Published October 2023, Pg. 4-9

Section: Geology and geophysics

UOT: 550: 622.276 (479.24)

DOI: 10.37474/0365-8554/2023-10-4-9

Hydrgeoological characteristics of underground waters of the southwest slope of the Great Caucasus

S.Sh. Salakhov Cand. in Geol.-Min.Sc. - National Service of Geological Survey, Ministry of Ecology and Natural Resources

Sh.S. Salakhov - Azerbaijan State University of Oil and Industry

Keywords:  
hydrography
quarternary deposits
level
groundwater
rock
slope
a discharge
sediments

Southwest flank of the Great Caucasus is very difficult on tectonic, geomorphological, stratigraphic, lithological and to other features. Hydrogeological conditions of investigated region are very diverse. Underground waters are formed in separate structure.
Paleogene, Neogene and Quaternary sediments are involved in the geological structure of the study area. There are 5 anticline zones in the Acinohur structure, which includes 31 anticline rises. These anticlines are either independent wrinkles or combined at the axis of the wrinkle. They are
Dashyuz, Kudbarakdag, Acinohur-Khoshavand, Kodjashen-Goychay and Garaja-Garamaryam.

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