Bulletin of Volcanology

, Volume 65, Issue 5, pp 331–345

New insight into the factors leading to the 1998 flank collapse and lahar disaster at Casita volcano, Nicaragua

  • Norman Kerle
  • Benjamin van Wyk de Vries
  • Clive Oppenheimer
Research Article

DOI: 10.1007/s00445-002-0263-9

Cite this article as:
Kerle, N., van Wyk de Vries, B. & Oppenheimer, C. Bull Volcanol (2003) 65: 331. doi:10.1007/s00445-002-0263-9


During unusually high rainfall associated with Hurricane Mitch in 1998, a flank collapse leading to a disastrous lahar occurred at Casita volcano, Nicaragua. The lack of a similar failure during a rainfall event of comparable magnitude in 1982 (Tropical Storm Alleta) suggests that additional factors influenced the 1998 collapse. We have investigated the potential contribution of erosional flank undercutting, seismic activity and anthropogenic land-cover change at the collapse site. Except for seismic events prior to Mitch, which may have increased flank instability, none of these factors appears significant. Instead, for failure to occur, the following conditions were required: (1) highly fractured slope material allowing deep and rapid infiltration of meteoric water, (2) a less permeable underlying layer to obstruct drainage, (3) strong, continuous antecedent rainfall to build up high pore-water pressure, and (4) episodic, high-intensity precipitation during Mitch to generate recurrent pressure waves. Prerequisite (1) was provided by edifice-wide deformation towards the south-east, seismic activity and proximity to a prominent fault, and local subsidence. Condition (2) was met by clay-rich layers resulting from hydrothermal alteration. More than 1,900 mm of rain fell in the 6 months prior to Mitch without significant interruption, while intense episodic precipitation occurred during the hurricane, satisfying conditions (3) and (4), respectively. The main difference with Alleta was that it occurred at the beginning of the rainy season and, therefore, without sufficient antecedent rainfall. Anthropogenic activity, including land-cover change, did not affect slope stability (i.e. the hazard). However, vulnerability was generated when two towns were established in the lowlands south of Casita, on top of previous lahar deposits. It was greatly increased when approximately 4 km of forest between the collapse site and the towns were cleared, paving the way for a largely unobstructed debris flow. Deforestation also facilitated erosion along the flanks to provide about 78% of the material contained in the lahar when it destroyed the towns, killing more than 2,500 people.


Flank collapse Gravity slide Hurricane Mitch Lahar Nicaragua 

Copyright information

© Springer-Verlag 2003

Authors and Affiliations

  • Norman Kerle
    • 1
    • 3
  • Benjamin van Wyk de Vries
    • 2
  • Clive Oppenheimer
    • 1
  1. 1.Dept. of Geography, Volcano Remote Sensing GroupUniversity of CambridgeCambridgeUK
  2. 2.Magmas et Volcans (UMR 6524)OPGC UniversitéClermont-FerrandFrance
  3. 3.ITCEnschedeThe Netherlands

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