Chronicle of destruction: the Wayanad landslide of July 30, 2024

Yunus, Ali P. ORCID: https://orcid.org/0000-0001-9545-0714; Sajinkumar, K.S.; Gopinath, Girish; Subramanian, Srikrishnan Siva; Kaushal, Sahil; Thanveer, Jiyadh; Achu, A.L.; Islam, Shah Masud Ul; Ishan, Adin; Krishnapriya, V.K.; Rajaneesh, A.; Dewrari, Manish; Dixit, Sudhanshu; Singh, Shiwam; Srivastava, Piyush; Oommen, Thomas; Nedumpallile Vasu, Nikhil; Sen, Sumit; Narayana, A.C.; Ambili, V.; Pradeep, G.S.; Kuriakose, Sekhar Lukose. 2025 Chronicle of destruction: the Wayanad landslide of July 30, 2024. Landslides, 22 (6). 1891-1908. 10.1007/s10346-025-02494-y

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Official URL: https://doi.org/10.1007/s10346-025-02494-y

Abstract/Summary

On the morning of July 30, 2024, a catastrophic landslide struck Wayanad, India, in the ecologically sensitive Western Ghats, claiming over 260 lives, with many still missing beneath the debris. Here, we present a comprehensive overview of the landslide event based on field, satellite, and aerial images analysis, numerical modeling, and geotechnical testing to unravel the failure mechanism and its catastrophic impact on downstream communities. Our analysis revealed that a pre-existing crack, formed in 2020, acted as the initiation point for the recent failure. The underlying weathered and sheared geology, coupled with structural discontinuities, and thick soil strata, exacerbated by intense rainfall on July 29–30, catalyzed the transition of a planar slide into a catastrophic debris flow. Numerical simulations indicate that the debris flow initiated around 01:00 h, peaked at 04:00 h, and reached a maximum velocity of 28 m/s. The estimated volume of displaced material ranged between 5.17 × 10⁶ and 5.72 × 10⁶ m3, ranking it among the largest debris flows in India. The flow’s run-up height in the transitional zone reached 32 m, amplified by multiple damming effects and topographic features such as cascades and river sinuosity, causing extensive infrastructure damage to the downstream population. Given the terrain’s known fragility and history of sequential events, this region requires urgent attention for real-time monitoring and mitigation strategies to reduce future risks.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	10.1007/s10346-025-02494-y
ISSN:	1612-510X
Date made live:	13 May 2025 11:23 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/539430

Item Type:

Publication - Article

Digital Object Identifier (DOI):

10.1007/s10346-025-02494-y

ISSN:

1612-510X

Date made live:

13 May 2025 11:23 +0 (UTC)

URI:

https://nora.nerc.ac.uk/id/eprint/539430