Yate
Stratovolcano · Chile · 2187m

- Type
- Stratovolcano
- Country
- Chile
- Region
- South America Volcanic Regions / Southern Andean Volcanic Arc
- Elevation
- 2187m
- Coordinates
- -41.755, -72.396
- Last eruption
- 1090
- Tectonic setting
- Subduction zone / Continental crust (> 25 km)
- Landform
- Composite
- Major rock type
- Andesite / Basaltic Andesite
Geological summary
Yate volcano is a late Pleistocene, glacially dissected basaltic andesite stratovolcano with Holocene flank vents. One of these flank vents is labeled Volcán Yate on the Volcán Hornopirén 1:50,000 quadrangle map. This isolated feature, NNE of Volcán Hornopirén and S of the Relancaví strait, shows evidence of Holocene eruptions. Elongated, it contains six eruptive centers localized along a NW-trending fissure ~7.5 km long. The most recent activity originated from basaltic andesite pyroclastic cones on the NW and W flanks. No reported eruptions are known, although the fresh morphology of its flank cones suggests recent activity (González-Ferrán, 1995). A non-eruptive landslide in 1965 produced a debris flow that reached Lake Cabrera, causing a tsunami that destroyed a settlement and caused 27 fatalities.
From Wikipedia
Yate Volcano is a large, glaciated stratovolcano located in the southern Andes, in the Los Lagos Region of Chile, south of the Reloncaví Estuary. Yate lies on the major regional Liquiñe-Ofqui Fault Zone, and is located 10 km north-east of the smaller Hornopiren volcano. The last known eruption occurred in 1090 CE. There are no historical records of recent volcanic activity, but there is strategic evidence of smaller eruptions sometime in the Holocene. The volcano is named after Juan Yates, also known as John Yates, a settler of Puerto Americano who played a significant role in the exploration and colonisation of Patagonia.
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Eruption history
Detailed timeline
- 1090 (±60 yrs)VEI ?Geological estimate1090 – OngoingSE flank
External links
⚠ For reference only. Not for emergency response.