Mineral veins

Mineral veins

Geological FeatureWaterfront/Riverside ParkBicycle Path Coastal HabitatPedestrian Friendly


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The intrusion of the sub-volcanic massif of Sintra occured 70/80 to 100 million years ago and it filled some of the existing gaps. Mineral veins can, therefore, be observable in many cliffs.


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Mineral veins

added by Cascais Portugal



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