{"id":20,"date":"2019-03-16T11:04:03","date_gmt":"2019-03-16T11:04:03","guid":{"rendered":"http:\/\/journal.geonatres.az\/?p=20"},"modified":"2019-07-23T22:50:26","modified_gmt":"2019-07-23T18:50:26","slug":"meqale-3","status":"publish","type":"post","link":"https:\/\/journal.geonatres.az\/en\/meqale-3\/","title":{"rendered":"INFLUENCE OF THE RELIEF FACTOR ON THE ECOGEOMORPHOLOGICAL CONDITIONS OF THE TALYSH MOUNTAIN REGION"},"content":{"rendered":"<div>\n<p style=\"text-align: justify;\"><span style=\"font-family: 'times new roman', times, serif;\"><strong>H.A.Khalilov, M.G.Almammadli<\/strong><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-family: 'times new roman', times, serif;\">mesudaz@mail.ru<\/span><\/p>\n<p class=\"section-title u-h3 u-margin-l-top u-margin-xs-bottom\" style=\"text-align: justify;\"><span style=\"font-family: 'times new roman', times, serif;\"><strong>Abstract.\u00a0<\/strong>As in all mountain geomorphic systems of the Earth in the formation of ecogeomorphological conditions of the Talysh mountain region, a significant role is played by the relief, which in the complex of natural and an\u00adthropogenic factors constitutes the main component. At the same time, each of the relief factors and the mor\u00adpho\u00adstructures and morphosculptures that complicate it are characterized by their inherent specific effects, both sta\u00adtic (lithologic-petrographic, structural, hypsometric, morphological, morphometric) and dynamic (endoge\u00adnous and exogenous processes and phenomena of geo\u00admorphogenesis). Consequently, a purposeful considera\u00adtion and a comprehensive analysis of these factors have wide possibilities in forming the necessary ideas for studying the ecogeomorphological conditions of the investigated territory and establishing the features of their evolution in the future.<\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-family: 'times new roman', times, serif;\"><strong>REFERENCES<\/strong><\/span><\/p>\n<ol style=\"text-align: justify;\">\n<li><span style=\"font-family: 'times new roman', times, serif;\">\u018flizad\u0259 E.K., Tanr\u0131verdiyev X,K., X\u0259lilov H.A. v\u0259 s. Geomorfoloji rayonla\u015fd\u0131rma . Az\u0259rbaycan Respublikas\u0131n\u0131n co\u011frafiyas\u0131. I cild, Fiziki co\u011frafiya. Ba\u00adk\u0131, 2014, s. 127-132.<\/span><\/li>\n<li><span style=\"font-family: 'times new roman', times, serif;\">\u018flizad\u0259 E.K., Taxiraz\u0259r S.\u018f., Quliyeva S.Y. L\u0259nk\u0259ran vilay\u0259ti. Az\u0259rbaycan Respublikas\u0131n\u0131n co\u011f\u00adrafiyas\u0131. I cild, Fiziki co\u011frafiya. Bak\u0131, 2014, s.495-499.<\/span><\/li>\n<li><span style=\"font-family: 'times new roman', times, serif;\">X\u0259lilov H.A. Tal\u0131\u015f da\u011fl\u0131q sistemind\u0259 relyefin m\u00fchit\u0259m\u0259l\u0259g\u0259tirici funksiyas\u0131 haqq\u0131nda (t\u0259dqiqat\u0131n eko\u00adgeomorfoloji aspekti) \/\/ AMEA X\u0259b\u0259rl\u0259ri, Yer elml\u0259ri, N2, 2010, s. 24-27.<\/span><\/li>\n<li><span style=\"font-family: 'times new roman', times, serif;\">A\u0433ecc P. \u041a\u043b\u044e\u0447\u0438 \u043a \u044d\u043a\u043e\u043b\u043e\u0433\u0438\u0438. \u0413\u0438\u0434\u0440\u043e\u043c\u0435\u0442\u0435\u00ad\u043e\u00ad\u0438\u0437\u0434\u0430\u0442. \u041b\u0435\u043d\u0438\u043d\u0433\u0440\u0430\u0434, 1982. 96\u0441.<\/span><\/li>\n<li><span style=\"font-family: 'times new roman', times, serif;\">\u0411\u0443\u0434\u0430\u0433\u043e\u0432 \u0411.\u0410. \u041e\u0441\u043d\u043e\u0432\u043d\u044b\u0435 \u0433\u0435\u043e\u0433\u0440\u0430\u0444\u0438\u0447\u0435\u0441\u043a\u0438\u0435 \u043f\u0440\u043e\u0431\u043b\u0435\u043c\u044b \u044d\u043a\u043e\u043b\u043e\u0433\u0438\u0447\u0435\u0441\u043a\u0438\u0445 \u0441\u0431\u0430\u043b\u0430\u043d\u0441\u0438\u0440\u043e\u0432\u0430\u043d\u043d\u043e\u0433\u043e \u0440\u0430\u0437\u0432\u0438\u00ad\u0442\u0438\u044f \u0410\u0437\u0435\u0440\u0431\u0430\u0439\u0434\u0436\u0430\u043d\u0441\u043a\u043e\u0439 \u0420\u0435\u0441\u043f\u0443\u0431\u043b\u0438\u043a\u0438\/\/ \u0412\u0435\u0441\u0442\u0438 \u0411\u0430\u043a\u0438\u043d\u00ad\u0441\u043a\u043e\u0433\u043e \u0443\u043d\u0438\u0432\u0435\u0440\u0441\u0438\u0442\u0435\u0442\u0430. \u0421\u0435\u0440. \u0415\u0441\u0442\u0435\u0441\u0442\u0432\u0435\u043d\u043d\u044b\u0445 \u043d\u0430\u0443\u043a. N- 1, 1999, \u0441.164-188.<\/span><\/li>\n<li><span style=\"font-family: 'times new roman', times, serif;\">\u041a\u0435\u043d\u0433\u0435\u0440\u043b\u0438 \u0422.\u041d. \u0422\u0435\u043a\u0442\u043e\u043d\u0438\u0447\u0435\u0441\u043a\u043e\u0435 \u0440\u0430\u0439\u043e\u043d\u0438\u0440\u043e\u0432\u0430\u00ad\u043d\u0438\u0435, \u0412\u043a\u043d.: \u0413\u0435\u043e\u043b\u043e\u0433\u0438\u044f \u0410\u0437\u0435\u0440\u0431\u0430\u0439\u0434\u0436\u0430\u043d\u0430, \u0442\u043e\u043c IV, \u0422\u0435\u043a\u00ad\u0442\u043e\u00ad\u043d\u0438\u043a\u0430, \u0411\u0430\u043a\u0443, 2005, \u0441.32-42.<\/span><\/li>\n<li><span style=\"font-family: 'times new roman', times, serif;\">\u0420\u0443\u0441\u0442\u0430\u043c\u043e\u0432 \u041c.\u0418. \u042e\u0436\u043d\u043e\u043a\u0430\u0441\u043f\u0438\u0439\u0441\u043a\u0438\u0439 \u0431\u0430\u0441\u0441\u0435\u0439\u043d-\u0433\u0435\u043e\u0434\u0438\u043d\u0430\u043c\u0438\u0447\u0435\u0441\u043a\u0438\u0435 \u0441\u043e\u0431\u044b\u0442\u0438\u044f \u0438 \u043f\u0440\u043e\u0446\u0435\u0441\u0441\u044b, \u0411\u0430\u043a\u0443, 2005, 345\u0441.<\/span><\/li>\n<li><span style=\"font-family: 'times new roman', times, serif;\">\u0425\u0430\u043b\u0438\u043b\u043e\u0432 \u0413.\u0410. \u042d\u043a\u043e\u043b\u043e\u0433\u0438\u0447\u0435\u0441\u043a\u0430\u044f \u0433\u0435\u043e\u043c\u043e\u0440\u0444\u043e\u043b\u043e\u00ad\u0433\u0438\u044f \u0438 \u0438\u043d\u0442\u0435\u0433\u0440\u0430\u0446\u0438\u044f \u043d\u0430\u0443\u043a\/\/ \u0412\u0435\u0441\u0442\u043d\u0438\u043a \u0411\u0430\u043a\u0438\u043d\u0441\u043a\u043e\u0433\u043e \u0443\u043d\u0438\u00ad\u0432\u0435\u0440\u0441\u0438\u0442\u0435\u0442\u0430, \u0441\u0435\u0440. \u0435\u0441\u0442\u0435\u0441\u0442\u0432. \u043d\u0430\u0443\u043a. 2002, N1, \u0441.210-215.<\/span><\/li>\n<\/ol>\n<\/div>\n<div style=\"text-align: justify;\"><a href=\"http:\/\/journal.geonatres.az\/wp-content\/uploads\/2019\/03\/H.X\u0259lilov-2018.pdf\"><strong>Download the article<\/strong><\/a><\/div>\n","protected":false},"excerpt":{"rendered":"<p>H.A.Khalilov, M.G.Almammadli mesudaz@mail.ru Abstract.\u00a0As in all mountain geomorphic systems of the Earth in the formation of ecogeomorphological conditions of the Talysh mountain region, a significant role is played by the relief, which in the complex of natural and an\u00adthropogenic factors constitutes the main component. At the same time, each of the relief factors and the [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":87,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[2],"tags":[],"class_list":["post-20","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-article"],"blocksy_meta":[],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.3 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>INFLUENCE OF THE RELIEF FACTOR ON THE ECOGEOMORPHOLOGICAL CONDITIONS OF THE TALYSH MOUNTAIN REGION<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/journal.geonatres.az\/en\/meqale-3\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:locale:alternate\" content=\"az\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"INFLUENCE OF THE RELIEF FACTOR ON THE ECOGEOMORPHOLOGICAL CONDITIONS OF THE TALYSH MOUNTAIN REGION\" \/>\n<meta property=\"og:description\" content=\"H.A.Khalilov, M.G.Almammadli mesudaz@mail.ru Abstract.\u00a0As in all mountain geomorphic systems of the Earth in the formation of ecogeomorphological conditions of the Talysh mountain region, a significant role is played by the relief, which in the complex of natural and an\u00adthropogenic factors constitutes the main component. 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At the same time, each of the relief factors and the [&hellip;]","og_url":"https:\/\/journal.geonatres.az\/en\/meqale-3\/","og_site_name":"Geography and Natural Resources","article_published_time":"2019-03-16T11:04:03+00:00","article_modified_time":"2019-07-23T18:50:26+00:00","og_image":[{"width":740,"height":1024,"url":"https:\/\/journal.geonatres.az\/wp-content\/uploads\/2019\/03\/JUrnal2019-740x1024.jpg","type":"image\/jpeg"}],"author":"admin","twitter_card":"summary_large_image","twitter_misc":{"Written by":"admin","Est. reading time":"3 minutes"},"schema":{"@context":"https:\/\/schema.org","@graph":[{"@type":"Article","@id":"https:\/\/journal.geonatres.az\/meqale-3\/#article","isPartOf":{"@id":"https:\/\/journal.geonatres.az\/meqale-3\/"},"author":{"name":"admin","@id":"https:\/\/journal.geonatres.az\/#\/schema\/person\/c46617384b2f64f0590d9621c932863c"},"headline":"INFLUENCE OF THE RELIEF FACTOR ON THE ECOGEOMORPHOLOGICAL CONDITIONS OF THE TALYSH MOUNTAIN 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