Abstract
The paper considers hazardous phenomena on the Earth’s surface such as sinkholes within the Lena River floodplain terrace, the Central Yakutia, in the areas of intrapermafrost groundwater development. Possible mechanisms for the formation of a dip based on thermosuffusion and the mechanism of formation of dissipative geological structures are investigated. The materials of monitoring and geophysical works in the areas of manifestation of failures are analyzed.
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