File:StoreggaTsunamiHauteurModèle Réel2005.png

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Français : Hauteur réelle (barre verticale), estimée d'après les preuves de dépôts in-situ du tsunami à "Maggie Kettles Loch" dans les îles Shetland comparée à deux modélisations de la hauteur de la crête de la vague du méga-tsunami du Storrega sur les îles Shetland basé (et variation sur quelques heures). Les deux modélisations (trait plein noir, et pointillé) sont respectivement basées sur des vitesses de glissement de 20 m/s et 35 m/s (Downson & al, en 2019 [1], d'après Bondevik et al., 2005).
English: True height (vertical bar), estimated from evidence of in-situ tsunami deposits at "Maggie Kettles Loch" in the Shetland Islands compared to two models of the wave crest height of the Storrega mega-tsunami on Shetland Islands based (and variation over a few hours). The two models (solid black line, and dotted line) are respectively based on sliding speeds of 20 m/s and 35 m/s (Downson & al, in 2019 [2], according to Bondevik et al., 2005).
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Source (en) Alastair G. Dawson et Sue Dawson, « Reconciling Storegga tsunami sedimentation patterns with modelled wave heights: A discussion from the Shetland Isles field laboratory » [archive], sur Sedimentology, avril 2020 (ISSN 0037-0746, DOI 10.1111/sed.12643, consulté le 18 février 2022), p. 1344–1353
Author Alastair G. Dawson et Sue Dawson,

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current15:34, 18 February 2022Thumbnail for version as of 15:34, 18 February 20221,397 × 1,160 (443 KB)Lamiot (talk | contribs)Uploaded a work by Alastair G. Dawson et Sue Dawson, from (en) Alastair G. Dawson et Sue Dawson, « Reconciling Storegga tsunami sedimentation patterns with modelled wave heights: A discussion from the Shetland Isles field laboratory » [archive], sur Sedimentology, avril 2020 (ISSN 0037-0746, DOI 10.1111/sed.12643, consulté le 18 février 2022), p. 1344–1353 with UploadWizard

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