Rhodopes

The Rhodopes (; bg, Родопи, ; el, Ροδόπη, ''Rodopi''; tr, Rodoplar) are a mountain range in Southeastern Europe, and the largest by area in Bulgaria, with over 83% of its area in the southern part of the country and the remainder in Greece. Golyam Perelik is its highest peak at . The mountain range gives its name to the terrestrial ecoregion Rodope montane mixed forests that belongs in the temperate broadleaf and mixed forests biome and the Palearctic realm. The region is particularly notable for its karst areas with their deep river gorges, large caves and specific sculptured forms, such as the Trigrad Gorge.

A significant part of Bulgaria's hydropower resources are located in the western areas of the range. There are a number of hydro-cascades and dams used for electricity production, irrigation, and as tourist destinations. In Greece, there are also the hydroelectric power plants of Thisavros and Platanovrysi. The Rhodopes have a rich cultural heritage including ancient Thracian sites such as Perperikon, Tatul and Belintash, and medieval castles, churches, monasteries, and picturesque villages with traditional Bulgarian architecture from the 18th and 19th centuries.

Name and mythology

The name of the Rhodope Mountains is of Thracian origin. Rhod-ope (Род-oпа) is interpreted as the first name of a river, meaning "rusty/reddish river", where ''Rhod-'' has the same Indo-European root as the Bulgarian "руда" (ore, "ruda"), "ръжда" (rust, "rǎžda"), "риж" (red-haired, "riž"), Latin "rufus" (red), German "rot" (red), English "red", Greek ροδ- (rodh).

In Greek mythology, Queen Rhodope of Thrace, the wife of King Haemus of Thrace, offended the gods, and was changed into a mountain by Zeus and Hera as a punishment along with her husband.

The mountains are also associated with the mythic figure of Orpheus.

In the Middle Ages, the mountains were known as the Slavey Mountains (Slaveyev Mountains), and under Ottoman rule were known as the Dospatsky Mountains, after the Dospat Municipality and Dospat River.

Geography

In geomorphological terms, the Rhodopes are part of the Rila-Rhodope massif, which is the oldest landmass on the Balkan peninsula. The Rhodopes are spread over , of which are on Bulgarian territory. They have the greatest extent of any single mountain range in Bulgaria. The mountains are about long and about wide, with an average altitude of . To the north the mountain slopes descend steeply towards the Upper Thracian Plain. To the west, the Rhodopes reach the Avram saddle, Yundola and the valley of the Mesta River. To the south and east they extend to the coastal plains of Greek Thrace. The Rhodopes are a complex system of ridges and deep river valleys.

Fifteen reserves have been established in the region, some of which are under UNESCO protection. The mountains are famous for the largest coniferous woods in the Balkans, their mild relief and the lush vegetation in the western parts as well as the abundance of birds of prey in the eastern areas.

Climate

The location of the Rhodopes in the southeastern part of the Balkan Peninsula largely determines the climate in the region. It is influenced both by the colder air coming from the north and by the warmer breeze from the Mediterranean.

The average annual temperature in the Eastern Rhodopes is , the maximum precipitation is in December, the minimum in August. In the Western Rhodopes, the temperature varies from and in the summer rainfalls prevail.

The mild climate, combined with some other factors, works in favour of the development of recreation and tourist activities. The Pamporovo resort, where the microclimate permits a heavy snow cover to be preserved for a long time, is an excellent example.

Temperatures as low as are common in winter, and due to this the Rhodopes are the southernmost place in the Balkans where tree species such as the Norway Spruce and the Silver Birch can be found.

Waters

The mountains have abundant water reserves, with a dense network of mountain springs and rivers. Nearly 80% of the mountain's territory falls within the drainage of the river Maritsa

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