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The Caucasian isthmus lies between the Black (Azov) and Caspian Seas. Its area comprises four main morphological and tectonic units: (1) the Ciscaucasian Plain and Platform, including the foredeeps of the Greater Caucasus; (2) the Great Caucasus itself; 3) Northern Transcaucasian system of intermontane basins, divided by the Okriba-Dzirula Uplift; and (4) the Lesser Caucasus (Caucasus Minor). In contrast to the Greater Caucasus, stretching in an WNW-ESE direction from the Black Sea shore to the Caspian shore, the Lesser Caucasus has an arcuate N-convex shape and no distinct boundaries on either side: it merges with the Anatolian Upland in the W and with the Iranian Upland in the SE and is the most heterogeneous unit of the whole Caucasus region (Fig. 97).

Fig. 97
figure 1_1-4020-4495-X_19

Tectonic scheme of the Caucasus

1, Archean and Lower Proterozoic crystalline rocks, overlapped by the cover; 2, Scythian Platform (S part); 3, Scythian Platform (N part, the Karpinsky ‘Ridge’); 4, Late Cenozoic molasse of the...

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© 1997 Chapman & Hall

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Khain, V.E., Koronousky, N.V. (1997). Caucasus. In: Encyclopedia of European and Asian Regional Geology. Encyclopedia of Earth Science. Springer, Dordrecht. https://doi.org/10.1007/1-4020-4495-X_19

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  • DOI: https://doi.org/10.1007/1-4020-4495-X_19

  • Publisher Name: Springer, Dordrecht

  • Print ISBN: 978-0-412-74040-4

  • Online ISBN: 978-1-4020-4495-3

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