| http://www.w3.org/ns/prov#value | - At the beginning of the Miocene (about 24 million years ago), the area that now constitutes the AOCs of CdP, Tavel, and Lirac were a part of the Urgonian limestone peaks of which modern-day Plateau du bois de Saint Victor, and the series of limestone buttes that are visible as you approach CdP, are a part.
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