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...
Published in: | GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY |
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Main Author: | |
Format: | Article in Journal/Newspaper |
Language: | English |
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Russian Geographical Society
2013
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Online Access: | https://ges.rgo.ru/jour/article/view/137 https://doi.org/10.24057/2071-9388-2013-6-3-4-20 |
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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