Ophiolite complex

Ophiolite Complex

The Ophiolite complex is a significant geological formation found in Cyprus. It consists of oceanic crust and upper mantle rocks that have been uplifted and exposed above sea level. This complex provides valuable insights into the Earth's geological history.

Formation of the Ophiolite Complex

The Ophiolite complex in Cyprus formed around 90 million years ago. It resulted from the collision of tectonic plates, which caused oceanic crust to be thrust onto the continental crust. This process is known as obduction.

Troodos Ophiolite

The most famous Ophiolite complex in Cyprus is the Troodos Ophiolite. It covers a large part of the island and is one of the best-preserved ophiolites in the world. The Troodos Ophiolite includes various rock types such as basalt, gabbro, and peridotite.

Geological Importance

The Ophiolite complex is crucial for understanding plate tectonics and the formation of oceanic crust. It offers a rare opportunity to study deep-sea geological processes on land. Geologists from around the world visit Cyprus to examine the Troodos Ophiolite.

Economic Significance

The Ophiolite complex in Cyprus also has economic importance. It contains valuable minerals such as chromite and copper. These resources have been mined for centuries and continue to contribute to the local economy.

Visiting the Ophiolite Complex

Tourists can explore the Ophiolite complex by visiting the Troodos Mountains. There are several hiking trails and geological sites that offer a glimpse into this fascinating geological formation. The area is also known for its natural beauty and biodiversity.