Syllogistic comparison of morphological levels of miniature model of groundwater aquifer with seams and gaps in the Yazd field

Abstract

Although the natural movements of the earth's crust have been noteworthy by the researchers from long time ago, but human power has had results in the Environmental, Widespread and profound changes which has been unbelievably appeared in different forms. As an example of such a process, it can be mentioned the slow sinking which are known as subsidence. Subsidence is one of the morphological phenomenon on which a part of earth's crust gradually is subsided. In other words, the regional subsidence of earth's surface includes the collapse toward the lower earth's surface which can be also included a little horizontal shift. It is said that some gaps are appeared by this subsidence which are called “SHAGH" in localism. The goal of this research which is from an empirical research in Esfahan University is more focus on the presented views which are about the mechanism and the reason of developing of the morphological results of the subsidence phenomenon. It was tried to explain the syllogistic comparison of Morphological levels of miniature model of groundwater aquifer with seams and gaps in the Yazd field depending on model behavior. The results showed that the subsidences which are result from the excessive water-laden from the groundwater aquifer are very little and cannot create a subsidence on the field surface. The superficial morphological change in minimized static model differs from the Yazd field and it shows the difference in the origin of this phenomenon © 2014 AENSI Publisher All rights reserved.