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Jonathan Gorvett: 'The ultimate Cyprob ‘beginning’ can even be Mesozoic. While ‘Turkish’ north of Cyprus is dominated by jagged, igneous uplift – really part of the ‘Turkish’ Anatolian mainland, forty odd miles away to the north – the ‘Greek’ south’s Troodos range is a more worn-down ophiolite, its rock, mud and shale mass long separated from the northern peaks by a shallow sea – today’s plain of Mesaoria, onto which Famagusta now backs.'

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