Research by J.P. Richards and M. Villeneuve has allowed the determination of the geological history of the region. Had volcanism during the Eocene and Oligocene been centered on the Precordillera, increased subduction of the Nazca Plate during the late Oligocene caused the volcanic arc to broaden to about . 25 million years ago, the Quechua event triggered the uplift of the Puna-Altiplano, a highland covering a surface area of and reaching an altitude of . In the late Miocene-Pliocene a phase of strong ignimbrite volcanism occurred. About 2 million years ago, the Diaguita deformation was characterized by a change in the deformation regimen from crustal shortening to strike-slip faulting and of volcanism from voluminous felsic eruptions to isolated stratovolcanoes and back-arc mafic volcanism. A slowdown in the subduction may have caused this change. Nowadays most volcanism occurs at the western edge of the Puna, where volcanoes such as Lascar and Llullaillaco formed.