Elevation Map: Find the Elevation of Any Place

Last updated 2026-10-21 · MapElevation

How to use this elevation map

Start with the location you actually want to inspect. A broad map view is useful for seeing mountain ranges, plains, and coastlines, while a closer view helps you choose a specific point. The number in the result belongs to that selected point, rather than to every place currently visible on screen. Roads and place labels help with orientation; they are not measurements of the land underneath them.

1. Move or zoom the map to a familiar area, or submit a complete US address in the search field.
2. Select the desired point and wait for its elevation result. If you searched an address, check where the matched pin landed.
3. Read the height in feet or metres, together with the model, original resolution, and vertical reference.
4. Use a related tool when your question needs coordinates, a flood-zone record, or a more detailed explanation of the reference.

The map starts over the United States, but terrain point queries are available globally within the map projection’s coverage. A loading indicator distinguishes an active query from an empty result. If a request takes too long, use Retry rather than assuming that a blank map means no terrain exists. The written guidance remains available while the map or an external service is loading.

What the colors and shading mean

The elevation color layer assigns a consistent color ramp to terrain heights. Read it against the legend in metres: greener lowlands transition through warmer upland tones toward the highest terrain. The ramp is a visual summary, so click a point for the actual reported value instead of estimating a precise number from a blended color. You can turn the colors off when roads and local labels are easier to read without them.

Hillshade adds simulated light and shadow to make slopes and ridges easier to recognise. A dark patch is not necessarily low land, and a bright patch is not necessarily high land. Their appearance also depends on slope direction and the simulated lighting. The ordinary basemap has colors for water, parks, and other mapped features; those colors should not be interpreted as height measurements. Optional 3D terrain changes the view, not the source accuracy.

Find elevation by address, coordinates, or current location

Choose the input method that matches the information you have. The address elevation finder explains address matching and why a pin can fall on a road instead of a building. US addresses currently use the Census service; worldwide address search requires an additional provider configuration. You can still inspect locations elsewhere by selecting the map.

The elevation finder is intended for latitude and longitude, including coordinates copied from a GPS receiver. It makes coordinate order and valid ranges explicit. If your question is what is my elevation, use browser location after choosing to grant access. The site obtains a horizontal position and looks up a surface height; it does not treat a device’s GPS altitude as the map elevation.

Explore US flood zones and sea level rise

A high or low elevation alone cannot answer whether a home is in a FEMA flood zone. Use the flood zone by address lookup for the relevant mapped information, then consult the flood zone codes guide to interpret the result. A base flood elevation by address query addresses a different quantity from the surface elevation shown here.

For coastal exploration, the sea level rise map includes a bounded illustrative connected-water demonstration. It is a simplified scenario rather than a forecast for a property or a particular year. The height above sea level guide explains why a geoid height and a local tidal reference are not interchangeable. Read the Flood Zone X meaning and Flood Zone AE meaning guides when those codes appear in a lookup. These distinctions matter more than the number of decimal places shown in a result.

Create and read contour maps

Contours connect equal modeled elevations and can make terrain structure clearer than isolated point readings. Open the contour map generator to choose an interval and inspect lines over the basemap. Tightly spaced contours indicate a faster change in the modeled surface; widely spaced contours indicate a gentler change. A line derived from a surface model may still be affected by vegetation, structures, and resampling.

Choose the right next step

For general exploration, compare nearby points and keep the data label in view. For a building, planning application, or insurance question, collect the specific records required for that decision. Our elevation certificate guide explains surveyed building information, and the LOMA flood guide explains what a map amendment review needs. The elevation data accuracy guide lists active sources and limitations so that a visual impression does not become an unsupported conclusion.

A recorded point-query example

At latitude 39.7392, longitude −104.9903, a Denver-area point query on 2026-10-21 decoded a GLO-30 terrain-tile sample of 1,596.5 metres. The result card rounds that to 1,597 m or 5,238 ft. The browser’s feet readout was checked against the independent tile decode. The saved example record includes the tile URL, pixel, RGB values, and file checksum; it is a surface-model observation in the EGM2008 reference, not a surveyed building height or an independent vertical-accuracy assessment.