The widest part of the Andean orogen is between 15° and 27°S (Figure 1), where the subduction angle is 20°-30°, flanked southwards and northwards by the flat subduction segments, where the subducted Nazca plate flattens out to become nearly horizontal. The Altiplano and Puna plateaus together constitute the second largest high plateau in the world, the Central Andean Plateau (Figure 1), which is also the only one that formed under a subduction regime. The Altiplano plateau (AP), in the northern part of the Central Andean Plateau, is characterized by a single internally drained basin with an average rather uniform elevation around 3,800 m, whereas the southern part of the Central Andean Plateau is the Puna plateau (PN), which exhibits a higher altitude around 4,500 m with more rugged relief, enclosing a series of internal drained basins. The Central Andean Plateau is flanked to the west by the Western Cordillera (WC) and to