La falla de Meyssac señala de manera espectacular la unión de los últimos contrafuertes arenosos del Macizo Central y de los sedimentos calcáreos depositados unos millones de años más tarde. También marca una clara ruptura en términos de paisaje, vegetación, uso del suelo y prácticas agrícolas. Esto es lo que les proponemos descubrir a través de las nueve estaciones pedagógicas.
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