In Famagusta.
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.'
Source: fortnightlyreview.co.uk