My Elevation
Find the elevation of your current location or any point on the map. View elevation above mean sea level in metres and feet, with transparent dataset sources, vertical datums, and accuracy specifications.
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How to Find Your Elevation Above Sea Level
Follow these simple steps to measure the elevation of your physical position or inspect topography worldwide.
Select Your Point
Click "Use My Location", search any worldwide address or landmark, or click anywhere on the interactive map.
Validate Coordinates
Coordinates are validated against international WGS 84 geographic limits (-90° to 90° latitude, -180° to 180° longitude).
Query Digital Elevation Model
Coordinates are queried against the Copernicus DEM GLO-90 raster model to retrieve true terrain height relative to the EGM2008 geoid.
Inspect Metres & Feet
View your elevation converted accurately into metres (m) and feet (ft), inspect topographic contours, and copy or share results.
Understanding Geographic Elevation and Digital Elevation Models
Explore how modern satellites measure planetary topography and why vertical elevation differs from GPS altitude.
Elevation vs. Altitude vs. Height
In geodesy, these terms describe different vertical reference frames:
- Elevation (Orthometric Height): The vertical distance of the fixed terrestrial ground surface above the Earth's mean sea level geoid.
- Altitude: The vertical distance of an unattached object (such as an aircraft or weather balloon) above sea level or ground.
- Height (AGL): The vertical height of a structure (such as a 400m skyscraper) measured from the local ground surface beneath it.
Digital Surface Models (DSM) vs. Bare Earth
Copernicus DEM GLO-90 is a Digital Surface Model (DSM), not a bare-earth Digital Terrain Model (DTM). It was generated from radar interferometry by the TanDEM-X and TerraSAR-X satellite missions:
- First Reflective Surface: Radar waves bounce off the tops of forest canopies, dense vegetation, and built structures. In woodlands, elevation reflects tree crown heights rather than ground soil.
- Global Coverage: Spans from the South Pole to the high Arctic (unlike NASA's legacy SRTM which ended at ±60° latitude).
Vertical Datums: Geoid vs. Ellipsoid
The Earth is not a smooth sphere or simple geometric ellipsoid. Mass variations in the planet's crust create localized gravitational anomalies:
- EGM2008 Geoid: The equipotential gravitational surface representing true mean sea level. This is the vertical datum used by Copernicus DEM.
- WGS 84 Ellipsoid: A smooth mathematical ellipsoid used by raw GPS satellites. Ellipsoidal height can differ from sea level by up to 100 metres!
Resolution vs. Accuracy (No Point Guarantees)
It is essential to understand the difference between spatial resolution and statistical dataset accuracy:
- 90m Grid Footprint: Each raster pixel represents an 8,100 m² cell. Microtopography and sharp crests are smoothed within the cell.
- Statistical Benchmark (< 4m LE90): The global error statistic is an aggregated benchmark across validation sites, not an individual point guarantee. Steep mountain cliffs and dense forest canopies can have vertical discrepancies of 10 to 15 metres or more.
- No False Precision: Displaying whole metres or feet reflects physical sensor realities.
Why Smartphone Altimeters Vary
If your phone displays a different number, consider the sensing mechanism:
- Vertical Dilution of Precision (VDOP): GPS satellites are all above the horizon, creating geometry where vertical errors are 2 to 3 times larger than horizontal errors.
- Barometer Drift: Smartphone pressure sensors infer height from air pressure. A passing thunderstorm can alter barometric readings by 20 to 50 metres without physical movement.
Depressions vs. Ocean Conventions
Elevation values naturally span both positive and negative values:
- Land Below Sea Level: Geological endorheic rift depressions (like Badwater Basin at -86m or the Dead Sea at -430m) are genuine terrestrial surfaces below mean sea level.
- Ocean 0m Convention: Open maritime waters report 0 metres representing the EGM2008 geoid datum surface. The Copernicus DEM is an overland terrestrial model and does NOT measure underwater seafloor depth (bathymetry).
Worldwide Elevation Reference Benchmarks
Compare common landmarks across metres and feet using the international conversion factor (1 m = 3.28084 ft):
| Geographic Landmark | Significance | Elevation (Metres) | Elevation (Feet) | Datum Status |
|---|---|---|---|---|
| Mount Everest (Sagarmatha) | Highest mountain peak on Earth | 8,849 m | 29,032 ft | Above sea level |
| La Paz, Bolivia | Highest administrative capital city | 3,640 m | 11,942 ft | Above sea level |
| Denver, Colorado | The "Mile High City" | 1,609 m | 5,280 ft | Above sea level |
| Global Mean Sea Level | Equipotential geoid reference surface | 0 m | 0 ft | Datum baseline |
| Amsterdam, Netherlands | Reclaimed polder land below sea level | -2 m | -7 ft | Below sea level |
| Badwater Basin (Death Valley) | Lowest land point in North America | -86 m | -282 ft | Below sea level |
| Dead Sea Shore (Jordan / Israel) | Lowest exposed land on Earth | -430 m | -1,411 ft | Below sea level |
Accuracy & Limitations
Calculation & Data Accuracy
- Copernicus DEM GLO-90 is a Digital Surface Model (DSM) with ~90m horizontal spatial resolution (3 arc-seconds at the equator). It samples radar reflections off surface canopy crowns and built structures rather than bare-earth LiDAR ground models.
- Global statistical validation reports absolute vertical accuracy < 4 meters LE90 (Linear Error 90%) across gentle terrain. These are aggregated regional benchmarks and do not guarantee point-level accuracy on individual steep mountain slopes or dense vegetation.
- Open ocean maritime coordinates report 0 meters as a datum convention (EGM2008 mean sea-level geoid baseline); the Copernicus DEM does not measure underwater seafloor bathymetry or ocean water depth.
- Valid negative elevations (e.g. Badwater Basin at -86m, Dead Sea at -427m) reflect genuine dry terrestrial land rifts located below global mean sea level, completely distinct from water bodies.
- Smartphone GPS chips measure ellipsoidal height relative to WGS 84, which can deviate from the EGM2008 geoid by up to 100 meters due to regional planetary gravity variations.
Important Limitations & Disclaimers
- Do not use for: Civil engineering construction staking, foundation grading, and legal boundary surveys requiring certified sub-centimeter RTK-GPS or geodetic leveling.
- Do not use for: Instrument Flight Rules (IFR) terrain avoidance avionics and low-altitude aircraft clearance navigation.
- Do not use for: Floodplain determination for formal insurance underwriting without certified LiDAR or FEMA Flood Insurance Studies.
Data Sources & Technologies
Global 90-meter digital surface model derived from TanDEM-X radar interferometry, queried directly via self-hosted raster lookup
Full, Free & Open license (COP-DEM-GLO-90-F) permitting commercial use with attribution. Self-hosted raster lookup eliminates external API dependencies and subscription costs.
Standard browser-level device location capture
Strictly executed with explicit user permission in browser.
Frequently Asked Questions
Everything you need to know about finding your elevation above sea level on GEO MAP TOOLS.
How do I find the elevation of my current location?
Click the 'Use My Location' button above. When prompted by your browser, grant location permission. GEO MAP TOOLS captures your coordinates and queries the Copernicus Digital Elevation Model (GLO-90) via an internal server service to display your elevation above mean sea level in both metres and feet.
What is the difference between elevation, altitude, and height?
Elevation refers specifically to the vertical distance of the fixed ground surface above mean sea level (orthometric height relative to the geoid). Altitude describes the vertical position of an airborne or flying object (like an airplane or weather balloon) above sea level. Height (or height above ground) measures the vertical extent of a structure, such as a building or tower, relative to the immediate ground surface beneath it.
What dataset does this tool use to calculate elevation?
This tool uses the Copernicus Digital Elevation Model (GLO-90) dataset produced by the European Space Agency (ESA) and Airbus Defence and Space, queried directly via a self-hosted elevation lookup service under the official COP-DEM-GLO-90-F Full, Free & Open license. Copernicus DEM GLO-90 is a global Digital Surface Model derived from satellite radar interferometry (TanDEM-X and TerraSAR-X).
What is a Digital Surface Model (DSM) and how does it affect accuracy?
Copernicus GLO-90 is a Digital Surface Model (DSM), not a bare-earth Digital Terrain Model (DTM). Satellite radar waves reflect off the first physical surface encountered — including dense forest canopies, tree crowns, and built urban structures. In dense woodlands, the reported elevation reflects tree canopy heights rather than bare soil, and in metropolitan centers, it can reflect building rooftops.
Does the dataset guarantee point-level elevation accuracy?
No. While global validation reports an aggregated absolute vertical accuracy of less than 4 metres LE90 (Linear Error 90%) on gentle terrain, these are statistical benchmarks and do not guarantee point-level accuracy at any individual coordinate. Accuracy can deviate by 10 to 15 metres or more on steep mountain slopes (> 20°) or multi-tiered vegetation canopies.
What are the commercial and licensing terms for this service?
The elevation data is provided under the official 'Licence for COP-DEM-GLO-90-F Global 90m Full, Free & Open', which explicitly permits free use for commercial applications including ad-supported web tools, with appropriate attribution to the European Space Agency (ESA) and the Copernicus Programme. By implementing a self-hosted raster query engine directly against the open dataset, GEO MAP TOOLS operates without external API rate limits, paywalls, or third-party subscription dependencies.
What does an elevation of 0 m in the open ocean mean?
In the open ocean, a reported elevation of 0 m is a datum baseline convention representing the EGM2008 mean sea-level geoid surface. Copernicus DEM is an overland terrestrial elevation dataset and does NOT measure underwater bathymetry (seafloor depth). Never interpret an ocean reading of 0 m as a measurement of the seabed floor.
Can elevation be below sea level (negative numbers)?
Yes. Depressions and dry geological rift basins located below global mean sea level have valid negative elevation values. Famous examples include Badwater Basin in Death Valley, California (-86 m / -282 ft) and the shores of the Dead Sea in Jordan/Israel (-430 m / -1,411 ft), which is the lowest exposed dry land on Earth.
How are metres converted to feet?
Elevation in feet is calculated using the international foot definition: 1 metre = 3.280839895013123 feet (standard 1 foot = 0.3048 metres exactly). For example, 1,000 metres equals approximately 3,281 feet.
Why might my smartphone GPS altimeter report a different number?
Consumer smartphone GPS chips measure ellipsoidal height relative to the WGS 84 mathematical ellipsoid, which can differ from true mean sea level (the geoid) by up to 100 metres depending on regional planetary gravity variations. Furthermore, satellite geometry produces vertical positioning errors 2 to 3 times greater than horizontal errors, and phone barometer sensors fluctuate with changing weather fronts.
Does GEO MAP TOOLS store or track my GPS coordinates?
No. GEO MAP TOOLS does not store, log, or track your coordinates in any database. To look up elevation, coordinates are processed solely in volatile memory by our self-hosted server service during your active session and are never saved to disk or tied to user profiles.
Can I share a specific elevation point with someone?
Yes. Click 'Share' to copy a direct coordinate link (e.g., '?lat=39.7392&lng=-104.9903'). When opened, the tool restores the coordinates and queries elevation without prompting the recipient for device location permissions.
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