De Thwaites-gletsjer in Antarctica kan binnen tien jaar loskomen van de onderzeese berg die hem momenteel nog op zijn plek houdt.
De catastrofale stijging van de zeespiegel die hierop zou volgen, kan een domino-effect veroorzaken dat ook het omliggende ijs beïnvloedt.
Lees verder op Newscientist.nl
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