File:Cap de la chèvre Grès armoricain2010 438.JPG

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English: "Cap de la Chèvre" (ou "Beg Penn ar Roz" in Breton), Finistère,West of France)
Français : Sol superficiel constitué de grès armoricain plus ou moins délité (ici sur une zone d'érosion de la couche de terre de bruyère, induite par la surfréquentation) ; au "Cap de la Chèvre" (ou "Beg Penn ar Roz" en Breton, sur la Presqu'île de Crozon, dans le Finistère, en Bretagne, dans l'Ouest de la France). Site classé pour son paysage, faisant partie du Parc naturel régional d'Armorique. Cette avancée rocheuse élevée (plus de 100 m) essentiellement constituée de "grès armoricain" datés du Paléozoïque anté-carbonifère (Schistes et Grès Primaires produits de - 570 à - 345 millions d'années) avec “Schistes pourprés” au sud, qui sont des formations détritiques rouges continentales, postorogéniques). Ce cap supporte une zone de lande rase poussant sur quelques cm à dizaines de cm de terre de bruyère, fortement exposée au vent, soleil (et embruns lors des tempêtes).
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Author Lamiot

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current22:05, 12 August 2010Thumbnail for version as of 22:05, 12 August 20102,560 × 1,920 (2.32 MB)Lamiot (talk | contribs){{Information |Description={{en|1="Cap de la Chèvre" (ou "Beg Penn ar Roz" in Breton), Finistère,West of France)}} {{fr|1=Sol superficiel constitué de grès armoricain plus ou moins délité (ici sur une zone d'érosion de la

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