Ministry of Communications and Works Department of Antiquities Nicosia
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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. Some 600 m below Malounda Bridge. This sites provides an excellent example of how seafloor spreading takes place with dyke swarms showing dyke-indyke intrusion between lava screens.