File:Cap de la chèvre Chemin 2010 440.JPG

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Français : creusement d'un sentier avec destruction de la couche de terre de bruyère, suite au passage répété des gens, ayant fait apparaître le substrat superficiel de grès armoricain, sur le site du "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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current22:18, 12 August 2010Thumbnail for version as of 22:18, 12 August 20102,544 × 1,560 (1.95 MB)Lamiot (talk | contribs){{Information |Description={{fr|1=creusement d'un sentier avec destruction de la couche de terre de bruyère, suite au passage répété des gens, ayant fait apparaître le substrat superficiel de grès armoricain, sur le site du "[[w:fr:Cap de la Chèvre

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