aariПроблемы Арктики и АнтарктикиArctic and Antarctic Research0555-26482618-6713Государственный научный центр Российской Федерации Арктический и антарктический научно-исследовательский институт10.30758/0555-2648-2023-69-4-486-500aari-576Research ArticleГЛЯЦИОЛОГИЯ И КРИОЛОГИЯGLACIOLOGY AND CRYOLOGY OF THE EARTHКлассификация криогенно-оползневых форм рельефа для целей картографирования и прогнозаClassification of cryogenic-landslide landforms for mapping and predictionhttps://orcid.org/0000-0003-4634-6413ЛейбманМ. О.LeibmanM. O.

Тюмень

Tyumen

 

molejbman@utmn.ruhttps://orcid.org/0000-0003-4912-1850КизяковА. И.KizyakovA. I.

Москва

Moscow

https://orcid.org/0000-0001-7055-9852НестероваН. Б.NesterovaN. B.

Тюмень

Германия

Tyumen

Germany

https://orcid.org/0000-0002-7581-731XТарасевичИ. И.TarasevichI. I.

Тюмень

Москва

Tyumen

Moscow

Институт криосферы Земли Тюменского научного центра СО РАН; Тюменский государственный университетРоссияEarth Cryosphere Institute, Tyumen Scientific Centre, Siberian Branch of the Russian Academy of Sciences; University of TyumenRussian FederationМосковский государственный университет им.М.В. ЛомоносоваРоссияLomonosov Moscow State UniversityRussian FederationТюменский государственный университет; Институт полярных и морских исследований им. Альфреда Вегенера, отделение в Потсдаме; Университет ПотсдамаРоссияUniversity of Tyumen; Alfred Wegener Institute on polar and marine research, Potsdam Unit; University of PotsdamRussian FederationИнститут криосферы Земли Тюменского научного центра СО РАН; Тюменский государственный университет; Московский государственный университет им.М.В. ЛомоносоваРоссияEarth Cryosphere Institute, Tyumen Scientific Centre, Siberian Branch of the Russian Academy of Sciences; University of Tyumen; Lomonosov Moscow State UniversityRussian Federation202309122023694486500Copyright © Лейбман М.О., Кизяков А.И., Нестерова Н.Б., Тарасевич И.И., 20232023Лейбман М.О., Кизяков А.И., Нестерова Н.Б., Тарасевич И.И.Leibman M.O., Kizyakov A.I., Nesterova N.B., Tarasevich I.I.This work is licensed under a Creative Commons Attribution 4.0 License.https://www.aaresearch.science/jour/article/view/576

Разработана классификация криогенно-оползневых форм рельефа, сформированных криогенными оползнями течения (КОТФР), для картографирования их распространения и динамики. В основе лежит значительный объем полевых исследований и интерпретации данных дистанционного зондирования Земли. Классификация включает генетические, морфологические и криолитологические особенности пород, определяющие морфологию и динамику КОТФР, их положение в рельефе, степень их активности, сочетание и комплексирование единичных КОТФР. Предложенная классификация и индикационные признаки используются для картографирования КОТФР на севере Западной Сибири.

A classification of cryogenic-landslide landforms is developed for mapping their distribution and dynamics. It is based on the previously suggested classification subdividing cryogenic landsliding into two main types: cryogenic translational landslides (or active-layer detachment slides), and cryogenic earth flows (or retrogressive thaw slumps). The increased proportion of retrogressive thaw slumps compared to active layer detachments in the North of West Siberia in the last decade creates the need for an expanded classification of cryogenic earth flows. One of the important issues is separating the process of landsliding and resulting landforms, which in English are covered by one term ‘retrogressive thaw slump’. In dealing with the landforms, we distinguish (1) open and (2) closed ones. Open cryogenic-landslide landforms are those formed by the retreating of the coast bluff due to the thaw of ice or ice-rich deposits with an additional impact from wave or stream action. Closed cryogenic-landslide landforms are those initiated on a slope landward, and thawed material is delivered to the coast or stream through an erosional channel. Morphologically we distinguish thermocirques and thermoterraces depending on the shape of the retreating headwall, crescent or linear, respectively. An important issue is the type of ground ice subjected to thaw: tabular, ice-wedge or constitutional ground ice are distinguished. Landforms can be active, stabilized or ancient. One can find both single landforms and their combination. The classification is based on a significant amount of field studies and interpretation of remote sensing data. Mapping of the cryogenic-landslide landforms is suggested using the proposed classification and indication features. The classification is based on the experience obtained mainly in the north of West Siberia. Applying it to other regions may require additional studies.

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The authors declare that there are no conflicts of interest present.