La ligne de stabilité est l'un des indicateurs de trait de côte utilisés dans le projet STORISK sur l'atoll de Hikueru (1965, 2016). Cette couche de géométrie polyligne correspond (i) sur les côtes naturelles, à la limite de la végétation ou à celle des débris anciens stabilisés issus de tempêtes, et (ii) sur les côtes anthropisées, à la limite externe des ouvrages de défense et des remblais.
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