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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Bibliographic Details
Published in:GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY
Main Author: Vyacheslav Konishchev
Format: Article in Journal/Newspaper
Language:English
Published: Lomonosov Moscow State University 2013
Subjects:
ice complex
cyclicity
content
mineralogy
weathering
soil
origin
Geography (General)
G1-922
Karga
Yakutia
Siberia
Online Access:https://doi.org/10.24057/2071-9388-2013-6-3-4-20
https://doaj.org/article/b6576a90f24e49919f380ab63aec9e03
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Summary: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

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