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Retreat of the Stabre Glacier in the Norra Storfjället Mountains of northern Sweden led to the emplacement of a broad expanse of glaciofluvial sediment, a virtual blanket of debris interspersed with recessional and push moraines. Episodic mass wasting of the glaciofluvial, moraine and loessic deposits yielded a pedostratigraphic succession of 14 C-dated sub-Boreal and sub-Atlantic Cryosols...
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