Geologically speaking, Corfu is an off-shore peak of ranges belonging to the deformed belt of mountains which run through Yugoslavia and Western Greece.
The oldest rocks of the Highlands are the Mesozoic limestone (about 135 million years old) which were crushed against the central core in the Tertiary era (about 75 million years ago) forming marls, silstones, and sandstone areas. The softer deposits have produced some beautiful caves and grottoes of which the best examples are on Paxos, an island south of Corfu. |