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Mineral palsas with thin peat covers are described from the continuous to discontinuous permafrost transition zone. They are up to 4 m high and are developed in a clast rich fine grained diamict. Their development post dates the land emergence ca. 4.3 ka BP following isostatic uplift. Morphological and vegetational data suggest a growth and decay cycle from small, emergent,Sphagnum covered mounds...
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