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Nature · Chile · summit-crater terrain without an eruption overlay

Villarrica: terrain elevation and local relief

Villarrica uses an approximately 2,857-meter surface estimate in EGM2008 from Copernicus GLO-30. The bounded terrain section has about 1,862 meters of local relief above its lowest sampled point. Published summit surveys are separate references.

Villarrica, Chile · summit-crater terrain without an eruption overlay. Highest sampled surface in the documented Copernicus terrain section · EGM2008: 2857.1 meters, data-derived estimate.
Data-derived neutral shaded surface, looking north with a horizontal orthographic camera. Horizontal and vertical scales are equal. Lower and surrounding terrain is omitted; fine summit details, vegetation and structures depend on the surface dataset. No photograph is stretched to a summit elevation.

2,857 m

Data-derived estimate
Measurement
Highest sampled surface in the documented Copernicus terrain section · EGM2008
Subject or version
Chile · summit-crater terrain without an eruption overlay
In feet, rounded
9,373.6 ft (1 ft = 0.3048 m)
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Terrain boundary, base and datum
Vertical reference
EGM2008. Published surveys are separate; no datum conversion is applied.
Highest sampled surface
2857.1 m at -39.421111°, -71.939722°.
Local base
994.7 m at -39.388611°, -72.003056°. Lowest sampled point within this bounded terrain section.
Section bounds in WGS84-G1150
West -72.003194°, east -71.875417°; south -39.451528°, north -39.388472°.
View and scale
Orthographic map section facing north. Equal horizontal and vertical map scales. Approximate grid spacing: 23.9 m east-west and 30.8 m north-south. Lower and surrounding terrain omitted.

produced using Copernicus WorldDEM-30 © DLR e.V. 2010-2014 and © Airbus Defence and Space GmbH 2014-2018 provided under COPERNICUS by the European Union and ESA; all rights reserved

A little more perspective

The Smithsonian Global Volcanism Program lists Villarrica at 2,847 meters. This Copernicus section reaches approximately 2,857 meters in EGM2008, numerically higher than the published reference. That difference is not interpreted as new volcanic growth. The older surface model depicts the bounded cone and slopes; it adds neither a lava lake depth nor the height of a plume above the rim.

The local-relief view subtracts the lowest sampled point in this section: 994.7 meters at -39.388611° latitude, -72.003056° longitude. This produces about 1,862 meters of relief within the stated boundary. It is not a universal mountain base, a route’s total ascent, or topographic prominence.

The rendered surface uses the public 2021 Copernicus release, primarily based on TanDEM-X observations from 2011–2015 with infill from other sources. It is a surface model rather than a current bare-earth survey. Neutral shading explains the geometry without claiming a snow season or photographic ground texture. No datum conversion or summit correction is applied.

Quick facts

Villarrica uses an approximately 2,857-meter surface estimate in EGM2008 from Copernicus GLO-30. The bounded terrain section has about 1,862 meters of local relief above its lowest sampled point. Published summit surveys are separate references.

For a presentation or a research note, include the subject, the measurement definition, and the measurement used. A picture alone cannot explain those choices. The comparison guide explains how to export an image and its source notes together.

Sources and measurement notes

The approximately 2,857-meter terrain sample and 2,847-meter Smithsonian listing remain separate. A plume’s altitude would be a different measurement.

Source review recorded . Maintained by Ishan Karunaratne. Suggest a correction with a source and the exact measurement being compared.

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