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LE CADRE GEOLOGIQUE - LE MUSÉE DE LA MINE DE GREASQUE
HISTOIRE & SCIENCE

LE CADRE GEOLOGIQUE

Le gisement de lignite de Provence doit son originalité à un environnement sédimentaire calcaire lacustre ainsi qu’en attestent les restes fossiles (flore et faune très riche) caractéristiques de conditions de vie sous un climat chaud.

Le bassin de l’Arc a une structure synclinale qui fait affleurer le charbon sur les bords de la cuvette et à proximité des reliefs.

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