Abstract
Caucasian Copper Age
The Caucasus region is dominated by the Caucasus mountains themselves. The Caucasian ridge is a main watershed, which divides the Caucasus into the two parts: northern and southern (or Transcaucasia). Owing to the natural conditions, the Caucasus is divided also into the West and East Caucasus. The former includes the Black sea and Azov sea basins, and the latter the Caspian sea basin. Altitude of the Caucasus varies between 28 m below sea level and 5,642 m above sea level. Over one half of this region is occupied by highlands and mountainous plateaus. The mountains are volcanic in origin and are rich in flint, ores (including copper and gold), and minerals. The South Caucasus is very rich in obsidian. Rivers, draining mountain runoff, create rich alluvial plains to the north and south of the main ranges.
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Chataigner, Christine (1995). La Transcaucasie au Neolithique et au Chalcolithique. Oxford: BAR International Series G24.
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Kiguradze, T. (2001). Caucasian Chalcolithic. In: Peregrine, P.N., Ember, M. (eds) Encyclopedia of Prehistory. Springer, Boston, MA. https://doi.org/10.1007/978-1-4615-1187-8_5
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DOI: https://doi.org/10.1007/978-1-4615-1187-8_5
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