Maipo is a stratovolcano in the Andes, lying on the border between Argentina and Chile. It is located 90km (56mi) south of Tupungato and about 100km (62mi) southeast of Santiago. It has a symmetrical, conical volcanic shape, and is among the southernmost 5,000metre peaks in the Andes.[3]
Maipo is located within the Diamante caldera, a feature measuring 15km by 20km that is about half a million years old. It rises about 1,900m (6,230ft) above the floor of the caldera. Immediately to the east of the peak, on the eastern side of the caldera floor, is Laguna del Diamante, a lake that formed when lava flows blocked drainage channels from the caldera in 1826. The Diamante Caldera erupted 450 cubic kilometers (108cumi) of tephra, 450ka.[4]
The region's climate is transitional between the drier Mediterranean climate of the peaks to the north and the cold, moist climate of Chilean Patagonia. Hence, while less glaciated than Patagonia, it has more permanent snow on the wet, Chilean side than peaks of similar elevation to the north.[3]
from Shuttle Radar Topography Mission (SRTM) data.
Sources
Volcan Maipo or Maipú (span.)
Sruoga, P.; Llambías, E.J.; Fauqué, L.; Schonwandt, D.; Repol, D.G. (2005). "Volcanological and geochemical evolution of the Diamante Caldera-Maipo volcano complex in the Southern Andes of Argentina (34°10'S)". J. South American Earth Sci. 19: 399–414. doi:10.1016/j.jsames.2005.06.003.
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