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R.S.Abdullayev,\u00a0 M.F.Umudova<\/strong><\/p>\n arso2010@rambler.ru<\/p>\n Abstract<\/strong>. The modern river valley system of the Lesser Caucasus has undergone two major planning periods throughout its evolution. First – Pre-Neotectonic development. By the end of this phase in the study – the Dutch century was taken and the plan structure of the river-valley system was restored. The second is the migration in the Neotectonic stage, where the river-valley network developed over four main epochs (May\u00adkop, Sarmat, Balakhani centuries, and modern plan) and was formed as a product of joint interactions of endoge\u00adnous exogenous processes. The article discusses the his\u00adtory of the development of this system, its entire evo\u00adlu\u00adtionary period, its migration, and the importance of ap\u00adplying the results of the study.<\/p>\n Keywords<\/strong>: Geochronological periods, Neotectonic stage, River valley, Geomorphology, Lesser Caucasus<\/p>\n \u00a0<\/p>\n REFERENCES<\/b><\/p>\n \u00a0<\/p>\n Publication Date: March 1, 2021<\/p>\n Download the article<\/strong><\/p>\n \u00a0<\/p>\n","protected":false},"excerpt":{"rendered":" \u00a0 R.S.Abdullayev,\u00a0 M.F.Umudova arso2010@rambler.ru Abstract. The modern river valley system of the Lesser Caucasus has undergone two major planning periods throughout its evolution. First – Pre-Neotectonic development. By the end of this phase in the study – the Dutch century was taken and the plan structure of the river-valley system was restored. The second is […]<\/p>\n","protected":false},"author":2,"featured_media":0,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[7],"tags":[],"class_list":["post-3563","post","type-post","status-publish","format-standard","hentry","category-mqallr"],"blocksy_meta":[],"yoast_head":"\n\n