Elevation Finder — Altitude of Any Address or Point
Look up the elevation above sea level of any place on Earth. Search an address, city, or landmark, click anywhere on the map, or paste coordinates. Reports altitude in feet and meters, atmospheric pressure, oxygen percentage, and a comparable landmark for scale. Free, worldwide, no sign-up. Want your own current spot?
Elevation is the height of a point above mean sea level, in meters or feet. Search an address or click the map, and this tool looks up the altitude at that exact spot from a global terrain model in a second or two.
Elevation is decoded in your browser from AWS Terrain Tiles (Mapzen “terrarium” PNG encoding), which merges USGS 3DEP (~2 m vertical RMSE in the US and Hawaii), SRTM v3 (~9 m RMSE, 60°N–56°S), ArcticDEM, and GMTED2010 as a global fallback. Phone GPS altitude is much less reliable — a DEM lookup by horizontal position is the standard.
Yes. The map and the elevation data cover the entire Earth — every continent, every island, including ocean depths (negative values where applicable). Reverse geocoding for the place name is best in well-mapped countries.
Yes — no sign-up, no API key, no usage limits. The tiles come from the AWS Terrain Tiles open dataset and are decoded in your browser.
What is elevation, and what is my elevation right now?
Elevationis the height of a point on Earth's surface above (or below) mean sea level — the average height of the ocean. It is usually measured in meters (the international standard) or feet (common in the US and aviation). Sea level is the universal zero, so a city on the coast has an elevation near 0 m, the top of Mt Everest is +8,849 m, and the floor of Death Valley is –86 m.
What is my elevation right now?Tap the "Detect My Location" button at the top of the tool. Your phone or browser shares its GPS coordinates with the tool, which then looks up a worldwide elevation dataset (AWS Terrain Tiles, decoded in your browser) and returns your current altitude in 1–2 seconds. No sign-up, no app install, no waiting on a satellite altitude reading.
People look up elevation for all kinds of reasons: planning hikes, training for altitude events, dealing with altitude sickness, monitoring barometric pressure for cooking and scientific work, picking property at a flood-safe altitude, researching real estate, doing school geography projects, and just plain curiosity. Whatever your reason, this tool answers the question in one click.
How to find your elevation
Famous elevations for reference
A reference table of well-known places. Useful as a sanity check and for getting a feel for what different elevations mean.
| Place | Meters | Feet | Category |
|---|---|---|---|
| Mt Everest summit, Nepal/Tibet | 8,849 m | 29,032 ft | Extreme altitude |
| Mt Whitney, California | 4,421 m | 14,505 ft | Alpine |
| Pikes Peak, Colorado | 4,302 m | 14,115 ft | Alpine |
| La Paz, Bolivia (city) | 3,640 m | 11,942 ft | High mountain |
| Lhasa, Tibet (city) | 3,656 m | 11,995 ft | High mountain |
| Aspen, Colorado | 2,438 m | 8,000 ft | High mountain |
| Denver, Colorado (Mile-High City) | 1,609 m | 5,280 ft | Highland |
| Mexico City, Mexico | 2,240 m | 7,349 ft | High mountain |
| Madrid, Spain | 667 m | 2,188 ft | Rolling hills |
| Paris, France | 35 m | 115 ft | Coastal / sea level |
| New York, NY | 10 m | 33 ft | Coastal / sea level |
| Amsterdam, Netherlands | –2 m | –7 ft | Below sea level |
| Death Valley, California | –86 m | –282 ft | Below sea level |
| Dead Sea shore | –430 m | –1,411 ft | Below sea level |
How altitude affects the human body
The higher you go, the thinner the air gets. Atmospheric pressure drops by about 12% per 1,000 m of elevation gain, which means each breath delivers proportionally less oxygen. Air is still 21% oxygen by composition at any altitude — there's just less air per cubic meter.
| Elevation range | Effective O₂ vs sea level | Typical effects |
|---|---|---|
| 0 – 1,500 m (0 – 5,000 ft) | 83 – 100% | No physiological effect |
| 1,500 – 2,500 m (5,000 – 8,200 ft) | 74 – 83% | Slight breathlessness on exertion |
| 2,500 – 3,500 m (8,200 – 11,500 ft) | 65 – 74% | Acute mountain sickness possible |
| 3,500 – 5,500 m (11,500 – 18,000 ft) | 50 – 65% | Acclimatization required |
| 5,500 – 8,000 m (18,000 – 26,000 ft) | 36 – 50% | Severe hypoxia, no permanent residence |
| > 8,000 m | < 36% | Death zone — supplemental O₂ required |
This is also why food cooks differently at altitude (water boils at lower temperatures), why airplane cabins are pressurized (typical cabin = ~2,400 m), and why endurance athletes train high. The result panel in the tool shows the effective oxygen percentage and atmospheric pressure for whichever location you're looking at.
Who uses elevation lookups
1. Hikers, climbers, and outdoor planners
Trail planners look up trailhead and summit elevations to estimate vertical gain and difficulty. Hikers check the elevation of a campsite to plan layers and hydration. Climbers use it for altitude acclimatization scheduling.
2. Real estate and property research
Buyers in coastal or low-lying areas check elevation to understand flood risk, insurance rates, and long-term sea-level exposure. Mountain property buyers use it for snow-line estimates and access concerns.
3. Aviation and drone planning
Drone pilots check ground elevation to set safe flight altitudes (FAA rules are relative to launch elevation). Pilots check airport elevations and terrain along flight routes.
4. Cooking and baking at altitude
Bakers and cooks adjust recipes for altitude — water boils lower, leavening rises faster, sugar concentrates faster. The atmospheric pressure card gives the exact number you need for technical adjustments.
5. Sports and athletic training
Endurance athletes plan altitude camps, time-trial venues, and recovery zones using elevation data. Coaches reference altitude for training stress calculations and pacing.
6. Scientific fieldwork
Biologists, ecologists, climatologists, and geologists log elevation as a standard field for any sample or observation. Many ecological zones are elevation-defined (alpine, montane, subalpine).
7. Engineering and construction
Civil engineers reference elevation for grading, drainage, and equipment specifications. Telecom installers check tower elevations for line-of-sight calculations.
8. Education and curiosity
Teachers, students, and trivia fans use elevation lookups to learn world geography. The comparison-to-landmark card is a fun way to internalize the scale of mountains, valleys, and cities.
Methodology & data sources
Elevation data
Elevation is decoded in your browser from AWS Terrain Tiles (Mapzen “terrarium” PNG encoding), the same open dataset used by What Is My Elevation?. It merges USGS 3DEP (~2 m vertical RMSE in the contiguous US and Hawaii), SRTM v3 (~9 m RMSE, 30 m resolution, 60°N–56°S), ArcticDEM (north of 60°N), and GMTED2010 (~25–42 m) as a global fallback. US and Europe are typically within a few meters; remote polar and small-island areas can be off by tens of meters.
Map and basemap
The interactive world map is rendered with MapLibre GL JS using vector tiles from OpenFreeMap, based on OpenStreetMap data. No API key, no rate limits.
Address autocomplete & reverse geocoding
Address suggestions in the search box come from Photon, and the place name shown for each result comes from Nominatim — both built on OpenStreetMap.
Atmospheric pressure formula
Pressure at altitude is computed with the standard barometric formula for the ISA (International Standard Atmosphere) troposphere:
P(h) = P₀ · (1 − L·h / T₀)^(g·M / R·L) P₀ = 101.325 kPa (sea-level pressure) L = 0.0065 K/m (temperature lapse rate) T₀ = 288.15 K (sea-level temperature) g = 9.80665 m/s² (gravity) M = 0.0289644 kg/mol (molar mass of air) R = 8.31432 J/mol·K (universal gas constant) exponent ≈ 5.255
The "effective oxygen percentage" is the partial pressure of oxygen at altitude divided by the partial pressure at sea level — equivalent to the ratio of total pressures, since air composition is constant.
Limitations & accuracy notes
- Resolution varies by region. AWS Terrain Tiles are ~30 m globally (SRTM) and finer over the US (USGS 3DEP). For sub-cell features (a building rooftop, a steep slope edge), the reported elevation is averaged across the grid cell.
- Vertical accuracy varies by source — roughly ~2 m in the contiguous US and Hawaii (3DEP), ~9 m elsewhere (SRTM), and tens of meters in remote polar or small-island areas (GMTED2010 fallback).
- Online-only. The map tiles, GPS lookup, address search, and terrain tiles all require an internet connection.
- GPS altitude is ignored.The tool uses GPS only for the horizontal position, then looks up elevation in a DEM — because phone GPS vertical accuracy is poor (±10–50 m). This is intentional and gives a more reliable answer than the device's own altitude reading.
- No bathymetry. Elevation over the ocean is reported as 0 m (the surface), not the depth below. For ocean depth, use a dedicated marine chart or the GEBCO grid.
- Pressure formula is theoretical. The barometric formula assumes the International Standard Atmosphere. Actual pressure at altitude varies with weather by ±5%.
- Not for legal or surveying use. For property surveys, flood-zone determinations, or engineering plans, use authoritative sources: USGS 3DEP in the US, national survey agencies elsewhere.
Glossary
- Elevation
- The height of a point on Earth's surface above (or below) a fixed reference, usually mean sea level. Measured in meters or feet.
- Altitude
- Often used interchangeably with elevation, but technically refers to height above ground (e.g. an aircraft's altitude) or above a specific reference. Aviation distinguishes "altitude" (above sea level) from "AGL" (above ground level).
- Mean sea level (MSL)
- The average height of the ocean's surface, used as the standard zero point for elevation worldwide. Specific national datums may differ slightly.
- Digital Elevation Model (DEM)
- A raster grid that stores the elevation of every point on Earth at a fixed resolution. Common DEMs: Copernicus (30 m / 90 m), SRTM (30 m / 90 m), ASTER GDEM (30 m), USGS 3DEP (1 m / 10 m, US only).
- Geoid
- The actual shape of mean sea level, distorted by Earth's gravity field. The geoid differs from a perfect ellipsoid by ±100 m worldwide. Modern elevation products are referenced to the geoid (orthometric heights).
- Ellipsoid
- A mathematical model of Earth's shape used as a reference for GPS coordinates. WGS84 is the most common. Heights above the ellipsoid (HAE) differ from heights above the geoid by 10–80 m depending on location.
- Vertical datum
- A reference surface for measuring elevation. Common datums: NAVD88 (North America), EVRF2000 (Europe), MSL. This tool reports orthometric heights tied to mean sea level.
- Atmospheric pressure
- The weight of the column of air above a point. At sea level, standard pressure is 101.325 kPa (1013.25 hPa, 29.92 inHg). It drops by about 12% per 1,000 m of elevation gain.
Related tools and resources
Standing somewhere and want your elevation right now? Use What Is My Elevation? — the GPS-first companion to this tool: tap once and it reads the elevation at your current location in feet and meters, no address needed.
Planning a route rather than a single point? The Elevation Profile tool charts the elevation gain and loss along a path you draw on the map.
New to this? Our guide How to Find Elevation on Google Maps walks through the Terrain layer, Google Earth, and route profiles — and where these tools are faster.
To find latitude and longitude for any location, use the Latitude & Longitude Finder. To measure between two points, use Distance Between Two Places. For radius circles around a point, use the Map Radius Tool. To find the time zone at any point, use the Time Zone Finder. Browsing the US by state? Each state has a county directory:
Frequently asked questions
Elevation data from AWS Terrain Tiles (Mapzen terrarium encoding), merging USGS 3DEP, SRTM v3, ArcticDEM, and GMTED2010. Map rendering by MapLibre GL JS with OpenFreeMap tiles. Address autocomplete by Photon and reverse geocoding by Nominatim. Atmospheric pressure computed with the standard ISA barometric formula.