Why are the Andes so High?
Wednesday, March 21, 2007 10:00:52 AM
Schellart W. P., et al. made three-dimensional computer models of subducting slabs of different width to see how they evolved over time. Subduction zones and their associated slabs are limited in lateral extent from 250–7,400 km (7,400 km being the length of the deep-sea trench along the South American west coast). One of the conclusions was that wide-slab behaviour may explain mountain building in the central Andes, as being a consequence of its tectonic setting, far from slab edges.
- Nature: http://www.nature.com/nature/journal/v446/n7133/abs/nature05615.html
- News@Nature: http://www.nature.com/news/2007/070312/full/070312-4.html
More on the South American Plate at http://whatonearth.olehnielsen.dk/plates/southamerican.asp








