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Author: WikiMatrix
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English[en]
The western escarpment, between the Col de l'Épine and the Col de Saint-Michel, is composed of limestones from the Kimmeridgian and Oxfordian formations, with scree at the base.
Spanish[es]
La vertiente occidental, entre el col de La Espina y el col de Saint-Michel, está compuesta de calizas de las formaciones de Kimmeridgian y Oxfordian, con pedregal en la base.