Reclus
Pyroclastic cone in Chile
Key Facts
Elevation
1,403 m (4,603 ft)
Type
Pyroclastic cone
Location
-50.940°, -73.580°
Region
Austral Andean Volcanic Arc
Rock Type
Dacite
Tectonic Setting
Subduction zone
Location
Loading map...
Overview
Reclus, the source of several Patagonian Holocene tephra layers, was recognized to be an independent volcanic edifice in 1987. The volcano consists of a large dacitic pyroclastic cone with a crater about 1 km in diameter. As many as six tephra layers overlie a peat layer dated at 3,780 years before present.
Research has also revealed evidence for eruptions in the 19th and early 20th centuries.
Volcanic Hazards & Risk Assessment
Primary Hazards
Risk Level
Geological Composition & Structure
Rock Types
Tectonic Setting
Age & Formation
Eruption Statistics & Analysis
| Metric | Value | Global Ranking | Significance |
|---|---|---|---|
| Total Recorded Eruptions | Unknown | Low | Moderately active volcano |
| Maximum VEI | VEI Unknown | Minor | Local impact potential |
| Recent Activity | 118 years ago | Historical | Historically active |
Monitoring & Alert Status
Monitoring Networks
Current Status
Nearby Volcanoes in South America Volcanic Regions
Quick Info
- •Smithsonian ID: 358063
- •Evidence: Eruption Observed
- •Epoch: Holocene
About the Photo
Amalia Glacier flows around the northern flank of Reclus in the Southern Patagonia Ice Field, shown in this 27 February 2018 PlanetScope satellite image (N is at the top; this image is approximately 8 km across). The flanks are heavily eroded and there is a landslide deposit from the northern flank on the glacier surface.
Satellite image courtesy of Planet Labs Inc., 2018 (https://www.planet.com/).
Authority Sources
Related Volcanoes
Basic Information
This page shows basic data from the Smithsonian Global Volcanism Program. For more detailed information, visit the official Smithsonian page.