Granite from more than 320 million years ago at the gates of a geological museum
The granite rocks of the Salamanca town of Juzbado were formed between 320 and 340 million years ago. They are deformed, precisely, because they are older than the fault in the terrain on which they are located.The data agrees with other dates in the surroundings and reveals that the geological origin of the area dates back to the collision that gave rise to the supercontinent Pangea. according to an international investigation in which the University of Salamanca and the Museo de la Falla, located in this municipality, have participated.