Πληροφορίες τοπωνυμίου

ΚΕΑ (Νησί) ΚΥΚΛΑΔΕΣ
The island's geological formation, as in most of the Cycladic islands, is composed of sedimentary rocks, formed on the sea bed some ten million years ago. The subsoil consists almost entirely of schists. A small percentage of marble (6 - 7%) can be found mainly on the island's eastern coastline.

Xenios Dias WebPage, University of Patras
• http://www.cyclades-info.gr/a/bba85c1f86ace148c225...