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. 2022 Apr 22;20(6):2825–3069. doi: 10.1007/s10518-022-01357-4

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Fig. 20 — Lateral spreading on the bank of the Lempa River in El Salvador due to liquefaction triggered by the M 7.7 subduction-zone earthquake of January 2001; notice the collapsed railway bridge in the background due to the separation of the piers caused by the spreading (Bommer et al. 2002)