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Cerro Tujle (also known as Cerro Tucle or Cerro Tugle) is a
mafic A mafic mineral or rock is a silicate mineral or igneous rock rich in magnesium and iron. Most mafic minerals are dark in color, and common rock-forming mafic minerals include olivine, pyroxene, amphibole, and biotite. Common mafic rocks include ...
volcanic centre in the
Central Volcanic Zone The Andean Volcanic Belt is a major volcanic belt along the Andean cordillera in Argentina, Bolivia, Chile, Colombia, Ecuador, and Peru. It is formed as a result of subduction of the Nazca Plate and Antarctic Plate underneath the South Americ ...
of the
Andes The Andes, Andes Mountains or Andean Mountains (; ) are the longest continental mountain range in the world, forming a continuous highland along the western edge of South America. The range is long, wide (widest between 18°S – 20°S ...
, Chile. It forms a deep
maar A maar is a broad, low-relief volcanic crater caused by a phreatomagmatic eruption (an explosion which occurs when groundwater comes into contact with hot lava or magma). A maar characteristically fills with water to form a relatively shallow ...
. Its eruption products are aphyric. Previously in 1977, this crater has been identified as a
meteor crater Meteor Crater, or Barringer Crater, is a meteorite impact crater about east of Flagstaff and west of Winslow in the desert of northern Arizona, United States. The site had several earlier names, and fragments of the meteorite are official ...
with diameters of . The crater lies between the
Salar de Atacama Salar de Atacama is the largest salt flat in Chile. It is located south of San Pedro de Atacama, is surrounded by mountains, and has no drainage outlets. In the east it is enclosed by the main chain of the Andes, while to the west lies a secondar ...
and the Western Cordillera at an elevation of on the Cordón de Tujle ridge, south-east of Peine. The crater is wide, elliptical and surrounded by volcanic deposits. The crater appears to have formed, after an initial
lava flow Lava is molten or partially molten rock (magma) that has been expelled from the interior of a terrestrial planet (such as Earth) or a moon onto its surface. Lava may be erupted at a volcano or through a fracture in the crust, on land or und ...
eruption turned
phreatomagmatic Phreatomagmatic eruptions are volcanic eruptions resulting from interaction between magma and water. They differ from exclusively magmatic eruptions and phreatic eruptions. Unlike phreatic eruptions, the products of phreatomagmatic eruptions cont ...
. It is embedded in the Tucúcaro Ignimbrite, which overlies an Ordovician basement and
Paleozoic The Paleozoic (or Palaeozoic) Era is the earliest of three geologic eras of the Phanerozoic Eon. The name ''Paleozoic'' ( ;) was coined by the British geologist Adam Sedgwick in 1838 by combining the Greek words ''palaiós'' (, "old") and ' ...
-
Mesozoic The Mesozoic Era ( ), also called the Age of Reptiles, the Age of Conifers, and colloquially as the Age of the Dinosaurs is the second-to-last era of Earth's geological history, lasting from about , comprising the Triassic, Jurassic and Cretaceo ...
volcanic and
Neozoic ''Neozoic'' is a science fiction/fantasy comic book published by Red 5 Comics. It is written by Paul Ens, who worked on ''Star Wars: Evasive Action''. The art is done by J. Korim and Jessie Lam. The setting is in a different universe where dinosau ...
mixed sediments. There are other volcanic systems in the vicinity.


See also

* Tilocálar


References

Volcanoes of Chile Maars of Chile Holocene volcanism Quaternary Chile Geography of Antofagasta Region Andean Volcanic Belt {{Volcanology-stub