The interactions between climate and tectonics in active mountain ranges are complex and important. Field and geophysical data from the St Elias Range of Alaska show that glacial erosion can influence the dynamics of the lithosphere in such settings.
References
Koons, P. O. Annu. Rev. Earth Planet. Sci. 23, 375–408 (1995).
Berger, A. L. et al. Nature Geosci. 1, 793–799 (2008).
Molnar, P. & England, P. Nature 346, 29–34 (1990).
Hallet, B., Hunter, I. & Bogen, J. Global Planet. Change 12, 213–235 (1996).
Zeitler, P. K. et al. GSA Today 11, 4–9 (2001).
Beaumont, C., Jamieson, R. A., Nguyen, M. H. & Lee, B. Nature 414, 738–742 (2001).
Willett, S. D. J. Geophys. Res. 104, 28957–28982 (1999).
Whipple, K. X. & Meade, B. J. J. Geophys. Res. 109, F01011 (2004).
Tomkin, J. H. & Roe, G. H. Earth Planet. Sci. Lett. 262, 385–397 (2007).
Dahlen, F. A., Suppe, J. & Davis, D. J. Geophys. Res. 89, 10087–10101 (1984).
Berendsen, H. J. A. De Vorming Van Het Land, Inleiding in de Geologie en de Geomorfologie, Vijfde Herziene Druk 5th edn (Van Gorcum IUGS, 2008).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Brocklehurst, S. A glacial driver of tectonics. Nature Geosci 1, 732–733 (2008). https://doi.org/10.1038/ngeo344
Issue Date:
DOI: https://doi.org/10.1038/ngeo344
- Springer Nature Limited