Khandria
CyprusMinistry of Communications and Works Department of Antiquities Nicosia
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Description
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. Still deeper into the oceanic crust (layer 2b) this is a most clear example of magmatic processes at this level and a demonstration of the existence of small multiple magma chambers at spreading, ridges.