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Finding a date with Mingle2 has never been simpler.The regional geology of the area concerned may influence the nature of any uplift, including features such as the relative competency of lithologies and inherited structure.The likely cause of the uplift of the Troodos Massif was the collision of the Eratosthenes Seamount, a large crustal edifice, with the Cyprus active margin, related to a northward-dipping subduction zone.Previous studies have suggested that the Kyrenia Range is of relatively recent origin (Ducloz 1972; Baroz 1979) but the detailed timing and processes involved remained elusive.The new data show that the Kyrenia Range was uplifted contemporaneously with the Troodos Massif in southern Cyprus.Plus as a green user, you cannot get banned by a Knight.

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The uplift of the Kyrenia Range appears to have been significantly faster than that affecting other comparable regions in the easternmost Mediterranean during the Pleistocene (e.g.

The driving mechanism for the uplift of both the Kyrenia Range and the Troodos Massif is inferred to be the collision of the Eratosthenes Seamount with the Cyprus trench to the south of Cyprus.

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New evidence for the uplift is presented here in relation to adjacent areas and alternative interpretations are discussed in their regional context.

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