Next Article in Journal
Slope Dynamics in Relation to the Occupation and Abandonment of a Mountain Farm in Þistilfjörður, Northeast Iceland
Previous Article in Journal
Earthquake-Induced Tsunamis in Western Greece (Ionian Sea and Western and Southern Peloponnese): Use of Tsunami Quantities, Impact and ITIS-2012 Intensities for Highlighting Susceptible Areas
 
 
Font Type:
Arial Georgia Verdana
Font Size:
Aa Aa Aa
Line Spacing:
Column Width:
Background:
Article

UAV Application for Short-Time Evolution Detection of the Vomice Landslide (South Italy)

by
Michele Mercuri
1,
Massimo Conforti
2,*,
Mariantonietta Ciurleo
2 and
Luigi Borrelli
2
1
National Research Council of Italy, Institute for Agricultural and Forest Systems in the Mediterranean (CNR-ISAFOM), Via Cavour 4/6, 87036 Rende, Italy
2
National Research Council of Italy, Research Institute for Geo-Hydrological Protection (CNR-IRPI), Via Cavour 4/6, 87036 Rende, Italy
*
Author to whom correspondence should be addressed.
Geosciences 2023, 13(2), 29; https://doi.org/10.3390/geosciences13020029
Submission received: 23 December 2022 / Revised: 20 January 2023 / Accepted: 23 January 2023 / Published: 25 January 2023

Abstract

This paper investigates the possibility to detect the short-time evolution of the slow-moving Vomice earth flow, located in the northeastern sector of the Calabria region (South Italy), by combining the information obtained from two different drone flights, carried out in February 2019 and June 2022, with field surveys. The obtained results consisted of delimiting all landslide bodies constituting the Vomice earth flow, detecting landslide types and the state of activity, as well as identifying spatial and volumetric changes. The obtained results showed that depletion and transition zones of the Vomice earth flow are active, while the accumulation zone appears prevalently dormant. Particularly, in the analyzed period, the depletion zone was characterized by local collapses of the main scarps where several slides evolving in earth flows caused more than 20 m of retrogressive fail upslope. The maximum elevation changes observed in these zones were about ±5 m. The volume of the material mobilized by mass movements was about 114.2 × 103 m3, whereas the volume of the accumulated material was approximately 92.7 × 103 m3. The transition zone was affected by several slow earthflows that re-mobilized the displaced material located in the middle portion of the landslide and reached the accumulation zone. Overall, the results of this study demonstrated the practicality and feasibility of using UAV tools for detecting the short-time evolution of a large landslide.
Keywords: earthflow; spatiotemporal analysis; morphological changes; UAV survey; structure-from-motion earthflow; spatiotemporal analysis; morphological changes; UAV survey; structure-from-motion

Share and Cite

MDPI and ACS Style

Mercuri, M.; Conforti, M.; Ciurleo, M.; Borrelli, L. UAV Application for Short-Time Evolution Detection of the Vomice Landslide (South Italy). Geosciences 2023, 13, 29. https://doi.org/10.3390/geosciences13020029

AMA Style

Mercuri M, Conforti M, Ciurleo M, Borrelli L. UAV Application for Short-Time Evolution Detection of the Vomice Landslide (South Italy). Geosciences. 2023; 13(2):29. https://doi.org/10.3390/geosciences13020029

Chicago/Turabian Style

Mercuri, Michele, Massimo Conforti, Mariantonietta Ciurleo, and Luigi Borrelli. 2023. "UAV Application for Short-Time Evolution Detection of the Vomice Landslide (South Italy)" Geosciences 13, no. 2: 29. https://doi.org/10.3390/geosciences13020029

APA Style

Mercuri, M., Conforti, M., Ciurleo, M., & Borrelli, L. (2023). UAV Application for Short-Time Evolution Detection of the Vomice Landslide (South Italy). Geosciences, 13(2), 29. https://doi.org/10.3390/geosciences13020029

Note that from the first issue of 2016, this journal uses article numbers instead of page numbers. See further details here.

Article Metrics

Back to TopTop