THE NATURE OF CYCLIC STRUCTURE OF THE ICE COMPLEX, EAST SIBERIA

The features of cyclic structure in the Karga-Sartan Ice Complex (IC) deposits in Northern Yakutia have been studied for the coastal lowlands. We have analyzed cycles of different genesis (cryolithological, structural, lithological, and soil-vegetation) and duration. Climate fluctuation was the majo...

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Main Author: Vyacheslav Konishchev
Format: Article
Language:English
Published: Lomonosov Moscow State University 2013-09-01
Series:Geography, Environment, Sustainability
Subjects:
Online Access:https://ges.rgo.ru/jour/article/view/137
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spelling doaj-b6576a90f24e49919f380ab63aec9e032021-07-28T21:10:05ZengLomonosov Moscow State UniversityGeography, Environment, Sustainability2071-93882542-15652013-09-016342010.24057/2071-9388-2013-6-3-4-20136THE NATURE OF CYCLIC STRUCTURE OF THE ICE COMPLEX, EAST SIBERIAVyacheslav KonishchevThe features of cyclic structure in the Karga-Sartan Ice Complex (IC) deposits in Northern Yakutia have been studied for the coastal lowlands. We have analyzed cycles of different genesis (cryolithological, structural, lithological, and soil-vegetation) and duration. Climate fluctuation was the major factor of cyclic structure in the IC deposits. Cyclic structure in the IC deposits develops in certain facial-genetic conditions characterized by cryogenic weathering and subsequent re-deposition of eroded soils in river valleys and alas depressionshttps://ges.rgo.ru/jour/article/view/137ice complexcyclicitycontentmineralogyweatheringsoilorigin
collection DOAJ
language English
format Article
sources DOAJ
author Vyacheslav Konishchev
spellingShingle Vyacheslav Konishchev
THE NATURE OF CYCLIC STRUCTURE OF THE ICE COMPLEX, EAST SIBERIA
Geography, Environment, Sustainability
ice complex
cyclicity
content
mineralogy
weathering
soil
origin
author_facet Vyacheslav Konishchev
author_sort Vyacheslav Konishchev
title THE NATURE OF CYCLIC STRUCTURE OF THE ICE COMPLEX, EAST SIBERIA
title_short THE NATURE OF CYCLIC STRUCTURE OF THE ICE COMPLEX, EAST SIBERIA
title_full THE NATURE OF CYCLIC STRUCTURE OF THE ICE COMPLEX, EAST SIBERIA
title_fullStr THE NATURE OF CYCLIC STRUCTURE OF THE ICE COMPLEX, EAST SIBERIA
title_full_unstemmed THE NATURE OF CYCLIC STRUCTURE OF THE ICE COMPLEX, EAST SIBERIA
title_sort nature of cyclic structure of the ice complex, east siberia
publisher Lomonosov Moscow State University
series Geography, Environment, Sustainability
issn 2071-9388
2542-1565
publishDate 2013-09-01
description The features of cyclic structure in the Karga-Sartan Ice Complex (IC) deposits in Northern Yakutia have been studied for the coastal lowlands. We have analyzed cycles of different genesis (cryolithological, structural, lithological, and soil-vegetation) and duration. Climate fluctuation was the major factor of cyclic structure in the IC deposits. Cyclic structure in the IC deposits develops in certain facial-genetic conditions characterized by cryogenic weathering and subsequent re-deposition of eroded soils in river valleys and alas depressions
topic ice complex
cyclicity
content
mineralogy
weathering
soil
origin
url https://ges.rgo.ru/jour/article/view/137
work_keys_str_mv AT vyacheslavkonishchev thenatureofcyclicstructureoftheicecomplexeastsiberia
AT vyacheslavkonishchev natureofcyclicstructureoftheicecomplexeastsiberia
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