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Although other alternatives exist, two models dominate the discussion aboutthe formation of the Altiplano-Puna and other orogenic plateaus.
Plateau growth may be the outcome of deep-seated mantle processes.
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Most of its extensive area is internally drained, leaving little opportunity for the shedding of sediment through erosion (Reiners et al., 2015).
It is likely accurate to limit the effects of physical erosion in the Altiplano-Puna to within a few hundred kilometers of the high elevation and relief of the Eastern Cordillera in a study of uplift and erosion dynamics (Reiners et al., 2015).
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