Tilocalar
Lava cone(es) in Chile
Key Facts
Elevation
3,109 m (10,200 ft)
Type
Lava cone(es)
Location
-23.970°, -68.130°
Region
Central Andean Volcanic Arc
Rock Type
Andesite / Basaltic Andesite
Tectonic Setting
Subduction zone
Location
Loading map...
Overview
Two small eruptive vents that produced lava flows lie about 3 km apart in the Callejón de Tilocálar area. Lava flows overlie Pliocene ignimbrites and were considered to be of Pleistocene-Holocene age by González-Ferrán (1995). The larger feature, Tilocálar Sur, lies about 3.
5 km SW of Tilocálar Norte. Four basaltic andesite to andesitic lava flows originated from Tilocálar Sur, and an explosion crater lies a kilometer to the south. The Tilocálar Norte lies near the eastern wall of the Callejón de Tilocálar and produced lava flows that traveled primarily to the north.
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 | Unknown | Historical | Historically active |
Monitoring & Alert Status
Monitoring Networks
Current Status
Nearby Volcanoes in South America Volcanic Regions
Quick Info
- •Smithsonian ID: 355105
- •Evidence: Evidence Uncertain
- •Epoch: Holocene
About the Photo
The Tilocalar volcanic center is shown here in this 25 November 2019 Sentinel-2 satellite image (N is at the top), with Tilocalar Norte near the center of the image and Tilocalar Sur to the SW. Tilocalar Norte erupted a single 4.3-km-long lava flow while Tilocalar Sur produced four lava flows. They overlie the Talabre ignimbrite.
Satellite image courtesy of Copernicus Sentinel Data, 2019.
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.