Study of the Geological Structure of the Jabrayil Foothills

Authors

  • S.B. Mammadova Azerbaijan State University of Oil and Industry (Azadlig Ave., 16/21, AZ1010, Baku, Azerbaijan)
  • E.N. Jafarova Azerbaijan State University of Oil and Industry (Azadlig Ave., 16/21, AZ1010, Baku, Azerbaijan)

DOI:

https://doi.org/10.52171/2076-0515_2023_15_02_116_12

Keywords:

climate, weather, mezakaynazoy, sediments, clay, structure, area, clays

Abstract

The article is devoted to the study of the geological structure of the Jabrayil foothills. The Jabrayil foothill plain is located in the southern part of the Republic of Azerbaijan. Climatic conditions are very different in the area. The average annual temperature varies from 10° to 13° C. The amount of atmospheric sediments is unevenly distributed throughout the area. Most sediments occur in the form of rain. The soil cover in the study area is mountain chestnut. Mesacaine sediments are involved in the structure of the study area. The lithological area consists of river stones-gravel, clay and clays.

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Published

2023-06-30

How to Cite

Mammadova, S., & Jafarova, E. (2023). Study of the Geological Structure of the Jabrayil Foothills. Herald of Azerbaijan Engineering Academy, 15(2), 116–121. https://doi.org/10.52171/2076-0515_2023_15_02_116_12

Issue

Vol. 15 No. 2 (2023)

Section

Articles

License

Creative Commons License

This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License.