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The Ambrona and Torralba archeological sites are related to the pleistocene evolution of the Conquezuela-Ambrona-Torralba polje. A study made of the centre-south sectors of this polje, nowadays, highly degraded in part though being dissected by the river Masegar, shows that Torralba and Ambrona occupy different geomorphological positions. This would mean that both the age and stratigraphic formations of the sites are different.
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