Geomorphic evolution of the Miage Lake: a morphometric evaluation of the changes from 2018 to 2024

The Miage Glacier, located on the Italian side of Mont Blanc, features the popular touristic Lake Miage. This lake has experienced significant changes in recent years, including a Glacial Lake Outburst Flood (GLOF) in July 2022. This study uses geomorphometry to analyze the lake's evolution and increasing hazard. Comparing photogrammetric surveys (2018, 2022, and 2024), changes were tracked in the lake's volume. In 2018, the lake held 170,000 m³ of water, with a potential capacity of 340,000 m³. By 2022, the volume increased to 450,000 m³. In 2024, the actual volume was 137,000 m³ and the potential volume decreased to 210,000 m³. These changes highlight the complex role of factors influencing the lake's dynamics, including glacier flow, ice melt, and debris input. Continuous monitoring is crucial to understanding these evolving processes including the natural risks that can affect the area.

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Publication Details

Journal
Zenodo (CERN European Organization for Nuclear Research)
Published
2025-04-07
DOI
https://doi.org/10.5281/zenodo.15166555
Primary Topic
Cryospheric studies and observations
Type
article
Field-Weighted Citation Impact
0.00
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article

Geomorphic evolution of the Miage Lake: a morphometric evaluation of the changes from 2018 to 2024

Zenodo (CERN European Organization for Nuclear Research)
Cryospheric studies and observations
article

Geomorphic evolution of the Miage Lake: a morphometric evaluation of the changes from 2018 to 2024

article en

Abstract

The Miage Glacier, located on the Italian side of Mont Blanc, features the popular touristic Lake Miage. This lake has experienced significant changes in recent years, including a Glacial Lake Outburst Flood (GLOF) in July 2022. This study uses geomorphometry to analyze the lake's evolution and increasing hazard. Comparing photogrammetric surveys (2018, 2022, and 2024), changes were tracked in the lake's volume. In 2018, the lake held 170,000 m³ of water, with a potential capacity of 340,000 m³. By 2022, the volume increased to 450,000 m³. In 2024, the actual volume was 137,000 m³ and the potential volume decreased to 210,000 m³. These changes highlight the complex role of factors influencing the lake's dynamics, including glacier flow, ice melt, and debris input. Continuous monitoring is crucial to understanding these evolving processes including the natural risks that can affect the area.

Zenodo (CERN European Organization for Nuclear Research)
University of Turin (IT), Sapienza University of Rome (IT)
Openalex Percentile: Top 54%
Cryospheric studies and observations
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