Study of the Geological Structure of the Jabrayil Foothills

Авторы

  • 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

Ключевые слова:

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

Аннотация

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.

Загрузки

Опубликован

2023-06-30

Как цитировать

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

Выпуск

Том 15 № 2 (2023)

Раздел

Articles

Лицензия

Лицензия Creative Commons

Это произведение доступно по лицензии Creative Commons «Attribution-NonCommercial» («Атрибуция — Некоммерческое использование») 4.0 Всемирная.

Похожие статьи

1 2 3 4 > >> 

Вы также можете начать расширеннвй поиск похожих статей для этой статьи.