Permafrost is permanently frozen soil where temperature does not rise above 0°C during two year period. Because of the repeating thawing of transient and active soil layer the upper organic soil horizon can be burried during process of cryoturbation. Also many unique geological structures are formed (polygons, ice wedges, etc.)
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Branišovská 1645/31a, 370 05 České Budějovice Tel. 387 776 201 | This email address is being protected from spambots. You need JavaScript enabled to view it.
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