Qüdrət Tərlan oğlu Məmmədli
Bakı Dövlət Universiteti
magistrant
BÖYÜK QAFQAZIN CƏNUB YAMACINDA
QIRIŞIQ RELYEFİN ƏSAS XARAKTERİSTİKASI
QIRIŞIQ RELYEFİN ƏSAS XARAKTERİSTİKASI
Açar sözlər: Böyük Qafqaz, Böyük Qafqazın cənub yamacı, morfostruktur, qırışıq relyef, geoloji inkişaf
The main characteristics of the wrinkled relief on the southern slope of the Greater Caucasus
Summary
Like other mountainous regions of the Caucasus, the South-Eastern Caucasus is an epigeosynclinal mountain system formed by the first and middle alpine folds. Between the Alpine fold stage and the orogenic stage, the South-East Caucasus Mountains were denuded and turned into hilly, low mountain plains in the Oligocene and Miocene. Wrinkled structures were destroyed by denudation and a mostly neutral relief type was formed.
Key words: Greater Caucasus, southern slope of the Greater Caucasus, morphostructure, wrinkled relief, geological development
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