Earth's central heating is thinning Greenland


POOR Greenland. Not only is its ice sheet melting thanks to rising temperatures, its rocks are being threatened by heat from below.


The rock beneath Greenland is hotter than expected given its radioactivity. Now a team led by Alexey Petrunin from the GFZ Helmholtz Centre Potsdam in Germany have combined seismic and gravitational data to estimate the thickness of Greenland's lithosphere, the rocky part of Earth's surface. They found that it is 80 to 100 kilometres thick, less than the 200 to 250 kilometres typically seen elsewhere on Earth (Nature Geoscience, doi.org/nfj).


This thinning is caused by a plume of magma that's rising up and eroding Greenland, giving the rocks their heat, says Petrunin.


This article appeared in print under the headline "Erosion by Earth's central heating"


Issue 2930 of New Scientist magazine


  • Subscribe to New Scientist and you'll get:

  • New Scientist magazine delivered every week

  • Unlimited access to all New Scientist online content -

    a benefit only available to subscribers

  • Great savings from the normal price

  • Subscribe now!




If you would like to reuse any content from New Scientist, either in print or online, please contact the syndication department first for permission. New Scientist does not own rights to photos, but there are a variety of licensing options available for use of articles and graphics we own the copyright to.



Have your say

Only subscribers may leave comments on this article. Please log in.


Only personal subscribers may leave comments on this article


Subscribe now to comment.




All comments should respect the New Scientist House Rules. If you think a particular comment breaks these rules then please use the "Report" link in that comment to report it to us.


If you are having a technical problem posting a comment, please contact technical support.