In this article we are going to analyze Maipo (volcano), a topic that has generated great interest in recent times. Maipo (volcano) is a topic that has captured the attention of many people due to its relevance in different areas, from science to popular culture. Furthermore, Maipo (volcano) has been the subject of numerous debates and discussions, which has contributed to its growing importance in today's society. Throughout this article, we will explore different aspects related to Maipo (volcano), from its origin and evolution to its impact today. Through detailed analysis, we will try to shed light on this topic and provide a more complete and deeper insight into Maipo (volcano).
Maipo | |
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Highest point | |
Elevation | 5,264 m (17,270 ft)[note 1] |
Coordinates | 34°09′39.6″S 69°49′58.8″W / 34.161000°S 69.833000°W |
Geography | |
Location | Argentina – Chile |
Parent range | Principal Cordillera, Andes |
Geology | |
Mountain type | Stratovolcano |
Last eruption | 1912 |
Climbing | |
First ascent | 1883 by Paul Güssfeldt |
Easiest route | snow/ice climb |
Maipo is a stratovolcano in the Andes, lying on the border between Argentina and Chile. It is located 90 km (56 mi) south of Tupungato and about 100 km (62 mi) southeast of Santiago. It has a symmetrical, conical volcanic shape, and is among the southernmost 5,000 metre peaks in the Andes.
Maipo is located within the Diamante caldera, a feature measuring 15 km by 20 km that is about half a million years old. It rises about 1,900 m (6,230 ft) 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 (108 cu mi) of tephra, 450 ka.
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.