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Late Holocene reexpansion of Laurentide Ice Sheet traced to Baffin Island

A new study in Science models the Late Holocene reexpansion of the Laurentide Ice Sheet as likely originating over Baffin Island in the Eastern Canadian Arctic. The work complements earlier findings that Arctic ice grew for centuries before progressively retreating in the mid‑20th century.

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2 articles from 2 sources