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Troodos (sometimes spelled Troödos; Greek: Τρόοδος [ˈtɾo.oðos]; Turkish: Trodos Dağları) is the largest mountain range in Cyprus, located in roughly the center of the island. Its highest peak is Mount Olympus (Greek: Όλυμπος), also known as Chionistra (Greek: Χιονίστρα), at 1,952 metres (6,404 ft), which hosts the Sun Valley and North Face ski areas with their five ski lifts.

The Troodos mountain range stretches across most of the western side of Cyprus. There are many mountain resorts, Byzantine monasteries, and churches on mountain peaks, and nestling in its valleys and mountains are villages clinging to terraced hills. The area has been known since antiquity for its mines, which for centuries supplied copper to the entire Mediterranean. In the Byzantine period it became a centre of Byzantine art, as churches and monasteries[1] were built in the mountains, away from the threatened coastline. The mountains are also home to RAF Troodos, a listening post for the NSA and GCHQ.[2]

The name Troodos probably comes from one of two sources: either τρία + ὁδός (tría + hodós), referring to the three roads that lead to the mountain, or τό + ὄρος + Ἄδος (to + oro + Ados), meaning the mountains of Adonis.[3][4]

Kykkos monastery

Painted Churches in the Troodos Region - UNESCO World Heritage

Archangelos Michail, Pedoulas | Panagia tis Podithou, Galata | Panagia tis Asinou, oder Panagia tis Forviotissas | Agiou Ioanni tou Lampadisti, Kalopanagiotis (Monastery)| Timiou Stavrou tou Agiasmati , Platanistasa | Timiou Stavrou, Pelentri | Panagia tou Moutoulla | Metamorfoseos Sotira (Agia Sotira), Palaichori | Panagia tou Arakos, Lagoudera | Agiou Nikolaou tis Stegis, Kakopetria


Troodos Mountains

The Troodos Mountains are known worldwide for their geology and the presence of an undisturbed ophiolite sequence, the Troodos Ophiolite. These mountains slowly rose from the sea due to the collision of the African and European tectonic plates, a process that eventually formed the island of Cyprus. The slowing and near-cessation of this process left the rock formations nearly intact, while subsequent erosion uncovered the magma chamber underneath the mountain, allowing a viewing of intact rocks and petrified pillow lava formed millions of years ago, an excellent example of ophiolite stratigraphy. The observations of the Troodos ophiolite by Ian Graham Gass and co-workers was one of the key points that led to the theory of sea floor spreading.

During the second half of 20th century most young people have the left the villages in the mountains, but efforts have been made to establish the region as a tourist resort.

Kykkos monastery, established end of 11th century by Isaias.

Troodos Mountains (Source)

Mesa Potamos

Troodos Mountains, Limassol District,

Villages of Troodos (selection)

Troodos Churches

References

"Cyprus Travel Series: Troodos Mountains". Expand Your Property World. 2017-11-23. Retrieved 2018-02-16.
Cora Currier; Henrik Moltke (January 29, 2016). "Spies in the sky". The Intercept.
"Places to visit - Troodos Cyprus". www.justaboutcyprus.com. Retrieved 2017-09-18.
"Snowy Mountains of Troodos - December at Olympos - Chionistra". www.cyprusalive.com. Retrieved 2017-09-18.
"Climatological and Meteorological Reports - Prodromos - 1991 - 2005" (PDF). Archived from the original (pdf) on 2016-03-27. Retrieved 2017-06-29.

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