Troodos, Mt. Olympus
NB- This site has to be considered as part of the Troodos ophiolite, a 90 million year old fragment of extremely well-preserved oceanic crust.
This is a site where the lower part of the oceanic crustal and upper mantle sequences are well exposed and where lower crustal and mantle processes can be studied and demonstrated.
Les noms des biens figurent dans la langue dans laquelle les Etats parties les ont soumis.