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Mount Nemrut or Nemrud (Turkish: Nemrut Dağı; Kurdish: Çiyayê Nemrûdê; Armenian: Նեմրութ լեռ; Greek: Όρος Νεμρούτ) is a 2,134-metre-high (7,001 ft) mountain in southeastern Turkey, notable for the summit where a number of large statues are erected around what is assumed to be a royal tomb from the 1st century BC.
Armenian Highlands range across Eastern Turkey including Agri (Ararat) Taurus Mountains range across southern Turkey between the coast and the Anatolian Plateau. Subranges include Akdağlar (or White Mountains) are in the south-western; Beydağlar (or Bey Mountains) Tahtalı Mountain Range south west Anatolia
Uludağ (Turkish pronunciation:), the ancient Mysian or Bithynian Olympus (Greek: Όλυμπος), is a mountain in Bursa Province, Turkey, with an elevation of 2,543 m (8,343 ft). In Turkish, Uludağ means "great mountain".
Mount Spil (Turkish: Spil Dağı), the ancient Mount Sipylus (Ancient Greek: Σίπυλος) (elevation 1,513 m or 4,964 ft), is a mountain rich in legends and history in Manisa Province, Turkey, in what used to be the heartland of the Lydians and what is now Turkey's Aegean Region.
Tahtalı Dağı, also known as Lycian Olympus, is a mountain near Kemer, a seaside resort on the Turkish Riviera in Antalya Province, Turkey. It was known as Olympus (Ancient Greek: Ὄλυμπος; also transliterated as Olympos) and Phoenicus or Phoinikous (Ancient Greek: Φοινικοῦς) in ancient times. [1]
Mount Honaz (Turkish: Honaz Dağı), known in ancient sources as Mount Kadmos or Cadmus, is a mountain and a national park, located in southwestern Turkey, 17 km (11 mi) east of the province seat of Denizli. In the Battle of Mount Cadmus in the Middle Ages, the Seljuks defeated the French on the mountain's
Archaeologists believe they may have discovered the final location of Noah’s Ark on Turkey’s Mount Ararat. Soil samples from atop the highest peaks in Turkey reveal human activity and marine ...
Mount Mycale seen from the island of Samos, across the Mycale Strait. Western Turkey is mainly fault-block terrain, with steep-sided ridges running east–west and rivers in the rifts. The source of the faulting is the closing of Tethys Sea and the collision of the African and Arabian Plates with the Eurasian Plate .
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