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My 3D model generated with photogrammetry software 3DF Zephyr v3.702 processing 44 images. Entre migmatites et gneiss d’une part et le leucogranite de Blond à l’ouest, la faille d’Oradour sur Glane a servi de drain à des fluides riches en silice échappés d’une chambre magmatique située en profondeur. La faille a permis à la silice de cristalliser sous la forme d’un filon de quartz blanc de près de 700 metres de long et formant une crête dans le paysage.
CC AttributionCreative Commons Attribution
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