The Nevados de Pastos Grandes complex encompasses several volcanic centres, the highest one at is called Cerro Queva or El Queva. The two other centres are named Gordo and Azufre, with some additional minor centres. These centres are aligned in a north-south direction, covering. The volcanic complex has been affected by physical erosion, which has brought to the surface the deeper parts of the complex. The Pleistocene glaciation has excavated cirques and U shaped valleys in the western and northern side of Azufre and Gordo above. It has left talus and moraines on the upper flanks of the volcano as well as exposing hydrothermally altered areas, chiefly on the western side of the range. Among these are separate moraines on the southwestern slope of Azufre and Quevar and till. Surface exposure dating indicates that these moraines developed during lake highstands in the Salar de Uyuni. Even today, rock glaciers and stone stripes testify to the persistence of glacial activity.
Petrology and geology
The volcano has generated welded ash flows. Later a stratovolcano was built by lava and pyroclastic flows, with lava flows dominating. As is typical for many Puna volcanoes, the first lava flows that were erupted are dacitic and are exposed in the northern and eastern flanks. They may be Pliocene or Pleistocene in age. Later the main edifice was built by andesitic lavas. Another view treats lava domes formed 8.6±0.5 million years ago as the final activity. In this view, the last activity coincides with the cessation of large ignimbritic volcanism in the northern Puna and is probably linked to a steeper subduction of the Nazca plate. Thermal springs are still present however. These include the Boratera Antuco spring. The ash flows are K-rich andesitic-dacitic and contain amphibole and biotite. Andesitic lava flows are also found, while the terminal lava domes are dacitic-rhyolitic in composition. One rhyolite lava flow is found at Azufre. Andesites contain quartz and dacites-rhyodacites contain sanidine megacrysts. In hydrothermally altered areals alunite, barite, dickite, kaolinite, pyrite and quartz are also found. Propylite-like degradation as well as veins contained inside of rock that has been heavily degraded to argillite.
Geologic context
The volcanic centre is underpinned by an Ordovician basement including metamorphed flysch and phyllites on the western side of the complex. On the eastern side a granitebatholith is intruded. It may be of Silurian age. Later Miocene-Pliocene sediments formed in a depositional environment, forming the Pastos Grandes Group. Fault activity has been widespread in the Puna with block faulting, but the volcanoes themselves are little affected by the faulting. However, the alignment of the centres may be linked to a north-south fault. A unique volcano La Pava-Ramadas is found north of Queva and has generated ash falls as far as the Subandean ranges 8.75 million years ago. The volcano was formed on top of the Calama–Olacapato–El Toro lineament. El Queva is one of many volcanoes in the Puna. Previous volcanism occurred in the east at the Aguas Calientes caldera and probably migrated later to El Queva.
Human Activity
Nevado de Pastos Grandes is a major polymetallic district, including lead, silver and tin. Mineralization post-dates the eruption of the host rocks by less than million years at depths of less than. The formation of these deposits seems to be linked to solfataric alteration. Sulfur is found in the alteration zone and at Azufre. Manganese oxides are found also near the El Queva mine, as well as six other deposits that mostly don't coincide with alteration zones and are found in variable environments. These manganese deposits appear to be associated with former thermal springs. Sulfur from this system was formerly mined at Azufre. Between 1968 and 1973 a rudimentary mining operation at El Queva mine yielded 3,000 tons of ore. This mine is located at altitude within a long belt that contains lead-silver mineralization within altered dacite. The area is cold and has an arid climate typical of the Altiplano, with less than precipitation falling mainly during the summer monsoon. The town of San Antonio de los Cobres is located northeast. Santa Rosa de los Pastos Grandes is a town southeast of Nevados de Pastos Grandes. A railway and road run around the Nevados de Pastos Grandes range in the northwest. The Alero Cuevas archeological site is located west of Nevados de Pastos Grandes and depended on water coming from the range. Quebrada Alta is another archeological site.
