Troodos Mountains Biodiversity and Climate Core
The Troodos Mountains rise from the heart of Cyprus as the island’s highest mountain system, with Mount Olympus reaching 1,952 meters above sea level. More than a scenic landscape, this mountain range forms the ecological and climatic core of the island. Its slopes regulate water supply, shape weather patterns, and support an extraordinary concentration of life found nowhere else in the Mediterranean. What makes Troodos truly exceptional is its geological origin. The mountains expose one of the most complete sections of ancient oceanic crust ever discovered on land, creating conditions that shaped a unique and fragile ecosystem over millions of years. britannica-com Historical Background The Troodos Mountains formed approximately 92 million years ago at the bottom of the ancient Tethys Ocean, nearly 8,000 meters below the sea surface. Molten rock from the Earth’s mantle rose through fractures in the ocean floor, solidifying into layers of basalt, gabbro, and peridotite. When the African and Eurasian tectonic plates collided, this section of oceanic crust was pushed upward rather than sinking back into the mantle. Geologists describe this phenomenon as an ophiolite complex, and Troodos represents the best preserved and most accessible example in the world. chooseyourcyprus-com Uplift began around 20 million years ago, with Mount Olympus at its center. Over time, erosion stripped away upper layers and exposed deeper geological formations normally…
Read more