Article | Published 2020

RELIEF FORMS OF MIRZACHUL OASIS

Collection: ACADEMICIA A n I n t e r n a t i o n a l M u l t i d i s c i p l i n a r y R e s e a r c h J o u r n a l (Double Blind Refereed & Peer Reviewed Journal)
Keywords: KEYWORDS: Anticline, Bending, Depression, Erosion, Eolian, Accumulative Structures Of Relief.

Abstract

ABSTRACT The article explores the forms of relief in the Mirzachul oasis, the stages of formation of relief forms, the role of the relief component in the formation of oasis landscapes. In the operation of irrigated lands and hydraulic structures, the development of new protected lands should be monitored and all natural processes occurring in the area should be taken into account. Each of its components plays a unique role in landscape development. In landscape development, the study of their role plays an important role in the assessment of landscape development because their components are interconnected and interact together. At the end of the epoch, it rose epherogenically, but as early as the Paleogene, the southeastern part of the Central Asian region began to fill up again below sea level due to subsequent bending, and included a shallow coastal basin or lagoon-type basin. Marine transgression lasted until the Lower Oligocene.

References

  1. 10.5958/2249-7137.2020.01299.9
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