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Nature · Iran · summit-crater section · differing published references

Mount Damavand: terrain elevation and local relief

Mount Damavand uses an approximately 5,599-meter surface estimate in EGM2008 from Copernicus GLO-30. The bounded terrain section has about 2,944 meters of local relief above its lowest sampled point. Published summit surveys are separate references.

Mount Damavand, Iran · summit-crater section · differing published references. Highest sampled surface in the documented Copernicus terrain section · EGM2008: 5598.7 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.

5,599 m

Data-derived estimate
Measurement
Highest sampled surface in the documented Copernicus terrain section · EGM2008
Subject or version
Iran · summit-crater section · differing published references
In feet, rounded
18,368.6 ft (1 ft = 0.3048 m)
Compare in terrain mode

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Terrain boundary, base and datum
Vertical reference
EGM2008. Published surveys are separate; no datum conversion is applied.
Highest sampled surface
5598.7 m at 35.954444°, 52.110556°.
Local base
2654.5 m at 35.925556°, 52.170000°. Lowest sampled point within this bounded terrain section.
Section bounds in WGS84-G1150
West 52.048194°, east 52.170139°; south 35.923750°, north 35.986806°.
View and scale
Orthographic map section facing north. Equal horizontal and vertical map scales. Approximate grid spacing: 25.1 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

Hatam Chavari and colleagues’ EGU 2009 research abstract gives Damavand’s maximum elevation as 5,610 meters while describing a gravity, GPS and leveling profile to the summit. The Smithsonian Global Volcanism Program lists a different 5,670-meter reference. This Copernicus section reaches about 5,599 meters in EGM2008. The published disagreement remains visible; neither value is used to stretch the raster or claim an unverified conversion between reference systems.

The local-relief view subtracts the lowest sampled point in this section: 2654.5 meters at 35.925556° latitude, 52.170000° longitude. This produces about 2,944 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

Mount Damavand uses an approximately 5,599-meter surface estimate in EGM2008 from Copernicus GLO-30. The bounded terrain section has about 2,944 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 5,599-meter surface estimate stays independent of both the research abstract’s 5,610 meters and the Smithsonian’s 5,670 meters.

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

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