Zlatitsa–Pirdop Valley
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Zlatitsa–Pirdop Valley
Zlatitsa–Pirdop Valley () is situated in central western Bulgaria and is the fifth of the eleven Sub-Balkan valleys in direction west–east. It is named after the two towns that lie within, Zlatitsa and Pirdop. The valley is an important hub of the Bulgarian copper and gold mining and processing industry. It contains numerous natural and architectural landmarks, including the ruins of the late Roman Elenska Basilica. Geography The valley is enclosed between the Etropole and Zlatitsa–Teteven divisions of the Balkan Mountains to the north and the Sredna Gora mountain range to the south and southwest. To the west the Galabets ridge (925 m) separates it from the Kamarska Valley and to the east the Koznitsa ridge (1,092 m) separates it from the Karlovo Valley. The valley spans a territory of 120 km2. It reaches a maximum length of 36 km from west to east; its width varies between 3 and 8 km. The average altitude is 750 m. Zlatitsa–Pirdop Valley ...
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Valley
A valley is an elongated low area often running between hills or mountains and typically containing a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In areas of limestone bedrock, dry valleys may also result from drainage now taking place underground rather than at the surface. Rift valleys arise principally from earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms that may be global in use or else applied only locally ...
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