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Talik è un terreno non gelato nell’area del permafrost. I talik possono avere origini diverse – possono rimanere non congelati a causa dell’effetto di accumulo di calore delle acque superficiali, delle acque sotterranee mineralizzate che fluiscono attraverso talik ecc.

Talik sono importanti risorse idriche per le comunità locali.

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