The Geosystem Analysis of Exogenesis of High-Mountain Landscapes of the Basin of the River Girdymanchay in Azerbaijan

Ilham Mardanov,Agayev Tahir

doi:10.4236/ijg.2015.611099

Abstract

For the geological systems, assessment of influencing exogenous relief forming processes having essential impact on development of landscape status arises need of development of various field and image interpretation methods for creation of scenarios of possible changes of a geo-ecological situation in various massif having harmful consequences, by identification of relationships of cause and effect. It was analyzed possibilities of prognosis of the changes of the geo-ecological situation in high-mountainous of Great Caucasus with use of the geological, geomorphologic, climate and landscape materials, data of digital processing of the photo images and visual observation. Also the possibilities of forecasting of change of landscape structure of highlands in natural area of Great Caucasus with use of various data were analyzed. It was defined the main differences of relief situation, hydro meteorological conditions in the various parts of high-mountainous geo systems in which exogenic processes were shown, character and intensity of land using which had the influence to the slope slides. These data allowed revealing the main distinctions of factors of a relief situation in which were shown exodynamic relief and landscape forming processes, character and intensity of the land use, to some extent influencing on descent of landslides and area of their destructive.

Highlights

Problems of identification of the reasons of geodynamic processes—taluses, scatterings and landslides—areHow to cite this paper: Mardanov, I. and Tahir, A. (2015) The Geosystem Analysis of Exogenesis of High-Mountain Landscapes of the Basin of the River Girdymanchay in Azerbaijan
Especially characteristic for the southern slope of Great Caucasus range lead to landslides of landslide character, in a root changing shape of a landscape of this site [4] [5]
Such sites can be subject to influence of others the exodynamic processes—to a soil erosion, accumulation and movement of taluses and the scatterings constituting not smaller danger to a landscape and all ecological situation [7] [8]

Summary

Introduction

Problems of identification of the reasons of geodynamic processes—taluses, scatterings and landslides—are. Within a mountain meadow zone steady sites in the landslide relation are characterized by existence of clearly expressed subalpine and Alpine landscapes [6] Such sites can be subject to influence of others the exodynamic processes—to a soil erosion, accumulation and movement of taluses and the scatterings constituting not smaller danger to a landscape and all ecological situation [7] [8]. It is known that an important element of development of landscapes is the transfer of chemical particles as part of circulation of substances In this regard mountain landscapes of Great Caucasus are low-studied and demand the analysis of impact of exogenous processes on changes of quantity and a ratio of various chemical elements and their connections in soils and vegetation depending on intensity of various natural phenomena

Objects and Methods of Their Researches

Conclusions

Assumed Measurement