The morphological structure of the Brive basin is broken down into two large groups: a plateau area made up of crystalline rocks to the northeast, surrounding a hilly area in the center, made up of upper Paleozoic sedimentary formations, and to the southwest Mesozoic sedimentary rocks.
Piedmont of the Massif Central, gateway to the Aquitain Basin, the Pays de Brive is a contact zone between two geological groups which marks the transition between the poor soils of a Hercynian massif and the more generous limestone soils of a sedimentary basin of secondary.
Don't miss the visit Pans de Travassac (open-air slate quarries), unique site in Europe!
The limestones of the margins of the Causse du Quercy or the Plaine d'Aquitaine, whose colors vary from white to beige through multiple shades of yellow. Don't miss the visit of Turenne or Noailles.
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