Its geological and geographical environment puts us in this area as belonging to one of the massifs of the Betic, belonging to Penibética systems, a range that runs from the southern province of Cadiz to Almeria, formed by a stacking of thrust sheets that overlap each other.
The robes and Filarbide-Nevado Alpujarride are that crop up in Sierra Nevada, thus presenting a sector with a vast wealth in metamorphic Paleozoic origin, consisting mainly during the Alpine orogeny in the Tertiary.
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