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Geophysics

A third way to rift continents

Nature volume 499, pages 157–159 (2013)Cite this article

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Rifting of continents is usually explained by one of two mechanisms based on effects that originate far from the zone of rifting. Laboratory experiments show that this geodynamic process can also be caused by local effects.

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Figure 1: Slow volcanic activity.

JEAN DU BOISBERRANGER/HEMIS/CORBIS

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Authors and Affiliations

  1. W. Roger Buck is at the Lamont-Doherty Earth Observatory, Columbia University, Palisades, New York 10960, USA.,

    W. Roger Buck

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  1. W. Roger Buck
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Correspondence to W. Roger Buck.

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Buck, W. A third way to rift continents. Nature 499, 157–159 (2013). https://doi.org/10.1038/499157a

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