Exomorphogenesis of cosmogenic ring structures of Kazakhstan
AbstractExogenous processes transform the relief of the identified cosmogenic structures within the plainsof Turan, the Kazakh melkosopochnik and the mountains of South-East Kazakhstan generally. Themain determining indicator features of cosmogenic structures are geomorphological, geological, andstructural-tectonic. The degree of change in the initial crater relief depends on the time of formationof cosmogenic structures and the physical and geographical conditions of the territories. Within themeteorite craters, the zonality of the development of the processes of exomorphogenesis is clearlyexpressed. As a result, the study found that the development of exomorphogenesis in cosmogenicring structures, as well as in natural mountain systems, corresponds to the law of altitude zonality. Themain processes of exomorphogenesis of meteorite craters in the arid zone of Kazakhstan are fluvialprocesses. The main modern processes include gravity-slope processes, surface flushing, gully andriver erosion, processes of complex accumulation.
How to Cite
ВЕСЕЛОВА, Л. К.. Exomorphogenesis of cosmogenic ring structures of Kazakhstan. Journal of Geography and Environmental Management, [S.l.], v. 50, n. 3, p. 4-10, oct. 2018. ISSN 1563-0234. Available at: <http://bulletin-geography.kaznu.kz/index.php/1-geo/article/view/522>. Date accessed: 19 oct. 2018.
Physical, economic and social geography