, Huand et al. [57] ont, quant à eux, utilisé le code GEOWAVE (code basé sur les équations de Boussinesq) pour modéliser cet évènement. Ils trouvent une amplitude de vague très différente, d'une valeur de 31,5 m, de celle trouvée avec le modèle numérique Tsunami Squares et de notre loi empirique

, Certains évènements sont très bien documentés mais avec malheureusement des données manquantes. C'est le cas pour les deux exemples qui vont suivre, Autres évènements avec des données manquantes Notre liste d'évènements n'est évidemment pas exhaustive. En effet, nous avons étudié les évènements pour lesquels nous avons trouvé toutes les données dont nous avions besoin

, Mont Colonel Foster -Canada, 1946.

, Ile de Vancouver (Canada), un séisme d'une magnitude M w = 7.2 a provoqué un effondrement de terrain sur la face nord du Mont Colonel Foster. Un volume de 1,5 10 6 m 3 s'est détaché, 1946.

;. Cependant and +. Fjord, et nous n'avons trouvé aucune profondeur d'eau répertoriée pour ce lac. Nous n'avons aussi aucune estimation de l'amplitude de la vague générée, juste des hauteurs de run-up de 51 m sur le flanc opposé et Lake, Canada, issue.1, 2007.

×. and ×. Pacì, Potentiels évènements : ( ) Cumbre Vieja, La Palma -Canaries ; ( , ) Es Vedrá, Indonésie, 1783.

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