Valley, SW Slovenia

Funder:Other - Other funder or multiple funders
Funding programme:International Consortium on Landslides Adriatic–Balkan Network

Similar documents

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

Back