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Earth science

How old roots lose their bounce

Active mountain belts have crustal 'roots' that gravitationally balance the high topography. So why do old mountains that have been worn flat by erosion still have these roots?

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Figure 1: Mountain building at 'collisional' boundaries, and the fate of crustal roots.

References

  1. Fischer, K. M. Nature 417, 933–936 (2002).

    ADS  CAS  Article  Google Scholar 

  2. Dewey, J. F. Tectonics 7, 1123–1139 (1988).

    ADS  Article  Google Scholar 

  3. Vanderhaeghe, O. & Teyssier, C. Tectonophysics 335, 211–228 (2001).

    ADS  Article  Google Scholar 

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Correspondence to David James.

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James, D. How old roots lose their bounce. Nature 417, 911–913 (2002). https://doi.org/10.1038/417911a

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  • DOI: https://doi.org/10.1038/417911a

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