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Outcrop of polyphase deformation and intrusion structures in gneiss at Lavertezzo, Ticino, Switzerland. The outcrop is part of the Penninic nappes, comprising metasedimntary and intrusive rocks of Variscan age, which have been deformed during both the Variscan and Alpine orogenies. This outcrop is excellent for field training and protected.
PhotoID82

Outcrop of polyphase deformation and intrusion structures in gneiss at Lavertezzo, Ticino, Switzerland. The outcrop is part of the Penninic nappes, comprising metasedimntary and intrusive rocks of Variscan age, which have been deformed during both the Variscan and Alpine orogenies. This outcrop is excellent for field training and protected.
PhotoID82

Photograph: Cees Passchier