# Hydrothermal weakening and slope instability at Vulcano (Italy) analyzed using drones and in-situ strength measurements

**Authors:** Benjamin F. De Jarnatt, Thomas R. Walter, Michael J. Heap, Daniel Müller, Antonino Fabio Pisciotta

PMC · DOI: 10.1038/s43247-025-03014-5 · Communications Earth & Environment · 2025-12-04

## TL;DR

Researchers studied how hydrothermal activity weakens volcanic rocks at Vulcano, Italy, using drones and strength tests to assess slope instability and improve hazard monitoring.

## Contribution

The study introduces an integrated drone and in-situ testing method to map rock strength and alteration on inaccessible volcanic slopes.

## Key findings

- Hydrothermal alteration correlates with a 50% reduction in rock strength at Vulcano.
- Alteration intensity, mapped via drone and PCA, aligns with past mass-wasting events.
- The method enables hazard assessment on steep, inaccessible volcanic flanks.

## Abstract

Instability at volcanic edifices poses significant hazards, yet the processes driving rock weakening, particularly on steep, eroding flanks, remain poorly understood due to limited accessibility. Hydrothermal alteration is a key factor in weakening volcanic rocks, contributing to edifice destabilization and flank instability. La Fossa cone (Vulcano, Italy) provides an ideal setting for this study, with accessible hydrothermal alteration at the crater rim and similar alteration along inaccessible flanks that have a recent history of mass wasting. Here, we developed an integrated methodology combining drone photogrammetry with in situ Schmidt hammer testing to derive an empirical alteration-to-strength relationship for the crater rim and applied this knowledge to alteration sites on inaccessible flanks. An alteration map was generated using a Principal Component Analysis (PCA) to aid our classifications. This map was used to transpose over 1000 Schmidt hammer measurements (R-values ranging from 10.5 to 82), creating a thematic strength-alteration map. Results indicate a ~50% reduction in relative rock strength correlating with areas of degassing and hydrothermal activity, which coincides with past mass-wasting events. This integrated approach offers a transferable workflow for assessing volcanic slope instability, with direct applications to hazard monitoring and early warning systems.

At La Fossa cone, Vulcano, Italy, alteration intensity, when categorized by color, correlates with rock weakening and past mass wasting events, as determined by drone mapping and in-situ strength surveys.

## Full-text entities

- **Genes:** PCSK1 (proprotein convertase subtilisin/kexin type 1) [NCBI Gene 5122] {aka BMIQ12, NEC1, PC1, PC1/3, PC3, SPC3}, PKD2 (polycystin 2, transient receptor potential cation channel) [NCBI Gene 5311] {aka APKD2, PC2, PKD4, Pc-2, TRPP2}
- **Diseases:** discoloration (MESH:D014075), wasting (MESH:D019282), mass-wasting (MESH:C536030), PC (MESH:D015324), Volcano flank failure (MESH:D051437)
- **Chemicals:** CO2 (MESH:D002245), silica (MESH:D012822), He (MESH:D006371), sulfur (MESH:D013455), Schmidt hammer (-), H2O (MESH:D014867), E (MESH:D004540), Fe2O3 (MESH:C000499), sulfate (MESH:D013431), acid (MESH:D000143), N2 (MESH:D009584)
- **Mutations:** rs15051405, C in 1991

## Full text

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## Figures

8 figures with captions in the complete paper: https://tomesphere.com/paper/PMC12764430/full.md

## References

20 references — full list in the complete paper: https://tomesphere.com/paper/PMC12764430/full.md

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Source: https://tomesphere.com/paper/PMC12764430