Français : Galets jurassiques (Callovien) torrentiels, provenant des calcaires siliceux (spiculites) liasiques ou oolithiques du Dogger dans le domaine intermédiaire, zone Château d'Oche-Corbeyrier, suite à la montée des blocs éjectés en transpression de la marge N-Briançonnaise. Septfontaine (1984,1995). Voir Wiki: Géologie des Alpes, le domaine Briançonnais.
English: Jurassic limestone and siliceous torrential pebbles (Callovian) from the Château d'Oche-Corbeyrier zone. Uplift of ejected paleotectonic blocks in a transpressive regime, N-Briançonnais margin. Septfontaine (1984,1995). See Wiki: Géologie des Alpes, le domaine Briançonnais.
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