TulTul, Del Medio and Pocitos

TulTul, Del Medio and Pocitos are three volcanoes in Argentina.
Since the Jurassic, subduction off the western margin of South America has generated volcanism, which after starting in the Cordillera de la Costa now occurs in the Andes. Since the Oligocene, the Puna has been volcanically active as well. There, some stratovolcanoes including TulTul, Del Medio and Pocitos are aligned on the Calama-Olacapato-El Toro fault which cuts across the plateau in southeast direction.
TulTul, Del Medio and Pocitos are constructed by andesite and dacite and form a long alignment. Del Medio and Pocitos both feature traces of their southern flank collapsing, and both have a summit caldera and wide respectively. Tul Tul had a central vent which formed andesitic lava flows and later above these lava flows dacitic domes.
The volcanoes were active 8 to 6 million years ago, during the Miocene. Lava domes were emplaced on all three volcanoes late in their history. The magmas that constructed these volcanoes appear to have originated in the lower crust from a garnet-bearing precursor. Moraines developed at elevations exceeding elevation on Del Medio and Pocitos, consisting of features on the walls of a cirque and two lateral moraines downvalley. These moraines formed before the last glacial maximum, but during wet periods in the Salar de Uyuni.