Circum Troodos White Ring Cyprus Route
While climbing the high slopes of Troodos we’ve been walking on the frozen machinery of an ancient ocean. But now it’s time to step away from the mountain, slightly change our story and observe what had been happening under the sea, as the Olympus peak was rising into the sky. Leaving the cool shade of Platres behind, we approach the wine village of Omodos. The dark volcanic surfaces give way to pale rocks. Chalk breaks easily under your fingers. Hills become rounder. Valleys widen. Vineyards, orchards and white stone villages appear. The geology has shifted from fire to sediment. Encircling the Troodos massif lies a vast geological belt known as the Circum-Troodos Sedimentary Succession. It is the quiet counterpart to the violent ophiolite core. While Troodos itself formed through submarine volcanism deep beneath the Neo-Tethys Ocean, these surrounding rocks were created slowly, grain by grain, as sediments settled on the seabed around the rising mountains. For nearly eighty million years, currents carried shells, clay, volcanic fragments and microscopic marine organisms into the surrounding basin. Layer upon layer accumulated. Over time these sediments hardened into limestones, chalks, marls and sandstones that now form the foothills surrounding the Troodos range. If the ophiolite tells the story of the ocean floor, the Circum-Troodos formations tell the story of the island emerging from that…
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