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Lateral spreading

Plugin ID: 3697

Lateral spreading for seismic microzonation

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Lateral spreading is a geotechnical phenomenon that occurs when the ground moves laterally under the influence of external forces, such as an earthquake. This phenomenon is also influenced by the morphological slope of the terrain. It primarily occurs in water-saturated sandy soils that, when subjected to stress, lose their cohesion and behave like a fluid; a phenomenon known as liquefaction. As a result, the ground moves laterally, creating potential risks for buildings and infrastructure.

Version QGIS >= QGIS <= Date
1.0.1 - 3.16.0 4.99.0 528 ls04ms 2026-03-13T13:41:53.957247+00:00
1.0.0 - 3.16.0 4.99.0 79 ls04ms 2026-03-11T10:56:49.513424+00:00
0.4 - 3.34.0 3.99.0 197 ls04ms 2026-02-08T16:36:46.531589+00:00
0.3 - 3.34.0 3.99.0 765 ls04ms 2025-02-01T13:33:02.309163+00:00
0.2 - 3.34.0 3.99.0 469 ls04ms 2025-01-24T07:59:02.435844+00:00