Peak Elevation Lookup
Click peaks or ridgelines to read elevation from global terrain data.
By Aryan Khan, Founder & Editor · Updated October 2026
For example, clicking Everest returns the neighbourhood of 8,849 m — the terrain model's grid slightly softens knife-edge summits, while the surveyed figure stands at 8,848.86 m.
How to use Peak Elevation Lookup
Click the summit; read its height:
The Peak Elevation Lookup reads the elevation of mountain peaks and ridgelines from global terrain data: click a summit and get its height in feet and metres. Use it to check the peak across the valley, settle which of two summits is higher, and put numbers on the skyline.
- 1Click the summit area.
- 2Read elevation.
What people use Peak Elevation Lookup for
1. Naming the skyline
Every viewpoint has an unidentified peak. Click it here, then argue about whether it is worth climbing — the route's full shape belongs to the Elevation Profile.
2. Expedition and trek research
Passes and subsidiary peaks rarely make the brochures; their heights from terrain data shape acclimatisation plans before the guidebooks come out.
3. Which summit is higher?
Neighbouring tops are misjudged by eye constantly — foreshortening flatters the nearer one. The clicks end the argument with numbers.
4. Photography captions
A named, correctly-heighted summit captions a landscape photo like a professional. Pair with the Elevation Finder for the valleys between.
Worked examples
Global terrain grids sample every ~30 m and average cells; a sharp summit's cell includes its shoulders, so model readings on pointy peaks run slightly low. Everest's cell will not read the full 8,848.86 m — the survey's theodolite-and-GNSS figure is the record; the model is the scout.
A 1,345 m Ben Nevis dominates its skyline more than a 3,000 m shoulder of a giant does — height is absolute, presence is relative. The lookup gives the absolute number; the eye reports the rest.
Famous summits (published survey heights)
The reference shelf — compare your click against these.
| Peak | Height |
|---|---|
| Everest (Asia) | 8,848.86 m / 29,032 ft |
| K2 (Asia) | 8,611 m / 28,251 ft |
| Kilimanjaro (Africa) | 5,895 m / 19,341 ft |
| Denali (North America) | 6,190 m / 20,310 ft |
| Mont Blanc (Europe) | 4,808 m / 15,774 ft |
| Ben Nevis (Britain) | 1,345 m / 4,413 ft |
Mont Blanc's figure breathes by a couple of metres with its summit snow cap between surveys. Rock summits hold still; snow summits negotiate.
Terrain profiles show the shape of the land, but DEM resolution limits small features
An elevation profile helps visualize climbs, descents, ridges and valleys along a route or line. It is useful for hiking, cycling, radio-path context and comparing alternative routes. The values come from a digital elevation model, so they represent sampled terrain rather than a surveyed measurement at every step.
Narrow ridges, buildings, trees and small cuttings can disappear at coarse grid resolution, especially in steep terrain. Use the profile to understand broad terrain shape; engineering, construction and official elevation work require higher-resolution authoritative data.
How to interpret the result
The most common errors come from using a correct result to answer the wrong geographic question. Keep these points in mind for Peak Elevation Lookup:
- Include your height inputs explicitly (eye height, mast height, deck level) when sharing visibility results: the same hill answers differently for a child, an adult and a 10 m antenna, and unstated heights make numbers unreproducible.
- Treat climate and hardiness outputs as 30-year character, not this year's weather: a zone tells you what winters usually allow, and microclimates — walls, slopes, urban heat — shift a real garden half a zone either way.
Limits & appropriate use
Terrain intelligence carries one dominant limit: the model sees bare earth at ~90 m spacing with metres of vertical error, and is blind to canopies, walls and wires. Every downstream answer inherits it — profiles show terrain truth with noisy amplitude, line-of-sight verdicts are pending trees, horizons assume open ground, and solar radiation averages assume an unshaded panel. The second limit is temporal: climate letters and hardiness zones are thirty-year character, not this year's behaviour, and seismicity is a mood, not a hazard model. Each result here is printed with its recipe precisely so these boundaries travel with the number.
The value proposition is screening-grade truth at zero cost: orientation for sites, gardens, antennas, shoots and curiosity, with the upgrade points clearly marked. When money or safety attaches to the answer — tower siting, flood insurance, structural shading, avalanche terrain — the escalation is professional: licensed survey, certified shade studies, regulatory flood determinations and geological hazard services. A good free tool makes that ladder visible instead of pretending to be the top of it.
- Construction and tower siting → licensed topographic survey.
- Flood decisions → regulatory determinations (FEMA/FIRM in the US).
- Solar finance → certified shade and production studies.
Data & methodology
The workspace queries Open-Meteo for the elevation of one selected point; it does not generate a route or peak elevation profile.
For source details, licences and model limitations, see Data Sources and Methodology.
Key terms worth knowing
- Refraction coefficient
- The standard 0.13 factor bending sightlines over the curvature.
- Antipode
- The diametrically opposite point; latitude flips, longitude shifts 180°.
Editorial guidance: MapBench explains the method and limitations so the tool can be used as a transparent reference, not as a black-box answer. For legal boundaries, safety-critical routing, surveying, engineering, regulated decisions or official statistics, verify the result with the responsible authority or a qualified professional.
Category: Earth Science. Results are intended for everyday analysis and planning unless a page explicitly states otherwise.
Method, assumptions & limits
- This tool’s method
- The workspace queries Open-Meteo for the elevation of one selected point; it does not generate a route or peak elevation profile.
- Before relying on the answer
- Check the location, height units and any model options shown by this calculator. A terrain lookup and a geometric Earth model answer different questions.
- What the result cannot establish
- Local terrain, atmospheric conditions and source resolution can matter more than numerical rounding. Do not use a planning result for safety-critical work.
Coverage: Worldwide. Search, basemap and external data requests may use third-party services; browser-based does not mean every operation is offline. Read the source and licence notes, calculation methodology and privacy policy. If a result looks inconsistent, report a correction with the inputs and mode used.
Frequently asked questions
Clear answers about the calculation, accuracy and appropriate use.
Named peak list?
Elevation at a point — peak names come from map labels and geocoders.
Is this suitable for engineering or legal decisions?
Treat the result as planning or educational context unless the page explicitly says otherwise. Engineering, hazard and legal decisions should use authoritative specialist data.
Why can terrain data differ between sources?
Elevation and earth datasets vary in resolution, collection date and processing method. Small local features may not be represented equally.
Can I verify the data source?
Yes. MapBench documents major providers and methodology on the Data Sources and Methodology pages.
Why does the summit read lower than the book value?
Grid averaging: the model's cell containing the summit also contains descending ground. The sharper the peak, the larger the shave — a known, bounded effect of ~30 m data.
Ridges and cols too?
Yes — any clicked point reads the terrain height there, so the col between two peaks (the number that defines prominence) is one click away.
Underwater peaks?
The terrain model's ocean is sea level; seamounts need bathymetry this dataset does not carry. Land peaks only, honestly stated.
Volcanoes that changed height?
Eruptions rewrite summits (St Helens lost 400 m in 1980). The model reflects its survey era; recently remodelled volcanoes may disagree with it — news beats data there.
Feet and metres?
Both shown together, converted exactly (1 ft = 0.3048 m).
Highest peak per continent?
The Seven Summits shelf: Everest, Aconcagua (6,961 m), Denali, Kilimanjaro, Elbrus (5,642 m), Vinson (4,892 m), and Puncak Jaya or Kosciuszko depending on the list's continent convention.
Can I trust it for a first ascent claim?
No — first-ascent and record claims live on surveyed GNSS measurements. This page is for research, captions and curiosity, and says so.
Named peak database?
The lookup reads terrain at your click rather than a gazetteer — an unnamed summit still gets its height, which gazetteers cannot offer.
Related tools and resources
Any point: the Elevation Finder; routes across them: the Elevation Profile; the climb's steepness: the Relief Ratio Calculator.
More free tools
Sources, methodology & editorial trust
- ✓ Browser-first processing where supported
- ✓ External sources are documented
- ✓ No account required for public tools
- ✓ Review data sources
Calculations are documented with their assumptions, limitations and source context rather than presented as unexplained answers.
Reviewed and maintained by Aryan Khan, Founder & Editor of MapBench.
Part of our elevation & terrain hub
Peak Elevation Lookup sits in the elevation & terrain cluster, alongside 40 other tools that answer neighbouring questions with different methods or datasets.
You may also need
When this answer is only part of the job, these clusters cover the next step.
Read the guide behind this tool
How to Find Elevation on Google Maps — Check the elevation of any spot on Google Maps — desktop, mobile, and the precise method with exact numbers.