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{"id":2666,"date":"2020-12-06T12:49:04","date_gmt":"2020-12-06T09:49:04","guid":{"rendered":"http:\/\/www.debrisflow.ru\/?page_id=2666"},"modified":"2024-09-30T08:48:31","modified_gmt":"2024-09-30T05:48:31","slug":"df20_proceedings_v1","status":"publish","type":"page","link":"https:\/\/www.debrisflow.ru\/en\/df18\/df20_proceedings_v1\/","title":{"rendered":"\u0421\u0431\u043e\u0440\u043d\u0438\u043a \u0442\u0440\u0443\u0434\u043e\u0432 \u043a\u043e\u043d\u0444\u0435\u0440\u0435\u043d\u0446\u0438\u0438"},"content":{"rendered":"\n<p><\/p>\n\n\n<div class=\"wp-block-image\">\n<figure class=\"aligncenter size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"239\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/07\/\u0432\u0435\u0440\u0445\u043d\u044f\u044f-\u043f\u043b\u0430\u0448\u043a\u0430_eng_\u043e\u0431\u043d\u043e\u0432\u043b\u0435\u043d\u043d\u044b\u0435-\u0434\u0430\u0442\u044b-1024x239.jpg\" alt=\"\" class=\"wp-image-2541\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/07\/\u0432\u0435\u0440\u0445\u043d\u044f\u044f-\u043f\u043b\u0430\u0448\u043a\u0430_eng_\u043e\u0431\u043d\u043e\u0432\u043b\u0435\u043d\u043d\u044b\u0435-\u0434\u0430\u0442\u044b-1024x239.jpg 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/07\/\u0432\u0435\u0440\u0445\u043d\u044f\u044f-\u043f\u043b\u0430\u0448\u043a\u0430_eng_\u043e\u0431\u043d\u043e\u0432\u043b\u0435\u043d\u043d\u044b\u0435-\u0434\u0430\u0442\u044b-300x70.jpg 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/07\/\u0432\u0435\u0440\u0445\u043d\u044f\u044f-\u043f\u043b\u0430\u0448\u043a\u0430_eng_\u043e\u0431\u043d\u043e\u0432\u043b\u0435\u043d\u043d\u044b\u0435-\u0434\u0430\u0442\u044b-768x179.jpg 768w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/07\/\u0432\u0435\u0440\u0445\u043d\u044f\u044f-\u043f\u043b\u0430\u0448\u043a\u0430_eng_\u043e\u0431\u043d\u043e\u0432\u043b\u0435\u043d\u043d\u044b\u0435-\u0434\u0430\u0442\u044b-1536x358.jpg 1536w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/07\/\u0432\u0435\u0440\u0445\u043d\u044f\u044f-\u043f\u043b\u0430\u0448\u043a\u0430_eng_\u043e\u0431\u043d\u043e\u0432\u043b\u0435\u043d\u043d\u044b\u0435-\u0434\u0430\u0442\u044b-2048x477.jpg 2048w\" sizes=\"auto, (max-width: 1024px) 100vw, 1024px\" \/><\/figure>\n<\/div>\n\n\n<p><\/p>\n\n\n<h2 style=\"text-align: center;\">Proceedings of the Conference<\/h2>\n<p style=\"text-align: center;\"><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/TitlePage_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter wp-image-2667 \" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/TitlePage_DF20-pdf.jpg\" alt=\"\" width=\"194\" height=\"275\" \/><\/a><\/p>\n<p><strong>Debris Flows: Disasters, Risk, Forecast, Protection. <\/strong>Proceedings of the 6th International Conference (Dushanbe\u2013Khorog, Tajikistan). Volume 1. \u2013 Ed. by S.S. Chernomorets, K.S. Viskhadzhieva. \u2013 Dushanbe: \u201cPromotion\u201d LLC, 2020, 610 p.<br \/>ISBN 978-99975-309-4-3<br \/><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/DF20_Proceedings_Vol_1.pdf\">Full text of the book (Volume 1)<\/a><\/p>\n<h2 style=\"text-align: center;\">Table of contents<\/h2>\n<table width=\"665\">\n<tbody>\n<tr>\n<td width=\"735\"><strong>Preface<\/strong><\/td>\n<td style=\"text-align: center;\" width=\"84\">vii<\/td>\n<td width=\"64\"><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Preface_DF20_1.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td>Risk and consequences of high-mountain lake outbursts in Tajikistan<br \/><strong>U.R. Pirmamadov, R.A. Bobov, Yu.Kh. Raimbekov,<br \/>F.O. Marodaseinov, I.I. Zikillobekov, S.S. Chernomorets,<br \/>E.A. Savernyuk, V.M. Kidyaeva, <\/strong><strong>I.V. Krylenko, I.N. \u041arylenko,<br \/>K.S. Viskhadzhieva<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">1<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Pirmamadov1_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td>Tailings dams &#8211; facilities of increased debris-flow hazard<br \/><strong>M.D. Dokukin, E.V. Zaporozhchenko, D.V. Znamensky<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">25<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Dokukin1_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">System of the debris flow protection in the Zailiyskiy Alatau range<br \/><strong>A.R. Medeu, V.P. Blagovechshenskiy, S.U. Ranova, N.E. Kasatkin, M.K. Kasenov, Zh.T. Raymbekova<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">39<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Medeu_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Debris flow hazard for the transportation network in the Eastern Siberia and the Russian Far East<br \/><strong>A.L. Shnyparkov, A.S. Turchaninova, T.I. Khismatullin,<br \/>S.A. Sokratov<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">49<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Shnyparkov1_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Debris flow risk for transportation network in the Eastern Siberia and the Russian Far East in the middle of the XXI century<br \/><strong>A.L. Shnyparkov, A.S. Turchaninova, T.I. Khismatullin,<br \/>S.A. Sokratov<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">60<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Shnyparkov2_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Assessments on debris flow distribution, triggering and evolution in the Dolomites area (North-Eastern Italy)<br \/><strong>P.R. Tecca, R. Genevois, G. Scarso<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">74<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Tecca_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Elastic mudflow regulating barrage and methodology for its calculation<br \/><strong>G.V. Gavardashvili, E.G. Kukhalashvili, Sh.G. Kupreishvili,<br \/>N.G. Gavardashvili<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">88<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Gavardashvili_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Debris flows on September 4, 2017 on the Okhotsk coast of Paramushir Island, Kuril Islands<br \/><strong>T.A. Kotenko, L.V. Kotenko<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">97<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Kotenko_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Rockslide dams and catastrophic outburst floods in the river valleys of the Pamir mountains<br \/><strong>A.L. Strom<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">111<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Strom_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Comprehensive analysis of surface characteristics of debris flow fans in Gilgit-Baltistan and Chitral regions of Pakistan using remote sensing<br \/><strong>G. Amin, D. Bano, S. Wali, S. Shah<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">122<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Amin_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Litho-structural mapping of debris flow hazard zones of Western Darvaz (Tajikistan and Afghanistan) from Sentinel data using remote sensing techniques<br \/><strong>J.H. Aminov, A.R. Fazilov, J.H. Aminov, Y. Mamadjanov,<br \/>M.Z. Kobuliev, J.B. Niyazov<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">135<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Aminov_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Badswat glacial lake outburst flood and debris dammed lake: a case study<br \/><strong>W. Anwar, D. Karim, U. Wahab, K. Din, D.R. Gurung<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">146<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Anwar_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Centralized national landslide database for the Kyrgyz Republic: initial steps<br \/><strong>R. Arnhardt, D. Boon, S. Erokhin, V. Zaginaev, N. Smith, A. Simister,<br \/>K. Lawrie, M. Krabbendam<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">157<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Arnhardt_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Outcomes of engineering-geological assessment of the debris flow hazard of Surkhdara sub-catchment and adjacent area (Ilyak River valley, Tajikistan)<br \/><strong>M.M. Azimshoev, R.A. Bobov, Y.S. Lalbekov, Sh.F. Valiev,<br \/>B.A. Alidodov<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">161<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Azimshoev_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Mapping and modelling of glacial lake outburst flood (GLOF) of Deran glacial lake, Ishkoman Valley, Ghizer District, Pakistan using GIS and remote sensing<br \/><strong>D. Bano, S. Wali, S. Shah, A. Hussain<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">170<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Bano_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">The outburst hazard of the landslide-dammed lakes of the Tien Shan<br \/><strong>S.A. Erokhin, V.V. Zaginaev<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">183<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Erokhin1_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Trends of outburst hazard for the dynamics of mountain lakes in Kyrgyzstan<br \/><strong>S.A. Erokhin, V.V. Zaginaev<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">194<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Erokhin2_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Glacier lake outburst flood modeling of Khurdopin glacier lake using HEC-RAS and GIS<br \/><strong>A. Hussain, N. Nasab, D. Bano, D. Karim, W. Anwar, K. Hussain,<br \/>N. Uddin<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">208<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Hussain_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Debris Flow Pilot Risk Management \u2013 a case from Sherqilla in Hindukush Region of Gilgit-Baltistan, Pakistan<br \/><strong>D. Karim, W. Anwar, G. Amin, Q. Rahim, D.R. Gurung<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">221<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Karim1_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Glacier hazard associated with surging glaciers \u2013 story of the Shishper Glacier from Hunza, Pakistan<br \/><strong>D. Karim, I. Karim, W. Anwar, K. Uddin, A. Ali, D.R. Gurung<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">234<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Karim2_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Climatic risks and food security in the Khatlon Region of Tajikistan<br \/><strong>A.S. Kodirov, U.A. Alizoda, A.A. Dorgaev<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">246<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Kodirov_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Assessment of debris-flow parameters for the 2015 debris flow event in Barsemdara stream valley (Tajikistan)<br \/><strong>V.A. Kurovskaia, S.S. Chernomorets, T.A. Vinogradova,<br \/>K.S. Viskhadzhieva, O.N. Mavlonazarov, <\/strong><strong>R.A. Bobov<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">252<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Kurovskaia_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Debris flow hazard in case of the outbursts of dammed lakes and reservoirs in Pamir and other mountain regions<br \/><strong>A.M. Lekhatinov<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">265<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Lekhatinov1_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Debris flow hazard of glacial lake in Chitral, Pakistan<br \/><strong>N. Uddin, M. Anjum, S. Uddin, Z. Uddin<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">272<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Uddin-N_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Debris flow mitigation in Chitral Region, Pakistan<br \/><strong>Z. Uddin, T. Zaman, M. Anjum, S. Uddin, N. Uddin<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">282<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Uddin-Z_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Integrated assessment and planning of watershed management in the Rasht valley of the Republic of Tajikistan<br \/><strong>U.R. Pirmamadov<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">290<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Pirmamadov2_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Assessment of a potential outburst for Lower Varshedzkul Lake (Pamir, Tajikistan) using bathymetric survey and modeling<br \/><strong>Y.K. Raimbekov, U.R. Pirmamadov, F.O. Marodaseinov,<br \/>I.I. Zikillobekov, A.G. Gulomaydarov, S.S. Chernomorets,<br \/>E.A. Savernyuk, I.V. Krylenko, I.N. Krylenko, V.M. Kidyaeva,<br \/>V.A. Kurovskaia, K.S. Viskhadzhieva, R.A. Bobov<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">303<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Raimbekov_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Remote sensing and monitoring of debris flow areas in the conditions of climate change (Kamarob, Tajikistan)<br \/><strong>M.S. Safarov, A.R. Fazilov<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">313<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Safarov_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td>Debris flow risk and vulnerability assessment for the territory of the Khorog town<br \/><strong>G.V. Shafiev<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">323<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Shafiev_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Role of vegetation cover for the landscape stabilization in Shashvalon catchment, Nurabad District, Republic of Tajikistan<br \/><strong>S.Y. Yusupov<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">335<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Yusupov_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Assessment of debris flows in the Shuraki Kapali River basin (left tributary of the Surkhob River, Tajikistan) and development of risk reduction measures<br \/><strong>R.G. Zaripov, F.S. Imomnazarov, A.S. Taghoybekov<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">342<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Zaripov_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Calculation of non-eroding velocities in mountain rivers of Azerbaijan<br \/><strong>F.S. Akhmedov, F.A. Imanov, E.V. Javadzade<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">351<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Akhmedov_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Neopleistocene debris flows in Gorny Altai<br \/><strong>G.Ya. Baryshnikov<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">355<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Baryshnikov_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Debris flow protection constructions design experience at the transport infrastructure facilities in dumped conditions<br \/><strong>I.S. Bogdanov<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">363<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Bogdanov_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Underground outbursts of lakes and other debris flow manifestations in rock glaciers<br \/><strong>M.D. Dokukin, M.Yu. Bekkiev, R.Kh. Kalov, E.A. Savernyuk,<br \/>S.S. Chernomorets<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">371<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Dokukin2_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Glaciogeomorphological conditions for the Gerkhozhan-Su River debris flow formation (Central Caucasus)<br \/><strong>M.D. Dokukin, M.Yu. Bekkiev, R.Kh. Kalov, E.A. Savernyuk,<br \/>S.S. Chernomorets, E.M. Bogachenko<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">388<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Dokukin3_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Application of forestry to protect against debris flows on the Black Sea coast of the West Caucasus<br \/><strong>L.M. Dzaganiia<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">405<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Dzaganiia_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Estimation of ground freezing depth as deterrent factor of debris flow process<br \/><strong>D.M. Frolov<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">418<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Frolov_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Vulnerability of buildings exposed to dynamic flooding<br \/><strong>S. Fuchs, M. Papathoma-K\u00f6hle, M. Keiler<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">422<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Fuchs_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Debris flow in the North-East of Russia<br \/><strong>Yu.V. Gensiorovskiy, L.E. Muzychenko, V.A. Lobkina,<br \/>A.A. Muzychenko, \u041c.V. Mikhalev, Y.A. Stepnova<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">430<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Gensiorovskiy_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Geomorphological consequences and hydrometeorological conditions of extreme flood in the Tsanyk River basin, Sochi region<br \/><strong>V.N. Golosov, Yu.S. Kuznetsova, N.N. Ivanova, A.S. Tsyplenkov,<br \/>D.V. Botavin, M.M. Ivanov<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">438<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Golosov_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Role of debris flows in the cycle of extremal exogenic processes in the mountains of the Central Caucasus (case study of the Cherek Balkarsky river basin)<br \/><strong>V.A. Karavaev, A.V. Voskova2, S.S. Seminozhenko3, A.V. Fedin,<br \/>E.G. Lappo, S.A. Bulanov<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">446<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Karavaev_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Temporary analysis of change of debris flow activity on the northern slope of the Great Caucasus<br \/><strong>N.V. Kondratyeva, A.Kh. Adzhiev, V.V. Razumov, A.B. Uzdenova<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">451<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Kondratyeva_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Features of debris flow formation in volcanic regions<br \/><strong>E.V. Lebedeva<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">460<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Lebedeva_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Influence of debris flows on the ecosystem and ecology of Tunkinsky National Park<br \/><strong>A.M. Lekhatinov, E.B. Lekhatinova, A.D. Dorzhiyev<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">470<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Lekhatinov2_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Characteristics of debris flows forming in permafrost areas<br \/><strong>V.A. Lobkina, Yu.V. Gensiorovskiy, M.V. Mikhalev<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">477<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Lobkina_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Assessment of the influence of space weather on the development of the debris flow process in the Elbrus region to clarify the operational forecasts of debris flows<br \/><strong>I.V. Malneva, A.A. Cherkesov<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">482<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Malneva_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Debris flow distribution within Khabarovsk Krai territory<br \/><strong>A.A. Muzychenko, Yu.V. Gensiorovskiy, L.E. Muzychenko<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">491<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/MuzychenkoAA_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Distribution of natural and man-made debris flows on Sakhalin Island<br \/><strong>L.E. Muzychenko, A.A. Muzychenko<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">499<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/MuzychenkoLE_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Impacts of debris flows on the technosphere according to the database analysis<br \/><strong>E.G. Petrova<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">509<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Petrova_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Effectiveness of debris flow protection measures within the mountain ski cluster of Krasnaya Polyana of Sochi (West Caucasus)<br \/><strong>K.G. Samarkin-Dzharskiy, E.V. Dzaganiia<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">517<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Samarkin-Dzharskiy_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Quantitative assessment of anthropogenic impact for debris flow activation in small catchments of the Aibga Ridge (Krasnaya Polyana village area)<br \/><strong>S.V. Shvarev, S.V. Kharchenko, V.N. Golosov, M.I. Uspensky<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">530<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Shvarev_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Use of remote sensing data for medium-scale geoinformation mapping of debris-flow hazard in the Baikal mountain country<br \/><strong>V.P. Stupin, L.A. Plastinin, B.N. Olzoev<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">541<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Stupin_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Ground-based slope stability radar for the discrimination of superficial deformation process and their correlation with environmental triggering factors<br \/><strong>A. Torres, E. Kanaev<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">553<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Torres_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Abnormal ice situation on the mountain rivers of South-East Kazakhstan as a sign of formation of ice-water flows<br \/><strong>V.V. Zhdanov<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">565<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Zhdanov_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\">Remarks on Mariana and Brumadinho tailings dams\u2019 disasters (Minas Gerais, Brazil)<br \/><strong>D.V. Znamensky<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">571<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Znamensky_DF20.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\"><strong>Author\u2019s Index<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">581<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/AuthorIndex_DF20_1.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<tr>\n<td width=\"735\"><strong>Contents<\/strong><\/td>\n<td>\n<p style=\"text-align: center;\">587<\/p>\n<\/td>\n<td><a href=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/Contents_DF20_1.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter size-full wp-image-2672\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png\" alt=\"\" width=\"1500\" height=\"1500\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2.png 1500w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-300x300.png 300w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-1024x1024.png 1024w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-150x150.png 150w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2020\/12\/pdf2-768x768.png 768w\" sizes=\"auto, (max-width: 1500px) 100vw, 1500px\" \/><\/a><\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<p>Conference participants&#8217; papers were published in issues 2 and 3 of the GeoRisk journal for 2020.<\/p>\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-9d6595d7 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\"><div class=\"wp-block-image\">\n<figure class=\"aligncenter size-large is-resized\"><img loading=\"lazy\" decoding=\"async\" width=\"719\" height=\"1024\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2024\/06\/GR2-2020-719x1024.jpg\" alt=\"\" class=\"wp-image-3939\" style=\"width:247px;height:auto\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2024\/06\/GR2-2020-719x1024.jpg 719w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2024\/06\/GR2-2020-211x300.jpg 211w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2024\/06\/GR2-2020-768x1094.jpg 768w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2024\/06\/GR2-2020-1079x1536.jpg 1079w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2024\/06\/GR2-2020-1438x2048.jpg 1438w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2024\/06\/GR2-2020-scaled.jpg 1798w\" sizes=\"auto, (max-width: 719px) 100vw, 719px\" \/><\/figure>\n<\/div><\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\"><div class=\"wp-block-image\">\n<figure class=\"aligncenter size-large is-resized\"><img loading=\"lazy\" decoding=\"async\" width=\"735\" height=\"1024\" src=\"http:\/\/www.debrisflow.ru\/wp-content\/uploads\/2024\/06\/GR3-2020-735x1024.jpg\" alt=\"\" class=\"wp-image-3940\" style=\"width:260px;height:auto\" srcset=\"https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2024\/06\/GR3-2020-735x1024.jpg 735w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2024\/06\/GR3-2020-215x300.jpg 215w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2024\/06\/GR3-2020-768x1070.jpg 768w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2024\/06\/GR3-2020-1102x1536.jpg 1102w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2024\/06\/GR3-2020-1469x2048.jpg 1469w, https:\/\/www.debrisflow.ru\/wp-content\/uploads\/2024\/06\/GR3-2020-scaled.jpg 1837w\" sizes=\"auto, (max-width: 735px) 100vw, 735px\" \/><\/figure>\n<\/div><\/div>\n<\/div>\n\n\n\n<div class=\"wp-block-columns is-layout-flex wp-container-core-columns-is-layout-9d6595d7 wp-block-columns-is-layout-flex\">\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<p class=\"has-text-align-center\"><a href=\"https:\/\/www.geomark.ru\/journals_list\/georisk-tom-xiv-%e2%84%962-2020\/?attach=14073\" title=\"\">Full version<\/a><\/p>\n<\/div>\n\n\n\n<div class=\"wp-block-column is-layout-flow wp-block-column-is-layout-flow\">\n<p class=\"has-text-align-center\"><a href=\"https:\/\/www.geomark.ru\/journals_list\/georisk-tom-xiv-%e2%84%963-2020\/?attach=14613\" title=\"\">Full version<\/a><\/p>\n<\/div>\n<\/div>\n","protected":false},"excerpt":{"rendered":"<p>Proceedings of the Conference Debris Flows: Disasters, Risk, Forecast, Protection. Proceedings of the 6th International Conference (Dushanbe\u2013Khorog, Tajikistan). Volume 1. \u2013 Ed. by S.S. Chernomorets, K.S. Viskhadzhieva. \u2013 Dushanbe: \u201cPromotion\u201d LLC, 2020, 610 p.ISBN 978-99975-309-4-3Full text of the book (Volume 1) Table of contents Preface vii Risk and consequences of high-mountain lake outbursts in TajikistanU.R. [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":580,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-2666","page","type-page","status-publish","hentry"],"aioseo_notices":[],"jetpack_sharing_enabled":true,"_links":{"self":[{"href":"https:\/\/www.debrisflow.ru\/en\/wp-json\/wp\/v2\/pages\/2666","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.debrisflow.ru\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.debrisflow.ru\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.debrisflow.ru\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.debrisflow.ru\/en\/wp-json\/wp\/v2\/comments?post=2666"}],"version-history":[{"count":52,"href":"https:\/\/www.debrisflow.ru\/en\/wp-json\/wp\/v2\/pages\/2666\/revisions"}],"predecessor-version":[{"id":3952,"href":"https:\/\/www.debrisflow.ru\/en\/wp-json\/wp\/v2\/pages\/2666\/revisions\/3952"}],"up":[{"embeddable":true,"href":"https:\/\/www.debrisflow.ru\/en\/wp-json\/wp\/v2\/pages\/580"}],"wp:attachment":[{"href":"https:\/\/www.debrisflow.ru\/en\/wp-json\/wp\/v2\/media?parent=2666"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}